80 results on '"González-Jiménez, J."'
Search Results
2. ViMantic, a distributed robotic architecture for semantic mapping in indoor environments
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Fernandez-Chaves, D., Ruiz-Sarmiento, J.R., Petkov, N., and Gonzalez-Jimenez, J.
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- 2021
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3. Geosciences for a Sustainable Planet: a new collaborative network to address societal and environmental challenges in the Anthropocene
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Ballesteros-Cánovas, Juan Antonio, Pueyo, Emilio L., Valero Garcés, Blas Lorenzo, Ayala, C., Karanasiou, Angeliki, Vázquez Garrido, Juan-Tomás, González-Jiménez, J. M., Calvo, Eva María, Mata Campo, Maria Pilar, Álvaro Blasco, José Javier, Moreno, Ana, Ballesteros-Cánovas, Juan Antonio, Pueyo, Emilio L., Valero Garcés, Blas Lorenzo, Ayala, C., Karanasiou, Angeliki, Vázquez Garrido, Juan-Tomás, González-Jiménez, J. M., Calvo, Eva María, Mata Campo, Maria Pilar, Álvaro Blasco, José Javier, and Moreno, Ana
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The Geosciences for a Sustainable Planet network is an initiative reinforced by the recent integration of the Spanish Geological Survey (IGME) and the Oceanographic Spanish Institute (IEO) within the Spanish Scientific Research Council (CSIC). The network is aimed to provide Geosciences in Spain with a collaborative framework, to maximize synergies and address sustainability and future challenges with a planetary perspective. The network shares the strategic vision for the study and care of planet Earth as the only home available for our future, as embraced by many international organizations (e. g. the European Geosciences Union (EGU), United Nations Environment Programme (UNEP), International Union of Geological Sciences (IUGS), and the European Marine Board (EMB)). In Spain, Geosciences have played a fundamental role in properly assessing, managing, and seeking solutions for several natural and anthropogenic crises, e.g. the oil spill after the sinking of the Prestige petroleum vessel, the dumping of toxic mine sludge in Aznalcóllar, the eruption of the Cumbre Vieja volcano in La Palma island, the 2011 earthquake of Lorca, the environmental collapse of the Mar Menor oastal lagoon, or the decline in the groundwaters of Doñana National Park. Geoscientists have engaged as first responders with government agencies in emergency situations. Besides, geosciences is providing essential knowledge for public administration, as well as energy and mineral resources companies, water supply, contamination and waste elimination and reuse, and adaptation to geological and natural hazards. The network will enhance the capacity of the CSIC to respond to both, societal and public administration demands. Geosciences also provide the temporal and spatial scale to place current climate and environmental crises in the appropriate context. The network will implement outreach activities to illustrate the interactions of surface processes and biosphere with climatic fluctuations, atmosphe
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- 2024
4. Heterogeneous Non Obtrusive Platform to Monitor, Assist and Provide Recommendations to Elders at Home: The MoveCare Platform
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Borghese, N. A., Bulgheroni, M., Miralles, F., Savanovic, A., Ferrante, S., Kounoudes, T., Cid Gala, M., Loutfi, A., Cangelosi, A., Gonzalez-Jimenez, J., Ianes, A., Angrisani, Leopoldo, Series Editor, Arteaga, Marco, Series Editor, Panigrahi, Bijaya Ketan, Series Editor, Chakraborty, Samarjit, Series Editor, Chen, Jiming, Series Editor, Chen, Shanben, Series Editor, Chen, Tan Kay, Series Editor, Dillmann, Ruediger, Series Editor, Duan, Haibin, Series Editor, Ferrari, Gianluigi, Series Editor, Ferre, Manuel, Series Editor, Hirche, Sandra, Series Editor, Jabbari, Faryar, Series Editor, Jia, Limin, Series Editor, Kacprzyk, Janusz, Series Editor, Khamis, Alaa, Series Editor, Kroeger, Torsten, Series Editor, Liang, Qilian, Series Editor, Ming, Tan Cher, Series Editor, Minker, Wolfgang, Series Editor, Misra, Pradeep, Series Editor, Möller, Sebastian, Series Editor, Mukhopadhyay, Subhas, Series Editor, Ning, Cun-Zheng, Series Editor, Nishida, Toyoaki, Series Editor, Pascucci, Federica, Series Editor, Qin, Yong, Series Editor, Seng, Gan Woon, Series Editor, Veiga, Germano, Series Editor, Wu, Haitao, Series Editor, Zhang, Junjie James, Series Editor, Casiddu, Niccolò, editor, Porfirione, Claudia, editor, Monteriù, Andrea, editor, and Cavallo, Filippo, editor
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- 2019
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5. Integration of CNN into a Robotic Architecture to Build Semantic Maps of Indoor Environments
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Chaves, D., Ruiz-Sarmiento, J. R., Petkov, N., Gonzalez-Jimenez, J., Hutchison, David, Editorial Board Member, Kanade, Takeo, Editorial Board Member, Kittler, Josef, Editorial Board Member, Kleinberg, Jon M., Editorial Board Member, Mattern, Friedemann, Editorial Board Member, Mitchell, John C., Editorial Board Member, Naor, Moni, Editorial Board Member, Pandu Rangan, C., Editorial Board Member, Steffen, Bernhard, Editorial Board Member, Terzopoulos, Demetri, Editorial Board Member, Tygar, Doug, Editorial Board Member, Goos, Gerhard, Founding Editor, Hartmanis, Juris, Founding Editor, Rojas, Ignacio, editor, Joya, Gonzalo, editor, and Catala, Andreu, editor
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- 2019
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6. Probability and Common-Sense: Tandem Towards Robust Robotic Object Recognition in Ambient Assisted Living
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Ruiz-Sarmiento, J. R., Galindo, C., Gonzalez-Jimenez, J., Hutchison, David, Series editor, Kanade, Takeo, Series editor, Kittler, Josef, Series editor, Kleinberg, Jon M., Series editor, Mattern, Friedemann, Series editor, Mitchell, John C., Series editor, Naor, Moni, Series editor, Pandu Rangan, C., Series editor, Steffen, Bernhard, Series editor, Terzopoulos, Demetri, Series editor, Tygar, Doug, Series editor, Weikum, Gerhard, Series editor, García, Carmelo R., editor, Caballero-Gil, Pino, editor, Burmester, Mike, editor, and Quesada-Arencibia, Alexis, editor
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- 2016
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7. Organic phosphorus in the terrestrial environment: a perspective on the state of the art and future priorities
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George, T. S., Giles, C. D., Menezes-Blackburn, D., Condron, L. M., Gama-Rodrigues, A. C., Jaisi, D., Lang, F., Neal, A. L., Stutter, M. I., Almeida, D. S., Bol, R., Cabugao, K. G., Celi, L., Cotner, J. B., Feng, G., Goll, D. S., Hallama, M., Krueger, J., Plassard, C., Rosling, A., Darch, T., Fraser, T., Giesler, R., Richardson, A. E., Tamburini, F., Shand, C. A., Lumsdon, D. G., Zhang, H., Blackwell, M. S. A., Wearing, C., Mezeli, M. M., Almås, Å. R., Audette, Y., Bertrand, I., Beyhaut, E., Boitt, G., Bradshaw, N., Brearley, C. A., Bruulsema, T. W., Ciais, P., Cozzolino, V., Duran, P. C., Mora, M. L., de Menezes, A. B., Dodd, R. J., Dunfield, K., Engl, C., Frazão, J. J., Garland, G., González Jiménez, J. L., Graca, J., Granger, S. J., Harrison, A. F., Heuck, C., Hou, E. Q., Johnes, P. J., Kaiser, K., Kjær, H. A., Klumpp, E., Lamb, A. L., Macintosh, K. A., Mackay, E. B., McGrath, J., McIntyre, C., McLaren, T., Mészáros, E., Missong, A., Mooshammer, M., Negrón, C. P., Nelson, L. A., Pfahler, V., Poblete-Grant, P., Randall, M., Seguel, A., Seth, K., Smith, A. C., Smits, M. M., Sobarzo, J. A., Spohn, M., Tawaraya, K., Tibbett, M., Voroney, P., Wallander, H., Wang, L., Wasaki, J., and Haygarth, P. M.
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- 2018
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8. Diffusion pathways of Fe2+ and Fe3+ during the formation of ferrian chromite: a µXANES study
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Gervilla, F., Asta, M. P., Fanlo, l., Grolimund, D., Ferreira-Sánchez, D., Samson, V. A., Hunziker, D., Colas, V., González-Jiménez, J. M., Kerestedjian, T. N., and Sergeeva, I.
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- 2019
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9. Metales estratégicos: pasado, presente y futuro
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González-Jiménez, J. M. and González-Jiménez, J. M.
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- 2023
10. A track record of Au–Ag nanomelt generation during fluid-mineral interactions
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Ministerio de Ciencia e Innovación (España), Agència de Gestió d'Ajuts Universitaris i de Recerca, Junta de Andalucía, Domínguez-Carretero, D., González-Jiménez, J. M., Proenza, Joaquín A., Villanova-de-Benavent, Cristina, Llovet, X., García-Casco, Antonio, Ministerio de Ciencia e Innovación (España), Agència de Gestió d'Ajuts Universitaris i de Recerca, Junta de Andalucía, Domínguez-Carretero, D., González-Jiménez, J. M., Proenza, Joaquín A., Villanova-de-Benavent, Cristina, Llovet, X., and García-Casco, Antonio
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Recent studies have reported the significant role of Au-bearing nanoparticles in the formation of hydrothermal gold deposits. Despite the ever-increasing understanding of the genesis and stability of Au-bearing nanoparticles, it is still unknown how they behave when exposed to hydrothermal fluids. Here, we study the nanostructural evolution of Au–Ag nanoparticles hosted within Co-rich diarsenides and sulfarsenides of a natural hydrothermal deposit. We use high-resolution transmission electron microscopy to provide a singular glimpse of the complete melting sequence of Au–Ag nanoparticles exposed to the hydrothermal fluid during coupled dissolution–precipitation reactions of their host minerals. The interaction of Au–Ag nanoparticles with hydrothermal fluids at temperatures (400–500 ºC) common to most hydrothermal gold deposits may promote melting and generation of Au–Ag nanomelts. This process has important implications in noble metal remobilization and accumulation during the formation of these deposits.
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- 2023
11. Correction to: Organic phosphorus in the terrestrial environment: a perspective on the state of the art and future priorities
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George, T. S., Giles, C. D., Menezes-Blackburn, D., Condron, L. M., Gama-Rodrigues, A. C., Jaisi, D., Lang, F., Neal, A. L., Stutter, M. I., Almeida, D. S., Bol, R., Cabugao, K. G., Celi, L., Cotner, J. B., Feng, G., Goll, D. S., Hallama, M., Krueger, J., Plassard, C., Rosling, A., Darch, T., Fraser, T., Giesler, R., Richardson, A. E., Tamburini, F., Shand, C. A., Lumsdon, D. G., Zhang, H., Blackwell, M. S. A., Wearing, C., Mezeli, M. M., Almås, Å. R., Audette, Y., Bertrand, I., Beyhaut, E., Boitt, G., Bradshaw, N., Brearley, C. A., Bruulsema, T. W., Ciais, P., Cozzolino, V., Duran, P. C., Mora, M. L., de Menezes, A. B., Dodd, R. J., Dunfield, K., Engl, C., Frazão, J. J., Garland, G., González Jiménez, J. L., Graca, J., Granger, S. J., Harrison, A. F., Heuck, C., Hou, E. Q., Johnes, P. J., Kaiser, K., Kjær, H. A., Klumpp, E., Lamb, A. L., Macintosh, K. A., Mackay, E. B., McGrath, J., McIntyre, C., McLaren, T., Mészáros, E., Missong, A., Mooshammer, M., Negrón, C. P., Nelson, L. A., Pfahler, V., Poblete-Grant, P., Randall, M., Seguel, A., Seth, K., Smith, A. C., Smits, M. M., Sobarzo, J. A., Spohn, M., Tawaraya, K., Tibbett, M., Voroney, P., Wallander, H., Wang, L., Wasaki, J., and Haygarth, P. M.
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- 2018
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12. H: A component-based specification language for heterogeneous applications
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Fernández-Madrigal, J.A., Llopis, L., Cruz-Martín, A., Galindo, C., and González-Jiménez, J.
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- 2013
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13. A record of metasomatism and crustal contamination of the Mediterranean lithosphere in chromitites of the Orhaneli Ophiolite Complex (NW Türkiye)
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Akbulut, Mehmet, González-Jiménez, J. M., Belousova, Elena, Colás Ginés, Vanessa, Farré de Pablo, Júlia, Solà, N. P., Proenza, Joaquín A., Akbulut, Mehmet, González-Jiménez, J. M., Belousova, Elena, Colás Ginés, Vanessa, Farré de Pablo, Júlia, Solà, N. P., and Proenza, Joaquín A.
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This study provides the first-ever report of U-Pb isotopic ages of zircon and rutile from high-Cr chromitites of the Orhaneli Ophiolite Complex (OOC). The chromites within the OOC chromitites yield Cr-numbers between 0.77 and 0.86, Mg-numbers between 0.46 and 0.71 and TiO < 0.26 wt%. They exhibit V, Ga and Ni depletion and Sc, Ti, Zn, Co and Mn enrichment relative to MORB spinels, with significant Sc and Ti positive anomalies. This, and the AlO and TiO compositions of the parental melts, suggest that the studied chromitites formed from island arc melts of boninitic affinity, in a supra-subduction environment. In addition to zircons, chromites host other solid mineral inclusions, including Os- and Ir-dominant platinum-group minerals (PGM), base-metal sulfides (BMS), alloys, ubiquitous silicate (some as micron-sized oriented lamellae), and two poorly defined Fe-Cr-O and Ti-Si-C grains. The zircons show Th/U ratios typical for magmatic zircons from felsic melts, and present Middle Devonian to Mesoproterozoic U-Pb isotopic ages. Although the reworked/resorbed forms of the zircons suggest a xenocrystic origin, coupling of U-Pb data from some zircons and rutile with the Ti positive anomaly in the chromites raises the possibility for an earlier Neoproterozoic metasomatic event affecting the relics now included within the chromitite bands. The current state of knowledge about the silicate micro-lamellae within the chromites has prompted reassessment of their early interpretation as direct evidence of deep mantle recycling. We currently suggest a more cautious approach on this issue by seeking additional evidences for an ultrahigh-pressure (UHP) history.
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- 2022
14. Formation of ferrian chromite in podiform chromitites from the Golyamo Kamenyane serpentinite, Eastern Rhodopes, SE Bulgaria: a two-stage process
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Gervilla, F., Padrón-Navarta, J. A., Kerestedjian, T., Sergeeva, I., González-Jiménez, J. M., and Fanlo, I.
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- 2012
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15. Magnetic Resonance Methods and Applications in Pharmaceutical Research
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Rodríguez, I., Pérez-Rial, S., González-Jimenez, J., Pérez-Sánchez, J.M., Herranz, F., Beckmann, N., and Ruíz-Cabello, J.
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- 2008
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16. Mantle-crust interation formed unique ores in the SCLM of the Serranía de Ronda peridotites (South Spain)
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Gervilla, Fernando, González-Jiménez, J. M., Marchesi, Claudio, Hidas, Károly, and Piña, Rubén
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Goldschmidt 2019, Barcelona (Spain), 18th-23th august, 2019, The Serranía de Ronda ultramafic massifs correspond to portions ofSCLM affected by infiltration of astenosphere-derived melts coeval with exhumation. This resulted in the formation of three petrostructural zones named as the spinel tectonite domain(STD), a granular peridotite domain (GPD) and a plagioclase tectonite domain(PTD). The STDrepresents the SCLMprotolith, the GPDdevelopedat expenses of the former by partial melting and melt accumulation at the boundary between both domains (namelythe recrystallization front) andthe PTD resulted from the ductile deformationof the GPDduring the crustal emplacement of the peridotites.These massifs host a rather unique set of magmatic ores including chromite and Ni arsenides associated with orthopyroxene and/or cordierite (Cr-Ni ores), Fe-Ni-Cu sulfides with graphite (S-G ores), and chromitities (Cr ores). These ores distribute spatially according to the petrological zoning of the massifs: the Ni arsenide-and cordierite-rich Cr-Ni ores, as well as most S-G ores, normally locate within the peripheral STD and the Cr ores occur in the PTD.Thesedifferent types of ores formed by variable degrees of mixing between mantle derived, small-volume melts and silica-rich fluids derived from dehydration of crustal metasediments. The former migrated and fractionated upward from the recrystallization front and mixed occasionally with the infiltrating fluids during the crustal emplacement of peridotites, forming the Ni arsenides-and cordierite-rich Cr-Ni ores. As the peridotite body cooled from the periphery inwards, progressively smaller volumes of crustal-derived fluids reached its interior and mixedwith less fractionated, mantle-derived melts forming Ni arsenide-poor Cr-Ni ores and subsequently the Cr ores. The genesis of S-G ores linked with that of Cr-Ni ores as attested bytheir frequent close spatial connection, the existence of mineralizations sharing characteristics of both ore types and the strong partitioning of platinum-group elements in Ni arsenides instead of sulfides.
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- 2019
17. Correction to:Organic phosphorus in the terrestrial environment: a perspective on the state of the art and future priorities (Plant and Soil, (2018), 427, 1-2, (191-208), 10.1007/s11104-017-3391-x)
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George, T. S., Giles, C. D., Menezes-Blackburn, D., Condron, L. M., Gama-Rodrigues, A. C., Jaisi, D., Lang, F., Neal, A. L., Stutter, M. I., Almeida, D. S., Bol, R., Cabugao, K. G., Celi, L., Cotner, J. B., Feng, G., Goll, D. S., Hallama, M., Krueger, J., Plassard, C., Rosling, A., Darch, T., Fraser, T., Giesler, R., Richardson, A. E., Tamburini, F., Shand, C. A., Lumsdon, D. G., Zhang, H., Blackwell, M. S.A., Wearing, C., Mezeli, M. M., Almås, R., Audette, Y., Bertrand, I., Beyhaut, E., Boitt, G., Bradshaw, N., Brearley, C. A., Bruulsema, T. W., Ciais, P., Cozzolino, V., Duran, P. C., Mora, M. L., de Menezes, A. B., Dodd, R. J., Dunfield, K., Engl, C., Frazão, J. J., Garland, G., González Jiménez, J. L., Graca, J., Granger, S. J., Harrison, A. F., Heuck, C., Hou, E. Q., Johnes, P. J., Kaiser, K., Kjær, H. A., Klumpp, E., Lamb, A. L., Macintosh, K. A., Mackay, E. B., McGrath, J., McIntyre, C., McLaren, T., Mészáros, E., Missong, A., Mooshammer, M., Negrón, C. P., Nelson, L. A., Pfahler, V., Poblete-Grant, P., Randall, M., Seguel, A., Seth, K., Smith, A. C., Smits, M. M., Sobarzo, J. A., Spohn, M., Tawaraya, K., Tibbett, M., Voroney, P., Wallander, H., Wang, L., Wasaki, J., Haygarth, P. M., George, T. S., Giles, C. D., Menezes-Blackburn, D., Condron, L. M., Gama-Rodrigues, A. C., Jaisi, D., Lang, F., Neal, A. L., Stutter, M. I., Almeida, D. S., Bol, R., Cabugao, K. G., Celi, L., Cotner, J. B., Feng, G., Goll, D. S., Hallama, M., Krueger, J., Plassard, C., Rosling, A., Darch, T., Fraser, T., Giesler, R., Richardson, A. E., Tamburini, F., Shand, C. A., Lumsdon, D. G., Zhang, H., Blackwell, M. S.A., Wearing, C., Mezeli, M. M., Almås, R., Audette, Y., Bertrand, I., Beyhaut, E., Boitt, G., Bradshaw, N., Brearley, C. A., Bruulsema, T. W., Ciais, P., Cozzolino, V., Duran, P. C., Mora, M. L., de Menezes, A. B., Dodd, R. J., Dunfield, K., Engl, C., Frazão, J. J., Garland, G., González Jiménez, J. L., Graca, J., Granger, S. J., Harrison, A. F., Heuck, C., Hou, E. Q., Johnes, P. J., Kaiser, K., Kjær, H. A., Klumpp, E., Lamb, A. L., Macintosh, K. A., Mackay, E. B., McGrath, J., McIntyre, C., McLaren, T., Mészáros, E., Missong, A., Mooshammer, M., Negrón, C. P., Nelson, L. A., Pfahler, V., Poblete-Grant, P., Randall, M., Seguel, A., Seth, K., Smith, A. C., Smits, M. M., Sobarzo, J. A., Spohn, M., Tawaraya, K., Tibbett, M., Voroney, P., Wallander, H., Wang, L., Wasaki, J., and Haygarth, P. M.
- Abstract
The article “Organic phosphorus in the terrestrial environment: a perspective on the state of the art and future priorities”, written by Timothy S George et al., was originally published with incorrect affiliation information for one of the co-authors, E. Klumpp.
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- 2018
18. Dating metasomatic events in the lithospheric mantle beneath the Calatrava volcanic field (central Spain)
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Ministerio de Economía y Competitividad (España), Universidad Complutense de Madrid, Villaseca, Carlos, Belousova, E., Barfod, D. N., González-Jiménez, J. M., Ministerio de Economía y Competitividad (España), Universidad Complutense de Madrid, Villaseca, Carlos, Belousova, E., Barfod, D. N., and González-Jiménez, J. M.
- Abstract
We report the first attempt to date metasomatic events in peridotite xenoliths from the Subcontinental Lithospheric Mantle (SCLM) beneath the Cenozoic Calatrava volcanic field of central Spain. The most metasomatized xenoliths of the El Aprisco olivine melilitite maar were selected to perform a geochronological study on metasomatic apatite (U-Pb method) and amphibole (Ar-Ar), integrated with an enlarged chemical data set on these minerals. The metasomatic agents in studied samples are mainly carbonate-rich ultra-alkaline melts of probable asthenospheric derivation. Some samples have been overprinted by more than one metasomatic event. The geochronological data confirm three metasomatic events that occurred within the SCLM beneath central Spain in Cretaceous (118 Ma), Oligocene (29 Ma), and Miocene (16–4 Ma) times, much earlier than the host volcanic magmatism. To date, no magmatic events of those ages have been recorded in central Spain. However, a correlation with several cycles of sporadic intraplate magmatism of alkaline affinity in the Iberian microplate is suggested. This study illustrates that the SCLM preserves the memory of a complex history of melt and/or fluid percolation processes in a metasomatic record that is generally unrelated to shallower crustal magmatic events.
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- 2018
19. Cold plumes trigger contamination of oceanic mantle wedges with continental crust-derived sediments: Evidence from chromitite zircon grains of eastern Cuban ophiolites
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Proenza, J., González-Jiménez, J., Garcia-Casco, A., Belousova, E., Griffin, W., Talavera, Cristina, Rojas-Agramonte, Y., Aiglsperger, T., Navarro-Ciurana, D., Pujol-Solà, N., Gervilla, F., O'Reilly, S., Jacob, D., Proenza, J., González-Jiménez, J., Garcia-Casco, A., Belousova, E., Griffin, W., Talavera, Cristina, Rojas-Agramonte, Y., Aiglsperger, T., Navarro-Ciurana, D., Pujol-Solà, N., Gervilla, F., O'Reilly, S., and Jacob, D.
- Abstract
© 2018 China University of Geosciences (Beijing) and Peking University. The origin of zircon grains, and other exotic minerals of typical crustal origin, in mantle-hosted ophiolitic chromitites are hotly debated. We report a population of zircon grains with ages ranging from Cretaceous (99 Ma) to Neoarchean (2750 Ma), separated from massive chromitite bodies hosted in the mantle section of the supra-subduction (SSZ)-type Mayarí-Baracoa Ophiolitic Belt in eastern Cuba. Most analyzed zircon grains (n = 20, 287 ± 3 Ma to 2750 ± 60 Ma) are older than the early Cretaceous age of the ophiolite body, show negative e Hf (t) (-26 to -0.6) and occasional inclusions of quartz, K-feldspar, biotite, and apatite that indicate derivation from a granitic continental crust. In contrast, 5 mainly rounded zircon grains (297 ± 5 Ma to 2126 ± 27 Ma) show positive e Hf (t) (+0.7 to +13.5) and occasional apatite inclusions, suggesting their possible crystallization from melts derived from juvenile (mantle) sources. Interestingly, younger zircon grains are mainly euhedral to subhedral crystals, whereas older zircon grains are predominantly rounded grains. A comparison of the ages and Hf isotopic compositions of the zircon grains with those of nearby exposed crustal terranes suggest that chromitite zircon grains are similar to those reported from terranes of Mexico and northern South America. Hence, chromitite zircon grains are interpreted as sedimentary-derived xenocrystic grains that were delivered into the mantle wedge beneath the Greater Antilles intra-oceanic volcanic arc by metasomatic fluids/melts during subduction processes. Thus, continental crust recycling by subduction could explain all populations of old xenocrystic zircon in Cretaceous mantle-hosted chromitites from eastern Cuba ophiolite. We integrate the results of this study with petrological-thermomechanical modeling and existing geodynamic models to propose that ancient zircon xenocrysts, with a wide spectrum of ages and H
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- 2018
20. The demersal artisanal fishery of Canary Islands in the EU’s Data Collection Framework
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Jurado-Ruzafa, A. (Alba), Perales-Raya, C. (Catalina), Jiménez, S. (Sebastián), González-Porto, M. (Marcos), González-Jiménez, J. (José), and Villegas, N. (Noemí)
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Small-scale fisheries ,Demersal species ,Data Collection Framework ,The Canary Islands ,Centro Oceanográfico de Canarias ,Pesquerías - Abstract
Poster, The long-term monitoring of small-scale fisheries (SSFs) is essential for the assessment and sustainable management of marine resources in the Canary Islands, where fisheries are mostly artisanal. Here, marine ecosystems are very sensitive to imbalances, with oligotrophic waters and a mixing of temperate, tropical and subtropical species. The SSF targeting demersal species is one of the most important fisheries in the Canary Islands, with mean annual values (period 2013-2014) of 1043 tons of landings, 28623 days of fishing effort and 343 boats. This fishing activity is carried out by a polyvalent and multi-species fleet using small fishing gears (traps, hooks, nets) and performing diurnal fishing trips of less than one day targeting demersal species (parrotfishes, sea breams, morays, amberjacks, alfonsinos, shrimps, etc.). In 2014, the Canary Oceanographic Center of the Instituto Español de Oceanografía proposed the inclusion of this métier in the Spanish National Programme, under the EU’s Data Collection Framework (DCF*) for the collection and management of fisheries data, in the context of the Common Fisheries Policy. Once approved by the Commission, and thanks to the extensive cooperation and support of the local fishermen’s associations, a monthly sampling at sea by scientific observers started in 2015, in Tenerife Island., This project has been funded by the EU through the European Maritime and Fisheries Fund (EMFF) within the National Program of collection, management and use of data in the fisheries sector and support for scientific advice regarding the Common Fisheries Policy
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- 2016
21. Correction to: Organic phosphorus in the terrestrial environment: a perspective on the state of the art and future priorities
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George, T. S., primary, Giles, C. D., additional, Menezes-Blackburn, D., additional, Condron, L. M., additional, Gama-Rodrigues, A. C., additional, Jaisi, D., additional, Lang, F., additional, Neal, A. L., additional, Stutter, M. I., additional, Almeida, D. S., additional, Bol, R., additional, Cabugao, K. G., additional, Celi, L., additional, Cotner, J. B., additional, Feng, G., additional, Goll, D. S., additional, Hallama, M., additional, Krueger, J., additional, Plassard, C., additional, Rosling, A., additional, Darch, T., additional, Fraser, T., additional, Giesler, R., additional, Richardson, A. E., additional, Tamburini, F., additional, Shand, C. A., additional, Lumsdon, D. G., additional, Zhang, H., additional, Blackwell, M. S. A., additional, Wearing, C., additional, Mezeli, M. M., additional, Almås, Å. R., additional, Audette, Y., additional, Bertrand, I., additional, Beyhaut, E., additional, Boitt, G., additional, Bradshaw, N., additional, Brearley, C. A., additional, Bruulsema, T. W., additional, Ciais, P., additional, Cozzolino, V., additional, Duran, P. C., additional, Mora, M. L., additional, de Menezes, A. B., additional, Dodd, R. J., additional, Dunfield, K., additional, Engl, C., additional, Frazão, J. J., additional, Garland, G., additional, González Jiménez, J. L., additional, Graca, J., additional, Granger, S. J., additional, Harrison, A. F., additional, Heuck, C., additional, Hou, E. Q., additional, Johnes, P. J., additional, Kaiser, K., additional, Kjær, H. A., additional, Klumpp, E., additional, Lamb, A. L., additional, Macintosh, K. A., additional, Mackay, E. B., additional, McGrath, J., additional, McIntyre, C., additional, McLaren, T., additional, Mészáros, E., additional, Missong, A., additional, Mooshammer, M., additional, Negrón, C. P., additional, Nelson, L. A., additional, Pfahler, V., additional, Poblete-Grant, P., additional, Randall, M., additional, Seguel, A., additional, Seth, K., additional, Smith, A. C., additional, Smits, M. M., additional, Sobarzo, J. A., additional, Spohn, M., additional, Tawaraya, K., additional, Tibbett, M., additional, Voroney, P., additional, Wallander, H., additional, Wang, L., additional, Wasaki, J., additional, and Haygarth, P. M., additional
- Published
- 2017
- Full Text
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22. Organic phosphorus in the terrestrial environment: a perspective on the state of the art and future priorities
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George, T. S., primary, Giles, C. D., additional, Menezes-Blackburn, D., additional, Condron, L. M., additional, Gama-Rodrigues, A. C., additional, Jaisi, D., additional, Lang, F., additional, Neal, A. L., additional, Stutter, M. I., additional, Almeida, D. S., additional, Bol, R., additional, Cabugao, K. G., additional, Celi, L., additional, Cotner, J. B., additional, Feng, G., additional, Goll, D. S., additional, Hallama, M., additional, Krueger, J., additional, Plassard, C., additional, Rosling, A., additional, Darch, T., additional, Fraser, T., additional, Giesler, R., additional, Richardson, A. E., additional, Tamburini, F., additional, Shand, C. A., additional, Lumsdon, D. G., additional, Zhang, H., additional, Blackwell, M. S. A., additional, Wearing, C., additional, Mezeli, M. M., additional, Almås, Å. R., additional, Audette, Y., additional, Bertrand, I., additional, Beyhaut, E., additional, Boitt, G., additional, Bradshaw, N., additional, Brearley, C. A., additional, Bruulsema, T. W., additional, Ciais, P., additional, Cozzolino, V., additional, Duran, P. C., additional, Mora, M. L., additional, de Menezes, A. B., additional, Dodd, R. J., additional, Dunfield, K., additional, Engl, C., additional, Frazão, J. J., additional, Garland, G., additional, González Jiménez, J. L., additional, Graca, J., additional, Granger, S. J., additional, Harrison, A. F., additional, Heuck, C., additional, Hou, E. Q., additional, Johnes, P. J., additional, Kaiser, K., additional, Kjær, H. A., additional, Klumpp, E., additional, Lamb, A. L., additional, Macintosh, K. A., additional, Mackay, E. B., additional, McGrath, J., additional, McIntyre, C., additional, McLaren, T., additional, Mészáros, E., additional, Missong, A., additional, Mooshammer, M., additional, Negrón, C. P., additional, Nelson, L. A., additional, Pfahler, V., additional, Poblete-Grant, P., additional, Randall, M., additional, Seguel, A., additional, Seth, K., additional, Smith, A. C., additional, Smits, M. M., additional, Sobarzo, J. A., additional, Spohn, M., additional, Tawaraya, K., additional, Tibbett, M., additional, Voroney, P., additional, Wallander, H., additional, Wang, L., additional, Wasaki, J., additional, and Haygarth, P. M., additional
- Published
- 2017
- Full Text
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23. Timing the tectonic mingling of ultramafic rocks and metasediments in the southern section of the coastal accretionary complex of central Chile
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Romero, R., González-Jiménez, J., Barra, F., Leisen, M., Garrido, L., Talavera, Cristina, Gain, S., Griffin, W., O Reilly, S., Reich, M., Morata, D., Romero, R., González-Jiménez, J., Barra, F., Leisen, M., Garrido, L., Talavera, Cristina, Gain, S., Griffin, W., O Reilly, S., Reich, M., and Morata, D.
- Abstract
Uranium-lead ages are reported for zircons from ultramafic bodies and metamorphic host rocks of the Western Series that outcrop at La Cabaña, in the southern section of the coastal accretionary complex of central Chile. Metasedimentary mica schists hosting the ultramafic bodies contain a main detrital zircon population of Devonian age (365–380 Ma) clustering around ~368 Ma, differing significantly from neighbouring areas where Devonian zircons are scarce. Zircons from the metasomatic reaction zones (albitites and chloritites), formed during the emplacement and alteration of the ultramafic bodies, are mainly Ordovician (~478 Ma) and lack Devonian zircons, resembling a typical detrital zircon pattern from other locations in the Western Series. Zircons from the chloritite reaction zone of the Lavanderos serpentinite, the easternmost ultramafic body in La Cabaña, are in textural equilibrium with metamorphic ilmenite. Some of these zircons yield an average age of 283.4 ± 7 Ma (n = 6) which is identical, within error, to a previously reported K-Ar fuchsite cooling age of 282 ± 6 Ma from the reaction zone. Most zircons extracted from chromitite boulders have euhedral oscillatory-zoned growth patterns with a similar range of ages than those reported for the Western Series (324–1090 Ma; n = 12), except for two zircons with cloudy appearance and high U/Th ratios which yielded an average age of 285.5 ± 7 Ma. The presence of Early Permian zircons (~280–290 Ma) in all studied rocks suggests remobilization of Zr, possibly triggered by metasomatic fluids released during the disequilibrium reaction associated with the tectonic emplacement of the ultramafic rocks into the metasedimentary rock. Simultaneously with the formation of metasomatic zircons, Palaeozoic and Mesoproterozoic zircons from the metasedimentary rocks were mechanically incorporated into the ultramafic rocks, thus providing a record of the timing of crustal emplacement of the ultramafic rocks into the accretionary c
- Published
- 2017
24. The recycling of chromitites in ophiolites from southwestern North America
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González-Jiménez, J., Camprubí, A., Colás, V., Griffin, W., Proenza, J., O'Reilly, S., Centeno-García, E., García-Casco, A., Belousova, E., Talavera, Cristina, Farré-de-Pablo, J., Satsukawa, T., González-Jiménez, J., Camprubí, A., Colás, V., Griffin, W., Proenza, J., O'Reilly, S., Centeno-García, E., García-Casco, A., Belousova, E., Talavera, Cristina, Farré-de-Pablo, J., and Satsukawa, T.
- Abstract
© 2017 Elsevier B.V. Podiform chromitites occur in mantle peridotites of the Late Triassic Puerto Nuevo Ophiolite, Baja California Sur State, Mexico. These are high-Cr chromitites [Cr# (Cr/Cr + Al atomic ratio = 0.61–0.69)] that contain a range of minor- and trace-elements and show whole-rock enrichment in IPGE (Os, Ir, Ru). That are similar to those of high-Cr ophiolitic chromitites crystallised from melts similar to high-Mg island-arc tholeiites (IAT) and boninites in supra-subduction-zone mantle wedges. Crystallisation of these chromitites from S-undersaturated melts is consistent with the presence of abundant inclusions of platinum-group minerals (PGM) such as laurite (RuS 2 )-erlichmanite (OsS 2 ), osmium and irarsite (IrAsS) in chromite, that yield T MA ˜ T RD model ages peaking at ~ 325 Ma. Thirty-three xenocrystic zircons recovered from mineral concentrates of these chromitites yield ages (2263 ± 44 Ma to 278 ± 4 Ma) and Hf-O compositions [? Hf (t) = - 18.7 to + 9.1 and 18 O values < 12.4‰] that broadly match those of zircons reported in nearby exposed crustal blocks of southwestern North America. We interpret these chromitite zircons as remnants of partly digested continental crust or continent-derived sediments on oceanic crust delivered into the mantle via subduction. They were captured by the parental melts of the chromitites when the latter formed in a supra-subduction zone mantle wedge polluted with crustal material. In addition, the Puerto Nuevo chromites have clinopyroxene lamellae with preferred crystallographic orientation, which we interpret as evidence that chromitites have experienced high-temperature and ultra high-pressure conditions ( < 12 GPa and ~ 1600 °C). We propose a tectonic scenario that involves the formation of chromitite in the supra-subduction zone mantle wedge underlying the Vizcaino intra-oceanic arc ca. 250 Ma ago, deep-mantle recycling, and subsequent diapiric exhumation in the intra-oceanic basin (the San Hipólito margin
- Published
- 2017
25. Zircon recycling and crystallization during formation of chromite- and Ni-arsenide ores in the subcontinental lithospheric mantle (Serranía de Ronda, Spain)
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González-Jiménez, J., Marchesi, C., Griffin, W., Gervilla, F., Belousova, E., Garrido, C., Romero, R., Talavera, Cristina, Leisen, M., O'Reilly, S., Barra, F., Martin, L., González-Jiménez, J., Marchesi, C., Griffin, W., Gervilla, F., Belousova, E., Garrido, C., Romero, R., Talavera, Cristina, Leisen, M., O'Reilly, S., Barra, F., and Martin, L.
- Abstract
The ultramafic massifs of the Serranía de Ronda (namely Ronda, Ojén and Carratraca) are portions of Proterozoic (~1.2-1.8Ga) subcontinental lithospheric mantle (SCLM) affected by partial melting and infiltration of melts. The latter of these events was broadly coeval with the tectonic emplacement of the peridotites into the continental crust in the Early Miocene. This resulted in the formation of chromite and Ni-arsenide ores (Cr-Ni) associated with orthopyroxenites and cordieritites. Six zircons recovered from a massive chromitite sample from the Ronda massif yield both concordant and discordant ages between 2309±37Ma and 109±15Ma, and d18O between 8.3‰ and 9.4‰. Two Proterozoic ages obtained for zircons of this population (1815±9Ma and 1794±17Ma) are identical, within error, to those of zircons reported previously in the garnet pyroxenites of Ronda (1783±37Ma). Similarly, concordant Early Jurassic (192±13Ma) and Cretaceous ages (109±15Ma) obtained from the core and rim, respectively, of a single zircon from the chromitite are also consistent with the ages (180±5Ma, 178±6Ma, and 131±3Ma) already reported for magmatic zircons from corunudum-bearing garnet pyroxenites in the Ronda massif. The observation that chromitites and garnet-pyroxenites contain similar populations of zircons suggests that the parental melts of chromitites inherited zircons from their protolithic garnet pyroxenites, representing relics of oceanic/arc crust recycled in the mantle. Eleven zircons recovered from a massive cordieritite associated with chromitite in the Ronda massif yield scattered concordant and discordant ages between 568Ma and 21Ma, with correspondingly variable d18O (4.8-13.5‰) and unradiogenic Hf-isotope ratios (eHf(t) from -12.36 to -4.43). The youngest age is concordant at 21.18±0.4Ma and matches the ages of zircons from the chromitite (weighted average age of 20.4±0.87Ma, n=4) and a plagioclasite dyke (scattering between 20.1±0.2Ma and 17.9±0.1Ma; n=11) associated with the C
- Published
- 2017
26. Désignation de zones littorales, sélection et évaluation d’indicateurs
- Author
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González-Lorenzo, J.G. (José Gustavo), Santamaría, M.T.G. (María Teresa García), Armas, D. (Demetrio) de, Jiménez, S. (Sebastián), González-Gil, S. (Sonsoles), González-Jiménez, J. (José), Boza-Vindel, C. (Cristina), Bartolomé-Baraza, A. (Aurora), Tello-Antón, M.O. (María Olvido), Hernández-González, C.L. (Carlos Luis), Martín-Sosa, P. (Pablo), Rodríguez, J.E. (Jaime Ezequiel), González, E.L. (Erika Lucía), González, Y. (Yulimar), Bilbao, A. (Alberto), Pérez, Y. (Yeray), Betancort, J.R. (Juana Rosa), and Santamaría, M.T.G. (María Teresa García)
- Subjects
Zona litoral ,Indicadores ,Gestión Integrada ,Estado ecológico - Published
- 2015
27. Caracterización del Sur de Fuerteventura
- Author
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Martín-Sosa, P. (Pablo), González-Porto, M. (Marcos), Almón, B. (Bruno), Acosta-Díaz, C. (Carolina), Arrese-González, B. (Beatriz), Falcón, J.M. (Jesús), Pascual-Fernández, J.J. (José Jaime), Chinea-Mederos, I. (Inés), Fraile-Nuez, E. (Eugenio), Presas-Navarro, C. (Carmen), Jiménez, S. (Sebastián), Bartolomé-Baraza, A. (Aurora), Tello-Antón, M.O. (María Olvido), Barreiro-Jueguen, S. (Santiago), Sarralde-Vizuete, R. (Roberto), González-Jiménez, J. (José), Papiol, V. (Vanesa), Boza-Vindel, C. (Cristina), Brito, A. (Alberto), Cartes, J. (Joan), Pascual-Alayón, P.J. (Pedro José), Druet-Vélez, M. (María), Acosta-Yepes, J. (Juan), Mangas, J. (José), Quevedo, L. (Luis), López-Rodríguez, F.J. (Francisco José), McKnight, L. (Lydia), Anger, J. (Johnatan), Vélez-Belchí, P. (Pedro), Benítez-Barrios, V.M. (Verónica María), González-Irusta, J.M. (José Manuel), Santana-Talavera, A. (Agustín), and Díaz-Rodríguez, P. (Pablo)
- Subjects
Sensitive habitats ,Marine Protected Areas ,Biodiversidad marina ,Seamounts ,Amanay ,Conservation ,Directiva Hábitats ,Gobernance ,Benthopelagic communities ,Modelización de comunidades e indicadores ecológicos ,Centro Oceanográfico de Canarias ,Hydrography ,Pesquerías ,Medio Marino ,Idoneidad de hábitats ,Arrecifes ,El Banquete ,Artisanal fisheries ,Comunidades endobentónicas ,Geomorphology ,Comunidades epibentónicas ,Biodiversity ,Pesquería artesanal ,Hidrografía ,Geomorfología ,Comunidades bentopelágicas ,Fuerteventura ,Endobenthic communities ,Epibenthic communities ,Habitat suitability ,Ecosistemas marinos ,Conservación ,Gobernanza ,Montes submarinos ,Reefs ,Hábitats sensibles ,Biocenosis ,Áreas Marinas Protegidas ,Marine ecosystems ,Community and ecologic indicators modelling - Abstract
Se integra información hidrográfica, geomorfológica, sedimentológica, biológica, sobre hábitats marinos y pesquera, para establecer las bases ecológicas necesarias para la protección y conservación del Sur de Fuerteventura (Montes de Amanay y El Banquete), El proyecto INDEMARES ha permitido utilizar amplios medios económicos y personales para estudiar en detalle y desde múltiples perspectivas la zona del Sur de Fuerteventura (montes de Amanay y El Banquete). Se han aplicado metodologías para el estudio de la hidrografía, caracterizando la región, describiendo sus principales masas de agua y la hidrodinámica de las corrientes. También se ha abordado la geología de la zona, incluyendo levantamientos batimétricos, perfiles sísmicos, muestreos de sedimento y petrológicos, obteniendo modelos digitales del terreno, mapas de tipos de fondo, geomorfológicos. Se han caracterizado las comunidades bentopelágicas, demersales, epibentónicas y endobentónicas, prestando especial atención a aquellas que conforman o estructuran los hábitats sensibles cuyo inventariado y cartografía era objeto principal del proyecto. Los trabajos de identificación de hábitats se han realizado con muestreadores directos, pero también con muestreadores visuales, que han permitido hacer un mayor esfuerzo de muestreo sin aumentar el impacto sobre los fondos de la zona. Por otro lado se ha estudiado la huella pesquera de la zona por medio del análisis de los datos VMS y los cuadernos de pesca proporcionados por la SGP, además de una ardua labor a pie de puerto de entrevistas y encuestas. Toda la información ha sido gestionada y analizada por diferentes grupos de investigación de diferentes centros (Universidad de La Laguna, Instituto Universitario de Ciencias Políticas y Sociales, Universidad de Las Palmas de Gran Canaria, Instituto de Ciencias del Mar de Barcelona, Universidad de Barcelona, Centro de Investigaciones Medioambientales del Atlántico, Centro Oceanográfico de Santander y Centro Oceanográfico de Málaga del Instituto Español de Oceanografía, …), aunque el grueso de esta labor, además de la coordinación, se ha llevado a cabo en el Centro Oceanográfico de Canarias del Instituto Español de Oceanografía. Los resultados permiten tener un conocimiento profundo y multidisciplinar de la zona de estudio comparable a pocos proyectos de investigación marina en la Macaronesia. El estudio oceanográfico, el geológico, y el de las comunidades biológicas, ha permitido la caracterización de los hábitats de la zona, y su cartografiado mediante el intenso muestreo y la aplicación de análisis de idoneidad de hábitats., INDEMARES Project made possible to bring together economic and staff resources to study in detail, and from multiple perspectives, the area of South of Fuerteventura (Amanay and El Banquete Semounts). Methodologies have been applied to study hydrography, making a regional characterization, depicting main water masses, and current hydrodynamics. Geology has been tackled including bathymetric uplifting, seismic profiles, sediment and petrological sampling, obtaining digital terrain models, type of bottom maps, geomorphological maps, as an output. Benthopelagic, demersal, epibenthic and endobenthic communities have been characterized, paying special attention to sensitive habitats which inventory and mapping was the project’s main aim. Habitat identification has been made with direct and visual samplers, the latter making a major sampling effort possible without an increase of bottom impact. Moreover, fisheries footprint has been identified by Vessel Monitoring System data, together with logbooks from Secretaría General de Pesca (Fisheries Ministry), as well as a hard interviewing and surveying task at landing points. Information has been managed and analysed by different research groups from different Centres (Universidad de La Laguna, Instituto Universitario de Ciencias Políticas y Sociales, Universidad de Las Palmas de Gran Canaria, Instituto de Ciencias del Mar de Barcelona, Universidad de Barcelona, Centro de Investigaciones Medioambientales del Atlántico, Centro Oceanográfico de Santander y Centro Oceanográfico de Málaga del Instituto Español de Oceanografía), although the main body of the work, plus coordination, has been made by the Canary Islands Oceanographic Centre, from the Spanish Institute of Oceanography. Results let us have a multidisciplinary profound knowledge of the study zone, comparable to few other marine research projects off Macaronesia. The study about oceanography, geology and biologic communities has allowed the habitats characterization and mapping by means of intensive sampling and habitat suitability analysis., Instituto Español de Oceanografía, Comisión Europea Programa LIFE+, Fundación Biodiversidad
- Published
- 2014
28. Mantle Recycling: Transition Zone Metamorphism of Tibetan Ophiolitic Peridotites and its Tectonic Implications
- Author
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Griffin, W. L., primary, Afonso, J. C., additional, Belousova, E. A., additional, Gain, S. E, additional, Gong, X.-H., additional, González-Jiménez, J. M., additional, Howell, D., additional, Huang, J.-X., additional, McGowan, N., additional, Pearson, N. J., additional, Satsukawa, T., additional, Shi, R., additional, Williams, P., additional, Xiong, Q., additional, Yang, J.-S., additional, Zhang, M., additional, and O’Reilly, Suzanne Y., additional
- Published
- 2016
- Full Text
- View/download PDF
29. Inventario y cartografía de los hábitats y de la huella pesquera de los montes submarinos 'Amanay' y 'El Banquete' (Sur de Fuerteventura, Islas Canarias). Análisis de criterios para la designación del área marina protegida
- Author
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Martín-Sosa, P. (Pablo), González-Porto, M. (Marcos), Almón, B. (Bruno), Acosta-Díaz, C. (Carolina), Arrese-González, B. (Beatriz), Falcón, J.M. (Jesús), Pascual-Fernández, J.J. (José Jaime), Chinea-Mederos, I. (Inés), Bartolomé-Baraza, A. (Aurora), González-Jiménez, J. (José), Barreiro-Jueguen, S. (Santiago), Sarralde-Vizuete, R. (Roberto), González-Irusta, J.M. (José Manuel), Díaz-Fernández, Pablo, Brito, A. (Alberto), and Jiménez, S. (Sebastián)
- Subjects
Sensitive habitats ,Marine Protected Areas ,Biodiversidad marina ,Seamounts ,Amanay ,Conservation ,Directiva Hábitats ,Gobernance ,Benthopelagic communities ,Modelización de comunidades e indicadores ecológicos ,Hydrography ,Pesquerías ,Idoneidad de hábitats ,Arrecifes ,El Banquete ,Artisanal fisheries ,Comunidades endobentónicas ,Geomorphology ,Comunidades epibentónicas ,Biodiversity ,Pesquería artesanal ,Hidrografía ,Geomorfología ,Comunidades bentopelágicas ,Fuerteventura ,Endobenthic communities ,Epibenthic communities ,Habitat suitability ,Ecosistemas marinos ,Conservación ,Gobernanza ,Montes submarinos ,Reefs ,Hábitats sensibles ,Biocenosis ,Áreas Marinas Protegidas ,Marine ecosystems ,Community and ecologic indicators modelling - Abstract
Sur de Fuerteventura is one of the areas chosen to be depicted in the frame of INDEMARES project. The midpoint of the study area is located at 25 km from Fuerteventura and 65 km from Gran Canaria. The main aim of the project was to end up with an inventory and mapping of habitats and fisheries footprint off the study area, information which would let the administrations to establish a new Natura 2000 area, trying to reconcile protection of biodiversity with artisanal local economic activities. Methodology approach complies with a multidisciplinary perspective, having described the area from geological, oceanographic, biological and fisheries points of view. Several surveys have taken place since 2009 to 2013 at Amanay and El Banquete waters. Data from VMS (Vessel Monitoring System) were used, combined with interviews to users (fishers), sampling at landing points and onboard observation programs, to describe the fishery uses in the area. Thirteen different types of communities have been identified as “Habitat 1170, Reefs”, following Annex 1 from Habitats Directive (Council Directive 92/43/CEE) from European Union. All of them have three dimensional structure and species with certain size turning these areas into important containers of biodiversity and hot spots for shelter. About protected species by Habitats Directive, Centrostephanus longispinus (Philippi, 1845) belongs to Annex IV. Chilomycterus reticulatus (Linnaeus, 1758) is included in the Canary Islands Catalog of Protected Species as a vulnerable species. Within the Red List of Threatened Species of the International Union for the Conservation of Nature, we can find several fishes as endangered species, Squatina squatina (Linnaeus, 1758) as critically endangered, while in the area can also be found several vulnerable species, special importance have several elasmobranchs species. Subsequent studies about deep water white corals Lophelia pertusa (Linnaeus, 1758) and Madrepora oculata Linnaeus, 1758, present in the study area, could conclude with these species inclusion in the list. Fishery activities identified during this study don’t interact with the bottom (tuna fishing with pole lines and surface longlines for sworfish), or as the most frequent activity, artisanal hook and line local fisheries, has very little impact on the bottom (arose from anchoring). Ecological assessment results from values assigned to different community or species features or parameters, not always in a quantitative manner, depending on their diverse nature. To use a totally aseptic quantitative index is impossible; therefore, an often used tool is to resort to an expert panel (group of experts) which members individually assign a value to each of the assessed parameters. This solution absorbs bias produced by individual criteria. We established three value levels (low, medium and high) for each of the twelve parameters used. After all we end up with a map of an ecological assessment index (EAI) which is simple and weighs every parameter equally. Higher EAI is assigned to bathial rocky bottoms with anthipatarians, closely followed by Corallium spp deep water coral reefs and circalittoral rocky bottoms with Antipathella wollastoni (Gray, 1857). Bathial rocky bottoms with Callogorgia verticillata (Pallas, 1766) and circalittoral rocky bottoms with calcareous algae concretions and leafy algae have a mid-high EAI. We find good collective action preconditions, which explain the capacity of human communities to design, implement and enforce designed institutions to resources management and protection. Strong ishermen organizations, leadership among effective users and experience in conservation initiatives and an a priori willing attitude are present. A proper step-zero at Sur de Fuerteventura marine protected area will be provided by sharing available scientific information with users, public report and open and full consultation about the protection possibilities, giving time to assimilation, involving local stakeholders, and finding coordination among institutions and security bodies to ensure protection measures enforcement.
- Published
- 2014
30. Banco de La Concepción (Canary Islands): Vunerable Marine Ecosystems (VMEs) spatial distribution
- Author
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González-Porto, M. (Marcos), Almón, B. (Bruno), Falcón, J.M. (Jesús), González-Irusta, J.M. (José Manuel), González-Jiménez, J. (José), Barreiro-Jueguen, S. (Santiago), Sarralde-Vizuete, R. (Roberto), Brito, A. (Alberto), Jiménez, S. (Sebastián), and Martín-Sosa, P. (Pablo)
- Subjects
modelización de comunidades e indicadores ecológicos ,habitat suitability ,ecosistemas marinos ,idoneidad de hábitats ,sensitive habitats ,Banco de La Concepción ,conservation ,Seamounts ,arrecifes ,conservación ,Directiva Hábitats ,biodiversidad marina ,reefs ,community and ecologic indicators modelling ,montes submarinos ,Centro Oceanográfico de Canarias ,Medio Marino ,marine ecosystems ,hábitats sensibles ,áreas marinas protegidas ,marine protected areas ,biodiversity - Abstract
Banco de La Concepción is one of the areas chosen to be depicted in the frame of INDEMARES project. It is located at 71 km to the NE of Lanzarote. Methodology approach complies with a multidisciplinary perspective, having described the area from geological, oceanographic, biological and fisheries points of view. Habitat identification and mapping has been possible through intense sampling and the use of habitat suitability modeling. Species structuring sensitive habitats have played a leading role, since those habitats inventory and mapping were the project’s main aim. Direct samplers have been complemented with visual samplers, the latter permitting a higher sampling effort without increasing benthic habitat impact. Several types of communities have been identified as “Habitat 1170, Reefs”, following Annex 1 from Habitats Directive (Council Directive 92/43/CEE) from European Union, representing VMEs. We have combined various types of multivariate analyses to describe the structure and spatial distribution of benthic communities, to analyze the relationship between these communities and environmental parameters, and subsequently, to build a community distribution model to predict the spatial distribution of the communities, creating community distribution maps covering the entire area. As a result of the analysis, we have identified, at bathyal zone, rocky bottoms with anthipatarians, other with big size hexactinellid sponges (Asconema setubalense Kent, 1870), frequently seen at rocky escarpments and outcrops. We also find at this depth Callogorgia verticillata (Pallas, 1766) and Narella bellissima (Kükenthal, 1915) erect sea fans real forests, accompanied by Bebryce mollis Philippi, 1842 and Eunicella verrucosa (Pallas, 1766) high densities. Pheronema carpenteri (Thomson, 1869) and Paramuricea biscaya Grasshoff, 1977 appear on rocky outcrops from 500 m down to 1500 m. Two kinds of VMEs are found from 500 m to 1000 m, isidid corals and lithistid sponges (Leiodermatium- Neophryssospongia), siliceous sponges mixed on rocky bottom silted up with sediments at upper bathyal zone. This community mixes with anthozoan Viminella flagellum (Johnson, 1863) from 500 m down to 1600 m, where we can also find Corallium niobe Bayer, 1964 and Corallium tricolor (Johnson, 1899) deep water coral reefs. Dendrophyllia cornigera (Lamarck, 1816) and Phakellia ventilabrum (Linnaeus, 1767) are remarkable 1170 habitat communities cohabiting with deep water white corals Lophelia pertusa (Linnaeus, 1758) and Madrepora oculata Linnaeus, 1758 at lower continental shelf and upper slope rocky bottoms. Here we can also find dead coral framework.
- Published
- 2014
31. Propuestas conjuntas de Unidades y Planes de Gestión en el Caso de Estudio 'Pesquerías Artesanales de las Islas Canarias. Tenerife'
- Author
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Santamaría, M.T.G. (María Teresa García), Falcón, J.M. (Jesús), Jiménez, S. (Sebastián), Villegas, N. (Noemí), and González-Jiménez, J. (José)
- Subjects
Pesquerias Artesanales ,Planes de Gestión ,Centro Oceanográfico de Canarias ,Pesquerías ,Unidades de Gestión - Published
- 2014
32. Project GEPETO. Final Report WP5. Management Plan. Activity 1. State of the art: Review of management plans currently in practice
- Author
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Consortium GEPETO, Santamaría, M.T.G. (María Teresa García), Jiménez, S. (Sebastián), and González-Jiménez, J. (José)
- Subjects
Planes de Gestión ,Pesquerías Mixtas ,Centro Oceanográfico de Canarias ,Pesquerías ,Pesquerías Artesanales ,Unidades de Gestión - Published
- 2014
33. Project GEPETO. Final Report WP5. Management Plan. Activity 2. To propose a working plan for each of the management units selected
- Author
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Consortium GEPETO, Santamaría, M.T.G. (María Teresa García), Jiménez, S. (Sebastián), and González-Jiménez, J. (José)
- Subjects
Planes de Gestión ,Pesquerías Mixtas ,Centro Oceanográfico de Canarias ,Pesquerías ,Pesquerías Artesanales ,Unidades de Gestión - Published
- 2014
34. Assessing sea grass meadows condition at 'El Río' Special Area of Conservation off 'La Graciosa e Islotes del Norte de Lanzarote' Marine Reserve
- Author
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Jiménez, S. (Sebastián), González, Y. (Yulimar), González, E.L. (Erika Lucía), González-Jiménez, J. (José), Hernández-González, C.L. (Carlos Luis), Martín-Sosa, P. (Pablo), González-Lorenzo, J.G. (José Gustavo), and Fernández, M.Á.R. (María de los Ángeles Rodríguez)
- Subjects
Marine Reserve ,La Graciosa ,Centro Oceanográfico de Canarias ,Lanzarote ,Medio Marino ,Cymodosea nodosa - Abstract
Cymodosea nodosa meadows, known as ‘sebadales’ or ‘manchones’ at Canary Islands, represent EUNIS habitat type code A5.5311, called Macaronesian Cymodocea beds. As it’s described at European Union Habitats Directive (92/43/CEE) Annex 1, sea grass meadows belong to 1110 Sandbanks which are slightly covered by seawater all the time, within Natura 2000 Network. Several ‘sebadales’ throughout the archipelago are included in this Network as Special Areas of Conservation. Cymodosea nodosa is regionally included within the Canary Islands Protected Species List (Ley 4/2010), as a species ‘of interest to ecosystems of Canary Islands”, is usually found at a narrow depth range (10 to 20 m of depth) and, on the whole, best structured meadows are settled at sheltered bays, away from wave and current beating, flimsier at exposed areas. Deeper meadows are also sparser, being C. nodosa replaced by green algae Caulerpa prolifera and Caulerpa racemosa, although mixed algae-sea grass meadows are often found at different depths. The project Assessment of marine flora (‘sebadal’, ma¨erl, ‘mujo’) of ‘La Graciosa e Islotes del Norte de Lanzarote’ Marine Reserve, funded by ‘Viceconsejer´ıa de Pesca y Aguas de la Consejer´ıa de Agricultura, Ganader´ıa, Pesca y Aguas’, Canary Islands Government, has had the aim of assessing sea grass meadows condition and distribution at ‘El R´ıo’ Natura 2000 Network Special Area of Conservation, the channel between La Graciosa and Lanzarote. ‘LA GRACIOSA 1311’ cruise was performed within the framework of the project. First of all previous information on sea grass shallow distribution (up to a depth of 20 m) in the study area was reviewed. Afterwards, a tugged underwater video camera was used onboard of the Marine Reserve Surveillance Vessel to update cartographic info performing a grid of sampling stations, covering previously known distribution limits and verifying current presence/absence data and density. Furthermore, population parameters were obtained in order to assess ‘sebadal’ condition. Fixed stations were selected in regards to this process, and methodology applied on them was as follows: five radial arranged transects were performed, identifying fragmentation (it estimates meadow continuity regarding observed cover), density (mean value of several shoots number counts with 20 x 20 cm grids placed every 2 m), height (mean value in cm of 10 independent samples by transect) and fish and macroinvertebrate species richness for each transect. Graphic picture of sea grass density was made depending on two levels: low density level transects ( 10 shoots/grid ( 50 shoots/m2) and medium density level transects ( 10 shoots/grid ( 50 shoots/m2). Main study result is an estimate for the study region (‘El R´ıo’) and time of year of Cymodocea nodosa population total distribution cover which comes to 1.640.076 m2, including a higher density ‘sebadal’ of 178.256 m2.
- Published
- 2014
35. Inventory and mapping of habitats and fisheries footprint off 'Banco de La Concepción' seamount (Canary Islands). Criteria analysis for the marine protected area establishment
- Author
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Martín-Sosa, P. (Pablo), González-Porto, M. (Marcos), Almón, B. (Bruno), Acosta-Díaz, C. (Carolina), Arrese-González, B. (Beatriz), Falcón, J.M. (Jesús), Pascual-Fernández, J.J. (José Jaime), Bartolomé-Baraza, A. (Aurora), González-Jiménez, J. (José), Barreiro-Jueguen, S. (Santiago), Sarralde-Vizuete, R. (Roberto), González-Irusta, J.M. (José Manuel), Brito, A. (Alberto), and Jiménez, S. (Sebastián)
- Subjects
comunidades epibentónicas ,modelización de comunidades e indicadores ecológicos ,habitat suitability ,idoneidad de hábitats ,gobernanza ,Banco de La Concepción ,comunidades bentopelágicas ,pesquerías ,Seamounts ,endobenthic communities ,arrecifes ,Directiva Hábitats ,reefs ,montes submarinos ,hydrography ,artisanal fisheries ,Centro Oceanográfico de Canarias ,pesquería artesanal ,Medio Marino ,marine ecosystems ,hábitats sensibles ,epibenthic communities ,biodiversity ,ecosistemas marinos ,sensitive habitats ,conservation ,biocenosis ,conservación ,geomorphology ,biodiversidad marina ,benthopelagic communities ,hidrografía ,community and ecologic indicators modelling ,áreas marinas protegidas ,gobernance ,geomorfología ,comunidades endobentónicas ,marine protected areas - Abstract
Banco de La Concepción is one of the areas chosen to be depicted in the frame of INDEMARES project. It is located at 71 km to the NE of Lanzarote. The main aim of the project was to end up with an inventory and mapping of habitats and fisheries footprint off the study area, information which would let the administrations to establish a new Natura 2000 area, trying to reconcile protection of biodiversity with artisanal local economic activities. Methodology approach complies with a multidisciplinary perspective, having described the area from geological, oceanographic, biological and fisheries points of view. Several surveys have taken place since 2009 to 2013 at Banco de La Concepción waters. Data from VMS (Vessel Monitoring System) were used, combined with interviews to users (fishers), to describe the fishery uses in the area. Ten different types of communities have been identified as “Habitat 1170, Reefs”, following Annex 1 from Habitats Directive (Council Directive 92/43/CEE) from European Union. All of them have three dimensional structure and species with certain size turning these areas into important containers of biodiversity and hot spots for shelter. About protected species by Habitats Directive, Centrostephanus longispinus (Philippi, 1845) belongs to Annex IV. Neophryssospongia nolitangere (Schmidt, 1870) is included in the Canary Islands Catalog of Protected Species as a vulnerable species. Within the Red List of Threatened Species of the International Union for the Conservation of Nature, we can find several fishes as endangered species, while in the area can also be found several vulnerable species, special importance have several elasmobranchs species. Subsequent studies about deep water white corals Lophelia pertusa (Linnaeus, 1758) and Madrepora oculata Linnaeus, 1758, present in the study area, could conclude with these species inclusion in the list. Fishery activities identified during this study with a higher degree of fishing intensity (tuna fishing with pole lines and surface longlines for sworfish) don’t interact with the bottom. Electric reel hook and line and bottom horizontal longline activities are not so frequent, but while the first one has very little impact on the bottom (arose from anchoring), the latter is performed by only two vessels but with a high degree of intensity and very spatially concentrated at rocky bottom areas, generating an important impact on the bottom during the raising maneuver by getting snagged with benthic epifauna. Ecological assessment results from values assigned to different community or species features or parameters, not always in a quantitative manner, depending on their diverse nature. To use a totally aseptic quantitative index is impossible; therefore, an often used tool is to resort to an expert panel (group of experts) which members individually assign a value to each of the assessed parameters. This solution absorbs bias produced by individual criteria. We established three value levels (low, medium and high) for each of the twelve parameters used. After all we end up with a map of an ecological assessment index (EAI) which is simple and weighs every parameter equally. Higher EAI is assigned to bathial rocky bottoms with anthipatarians, closely followed by Corallium spp deep water coral reefs. Bathial rocky bottoms with Callogorgia verticillata (Pallas, 1766) have a mid-high EAI. We are not very optimistic about collective action preconditions, which explain the capacity of human communities to design, implement and enforce designed institutions to resources management and protection. There is an absence of fishermen organizations closely linked to the area, of leadership among effective users, which have a very limited experience in conservation initiatives and an a priori reluctant attitude. A proper step-zero at Banco de La Concepción marine protected area will be provided by sharing available scientific information with users, public report and open and full consultation about the protection possibilities, giving time to assimilation, involving local stakeholders, and finding coordination among institutions and security bodies to ensure protection measures enforcement, EC Life+ Project INDEMARES (Code no. 110300900)
- Published
- 2014
36. Proposal of an index of market capitalization for the stock market MILA
- Author
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González-Jiménez, J. C. (Juan Camilo), Lochmüller, C. (Christian), and Yarce-Vélez, R. (Ricardo )
- Subjects
STOCK EXCHANGE ,ÍNDICE BURSÁTIL ,RSO00090 ,BOLSA DE VALORES ,REGIONAL INVESTMENT ,STOCK INDEX ,ORGANIZACIÓN E INDUSTRIA ,INVERSIÓN REGIONAL ,MILA ,ORGANIZATION AND INDUSTRY - Abstract
Desde mediados del año 2010 se realizaban reuniones respecto a la integración de un nuevo mercado que involucraba tres grandes economías de América Latina de tal modo que se facilitaran operaciones bursátiles entre estos tres países, que se generara la oportunidad de invertir en un mercado más amplio y que se incentivara la inversión en economías emergentes. Este desarrollo justifica proponer un índice que reflejará el comportamiento del precio de las acciones más representativas que hacen parte del nuevo mercado MILA (Mercado Integrado Latinoamericano). Motivado por lo anterior, este artículo es resultado de un trabajo de grado a nivel de pregrado que se desarrolló durante el segundo semestre de 2011, el cual propone el desarrollo de un índice bursátil denominado “MILCA P”. La propuesta se presenta en tres partes. En la primera se analizan los mercados de los tres países que conforman el MILA , se revisan las formas cómo construir un índice y se describen algunos índices ya existentes y de referencia. Se exponen metodologías utilizadas para la construcción del índice propuesto y se definen los parámetros y variables que se van a utilizar en su construcción. El índice se construye basado en datos históricos desde el primero de Junio de 2006, partiendo de una base de 1000 puntos, y se construye a lo largo de 5 años teniendo en cuenta cada fecha clave de rebalanceo y selección de canasta, para finalmente presentar la validación y, al respecto, los resultados obtenidos del índice propuesto. Since the middle of 2010 meetings were held regarding the creation of a new market that involved and integrates three major Latin American economies with the objective to facilitate trading between these three countries and in order to generate opportunities to invest in a wider market and to stimulate investment in emerging economies. This development justifies the proposal of an index which reflects the movement of price of the most representative stocks that are traded in the new MILA (Mercado Integrado Latinoamericano) market. This article is a result of thesis which was developed during the second half of 2011 at the undergraduate level and that proposes the development of a stock market index called "MILCA P". The proposal is presented in three parts. The markets of the three countries that participate in MILA are analized, the concepts to build an undex are analized and some of the existing indexes, that serve as a reference described. The methodologies for the construction of the porposed index are outlined, as well as the parameters and variables that are used in its construction. the index is constructed by using historical data that start from the first of June 2006, from a baseline of a 1000 points, and that comprise a period of five years, taking into account each date for rebalancing and for the selection of the stock basket. Finally, the validation and the obtained results for the proposed index are presented.
- Published
- 2012
37. Evolución de capturas de pequeños pelágicos en la isla de Tenerife durante el periodo 2001-2009
- Author
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Borges-Perera, C., González-Jiménez, J. (José), and Santamaría, M.T.G. (María Teresa García)
- Subjects
Centro Oceanográfico de Canarias ,Pesquerías - Published
- 2010
38. Godlevskite Ni9S8 from Dobromirtsi, Central Rhodopes, Bulgaria: First report for the country and genetic implications
- Author
-
Kerestedjian, T., Gervilla, Fernando, González-Jiménez, J. M., and Proenza, Joaquín A.
- Subjects
Godlevskite ,Serpentinized ultramafics ,Rhodopes ,Bulgaria ,Postmagmatic ,Metamorphic - Abstract
10 pages, 4 figures, 1 table., Godlevskite Ni9S8 is recorded for the first time in Bulgaria. The find comes from chromitites in serpentinized ultramafics (dunites, peridotites), near the village of Dobromirtsi, Central Rhodopes. The postmagmatic assemblage of the chromitites comprises pentlandite, godlevskite, heazlewoodite, maucherite, orcelite, chalcopyrite and gersdorffite (in the order of decreasing abundance). The magmatic assemblage (in unaltered chromites) also includes pentlandite and less heazlewoodite and millerite as well as PGM – laurite, scarce OsIr alloys and Ir-sulpharsenides. The generalized formula of the recorded mineral, derived from microprobe analyses is: Ni8.82 Fe0.14 S8.04. Observed textural and structural specifics of the mineral are interpreted as evidences for a solid state re-equilibration from high-temperature MSS (Monosulfide Solid Solution), stable in the 577 – 436ºC temperature range, followed by slow annealing below 379ºC, well corresponding to the temperature conditions of the regional metamorphic events in the area., We gratefully acknowledge the support, provided by the local chief geologist K. Peryov. Without his kind attention field works in the area wouldn’t be possible, or at least not so successful and pleasant.
- Published
- 2007
39. A LEGO Mindstorms NXT approach for teaching at Data Acquisition, Control Systems Engineering and Real-Time Systems undergraduate courses
- Author
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Cruz-Martín, A., primary, Fernández-Madrigal, J.A., additional, Galindo, C., additional, González-Jiménez, J., additional, Stockmans-Daou, C., additional, and Blanco-Claraco, J.L., additional
- Published
- 2012
- Full Text
- View/download PDF
40. Análisis de las capturas y distribución de los Cefalópodos de la Campaña Guinea-90
- Author
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Ramos, A. (Ana) and González-Jiménez, J. (José)
- Subjects
Centro Oceanográfico de Vigo ,Pesquerías - Published
- 1992
41. The Fluorescent Probe Prodan Characterizes the Warfarin Binding Site on Human Serum Albumin
- Author
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Moreno, F., primary, Cortijo, M., additional, and González-Jiménez, J., additional
- Published
- 1999
- Full Text
- View/download PDF
42. Distribution of platinum-group elements and Os isotopes in chromite ores from Mayarí-Baracoa Ophiolitic Belt (eastern Cuba).
- Author
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Gervilla, F., Proenza, J. A., Frei, R., González-Jiménez, J. M., Garrido, C. J., Melgarejo, J. C., Meibom, A., Díaz-Martínez, R., and Lavaut, W.
- Subjects
PLATINUM group ,TRANSITION metals ,PLATINUM ,CHROMIUM ,MAGMAS ,IGNEOUS rocks ,CHROMITE ,MINERALOGY ,PHYSICAL & theoretical chemistry - Abstract
The Mayarí-Baracoa ophiolitic belt in eastern Cuba hosts abundant chromite deposits of historical economic importance. Among these deposits, the chemistry of chromite ore is very variable, ranging from high Al (Cr#=0.43–0.55) to high Cr (Cr#=0.60–0.83) compositions. Platinum-group element (PGE) contents are also variable (from 33 ppb to 1.88 ppm) and correlate positively with the Cr# of the ore. Bulk PGE abundances correlate negatively with the Pd/Ir ratio showing that chromite concentrates mainly Os, Ir and Ru which gives rise to the characteristic negatively sloped, chrondrite-normalized PGE patterns in many chromitites. This is consistent with the mineralogy of PGEs, which is dominated by members of the laurite–erlichmanite solid solution series (RuS
2 –OsS2 ), with minor amounts of irarsite (IrAsS), Os–Ir alloys, Ru–Os–Ir–Fe–Ni alloys, Ni–Rh–As, and sulfides of Ir, Os, Rh, Cu, Ni, and/or Pd. Measured187 Os/188 Os ratios (from 0.1304 to 0.1230) are among the lower values reported for podiform chromitites. The187 Os/188 Os ratios decrease with increasing whole-rock PGE contents and Cr# of chromite. Furthermore, γOs values of all but one of the chromitite samples are negative indicating a subchondiritc mantle source. γOs decrease with increasing bulk Os content and decreasing187 Re/188 Os ratios. These mineralogical and geochemical features are interpreted in terms of chromite crystallization from melts varying in composition from back-arc basalts (Al-rich chromite) to boninites (Cr-rich chromite) in a suprasubduction zone setting. Chromite crystallization occurs as a consequence of magma mixing and assimilation of preexisting gabbro sills at the mantle–crust transition zone. Cr#, PGE abundances, and bulk Os isotopic composition of chromitites are determined by the combined effects of mantle source heterogeneity, the degree of partial melting, the extent of melt-rock interactions, and the local sulfur fugacity. Small-scale (μm to cm) chemical and isotopic heterogeneities in the platinum-group minerals are controlled by the mechanism(s) of chromite crystallization in a heterogeneous environment created by the turbulent regime generated by successive inputs of different batches of melt. [ABSTRACT FROM AUTHOR]- Published
- 2005
- Full Text
- View/download PDF
43. Diffusion pathways of Fe2+ and Fe3+ during the formation of ferrian chromite: a µXANES study.
- Author
-
Gervilla, F., Asta, M. P., Fanlo, l., Grolimund, D., Ferreira-Sánchez, D., Samson, V. A., Hunziker, D., Colas, V., González-Jiménez, J. M., Kerestedjian, T. N., and Sergeeva, I.
- Subjects
MAGNETITE ,X-ray absorption near edge structure ,CRYSTAL grain boundaries ,SYNCHROTRONS ,CHROMITE - Abstract
The alteration of chromian spinel is a key process during serpentinization and metamorphism of ultramafic rocks controlled by oxygen fugacity (fO
2 ) and Fe2+ ↔ Fe3+ exchange during fluid–rock interaction. Chromian spinel alteration is better recorded in less permeable chromitite than in peridotites where extensive fluid–rock interaction frequently overprints the record of earlier stages of alteration. To shed light on that process we have studied the distribution of Fe2+ and Fe3+ in variably altered chromian spinel grains from a set of chromitite samples from the same mining district using synchrotron-based microscopic chemical imaging and spatially resolved X-ray absorption near edge structure spectroscopy. Our results show that early stages of alteration do not involve changes in Cr3+ and Fe2+ contents or in Fe speciation but only depletion in Al3+ and Mg2+ resulting in the formation of porous chromite. With ongoing alteration Fe3+ migrates into porous chromite mainly along fracture walls and fracture zones as well as along grain boundaries. Sheared-type chromitites record the maximum rates of fluid–rock interaction because in these chromitite-types the accommodation of deformation on porous chromite allowed higher rates of diffusion of Fe3+ and Fe2+ (a magnetite component with Fe3+ /Fetotal = 0.66) into the newly formed neoblasts. In porous chromite-type texture (all the original chromite grains fully transformed to porous chromite) the deformation and accompanying diffusion processes result in the formation of homogenous ferrian chromite grains. In contrast, in partly altered-type texture (chromite grains with original cores surrounded by porous chromite), such processes are only restricted to the porous rims, giving rise to zoned chromian spinel-ferrian chromite grains. [ABSTRACT FROM AUTHOR]- Published
- 2019
- Full Text
- View/download PDF
44. Trace-element fingerprints of chromites link ultramafic massifs of the Bulgarian Rhodopes
- Author
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Colas, V., González-Jiménez, J. M., Fanlo, I., William L Griffin, Gervilla, F., Reilly, Suzanne Y. O., Pearson, N. J., and Kerestedjian, T.
45. Pseudoaneurysm in the radial artery after catheterization | Seudoaneurisma de arteria radial post-canulación
- Author
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Manuel Llácer Pérez, González Jiménez, J. M., and Jiménez Ruiz, A.
46. Neo-Archean domains in the Mediterranean and their implications
- Author
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González-Jiménez, J. M., Villaseca, C., William L Griffin, Elena Belousova, Konc, Z., Ancochea, E., Reilly, Suzanne Y. O., Pearson, N. J., Garrido, C. J., and Gervilla, F.
47. Different scales of Os isotopic heterogeneity in ophiolite chromitites from Sagua de Tanamo and Mayara mining districts (Eastern Cuba)
- Author
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Gervilla, F., Claudio Marchesi, González-Jiménez, J. M., Proenza, J. A., Garrido, C. J., Griffin, William L., and Suzanne Y O'Reilly
48. Chlorpheniramine binding to human serum albumin by fluorescence quenching measurements
- Author
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Gonzalez-Jimenez, J., Frutos, G., Cayre, I., and Cortijo, M.
- Published
- 1991
- Full Text
- View/download PDF
49. Fluorescence quenching studies on binding fluoreno-9-spiro-oxazolidinedione to human serum albumin
- Author
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Gonzalez-Jimenez, J., Jacquotte, H., and Cayre, I.
- Published
- 1992
- Full Text
- View/download PDF
50. Analysis of the binding of chlorpheniramine to human serum albumin by spectroscopic techniques
- Author
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Gonzàlez-Jimènez, J.
- Published
- 1994
- Full Text
- View/download PDF
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