Deep Atlantic carbonate ion and CaCO3 Compensation during the Ice Ages
Supporting Files
-
2018
Details
-
Journal Title:Paleoceanography and Paleoclimatology
-
Personal Author:
-
NOAA Program & Office:
-
Description:Here we present a 1.5 Myr orbitally resolved deep ocean calcite saturation record (ΔCO32−) derived from benthic foraminiferal B/Ca ratios in the North Atlantic. Glacial ΔCO32− declines across the mid-Pleistocene transition suggesting increased sequestration of carbon in the deep Atlantic.
-
Keywords:
-
Source:Paleoceanography and Paleoclimatology, 33(6)
-
DOI:
-
Document Type:
-
Rights Information:Other
-
Compliance:Submitted
-
Main Document Checksum:urn:sha256:20b07ad333464fd4d6f2c9ba03b24f72da2a3962f771f31fecf29ede6b14c969
-
Download URL:
-
File Type:
Supporting Files
ON THIS PAGE
The NOAA IR serves as an archival repository of NOAA-published products including scientific findings, journal articles,
guidelines, recommendations, or other information authored or co-authored by NOAA or funded partners. As a repository, the
NOAA IR retains documents in their original published format to ensure public access to scientific information.
You May Also Like