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1. Functional Groups Accessibility and the Origin of Photoluminescence in N/O-containing Bottom-up Carbon Nanodots

Author

Debes, P. P., Langer, M., Pagel, M., Menna, E., Smarsly, B., Osella, S., Gallego, J., and Gatti, T.

Subjects
Condensed Matter - Materials Science
Abstract

Chemical functionalization of carbon nanodots (CNDs) offers a valuable opportunity to tailor multifunctionality in these nanocarbons, by engineering the composition of their molecular surface. Therefore, it is important to elucidate the type and amount of CNDs functionalization to be able to design their properties accurately. CNDs are often functionalized through amide coupling without validating the degree of functionalization. As a measure of functionalization, the amounts of primary amines via Kaiser test (KT) or imine reactions of the bare CNDs is often considered. However, this may lead to overestimating the degree of functionalization obtained by the pure amide coupling due to different reaction mechanisms and involved intermediates. Herein, four different CNDs prepared by microwave-assisted synthesis from arginine or citric acid with varying amounts of ethylenediamine are presented. We resorted to a combination of physicochemical methods to provide elemental, structural, and optical information. By that, we developed a method to quantify the degree of functionalization by amide coupling and show that the functionalization is lower than one would expect. Comparing experimental optical features of the CNDs with different computed model systems further allows us to provide a more advanced vision of structure-property relationships in these still elusive nanocarbons.

Published
2024

4. 293 Acidosis promotes immune escape through the IFN-γ-induced induction of PD-L1 transcription in cancer cells

Author

Stowbur, D., primary, Knopf, P., additional, Hoffmann, S., additional, Buchner, V., additional, Poxleitner, M., additional, Gonzalez-Menendez, I., additional, Kramer, D., additional, Schaller, M., additional, Forchhammer, S., additional, Quintanilla-Martinez Fend, L., additional, Schulze-Osthoff, K., additional, Pagel, M., additional, Martins, A., additional, Fransen, M., additional, Pichler, B., additional, Ghoreschi, K., additional, and Kneilling, M., additional

Published
2023
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13. A small molecule antagonist of the αvβ3 integrin suppresses MDA-MB-435 skeletal metastasis

Author

Harms, John F., Welch, Danny R., Samant, Rajeev S., Shevde, Lalita A., Miele, Mary E., Babu, Geetha R., Goldberg, Steven F., Gilman, Virginia R., Sosnowski, Donna M., Campo, Dianalee A., Gay, Carol V., Budgeon, Lynn R., Mercer, Robin, Jewell, Jennifer, Mastro, Andrea M., Donahue, Henry J., Erin, Nuray, Debies, Michael T., Meehan, William J., Jones, Amy L., Mbalaviele, Gabriel, Nickols, Allen, Christensen, Neil D., Melly, Robert, Beck, Lisa N., Kent, Julia, Rader, Randall K., Kotyk, John J., Pagel, M. D., Westlin, William F., and Griggs, David W.

Published
2004

19. Contribution of the lichen symbiosis to the diversification of fungi: a new approach to determining confidence levels for ancestral character states

Author

LUTZONI, F., PAGEL, M., and REEB, V.

Subjects
Zoological research -- Analysis, Fungi -- Research, Lichens -- Research, Symbiosis -- Research, Zoology and wildlife conservation
Abstract

The acceptance by the mycological and lichenological communities, more than 12 years ago, that basidiomycetes tightly associated with green algae or cyanobacteria are lichens, simultaneously established, for the first time, that lichens (including both asco- and basidiolichens) are derived from multiple independent origins. Because approximately one-fifth of all known fungi are lichenized and more than 98% of the diversity of lichens is within the ascomycetes, one crucial question remains to be answered: How many independent origins of lichens took place during the evolution of the ascomycetes? To address this question we have sequenced a 1 kb and a 1.4 kb fragment at the 5' end of the small and large subunits of the nuclear ribosomal DNA, respectively, for 54 species representing 31 orders of ascomycetes. The combined maximum parsimony analysis revealed two equally most parsimonious trees. The ancestral character states (lichenized versus non-lichenized) were reconstructed for every node using maximum likelihood and by taking into consideration phylogenetic uncertainty. The confidence levels for each of the ancestral character states were estimated by reconstructing the evolution of lichenization on a large number of trees randomly sampled within the confidence envelope surrounding the best trees.

Published
2000

21. Role of compressive tectonics on gas charging into the Ordovician sandstone reservoirs in the Sbaa Basin, Algeria: constrained by fluid inclusions and mineralogical data

Author

Gomes, Marcia E.B., Barats, Aurélie, Gerbe, Marie, Lopes, Rodrigo, Nardi, Lauro V.S., Lopes, R.W., Mexias, A.S., Philipp, R.P., Bicca, M.M., Fontana, Eduardo, Pires, G.L.C., Bongiolo, E.M., Geraldes, M.C., Santos, A.C., Jourdan, F., Neumann, R., Pires, Gustavo Luiz Campos, Nascimento, Débora Barros, Prado, Maurício, Bongiolo, Everton Marques, Piza, Patricia d'Almeida de Toledo, Schmitt, Renata da Silva, Mexias, André Sampaio, Mohammed, Tabeliouna, Jean-Yves, Cottin, Peter, Bowden, Christophe, Renac, Mexias, Andre, Louni-Hacini, Amina, Brouillet, Stéphanie, Cottin, Jean-Yves, Wazir, I., Pagel, M., Tournier, F., Portier, E., Renac, C., Univ Fed Rio Grande do Sul, Inst Geociencias, BR-91501970 Porto Alegre, RS, Brazil, Univ Fed Rio Grande do Sul, Fac Agron, Dept Solos, Laboratoire de Chimie Analytique Bio-Inorganique et Environnement (LCABIE), Université de Pau et des Pays de l'Adour (UPPA)-Centre National de la Recherche Scientifique (CNRS), COMUE Université Côte d'Azur (2015-2019) (COMUE UCA), Instituto de Geociências, Universidade Federal do Rio Grande do Sul [Porto Alegre] (UFRGS), Instituto de Geociencias, JRC Institute for Transuranium Elements [Karlsruhe] (ITU ), European Commission - Joint Research Centre [Karlsruhe] (JRC), insituto de geociencias, universidade federal do rio de janeiro, Instituto de Biofísica e Biomatemática, Universidade de Coimbra [Coimbra], Helmholtz zentrum für Schwerionenforschung GmbH (GSI), Laboratoire Magmas et Volcans (LMV), Institut national des sciences de l'Univers (INSU - CNRS)-Université Jean Monnet - Saint-Étienne (UJM)-Institut de Recherche pour le Développement et la société-Université Clermont Auvergne [2017-2020] (UCA [2017-2020])-Centre National de la Recherche Scientifique (CNRS)-Observatoire de Physique du Globe de Clermont-Ferrand (OPGC), Institut national des sciences de l'Univers (INSU - CNRS)-Université Clermont Auvergne [2017-2020] (UCA [2017-2020])-Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Clermont Auvergne [2017-2020] (UCA [2017-2020])-Centre National de la Recherche Scientifique (CNRS), Géoazur (GEOAZUR 7329), Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire de la Côte d'Azur, COMUE Université Côte d'Azur (2015-2019) (COMUE UCA)-Université Côte d'Azur (UCA)-COMUE Université Côte d'Azur (2015-2019) (COMUE UCA)-Université Côte d'Azur (UCA)-Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche pour le Développement (IRD [France-Sud]), Univ Fed Rio Grande do Sul, Inst Geociencias, Université des Sciences et de la Technologie Houari Boumediene = University of Sciences and Technology Houari Boumediene [Alger] (USTHB), Cité de la céramique - Sèvres et Limoges, Observatoire de Physique du Globe de Clermont-Ferrand (OPGC), Université Blaise Pascal - Clermont-Ferrand 2 (UBP)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université Blaise Pascal - Clermont-Ferrand 2 (UBP)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université Jean Monnet - Saint-Étienne (UJM)-Centre National de la Recherche Scientifique (CNRS), Interactions et dynamique des environnements de surface (IDES), Université Paris-Sud - Paris 11 (UP11)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS), Géosciences Paris Sud (GEOPS), Université Paris-Sud - Paris 11 (UP11)-Centre National de la Recherche Scientifique (CNRS), Gaz de France Suez (GDF Suez), Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche pour le Développement et la société-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire de Physique du Globe de Clermont-Ferrand (OPGC), Institut national des sciences de l'Univers (INSU - CNRS)-Université Clermont Auvergne [2017-2020] (UCA [2017-2020])-Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Clermont Auvergne [2017-2020] (UCA [2017-2020])-Centre National de la Recherche Scientifique (CNRS)-Université Clermont Auvergne [2017-2020] (UCA [2017-2020])-Université Jean Monnet [Saint-Étienne] (UJM), Université Côte d'Azur (UCA)-Institut national des sciences de l'Univers (INSU - CNRS)-Institut de Recherche pour le Développement (IRD [France-Sud])-Centre National de la Recherche Scientifique (CNRS)-Observatoire de la Côte d'Azur, Université Côte d'Azur (UCA)-COMUE Université Côte d'Azur (2015-2019) (COMUE UCA)-COMUE Université Côte d'Azur (2015-2019) (COMUE UCA), USTBH, Alger, Institut national des sciences de l'Univers (INSU - CNRS)-Université Jean Monnet [Saint-Étienne] (UJM)-Université Blaise Pascal - Clermont-Ferrand 2 (UBP)-Observatoire de Physique du Globe de Clermont-Ferrand (OPGC), Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Blaise Pascal - Clermont-Ferrand 2 (UBP)-Centre National de la Recherche Scientifique (CNRS)-Centre National de la Recherche Scientifique (CNRS), Institut national des sciences de l'Univers (INSU - CNRS)-Université Jean Monnet [Saint-Étienne] (UJM)-Institut de Recherche pour le Développement et la société-Université Clermont Auvergne [2017-2020] (UCA [2017-2020])-Centre National de la Recherche Scientifique (CNRS)-Observatoire de Physique du Globe de Clermont-Ferrand (OPGC), and Université Blaise Pascal - Clermont-Ferrand 2 (UBP)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Centre National de la Recherche Scientifique (CNRS)-Centre National de la Recherche Scientifique (CNRS)

Subjects
010504 meteorology & atmospheric sciences, Geochemistry, [SDU.STU]Sciences of the Universe [physics]/Earth Sciences, engineering.material, 010502 geochemistry & geophysics, 01 natural sciences, Siderite, chemistry.chemical_compound, [SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/Geochemistry, Fluid inclusions, [SDU.STU.HY]Sciences of the Universe [physics]/Earth Sciences/Hydrology, Quartz, [SDU.STU.AG]Sciences of the Universe [physics]/Earth Sciences/Applied geology, ComputingMilieux_MISCELLANEOUS, 0105 earth and related environmental sciences, Calcite, Cementation (geology), Diagenesis, chemistry, 13. Climate action, [SDU]Sciences of the Universe [physics], [SDE]Environmental Sciences, engineering, General Earth and Planetary Sciences, Carbonate, Geology, Dickite
Abstract

Structure- and tectonic-related gas migration into Ordovician sandstone reservoirs and its impact on diagenesis history were reconstructed in two fields in the Sbaa Basin, in SW Algeria. This was accomplished by petrographical observations, fluid inclusion microthermometry and stable isotope geochemistry on quartz, dickite and carbonate cements and veins. Two successive phases of quartz cementation (CQ1 and CQ2) occurred in the reservoirs. Two- phase aqueous inclusions show an increase in temperatures and salinities from the first CQ1 diagenetic phase toward CQ2 in both fields. Microthermometric data on gas inclusions in quartz veins reveal the presence of an average of 92 ± 5 mole% of CH4 considering a CH4-CO2 system, which is similar to the present-day gas composition in the reservoirs. The presence of primary methane inclusions in early quartz overgrowths and in quartz and calcite veins suggests that hydrocarbon migration into the reservoir occurred synchronically with early quartz cementation in the sandstones located near the contact with the Silurian gas source rock at 100-140°C during the Late Carboniferous period and the late Hercynian episode fracturing at temperatures between 117 and 185°C, which increased in the NW-direction of the basin. During the fracture filling, three main types of fluids were identified with different salinities and formation temperatures. A supplementary phase of higher fluid temperature (up to 226°C) recorded in late quartz, and calcite veins is related to a Jurassic thermal event. The occurrence of dickite cements close to the Silurian base near the main fault areas in both fields is mainly correlated with the sandstones where the early gas was charged. It implies that dickite precipitation is related to acidic influx. Late carbonate cements and veins (calcite - siderite - ankerite and strontianite) occurred at the same depths resulting from the same groundwater precipitation. The absence o

Published
2014
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23. Role of compressive tectonics on gas charging into the Ordovician sandstone reservoirs in the Sbaa, Algeria : constrained by fluid inclusions and mineralogical data

Author

Wazir, I., Pagel, M., Tournier, F., Renac, Christophe, Géosciences Paris Sud (GEOPS), Université Paris-Sud - Paris 11 (UP11)-Centre National de la Recherche Scientifique (CNRS), DEP-NAD GDF-SUEZ, Gaz de France Suez (GDF Suez), Géoazur (GEOAZUR 7329), Université Côte d'Azur (UCA)-Institut national des sciences de l'Univers (INSU - CNRS)-Institut de Recherche pour le Développement (IRD [France-Sud])-Centre National de la Recherche Scientifique (CNRS)-Observatoire de la Côte d'Azur, Université Côte d'Azur (UCA)-COMUE Université Côte d'Azur (2015-2019) (COMUE UCA)-COMUE Université Côte d'Azur (2015-2019) (COMUE UCA), Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire de la Côte d'Azur, and Université Côte d'Azur (UCA)-Université Côte d'Azur (UCA)-Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche pour le Développement (IRD [France-Sud])

Subjects
[SDU.STU]Sciences of the Universe [physics]/Earth Sciences
Abstract

International audience; Structure- and tectonic-related gas migration into Ordovician sandstone reservoirs and its impact on diagenesis history were reconstructed in two fields in the Sbaa Basin, in SW Algeria. This was accomplished by petrographical observations, fluid inclusion microthermometry and stable isotope geochemistry on quartz, dickite and carbonate cements and veins. Two successive phases of quartz cementation (CQ1 and CQ2) occurred in the reservoirs. Two- phase aqueous inclusions show an increase in temperatures and salinities from the first CQ1 diagenetic phase toward CQ2 in both fields. Microthermometric data on gas inclusions in quartz veins reveal the presence of an average of 92 ± 5 mole% of CH4 considering a CH4-CO2 system, which is similar to the present-day gas composition in the reservoirs. The presence of primary methane inclusions in early quartz overgrowths and in quartz and calcite veins suggests that hydrocarbon migration into the reservoir occurred synchronically with early quartz cementation in the sandstones located near the contact with the Silurian gas source rock at 100-140°C during the Late Carboniferous period and the late Hercynian episode fracturing at temperatures between 117 and 185°C, which increased in the NW-direction of the basin. During the fracture filling, three main types of fluids were identified with different salinities and formation temperatures. A supplementary phase of higher fluid temperature (up to 226°C) recorded in late quartz, and calcite veins is related to a Jurassic thermal event. The occurrence of dickite cements close to the Silurian base near the main fault areas in both fields is mainly correlated with the sandstones where the early gas was charged. It implies that dickite precipitation is related to acidic influx. Late carbonate cements and veins (calcite - siderite - ankerite and strontianite) occurred at the same depths resulting from the same groundwater precipitation. The absence o

Published
2014

25. Bassins sédimentaires - les marqueurs de leur histoire thermique

Author

Pagel, M., Barbarand, J., Beaufort, Daniel, Gautheron, C., Pironon, J., Géosciences Paris Sud (GEOPS), Université Paris-Sud - Paris 11 (UP11)-Centre National de la Recherche Scientifique (CNRS), Institut de Chimie des Milieux et Matériaux de Poitiers (IC2MP), Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université de Poitiers-Institut de Chimie du CNRS (INC), GeoRessources, Institut national des sciences de l'Univers (INSU - CNRS)-Centre de recherches sur la géologie des matières premières minérales et énergétiques (CREGU)-Université de Lorraine (UL)-Centre National de la Recherche Scientifique (CNRS), and EDP Sciences

Subjects
[SDU.STU]Sciences of the Universe [physics]/Earth Sciences
Abstract

Depuis une quarantaine d'années, la reconstitution de l'histoire thermique des bassins sédimentaires s'appuie sur les propriétés chimiques, physiques et moléculaires de la matière organique présente dans les sédiments. Puis progressivement, des marqueurs minéraux se sont avérés être d'excellents témoins de cette histoire thermique. Ce livre (inspiré d'un séminaire de formation continue de l'Université de Paris-Sud) a pour but de présenter d'abord toutes les méthodes organiques et minérales actuellement disponibles incluant celles qui sont apparues très récemment et de se focaliser sur les marqueurs minéraux qui ont atteint un degré de maturité suffisant. L'histoire thermique est reconstituée à partir de géothermomètres, de chronomètres, de chronothermomètres et enfin de géothermomètres cinétiques ou cumulatifs. La combinaison de toutes ces méthodes aboutit à des histoires dont les implications géodynamiques, pétrolières, minières, environnementales sont très importantes. Il n'existe pas une démarche unique puisque les méthodes utilisées ont des domaines d'application différents, des précisions variables et dépendent de la nature des sédiments. De niveau master, cet ouvrage s'adresse aux étudiants et aux enseignants mais également à tous les géologues qui s'intéressent à la thermicité des bassins et qui se demandent quelles sont les méthodes qui peuvent permettre de résoudre leurs énigmes.

Published
2014

29. Reconstruction of low burial (< 100 °C) in sedimentary basins: A comparison of geothermometer sensitivity in the intracontinental Paris

Author

Blaise, T., Barbarand, J., Kars, M., Ploquin, Florian, Aubourg, Charles, Brigaud, B., Catherlineau, M., El Albani, A., Gautheron, C., Izart, A., Janots, D., Michel, R., Pagel, M., Pozzi, J.P., Boiron, M.C., Landrein, P., GeoRessources, Institut national des sciences de l'Univers (INSU - CNRS)-Centre de recherches sur la géologie des matières premières minérales et énergétiques (CREGU)-Université de Lorraine (UL)-Centre National de la Recherche Scientifique (CNRS), Géosciences Paris Sud (GEOPS), Université Paris-Sud - Paris 11 (UP11)-Centre National de la Recherche Scientifique (CNRS), Laboratoire des Fluides Complexes et leurs Réservoirs (LFCR), Centre National de la Recherche Scientifique (CNRS)-Université de Pau et des Pays de l'Adour (UPPA)-TOTAL FINA ELF, Laboratoire de géologie de l'ENS (LGENS), Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Département des Géosciences - ENS Paris, École normale supérieure - Paris (ENS Paris), Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-École normale supérieure - Paris (ENS Paris), Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL), and Agence Nationale pour la Gestion des Déchets Radioactifs (ANDRA)

Subjects
[SDU.STU]Sciences of the Universe [physics]/Earth Sciences, ComputingMilieux_MISCELLANEOUS
Abstract

International audience

Published
2013
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30. Lithostratigraphy, hydrodynamism and thermicity in the multi-layer sedimentary system intersected by the Andra deep borehole of Montiers-sur-Saulx (Meuse, France)

Author

Landrein, P., Vigneron, Georges, Lebon, Patrick, Jacques, Delay, Pagel, M., ANDRA BURE, Agence Nationale pour la Gestion des Déchets Radioactifs (ANDRA), Géosciences Paris Sud (GEOPS), and Université Paris-Sud - Paris 11 (UP11)-Centre National de la Recherche Scientifique (CNRS)

Subjects
[SDU]Sciences of the Universe [physics], [SDU.STU]Sciences of the Universe [physics]/Earth Sciences, ComputingMilieux_MISCELLANEOUS
Abstract

International audience

Published
2013

34. Interdisciplinary prospective analysis of nuclear power technological transition

Author

Zakari, A.-A., Bidaud, A., Criqui, Patrick, David, S., Pagel, M., Menanteau, Philippe, Mima, Silvana, Laboratoire de Physique Subatomique et de Cosmologie (LPSC), Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Institut Polytechnique de Grenoble - Grenoble Institute of Technology-Institut National de Physique Nucléaire et de Physique des Particules du CNRS (IN2P3)-Université Joseph Fourier - Grenoble 1 (UJF)-Centre National de la Recherche Scientifique (CNRS), équipe EDDEN (LEPII-EDDEN), Laboratoire d'Economie de la Production et de l'Intégration Internationale (LEPII), Centre National de la Recherche Scientifique (CNRS)-Université Pierre Mendès France - Grenoble 2 (UPMF)-Centre National de la Recherche Scientifique (CNRS)-Université Pierre Mendès France - Grenoble 2 (UPMF), Institut de Physique Nucléaire d'Orsay (IPNO), Centre National de la Recherche Scientifique (CNRS)-Institut National de Physique Nucléaire et de Physique des Particules du CNRS (IN2P3)-Université Paris-Sud - Paris 11 (UP11), Interactions et dynamique des environnements de surface (IDES), and Université Paris-Sud - Paris 11 (UP11)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)

Subjects
Hardware_CONTROLSTRUCTURESANDMICROPROGRAMMING, [PHYS.NEXP]Physics [physics]/Nuclear Experiment [nucl-ex], ComputingMilieux_MISCELLANEOUS
Abstract

Proc. on CD Rom paper 11260; International audience

Published
2011

35. Climate and sea-level variations along the northwestern Tethyan margin during the Valanginian C-isotope excursion : mineralogical evidence from the Vocontian Basin (SE France)

Author

Duchamp-Alphonse, S., Fiet, N., Adatte, T., Pagel, M., CRINON, Evelyne, Interactions et dynamique des environnements de surface (IDES), Université Paris-Sud - Paris 11 (UP11)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS), AREVA, Groupe AREVA, Institut of Geology & Palaeontology, and Université de Lausanne (UNIL)

Subjects
[SDU.STU] Sciences of the Universe [physics]/Earth Sciences, [SDU.STU]Sciences of the Universe [physics]/Earth Sciences
Abstract

International audience; A high resolution mineralogical study (bulk-rock and clay-fraction) was carried out upon the hemipelagic strata of the Angles section (Vocontian Basin, SE France) in which the Valanginian positive C-isotope excursion occurs. To investigate sea-level fluctuations and climate change respectively, a Detrital Index (DI: (phyllosilicates and quartz)/calcite) and a Weathering Index (WI: kaolinite/(illite + chlorite)) were established and compared to second-order sea-level fluctuations. In addition, the mineralogical data were compared with the High Nutrient Index (HNI, based on calcareous nannofossil taxa) data obtained by Duchamp-Alphonse et al. (2007), in order to assess the link between the hydrolysis conditions recorded on the surrounding continents and the trophic conditions inferred for the Vocontian Basin. It appears that the mineralogical distribution along the northwestern Tethyan margin is mainly influenced by sea-level changes during the Early Valanginian (Pertransiens to Stephanophorus ammonite Zones) and by climate variations from the late Early Valanginian to the base of the Hauterivian (top of the Stephanophorus to the Radiatus ammonite Zones). The sea-level fall observed in the Pertransiens ammonite Zone (Early Valanginian) is well expressed by an increase in detrital inputs (an increase in the DI) associated with a more proximal source and a shallower marine environment, whereas the sea-level rise recorded in the Stephanophorus ammonite Zone corresponds to a decrease in detrital influx (a decrease in the DI) as the source becomes more distal and the environment deeper. Interpretation of both DI and WI, indicates that the positive C-isotope excursion (top of the Stephanophorus to the Verrucosum ammonite Zones) is associated with an increase of detrital inputs under a stable, warm and humid climate, probably related to greenhouse conditions, the strongest hydrolysis conditions being reached at the maximum of the positive C-isotope excursion. From the Verrucosum ammonite Zone to the base of the Hauterivian (Radiatus ammonite Zone) climatic conditions evolved from weak hydrolysis conditions and, most likely, a cooler climate (resulting in a decrease in detrital inputs) to a seasonal climate in which more humid seasons alternated with more arid ones. The comparison of the WI to the HNI shows that the nutrification recorded al: the Angles section from the top of the Stephanophorus to the Radiatus ammonite Zones (including the positive C-isotope shift), is associated with climatic changes in the source areas. At that time, increased nutrient inputs were generally triggered by increased weathering processes in the source areas due to acceleration in the hydrological cycle under greenhouse conditions This scenario accords with the widely questioned palaeoenvironmental model proposed by Lini et al., (1992) and suggests that increasing greenhouse conditions are the main factor that drove the palaeoenvironmental changes observed in the hemipelagic realm of the Vocontian Basin, during the Valanginian positive C-isotope shift. This high-resolution mineralogical study highlights short-term climatic changes during the Valanginian, probably associated to rapid changes in the C-cycle. Coeval Massive Parana-Etendeka flood basalt eruptions may explain such rapid perturbations. (C) 2011 Elsevier B.V. All rights reserved.

Published
2011

36. Peptides@mica: from affinity to adhesion mechanism

Author

Gladytz, A., primary, John, T., additional, Gladytz, T., additional, Hassert, R., additional, Pagel, M., additional, Risselada, H. J., additional, Naumov, S., additional, Beck-Sickinger, A. G., additional, and Abel, B., additional

Published
2016
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37. Une nomenclature génétique des sources d'uranium

Author

Pagel, M., Interactions et dynamique des environnements de surface (IDES), Université Paris-Sud - Paris 11 (UP11)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS), and CRINON, Evelyne

Subjects
[SDU.STU] Sciences of the Universe [physics]/Earth Sciences, [SDU.STU]Sciences of the Universe [physics]/Earth Sciences
Published
2010

38. Etude prospective de la transition technologique électronucléaire

Author

Zakari, A.A., Bidaud, A., Criqui, P., Menanteau, P., David, S., Pagel, M., Mima, Silvana, Laboratoire de Physique Subatomique et de Cosmologie (LPSC), Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Institut Polytechnique de Grenoble - Grenoble Institute of Technology-Institut National de Physique Nucléaire et de Physique des Particules du CNRS (IN2P3)-Université Joseph Fourier - Grenoble 1 (UJF)-Centre National de la Recherche Scientifique (CNRS), équipe EDDEN (LEPII-EDDEN), Laboratoire d'Economie de la Production et de l'Intégration Internationale (LEPII), Centre National de la Recherche Scientifique (CNRS)-Université Pierre Mendès France - Grenoble 2 (UPMF)-Centre National de la Recherche Scientifique (CNRS)-Université Pierre Mendès France - Grenoble 2 (UPMF), Institut de Physique Nucléaire d'Orsay (IPNO), Centre National de la Recherche Scientifique (CNRS)-Institut National de Physique Nucléaire et de Physique des Particules du CNRS (IN2P3)-Université Paris-Sud - Paris 11 (UP11), Interactions et dynamique des environnements de surface (IDES), Université Paris-Sud - Paris 11 (UP11)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS), and CRINON, Evelyne

Subjects
[SDU.STU] Sciences of the Universe [physics]/Earth Sciences, [SDU.STU]Sciences of the Universe [physics]/Earth Sciences, ComputingMilieux_MISCELLANEOUS
Abstract

International audience

Published
2010

39. La diffusion de l'hélium dans l'apatite : effet des dommages causés par recul alpha

Author

Gautheron, C., Tassan-Got, L., Pagel, M., Barbarand, J., Interactions et dynamique des environnements de surface (IDES), Université Paris-Sud - Paris 11 (UP11)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS), Institut de Physique Nucléaire d'Orsay (IPNO), Centre National de la Recherche Scientifique (CNRS)-Institut National de Physique Nucléaire et de Physique des Particules du CNRS (IN2P3)-Université Paris-Sud - Paris 11 (UP11), and CRINON, Evelyne

Subjects
[SDU.STU] Sciences of the Universe [physics]/Earth Sciences, [SDU.STU]Sciences of the Universe [physics]/Earth Sciences
Published
2010

40. Histoire thermique du Massif Bohémien et conséquences sur la dynamique de l'Europe de l'Ouest au méso-cénozoïque

Author

Bour, I., Barbarand, J., Gautheron, C., Gunnell, Y., Pagel, M., Interactions et dynamique des environnements de surface (IDES), Université Paris-Sud - Paris 11 (UP11)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS), Laboratoire de géographie physique : Environnements Quaternaires et Actuels (LGP), Université Paris 1 Panthéon-Sorbonne (UP1)-Université Paris-Est Créteil Val-de-Marne - Paris 12 (UPEC UP12)-Centre National de la Recherche Scientifique (CNRS), and CRINON, Evelyne

Subjects
[SDU.STU] Sciences of the Universe [physics]/Earth Sciences, [SDU.STU]Sciences of the Universe [physics]/Earth Sciences
Published
2010

41. Paléo-enfouissement des argilites du Callovo-Oxfordien dans l'Est du Bassin de Paris

Author

Barbarand, J., florence QUESNEL, Pagel, M., Interactions et dynamique des environnements de surface (IDES), Université Paris-Sud - Paris 11 (UP11)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS), Bureau de Recherches Géologiques et Minières (BRGM) (BRGM), and CRINON, Evelyne

Subjects
[SDU.STU] Sciences of the Universe [physics]/Earth Sciences, [SDU.STU]Sciences of the Universe [physics]/Earth Sciences
Published
2010

42. Potentiel géothermique du secteur Meuse/Haute-Marne de l'Andra (Est du Bassin de Paris)

Author

Landrein, P., Vigneron, G., Delay, J., Lebon, P., Pagel, M., Laboratoire d'Ingénierie des Matériaux de Bretagne (LIMATB), Université de Bretagne Sud (UBS)-Institut Brestois du Numérique et des Mathématiques (IBNM), Université de Brest (UBO)-Université de Brest (UBO)-Université de Brest (UBO), Laboratoire de Virologie, Hôpital Cochin [AP-HP], Assistance publique - Hôpitaux de Paris (AP-HP) (AP-HP)-Assistance publique - Hôpitaux de Paris (AP-HP) (AP-HP), Interactions et dynamique des environnements de surface (IDES), Université Paris-Sud - Paris 11 (UP11)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS), and CRINON, Evelyne

Subjects
[SDU.STU] Sciences of the Universe [physics]/Earth Sciences, [SDU.STU]Sciences of the Universe [physics]/Earth Sciences
Published
2010

43. A review of the sources of uranium and associated elements in sediments-hosted U-Zr-Mo-V-Zn-(Hg) deposits

Author

Pagel, M., Interactions et dynamique des environnements de surface (IDES), Université Paris-Sud - Paris 11 (UP11)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS), Williams P.J., and CRINON, Evelyne

Subjects
[SDU.STU] Sciences of the Universe [physics]/Earth Sciences, [SDU.STU]Sciences of the Universe [physics]/Earth Sciences, ComputingMilieux_MISCELLANEOUS
Abstract

International audience

Published
2010

44. Dating fluid circulation in faults using secondary calcite (U-Th)/He ages

Author

Cros, A., Gautheron, C., Pagel, M., Interactions et dynamique des environnements de surface (IDES), and Université Paris-Sud - Paris 11 (UP11)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)

Subjects
[SDU.STU]Sciences of the Universe [physics]/Earth Sciences, ComputingMilieux_MISCELLANEOUS
Abstract

International audience

Published
2010

45. A 3D Monte Carlo approach to diffusion to (U-Th)/He thermochronology

Author

Gautheron, C., Tassan-Got, L., Barbarand, J., Pagel, M., Interactions et dynamique des environnements de surface (IDES), Université Paris-Sud - Paris 11 (UP11)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS), Institut de Physique Nucléaire d'Orsay (IPNO), Centre National de la Recherche Scientifique (CNRS)-Institut National de Physique Nucléaire et de Physique des Particules du CNRS (IN2P3)-Université Paris-Sud - Paris 11 (UP11), and CRINON, Evelyne

Subjects
[SDU.STU] Sciences of the Universe [physics]/Earth Sciences, [SDU.STU]Sciences of the Universe [physics]/Earth Sciences, ComputingMilieux_MISCELLANEOUS
Abstract

International audience

Published
2010

47. Relation entre la cimentation profonde du quartz et le faciès sédimentaire dans les grès de l'Ordovicien glaciaire du Bassin de Sbaa, Algérie

Author

Tournier, F., Pagel, M., Portier, E., Wazir, I., Fiet, N., CRINON, Evelyne, Interactions et dynamique des environnements de surface (IDES), Université Paris-Sud - Paris 11 (UP11)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS), Gaz de France Suez (GDF Suez), AREVA, and Groupe AREVA

Subjects
ComputingMilieux_MISCELLANEOUS
Abstract

International audience

Published
2010

48. Fluid inclusions as constraints in a three-dimensional hydro-thermo-mechanical model of the Paris basin, France

Author

Goncalves, J., Pagel, M., Violette, S., Guillocheau, F., Robin, C., Structure et fonctionnement des systèmes hydriques continentaux (SISYPHE), Université Pierre et Marie Curie - Paris 6 (UPMC)-École pratique des hautes études (EPHE), Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-MINES ParisTech - École nationale supérieure des mines de Paris, Université Paris sciences et lettres (PSL)-Centre National de la Recherche Scientifique (CNRS), Géosciences Paris Sud (GEOPS), Université Paris-Sud - Paris 11 (UP11)-Centre National de la Recherche Scientifique (CNRS), Géosciences Rennes (GR), Université de Rennes 1 (UR1), Université de Rennes (UNIV-RENNES)-Université de Rennes (UNIV-RENNES)-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire des Sciences de l'Univers de Rennes (OSUR)-Centre National de la Recherche Scientifique (CNRS), Université Pierre et Marie Curie - Paris 6 (UPMC)-École Pratique des Hautes Études (EPHE), Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Mines Paris - PSL (École nationale supérieure des mines de Paris), Université de Rennes (UR)-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire des Sciences de l'Univers de Rennes (OSUR), and Université de Rennes (UR)-Institut national des sciences de l'Univers (INSU - CNRS)-Université de Rennes 2 (UR2)-Centre National de la Recherche Scientifique (CNRS)-Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE)-Institut national des sciences de l'Univers (INSU - CNRS)-Université de Rennes 2 (UR2)-Centre National de la Recherche Scientifique (CNRS)-Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE)-Centre National de la Recherche Scientifique (CNRS)

Subjects
[SDU.STU.HY]Sciences of the Universe [physics]/Earth Sciences/Hydrology
Abstract

International audience; Fluid inclusion homogenization temperatures and three-dimensional hydro-thermo-mechanical modelling were combined to constrain fluid flow, solute and heat transport in the Paris basin, France, focusing on the two main petroleum reservoirs i.e. the Dogger and the Triassic (Keuper) formations. The average homogenization temperatures of two-phase aqueous inclusions in different samples range from 66 degrees C to 88 degrees C in the Dogger calcite cement, from 106 degrees C to 118 degrees C in the Keuper dolomite cement and from 89 degrees C to 126 degrees C in the Keuper quartz and K-feldspar cements. The maximum homogenization temperatures for inclusions in the Keuper quartz and K-feldspar cements were 17-47 degrees C higher than present-day temperatures in the boreholes at similar depths. Processes that might explain higher temperatures in the past were examined through numerical simulations and sensitivity tests. A warmer climate in the Late Cretaceous-Early Tertiary resulted in a temperature rise of only 8 degrees C. Late Cretaceous chalk had a thermal blanketing effect that resulted in simulated temperatures as high as 15-20 degrees C above the present day ones. An additional 300 m deposition and subsequent erosion of chalk, not taken into account so far, has to be considered to simulate the high palaeo-temperatures recorded by fluid inclusions in both reservoirs. In view of the simulated thermal history of the basin, in the Keuper, an age of about 85 Ma is consistent with quartz/K-feldspar temperatures and an age of about 65 Ma is in agreement with the precipitation temperature of the dolomite cement. Our models suggest an age of about 50 Ma for the Dogger calcite cementation.

Published
2010
Full Text
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49. A chemical method for extracting delicate calcareous microfossils from indurated calcareous rocks exemplified by calpionellids

Author

Duchamp-Alphone, S., Fiet, N., Pagel, M., Remane, J., Interactions et dynamique des environnements de surface (IDES), Université Paris-Sud - Paris 11 (UP11)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS), and CRINON, Evelyne

Subjects
[SDU.STU] Sciences of the Universe [physics]/Earth Sciences, [SDU.STU]Sciences of the Universe [physics]/Earth Sciences, ComputingMilieux_MISCELLANEOUS
Abstract

International audience

Published
2009

50. Influence des dommages alpha sur la cinétique de l'He : mise en évidence par l'(U-Th)/He sur apatite appliqué à la bordure sud-est du Massif Central

Author

Gautheron, C.E, Barbarand, J., Tassan-Got, L., Pagel, M., Interactions et dynamique des environnements de surface (IDES), and Université Paris-Sud - Paris 11 (UP11)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)

Subjects
[SDU.STU]Sciences of the Universe [physics]/Earth Sciences
Published
2008

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