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Stable and radiogenic isotope record for sediments cores from the Southern Indian Ocean

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Here we present reconstructions of water residence times (depicted as ΔΔ14C and δ13C) for the last 32,000 years on sediment records from the Kerguelen Plateau and the Conrad Rise (~570-2500 m water depth), along with simulated changes in ocean stratification from a transient climate model experiment.

Description

Our data indicate that Circumpolar Deep Waters in the Indian Ocean were part of the glacial carbon pool.

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Catalogue records · 1

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Inferred from text
Climate model simulation 65%
Provenance · 1 source records, 8 field assertions
SourceKeyLast seenRaw
PANGAEAoai:pangaea.de:doi:10.1594/PANGAEA.90636515 d agoJSON v1
FieldAssertionExtractorEvidence
access_levelsource · PANGAEAconnector:pangaea@1.0.0
concepts[field].local:field:earth-environmentalmapping · PANGAEAconnector:pangaea@1.0.0
concepts[method].local:method:climate-modelenrichment · PANGAEAkeyword-concept-rules@1.0.0title+description (65%)
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