{"data":{"id":"10.1594/pangaea.692143","type":"dois","attributes":{"doi":"10.1594/pangaea.692143","prefix":"10.1594","suffix":"pangaea.692143","identifiers":[],"alternateIdentifiers":[],"creators":[{"name":"Pfannkuche, Olaf","givenName":"Olaf","familyName":"Pfannkuche","affiliation":[],"nameIdentifiers":[]}],"titles":[{"title":"Organic carbon flux through the benthic community in the temperate abyssal Northeast Atlantic"}],"publisher":"PANGAEA","container":{},"publicationYear":1992,"subjects":[{"subject":"Giant box corer","subjectScheme":"Method"},{"subject":"MultiCorer","subjectScheme":"Method"},{"subject":"M69","subjectScheme":"Campaign"},{"subject":"ANT-IV/1a","subjectScheme":"Campaign"},{"subject":"Meteor (1964)","subjectScheme":"Basis"},{"subject":"Polarstern","subjectScheme":"Basis"},{"subject":"Atlantic Data Base for Exchange Processes at the Deep Sea Floor (ADEPD)","subjectScheme":"Project"}],"contributors":[],"dates":[{"date":"1992","dateType":"Issued"}],"language":"en","types":{"ris":"GEN","bibtex":"misc","citeproc":"article","schemaOrg":"Collection","resourceType":"Supplementary Publication Series of Datasets","resourceTypeGeneral":"Collection"},"relatedIdentifiers":[],"relatedItems":[],"sizes":["6 datasets"],"formats":["application/zip"],"version":null,"rightsList":[{"rights":"Creative Commons Attribution 3.0 Unported","rightsUri":"https://creativecommons.org/licenses/by/3.0/legalcode","schemeUri":"https://spdx.org/licenses/","rightsIdentifier":"cc-by-3.0","rightsIdentifierScheme":"SPDX"}],"descriptions":[{"description":"In order to assess the carbon flux through the deep-sea benthic boundary layer, sediment community oxygen consumption (SCOC) was measured in different months and years at the BIOTRANS area in the abyssal northeastern Atlantic. SCOC varied seasonally with a maximum in July/August. Evidence is given for a direct coupling between a substantial sedimentation of phytodetritus and the seasonal increase in SCOC. Rapid colonization, growth and decomposition rates indicate that the deep-sea benthic microbial and protozoan biota can react quickly to substantial falls of particulate organic matter. They seem to be the most important groups to generate seasonal changes in deep-sea benthic carbon flux rates.","descriptionType":"Abstract"},{"description":"Supplement to: Pfannkuche, Olaf (1992): Organic carbon flux through the benthic community in the temperate abyssal northeast Atlantic. In: Rowe, G T \u0026amp; Pariente, V (eds.), Deep-sea food chains and the global carbon cycle. Dordrecht, Kluwer Academic Publishers, 183-198","descriptionType":"Other"}],"geoLocations":[{"geoLocationBox":{"eastBoundLongitude":"-19.175","northBoundLatitude":"47.469833","southBoundLatitude":"46.502666","westBoundLongitude":"-19.7717"}},{"geoLocationPlace":"Biotrans"},{"geoLocationPlace":"North Atlantic Ocean"}],"fundingReferences":[{"awardUri":"https://cordis.europa.eu/project/id/MAS3970126","awardTitle":"Atlantic Data Base for Exchange Processes at the Deep Sea Floor","funderName":"Fourth Framework Programme","awardNumber":"MAS3970126","funderIdentifier":"https://doi.org/10.13039/100011105","funderIdentifierType":"Crossref Funder 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