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description Publicationkeyboard_double_arrow_right Article , Other literature type 2019 FrancePublisher:Elsevier BV Authors: Marie-Noelle De Casamajor; Yann Lalanne; Sandrine Derrien-Courtel; J.M. Gorostiaga; +4 AuthorsMarie-Noelle De Casamajor; Yann Lalanne; Sandrine Derrien-Courtel; J.M. Gorostiaga; Aodren Le Gal; Laura Huguenin; Endika Quintano; Muriel Lissardy;Abstract Cystoseira baccata, a biological quality element for the implementation of the Water Framework and Marine Strategy EU Directives, is a dominant species in the subtidal rocky bottoms of the Basque coast. As part of this issue and given the need to better understand the functional character of benthic rocky ecosystems and use them as a reference to anthropogenic changes, two samplings campaigns were conducted in 2014 and 2017. Several population parameters (i.e. frond density, frond length frond-length/total frond-length ratio and taxonomic richness of epibionts) of C. baccata were studied from three sites monitored within the Water Directive Framework in relation to bathymetry during the two campaigns. The results showed a significant influence of bathymetry on frond density, frond length and the epibiotic load, and also an effect of sampling time for the seaweed and epibionts (epiflora and epifauna). The characterization of these functional population parameters for C. baccata under natural conditions are extremely valuable for its application to monitoring programs evaluating the ecological status of coastal waters in this region.
ArchiMer - Instituti... arrow_drop_down ArchiMer - Institutional Archive of IfremerOther literature type . 2019Data sources: ArchiMer - Institutional Archive of IfremerContinental Shelf ResearchArticle . 2019 . Peer-reviewedLicense: Elsevier TDMData sources: Crossrefadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.eu5 citations 5 popularity Top 10% influence Average impulse Average Powered by BIP!more_vert ArchiMer - Instituti... arrow_drop_down ArchiMer - Institutional Archive of IfremerOther literature type . 2019Data sources: ArchiMer - Institutional Archive of IfremerContinental Shelf ResearchArticle . 2019 . Peer-reviewedLicense: Elsevier TDMData sources: Crossrefadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Other literature type , Article 2016 France, Italy, France, France, Italy, Malta, Germany, France, FrancePublisher:American Geophysical Union (AGU) Funded by:EC | SCARP, EC | ASTARTEEC| SCARP ,EC| ASTARTEAuthors: Marc-André Gutscher; Stéphane Dominguez; Bernard Mercier de Lépinay; Luis M. Pinheiro; +7 AuthorsMarc-André Gutscher; Stéphane Dominguez; Bernard Mercier de Lépinay; Luis M. Pinheiro; Flora Gallais; Nathalie Babonneau; Antonio Cattaneo; Yann Le Faou; Giovanni Barreca; Aaron Micallef; Marzia Rovere;doi: 10.1002/2015tc003898
handle: 20.500.11769/497146
Subduction of a narrow slab of oceanic lithosphere beneath a tightly curved orogenic arc requires the presence of at least one lithospheric scale tear fault. While the Calabrian subduction beneath southern Italy is considered to be the type example of this geodynamic setting, the geometry, kinematics and surface expression of the associated lateral, slab tear fault offshore eastern Sicily remain controversial. Results from a new marine geophysical survey conducted in the Ionian Sea, using high-resolution bathymetry and seismic profiling reveal active faulting at the seafloor within a 140 km long, two-branched fault system near Alfeo Seamount. The previously unidentified 60 km long NW trending North Alfeo Fault system shows primarily strike-slip kinematics as indicated by the morphology and steep-dipping transpressional and transtensional faults. Available earthquake focal mechanisms indicate dextral strike-slip motion along this fault segment. The 80 km long SSE trending South Alfeo fault system is expressed by one or two steeply dipping normal faults, bounding the western side of a 500+ m thick, 5 km wide, elongate, syntectonic Plio-Quaternary sedimentary basin. Both branches of the fault system are mechanically capable of generating magnitude 6–7 earthquakes like those that struck eastern Sicily in 1169, 1542, and 1693. International audience
IRIS - Università de... arrow_drop_down ArchiMer - Institutional Archive of IfremerOther literature type . 2016Data sources: ArchiMer - Institutional Archive of IfremerIRIS - Università degli Studi di CataniaArticle . 2016Data sources: IRIS - Università degli Studi di CataniaArchiMer - Institutional Archive of IfremerOther literature type . 2016Data sources: ArchiMer - Institutional Archive of Ifremerhttps://doi.org/10.1002/2015TC...Other literature typeData sources: European Union Open Data Portaladd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.euAccess RoutesGreen bronze 75 citations 75 popularity Top 10% influence Top 10% impulse Top 1% Powered by BIP!visibility 13visibility views 13 download downloads 3 Powered bymore_vert IRIS - Università de... arrow_drop_down ArchiMer - Institutional Archive of IfremerOther literature type . 2016Data sources: ArchiMer - Institutional Archive of IfremerIRIS - Università degli Studi di CataniaArticle . 2016Data sources: IRIS - Università degli Studi di CataniaArchiMer - Institutional Archive of IfremerOther literature type . 2016Data sources: ArchiMer - Institutional Archive of Ifremerhttps://doi.org/10.1002/2015TC...Other literature typeData sources: European Union Open Data Portaladd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://www.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1002/2015tc003898&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Article , Other literature type 2005 Spain, FrancePublisher:Elsevier BV Michaud, François; Chabert, Anne; Collot, Jean-Yves; Sallarès, Valentí; Flueh, Ernst R.; Charvis, Philippe; Graindorge, David; Gustcher, Marc-André; Bialas, Joerg;handle: 10261/201194
Offshore Ecuador, the Carnegie Ridge is a volcanic ridge with a carbonate sediment drape. During the SALIERI Cruise, multibeam bathymetry was collected across Carnegie Ridge with the Simrad EM120 of the R/V SONNE. The most conspicuous features discovered on the Carnegie Ridge are fields of circular closed depressions widely distributed along the mid-slope of the northern and southern flanks of the ridge between 1500 and 2600 m water depth. These circular depressions are 1–4 km wide and typically 100–400 m deep. Most are flat floored and some are so densely packed that they form a honeycomb pattern. The depressions were carved into the ridge sedimentary blanket, which consists of carbonate sediment and has been dated from upper Miocene to upper Pleistocene. Several hypotheses including pockmark origin, sediment creeping, paleo-topography of the volcanic basement, effects of subbottom currents, and both marine and subaerial karstic origins are discussed. We believe that underwater dissolution process merits the most serious consideration regarding the origin of the closed depression 15 pages, 7 figures
add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.euAccess Routesbronze 32 citations 32 popularity Top 10% influence Top 10% impulse Average Powered by BIP!visibility 24visibility views 24 Powered bymore_vert add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Article , Other literature type 2018 Netherlands, United Kingdom, United Kingdom, Netherlands, Netherlands, Spain, France, Portugal, Germany, Spain, United Kingdom, United Kingdom, Switzerland, United Kingdom, Netherlands, United Kingdom, Germany, Spain, United StatesPublisher:Elsevier BV Funded by:NWO | Feasibility of commercial..., NSF | Support for International..., NSF | Support for International... +3 projectsNWO| Feasibility of commercial application of negative stiffness bar balancers ,NSF| Support for International Research Projects and Working Groups Through SCOR ,NSF| Support for International Ocean Science Activities Through the Scientific Committee on Oceanic Research ,NSF| Support for International Ocean Science Activities Through the Scientific Committee on Oceanic Research ,NSF| Support for International Research Projects and Working Groups Through SCOR ,UKRI| RootDetect: Remote Detection and Precision Management of Root HealthReiner Schlitzer; Robert F. Anderson; Elena Masferrer Dodas; Maeve C. Lohan; Walter Geibert; Andrew R. Bowie; Catherine Jeandel; William M. Landing; Cyril Abadie; Wafa Abouchami; Eric P. Achterberg; Morten B. Andersen; Corey Archer; Maureen E. Auro; Oliver Baars; Alex R. Baker; Karel Bakker; Chandranath Basak; Nicholas R. Bates; Dorothea Bauch; Pieter van Beek; Erin E. Black; Katrin Bluhm; Laurent Bopp; Heather A. Bouman; Philip W. Boyd; Marie Boye; Edward A. Boyle; Pierre Branellec; Luke Bridgestock; Guillaume Brissebrat; Thomas J. Browning; Hans-Jürgen Brumsack; Mark A. Brzezinski; Clifton S. Buck; Kristen N. Buck; Abby Bull; Pinghe Cai; Damien Cardinal; Craig A. Carlson; Gonzalo Carrasco; Núria Casacuberta; Karen L. Casciotti; Maxi Castrillejo; Rosie Chance; Matthew A. Charette; Hai Cheng; Marcus Christl; Thomas M. Church; Ivia Closset; Peter Croot; Jay T. Cullen; Chris J. Daniels; Feifei Deng; Brian Duggan; Gabriel Dulaquais; Cynthia Dumousseaud; Yolanda Echegoyen-Sanz; Michael J. Ellwood; Jessica N. Fitzsimmons; A. Russell Flegal; Martin Q. Fleisher; Tina van de Flierdt; Martin Frank; Jana Friedrich; François Fripiat; Henning Fröllje; Stephen J.G. Galer; Toshitaka Gamo; Raja S. Ganeshram; Jordi Garcia-Orellana; Ester Garcia-Solsona; Melanie Gault-Ringold; Loes J. A. Gerringa; Melissa Gilbert; José Marcus Godoy; Steven L. Goldstein; Santiago R. Gonzalez; Karen Grissom; Chad R. Hammerschmidt; Alison E. Hartman; Christel S. Hassler; Ed C Hathorne; Mariko Hatta; Nicholas J. Hawco; Lars-Eric Heimbürger; Josh Helgoe; Gideon M. Henderson; Paul B. Henderson; Peng Ho; Tristan J. Horner; Yu-Te Hsieh; Kuo-Fang Huang; Matthew P. Humphreys; Jeremy E. Jacquot; David J. Janssen; Janice L. Jones; Lauren Kipp; J. K. Klar; Sven Kretschmer; Yuichiro Kumamoto; Patrick Laan; François Lacan; Phoebe J. Lam; Myriam Lambelet; Carl H. Lamborg; Emilie Le Roy; Jong-Mi Lee; Pascale Lherminier; Susan H. Little; Mercedes López-Lora; Pere Masqué; Edward Mawji; Charles R. McClain; Christopher I. Measures; Sanjin Mehic; Pier van der Merwe; Rob Middag; Sebastian Mieruch; Angela Milne; Tomoharu Minami; James W. Moffett; Gwenaelle Moncoiffe; Willard S. Moore; Paul J. Morris; Peter L. Morton; John Niedermiller; Jun Nishioka; Akira Nishiuchi; Abigail E. Noble; Sven Ober; Daniel C. Ohnemus; Jan van Ooijen; Stephanie Owens; Katharina Pahnke; Maxence Paul; Leopoldo D. Pena; Brian Peters; Frédéric Planchon; Hélène Planquette; Viena Puigcorbé; Paul D. Quay; Sara Rauschenberg; Mark Rehkämper; Tomas A. Remenyi; Joseph A. Resing; Joerg Rickli; Sylvain Rigaud; Montserrat Roca-Martí; Valentí Rodellas; Saeed Roshan; Evgenia Ryabenko; Mak A. Saito; Lesley Salt; Virginie Sanial; Géraldine Sarthou; Christina Schallenberg; Ursula Schauer; Christian Schlosser; Bernhard Schnetger; Peter N. Sedwick; Igor Semiletov; Rachel U. Shelley; Robert M. Sherrell; Alan M. Shiller; Daniel M. Sigman; Sunil K. Singh; Hans A. Slagter; Emma Slater; William M. Smethie; Helen M. Snaith; Yoshiki Sohrin; Bettina Sohst; Jeroen E. Sonke; Sabrina Speich; Reiner Steinfeldt; Gillian Stewart; Torben Stichel; Claudine H. Stirling; Johnny Stutsman; Alexander L. Thomas; Kay Thorne; Claire P. Till; Ralph Till; Ashley T. Townsend; Robyn E. Tuerena; Benjamin S. Twining; Celia Venchiarutti; María Villa-Alfageme; Sebastian M. Vivancos; Bronwyn Wake; Ros Watson; Evaline M. van Weerlee; Yishai Weinstein; E. Malcolm S. Woodward; Jingfeng Wu; Yingzhe Wu; Kathrin Wuttig; Neil J. Wyatt; Yang Xiang; Zichen Xue; Jing Zhang; Pu Zhang; Ye Zhao; Linjie Zheng; Xin Yuan Zheng; Louise A. Zimmer; Patrizia Ziveri; Patricia Zunino;The GEOTRACES Intermediate Data Product 2017 (IDP2017) is the second publicly available data product of the international GEOTRACES programme, and contains data measured and quality controlled before the end of 2016. The IDP2017 includes data from the Atlantic, Pacific, Arctic, Southern and Indian oceans, with about twice the data volume of the previous IDP2014. For the first time, the IDP2017 contains data for a large suite of biogeochemical parameters as well as aerosol and rain data characterising atmospheric trace element and isotope (TEI) sources. The TEI data in the IDP2017 are quality controlled by careful assessment of intercalibration results and multi-laboratory data comparisons at crossover stations. The IDP2017 consists of two parts: (1) a compilation of digital data for more than 450 TEIs as well as standard hydrographic parameters, and (2) the eGEOTRACES Electronic Atlas providing an on-line atlas that includes more than 590 section plots and 130 animated 3D scenes. The digital data are provided in several formats, including ASCII, Excel spreadsheet, netCDF, and Ocean Data View collection. Users can download the full data packages or make their own custom selections with a new on-line data extraction service. In addition to the actual data values, the IDP2017 also contains data quality flags and 1-σ data error values where available. Quality flags and error values are useful for data filtering and for statistical analysis. Metadata about data originators, analytical methods and original publications related to the data are linked in an easily accessible way. The eGEOTRACES Electronic Atlas is the visual representation of the IDP2017 as section plots and rotating 3D scenes. The basin-wide 3D scenes combine data from many cruises and provide quick overviews of large-scale tracer distributions. These 3D scenes provide geographical and bathymetric context that is crucial for the interpretation and assessment of tracer plumes near ocean margins or along ridges. The IDP2017 is the result of a truly international effort involving 326 researchers from 25 countries. This publication provides the critical reference for unpublished data, as well as for studies that make use of a large cross-section of data from the IDP2017. This article is part of a special issue entitled: Conway GEOTRACES - edited by Tim M. Conway, Tristan Horner, Yves Plancherel, and Aridane G. González. National Science Foundation (U.S.) (Grant OCE-1243377) National Science Foundation (U.S.) (Grant OCE-1546580) National Science Foundation (U.S.) (Grant OCE-0608600) National Science Foundation (U.S.) (Grant OCE0938349)
CORE (RIOXX-UK Aggre... arrow_drop_down CORE (RIOXX-UK Aggregator)Article . 2018License: CC BY NC NDData sources: CORE (RIOXX-UK Aggregator)Chemical GeologyArticle . 2018Full-Text: http://repository.kulib.kyoto-u.ac.jp/dspace/bitstream/2433/233927/1/j.chemgeo.2018.05.040.pdfData sources: JAIRONARCIS; Chemical GeologyArticle . 2018Diposit Digital de la Universitat de Barcelona; Recolector de Ciencia Abierta, RECOLECTAArticle . 2019 . 2018License: CC BYUniversity of East Anglia digital repositoryArticle . 2018 . Peer-reviewedData sources: University of East Anglia digital repositorySapientia Repositório da Universidade do AlgarveArticle . 2020Data sources: Sapientia Repositório da Universidade do AlgarveRecolector de Ciencia Abierta, RECOLECTA; DIGITAL.CSICArticle . 2018 . 2019 . Peer-reviewedSpiral - Imperial College Digital RepositoryArticle . 2018Data sources: Spiral - Imperial College Digital RepositoryElectronic Publication Information CenterArticle . 2018Data sources: Electronic Publication Information CenterOxford University Research ArchiveArticle . 2018License: CC BYData sources: Oxford University Research ArchiveArchiMer - Institutional Archive of IfremerOther literature type . 2018Data sources: ArchiMer - Institutional Archive of IfremerRecolector de Ciencia Abierta, RECOLECTA; Dipòsit Digital de Documents de la UABArticle . 2018License: CC BYHAL AMU; Mémoires en Sciences de l'Information et de la Communication; HAL-CEA; HAL-IRDArticle . 2018License: CC BYArchiMer - Institutional Archive of IfremerOther literature type . 2018Data sources: ArchiMer - Institutional Archive of Ifremeradd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.euAccess RoutesGreen hybrid 251 citations 251 popularity Top 1% influence Top 10% impulse Top 0.1% Powered by BIP!visibility 288visibility views 288 download downloads 749 Powered bymore_vert CORE (RIOXX-UK Aggre... arrow_drop_down CORE (RIOXX-UK Aggregator)Article . 2018License: CC BY NC NDData sources: CORE (RIOXX-UK Aggregator)Chemical GeologyArticle . 2018Full-Text: http://repository.kulib.kyoto-u.ac.jp/dspace/bitstream/2433/233927/1/j.chemgeo.2018.05.040.pdfData sources: JAIRONARCIS; Chemical GeologyArticle . 2018Diposit Digital de la Universitat de Barcelona; Recolector de Ciencia Abierta, RECOLECTAArticle . 2019 . 2018License: CC BYUniversity of East Anglia digital repositoryArticle . 2018 . Peer-reviewedData sources: University of East Anglia digital repositorySapientia Repositório da Universidade do AlgarveArticle . 2020Data sources: Sapientia Repositório da Universidade do AlgarveRecolector de Ciencia Abierta, RECOLECTA; DIGITAL.CSICArticle . 2018 . 2019 . Peer-reviewedSpiral - Imperial College Digital RepositoryArticle . 2018Data sources: Spiral - Imperial College Digital RepositoryElectronic Publication Information CenterArticle . 2018Data sources: Electronic Publication Information CenterOxford University Research ArchiveArticle . 2018License: CC BYData sources: Oxford University Research ArchiveArchiMer - Institutional Archive of IfremerOther literature type . 2018Data sources: ArchiMer - Institutional Archive of IfremerRecolector de Ciencia Abierta, RECOLECTA; Dipòsit Digital de Documents de la UABArticle . 2018License: CC BYHAL AMU; Mémoires en Sciences de l'Information et de la Communication; HAL-CEA; HAL-IRDArticle . 2018License: CC BYArchiMer - Institutional Archive of IfremerOther literature type . 2018Data sources: ArchiMer - Institutional Archive of Ifremeradd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Article 2004 SpainPublisher:Editorial CSIC D´Onghia, Gianfranco; Lloris, Domingo; Sion, Letizia; Politou, Chrissi-Yianna; Dokos, John;handle: 10261/5789
[ES] Se recolectaron especies de peces en el mar Balear y en el Iónico oriental y occidental, gracias a una investigación subvencionada por la CE en aguas profundas del Mediterráneo (600-4000 m). Caelorhynchus mediterraneus es una nueva cita para el mar Balear, Cyclothone braueri, Hygophum benoiti, Paralepis speciosa, Chalinura mediterranea, Coryphaenoides guentheri, C. mediterraneus, Lepidion lepidion y Cataetyx laticeps lo son para el mar Iónico occidental, Polyacanthonotus rissoanus, C. guentheri, C. mediterraneus, L. lepidion y C. laticeps para el mar Iónico oriental. También se ha puesto al día la distribución batimétrica de otras especies. En las tres áreas muestreadas se ha observado que la riqueza específica desciende con la profundidad, marcándose un cambio significativo por debajo de los 1500 m. A profundidades superiores a 1000 m las especies de macrúridos y móridos fueron dominantes excepto para el mar Balear donde Alepocephalus rostratus fue la especie más abundante hasta 1500 m. A profundidades superiores a los 1500 m las especies dominantes fueron Bathypterois mediterraneus, C. mediterranea y C. guentheri. Los resultados confirman la escasez de ictiofauna profunda en el Mediterráneo comparada con la del Atlántico. Hasta las máximas profundidades muestradas, la diferencia faunística entre el Mediterráneo occidental y oriental parece ser debida, más al menor número de investigaciones llevados a cabo en el Mediterráneo oriental, que no a unas determinadas pautas en la distribución y abundancia dicha ictiofauna [EN] During an EC-funded research carried out in the Mediterranean Sea deep-water fish (600-4000 m) were collected in the Balearic Sea as well as the western and eastern Ionian Sea. Caelorhynchusmediterraneus is a new record for the Balearic Sea, Cyclothone braueri, Hygophum benoiti, Paralepis speciosa, Chalinura mediterranea, Coryphaenoides guentheri, C. mediterraneus, Lepidion lepidion and Cataetyx laticeps for the western Ionian Sea, and Polyacanthonotus rissoanus, C. guentheri, C. mediterraneus, L. lepidion and C. laticeps for the eastern Ionian Sea. The bathymetric distribution of other species has been updated. Species richness decreased with depth in the three surveyed areas, showing a significant shift below 1500 m. At depths greater than 1000 m macrourid and morid species were dominant except in the Balearic Sea, where Alepocephalus rostratus was found to be very abundant as deep as 1500 m. At depths greater than 1500 m the dominant species were Bathypterois mediterraneus, C. mediterranea and C. guentheri. The results of this research confirm the scarcity of deep fish fauna in the Mediterranean compared to the Atlantic. For the greatest depths are concerned, the faunistic difference between the western and eastern Mediterranean seems to be most probably due to a lesser number of investigations on the eastern side rather than any real paucity of ichthyofauna This work was supported by the Directorate General of Fisheries of the European Commission as part of the project DESEAS (Exploratory survey to collect data of the exploited and virgin stocks of deep-sea shrimp A. antennatus, of interest to the CFP - Study contract nº 2000/39, DGXIV). The authors wish to thank V. Catalano for providing helpful literature Peer reviewed
Scientia Marina arrow_drop_down Recolector de Ciencia Abierta, RECOLECTAArticle . 2004 . Peer-reviewedLicense: CC BYData sources: Recolector de Ciencia Abierta, RECOLECTARecolector de Ciencia Abierta, RECOLECTA; DIGITAL.CSICArticle . 2008 . 2004 . Peer-reviewedadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.euAccess Routesgold 25 citations 25 popularity Average influence Top 10% impulse Average Powered by BIP!visibility 19visibility views 19 download downloads 40 Powered bymore_vert Scientia Marina arrow_drop_down Recolector de Ciencia Abierta, RECOLECTAArticle . 2004 . Peer-reviewedLicense: CC BYData sources: Recolector de Ciencia Abierta, RECOLECTARecolector de Ciencia Abierta, RECOLECTA; DIGITAL.CSICArticle . 2008 . 2004 . Peer-reviewedadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Article 2012 SpainPublisher:Springer Science and Business Media LLC Authors: León Buendía, Ricardo F.; Somoza, Luis; Medialdea Cela, Teresa; Vázquez, Juan Tomás; +7 AuthorsLeón Buendía, Ricardo F.; Somoza, Luis; Medialdea Cela, Teresa; Vázquez, Juan Tomás; González Sanz, Francisco Javier; López-González, Nieves; Casas, David; Mata Campo, Maria Pilar; Fernández Puga, María del Carmen; Giménez-Moreno, Julia; Díaz del Río, Victor;handle: 10508/8416 , 10261/276844
During the MVSEIS-08 cruise of 2008, ten new mud volcanoes (MVs) were discovered on the offshore Moroccan continental margin (Gulf of Cádiz) at water depths between 750 and 1,600 m, using multibeam bathymetry, backscatter imagery, high-resolution seismic and gravity core data. Mud breccias were recovered in all cases, attesting to the nature of extrusion of these cones. The mud volcanoes are located in two fields: the MVSEIS, Moundforce, Pixie, Las Negras, Madrid, Guadix, Almanzor and El Cid MVs in the western Moroccan field, where mud volcanoes have long been suspected but to date not identified, and the Boabdil and Al Gacel MVs in the middle Moroccan field. Three main morphologies were observed: asymmetric, sub-circular and flat-topped cone-shaped types, this being the first report of asymmetric morphologies in the Gulf of Cádiz. Based on morpho-structural analysis, the features are interpreted to result from (1) repeated constructive (expulsion of fluid mud mixtures) and destructive (gravity-induced collapse and submarine landsliding) episodes and (2) interaction with bottom currents 10th International Conference on Gas in Marine Sediments, 6-11 September 2010, Listvyanka, Russia División de Geología Marina, Instituto Geológico y Minero de España, España Facultad de Ciencias Geológicas, Universidad Complutense de Madrid, España Centro Oceanográfico de Málaga, Instituto Español de Oceanografía, España Facultad de Ciencias del Mar, Universidad de Cádiz, España
Recolector de Cienci... arrow_drop_down Recolector de Ciencia Abierta, RECOLECTAArticle . 2012Data sources: Recolector de Ciencia Abierta, RECOLECTARecolector de Ciencia Abierta, RECOLECTA; DIGITAL.CSICArticle . 2012 . 2022Recolector de Ciencia Abierta, RECOLECTAArticle . 2012License: CC BY NC NDData sources: Recolector de Ciencia Abierta, RECOLECTARepositorio Institucional Digital del IEOArticle . 2012License: CC BY NC NDData sources: Repositorio Institucional Digital del IEOadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.euAccess RoutesGreen 43 citations 43 popularity Top 10% influence Average impulse Top 10% Powered by BIP!visibility 18visibility views 18 download downloads 66 Powered bymore_vert Recolector de Cienci... arrow_drop_down Recolector de Ciencia Abierta, RECOLECTAArticle . 2012Data sources: Recolector de Ciencia Abierta, RECOLECTARecolector de Ciencia Abierta, RECOLECTA; DIGITAL.CSICArticle . 2012 . 2022Recolector de Ciencia Abierta, RECOLECTAArticle . 2012License: CC BY NC NDData sources: Recolector de Ciencia Abierta, RECOLECTARepositorio Institucional Digital del IEOArticle . 2012License: CC BY NC NDData sources: Repositorio Institucional Digital del IEOadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Article 2017 United Kingdom, Norway, United Kingdom, IcelandPublisher:Springer Science and Business Media LLC Funded by:EC | Blue-Action, EC | NACLIM, EC | ATLASEC| Blue-Action ,EC| NACLIM ,EC| ATLASHátún, H.; Azetsu-Scott, K.; Somavilla, R.; Rey, F.; Johnson, C.; Mathis, M.; Mikolajewicz, U.; Coupel, P.; Tremblay, J.-É.; Hartman, S.; Pacariz, S. V.; Salter, I.; Ólafsson, J.;The North Atlantic is characterized by diatom-dominated spring blooms that results in significant transfer of carbon to higher trophic levels and the deep ocean. These blooms are terminated by limiting silicate concentrations in summer. Numerous regional studies have demonstrated phytoplankton community shifts to lightly-silicified diatoms and non-silicifying plankton at the onset of silicate limitation. However, to understand basin-scale patterns in ecosystem and climate dynamics, nutrient inventories must be examined over sufficient temporal and spatial scales. Here we show, from a new comprehensive compilation of data from the subpolar Atlantic Ocean, clear evidence of a marked pre-bloom silicate decline of 1.5-2 mu M throughout the winter mixed layer during the last 25 years. This silicate decrease is primarily attributed to natural multi-decadal variability through decreased winter convection depths since the mid-1990s, a weakening and retraction of the subpolar gyre and an associated increased influence of nutrient-poor water of subtropical origin. Reduced Arctic silicate import and the projected hemispheric-scale climate change-induced weakening of vertical mixing may have acted to amplify the recent decline. These marked fluctuations in pre-bloom silicate inventories will likely have important consequences for the spatial and temporal extent of diatom blooms, thus impacting ecosystem productivity and ocean-atmosphere climate dynamics. This work was initiated through the Nordic Council of Ministers project (AEG-11323). H.H. is supported by the European Union 7th Framework Programme (n. 308299 NACLIM www.naclim.eu), the EU Horizon 2020 Blue-Action project (BG-10-2016, www.blue-action.eu) and the Danish project NAACOS 10-093903/DSF. R.S. is supported by a Marie Curie Clarin Cofund Grant (ACB-1431). S.P. was funded by the Danish government through the research center 'Climate and oceanographic changes in the marine area between Greenland and Faroes - Influences on plankton and fish'. C.J. was funded under the European Union's Horizon 2020 research and innovation under grant agreement No. 678760 (ATLAS). This output reflects only the author's view and the European Union cannot be held responsible for any use that may be made of the information contained therein. Funding information on the model simulations and the observation programs is given in the Supplementary Information 1. The model simulations were supported by the co-operative project "RACE - Regional Atlantic Circulation and Global Change" funded by the German Federal Ministry for Education and Research (BMBF). We thank Solva Jacobsen for providing the Faroe Shelf silicate record. Peer Reviewed
e-Prints Soton arrow_drop_down Europe PubMed CentralArticle . 2017Full-Text: http://europepmc.org/articles/PMC5674075Data sources: PubMed CentralZENODO; Scientific Reports; NERC Open Research ArchiveOther literature type . Article . 2017 . Peer-reviewedLicense: CC BYadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.euAccess RoutesGreen gold 76 citations 76 popularity Top 1% influence Top 10% impulse Top 10% Powered by BIP!visibility 114visibility views 114 download downloads 93 Powered bymore_vert e-Prints Soton arrow_drop_down Europe PubMed CentralArticle . 2017Full-Text: http://europepmc.org/articles/PMC5674075Data sources: PubMed CentralZENODO; Scientific Reports; NERC Open Research ArchiveOther literature type . Article . 2017 . Peer-reviewedLicense: CC BYadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Article 2014 Norway, Spain, United KingdomPublisher:Editorial CSIC Mechó, Ariadna; Billett, David S.M.; Ramírez-Llodra, Eva; Aguzzi, Jacopo; Tyler, P.A.; Company, Joan B.;handle: 11250/227091 , 10261/99973
[ES] Este estudio presenta una recopilación de toda la información disponible sobre los equinodermos de profundidad en el talud continental medio e inferior del mar Mediterráneo, con el fin de proporcionar una fuente de información unificada sobre la taxonomía de este grupo. Se han actualizado los registros anteriores mediante nuevos datos provenientes de 223 pescas de arrastre de 11 campañas oceanográficas realizadas en el noroeste Mediterráneo entre 800 y 2845 m de profundidad. Se ha actualizado el nombre de las especies, sus rangos batimétricos y sus distribuciones geográficas. Los nuevos datos presentan, por primera vez, la presencia del equinoideo Atlántico Gracilechinus elegans (Düben and Koren, 1844) en el mar Mediterráneo. También se cita la presencia en el noroeste Mediterráneo de dos especies de holoturias endémicas del Mediterráneo, Hedingia mediterranea (Bartolini Baldelli, 1914), muestreada una única vez en 1914 en el mar Tirreno, y Penilpidia ludwigi (von Marenzeller, 1893), muestreada tres veces, dos en el mar Egeo y una en el mar Balear. Además se expanden los límites de distribución batimétrica para cuatro especies: el asteroideo Ceramaster grenadensis (Perrier, 1881) hasta 2845 m; el equinoideo Brissopsis lyrifera (Forbes, 1841) hasta los 2250 m; y las holoturias Hedingia mediterranea y Holothuria (Panningothuria) forskali Delle Chiaje, 1823, hasta los 1500 m y 850 m respectivamente [EN] This study provides a compilation of all available information on deep-sea echinoderms from the middle and lower slopes of the Mediterranean Sea, with the aim of providing a unified source of information on the taxonomy of this group. Previous records of species are updated with new data obtained from 223 trawl hauls conducted in 11 cruises within the northwestern Mediterranean Sea between 800 m and 2845 m depth. Valid names, bathymetric ranges and geographic distributions are given for all species. The new data report, for the first time, the presence of the Atlantic echinoid Gracilechinus elegans (Düben and Koren, 1844) in the Mediterranean Sea. We also report the presence of the endemic holothurians Hedingia mediterranea (Bartolini Baldelli, 1914), dredged only once previously in 1914 in the Tyrrhenian Sea, and Penilpidia ludwigi (von Marenzeller, 1893), known previously only from three samples, two in the Aegean Sea and one in the Balearic Sea. Additionally, the deeper limits of the bathymetric distribution of four species have been expanded: the asteroid Ceramaster grenadensis (Perrier, 1881) to 2845 m; the echinoid Brissopsis lyrifera (Forbes, 1841) to 2250 m; and the holothurians Hedingia mediterranea and Holothuria (Panningothuria) forskali Delle Chiaje, 1823, to 1500 m and 850 m, respectively This study was funded by the PROMETEO project (CTM2007-66316-C02/MAR, CICYT), the BIOFUN project (CTM2007-28739-E, European Science Foundation and national funding agencies) and the DOSMARES project (CTM2010-21810-C03-03). ERLL was funded by a JAE-DOC postdoctoral grant (CSIC, Spain) with co-funding from the European Social Fund. JA is a fellow of the Ramón y Cajal Programme (MICINN) 22 pages, 13 figures, 3 tables Peer reviewed
NIVA Open Access Arc... arrow_drop_down Scientia MarinaArticle . 2014 . Peer-reviewedLicense: CC BYNERC Open Research ArchiveArticle . 2014 . Peer-reviewedFull-Text: http://nora.nerc.ac.uk/508010/1/Mecho%20et%20al.%20final%20manuscript%20as%20submitted.pdfData sources: NERC Open Research ArchiveRecolector de Ciencia Abierta, RECOLECTAArticle . 2014 . Peer-reviewedLicense: CC BYData sources: Recolector de Ciencia Abierta, RECOLECTARecolector de Ciencia Abierta, RECOLECTA; DIGITAL.CSICArticle . 2014 . Peer-reviewedadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.euAccess RoutesGreen gold 23 citations 23 popularity Top 10% influence Average impulse Top 10% Powered by BIP!visibility 26visibility views 26 download downloads 162 Powered bymore_vert NIVA Open Access Arc... arrow_drop_down Scientia MarinaArticle . 2014 . Peer-reviewedLicense: CC BYNERC Open Research ArchiveArticle . 2014 . Peer-reviewedFull-Text: http://nora.nerc.ac.uk/508010/1/Mecho%20et%20al.%20final%20manuscript%20as%20submitted.pdfData sources: NERC Open Research ArchiveRecolector de Ciencia Abierta, RECOLECTAArticle . 2014 . Peer-reviewedLicense: CC BYData sources: Recolector de Ciencia Abierta, RECOLECTARecolector de Ciencia Abierta, RECOLECTA; DIGITAL.CSICArticle . 2014 . Peer-reviewedadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Article 2009 SpainPublisher:Elsevier BV Authors: Fernández Salas, Luis Miguel; Dabrio, Cristino J.; Goy Goy, José Luis; Díaz del Río, Víctor; +4 AuthorsFernández Salas, Luis Miguel; Dabrio, Cristino J.; Goy Goy, José Luis; Díaz del Río, Víctor; Zazo Cardeña , Caridad; Lobo Sánchez, Francisco José; Sanz Alonso, José Luis; Lario, Javier;handle: 10261/247560 , 10508/7758 , 10261/318956 , 20.500.14352/41786
The well-exposed systems of prograding beach ridges on the Carchuna-Calahonda (Granada) and Campo de Dalías-Roquetas (Almería) coastal plains continue offshore as infralittoral prograding wedges (IPW). The Holocene IPW is a narrow morpho-sedimentary unit up to 2.5 km wide which develops seaward from the lower edge of the shoreface to 15-20 m depth, extending to a well-defined break of slope at water depths of 35-40 m. These IPWs have been recognized and studied using very high-resolution seismic profiles (TOPAS) and multibeam data (EM-3000D). In detail they are complex morpho-sedimentary units in which internal structures are closely linked to the pattern of progradation of the adjacent coastal plains. When longshore currents produce significant littoral drift, the IPWs are composed of several minor units arranged in offlap, which accrete parallel or oblique to the main shoreline. Therefore, it is possible to correlate progradational units in the coastal plain (H-units, sensu[Goy, J.L., Zazo, C., Dabrio, C.J., 2003. A beach-ridge progradation complex reflecting periodical sea-level and climate variability during the Holocene (Gulf of Almería, Western Mediterranean). Geomorphology 50, 251-268]) and subunits in the IPW, but special care is required depending on the local arrangement of morpho-sedimentary units. Besides, it is not realistic to draw conclusions regarding the age of the subunits inside a given IPW without adequate dating, as the number of subunits will greatly vary from place to place depending on local factors, magnitude of sea-level oscillations, and sediment supply. The geophysical information of marine areas was provided by research project: “Estudio Geológico de la Plataforma Continental Española”, funded by “Secretaría General de Pesca Maritima, Ministerio de Agricultura, Pesca y Alimentación”. Research on land was funded by Projects CGL 2005-01336/BTE and CGL 2005-04655/BTE. This is a contribution to IGCP projects 464 (Continental shelves during the last glacial cycles: knowledge and applications) and 495 (Quaternary land–ocean interactions: driving mechanisms and coastal responses), and to Work Group UCM: “Paleoclimatology and Global Change (910198)”.
E-Prints Complutense arrow_drop_down Recolector de Ciencia Abierta, RECOLECTA; Docta ComplutenseArticle . 2023 . 2009Recolector de Ciencia Abierta, RECOLECTA; DIGITAL.CSICArticle . 2021 . 2009Recolector de Ciencia Abierta, RECOLECTAArticle . 2009 . Peer-reviewedData sources: Recolector de Ciencia Abierta, RECOLECTARepositorio Institucional Digital del IEOArticle . 2009License: CC BY NC NDData sources: Repositorio Institucional Digital del IEOadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.euAccess RoutesGreen bronze 40 citations 40 popularity Top 10% influence Top 10% impulse Top 10% Powered by BIP!visibility 17visibility views 17 download downloads 21 Powered bymore_vert E-Prints Complutense arrow_drop_down Recolector de Ciencia Abierta, RECOLECTA; Docta ComplutenseArticle . 2023 . 2009Recolector de Ciencia Abierta, RECOLECTA; DIGITAL.CSICArticle . 2021 . 2009Recolector de Ciencia Abierta, RECOLECTAArticle . 2009 . Peer-reviewedData sources: Recolector de Ciencia Abierta, RECOLECTARepositorio Institucional Digital del IEOArticle . 2009License: CC BY NC NDData sources: Repositorio Institucional Digital del IEOadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Article 2006Publisher:American Geophysical Union (AGU) Publicly fundedTrevor William; Akihiro Kano; Timothy G. Ferdelman; Jean-Pierre Henriet; Kohei Abe; Miriam S. Andres; Morten Bjerager; Emily L Browning; Barry Andrew Cragg; Ben De Mol; Boris Dorschel; Anneleen Foubert; Tracy D. Frank; Yuji Fuwa; Philippe Gaillot; Jamshid J. Gharib; Jay M. Gregg; Veerle A.I. Huvenne; Philippe Léonide; Xianghui Li; Kai Mangelsdorf; Akiko Tanaka; Xavier Monteys; Ivana Novosel; Saburo Sakai; Vladimir A. Samarkin; Keiichi Sasaki; Arthur J. Spivack; Chizuru Takashima; Jürgen Titschak;doi: 10.1029/2006eo470001
The discovery of mounds and reefs hosting cold‐water coral ecosystems along the northeastern Atlantic continental margins has propelled a vigorous effort over the past decade to study the distribution of the mounds, surface sediments, the ecosystems they host, and their environments [Hovland et al., 1994; Freiwald and Roberts, 2005].This effort has involved swath bathymetry, remotely operated vehicle deployments, shallow coring, and seismic surveys.Global coverage is difficult to gauge, but studies indicate that cold‐water corals may cover as large an area as the better known warm‐water corals that form shallow reefs (284,300 square kilometers) [Freiwald et al., 2005]. Cold‐water corals occur in a variety of forms and settings, from small isolated colonies or patch reefs to giant mound structures such as those found west of Ireland.
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For further information contact us at helpdesk@openaire.euAccess Routesbronze 37 citations 37 popularity Average influence Top 10% impulse Top 10% Powered by BIP!more_vert add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
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description Publicationkeyboard_double_arrow_right Article , Other literature type 2019 FrancePublisher:Elsevier BV Authors: Marie-Noelle De Casamajor; Yann Lalanne; Sandrine Derrien-Courtel; J.M. Gorostiaga; +4 AuthorsMarie-Noelle De Casamajor; Yann Lalanne; Sandrine Derrien-Courtel; J.M. Gorostiaga; Aodren Le Gal; Laura Huguenin; Endika Quintano; Muriel Lissardy;Abstract Cystoseira baccata, a biological quality element for the implementation of the Water Framework and Marine Strategy EU Directives, is a dominant species in the subtidal rocky bottoms of the Basque coast. As part of this issue and given the need to better understand the functional character of benthic rocky ecosystems and use them as a reference to anthropogenic changes, two samplings campaigns were conducted in 2014 and 2017. Several population parameters (i.e. frond density, frond length frond-length/total frond-length ratio and taxonomic richness of epibionts) of C. baccata were studied from three sites monitored within the Water Directive Framework in relation to bathymetry during the two campaigns. The results showed a significant influence of bathymetry on frond density, frond length and the epibiotic load, and also an effect of sampling time for the seaweed and epibionts (epiflora and epifauna). The characterization of these functional population parameters for C. baccata under natural conditions are extremely valuable for its application to monitoring programs evaluating the ecological status of coastal waters in this region.
ArchiMer - Instituti... arrow_drop_down ArchiMer - Institutional Archive of IfremerOther literature type . 2019Data sources: ArchiMer - Institutional Archive of IfremerContinental Shelf ResearchArticle . 2019 . Peer-reviewedLicense: Elsevier TDMData sources: Crossrefadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.eu5 citations 5 popularity Top 10% influence Average impulse Average Powered by BIP!more_vert ArchiMer - Instituti... arrow_drop_down ArchiMer - Institutional Archive of IfremerOther literature type . 2019Data sources: ArchiMer - Institutional Archive of IfremerContinental Shelf ResearchArticle . 2019 . Peer-reviewedLicense: Elsevier TDMData sources: Crossrefadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Other literature type , Article 2016 France, Italy, France, France, Italy, Malta, Germany, France, FrancePublisher:American Geophysical Union (AGU) Funded by:EC | SCARP, EC | ASTARTEEC| SCARP ,EC| ASTARTEAuthors: Marc-André Gutscher; Stéphane Dominguez; Bernard Mercier de Lépinay; Luis M. Pinheiro; +7 AuthorsMarc-André Gutscher; Stéphane Dominguez; Bernard Mercier de Lépinay; Luis M. Pinheiro; Flora Gallais; Nathalie Babonneau; Antonio Cattaneo; Yann Le Faou; Giovanni Barreca; Aaron Micallef; Marzia Rovere;doi: 10.1002/2015tc003898
handle: 20.500.11769/497146
Subduction of a narrow slab of oceanic lithosphere beneath a tightly curved orogenic arc requires the presence of at least one lithospheric scale tear fault. While the Calabrian subduction beneath southern Italy is considered to be the type example of this geodynamic setting, the geometry, kinematics and surface expression of the associated lateral, slab tear fault offshore eastern Sicily remain controversial. Results from a new marine geophysical survey conducted in the Ionian Sea, using high-resolution bathymetry and seismic profiling reveal active faulting at the seafloor within a 140 km long, two-branched fault system near Alfeo Seamount. The previously unidentified 60 km long NW trending North Alfeo Fault system shows primarily strike-slip kinematics as indicated by the morphology and steep-dipping transpressional and transtensional faults. Available earthquake focal mechanisms indicate dextral strike-slip motion along this fault segment. The 80 km long SSE trending South Alfeo fault system is expressed by one or two steeply dipping normal faults, bounding the western side of a 500+ m thick, 5 km wide, elongate, syntectonic Plio-Quaternary sedimentary basin. Both branches of the fault system are mechanically capable of generating magnitude 6–7 earthquakes like those that struck eastern Sicily in 1169, 1542, and 1693. International audience
IRIS - Università de... arrow_drop_down ArchiMer - Institutional Archive of IfremerOther literature type . 2016Data sources: ArchiMer - Institutional Archive of IfremerIRIS - Università degli Studi di CataniaArticle . 2016Data sources: IRIS - Università degli Studi di CataniaArchiMer - Institutional Archive of IfremerOther literature type . 2016Data sources: ArchiMer - Institutional Archive of Ifremerhttps://doi.org/10.1002/2015TC...Other literature typeData sources: European Union Open Data Portaladd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.euAccess RoutesGreen bronze 75 citations 75 popularity Top 10% influence Top 10% impulse Top 1% Powered by BIP!visibility 13visibility views 13 download downloads 3 Powered bymore_vert IRIS - Università de... arrow_drop_down ArchiMer - Institutional Archive of IfremerOther literature type . 2016Data sources: ArchiMer - Institutional Archive of IfremerIRIS - Università degli Studi di CataniaArticle . 2016Data sources: IRIS - Università degli Studi di CataniaArchiMer - Institutional Archive of IfremerOther literature type . 2016Data sources: ArchiMer - Institutional Archive of Ifremerhttps://doi.org/10.1002/2015TC...Other literature typeData sources: European Union Open Data Portaladd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Article , Other literature type 2005 Spain, FrancePublisher:Elsevier BV Michaud, François; Chabert, Anne; Collot, Jean-Yves; Sallarès, Valentí; Flueh, Ernst R.; Charvis, Philippe; Graindorge, David; Gustcher, Marc-André; Bialas, Joerg;handle: 10261/201194
Offshore Ecuador, the Carnegie Ridge is a volcanic ridge with a carbonate sediment drape. During the SALIERI Cruise, multibeam bathymetry was collected across Carnegie Ridge with the Simrad EM120 of the R/V SONNE. The most conspicuous features discovered on the Carnegie Ridge are fields of circular closed depressions widely distributed along the mid-slope of the northern and southern flanks of the ridge between 1500 and 2600 m water depth. These circular depressions are 1–4 km wide and typically 100–400 m deep. Most are flat floored and some are so densely packed that they form a honeycomb pattern. The depressions were carved into the ridge sedimentary blanket, which consists of carbonate sediment and has been dated from upper Miocene to upper Pleistocene. Several hypotheses including pockmark origin, sediment creeping, paleo-topography of the volcanic basement, effects of subbottom currents, and both marine and subaerial karstic origins are discussed. We believe that underwater dissolution process merits the most serious consideration regarding the origin of the closed depression 15 pages, 7 figures
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For further information contact us at helpdesk@openaire.euAccess Routesbronze 32 citations 32 popularity Top 10% influence Top 10% impulse Average Powered by BIP!visibility 24visibility views 24 Powered bymore_vert add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Article , Other literature type 2018 Netherlands, United Kingdom, United Kingdom, Netherlands, Netherlands, Spain, France, Portugal, Germany, Spain, United Kingdom, United Kingdom, Switzerland, United Kingdom, Netherlands, United Kingdom, Germany, Spain, United StatesPublisher:Elsevier BV Funded by:NWO | Feasibility of commercial..., NSF | Support for International..., NSF | Support for International... +3 projectsNWO| Feasibility of commercial application of negative stiffness bar balancers ,NSF| Support for International Research Projects and Working Groups Through SCOR ,NSF| Support for International Ocean Science Activities Through the Scientific Committee on Oceanic Research ,NSF| Support for International Ocean Science Activities Through the Scientific Committee on Oceanic Research ,NSF| Support for International Research Projects and Working Groups Through SCOR ,UKRI| RootDetect: Remote Detection and Precision Management of Root HealthReiner Schlitzer; Robert F. Anderson; Elena Masferrer Dodas; Maeve C. Lohan; Walter Geibert; Andrew R. Bowie; Catherine Jeandel; William M. Landing; Cyril Abadie; Wafa Abouchami; Eric P. Achterberg; Morten B. Andersen; Corey Archer; Maureen E. Auro; Oliver Baars; Alex R. Baker; Karel Bakker; Chandranath Basak; Nicholas R. Bates; Dorothea Bauch; Pieter van Beek; Erin E. Black; Katrin Bluhm; Laurent Bopp; Heather A. Bouman; Philip W. Boyd; Marie Boye; Edward A. Boyle; Pierre Branellec; Luke Bridgestock; Guillaume Brissebrat; Thomas J. Browning; Hans-Jürgen Brumsack; Mark A. Brzezinski; Clifton S. Buck; Kristen N. Buck; Abby Bull; Pinghe Cai; Damien Cardinal; Craig A. Carlson; Gonzalo Carrasco; Núria Casacuberta; Karen L. Casciotti; Maxi Castrillejo; Rosie Chance; Matthew A. Charette; Hai Cheng; Marcus Christl; Thomas M. Church; Ivia Closset; Peter Croot; Jay T. Cullen; Chris J. Daniels; Feifei Deng; Brian Duggan; Gabriel Dulaquais; Cynthia Dumousseaud; Yolanda Echegoyen-Sanz; Michael J. Ellwood; Jessica N. Fitzsimmons; A. Russell Flegal; Martin Q. Fleisher; Tina van de Flierdt; Martin Frank; Jana Friedrich; François Fripiat; Henning Fröllje; Stephen J.G. Galer; Toshitaka Gamo; Raja S. Ganeshram; Jordi Garcia-Orellana; Ester Garcia-Solsona; Melanie Gault-Ringold; Loes J. A. Gerringa; Melissa Gilbert; José Marcus Godoy; Steven L. Goldstein; Santiago R. Gonzalez; Karen Grissom; Chad R. Hammerschmidt; Alison E. Hartman; Christel S. Hassler; Ed C Hathorne; Mariko Hatta; Nicholas J. Hawco; Lars-Eric Heimbürger; Josh Helgoe; Gideon M. Henderson; Paul B. Henderson; Peng Ho; Tristan J. Horner; Yu-Te Hsieh; Kuo-Fang Huang; Matthew P. Humphreys; Jeremy E. Jacquot; David J. Janssen; Janice L. Jones; Lauren Kipp; J. K. Klar; Sven Kretschmer; Yuichiro Kumamoto; Patrick Laan; François Lacan; Phoebe J. Lam; Myriam Lambelet; Carl H. Lamborg; Emilie Le Roy; Jong-Mi Lee; Pascale Lherminier; Susan H. Little; Mercedes López-Lora; Pere Masqué; Edward Mawji; Charles R. McClain; Christopher I. Measures; Sanjin Mehic; Pier van der Merwe; Rob Middag; Sebastian Mieruch; Angela Milne; Tomoharu Minami; James W. Moffett; Gwenaelle Moncoiffe; Willard S. Moore; Paul J. Morris; Peter L. Morton; John Niedermiller; Jun Nishioka; Akira Nishiuchi; Abigail E. Noble; Sven Ober; Daniel C. Ohnemus; Jan van Ooijen; Stephanie Owens; Katharina Pahnke; Maxence Paul; Leopoldo D. Pena; Brian Peters; Frédéric Planchon; Hélène Planquette; Viena Puigcorbé; Paul D. Quay; Sara Rauschenberg; Mark Rehkämper; Tomas A. Remenyi; Joseph A. Resing; Joerg Rickli; Sylvain Rigaud; Montserrat Roca-Martí; Valentí Rodellas; Saeed Roshan; Evgenia Ryabenko; Mak A. Saito; Lesley Salt; Virginie Sanial; Géraldine Sarthou; Christina Schallenberg; Ursula Schauer; Christian Schlosser; Bernhard Schnetger; Peter N. Sedwick; Igor Semiletov; Rachel U. Shelley; Robert M. Sherrell; Alan M. Shiller; Daniel M. Sigman; Sunil K. Singh; Hans A. Slagter; Emma Slater; William M. Smethie; Helen M. Snaith; Yoshiki Sohrin; Bettina Sohst; Jeroen E. Sonke; Sabrina Speich; Reiner Steinfeldt; Gillian Stewart; Torben Stichel; Claudine H. Stirling; Johnny Stutsman; Alexander L. Thomas; Kay Thorne; Claire P. Till; Ralph Till; Ashley T. Townsend; Robyn E. Tuerena; Benjamin S. Twining; Celia Venchiarutti; María Villa-Alfageme; Sebastian M. Vivancos; Bronwyn Wake; Ros Watson; Evaline M. van Weerlee; Yishai Weinstein; E. Malcolm S. Woodward; Jingfeng Wu; Yingzhe Wu; Kathrin Wuttig; Neil J. Wyatt; Yang Xiang; Zichen Xue; Jing Zhang; Pu Zhang; Ye Zhao; Linjie Zheng; Xin Yuan Zheng; Louise A. Zimmer; Patrizia Ziveri; Patricia Zunino;The GEOTRACES Intermediate Data Product 2017 (IDP2017) is the second publicly available data product of the international GEOTRACES programme, and contains data measured and quality controlled before the end of 2016. The IDP2017 includes data from the Atlantic, Pacific, Arctic, Southern and Indian oceans, with about twice the data volume of the previous IDP2014. For the first time, the IDP2017 contains data for a large suite of biogeochemical parameters as well as aerosol and rain data characterising atmospheric trace element and isotope (TEI) sources. The TEI data in the IDP2017 are quality controlled by careful assessment of intercalibration results and multi-laboratory data comparisons at crossover stations. The IDP2017 consists of two parts: (1) a compilation of digital data for more than 450 TEIs as well as standard hydrographic parameters, and (2) the eGEOTRACES Electronic Atlas providing an on-line atlas that includes more than 590 section plots and 130 animated 3D scenes. The digital data are provided in several formats, including ASCII, Excel spreadsheet, netCDF, and Ocean Data View collection. Users can download the full data packages or make their own custom selections with a new on-line data extraction service. In addition to the actual data values, the IDP2017 also contains data quality flags and 1-σ data error values where available. Quality flags and error values are useful for data filtering and for statistical analysis. Metadata about data originators, analytical methods and original publications related to the data are linked in an easily accessible way. The eGEOTRACES Electronic Atlas is the visual representation of the IDP2017 as section plots and rotating 3D scenes. The basin-wide 3D scenes combine data from many cruises and provide quick overviews of large-scale tracer distributions. These 3D scenes provide geographical and bathymetric context that is crucial for the interpretation and assessment of tracer plumes near ocean margins or along ridges. The IDP2017 is the result of a truly international effort involving 326 researchers from 25 countries. This publication provides the critical reference for unpublished data, as well as for studies that make use of a large cross-section of data from the IDP2017. This article is part of a special issue entitled: Conway GEOTRACES - edited by Tim M. Conway, Tristan Horner, Yves Plancherel, and Aridane G. González. National Science Foundation (U.S.) (Grant OCE-1243377) National Science Foundation (U.S.) (Grant OCE-1546580) National Science Foundation (U.S.) (Grant OCE-0608600) National Science Foundation (U.S.) (Grant OCE0938349)
CORE (RIOXX-UK Aggre... arrow_drop_down CORE (RIOXX-UK Aggregator)Article . 2018License: CC BY NC NDData sources: CORE (RIOXX-UK Aggregator)Chemical GeologyArticle . 2018Full-Text: http://repository.kulib.kyoto-u.ac.jp/dspace/bitstream/2433/233927/1/j.chemgeo.2018.05.040.pdfData sources: JAIRONARCIS; Chemical GeologyArticle . 2018Diposit Digital de la Universitat de Barcelona; Recolector de Ciencia Abierta, RECOLECTAArticle . 2019 . 2018License: CC BYUniversity of East Anglia digital repositoryArticle . 2018 . Peer-reviewedData sources: University of East Anglia digital repositorySapientia Repositório da Universidade do AlgarveArticle . 2020Data sources: Sapientia Repositório da Universidade do AlgarveRecolector de Ciencia Abierta, RECOLECTA; DIGITAL.CSICArticle . 2018 . 2019 . Peer-reviewedSpiral - Imperial College Digital RepositoryArticle . 2018Data sources: Spiral - Imperial College Digital RepositoryElectronic Publication Information CenterArticle . 2018Data sources: Electronic Publication Information CenterOxford University Research ArchiveArticle . 2018License: CC BYData sources: Oxford University Research ArchiveArchiMer - Institutional Archive of IfremerOther literature type . 2018Data sources: ArchiMer - Institutional Archive of IfremerRecolector de Ciencia Abierta, RECOLECTA; Dipòsit Digital de Documents de la UABArticle . 2018License: CC BYHAL AMU; Mémoires en Sciences de l'Information et de la Communication; HAL-CEA; HAL-IRDArticle . 2018License: CC BYArchiMer - Institutional Archive of IfremerOther literature type . 2018Data sources: ArchiMer - Institutional Archive of Ifremeradd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.euAccess RoutesGreen hybrid 251 citations 251 popularity Top 1% influence Top 10% impulse Top 0.1% Powered by BIP!visibility 288visibility views 288 download downloads 749 Powered bymore_vert CORE (RIOXX-UK Aggre... arrow_drop_down CORE (RIOXX-UK Aggregator)Article . 2018License: CC BY NC NDData sources: CORE (RIOXX-UK Aggregator)Chemical GeologyArticle . 2018Full-Text: http://repository.kulib.kyoto-u.ac.jp/dspace/bitstream/2433/233927/1/j.chemgeo.2018.05.040.pdfData sources: JAIRONARCIS; Chemical GeologyArticle . 2018Diposit Digital de la Universitat de Barcelona; Recolector de Ciencia Abierta, RECOLECTAArticle . 2019 . 2018License: CC BYUniversity of East Anglia digital repositoryArticle . 2018 . Peer-reviewedData sources: University of East Anglia digital repositorySapientia Repositório da Universidade do AlgarveArticle . 2020Data sources: Sapientia Repositório da Universidade do AlgarveRecolector de Ciencia Abierta, RECOLECTA; DIGITAL.CSICArticle . 2018 . 2019 . Peer-reviewedSpiral - Imperial College Digital RepositoryArticle . 2018Data sources: Spiral - Imperial College Digital RepositoryElectronic Publication Information CenterArticle . 2018Data sources: Electronic Publication Information CenterOxford University Research ArchiveArticle . 2018License: CC BYData sources: Oxford University Research ArchiveArchiMer - Institutional Archive of IfremerOther literature type . 2018Data sources: ArchiMer - Institutional Archive of IfremerRecolector de Ciencia Abierta, RECOLECTA; Dipòsit Digital de Documents de la UABArticle . 2018License: CC BYHAL AMU; Mémoires en Sciences de l'Information et de la Communication; HAL-CEA; HAL-IRDArticle . 2018License: CC BYArchiMer - Institutional Archive of IfremerOther literature type . 2018Data sources: ArchiMer - Institutional Archive of Ifremeradd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Article 2004 SpainPublisher:Editorial CSIC D´Onghia, Gianfranco; Lloris, Domingo; Sion, Letizia; Politou, Chrissi-Yianna; Dokos, John;handle: 10261/5789
[ES] Se recolectaron especies de peces en el mar Balear y en el Iónico oriental y occidental, gracias a una investigación subvencionada por la CE en aguas profundas del Mediterráneo (600-4000 m). Caelorhynchus mediterraneus es una nueva cita para el mar Balear, Cyclothone braueri, Hygophum benoiti, Paralepis speciosa, Chalinura mediterranea, Coryphaenoides guentheri, C. mediterraneus, Lepidion lepidion y Cataetyx laticeps lo son para el mar Iónico occidental, Polyacanthonotus rissoanus, C. guentheri, C. mediterraneus, L. lepidion y C. laticeps para el mar Iónico oriental. También se ha puesto al día la distribución batimétrica de otras especies. En las tres áreas muestreadas se ha observado que la riqueza específica desciende con la profundidad, marcándose un cambio significativo por debajo de los 1500 m. A profundidades superiores a 1000 m las especies de macrúridos y móridos fueron dominantes excepto para el mar Balear donde Alepocephalus rostratus fue la especie más abundante hasta 1500 m. A profundidades superiores a los 1500 m las especies dominantes fueron Bathypterois mediterraneus, C. mediterranea y C. guentheri. Los resultados confirman la escasez de ictiofauna profunda en el Mediterráneo comparada con la del Atlántico. Hasta las máximas profundidades muestradas, la diferencia faunística entre el Mediterráneo occidental y oriental parece ser debida, más al menor número de investigaciones llevados a cabo en el Mediterráneo oriental, que no a unas determinadas pautas en la distribución y abundancia dicha ictiofauna [EN] During an EC-funded research carried out in the Mediterranean Sea deep-water fish (600-4000 m) were collected in the Balearic Sea as well as the western and eastern Ionian Sea. Caelorhynchusmediterraneus is a new record for the Balearic Sea, Cyclothone braueri, Hygophum benoiti, Paralepis speciosa, Chalinura mediterranea, Coryphaenoides guentheri, C. mediterraneus, Lepidion lepidion and Cataetyx laticeps for the western Ionian Sea, and Polyacanthonotus rissoanus, C. guentheri, C. mediterraneus, L. lepidion and C. laticeps for the eastern Ionian Sea. The bathymetric distribution of other species has been updated. Species richness decreased with depth in the three surveyed areas, showing a significant shift below 1500 m. At depths greater than 1000 m macrourid and morid species were dominant except in the Balearic Sea, where Alepocephalus rostratus was found to be very abundant as deep as 1500 m. At depths greater than 1500 m the dominant species were Bathypterois mediterraneus, C. mediterranea and C. guentheri. The results of this research confirm the scarcity of deep fish fauna in the Mediterranean compared to the Atlantic. For the greatest depths are concerned, the faunistic difference between the western and eastern Mediterranean seems to be most probably due to a lesser number of investigations on the eastern side rather than any real paucity of ichthyofauna This work was supported by the Directorate General of Fisheries of the European Commission as part of the project DESEAS (Exploratory survey to collect data of the exploited and virgin stocks of deep-sea shrimp A. antennatus, of interest to the CFP - Study contract nº 2000/39, DGXIV). The authors wish to thank V. Catalano for providing helpful literature Peer reviewed
Scientia Marina arrow_drop_down Recolector de Ciencia Abierta, RECOLECTAArticle . 2004 . Peer-reviewedLicense: CC BYData sources: Recolector de Ciencia Abierta, RECOLECTARecolector de Ciencia Abierta, RECOLECTA; DIGITAL.CSICArticle . 2008 . 2004 . Peer-reviewedadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.euAccess Routesgold 25 citations 25 popularity Average influence Top 10% impulse Average Powered by BIP!visibility 19visibility views 19 download downloads 40 Powered bymore_vert Scientia Marina arrow_drop_down Recolector de Ciencia Abierta, RECOLECTAArticle . 2004 . Peer-reviewedLicense: CC BYData sources: Recolector de Ciencia Abierta, RECOLECTARecolector de Ciencia Abierta, RECOLECTA; DIGITAL.CSICArticle . 2008 . 2004 . Peer-reviewedadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Article 2012 SpainPublisher:Springer Science and Business Media LLC Authors: León Buendía, Ricardo F.; Somoza, Luis; Medialdea Cela, Teresa; Vázquez, Juan Tomás; +7 AuthorsLeón Buendía, Ricardo F.; Somoza, Luis; Medialdea Cela, Teresa; Vázquez, Juan Tomás; González Sanz, Francisco Javier; López-González, Nieves; Casas, David; Mata Campo, Maria Pilar; Fernández Puga, María del Carmen; Giménez-Moreno, Julia; Díaz del Río, Victor;handle: 10508/8416 , 10261/276844
During the MVSEIS-08 cruise of 2008, ten new mud volcanoes (MVs) were discovered on the offshore Moroccan continental margin (Gulf of Cádiz) at water depths between 750 and 1,600 m, using multibeam bathymetry, backscatter imagery, high-resolution seismic and gravity core data. Mud breccias were recovered in all cases, attesting to the nature of extrusion of these cones. The mud volcanoes are located in two fields: the MVSEIS, Moundforce, Pixie, Las Negras, Madrid, Guadix, Almanzor and El Cid MVs in the western Moroccan field, where mud volcanoes have long been suspected but to date not identified, and the Boabdil and Al Gacel MVs in the middle Moroccan field. Three main morphologies were observed: asymmetric, sub-circular and flat-topped cone-shaped types, this being the first report of asymmetric morphologies in the Gulf of Cádiz. Based on morpho-structural analysis, the features are interpreted to result from (1) repeated constructive (expulsion of fluid mud mixtures) and destructive (gravity-induced collapse and submarine landsliding) episodes and (2) interaction with bottom currents 10th International Conference on Gas in Marine Sediments, 6-11 September 2010, Listvyanka, Russia División de Geología Marina, Instituto Geológico y Minero de España, España Facultad de Ciencias Geológicas, Universidad Complutense de Madrid, España Centro Oceanográfico de Málaga, Instituto Español de Oceanografía, España Facultad de Ciencias del Mar, Universidad de Cádiz, España
Recolector de Cienci... arrow_drop_down Recolector de Ciencia Abierta, RECOLECTAArticle . 2012Data sources: Recolector de Ciencia Abierta, RECOLECTARecolector de Ciencia Abierta, RECOLECTA; DIGITAL.CSICArticle . 2012 . 2022Recolector de Ciencia Abierta, RECOLECTAArticle . 2012License: CC BY NC NDData sources: Recolector de Ciencia Abierta, RECOLECTARepositorio Institucional Digital del IEOArticle . 2012License: CC BY NC NDData sources: Repositorio Institucional Digital del IEOadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.euAccess RoutesGreen 43 citations 43 popularity Top 10% influence Average impulse Top 10% Powered by BIP!visibility 18visibility views 18 download downloads 66 Powered bymore_vert Recolector de Cienci... arrow_drop_down Recolector de Ciencia Abierta, RECOLECTAArticle . 2012Data sources: Recolector de Ciencia Abierta, RECOLECTARecolector de Ciencia Abierta, RECOLECTA; DIGITAL.CSICArticle . 2012 . 2022Recolector de Ciencia Abierta, RECOLECTAArticle . 2012License: CC BY NC NDData sources: Recolector de Ciencia Abierta, RECOLECTARepositorio Institucional Digital del IEOArticle . 2012License: CC BY NC NDData sources: Repositorio Institucional Digital del IEOadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Article 2017 United Kingdom, Norway, United Kingdom, IcelandPublisher:Springer Science and Business Media LLC Funded by:EC | Blue-Action, EC | NACLIM, EC | ATLASEC| Blue-Action ,EC| NACLIM ,EC| ATLASHátún, H.; Azetsu-Scott, K.; Somavilla, R.; Rey, F.; Johnson, C.; Mathis, M.; Mikolajewicz, U.; Coupel, P.; Tremblay, J.-É.; Hartman, S.; Pacariz, S. V.; Salter, I.; Ólafsson, J.;The North Atlantic is characterized by diatom-dominated spring blooms that results in significant transfer of carbon to higher trophic levels and the deep ocean. These blooms are terminated by limiting silicate concentrations in summer. Numerous regional studies have demonstrated phytoplankton community shifts to lightly-silicified diatoms and non-silicifying plankton at the onset of silicate limitation. However, to understand basin-scale patterns in ecosystem and climate dynamics, nutrient inventories must be examined over sufficient temporal and spatial scales. Here we show, from a new comprehensive compilation of data from the subpolar Atlantic Ocean, clear evidence of a marked pre-bloom silicate decline of 1.5-2 mu M throughout the winter mixed layer during the last 25 years. This silicate decrease is primarily attributed to natural multi-decadal variability through decreased winter convection depths since the mid-1990s, a weakening and retraction of the subpolar gyre and an associated increased influence of nutrient-poor water of subtropical origin. Reduced Arctic silicate import and the projected hemispheric-scale climate change-induced weakening of vertical mixing may have acted to amplify the recent decline. These marked fluctuations in pre-bloom silicate inventories will likely have important consequences for the spatial and temporal extent of diatom blooms, thus impacting ecosystem productivity and ocean-atmosphere climate dynamics. This work was initiated through the Nordic Council of Ministers project (AEG-11323). H.H. is supported by the European Union 7th Framework Programme (n. 308299 NACLIM www.naclim.eu), the EU Horizon 2020 Blue-Action project (BG-10-2016, www.blue-action.eu) and the Danish project NAACOS 10-093903/DSF. R.S. is supported by a Marie Curie Clarin Cofund Grant (ACB-1431). S.P. was funded by the Danish government through the research center 'Climate and oceanographic changes in the marine area between Greenland and Faroes - Influences on plankton and fish'. C.J. was funded under the European Union's Horizon 2020 research and innovation under grant agreement No. 678760 (ATLAS). This output reflects only the author's view and the European Union cannot be held responsible for any use that may be made of the information contained therein. Funding information on the model simulations and the observation programs is given in the Supplementary Information 1. The model simulations were supported by the co-operative project "RACE - Regional Atlantic Circulation and Global Change" funded by the German Federal Ministry for Education and Research (BMBF). We thank Solva Jacobsen for providing the Faroe Shelf silicate record. Peer Reviewed
e-Prints Soton arrow_drop_down Europe PubMed CentralArticle . 2017Full-Text: http://europepmc.org/articles/PMC5674075Data sources: PubMed CentralZENODO; Scientific Reports; NERC Open Research ArchiveOther literature type . Article . 2017 . Peer-reviewedLicense: CC BYadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.euAccess RoutesGreen gold 76 citations 76 popularity Top 1% influence Top 10% impulse Top 10% Powered by BIP!visibility 114visibility views 114 download downloads 93 Powered bymore_vert e-Prints Soton arrow_drop_down Europe PubMed CentralArticle . 2017Full-Text: http://europepmc.org/articles/PMC5674075Data sources: PubMed CentralZENODO; Scientific Reports; NERC Open Research ArchiveOther literature type . Article . 2017 . Peer-reviewedLicense: CC BYadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Article 2014 Norway, Spain, United KingdomPublisher:Editorial CSIC Mechó, Ariadna; Billett, David S.M.; Ramírez-Llodra, Eva; Aguzzi, Jacopo; Tyler, P.A.; Company, Joan B.;handle: 11250/227091 , 10261/99973
[ES] Este estudio presenta una recopilación de toda la información disponible sobre los equinodermos de profundidad en el talud continental medio e inferior del mar Mediterráneo, con el fin de proporcionar una fuente de información unificada sobre la taxonomía de este grupo. Se han actualizado los registros anteriores mediante nuevos datos provenientes de 223 pescas de arrastre de 11 campañas oceanográficas realizadas en el noroeste Mediterráneo entre 800 y 2845 m de profundidad. Se ha actualizado el nombre de las especies, sus rangos batimétricos y sus distribuciones geográficas. Los nuevos datos presentan, por primera vez, la presencia del equinoideo Atlántico Gracilechinus elegans (Düben and Koren, 1844) en el mar Mediterráneo. También se cita la presencia en el noroeste Mediterráneo de dos especies de holoturias endémicas del Mediterráneo, Hedingia mediterranea (Bartolini Baldelli, 1914), muestreada una única vez en 1914 en el mar Tirreno, y Penilpidia ludwigi (von Marenzeller, 1893), muestreada tres veces, dos en el mar Egeo y una en el mar Balear. Además se expanden los límites de distribución batimétrica para cuatro especies: el asteroideo Ceramaster grenadensis (Perrier, 1881) hasta 2845 m; el equinoideo Brissopsis lyrifera (Forbes, 1841) hasta los 2250 m; y las holoturias Hedingia mediterranea y Holothuria (Panningothuria) forskali Delle Chiaje, 1823, hasta los 1500 m y 850 m respectivamente [EN] This study provides a compilation of all available information on deep-sea echinoderms from the middle and lower slopes of the Mediterranean Sea, with the aim of providing a unified source of information on the taxonomy of this group. Previous records of species are updated with new data obtained from 223 trawl hauls conducted in 11 cruises within the northwestern Mediterranean Sea between 800 m and 2845 m depth. Valid names, bathymetric ranges and geographic distributions are given for all species. The new data report, for the first time, the presence of the Atlantic echinoid Gracilechinus elegans (Düben and Koren, 1844) in the Mediterranean Sea. We also report the presence of the endemic holothurians Hedingia mediterranea (Bartolini Baldelli, 1914), dredged only once previously in 1914 in the Tyrrhenian Sea, and Penilpidia ludwigi (von Marenzeller, 1893), known previously only from three samples, two in the Aegean Sea and one in the Balearic Sea. Additionally, the deeper limits of the bathymetric distribution of four species have been expanded: the asteroid Ceramaster grenadensis (Perrier, 1881) to 2845 m; the echinoid Brissopsis lyrifera (Forbes, 1841) to 2250 m; and the holothurians Hedingia mediterranea and Holothuria (Panningothuria) forskali Delle Chiaje, 1823, to 1500 m and 850 m, respectively This study was funded by the PROMETEO project (CTM2007-66316-C02/MAR, CICYT), the BIOFUN project (CTM2007-28739-E, European Science Foundation and national funding agencies) and the DOSMARES project (CTM2010-21810-C03-03). ERLL was funded by a JAE-DOC postdoctoral grant (CSIC, Spain) with co-funding from the European Social Fund. JA is a fellow of the Ramón y Cajal Programme (MICINN) 22 pages, 13 figures, 3 tables Peer reviewed
NIVA Open Access Arc... arrow_drop_down Scientia MarinaArticle . 2014 . Peer-reviewedLicense: CC BYNERC Open Research ArchiveArticle . 2014 . Peer-reviewedFull-Text: http://nora.nerc.ac.uk/508010/1/Mecho%20et%20al.%20final%20manuscript%20as%20submitted.pdfData sources: NERC Open Research ArchiveRecolector de Ciencia Abierta, RECOLECTAArticle . 2014 . Peer-reviewedLicense: CC BYData sources: Recolector de Ciencia Abierta, RECOLECTARecolector de Ciencia Abierta, RECOLECTA; DIGITAL.CSICArticle . 2014 . Peer-reviewedadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.euAccess RoutesGreen gold 23 citations 23 popularity Top 10% influence Average impulse Top 10% Powered by BIP!visibility 26visibility views 26 download downloads 162 Powered bymore_vert NIVA Open Access Arc... arrow_drop_down Scientia MarinaArticle . 2014 . Peer-reviewedLicense: CC BYNERC Open Research ArchiveArticle . 2014 . Peer-reviewedFull-Text: http://nora.nerc.ac.uk/508010/1/Mecho%20et%20al.%20final%20manuscript%20as%20submitted.pdfData sources: NERC Open Research ArchiveRecolector de Ciencia Abierta, RECOLECTAArticle . 2014 . Peer-reviewedLicense: CC BYData sources: Recolector de Ciencia Abierta, RECOLECTARecolector de Ciencia Abierta, RECOLECTA; DIGITAL.CSICArticle . 2014 . Peer-reviewedadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Article 2009 SpainPublisher:Elsevier BV Authors: Fernández Salas, Luis Miguel; Dabrio, Cristino J.; Goy Goy, José Luis; Díaz del Río, Víctor; +4 AuthorsFernández Salas, Luis Miguel; Dabrio, Cristino J.; Goy Goy, José Luis; Díaz del Río, Víctor; Zazo Cardeña , Caridad; Lobo Sánchez, Francisco José; Sanz Alonso, José Luis; Lario, Javier;handle: 10261/247560 , 10508/7758 , 10261/318956 , 20.500.14352/41786
The well-exposed systems of prograding beach ridges on the Carchuna-Calahonda (Granada) and Campo de Dalías-Roquetas (Almería) coastal plains continue offshore as infralittoral prograding wedges (IPW). The Holocene IPW is a narrow morpho-sedimentary unit up to 2.5 km wide which develops seaward from the lower edge of the shoreface to 15-20 m depth, extending to a well-defined break of slope at water depths of 35-40 m. These IPWs have been recognized and studied using very high-resolution seismic profiles (TOPAS) and multibeam data (EM-3000D). In detail they are complex morpho-sedimentary units in which internal structures are closely linked to the pattern of progradation of the adjacent coastal plains. When longshore currents produce significant littoral drift, the IPWs are composed of several minor units arranged in offlap, which accrete parallel or oblique to the main shoreline. Therefore, it is possible to correlate progradational units in the coastal plain (H-units, sensu[Goy, J.L., Zazo, C., Dabrio, C.J., 2003. A beach-ridge progradation complex reflecting periodical sea-level and climate variability during the Holocene (Gulf of Almería, Western Mediterranean). Geomorphology 50, 251-268]) and subunits in the IPW, but special care is required depending on the local arrangement of morpho-sedimentary units. Besides, it is not realistic to draw conclusions regarding the age of the subunits inside a given IPW without adequate dating, as the number of subunits will greatly vary from place to place depending on local factors, magnitude of sea-level oscillations, and sediment supply. The geophysical information of marine areas was provided by research project: “Estudio Geológico de la Plataforma Continental Española”, funded by “Secretaría General de Pesca Maritima, Ministerio de Agricultura, Pesca y Alimentación”. Research on land was funded by Projects CGL 2005-01336/BTE and CGL 2005-04655/BTE. This is a contribution to IGCP projects 464 (Continental shelves during the last glacial cycles: knowledge and applications) and 495 (Quaternary land–ocean interactions: driving mechanisms and coastal responses), and to Work Group UCM: “Paleoclimatology and Global Change (910198)”.
E-Prints Complutense arrow_drop_down Recolector de Ciencia Abierta, RECOLECTA; Docta ComplutenseArticle . 2023 . 2009Recolector de Ciencia Abierta, RECOLECTA; DIGITAL.CSICArticle . 2021 . 2009Recolector de Ciencia Abierta, RECOLECTAArticle . 2009 . Peer-reviewedData sources: Recolector de Ciencia Abierta, RECOLECTARepositorio Institucional Digital del IEOArticle . 2009License: CC BY NC NDData sources: Repositorio Institucional Digital del IEOadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.euAccess RoutesGreen bronze 40 citations 40 popularity Top 10% influence Top 10% impulse Top 10% Powered by BIP!visibility 17visibility views 17 download downloads 21 Powered bymore_vert E-Prints Complutense arrow_drop_down Recolector de Ciencia Abierta, RECOLECTA; Docta ComplutenseArticle . 2023 . 2009Recolector de Ciencia Abierta, RECOLECTA; DIGITAL.CSICArticle . 2021 . 2009Recolector de Ciencia Abierta, RECOLECTAArticle . 2009 . Peer-reviewedData sources: Recolector de Ciencia Abierta, RECOLECTARepositorio Institucional Digital del IEOArticle . 2009License: CC BY NC NDData sources: Repositorio Institucional Digital del IEOadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Article 2006Publisher:American Geophysical Union (AGU) Publicly fundedTrevor William; Akihiro Kano; Timothy G. Ferdelman; Jean-Pierre Henriet; Kohei Abe; Miriam S. Andres; Morten Bjerager; Emily L Browning; Barry Andrew Cragg; Ben De Mol; Boris Dorschel; Anneleen Foubert; Tracy D. Frank; Yuji Fuwa; Philippe Gaillot; Jamshid J. Gharib; Jay M. Gregg; Veerle A.I. Huvenne; Philippe Léonide; Xianghui Li; Kai Mangelsdorf; Akiko Tanaka; Xavier Monteys; Ivana Novosel; Saburo Sakai; Vladimir A. Samarkin; Keiichi Sasaki; Arthur J. Spivack; Chizuru Takashima; Jürgen Titschak;doi: 10.1029/2006eo470001
The discovery of mounds and reefs hosting cold‐water coral ecosystems along the northeastern Atlantic continental margins has propelled a vigorous effort over the past decade to study the distribution of the mounds, surface sediments, the ecosystems they host, and their environments [Hovland et al., 1994; Freiwald and Roberts, 2005].This effort has involved swath bathymetry, remotely operated vehicle deployments, shallow coring, and seismic surveys.Global coverage is difficult to gauge, but studies indicate that cold‐water corals may cover as large an area as the better known warm‐water corals that form shallow reefs (284,300 square kilometers) [Freiwald et al., 2005]. Cold‐water corals occur in a variety of forms and settings, from small isolated colonies or patch reefs to giant mound structures such as those found west of Ireland.
add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.euAccess Routesbronze 37 citations 37 popularity Average influence Top 10% impulse Top 10% Powered by BIP!more_vert add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
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