{"data":{"id":"10.1594/pangaea.713295","type":"dois","attributes":{"doi":"10.1594/pangaea.713295","prefix":"10.1594","suffix":"pangaea.713295","identifiers":[],"alternateIdentifiers":[],"creators":[{"name":"Plank, Terry","givenName":"Terry","familyName":"Plank","nameIdentifiers":[{"schemeUri":"https://orcid.org","nameIdentifier":"https://orcid.org/0000-0002-1665-0484","nameIdentifierScheme":"ORCID"}],"affiliation":[]},{"name":"Balzer, Vaughn","givenName":"Vaughn","familyName":"Balzer","affiliation":[],"nameIdentifiers":[]},{"name":"Carr, Michael J","givenName":"Michael J","familyName":"Carr","affiliation":[],"nameIdentifiers":[]}],"titles":[{"title":"Chemical composition of ODP Leg 138 sediments"}],"publisher":"PANGAEA","container":{},"publicationYear":2002,"subjects":[{"subject":"Drilling/drill rig","subjectScheme":"Method"},{"subject":"Leg138","subjectScheme":"Campaign"},{"subject":"Joides Resolution","subjectScheme":"Basis"},{"subject":"Ocean Drilling Program (ODP)","subjectScheme":"Project"}],"contributors":[],"dates":[{"date":"2002","dateType":"Issued"}],"language":"en","types":{"ris":"GEN","bibtex":"misc","citeproc":"article","schemaOrg":"Collection","resourceType":"Supplementary Publication Series of Datasets","resourceTypeGeneral":"Collection"},"relatedIdentifiers":[{"relationType":"IsSupplementTo","relatedIdentifier":"10.1130/0091-7613(2002)030\u003c1087:nvrpca\u003e2.0.co;2","relatedIdentifierType":"DOI"}],"relatedItems":[],"sizes":["2 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":"A major oceanographic event preserved in the Cocos plate sedimentary column survived subduction and is recorded in the changing composition of Nicaraguan magmas. A uranium increase in these magmas since the latest Miocene (after 7 Ma) resulted from the 'carbonate crash' at 10 Ma and the ensuing high organic carbon burial in the sediments. The response of the arc to this paleoceanographic event requires near steady-state sediment recycling at this margin since 20 Ma. This relative stability in sediment subduction invites one of the first attempts to balance sedimentary input and arc output across a subduction zone. Calculations based on Th indicate that as much as 75% of the sedimentary column was subducted beneath the arc. The Nicaraguan margin is one of the few places to observe such strong links between the oceans and the solid earth.","descriptionType":"Abstract"},{"description":"Supplement to: Plank, Terry; Balzer, Vaughn; Carr, Michael J (2002): Nicaraguan volcanoes record paleoceanographic changes accompanying closure of the Panama gateway. Geology, 30, 1087-1090","descriptionType":"Other"}],"geoLocations":[{"geoLocationBox":{"eastBoundLongitude":"-90.48076000000003","northBoundLatitude":"9.5825","southBoundLatitude":"7.92131","westBoundLongitude":"-94.5908"}},{"geoLocationPlace":"North Pacific 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