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Globorotalia inflata oxygen isotope (δ¹⁸O), Mg/Ca-derived thermocline temperature and ice-volume free seawater δ¹⁸O from subtropical western South Atlantic core GL-1090 during the last glacial cycle

Listed in PANGAEA

These data contain the Monte Carlo ensemble δ¹⁸O, Mg/Ca-derived thermocline temperature and ice-volume free seawater δ¹⁸O from a thermocline-dweller planktic foraminifera (Globorotalia inflata) from the subtropical western South Atlantic (Santos Basin) analyzed in core GL-1090.

Description

The data reports the measured proxies and the Quantiles (Q0.025, Q0.16, Q0.84, Q0.975).

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Where it is published

Catalogue records · 1

Topics

Inferred from text
Geochemistry 75%
Provenance · 1 source records, 8 field assertions
SourceKeyLast seenRaw
PANGAEAoai:pangaea.de:doi:10.1594/PANGAEA.91620015 d agoJSON v1
FieldAssertionExtractorEvidence
access_levelsource · PANGAEAconnector:pangaea@1.0.0
concepts[field].anzsrc:group:3703enrichment · PANGAEAtaxonomy-embedding@1.1.0title+keywords+description (75%)
concepts[field].local:field:earth-environmentalmapping · PANGAEAconnector:pangaea@1.0.0
descriptionsource · PANGAEAconnector:pangaea@1.0.0/metadata/dc/description
licensesource · PANGAEAconnector:pangaea@1.0.0/metadata/dc/rights
publication_datesource · PANGAEAconnector:pangaea@1.0.0
spatialsource · PANGAEAconnector:pangaea@1.0.0
titlesource · PANGAEAconnector:pangaea@1.0.0/metadata/dc/title