Search

Your search keyword '"Rousakis, G."' showing total 113 results
Start Over Author "Rousakis, G."
113 results on '"Rousakis, G."'

1. Geomorphology, Geological Structure, Active Tectonics, and Basin Formation in the Aegean Sea

Author

Sakellariou, D., Rousakis, G., Drakopoulou, P., Tsampouraki-Kraounaki, K., Morfis, I., Panagiotopoulos, I., Livanos, I., Loukaidi, V., Kyriakidou, C., Manta, K., Lykousis, V., Anagnostou, Christos L., editor, Kostianoy, Andrey G., editor, Mariolakos, Ilias D., editor, Panayotidis, Panayotis, editor, Soilemezidou, Marina, editor, and Tsaltas, Grigoris, editor

Published
2024
Full Text
View/download PDF

5. Evolution of the North Anatolian Fault from a diffuse to a localized shear zone in the North Aegean Sea during the Plio-Pleistocene

Author

Rodriguez, M, primary, Sakellariou, D, additional, Gorini, C, additional, Janin, A, additional, D'Acremont, E, additional, Pourhiet, L Le, additional, Chamot-Rooke, N, additional, Tsampouraki-Kraounaki, K, additional, Morfis, I, additional, Rousakis, G, additional, Henry, P, additional, Lurin, A, additional, Delescluse, M, additional, Briole, P, additional, Rigo, A, additional, Arsenikos, S, additional, Bulois, C, additional, Fernández-Blanco, D, additional, Beniest, A, additional, Grall, C, additional, Chanier, F, additional, Caroir, F, additional, Dessa, J-X, additional, Oregioni, D, additional, and Nercessian, A, additional

Published
2023
Full Text
View/download PDF

6. Evolution of the North Anatolian Fault from a diffuse to a localized shear zone in the North Aegean Sea during the Plio-Pleistocene

Author

Rodriguez, M, Sakellariou, D, Gorini, C, Janin, A, D'Acremont, E, Le Pourhiet, L, Chamot-rooke, N, Tsampouraki-kraounaki, K, Morfis, I, Rousakis, G, Henry, P, Lurin, A, Delescluse, M, Briole, P, Rigo, A, Arsenikos, S, Bulois, C, Fernández-blanco, D, Beniest, A, Grall, C, Chanier, F, Caroir, F, Dessa, J-x, Oregioni, D, Nercessian, A, Rodriguez, M, Sakellariou, D, Gorini, C, Janin, A, D'Acremont, E, Le Pourhiet, L, Chamot-rooke, N, Tsampouraki-kraounaki, K, Morfis, I, Rousakis, G, Henry, P, Lurin, A, Delescluse, M, Briole, P, Rigo, A, Arsenikos, S, Bulois, C, Fernández-blanco, D, Beniest, A, Grall, C, Chanier, F, Caroir, F, Dessa, J-x, Oregioni, D, and Nercessian, A

Abstract

Summary The North Anatolian Fault is the ∼1200-km-long active continental transform boundary between Anatolia and Eurasia. This strike-slip system initiated around 10-12 Ma and experienced diachronous episodes of strain localization along its strike. The structural evolution of the ∼350-km-long fault segments crossing the North Aegean Sea remains to be accurately investigated. There, the modern North Anatolian Fault is localized along two main branches: the northern branch ends at the North Aegean Trough and the southern branch ends at the Edremit-Skyros Trough. The Evia Basin is located in the North Aegean Domain between the North Anatolian Fault and the Corinth Rift. This study presents seismic reflection lines crossing the aforementioned structures of the North Aegean Domain, which document their subsurface structure and the sedimentary record of their activity since the Messinian. The seismic-reflection dataset is tied to regional-scale stratigraphic markers, which constrains the age of main tectonic events related to the formation of the North Anatolian Fault. The seismic-reflection lines show that the two main branches of the North Anatolian Fault became localized structures at 1.3-2 Ma, coevally with the formation of the Evia Basin. Since 2 Ma, the North Aegean Troughs developed as a series of horsetail basins propagating westwards at the termination of the branches of the North Anatolian Fault. On a regional scale, the wide and diffuse North Anatolian transtensive shear zone active from Serravalian to Late Pliocene turned into a narrower shear zone at the two main branches of the North Anatolian Fault since the Early Pleistocene. This abrupt episode of strain localization occurred in the frame of the major Early Pleistocene change in stress regime from NE-SW to N-S extension, which has been observed throughout the Aegean Sea.

Published
2023
Full Text
View/download PDF

7. Evolution of the North Anatolian Fault from a diffuse to a localized shear zone in the North Aegean Sea during the Plio-Pleistocene

Author

Centre National de la Recherche Scientifique (France), Agencia Estatal de Investigación (España), Rodriguez, Mathieu, Sakellariou, Dimitris, Gorini, Christian, Janin, A., D'Acremont, Elia, Le Pourhiet, Laetitia, Chamot-Rooke, N., Tsampouraki-Kraounaki, K., Morfis, I., Rousakis, G., Henry, Pierre, Lurin, A., Delescluse, M., Briole, P., Rigo, A., Arsenikos, S., Bulois, C., Fernández-Blanco, David, Beniest, Anouk, Grall, C., Chanier, Frank, Caroir, F., Dessa, J.-X., Oregioni, D., Nercessian, Alexandre, Centre National de la Recherche Scientifique (France), Agencia Estatal de Investigación (España), Rodriguez, Mathieu, Sakellariou, Dimitris, Gorini, Christian, Janin, A., D'Acremont, Elia, Le Pourhiet, Laetitia, Chamot-Rooke, N., Tsampouraki-Kraounaki, K., Morfis, I., Rousakis, G., Henry, Pierre, Lurin, A., Delescluse, M., Briole, P., Rigo, A., Arsenikos, S., Bulois, C., Fernández-Blanco, David, Beniest, Anouk, Grall, C., Chanier, Frank, Caroir, F., Dessa, J.-X., Oregioni, D., and Nercessian, Alexandre

Abstract

The North Anatolian Fault is the ∼1200-km-long active continental transform boundary between Anatolia and Eurasia. This strike-slip system initiated around 10–12 Ma and experienced diachronous episodes of strain localization along its strike. The structural evolution of the ∼350-km-long fault segments crossing the North Aegean Sea remains to be accurately investigated. There, the modern North Anatolian Fault is localized along two main branches: the northern branch ends at the North Aegean Trough and the southern branch ends at the Edremit-Skyros Trough. The Evia Basin is located in the North Aegean Domain between the North Anatolian Fault and the Corinth Rift. This study presents seismic reflection lines crossing the aforementioned structures of the North Aegean Domain, which document their subsurface structure and the sedimentary record of their activity since the Messinian. The seismic-reflection data set is tied to regional-scale stratigraphic markers, which constrains the age of main tectonic events related to the formation of the North Anatolian Fault. The seismic-reflection lines show that the two main branches of the North Anatolian Fault became localized structures at 1.3–2 Ma, coevally with the formation of the Evia Basin. Since 2 Ma, the North Aegean Troughs developed as a series of horsetail basins propagating westwards at the termination of the branches of the North Anatolian Fault. On a regional scale, the wide and diffuse North Anatolian transtensive shear zone active from Serravalian to Late Pliocene turned into a narrower shear zone at the two main branches of the North Anatolian Fault since the Early Pleistocene. This abrupt episode of strain localization occurred in the frame of the major Early Pleistocene change in stress regime from NE–SW to N–S extension, which has been observed throughout the Aegean Sea

Published
2023

8. The Detection of Volcanic Debris Avalanches (VDAs) Along the Hellenic Volcanic Arc, Through Marine Geophysical Techniques

Author

Nomikou, P., Papanikolaou, D., Tibaldi, A., Carey, S., Livanos, I., Bell, K. L. C., Pasquarè, F. A., Rousakis, G., Krastel, Sebastian, editor, Behrmann, Jan-Hinrich, editor, Völker, David, editor, Stipp, Michael, editor, Berndt, Christian, editor, Urgeles, Roger, editor, Chaytor, Jason, editor, Huhn, Katrin, editor, Strasser, Michael, editor, and Harbitz, Carl Bonnevie, editor

Published
2014
Full Text
View/download PDF

16. Pre‐messinian deposits of the mediterranean ridge: Biostratigraphic and geochemical evidence from the olimpi mud volcano field

Author

Nikitas, A. Triantaphyllou, M.V. Rousakis, G. Panagiotopoulos, I. Pasadakis, N. Hatzianestis, I. Gogou, A.

Abstract

This study presents the results derived from micropaleontological and organic geochemical analyses of mud breccia samples obtained (through gravity coring) from five mud volcanoes (Gelendzhik, Heraklion, Moscow, Milano, Leipzig) located at the Olimpi mud volcano field on the Mediterranean Ridge accretionary complex. A thorough calcareous nannofossil semi‐quantitative analysis was performed to determine the biostratigraphic assignment of the deep‐seated source strata. Mudstone/shale clasts of different stratigraphic levels were identified and assigned to the Miocene nannofossil biozones CNM10, CNM8–9, CNM7, CNM6–7, and Oli-gocene CNO4/CNO5. A single mudstone clast from the Gelendzhik plateau, assigned to the bi-ozone CNM10, demonstrated unique micropaleontological and geochemical characteristics, sug-gesting a sapropelic origin. Subsequently, the total organic carbon (TOC) content and thermal maturity of the collected mud breccias was evaluated using the Rock‐Eval pyrolysis technique, and their oil and gas potential was estimated. The pyrolyzed sediments were both organic rich and organic poor (TOC >0.5% or

Published
2021

17. Particle dynamics and fluxes in canyons and open slopes of the southern Cretan margin (Eastern Mediterranean)

Author

Karageorgis, A, Kontoyiannis, H, Stavrakakis, S, Krasakopoulou, E, Gogou, A, Papadopoulos, A, Kanellopoulos, T, Rousakis, G, Malinverno, E, Triantaphyllou, M, Lykousis, V, Karageorgis, A. P., Kontoyiannis, H., Stavrakakis, S., Krasakopoulou, E., Gogou, A., Papadopoulos, A., Kanellopoulos, Th. D., Rousakis, G., Malinverno, E., Triantaphyllou, M. V., Lykousis, V., Karageorgis, A, Kontoyiannis, H, Stavrakakis, S, Krasakopoulou, E, Gogou, A, Papadopoulos, A, Kanellopoulos, T, Rousakis, G, Malinverno, E, Triantaphyllou, M, Lykousis, V, Karageorgis, A. P., Kontoyiannis, H., Stavrakakis, S., Krasakopoulou, E., Gogou, A., Papadopoulos, A., Kanellopoulos, Th. D., Rousakis, G., Malinverno, E., Triantaphyllou, M. V., and Lykousis, V.

Abstract

The Samaria and Lithinon canyons at the southern Cretan margin (Eastern Mediterranean) were studied with respect to hydrography, deep currents, particle dynamics and settling fluxes by utilizing: (a) current-meter and sediment trap records from May 2005 to May 2006; and (b) hydrographic and optical measurements along with particulate matter and particulate organic carbon concentrations (PMC and POC, respectively) in two surveys (May and October 2005). The deep currents were very weak with mean velocity ~3-4 cm s-1and their direction was controlled by the local bottom topography. The entire area was characterized by very low PMC and POC, depicted both by transmissometry profiles and discrete bottle data. The fluxes of downward settling particles are comparable with the fluxes measured in the broader Eastern Mediterranean and hence point to an oligotrophic environment with low atmospheric and lateral inputs. A series of relatively high total mass fluxes (>1000 mg m-2d-1) were recorded near the head of the Samaria canyon, at the trap closest to Crete, and was attributed to: (a) high temporal lithogenic inputs (mineral calcite) transferred to the sea by a small, intermittent stream flowing through the Samaria gorge, which was activated by short rainfall events and spring snowmelt; and (b) inputs of numerous coccoliths of E. huxleyi and calcite by shallow sediment resuspension generated by wind-induced waves. Apart from this local-scale event, there was very little evidence of matter transfer through the canyons, thus, during the one-year of observations, the canyons were dormant. Because of this lack of down-canyon transport during the study period, open slopes and canyons exhibited roughly similar characteristics in terms both of particle dynamics and fluxes. However, the presence of coarse-grained sediments along the canyon axes point to episodic canyon activity, occurring at unknown time scales and periodicity

Published
2018

18. Deep-sea benthic foraminifera record of the last 1500 years in the NorthAegean Trough (northeastern Mediterranean): A paleoclimaticreconstruction scenario

Author

Dimiza, M. D. Fatourou, M. Arabas, A. Panagiotopoulos, I and Gogou, A. Kouli, K. Parinos, C. Rousakis, G. and Triantaphyllou, V, M.

Abstract

A 1500-year, high-resolution deep-sea benthic foraminifera record from the Athos Basin of the North Aegean Trough (northeastern Mediterranean) has been analyzed for the development of a paleoclimatic scenario. The data analysis points out that the quantity and quality of the seafloor's organic matter could be a crucial controlling factor for the faunal succession. During 550-1000 AD (within the Medieval Climate Anomaly), the relatively high benthic foraminiferal accumulation rates together with the predominance of meso-eutrophic taxa, such as Bolivina dilatata/spathulata, may be interpreted as the result of high precipitation. Consequently, increased riverine discharges into the North Aegean Sea and the associated warm climatic conditions appear to persist for a long time and are related to a negative phase of the North Atlantic Oscillation. Later on, the establishment of an oligo-mesotrophic seafloor environment is documented by the diminishing benthic foraminiferal accumulation rates associated with an increment in the abundances of Gyroidinotdes altiformis. During a colder phase of the Little Ice Age (17th century), the relative abundances of the opportunistic foraminiferal species Bulimina inflate and Bulimina marginata can be related to high marine productivity, most probably due to enhanced winter mixing conditions. Finally, during the last 100 years, a faunal shift to eutrophication preferent species, and the persistent occurrence of Chilostomella mediterranensis, reflects a pronounced change in trophic conditions, characterized by high amounts of potentially low-quality organic matter in the seafloor, which are the result of a gradual temperature increase accompanied with enhanced terrigenous inputs.

Published
2020

19. Assessment of the eruptive activity and identification of the mud breccia's source in the Olimpi mud volcano field, Eastern Mediterranean

Author

Panagiotopoulos, I.P. Paraschos, F. Rousakis, G. Hatzianestis, I. Parinos, C. Morfis, I. Gogou, A.

Abstract

Even though the intensity and frequency of the eruptive episodes of deep-sea mud volcanoes (MVs) substantially regulate the methane fluxes into the hydrosphere and the development of the near-seafloor sulfate zone that affects the position of the gas hydrate stability zone, these factors are not yet adequately investigated. Moreover, the evaluation of the eruptive sediment's thermal maturity may provide solid documentation of the petroleum generation potential in high depths below seafloor (bsf). Hence, the present study, through the integration of sedimentary facies analysis with hydrocarbon biomarker analysis (based on the concentrations of long-chain (C25–C35) n-alkanes, hopanes and steranes), supported by swath bathymetry data, examined five sediment cores recovered from the Gelendzhik, Moscow, Milano, Leipzig and Heraklion MVs of the Olimpi mud volcano field (OMVF) on the central Mediterranean Ridge. The main objective of this investigation was to assess the ‘modern’ eruptive activity in the OMVF and identify the mud breccia's origin and mobilization depth (based on its maturity level), and the ages of the source beds. Among the studied MVs, Milano, Leipzig and Heraklion appear ‘recently’ active, while Moscow perhaps remains in dormancy for at least one century. The eruptive activity in the OMVF seems to be, generally, vigorous and persistent, while it is linked with several source beds of variable stratigraphy or environmental condition. The multiple eruptive episodes, occurring as uninterrupted events or via pulses, create conditions that perhaps favour high releases of methane into the water column as well as the growth of the gas hydrate phase near the seafloor. The identified ‘modern’ mudflows appear thermally immature for oil generation, while they most probably originate from terrestrial source beds located not deeper than 2 km bsf. A Messinian age could be suggested for the principal sources of the very soft to soft mud breccias of the OMVF, while stratigraphic horizons of Early-Middle Miocene might be proposed as the likely major sources for the firm to very stiff mud breccias of the area. © 2019 Elsevier Ltd

Published
2020

24. Sediment transport mechanisms from the slopes and canyons to the deep basins south of Crete Island (southeast Mediterranean)

Author

Manta, K. Rousakis, G. Anastasakis, G. Lykousis, V. Sakellariou, D. Panagiotopoulos, I.P.

Abstract

Sediment transport processes from the slopes to the deep basins were studied in the southern Cretan margin (Eastern Mediterranean) by means of swath bathymetry, seismic reflection (airgun) profiling, and gravity coring. Mud/silt turbidites, developed in structureless or laminated patterns, appear to dominate the continental slope and the 2700–3600-m deep depressions of Samaria, Messara, and Gortys. These deposits are the result of successive mass transport events and turbidity currents. Over-steepening caused by strike–slip shearing associated with extensional tectonic activity in the shallow crustal levels, shaking due to significant seismic activity, and the presence of weak sediment layers are responsible for frequent triggering of slope failures and the subsequent formation of turbidity currents on the Gavdos slope. On the Cretan slope, sediments channeled as turbidity currents through canyons proved to be the major delivery mechanism, together with debris flows. Subordinate contributions of hemipelagic sediments occur only in the Messara basin. Moreover, steep non-incised slope areas and slope-confined canyons of the Gavdos slope were found to provide comparable sediment contribution with the fluvially connected canyons of the Cretan slope. © 2019, Springer-Verlag GmbH Germany, part of Springer Nature.

Published
2019

26. Particle dynamics and fluxes in canyons and open slopes of the southern Cretan margin (Eastern Mediterranean)

Author

Karageorgis, A.P. Kontoyiannis, H. Stavrakakis, S. Krasakopoulou, E. Gogou, A. Papadopoulos, A. Kanellopoulos, T.D. Rousakis, G. Malinverno, E. Triantaphyllou, M.V. Lykousis, V.

Abstract

The Samaria and Lithinon canyons at the southern Cretan margin (Eastern Mediterranean) were studied with respect to hydrography, deep currents, particle dynamics and settling fluxes by utilizing: (a) current-meter and sediment trap records from May 2005 to May 2006; and (b) hydrographic and optical measurements along with particulate matter and particulate organic carbon concentrations (PMC and POC, respectively) in two surveys (May and October 2005). The deep currents were very weak with mean velocity ∼3–4 cm s−1 and their direction was controlled by the local bottom topography. The entire area was characterized by very low PMC and POC, depicted both by transmissometry profiles and discrete bottle data. The fluxes of downward settling particles are comparable with the fluxes measured in the broader Eastern Mediterranean and hence point to an oligotrophic environment with low atmospheric and lateral inputs. A series of relatively high total mass fluxes (>1000 mg m−2 d−1) were recorded near the head of the Samaria canyon, at the trap closest to Crete, and was attributed to: (a) high temporal lithogenic inputs (mineral calcite) transferred to the sea by a small, intermittent stream flowing through the Samaria gorge, which was activated by short rainfall events and spring snowmelt; and (b) inputs of numerous coccoliths of E. huxleyi and calcite by shallow sediment resuspension generated by wind-induced waves. Apart from this local-scale event, there was very little evidence of matter transfer through the canyons, thus, during the one-year of observations, the canyons were dormant. Because of this lack of down-canyon transport during the study period, open slopes and canyons exhibited roughly similar characteristics in terms both of particle dynamics and fluxes. However, the presence of coarse-grained sediments along the canyon axes point to episodic canyon activity, occurring at unknown time scales and periodicity. © 2017 Elsevier Ltd

Published
2018

29. The Detection of Volcanic Debris Avalanches (VDAs) Along the Hellenic Volcanic Arc Through Marine Geophysical Techniques

Author

Krastel, S, Nomikou, P, Tibaldi, A, Carey, S, Livanos, I, Bell, K, Pasquarè, F, Rousakis, G, Nomikou, PD, TIBALDI, ALESSANDRO, Rousakis, G., Krastel, S, Nomikou, P, Tibaldi, A, Carey, S, Livanos, I, Bell, K, Pasquarè, F, Rousakis, G, Nomikou, PD, TIBALDI, ALESSANDRO, and Rousakis, G.

Abstract

Recent marine oceanographic surveys using geophysical techniques have revealed a number of volcanic debris avalanche deposits (VDAs) on the external flanks of Antimilos, Santorini and Nisyros volcanoes in the South Aegean Sea. Swath bathymetry and side-scan sonar surveys led to the recognition of characteristic hummocky topography on all of these deposits. On seismic profiles the VDAs are identified by chaotic facies, with incoherent areas bordered by continuous undisturbed seismic reflectors. High-resolution examination of the morphological characteristics of the VDAs was accomplished by using Remotely Operated Vehicles (ROVs), in order to distinguish them from other clastic deposits. In some cases the VDAs can be traced upslope to horseshoe-shaped collapse depressions and represent the expression of the complex evolution of these volcanic edifices. Recognition of VDAs at these volcanic centers has important implications for geohazard assessments as flank collapses have the potential for triggering of large-scale tsunamis. The relationship between the distribution/emplacement mechanisms of the VDA deposits and the source flank collapses remains an area of ongoing research.

Published
2014

30. Climate variability and socio-environmental changes in the northern Aegean (NE Mediterranean) during the last 1500 years

Author

Gogou, A. Triantaphyllou, M. Xoplaki, E. Izdebski, A. Parinos, C. Dimiza, M. Bouloubassi, I. Luterbacher, J. Kouli, K. Martrat, B. Toreti, A. Fleitmann, D. Rousakis, G. Kaberi, H. Athanasiou, M. Lykousis, V.

Abstract

We provide new evidence on sea surface temperature (SST) variations and paleoceanographic/paleoenvironmental changes over the past 1500 years for the north Aegean Sea (NE Mediterranean). The reconstructions are based on multiproxy analyses, obtained from the high resolution (decadal to multi-decadal) marine record M2 retrieved from the Athos basin. Reconstructed SSTs show an increase from ca. 850 to 950 AD and from ca. 1100 to 1300 AD. A cooling phase of almost 1.5 °C is observed from ca. 1600 AD to 1700 AD. This seems to have been the starting point of a continuous SST warming trend until the end of the reconstructed period, interrupted by two prominent cooling events at 1832 ± 15 AD and 1995 ± 1 AD. Application of an adaptive Kernel smoothing suggests that the current warming in the reconstructed SSTs of the north Aegean might be unprecedented in the context of the past 1500 years. Internal variability in atmospheric/oceanic circulations systems as well as external forcing as solar radiation and volcanic activity could have affected temperature variations in the north Aegean Sea over the past 1500 years. The marked temperature drop of approximately ~2 °C at 1832 ± 15 yr AD could be related to the 1809 ΑD 'unknown' and the 1815 AD Tambora volcanic eruptions. Paleoenvironmental proxy-indices of the M2 record show enhanced riverine/continental inputs in the northern Aegean after ca. 1450 AD.The paleoclimatic evidence derived from the M2 record is combined with a socio-environmental study of the history of the north Aegean region. We show that the cultivation of temperature-sensitive crops, i.e. walnut, vine and olive, co-occurred with stable and warmer temperatures, while its end coincided with a significant episode of cooler temperatures. Periods of agricultural growth in Macedonia coincide with periods of warmer and more stable SSTs, but further exploration is required in order to identify the causal links behind the observed phenomena. The Black Death likely caused major changes in agricultural activity in the north Aegean region, as reflected in the pollen data from land sites of Macedonia and the M2 proxy-reconstructions. Finally, we conclude that the early modern peaks in mountain vegetation in the Rhodope and Macedonia highlands, visible also in the M2 record, were very likely climate-driven. © 2016 Elsevier Ltd.

Published
2016

31. HIGH-RESOLUTION GEOMORPHOLOGICAL MAPPING OF THE SHALLOW CONTINENTAL SHELF WEST OF THE KAVALA BAY, NORTH AEGEAN

Author

Panagiotopoulos, I.P., primary, Kapsimalis, V., additional, Ioakim, Chr., additional, Karageorgis, A., additional, Rousakis, G., additional, Morfis, I., additional, Hatiris, G.A., additional, Anagnostou, C., additional, Koukoulis, A., additional, Papatrechas, Ch., additional, Koutsovitis, P.D., additional, Economou, G., additional, Tsapara, E., additional, and Kyriakidou, C., additional

Published
2017
Full Text
View/download PDF

32. GEOMORPHOLOGY, SEDIMENTOLOGY AND GEOCHEMISTRY IN THE MARINE AREA BETWEEN SIFNOS AND KIMOLOS ISLANDS, GREECE

Author

Karageorgis, A.P., primary, Ioakim, Chr., additional, Rousakis, G., additional, Sakellariou, D., additional, Vougioukalakis, G., additional, Panagiotopoulos, I.P., additional, Zimianitis, E., additional, Koutsopoulou, E., additional, Kanellopoulos, Th., additional, Papatrechas, Ch., additional, Georgiou, P., additional, Xirokostas, N., additional, Stavrakaki, I., additional, Vakalas, I., additional, Morfis, I., additional, Koutsovitis, P., additional, Drakopoulou, P., additional, Kyriakidou, Ch., additional, and Marantos, I., additional

Published
2017
Full Text
View/download PDF

35. The detection of volcanic debris avalanches (VDAs) along the hellenic volcanic arc, through marine geophysical techniques

Author

Nomikou, P., Papanikolaou, D., Tibaldi, A., Carey, S., Livanos, I., Bell, K. L.C., Pasquarè, F. A., Rousakis, G., Nomikou, P., Papanikolaou, D., Tibaldi, A., Carey, S., Livanos, I., Bell, K. L.C., Pasquarè, F. A., and Rousakis, G.

Abstract

Recent marine oceanographic surveys using geophysical techniques have revealed a number of volcanic debris avalanche deposits (VDAs) on the external flanks of Antimilos, Santorini and Nisyros volcanoes in the South Aegean Sea. Swath bathymetry and side-scan sonar surveys led to the recognition of characteristic hummocky topography on all of these deposits. On seismic profiles the VDAs are identified by chaotic facies, with incoherent areas bordered by continuous undisturbed seismic reflectors. High-resolution examination of the morphological characteristics of the VDAs was accomplished by using Remotely Operated Vehicles (ROVs), in order to distinguish them from other clastic deposits. In some cases the VDAs can be traced upslope to horseshoe-shaped collapse depressions and represent the expression of the complex evolution of these volcanic edifices. Recognition of VDAs at these volcanic centers has important implications for geohazard assessments as flank collapses have the potential for triggering of large-scale tsunamis. The relationship between the distribution/emplacement mechanisms of the VDA deposits and the source flank collapses remains an area of ongoing research.

Published
2016

36. Climate variability at the North Aegean Sea (Eastern Mediterranean Sea) during the last two millennia: coccolithophore evidence

Author

Athanasiou, M., Triantaphyllou, Maria V., Gogou, Alexandra, Dimiza, Margarita D., Parinos, C., Bouloubassi, Ioanna, Rousakis, G., Lykousis, V., Biogéochimie-Traceurs-Paléoclimat (BTP), Laboratoire d'Océanographie et du Climat : Expérimentations et Approches Numériques (LOCEAN), Institut de Recherche pour le Développement (IRD)-Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Muséum national d'Histoire naturelle (MNHN)-Institut Pierre-Simon-Laplace (IPSL (FR_636)), École normale supérieure - Paris (ENS Paris), Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris Diderot - Paris 7 (UPD7)-École polytechnique (X)-Centre National d'Études Spatiales [Toulouse] (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-École normale supérieure - Paris (ENS Paris), Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université Paris Diderot - Paris 7 (UPD7)-École polytechnique (X)-Centre National d'Études Spatiales [Toulouse] (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche pour le Développement (IRD)-Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Muséum national d'Histoire naturelle (MNHN)-Institut Pierre-Simon-Laplace (IPSL (FR_636)), Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université Paris Diderot - Paris 7 (UPD7)-École polytechnique (X)-Centre National d'Études Spatiales [Toulouse] (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS), Muséum national d'Histoire naturelle (MNHN)-Institut de Recherche pour le Développement (IRD)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Institut Pierre-Simon-Laplace (IPSL (FR_636)), École normale supérieure - Paris (ENS-PSL), Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris Diderot - Paris 7 (UPD7)-École polytechnique (X)-Centre National d'Études Spatiales [Toulouse] (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-École normale supérieure - Paris (ENS-PSL), and Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université Paris Diderot - Paris 7 (UPD7)-École polytechnique (X)-Centre National d'Études Spatiales [Toulouse] (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Muséum national d'Histoire naturelle (MNHN)-Institut de Recherche pour le Développement (IRD)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Institut Pierre-Simon-Laplace (IPSL (FR_636))

Subjects
[PHYS.PHYS.PHYS-GEO-PH]Physics [physics]/Physics [physics]/Geophysics [physics.geo-ph], ComputingMilieux_MISCELLANEOUS
Abstract

International audience

Published
2014

37. Late Interglacial to Holocene paleoenvironmental evolution of western Cyclades plateau (SW Aegean Sea)

Author

Raftopoulou, M., Triantaphyllou, Maria V., Rousakis, G., Bouloubassi, Ioanna, Dimiza, Margarita D., Kapsimalis, A. V., Gogou, Alexandra, Lykousis, V., Biogéochimie-Traceurs-Paléoclimat (BTP), Laboratoire d'Océanographie et du Climat : Expérimentations et Approches Numériques (LOCEAN), Institut de Recherche pour le Développement (IRD)-Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Muséum national d'Histoire naturelle (MNHN)-Institut Pierre-Simon-Laplace (IPSL (FR_636)), École normale supérieure - Paris (ENS Paris), Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris Diderot - Paris 7 (UPD7)-École polytechnique (X)-Centre National d'Études Spatiales [Toulouse] (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-École normale supérieure - Paris (ENS Paris), Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université Paris Diderot - Paris 7 (UPD7)-École polytechnique (X)-Centre National d'Études Spatiales [Toulouse] (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche pour le Développement (IRD)-Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Muséum national d'Histoire naturelle (MNHN)-Institut Pierre-Simon-Laplace (IPSL (FR_636)), Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université Paris Diderot - Paris 7 (UPD7)-École polytechnique (X)-Centre National d'Études Spatiales [Toulouse] (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS), Muséum national d'Histoire naturelle (MNHN)-Institut de Recherche pour le Développement (IRD)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Institut Pierre-Simon-Laplace (IPSL (FR_636)), École normale supérieure - Paris (ENS-PSL), Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris Diderot - Paris 7 (UPD7)-École polytechnique (X)-Centre National d'Études Spatiales [Toulouse] (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-École normale supérieure - Paris (ENS-PSL), and Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université Paris Diderot - Paris 7 (UPD7)-École polytechnique (X)-Centre National d'Études Spatiales [Toulouse] (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Muséum national d'Histoire naturelle (MNHN)-Institut de Recherche pour le Développement (IRD)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Institut Pierre-Simon-Laplace (IPSL (FR_636))

Subjects
[PHYS.PHYS.PHYS-GEO-PH]Physics [physics]/Physics [physics]/Geophysics [physics.geo-ph], ComputingMilieux_MISCELLANEOUS
Abstract

International audience

Published
2014

38. Multi-proxy evidence of Holocene paleoceanographic and paleoclimatic instability in the NE Mediterranean: connections to global-scale variability

Author

Gogou, Alexandra, Triantaphyllou, Maria V., Bouloubassi, Ioanna, Emeis, K.-C., Katsouras, G., Dimiza, Margarita D., Kouli, K., Parinos, C., Möbius, J., Rousakis, G., Athanasiou, M., Lykousis, V., Biogéochimie-Traceurs-Paléoclimat (BTP), Laboratoire d'Océanographie et du Climat : Expérimentations et Approches Numériques (LOCEAN), Muséum national d'Histoire naturelle (MNHN)-Institut de Recherche pour le Développement (IRD)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Institut Pierre-Simon-Laplace (IPSL (FR_636)), École normale supérieure - Paris (ENS-PSL), Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris Diderot - Paris 7 (UPD7)-École polytechnique (X)-Centre National d'Études Spatiales [Toulouse] (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-École normale supérieure - Paris (ENS-PSL), Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université Paris Diderot - Paris 7 (UPD7)-École polytechnique (X)-Centre National d'Études Spatiales [Toulouse] (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Muséum national d'Histoire naturelle (MNHN)-Institut de Recherche pour le Développement (IRD)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Institut Pierre-Simon-Laplace (IPSL (FR_636)), Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université Paris Diderot - Paris 7 (UPD7)-École polytechnique (X)-Centre National d'Études Spatiales [Toulouse] (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS), Institut de Recherche pour le Développement (IRD)-Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Muséum national d'Histoire naturelle (MNHN)-Institut Pierre-Simon-Laplace (IPSL (FR_636)), École normale supérieure - Paris (ENS Paris), Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris Diderot - Paris 7 (UPD7)-École polytechnique (X)-Centre National d'Études Spatiales [Toulouse] (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-École normale supérieure - Paris (ENS Paris), and Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université Paris Diderot - Paris 7 (UPD7)-École polytechnique (X)-Centre National d'Études Spatiales [Toulouse] (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche pour le Développement (IRD)-Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Muséum national d'Histoire naturelle (MNHN)-Institut Pierre-Simon-Laplace (IPSL (FR_636))

Subjects
[PHYS.PHYS.PHYS-GEO-PH]Physics [physics]/Physics [physics]/Geophysics [physics.geo-ph], ComputingMilieux_MISCELLANEOUS
Abstract

International audience

Published
2014

39. The detection of volcanic debris avalanches (VDAs) along the Hellenic volcanic arc, through marine geophysical techniques

Author

Nomikou, P. Papanikolaou, D. Tibaldi, A. Carey, S. Livanos, I. Bell, K.L.C. Pasquarè, F.A. Rousakis, G.

Abstract

Recent marine oceanographic surveys using geophysical techniques have revealed a number of volcanic debris avalanche deposits (VDAs) on the external flanks of Antimilos, Santorini and Nisyros volcanoes in the South Aegean Sea. Swath bathymetry and side-scan sonar surveys led to the recognition of characteristic hummocky topography on all of these deposits. On seismic profiles the VDAs are identified by chaotic facies, with incoherent areas bordered by continuous undisturbed seismic reflectors. High-resolution examination of the morphological characteristics of the VDAs was accomplished by using Remotely Operated Vehicles (ROVs), in order to distinguish them from other clastic deposits. In some cases the VDAs can be traced upslope to horseshoe-shaped collapse depressions and represent the expression of the complex evolution of these volcanic edifices. Recognition of VDAs at these volcanic centers has important implications for geohazard assessments as flank collapses have the potential for triggering of large-scale tsunamis. The relationship between the distribution/emplacement mechanisms of the VDA deposits and the source flank collapses remains an area of ongoing research. © Springer International Publishing Switzerland 2014.

Published
2014

40. Evidence for a warm and humid Mid-Holocene episode in the Aegean and northern Levantine Seas (Greece, NE Mediterranean)

Author

Triantaphyllou, M.V. Gogou, A. Bouloubassi, I. Dimiza, M. Kouli, K. Rousakis, G. Kotthoff, U. Emeis, K.-C. Papanikolaou, M. Athanasiou, M. Parinos, C. Ioakim, C. Lykousis, V.

Abstract

Marine and terrestrial biological and biogeochemical proxies in three sediment cores from North and SE Aegean and northern Levantine Seas record continuous warm and humid conditions between 5.5 and 4.0 ka BP related to the establishment of relatively stratified conditions in the upper water column. These conditions may have resulted from the concordant albeit weak Mid-Holocene South Asian monsoon forcing, combined with lighter Etesian winds. During this interval, sea surface temperatures fluctuate in the Aegean Sea, although exhibiting a strong positive shift at ~4.8 ka BP. The warm and humid climatic conditions triggered upper water column stratification and enhancement of the deep chlorophyll maximum (DCM), leading to dysoxic conditions and the deposition of a sapropel-like layer, but only in the SE Aegean site. In contrast to the shallow water SE Aegean, the deeper North Aegean and the northern Levantine sites, although experiencing stratification in the upper parts of the water column, did not achieve bottom-water dysoxia. Thus, a top–bottom mechanism of stratification–DCM development accompanied by fast transport and burial of organic matter is a likely explanation for the preservation of productivity signal in the shallow sites of the SE Aegean and establishment of sapropelic conditions during the warm and humid Mid-Holocene. The termination of the Mid-Holocene warm and humid phase coincides with the “4.2 ka” climate event. Our data exhibit an N–S time transgressive aridification gradient around the Aegean Sea, most probably associated with the reorganization of the general atmospheric circulation during the Mid-Holocene. © 2013, Springer-Verlag Berlin Heidelberg.

Published
2014

41. Organic contamination of surface sediments in the metropolitan coastal zone of Athens, Greece: Sources, degree, and ecological risk

Author

Kapsimalis, V. Panagiotopoulos, I.P. Talagani, P. Hatzianestis, I. Kaberi, H. Rousakis, G. Kanellopoulos, T.D. Hatiris, G.A.

Abstract

Bottom sediments represent a crucial component of the marine environment, since they constitute a habitat, a trophic resource, and a spawning place for various organisms. Unfortunately, the sediments of urban coastal areas are deeply impacted by anthropogenic activities that degrade their quality. In the Drapetsona-Keratsini metropolitan coastal zone of Athens, current industrial and shipping activities together with the effluents from a sewage outfall, which was in operation in the past, have resulted in one of the most contaminated sedimentary environments, in terms of organic compound loads, in Mediterranean. Exceptionally high concentrations of aliphatic hydrocarbons (up to 4457μgg-1), carcinogenic PAHs (up to 7284ngg-1), and organochlorines (up to 544ngg-1 for PCBs; up to 208ngg-1 for DDTs) constitute a major threat to the marine life of the associated Saronikos Gulf. © 2013 Elsevier Ltd.

Published
2014

44. Submarine volcanoes along the aegean volcanic arc

Author

Nomikou, P. Papanikolaou, D. Alexandri, M. Sakellariou, D. Rousakis, G.

Abstract

Aegean volcanic arc has been investigated along its offshore areas and several submarine volcanic outcrops have been discovered in the last 25 years of research. The basic data including swath bathymetric maps, air-gun profiles, underwater photos and samples analysis have been presented along the four main volcanic groups of the arc. The description concerns: (i) Paphsanias submarine volcano in the Methana group, (ii) three volcanic domes to the east of Antimilos Volcano and hydrothermal activity in southeast Milos in the Milos group, (iii) three volcanic domes east of Christiana and a chain of about twenty volcanic domes and craters in the Kolumbo zone northeast of Santorini in the Santorini group and (iv) several volcanic domes and a volcanic caldera together with very deep slopes of several volcanic islands in the Nisyros group. The tectonic structure of the volcanic centers is described and related to the geometry of the arc and the neotectonic graben structures that usually host them. The NE-SW direction is dominant in the Santorini and Nisyros volcanic groups, located at the eastern part of the arc, where strike-slip is also present, whereas NW-SE direction dominates in Milos and Methana at the western part, where co-existence of E-Wdisrupting normal faults is observed. The volcanic relief reaches 1100-1200 m in most cases. This is produced from the outcrops of the volcanic centers emerging usually at 400-600 mdepth and ending either below sea level or at high altitudes of 600-700 m on the islands. Hydrothermal activity at relatively high temperatures observed in Kolumbo is remarkable whereas low temperature phenomena have been detected in the Santorini caldera around Kameni islands and in the area southeast of Milos. In Methana and Nisyros, hydrothermal activity seems to be limited in the coastal areas without other offshore manifestations. © 2012 Elsevier B.V.

Published
2013

45. The volcanic debris avalanche on the SE submarine slope of Nisyros volcano, Greece: Geophysical exploration and implications for subaerial eruption history

Author

Livanos, I. Nomikou, P. Papanikolaou, D. Rousakis, G.

Abstract

A spectacular hummocky topography was discovered offshore of the south-eastern slope of the Nisyros island volcano in the eastern sector of the Aegean volcanic arc in 2000-2001, using multibeam bathymetric mapping and seismic profiling, and interpreted as part of a volcanic debris avalanche originating onland. During E/V Nautilus cruise NA011 in 2010, a detailed side-scan sonar and ROV exploration aimed at evaluating the surface morphology of this avalanche field. Combining the new data with selected older datasets reveals that the debris avalanche is characterized by numerous (at least 78) variously sized and shaped hummocks. Some of these are distinctly round, either scattered or aligned in groups, whereas others are elongated in the form of ridges. This is consistent with existing models accounting for variations in the longitudinal and lateral velocity ratio of landslides. Maximum dimensions reach 60 m in height above the sea bottom, 220 m in length and 230 m in width. The structures outline a large tongue-shaped, submarine hummock field of about 22.2 km2, approx. 4.8 km wide and 4.6 km long and with an estimated volume of 0.277 km3. Due to its characteristic shape, the collapsed volcanic flank is interpreted to represent a singular failing event, involving a rapid and virtually instantaneous downslope movement of the slide mass into the sea. Indeed, the H/L (height of 280 m vs. run-out of 7 km) ratio for the Nisyros slide is 0.04; plotted against volume, this falls within the theoretical bounds as well as measured values typical of submarine landslides. The timing of the event is probably related to the extrusion of Nikia lavas and their subsequent failure and formation of a main scarp observed at about 120 m depth on an 8-km-long seismic profile and a map of slope angle distribution, at the depth where the palaeo-coastline was located 40 ka ago. An inferred age of ca. 40 ka for the avalanche awaits confirmation based on dating of core material. © 2013 Springer-Verlag Berlin Heidelberg.

Published
2013

47. Holocene climate variability and environmental changes in the NE Mediterranean Sea along a N-S transect

Author

Gogou, Alexandra, Bouloubassi, Ioanna, Emeis, K.-C., Triantaphyllou, M., Katsouras, G., Rousakis, G., Lykousis, V., Laboratoire d'Océanographie et du Climat : Expérimentations et Approches Numériques (LOCEAN), Muséum national d'Histoire naturelle (MNHN)-Institut de Recherche pour le Développement (IRD)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Institut Pierre-Simon-Laplace (IPSL (FR_636)), École normale supérieure - Paris (ENS-PSL), Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris Diderot - Paris 7 (UPD7)-École polytechnique (X)-Centre National d'Études Spatiales [Toulouse] (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-École normale supérieure - Paris (ENS-PSL), Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université Paris Diderot - Paris 7 (UPD7)-École polytechnique (X)-Centre National d'Études Spatiales [Toulouse] (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS), Institut de Recherche pour le Développement (IRD)-Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Muséum national d'Histoire naturelle (MNHN)-Institut Pierre-Simon-Laplace (IPSL (FR_636)), École normale supérieure - Paris (ENS Paris), and Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris Diderot - Paris 7 (UPD7)-École polytechnique (X)-Centre National d'Études Spatiales [Toulouse] (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-École normale supérieure - Paris (ENS Paris)

Subjects
[SDU.STU.GP]Sciences of the Universe [physics]/Earth Sciences/Geophysics [physics.geo-ph], [PHYS.PHYS.PHYS-GEO-PH]Physics [physics]/Physics [physics]/Geophysics [physics.geo-ph]
Abstract

International audience; The Eastern Mediterranean Sea (EMS) lies in a climatological transition zone, under the influence of both tropical and mid-latitude climate processes. Early Holocene sediment records collected in the EMS bear witnesses for the formation of the most recent sapropel S1, closely associated with distinct minima in the orbital precession cycle and the insolation-driven monsoon maxima. The different scenarios of S1 deposition involve changes in marine productivity, organic matter preservation and circulation changes and are still under debate. Herewith, we focus on combined geochemical and micropaleontological proxies, namely organic biomarkers, organic carbon and nitrogen stable isotopes and coccolithophore assemblages, aiming at reconstructing climate-related parameters such as sea surface temperature (SST), marine productivity patterns, stratification and nutricline fluctuations and continental inputs in three gravity cores collected along a north-south transect in the EMS. Depending on the water column depth, the sediment accumulation rates and the hydrographic circulation patterns, S1 deposited in our records between ~9.8 to 6.4 kyr BP. During the Holocene climatic optimum, SSTs increase gradually more than 4° C and reaches values as high as 21.2° C, 22.5° C and 23° C along the N-S transect. Our records also show a pronounced centennial-scale cooling that culminates at ~ 8.0 kyrs BP, coeval to the N. Atlantic cooling event, causing an interruption in the deposition of S1 in all sites. Moreover, SST fluctuations are detected between 4.9 and 4.1 kyr BP, with a sharp positive shift to 24.9° C indicating the presence of a warm period in the mid Holocene. Higher accumulation rates of TOC, marine biomarkers and coccolithophore assemblages were recorded during the S1a, S1b and Mid Holocene Humid (MHH) phases, indicating higher productivity and/or better preservation of organic matter. Furthermore, distribution patterns, composition and characteristic ratios of marine biomarkers and of coccolithophoride species exhibit variability in paleoproductivity trends, hydrographic dynamics and nutricline levels during the Holocene. The distributions of land plant biomarkers are indicative of variable terrigenous organic matter supply and the concomitant transport of nutrients to surface waters. The different types of δ13Corg excursions associated with stronger fluvial delivery (terrestrial inputs) in the north site, whereas the other two sites received most marine organic matter. Lighter values of δ15N within S1 and MHH phases reflect a significant contribution of N-fixing organisms to the N-cycle, related probably to higher demand for nitrogen due to the established dysoxia in the water column/sediment interface, leading to denitrification and P regeneration.

Published
2012

48. Poster session 1GENERAL PRINCIPLESP194Ultrasound indexes of adipose tissue and lipid goals attainment in high and very high cardiovascular risk patientsTHE IMAGING EXAMINATIONP195Right ventricular global longitudinal strain provides higher prognostic value than right free wall longitudinal strain in patients with left heart diseaseP196Normal values of echocardiographlc left and right cardiac chambers dimensions as multifactorially determined by sex, level of physical activity, age, BMI, systolic blood pressure and heart rateAnatomy and physiology of the heart and great vesselsP197Echocardiographic phenotypes according to levels of oxygen consumption at peak exercise: findings from the EURO(pean) EX(ercise) population-based studyAnatomy and physiology of the heart and great vesselsP198Systemic vascular resistance and central arterial stiffness in relation to left ventricular geometry and diastolic function in essential hypertensionAssessment of diameters, volumes and massP199Left atrial diameter predicts a new diagnosis of paroxysmal atrial fibrillation in a population presenting with palpitationsP200Interventricular septum thickness and acute coronary syndromes: small differences, big prognostic influence?P201Detection of abdominal aortic aneurysm in a population referred for an ultrasonographyAssessments of haemodynamicsP202The ultrasound vector velocity method transverse oscillation validated in a flowrig with constant and pulsatile flow and in-vivo of blood flow in the ascending aortaASSESSMENT OF SYSTOLIC FUNCTIONP203Different types of left ventrical remodeling in children with arterial hypertensionP204Assessment of myocardial performance index in hypertensive patients with or without hyperuricemiaP205Strain echocardiography detects mild impairment of systolic function in patients with frequent premature ventricular contractionsP206Speckle tracking strain correlates better with functional capacity and hemodynamic burden than ejection fraction in patients with severe heart failureP207Prognostic value of 2D and 3D echocardiographic volumes, ejection fraction and strain as markers of abnormal left ventricular performanceP208Long-term prognostic value of left ventricular ejection fraction assessed by echocardiography and magnetic resonance imaging after acute STEMIP209Assessment of left ventricular function after percutaneous coronary intervention of chronic total occluded coronary artery by speckle tracking and cardiac magnetic resonanceP210Physiologic variations of tricuspid annular plane systolic excursion in healthy subjects: clinical and echocardiographic correlatesP211Predictors of incipient ventricular dysfunction with tyrosine kinase inhibitors in metastatic renal cell carcinomaAssessment of diastolic functionP212Disagreement between the American Society of Echocardiography (ASE) and gastroenterology-based guidelines for the diagnosis of diastolic dysfunction among patients with advanced liver diseaseP213Nomograms for mitral inflow doppler and tissue doppler velocities in caucasian childrenP215Diastolic function is impaired in women with angina pectoris and no obstructive coronary artery disease independently of coronary microvascular functionP216Clinical value of myocardial performance index in patients with isolated diastolic dysfunctionIschemic heart diseaseP217Cardiac imaging strategy is clinically more effective and at lower cost than traditional ETT strategy for the diagnosis of stable coronary artery diseaseP218Does the ESC clinical pretest probability score stratify our patients correctly? Validation with stress echocardiographyP219Incremental value of exercise echocardiography over exercise electrocardiography in a chest pain unit: a decision curve analysisP220A bedside echocardiographic score for risk stratification of ST-elevation myocardial infarction patients undergoing primary percutaneous coronary interventionP221Interventricular and intraventricular dyssynchrony in patients with Q-wave acute myocardial infarctionP222Comparison of tagging and tissue tracking for myocardial strain assessment at 1.5T and 3.0T following ST-segment elevation myocardial infarctionP223Left atrial strain rate evaluated by two-dimensional speckle tracking is predictor of left ventricular arrhythmias in STEMI patients treated by primary PCIP224Impact of percutaneous coronary intervention of chronic total oclussion on left ventricular function using speckle tracking and cardiac magnetic resonanceHeart valve DiseasesP225Clinical and echocardiographic characteristics of patients with low flow severe aortic stenosis and preserved ejection fractionP226Ventricular-arterial interplay in patients with severe aortic stenosis: additional role of wave intensity analysisP227Degenerative aortic stenosis: don't forget the vascular componentP228Reclassifying low gradient aortic stenosis with 3D transesophageal echocardiography and global longitudinal strainP229Importance of mitral regurgitation on pre- and postoperative clinical status and echocardiographic findings in patients with severe aortic stenosis admitted for aortic valve replacementsP230Aorto-septal angle and degenerative aortic stenosis: a case-control study stenosisP231Difference of sST2 level in mitral stenosis compare with control subjectsP232Velocity-time integral of aortic regurgitation: a novel echocardiographic marker in the evaluation of aortic regurgitation severityP233Color doppler 3D echocardiography-derived regurgitant volume in primary mitral regurgitation: a comparison of different techniques with magnetic resonanceP234Outcome of surgery for degenerative mitral regurgitationP235Mitral valve repair or replacement for functional regurgitation and left ventricular dysfunction: clinical and echocardiographic outcomeP236Prevalence, characteristics and prognosis of moderate to severe tricuspid regurgitation in patients with precapillary pulmonary hypertensionP237Management of late bioprosthetic mitral valve thrombosisP238Relationship between pulmonary venous flow and prosthetic mitral valve thrombosisP239Transcatheter aortic valve implantation does not reduce acutely valvuloarterial impedance in an elderly population with degenerative calcific aortic valve stenosisP240Influence of type of prosthesis on mitral regurgitation change after transcatheter aortic valve replacement for aortic stenosisP241The prevalence of valve disease in patients undergoing atrial fibrillation ablationCardiomyopathiesP242The prognostic value of lung ultrasound at discharge in heart failureP243Prognostic value of global longitudinal strain in non-ischaemic dilated cardiomyopathyP244Additional effect of high intensity exercise training to cardiac resynchronization in heart failure: the reduction on left venticular massP245Dobutamine-induced changes of longitundinal strain predicts longterm mortality in severe heart failureP246Myocardial fibrosis is not related to two-dimensional longitudinal strain in dilated cardiomyopathyP247Echocardiographic parameters are predictors of positive genetic study in a Portuguese population with hypertrophic cardiomyopathy: a multicentre studyP248Myocardial deformation techniques for the evaluation of the right ventricle in fabry diseaseP249Borderline hypertrophic cardiomyopathy or athlete's heart: what is the role for genetic testing in athletes?P250Isolated papillary muscle hypertrophy. Clinical, electrocardiographic and morphologic characteristicsP251Prognostic value of the assessment of left atrial deformation in hypertrophic cardiomyopathyP252Assessment of subtle echocardiographic changes may improve risk stratification of arrhythmias in early stages of arrhythmogenic right ventricular cardiomyopathy (ARVC)P253Long-term correlation of electrocardiography with structural echocardiography changes in patients with arrhythmogenic right ventricular cardiomyopathyP254Right ventricular strain and dyssynchrony assessment in arrhythmogenic right ventricular cardiomyopathy: a cardiac magnetic resonance feature-tracking studyP255Association of non compaction and hypertrophic cardiomyopathies, Noonan and long QT syndromesP256Predictors of mortality in patients with acute myocarditisP257Clinical characteristics and natural history of acute myocarditisP258One-beat 3dimensional echocardiography for the assessment of right ventricular function in heart transplant recipientsP259Hemodynamically irrelevant, non-surgery related pericardial effusion is a predictor of mortality in heart transplanted patientsSystemic diseases and other conditionsP260Left ventricular function as a cardiac marker of target organ damage in non-diabetic, never treated hypertensive patients: Camparison with microalbuminuriaP261Subclinical myocardial dysfunction in hypertensive patients with hyperuricemiaP262Can deformation indices (strain/strain rate) establish differential diagnosis in infiltrative cardiomyopathies?P263Prevalence and factors associated with inappropriately high left ventricular mass in patients with rheumatoid arthritisP264Echocardiographic evaluation of patients with end-stage liver disease, the importance of follow up after liver transplantationP265Cardiovasclular involvement in asymptomatic juvenile localized scleroderma patientsP267Can the left ventricular mechanics using speckle tracking echocardiography in pregnancy predict the new onset heart failure?P268What causes impaired exercise tolerance in HFpEF? Relative contribution from LV filling pressure and other factorsCongenital heart diseaseP269Pregnancy in patients with Ebsteins anomaly - echocardiographic and clinical studyP270Double aortic arch anomalies in clinical practiceP271Echocardiography as the essential imaging modality in congenital heart disease - first one to begin with and the one who staysMasses, tumors and sources of embolismP272Can the reduction of wall shear stress in diskinetic myocardial wall segments be used to predict trombogenicity?Diseases of the aortaP273The role of modified transoesophageal echocardiography for optimal access decision making for transcatheter aortic valve replacement proceduresStress echocardiographyP274Is aortic valve resistance different in patients with severe aortic stenosis and left ventricular fraction below 40% with low or high gradient?P275Does wall motion score index in dobutamine stress echocardiography predict syntax score in catheterization lab?P276Sex-related differences in peak stress left ventricular global longitudinal strain during dobutamine stress echocardiography in patients with significant coronary artery diseaseP277Exercise stress echocardiography complications: a 4-year single center experienceP278Reduced baseline left ventricular longitudinal systolic function is a marker of inducible myocardial ischemia in patients undergoing exercise echocardiographyP279Estimation of mean pulmonary arterial pressure based on right ventricle systolic pressure observed from exercise echocardiography among non-pulmonary hypertension with systemic sclerosisTransesophageal echocardiographyP280Transoesophageal echocardiography in patients with neuroendocrine tumour and carcinoid symptoms is safe without intravenous octreotideP281The feasibility and the clinical benefit of the cognitive-behavioral intervention for preparing patients for transesophageal echocardiographic studyP282Dynamic changes of mitral annulus shape in different types of mitral valve prolapse. A three-dimensional transoesophageal studyReal-time three-dimensional TEEP283Severe aortic stenosis: evaluation of effective and anatomy valve by 2D transthoracic echocardiography and 3D transesophageal echocardiographyP2843D-transeosphageal echocardiography usefulness for assessment of cardiac output in intensive care unit: an ultrasound versus thermodilution comparative study for patients under mechanical ventilationP285The predictive value of three-dimensional vena-contracta in determining the number of MitraClip devices needed during the procedure in functional mitral regurgitationTissue Doppler and speckle trackingP286Should the septum be included in the assessment of right ventricular longitudinal strain?P287Can machine learning help to identify heart failure with preserved ejection fraction?P288Concordance of atrial function measurement by 3D volumetric echocardiography and speckle tracking deformation imagingP289Heterogonous regional diastolic function revealed by 2D speckle tracking echocardiography identifies patients with ischemic etiology of left ventricular systolic dysfunctionP290The values from Real time 3-dimensional strain is not independent from preload changesP291Risk stratification in hypertrophic cardiomyopathy. a potential role for speckle-tracking parameters by cardiac magnetic resonanceP292Abnormal longitudinal peak systolic strain in asymptomatic patients with type-I diabetes mellitusP294Strain evaluation of subclinical cardiac dysfunction in patients with myotonic dystrophy type 1P295Heart function assessment in perinatal asphyxia; speckle tracking indices from greyscale recordings perform better than from tissue Doppler recordings, fractional shortening and tissue Doppler indicesP297Longitudinal strain assessed by automatic function imaging - a useful tool in significant coronary artery disease detection in patients with low risk anginaP298Global 2-Dimensional strain as a predictor of mortality in heart transplant patients with cardiac allograft vasculopathyP299Two-dimensional longitudinal strain and strain rate in asymptomatic middle-aged patients with type 2 diabetes mellitus - a pilot study resultsP300Limited accuracy of myocardial deformation imaging in diagnosis of left ventricular segmental dysfunction in patients with acute myocardial infarction: is it only a limitation of the strain software?Computed Tomography & Nuclear CardiologyP301Evaluation of the actual prevalence of myocardial ischemia in patients prior to performing a peripheral vascular surgeryP302Prognostic value of myocardial ischemia detected by myocardial perfusion imaging in asymptomatic patients with diabetes type 2P303Economic cost analysis derived by coronary computed tomography angiography inappropriate indications to rule out coronary heart disease

Author

Haberka, M, primary, Garcia Martin, A, primary, Barbier, P, primary, Pellegrino, M, primary, Angelis, A, primary, Howlett, PJ, primary, Madeira, M, primary, Carrero, PJ, primary, Hansen, KL, primary, Trunina, I, primary, Basar, C, primary, Lie, OH, primary, Sade, LE, primary, Gopal, A S, primary, Klug, G, primary, Rodriguez Gonzalez, E, primary, Ferrara, F, primary, Moustafa, S, primary, Naksuk, N, primary, Cantinotti, M, primary, Michelsen, MM, primary, Fernandes, JMG, primary, Demir, OM, primary, Cano Carrizal, R, primary, Bouzas-Mosquera, A, primary, Leao, S, primary, Kuznetsov, VA, primary, Nazir, S A, primary, Trifunovic, D, primary, Spampinato, RA, primary, Antonini-Canterin, F, primary, Ribeiro, JM, primary, Morgado, GJ, primary, Reis, L, primary, Naratrekoon, B, primary, Soto-Ruiz, RM, primary, Penicka, M, primary, Zilberszac, R, primary, De Chiara, B, primary, Rifai, R, primary, Gunduz, S, primary, Cersit, S, primary, Devecchi, C, primary, Ancona, F, primary, Smith, D, primary, Gargani, L, primary, Asmarats Serra, L, primary, Abreu, A, primary, Ikonomidis, I, primary, Biernacka, B, primary, Gomes, AC, primary, Caballero, L, primary, Mansencal, N, primary, Venturini, C, primary, Zaroui, A, primary, Leren, I S, primary, Astrom Aneq, M, primary, Nucifora, G, primary, Rocon, CRLA, primary, Cho, J Y, primary, Stampfli, S F, primary, Cho, EJ, primary, Stevanovic, A, primary, Pena, J L, primary, Ognibeni, F, primary, Colunga, S, primary, Borowiec, A, primary, Hristova, K, primary, Kosmala, W, primary, Lesniak-Sobelga, A M, primary, Kaldararova, M, primary, Stanojevic, D, primary, Carbonell San Roman, A, primary, Hoetink, A, primary, Ferreira, R, primary, Rohani, A, primary, Wierzbowska-Drabik, K, primary, Carvalho, J F, primary, Cherubini, A, primary, Teramoto, K, primary, May, CJH, primary, Wejner-Mik, P, primary, Gurzun, M M, primary, Perea, GO, primary, Laveau, F, primary, Mahmoud, HM, primary, Sanz, M, primary, Sanchez-Martinez, S, primary, Montserrat, S, primary, Kowalczyk, E, primary, Park, CS, primary, Hinojar, R, primary, Van Berendoncks, A M, primary, Guedes, H, primary, Nestaas, E, primary, Onut, R, primary, Moran, L, primary, Kisko, A, primary, Agmon, Y, primary, Corneli, M, primary, Peovska Mitevska, IPM, primary, Barreiro Perez, M, primary, Banska, K, additional, Gasior, Z, additional, Moya-Mur, JL, additional, Carbonell-San Roman, S-A, additional, Rodriguez-Munoz, D, additional, Garcia-Lledo, A, additional, Casas-Rojo, E, additional, Hinojar, R, additional, Jimenez-Nacher, JJ, additional, Fernandez-Golfin, C, additional, Zamorano-Gomez, JL, additional, Ravani, A, additional, Cefalu, C, additional, Maltagliati, A, additional, Frigerio, B, additional, Sansaro, D, additional, Amato, M, additional, Baldassarre, D, additional, Bandera, F, additional, Generati, G, additional, Labate, V, additional, Alfonzetti, E, additional, Guazzi, M, additional, Aggeli, K, additional, Ioakeimidis, N, additional, Abdelrasoul, M, additional, Felekos, I, additional, Gourgouli, I, additional, Aznaouridis, K, additional, Rousakis, G, additional, Vlachopoulos, C, additional, Tousoulis, D, additional, Darasz, K, additional, Mahmoudi, M, additional, Shah, N, additional, Jabr, RI, additional, Hickman, M, additional, Leatham, EW, additional, Fry, CH, additional, Teixeira, R, additional, Almeida, I, additional, Caetano, F, additional, Fernandes, A, additional, Cassandra, M, additional, Reis, L, additional, Costa, M, additional, Goncalves, L, additional, Nielsen, AJ, additional, Carrero, MC, additional, Saubidet, GL, additional, Peralta, SP, additional, Moeller-Soerensen, H, additional, Kjaergaard, J, additional, Jensen, MB, additional, Lund, JT, additional, Pedersen, MM, additional, Olesen, JB, additional, Jensen, JA, additional, Nielsen, MB, additional, Sharykin, AS, additional, Karelina, EV, additional, Telezhnikova, ND, additional, Ozhan, H, additional, Kayapinar, O, additional, Albayrak, ES, additional, Saberniak, J, additional, Dejgaard, L, additional, Nestaas, E, additional, Edvardsen, T, additional, Haugaa, KH, additional, Bal, U, additional, Eroglu, S, additional, Pirat, B, additional, Muderrisoglu, H, additional, Muthukumar, L, additional, Saha, SK, additional, Toole, RS, additional, Reinstadler, S, additional, Feistritzer, HJ, additional, Pernter, B, additional, Mayr, A, additional, Franz, WM, additional, Mueller, S, additional, Metzler, B, additional, Mingo Santos, S, additional, Palomero Monivas, V, additional, Gonzalez Mirelis, J, additional, Goirigolzarri Artaza, J, additional, Zorita Gil, B, additional, Fernandez Diaz, JA, additional, Goicolea Ruigomez, J, additional, Restrepo Cordoba, MA, additional, Alonso Pulpon, L, additional, Gargani, L, additional, D'alto, M, additional, Ghio, S, additional, Acri, E, additional, Carannante, L, additional, Argiento, P, additional, D'andrea, A, additional, Vriz, O, additional, Bossone, E, additional, Ho, TH, additional, Shah, P, additional, Murphy, K, additional, Nelluri, BK, additional, Lee, H, additional, Wilansky, S, additional, Mookadam, F, additional, Peeraphatdit, T, additional, Chaiteerakij, R, additional, Klarich, KW, additional, Scalese, M, additional, Melo, M, additional, Assanta, N, additional, Marotta, M, additional, Crocetti, M, additional, Spadoni, I, additional, Giordano, R, additional, Kutty, S, additional, Iervasi, I, additional, Mygind, ND, additional, Pena, A, additional, Frestad, D, additional, Hoest, N, additional, Prescott, E, additional, Romao, BO, additional, Rivera, IR, additional, Mendonca, MA, additional, Carvalho, AC, additional, Campos, O, additional, Amato, A, additional, Moises, VA, additional, Bashir, A, additional, Marshall, K, additional, Douglas, M, additional, Wasan, B, additional, Plein, S, additional, Alfakih, K, additional, Casanova Rodriguez, C, additional, Cadenas Chamorro, R, additional, Iglesias Del Valle, D, additional, Martin-Penato Molina, A, additional, De Juan Baguda, J, additional, Prieto Moriche, E, additional, Garcia Garcia, A, additional, De La Cruz Berlanga, E, additional, Plaza Perez, I, additional, Peteiro, J, additional, Broullon, FJ, additional, Alvarez-Garcia, N, additional, Barbeito-Caamano, C, additional, Larranaga-Moreira, JM, additional, Maneiro-Melon, N, additional, Martinez-Ruiz, D, additional, Yanez, JC, additional, Vazquez-Rodriguez, JM, additional, Cordeiro, F, additional, Magalhaes, P, additional, Moz, M, additional, Trigo, J, additional, Mateus, P, additional, Fontes, P, additional, Moreira, I, additional, Krinochkin, DV, additional, Plusnin, AV, additional, Soldatova, AM, additional, Shetye, A, additional, Khan, JN, additional, Singh, A, additional, Kanagala, P, additional, Swarbrick, DJ, additional, Graham-Brown, M, additional, Mccann, GP, additional, Krljanac, G, additional, Savic, L, additional, Asanin, M, additional, Aleksandric, S, additional, Lasica, R, additional, Srdic, M, additional, Zlatic, N, additional, Petrovic, M, additional, Mrdovic, I, additional, Monivas Palomero, V, additional, Rivero Arribas, B, additional, Dobrovie, M, additional, Da Rocha E Silva, JG, additional, Bonamigo Thome, F, additional, Kluttig, R, additional, Schloma, V, additional, Dmitrieva, Y, additional, Strotdrees, E, additional, Mohr, FW, additional, Luzza, G, additional, Caruso, R, additional, Belfiore, R, additional, Della Mattia, A, additional, Poli, S, additional, Zito, C, additional, La Carrubba, S, additional, Carerj, S, additional, Carvalho, JF, additional, Gomes, AC, additional, Caldeira, D, additional, Cruz, IR, additional, Stuart, B, additional, Maia, R, additional, Fazendas, P, additional, Pereira, H, additional, Rakocevic, I, additional, Tutos, V, additional, Petrovic, O, additional, Boricic-Kostic, M, additional, Stepanovic, J, additional, Jovanovic, I, additional, Banovic, M, additional, Vujisic-Tesic, B, additional, Leite, L, additional, Madeira, M, additional, Botelho, A, additional, Santos, M, additional, Nascimento, J, additional, Yingchoncharoen, T, additional, Vathesatogkit, P, additional, Yamwong, S, additional, Sritara, P, additional, Bonaque Gonzalez, J C, additional, Abellan-Huerta, J, additional, Rubio-Paton, R, additional, Soria, F, additional, Ramos, JL, additional, Egea, S, additional, Garcia-Gomez, J, additional, Martinez Diaz, JJ, additional, Castillo, JA, additional, Vecera, J, additional, Mirica, C, additional, Kotrc, M, additional, Kockova, R, additional, Gabriel, H, additional, Maurer, G, additional, Rosenhek, R, additional, Botta, L, additional, Musca, F, additional, Belli, O, additional, Costetti, A, additional, Trolese, I, additional, Spano, F, additional, Russo, C, additional, Giannattasio, C, additional, Moreo, A, additional, Berthelot, E, additional, Le, MT, additional, Hilpert, L, additional, Montani, D, additional, Sitbon, O, additional, Jais, X, additional, Humbert, M, additional, Assayag, P, additional, Yesin, M, additional, Kalcik, M, additional, Gursoy, MO, additional, Cersit, S, additional, Astarcioglu, MA, additional, Karakoyun, S, additional, Aykan, AC, additional, Ozkan, M, additional, Gunduz, S, additional, Tabakci, M, additional, Bayam, E, additional, Degiovanni, A, additional, Di Ruocco, MV, additional, Marino, P, additional, Rosa, I, additional, Stella, S, additional, Barletta, M, additional, Marini, C, additional, Latib, A, additional, Montorfano, M, additional, Colombo, A, additional, Margonato, A, additional, Agricola, E, additional, Ray, R, additional, Gallagher, M, additional, Nazir, M, additional, Perreso, V, additional, Sharma, R, additional, Pang, PS, additional, Miglioranza, M, additional, Landi, P, additional, Dini, FL, additional, Picano, E, additional, Pons Llinares, J, additional, Macaya Ten, F, additional, Pericas Ramis, P, additional, Caldes Llull, O, additional, Grau Sepulveda, A, additional, Frontera, G, additional, Bethencourt, A, additional, Santa Clara, H, additional, Santos, V, additional, Oliveira, M, additional, Cunha, P, additional, Portugal, G, additional, Rio, P, additional, Branco, L, additional, Ferreira, R, additional, Mota Carmo, M, additional, Paraskevaidis, I, additional, Papadopoulos, C, additional, Stasinos, V, additional, Parissis, J, additional, Lekakis, J, additional, Rubis, P, additional, Gackowski, A, additional, Wisniowska-Smialek, S, additional, Lesniak-Sobelga, A, additional, Kostkiewicz, M, additional, Bento, D, additional, Correia, E, additional, Teles, L, additional, Picarra, B, additional, Lourenco, C, additional, Faria, R, additional, Domingues, K, additional, Azevedo, O, additional, Climent Paya, V, additional, Martinez Moreno, M, additional, Gimeno, JR, additional, Oliva, MJ, additional, Saura, D, additional, Sanchez Quinones, J, additional, Garcia Honrubia, A, additional, Valdes, M, additional, De La Morena, G, additional, Richard, P, additional, Guerard, S, additional, Brion, R, additional, Paul, P, additional, Dubourg, O, additional, Komajda, M, additional, Isnard, R, additional, Arslan, M, additional, Charron, P, additional, Avegliano, G, additional, Andres, S, additional, Costabel, JP, additional, Kuschnir, P, additional, Sciancalepore, A, additional, Mendoza, O, additional, Perea, G, additional, Ronderos, R, additional, Ben Said, RYM, additional, EL Chalbia, TEJ, additional, Wali, SANA, additional, Mourali, MS, additional, Mechmeche, RACHID, additional, Haland, TF, additional, Svetlichnaya, J S, additional, Shikha, SS, additional, Scheinmann, MS, additional, Klein, LK, additional, Prati, G, additional, Vitrella, G, additional, Allocca, G, additional, Cukon Buttignoni, S, additional, Muser, D, additional, Morocutti, G, additional, Pinamonti, B, additional, Sinagra, G, additional, Proclemer, A, additional, Melo, MDTM, additional, Bocchi, EAB, additional, Araujo, JABAF, additional, Demarchi, LMMFD, additional, Mady, CM, additional, Biselli, BB, additional, Kalil, RKF, additional, Salemi, VMCS, additional, Tuma, RT, additional, Kim, K H, additional, Yoon, H J, additional, Lee, K J, additional, Park, H, additional, Kim, J H, additional, Ahn, Y, additional, Jeong, M H, additional, Cho, J G, additional, Park, J C, additional, Park, H J, additional, Kozan, H, additional, Sezgin, A, additional, Aydinalp, A, additional, Oezkartal, T, additional, Bernhart, S, additional, Flammer, AJ, additional, Vecchiati, A, additional, Froehlich, GM, additional, Ruschitzka, F, additional, Tanner, FC, additional, Choi, KY, additional, Kim, DB, additional, Jang, SW, additional, Cho, JS, additional, Park, CS, additional, Jung, HO, additional, Jeon, HK, additional, Youn, HJ, additional, Dekleva, M, additional, Fortes, PRL, additional, Passos, BR, additional, Rodrigues, AB, additional, Sampaio, IH, additional, Oliveira, MCN, additional, Silva, MG, additional, Cardoso, RAF, additional, Tofani, FA, additional, Moreira, MCV, additional, Cioffi, G, additional, Viapiana, O, additional, Dalbeni, A, additional, Fracassi, E, additional, Di Nora, C, additional, Cherubini, A, additional, Mazzone, C, additional, Di Lenarda, A, additional, Rossini, M, additional, Corros, C, additional, Garcia-Campos, A, additional, Martin, M, additional, Rodriguez-Suarez, M, additional, Leon, V, additional, Fidalgo, A, additional, Lopez-Iglesias, F, additional, Moris, C, additional, De La Hera, JM, additional, Dabrowski, R, additional, Wozniak, J, additional, Jasek, S, additional, Chwyczko, T, additional, Kowalik, I, additional, Musiej-Nowakowska, E, additional, Szwed, H, additional, Marinov, R, additional, Stamenov, G, additional, Mihova, M, additional, Chacheva, K, additional, Persenska, S, additional, Racheva, A, additional, Przewlocka-Kosmala, M, additional, Rojek, A, additional, Karolko, B, additional, Mysiak, A, additional, Marwick, TH, additional, Biernacka, B, additional, Tittel, P, additional, Kardos, M, additional, Vrsanska, V, additional, Ondriska, M, additional, Hraska, V, additional, Nosal, M, additional, Masura, J, additional, Simkova, I, additional, Apostolovic, S, additional, Salinger-Martinovic, S, additional, Jankovic-Tomasevic, R, additional, Djordjevic-Radojkovic, D, additional, Stanojlovic, T, additional, Atanaskovic, V, additional, Pavlovic, M, additional, Tahirovic, E, additional, Dungen, HD, additional, Moya Mur, JL, additional, Lozano Granero, C, additional, Jimenez Nacher, JJ, additional, Gonzalez Gomez, A, additional, Fraile Sanz, C, additional, Segura De La Cal, T, additional, Zamorano Gomez, JL, additional, Jansen Klomp, WW, additional, Van 'T Hof, AWJ, additional, Brandon Bravo Bruinsma, GJ, additional, Spanjersberg, AJ, additional, Grandjean, J, additional, Nierich, AP, additional, Ferreira, J, additional, Lazaro Mendes, S, additional, Martins, R, additional, Monteiro, S, additional, Pego, M, additional, Khamene Bagheri, R, additional, Peruga, JZ, additional, Sobczak, M, additional, Plewka, M, additional, Wcislo, T, additional, Krecki, R, additional, Kasprzak, JD, additional, Morgado, G, additional, Cruz, I, additional, Almeida, AR, additional, Joao, I, additional, Lopes, L, additional, Cotrim, C, additional, Faganello, G, additional, Pandullo, C, additional, Russo, G, additional, Stefenelli, C, additional, Furlanello, F, additional, Tarantini, L, additional, Suzuki, K, additional, Satoh, Y, additional, Minami, K, additional, Mizukoshi, K, additional, Kamijima, R, additional, Kou, S, additional, Takai, M, additional, Izumo, M, additional, Akashi, YJ, additional, Ayuk, J, additional, Geh, I, additional, Shah, T, additional, Edwards, NC, additional, Steeds, RP, additional, Miskowiec, D, additional, Wdowiak-Okrojek, K, additional, Lipiec, P, additional, Rosca, M, additional, Calin, A, additional, Beladan, C, additional, Serban, M, additional, Ginghina, C, additional, Popescu, BA, additional, Lombardero, M, additional, Henquin, R, additional, Corneli, M, additional, Tinetti, M, additional, Hekimian, G, additional, Achkar, M, additional, Combes, A, additional, Hammoudi, N, additional, Al-Ghamdi, M, additional, Ghabashi, A, additional, Ezzat, M H, additional, Al-Amin, A, additional, Giraldeau, G, additional, Sarvari, SI, additional, Marin, J, additional, Brambila, C, additional, Gabrielli, L, additional, Bijnens, B, additional, Sitges, M, additional, Duchateau, N, additional, Erdei, T, additional, Fraser, A, additional, Bijnens, B H, additional, Piella, G, additional, Sanchis, L, additional, Borras, R, additional, Vidal, B, additional, Prat, S, additional, Azqueta, M, additional, Pare, C, additional, Grazioli, G, additional, Sanz, M, additional, Wejner-Mik, P, additional, Jung, MH, additional, Ahn, HS, additional, Kim, JH, additional, Megias, A, additional, Alonso, GL, additional, Gonzalez-Gomez, A, additional, Rincon, LM, additional, Esteban, A, additional, Fernandez Mendez, MA, additional, Barrios, V, additional, Zamorano, JL, additional, Van Gaal, L, additional, De Block, C, additional, Salgado, R, additional, Vrints, C, additional, Shivalkar, B, additional, Pereira, A, additional, Santos, R, additional, Marques, L, additional, Moreno, N, additional, Carvalho, R, additional, Pires, M, additional, Sousa, R, additional, Andrade, A, additional, Pinto, P, additional, Stoylen, A, additional, Fugelseth, D, additional, Tautu, O, additional, Onciul, S, additional, Marinescu, C, additional, Zamfir, D, additional, Dorobantu, M, additional, Sanchez Sanchez, V, additional, Navas, P, additional, Garcia-Cosio, D, additional, Diaz, B, additional, Carballo-Alzola, L, additional, Lombera, F, additional, Delgado, J, additional, Babcak, M, additional, Kishko, N, additional, Eitan, A, additional, Mutlak, D, additional, Kehat, I, additional, Meretta, AH, additional, Perea, GO, additional, Belcastro, F, additional, Aguirre, E, additional, Rosa, D, additional, Zaefferer, P, additional, Masoli, O, additional, Srbinovska, ES, additional, Bosevski, MB, additional, Antova, EA, additional, Pop Gorceva, DPG, additional, Martin Fernandez, M, additional, Costilla Garcia, SM, additional, Diaz Pelaez, E, additional, and Moris De La Tassa, C, additional

Published
2015
Full Text
View/download PDF

49. Poster session 5The imaging examinationP1097Correlation between visual and quantitative assessment of left ventricle: intra- and inter-observer agreementP1099Incremental prognostic value of late gadolinium-enhanced by cardiac magnetic resonance in patients with heart failureAnatomy and physiology of the heart and great vesselsP1100Left ventricular geometry and diastolic performance in erectile dysfunction patients; a topic of differential arterial stiffness influenceAssessment of diameters, volumes and massP1101Impact of the percutaneous closure of atrial septal defect on the right heart "remodeling"P1102Left Ventricular Mass Indexation in Infants, Children and Adolescents: a Simplified Approach for the Identification of Left Ventricular Hypertrophy in Clinical PracticeP1103Impact of trabecules while quantifying cardiac magnetic resonance exams in patients with systemic right ventricleP1104Detection of subclinical atherosclerosis by carotid intima-media thickness: correlation with leukocytes telomere shorteningAssessments of haemodynamicsP1105Flow redirection towards the left ventricular outflow tract: vortex formation is not affected by variations in atrio-ventricular delayAssessment of systolic functionP1106Reproducibility and feasibility of cardiac MRI feature tracking in Fabry diseaseP1107Normal left ventricular strain values by two-dimensional strain echocardiography; result of normal (normal echocardiographic dimensions and functions in korean people) studyP1108Test-retest repeatability of global strain following st-elevation myocardial infarction - a comparison of tagging and feature trackingP1109Cardiotoxicity induced by tyrosine kinase inhibitors in patients with gastrointestinal stromal tumors (GIST)P1110Finite strain ellipses for the analysis of left ventricular principal strain directions using 3d speckle tracking echocardiographyP1111Antihypertensive therapy reduces time to peak longitudinal strainP1112Right ventricular systolic function as a marker of prognosis after inferior myocardial infarction - 5-year follow-upP1113Is artery pulmonary dilatation related with right but also early left ventricle dysfunction in pulmonary artery hypertension?P1114Right ventricular mechanics changes according to pressure overload increasing, a 2D-speckle tracking echocardiographic evaluationAssessment of diastolic functionP1115Paired comparison of left atrial strain from P-wave to P-wave and R-wave to R-waveP1116Diagnostic role of Tissue Doppler Imaging echocardiographic criteria in obese heart failure with preserved ejection fraction patientsP1117Evaluation of diastolic function of right ventricle in idiopathic pulmonary arterial hypertensionP1118Severity and predictors of diastolic dysfunction in a non-hypertensive non-ischemic cohort of Egyptian patients with documented systemic autoimmune disease; pilot reportP1119correlation between ST segment shift and cardiac diastolic function in patients with acute myocardial infarctionIschemic heart diseaseP1120Computed tomography coronary angiography verSus sTRess cArdiac magneTic rEsonance for the manaGement of sYmptomatic revascularized patients: a cost effectiveness study (STRATEGY study)P1121Utility of transmural myocardial mechanic for early infarct size prediction after primary percutaneous coronary intervention in STEMI patientsP1122Progressive Improvements of the echocardiographic deformation parameters in ST Elevation Myocardial Infarction after five years follow-upP1123Long-term prognostic value of left ventricular dyssynchrony as assessed by cardiac magnetic resonance feature-tracking imaging after a first st-segment elevation myocardial infarctionP1124Differences in mitral annulus remodeling in acute anterior ST elevation and acute inferior ST elevation myocardial infarctionP1125Reduction of microvascular injury using a novel theragnostic ultrasound strategy: a first in men feasibility and safety studyP1126Impact of focused echocardiography in clinical decision of patient presented with st elevation myocardial infarction underwent primary angioplastyHeart valve DiseasesP1127Aortic valve area calculation in aortic stenosis: a comparison among conventional and 3D-transesophageal echocardiography and computed tomographyP1128Myocardial fibrosis and microRNA-21 expression in patients with severe aortic valve stenosis and preserved ejection fraction: a 2D speckle tracking echocardiography, tissutal and plasmatic studyP1129Quantification of calcium amount in a new experimental model: a comparison between calibrated integrated backscatter of ultrasound and computed tomographyP1130Altered diffusion capacity in aortic stenosis: role of the right heartP1131Osteoprotegerin predicts all-cause mortality in calcific aortic stenosis patients with preserved left ventricle ejection fraction in long term observationP1132Mitral regurgitation as a risk factor for pulmonary hypertension in patients with aortic stenosisP1133The relationship between the level of plasma B-type natriuretic peptide and mitral stenosisP1134Aortic regurgitation, left ventricle mechanics and vascular load: a single centre 2d derived-speckle tracking studyP1135Feasibility and reproducibility issues limit the usefulness of quantitative colour Doppler parameters in the assessment of chronic aortic and mitral regurgitation severityP1136Predictors of postoperative outcome in degenerative mitral regurgitationP1137Left ventricular mechanical dyssynchrony in patients with severe mitral regurgitation of rheumatic etiology; three dimensional echocardiography studyP1138Functional mitral regurgitation and left atrial dysfunction concur in determining pulmonary hypertension and functional status in subjects with left ventricular systolic dysfunctionP11393D echocardiography allows more effective quantitative assessment of the severity of functional tricuspid regurgitation than conventional 2D/Doppler echocardiographyP1140Prosthetic valve thrombosis: still a severe disease? 10-years experience in a university hospitalP1141Validity of echocardiography in the hospital course of patients with feverP1142Do baseline 3DTEE characteristics of mitral valve apparatus predict long term result in patients undergoing percutaneous valve repair for degenerative regurgitation?P1143Influence of baseline aortic regurgitation on mitral regurgitation change after transcatheter aortic valve replacement for aortic stenosisP1144Prevalence of echocardiography detected significant valvular regurge in subclinical rheumatic carditis in assiut childrenCardiomyopathiesP1145Can we early detect left ventricular systolic dysfunction in patients with Duchenne muscular dystrophy using global longitudinal strain assessment?P1146Prevalence of isolated papillary muscle hypertrophy in young competitive athletesP1147Troponin release after exercise in patients with hypertrophic cardiomyopathy: associations with clinical and mr imaging characteristicsP1148Atrial fibrillation in hypertrophic cardiomyopathy: can we score the risk?P1149Impact of hypertrophy on multiple layer longitudinal deformation in hypertrophy cardiomyopathy and cardiac amyloidosis compared to controlsP1150Functional evaluation in hypertrophic cardiomyopathy combining cardiopulmonary exercise testing combined with exercise-echocardiographyP1151Refinement of the old diagnostic criteria of left ventricular noncompaction cardiomyopathy (LVNC) based on cardiac magnetic resonance (CMR)P1152Differences of clinical characteristics and outcomes between acute myocarditis with preserved and reduced left ventricular systolic functionP1153Value of longitudinal strain for distinguishing left ventricular non-compaction from idiopathic dilated cardiomyopathyP1154Speed of recovery of left ventricular function is not related to the prognosis of Takotsubo cardiomyopathy. A Portuguese multicentre studyP1155Predictors of in-hospital left ventricular systolic function recovery after admission with takotsubo cardiomyopathy. Portuguese multicentre studyP1156Mid-ventricular takotsubo detected by initial echocardiogram associates with recurrence of takotsubo cardiomyopathy - a portuguese multicentre studySystemic diseases and other conditionsP1157Relations between left ventricle remodelling and expression of angiotensin 2 AT2R1 geneP1158Impact of renal denervation on long-term blood pressure variability and surrogate markers of target organ damage in individuals with drug-resistant arterial hypertensionP1159Greater improvement of coronary artery function, left ventricular deformation and twisting by IL12/23 compared to TNF-a inhibition in psoriasisP1160Advanced glycation end products play a role in adverse LV remodeling following MIP1161Incidence of subclinical myocardial dysfunction in patients with systemic sclerosis and normal left ventricular systolic and diastolic functionP1162Left atrial remodeling and dysfunction occur early in patients with systemic sclerosis and normal left ventricular functionP1163Intrinsic vortex formation : a unique performance indicatorP1164P-wave morphology is unaffected by training-induced biatrial dilatation: a prospective, longitudinal study in healthy athletesP1165Usefulness of transthoracic echocardiography in diagnosis of young patients with ischemic strokeP1166Primary cardiac lymphoma: role of echocardiography in the clinical managementP1167Abnormal echocardiographic findings in cancer patients before chemotherapyMasses, tumors and sources of embolismP1168Three-dimensional transesophageal echocardiography of the left atrial appendage reduces rate of postpone electrical cardioversionP1169Detection of ventricular thrombus by cmr after reperfused st-segment elevation myocardial infarction correlated with echocardiographyP1170Clinical and transthoracic echocardiographic predictors of left atrial appendage thrombus in patients with atrial fibrillationStress echocardiographyP1171Pharmacological stress echocardiography complications: a 4-year single center experienceP1172Myocardial functional and perfusion reserve in type I diabetesP1173Feasibility of incorporating 3D Dobutamine stress echocardiography into routine clinical practiceP1174Right ventricular isovolumic acceleration at rest and during exercise in children after heart transplantP1175Right ventricular systolic and diastolic response to exercise in children after heart transplant -a bicycle exercise studyP1176Determinants of functional capacity in heart failure patients with reduced ejection fractionP1177Handgrip stress echocardiography with emotional component compared to conventional isometric exercise in coronary artery disease diagnosisP1178The relationship between resting transthoracic echocardiography and exercise capacity in patients with paroxysmal atrial fibrillationP1179Correlation between NT-proBNP and selected echocardiography parameters at rest and after exercise in patients with functional ischemic mitral regurgitation qualified for cardiosurgical treatmentReal-time three-dimensional TEEP1180Vena contracta area for severity grading in functional and degenerative mitral regurgitation: A study based on transesophageal 3D colour Doppler in 419 patientsP1181Proximal flow convergence by 3D echocardiography in the evaluation of mitral valve area in rheumatic mitral stenosisP1182Quantification of valve dimensions by transesophageal 3D echocardiography in patients with functional and degenerative mitral regurgitationTissue Doppler and speckle trackingP1183Automatic calculation of left ventricular volume changes over a cardiac cycle from echocardiography images by nonlinear dimensionality reductionP1184Effect of the mitral valve repairs on the left ventricular blood flow formationP1185Quantification of left atrial strain using cardiovascular magnetic resonance. a comparison between hypertrophic cardiomyopathy and healthy controlsP1186The role of early systolic lengthening in patients with non-ST elevation acute coronary syndrome and its relation to syntax scoreP1187Different standard two dimensional strain methods to quantity left ventricular mechanicsP1188Atrial function and electrocardiography caracteristics in sportsmen with or without paroxysmal atrial fibrillationP1189Right ventricular outflow premature contractions induce regional left ventricular dysfunctionP1190Ultrasound guided venous access for pacemaker and defibrillators. Randomized TrialP1191Atrial function analysis correlates with symptoms and quality of life of heart failure patientsP1192The use of tissue doppler echocardiography in myocardial iron overload in patients with thalassaemia majorP1193Independent association between pulse pressure and left ventricular global longitudinal strainP1194Global and regional longitudinal strain identifies the presence of coronary artery disease in patients with suspected reduction of coronary flow reserve and absence of wall motion abnormalitiesP1195Prognostic value of invasive and noninvasive parameters of right ventricular function in patients with pulmonary arterial hypertension receiving specific vasodilator therapyP1196Myocardial deformation analysis to improve arrhythmic risk stratificationP1197Quantitative assessment of regional systolic and diastolic function parameters for detecting prior transient ischemia in normokinetic segmentsP1198Left atrial function in patients with corrected tetralogy of Fallot - a three-dimensional speckle-tracking echocardiographic studyP1199Left atrial ejection force correlates with left atrial strain and volume-based functional properties as assessed by three-dimensional speckle tracking echocardiographyP1200Acute angulation of the aortic arch late after the arterial switch operation for transposition of the great arteries: impact on cardiac mechanicsP1201Circumferential deformation of the ascending thoracic aorta in hypertensive patients by three-dimensional speckle tracking echocardiographyCardiac Magnetic ResonanceP1202The incremental value of cardiac magnetic resonance on diagnosis myocardial infarction and non-obstructed coronary arteriesP1204Reference ranges of global and regional myocardial T1 values derived from MOLLI and shMOLLI at 3TComputed Tomography & Nuclear CardiologyP1205Deformation of the left atrial appendage after percutaneous closure with the Amplatzer cardiac plugP1206Prognostic impact of non-obstructive coronary artery disease on coronary computed tomographic angiography: A single-center study

Author

Colunga Blanco, S, primary, Gonzalez Matos, C, primary, Angelis, A, primary, Dinis, P G, primary, Chinali, M, primary, Toth, A, primary, Andreassi, M G, primary, Rodriguez Munoz, D, primary, Reid, A B, primary, Park, JH, primary, Shetye, A, primary, Novo, G, primary, De Marchi, S F, primary, Cikes, M, primary, Smarz, K, primary, Illatopa, V, primary, Peluso, D, primary, Wellnhofer, E, primary, De La Rosa Riestra, A, primary, Sattarzadeh Badkoubeh, R, primary, Mandour Ali, M, primary, Azoz, A, primary, Pontone, G, primary, Krljanac, G, primary, Acar, R, primary, Nucifora, G, primary, Sirtautas, A, primary, Roos, S T, primary, Qasem, M S, primary, Marini, C, primary, Fabiani, I, primary, Gillis, K, primary, Bandera, F, primary, Borowiec, A, primary, Lim, YJ, primary, Chalbia, T E, primary, Santos, M, primary, Gao, S A, primary, Zilberszac, R, primary, Farrag, AAM, primary, Palmiero, G, primary, Aruta, P, primary, De Diego Soler, O, primary, Fasano, D, primary, Tamborini, G, primary, Ancona, F, primary, Raafat, D M, primary, Marchel, M, primary, De Gregorio, C, primary, Gommans, D H F, primary, Godinho, A R, primary, Mielczarek, M, primary, Kubik, M, primary, Cho, J Y, primary, Tarando, F, primary, Lourenco Marmelo, B F, primary, Reis, L, primary, Domingues, K, primary, Krestjyaninov, MV, primary, Mesquita, J, primary, Ikonomidis, I, primary, Ferferieva, V, primary, King, GJ, primary, D'ascenzi, F, primary, Ferrera Duran, C, primary, Sormani, P, primary, Gonzalez Fernandez, O, primary, Tereshina, O, primary, Cambronero Cortinas, E, primary, Kupczynska, K, primary, Carvalho, J F, primary, Shivalkar, B, primary, Aghamohammadzadeh, R, primary, Cifra, B, primary, Kuznetsov, VA, primary, Van Zalen, JJ, primary, Kochanowski, J, primary, Goebel, B, primary, Ladeiras-Lopes, R, primary, Karvandi, M, primary, Alonso Salinas, G, primary, Unkun, T, primary, Ranjbar, S, primary, Hubert, A, primary, Enescu, OA, primary, Liccardo, M, primary, Cameli, M, primary, Ako, E, primary, Lembo, M, primary, Goffredo, C, primary, Enache, R, primary, Wdowiak-Okrojek, K, primary, Nemes, A, primary, Di Salvo, G, primary, Capotosto, L, primary, Caravaca, P, primary, Maceira Gonzalez, A M, primary, Iriart, X, primary, Jug, B, primary, Garcia Campos, A, additional, Capin Sampedro, E, additional, Corros Vicente, C, additional, Martin Fernandez, M, additional, Leon Arguero, V, additional, Fidalgo Arguelles, A, additional, Velasco Alonso, E, additional, Lopez Iglesias, F, additional, De La Hera Galarza, JM, additional, Chaparro-Munoz, M, additional, Recio-Mayoral, A, additional, Vlachopoulos, C, additional, Ioakeimidis, N, additional, Felekos, I, additional, Abdelrasoul, M, additional, Aznaouridis, K, additional, Chrysohoou, C, additional, Rousakis, G, additional, Aggeli, K, additional, Tousoulis, D, additional, Faustino, AC, additional, Paiva, L, additional, Fernandes, A, additional, Costa, M, additional, Cachulo, MC, additional, Goncalves, L, additional, Emma, F, additional, Rinelli, G, additional, Esposito, C, additional, Franceschini, A, additional, Doyon, A, additional, Raimondi, F, additional, Schaefer, F, additional, Pongiglione, G, additional, Mateucci, MC, additional, Vago, H, additional, Juhasz, C, additional, Janosa, C, additional, Oprea, V, additional, Balint, OH, additional, Temesvari, A, additional, Simor, T, additional, Kadar, K, additional, Merkely, B, additional, Bruno, R M, additional, Borghini, A, additional, Stea, F, additional, Gargani, L, additional, Mercuri, A, additional, Sicari, R, additional, Picano, E, additional, Lozano Granero, C, additional, Carbonell San Roman, A, additional, Moya Mur, JL, additional, Fernandez-Golfin, C, additional, Moreno Planas, J, additional, Fernandez Santos, S, additional, Casas Rojo, E, additional, Hernandez-Madrid, A, additional, Zamorano Gomez, JL, additional, Pearce, K, additional, Gamlin, W, additional, Miller, C, additional, Schmitt, M, additional, Seong, IW, additional, Kim, KH, additional, Kim, MJ, additional, Jung, HO, additional, Sohn, IS, additional, Park, SM, additional, Cho, GY, additional, Choi, JO, additional, Park, SW, additional, Nazir, SA, additional, Khan, JN, additional, Singh, A, additional, Kanagala, P, additional, Squire, I, additional, Mccann, GP, additional, Di Lisi, D, additional, Meschisi, MC, additional, Brunco, V, additional, Badalamenti, G, additional, Bronte, E, additional, Russo, A, additional, Novo, S, additional, Von Tscharner, M, additional, Urheim, S, additional, Aakhus, S, additional, Seiler, C, additional, Schmalholz, S, additional, Biering-Sorensen, T, additional, Cheng, S, additional, Oparil, S, additional, Izzo, J, additional, Pitt, B, additional, Solomon, SD, additional, Zaborska, B, additional, Jaxa-Chamiec, T, additional, Tysarowski, M, additional, Budaj, A, additional, Cordova, F, additional, Aguirre, O, additional, Sanabria, S, additional, Ortega, J, additional, Romeo, G, additional, Perazzolo Marra, M, additional, Tona, F, additional, Famoso, G, additional, Pigatto, E, additional, Cozzi, F, additional, Iliceto, S, additional, Badano, LP, additional, Kriatselis, C, additional, Gerds-Li, JH, additional, Kropf, M, additional, Pieske, B, additional, Graefe, M, additional, Martinez Santos, P, additional, Batlle Lopez, E, additional, Vilacosta, I, additional, Sanchez Sauce, B, additional, Espana Barrio, E, additional, Jimenez Valtierra, J, additional, Campuzano Ruiz, R, additional, Alonso Bello, J, additional, Martin Rios, MD, additional, Farrashi, M, additional, Abtahi, H, additional, Sadeghi, H, additional, Sadeghipour, P, additional, Tavoosi, A, additional, Abdel Rahman, TA, additional, Mohamed, LA, additional, Maghraby, HM, additional, Kora, IM, additional, Abdel Hameed, FR, additional, Ali, MN, additional, Al Shehri, A, additional, Youssef, A, additional, Gad, A, additional, Alsharqi, M, additional, Alsaikhan, L, additional, Andreini, D, additional, Rota, C, additional, Guglielmo, M, additional, Mushtaq, S, additional, Baggiano, A, additional, Beltrama, V, additional, Solbiati, A, additional, Guaricci, AI, additional, Pepi, M, additional, Trifunovic, D, additional, Sobic Saranovic, D, additional, Savic, L, additional, Grozdic Milojevic, I, additional, Asanin, M, additional, Srdic, M, additional, Petrovic, M, additional, Zlaic, N, additional, Mrdovic, I, additional, Dogan, C, additional, Izci, S, additional, Gecmen, C, additional, Unkun, T, additional, Cap, M, additional, Erdogan, E, additional, Onal, C, additional, Yilmaz, F, additional, Ozdemir, N, additional, Muser, D, additional, Tioni, C, additional, Zanuttini, D, additional, Morocutti, G, additional, Spedicato, L, additional, Bernardi, G, additional, Proclemer, A, additional, Pranevicius, R, additional, Zapustas, N, additional, Briedis, K, additional, Valuckiene, Z, additional, Jurkevicius, R, additional, Juffermans, LJM, additional, Enait, V, additional, Van Royen, N, additional, Van Rossum, AC, additional, Kamp, O, additional, Khalaf, HASSEN, additional, Hitham, SAKER, additional, Osama, AS, additional, Abazid, RAMI, additional, Guall, RAHIM, additional, Durdan, SHAFAT, additional, Mohammed, ZYAD, additional, Stella, S, additional, Rosa, I, additional, Ancona, F, additional, Spartera, M, additional, Italia, L, additional, Latib, A, additional, Colombo, A, additional, Margonato, A, additional, Agricola, E, additional, Scatena, C, additional, Mazzanti, C, additional, Conte, L, additional, Pugliese, N, additional, Barletta, V, additional, Bortolotti, U, additional, Naccarato, AG, additional, Di Bello, V, additional, Bala, G, additional, Roosens, B, additional, Hernot, S, additional, Remory, I, additional, Droogmans, S, additional, Cosyns, B, additional, Generati, G, additional, Labate, V, additional, Donghi, V, additional, Pellegrino, M, additional, Carbone, F, additional, Alfonzetti, E, additional, Guazzi, M, additional, Dabrowski, R, additional, Kowalik, I, additional, Firek, B, additional, Chwyczko, T, additional, Szwed, H, additional, Kawamura, A, additional, Kawano, S, additional, Zaroui, A, additional, Ben Said, R, additional, Ben Halima, M, additional, Kheder, N, additional, Farhati, A, additional, Mourali, S, additional, Mechmech, R, additional, Leite, L, additional, Martins, R, additional, Baptista, R, additional, Barbosa, A, additional, Ribeiro, N, additional, Oliveira, A, additional, Castro, G, additional, Pego, M, additional, Polte, C L, additional, Lagerstrand, K, additional, Johnsson, Å A, additional, Janulewicz, M, additional, Bech-Hanssen, O, additional, Gabriel, H, additional, Wisser, W, additional, Maurer, G, additional, Rosenhek, R, additional, El Aroussy, W, additional, Abdel Ghany, M, additional, Al Adeeb, K, additional, Ascione, L, additional, Carlomagno, G, additional, Sordelli, C, additional, Ferro, A, additional, Ascione, R, additional, Severino, S, additional, Caso, P, additional, Muraru, D, additional, Janei, C, additional, Haertel Miglioranza, M, additional, Cavalli, G, additional, Peluso, D, additional, Cucchini, U, additional, Badano, L, additional, Armario Bel, X, additional, Garcia-Garcia, C, additional, Ferrer Sistach, E, additional, Rueda Sobella, F, additional, Oliveras Vila, T, additional, Labata Salvador, C, additional, Serra Flores, J, additional, Lopez-Ayerbe, J, additional, Bayes-Genis, A, additional, Conte, E, additional, Gonella, A, additional, Morena, L, additional, Civelli, D, additional, Losardo, L, additional, Margaria, F, additional, Riva, L, additional, Tanga, M, additional, Carminati, C, additional, Muratori, M, additional, Gripari, P, additional, Ghulam Ali, S, additional, Fusini, L, additional, Vignati, C, additional, Bartorelli, AL, additional, Alamanni, F, additional, Marini, C, additional, Montorfano, M, additional, Ismaiel, A, additional, Ali, N, additional, Amry, S, additional, Serafin, A, additional, Kochanowski, J, additional, Filipiak, KJ, additional, Opolski, G, additional, Speranza, G, additional, Ando', G, additional, Magaudda, L, additional, Cramer, GE, additional, Bakker, J, additional, Michels, M, additional, Dieker, HJ, additional, Fouraux, MA, additional, Marcelis, CLM, additional, Timmermans, J, additional, Brouwer, MA, additional, Kofflard, MJM, additional, Vasconcelos, M, additional, Araujo, V, additional, Almeida, P, additional, Sousa, C, additional, Macedo, F, additional, Cardoso, JS, additional, Maciel, MJ, additional, Voilliot, D, additional, Huttin, O, additional, Venner, C, additional, Olivier, A, additional, Villemin, T, additional, Deballon, R, additional, Manenti, V, additional, Juilliere, Y, additional, Selton-Suty, C, additional, Dabrowska-Kugacka, A, additional, Dorniak, K, additional, Lewicka, E, additional, Szalewska, D, additional, Kutniewska-Kubik, M, additional, Raczak, G, additional, Kim, K H, additional, Yoon, H J, additional, Park, H J, additional, Ahn, Y, additional, Jeong, M H, additional, Cho, J G, additional, Park, J C, additional, Kim, J H, additional, Galli, E, additional, Habib, G, additional, Schnell, F, additional, Lederlin, M, additional, Daubert, JC, additional, Mabo, P, additional, Donal, E, additional, Faria, R, additional, Magalhaes, P, additional, Marques, N, additional, Domingues, K, additional, Lourenco, C, additional, Almeida, AR, additional, Teles, L, additional, Picarra, B, additional, Azevedo, O, additional, Oliveira, M, additional, Marmelo, B, additional, Almeida, A, additional, Bento, D, additional, Cruz, I, additional, Reis, L, additional, Gimaev, RH, additional, Melnikova, MA, additional, Olezov, NV, additional, Ruzov, VI, additional, Goncalves, P, additional, Almeida, M S, additional, Branco, P, additional, Carvalho, M S, additional, Dores, H, additional, Gaspar, M A, additional, Sousa, H, additional, Andrade, M J, additional, Mendes, M, additional, Makavos, G, additional, Varoudi, M, additional, Papadavid, E, additional, Andreadou, I, additional, Gravanis, K, additional, Liarakos, N, additional, Pavlidis, G, additional, Rigopoulos, D, additional, Lekakis, J, additional, Deluyker, D, additional, Bito, V, additional, Punzi, L, additional, Neilan, T, additional, Coen, K, additional, Gannon, S, additional, Bennet, K, additional, Clarke, JG, additional, Solari, M, additional, Cameli, M, additional, Focardi, M, additional, Corrado, D, additional, Bonifazi, M, additional, Henein, M, additional, Mondillo, S, additional, Gomez-Escalonilla, C, additional, De Agustin, A, additional, Egido, J, additional, Islas, F, additional, Simal, P, additional, Gomez De Diego, JJ, additional, Luaces, M, additional, Macaya, C, additional, Perez De Isla, L, additional, Zancanella, M, additional, Rusconi, C, additional, Musca, F, additional, Santambrogio, G, additional, De Chiara, B, additional, Vallerio, P, additional, Cairoli, R, additional, Giannattasio, G, additional, Moreo, A, additional, Alvarez Ortega, C, additional, Mori Junco, R, additional, Caro Codon, J, additional, Meras Colunga, P, additional, Ponz De Antonio, I, additional, Lopez Fernandez, T, additional, Valbuena Lopez, S, additional, Moreno Yanguela, M, additional, Lopez-Sendon, JL, additional, Surkova, E, additional, Bonanad-Lozano, C, additional, Lopez-Lereu, MP, additional, Monmeneu-Menadas, JV, additional, Gavara, J, additional, De Dios, E, additional, Paya-Chaume, A, additional, Escribano-Alarcon, D, additional, Chorro-Gasco, FJ, additional, Bodi-Peris, V, additional, Michalski, BW, additional, Miskowiec, D, additional, Kasprzak, JD, additional, Lipiec, P, additional, Morgado, G, additional, Caldeira, D, additional, Joao, I, additional, Almeida, A R, additional, Lopes, L, additional, Fazendas, P, additional, Cotrim, C, additional, Pereira, H, additional, De Block, C, additional, Buys, D, additional, Salgado, R, additional, Vrints, C, additional, Van Gaal, L, additional, Mctear, C, additional, Irwin, RB, additional, Dragulescu, A, additional, Friedberg, M, additional, Mertens, L, additional, Krinochkin, DV, additional, Yaroslavskaya, EI, additional, Zaharova, EH, additional, Pushkarev, GS, additional, Sugihara, C, additional, Patel, NR, additional, Sulke, AN, additional, Lloyd, GW, additional, Piatkowski, R, additional, Scislo, P, additional, Grabowski, M, additional, Marchel, M, additional, Roland, H, additional, Hamadanchi, A, additional, Otto, S, additional, Jung, C, additional, Lauten, A, additional, Figulla, HC, additional, Poerner, TC, additional, Sampaio, F, additional, Fonseca, P, additional, Fontes-Carvalho, R, additional, Pinho, M, additional, Campos, AS, additional, Castro, P, additional, Fonseca, C, additional, Ribeiro, J, additional, Gama, V, additional, Heck, R, additional, Hamdanchi, A, additional, Figulla, HR, additional, Ranjbar, S, additional, Ghaffaripour Jahromi, M, additional, Hinojar, R, additional, Fernandez Golfin, C, additional, Esteban, A, additional, Pascual-Izco, M, additional, Garcia-Martin, A, additional, Jimenez-Nacher, JJ, additional, Zamorano, JL, additional, Acar, R, additional, Bakal, RB, additional, Kaymaz, C, additional, Karvandi, M, additional, Galand, V, additional, Matelot, D, additional, Leclercq, C, additional, Carre, F, additional, Suran, BC, additional, Margulescu, AD, additional, Rimbas, RC, additional, Siliste, C, additional, Vinereanu, D, additional, Nocerino, P, additional, Urso, AC, additional, Borrino, A, additional, Carbone, C, additional, Follero, P, additional, Ciardiello, C, additional, Prato, L, additional, Salzano, G, additional, Marino, F, additional, Ruspetti, A, additional, Sparla, S, additional, Di Tommaso, C, additional, Loiacono, F, additional, D'ascenzi, F, additional, Porter, J, additional, Walker, M, additional, Lo Iudice, F, additional, Esposito, R, additional, Santoro, C, additional, Cocozza, S, additional, Izzo, R, additional, De Luca, N, additional, De Simone, G, additional, Trimarco, B, additional, Galderisi, M, additional, Gervasi, F, additional, Patti, G, additional, Mega, S, additional, Bono, M, additional, Di Sciascio, G, additional, Buture, A, additional, Badea, R, additional, Platon, P, additional, Ghiorghiu, I, additional, Jurcut, R, additional, Coman, IM, additional, Popescu, BA, additional, Ginghina, C, additional, Lunetta, M, additional, Spoto, MS, additional, Lo Vi, AM, additional, Pensabene, G, additional, Carita, P, additional, Coppola, G, additional, Assennato, P, additional, Shim, A, additional, Wejner-Mik, P, additional, Havasi, K, additional, Domsik, P, additional, Kalapos, A, additional, Forster, T, additional, Piros, GA, additional, Lengyel, C, additional, Orosz, A, additional, Bulbul, Z, additional, Issa, Z, additional, Al Sehly, A, additional, Pergola, V, additional, Oufi, S, additional, Conde, Y, additional, Cimino, E, additional, Rinaldi, E, additional, Ashurov, R, additional, Ricci, S, additional, Pergolini, M, additional, Vitarelli, A, additional, Lujan Valencia, JE, additional, Chaparro, M, additional, Garcia-Guerrero, A, additional, Cristo Ropero, MJ, additional, Izquierdo Bajo, A, additional, Madrona, L, additional, Monmeneu, JV, additional, Igual, B, additional, Lopez Lereu, P, additional, Garcia, MP, additional, Selmi, W, additional, Jalal, Z, additional, Thambo, JB, additional, Kosuta, D, additional, and Fras, Z, additional

Published
2015
Full Text
View/download PDF

Catalog

Books, media, physical & digital resources
See catalog results