{"data":{"id":"10.1594/pangaea.701230","type":"dois","attributes":{"doi":"10.1594/pangaea.701230","prefix":"10.1594","suffix":"pangaea.701230","identifiers":[],"alternateIdentifiers":[],"creators":[{"name":"Morad, S","givenName":"S","familyName":"Morad","nameIdentifiers":[{"schemeUri":"https://orcid.org","nameIdentifier":"https://orcid.org/0000-0002-8214-0896","nameIdentifierScheme":"ORCID"}],"affiliation":[]},{"name":"Al-Aasm, Ihsan S","givenName":"Ihsan S","familyName":"Al-Aasm","affiliation":[],"nameIdentifiers":[]}],"titles":[{"title":"(Table 1) Carbon, oxygen and strontium isotopic composition of the rhodochrosite nodules from DSDP Sites 503A and 503B"}],"publisher":"PANGAEA","container":{},"publicationYear":1997,"subjects":[{"subject":"DEPTH, sediment/rock","subjectScheme":"Parameter"},{"subject":"Sample code/label","subjectScheme":"Parameter"},{"subject":"Sample type","subjectScheme":"Parameter"},{"subject":"δ13C","subjectScheme":"Parameter"},{"subject":"δ18O","subjectScheme":"Parameter"},{"subject":"Strontium-87/Strontium-86 ratio","subjectScheme":"Parameter"},{"subject":"Age, dated","subjectScheme":"Parameter"},{"subject":"Drilling/drill rig","subjectScheme":"Method"},{"subject":"DSDP/ODP/IODP sample designation","subjectScheme":"Method"},{"subject":"Mass spectrometer VG SIRA 12","subjectScheme":"Method"},{"subject":"Mass spectrometer Finnigan MAT 261","subjectScheme":"Method"},{"subject":"Age, paleomagnetic","subjectScheme":"Method"},{"subject":"Leg68","subjectScheme":"Campaign"},{"subject":"Glomar Challenger","subjectScheme":"Basis"},{"subject":"Deep Sea Drilling Project (DSDP)","subjectScheme":"Project"}],"contributors":[],"dates":[{"date":"1979-09-06T00:00:00","dateType":"Collected"},{"date":"1997","dateType":"Issued"}],"language":"en","types":{"ris":"DATA","bibtex":"misc","citeproc":"dataset","schemaOrg":"Dataset","resourceType":"Supplementary Dataset","resourceTypeGeneral":"Dataset"},"relatedIdentifiers":[{"relationType":"IsSupplementTo","relatedIdentifier":"10.1016/s0037-0738(97)00066-3","relatedIdentifierType":"DOI"}],"relatedItems":[],"sizes":["158 data points"],"formats":["text/tab-separated-values"],"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":"Calcic rhodochrosite occurs as nodules around burrows in late Neogene-early Pleistocene pelagic sediments of the Galapagos Ridge in the Guatemala Basin, eastern equatorial Pacific (DSDP Leg 68; Site 503). Growth was accomplished in the suboxic zone (d13C = -4.3 per mil to -1.3 per mil) at an estimated depth between ~30 and 70 cm beneath the seafloor. The rhodochrosites have 87Sr/86Sr ratios (0.708945–0.709073) that largely record the small-scale changes in seawater Sr-isotopic composition. The anomalous enrichment of the rhodochrosite in 18O isotopes (d18OPDB up to +6.4 per mil is attributed to the dissociation of gas hydrates.","descriptionType":"Abstract"},{"description":"Supplement to: Morad, S; Al-Aasm, Ihsan S (1997): Conditions of rhodochrosite-nodule formation in Neogene-Pleistocene deep-sea sediments: evidence from O, C and Sr isotopes. Sedimentary Geology, 114(1-4), 295-304","descriptionType":"Other"}],"geoLocations":[{"geoLocationPoint":{"pointLatitude":"4.0507","pointLongitude":"-95.6368"}},{"geoLocationPlace":"North 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