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Data · dataset · 1997

(Table 1) Carbon, oxygen and strontium isotopic composition of the rhodochrosite nodules from DSDP Sites 503A and 503B

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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).

Description

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.

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Inferred from text
Geochemistry 74% · Tabular 65%
Provenance · 1 source records, 8 field assertions
SourceKeyLast seenRaw
DataCite10.1594/pangaea.70123014 d agoJSON v1
FieldAssertionExtractorEvidence
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concepts[field].anzsrc:group:3703enrichment · DataCitetaxonomy-embedding@1.1.0title+keywords+description (74%)
concepts[modality].local:modality:tabularenrichment · DataCitekeyword-concept-rules@1.0.0title+description (65%)
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