Stable isotope ratios measured on molluscan from the CRP sediment cores in the Ross Sea, Antarctica

Stable isotope analyses of marine bivalve growth increment samples have been used to estimate early Oligocene (29.4 - 31.2) Ma and early Miocene (24.0 Ma) seafloor palaeotemperature from the southwestern continental margin of the Ross Sea. Measured d18O values average +2.5 ‰ in the early Miocene and...

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Bibliographic Details
Main Authors: Lavelle, Mark, Fielding, Christopher R, Hall, Michael A
Format: Dataset
Language:English
Published: PANGAEA 2001
Subjects:
CRP
CWS
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.510768
https://doi.org/10.1594/PANGAEA.510768