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dc.creatorWild, Christian
dc.creatorRixen, Tim
dc.creatorSánchez Noguera, Celeste
dc.creatorMerico, Agostino
dc.creatorJiménez Centeno, Carlos
dc.creatorCortés Núñez, Jorge
dc.creatorNaumann, Malik S.
dc.date.accessioned2018-07-27T14:41:39Z
dc.date.available2018-07-27T14:41:39Z
dc.date.issued2015
dc.identifier.citationhttps://www.jstage.jst.go.jp/article/galaxea/17/1/17_13/_articlees_ES
dc.identifier.issn1883-3969
dc.identifier.issn1883-0838
dc.identifier.urihttp://hdl.handle.net/10669/75294
dc.description.abstractMarine methane seeps are typically observed in cold, anoxic and organic-rich deep-sea environments, such as in the Black Sea, where methane emissions fuel the authigenic accretion of calcium carbonate structures via microbial sulphate reduction and anaerobic methane oxidation (Michaelis et al. 2002). For shallow tropical waters, methane seeps are only known from hydrothermal vents (Nakamura et al. 2006). Here, we report about our recent discovery of a cold methane seep in warm (ca. 29℃) and O2-saturated (97-100%) Golfo Dulce (8.496450°N, 83.262610°W) that is located at the Southern Pacific coast of Costa Rica, Central America.es_ES
dc.language.isoen_USes_ES
dc.sourceGalaxea, Journal of Coral Reef Studies,vol.17(1),pp.13-14.es_ES
dc.subjectCarbonate platformes_ES
dc.subjectMethane seepes_ES
dc.subjectGolfo Dulcees_ES
dc.subjectCosta Ricaes_ES
dc.subjectPorites lobataes_ES
dc.subjectHalimedaes_ES
dc.titleA carbonate platform associated with shallow cold methane seeps in Golfo Dulce, Pacific Costa Ricaes_ES
dc.typeinfo:eu-repo/semantics/articlees_ES
dc.typeArtículo científicoes_ES
dc.identifier.doi10.3755/galaxea.17.13
dc.description.procedenceUCR::Vicerrectoría de Investigación::Unidades de Investigación::Ciencias Básicas::Centro de Investigación en Ciencias del Mar y Limnología (CIMAR)es_ES


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