Carbon 13 isotopes reveal limited ocean circulation changes between interglacials of the last 800 ka

DOI

We present a compilation of δ13C data to characterize the ocean circulation during the interglacials of the last 800 000 years. We selected 9 interglacials for which we have collected the available δ13C and δ18O values.

Identifier
DOI https://doi.org/10.1594/PANGAEA.913661
Related Identifier IsSupplementTo https://doi.org/10.1029/2019PA003776
Metadata Access https://ws.pangaea.de/oai/provider?verb=GetRecord&metadataPrefix=datacite4&identifier=oai:pangaea.de:doi:10.1594/PANGAEA.913661
Provenance
Creator Bouttes, Nathaëlle
Publisher PANGAEA
Publication Year 2020
Rights Creative Commons Attribution 4.0 International; https://creativecommons.org/licenses/by/4.0/
OpenAccess true
Representation
Resource Type Dataset
Format text/tab-separated-values
Size 558 data points
Discipline Earth System Research
Spatial Coverage (-110.518W, -42.914S, 159.361E, 60.404N); Caribbean Sea/RIDGE; North Atlantic/PLATEAU; North Atlantic/FLANK; Canarias Sea; South Atlantic Ocean; Indian Ocean; North Pacific Ocean; South Pacific Ocean; South China Sea; Walvis Ridge, Southeast Atlantic Ocean; North Atlantic; Walvis Ridge; Cape Basin; off Chile
Temporal Coverage Begin 1970-04-26T00:00:00Z
Temporal Coverage End 2004-10-30T00:00:00Z