Oxygen isotope composition of benthic and planktonic foraminifera from ODP Holes 146-893A and 167-1017B, supplement to: Cannariato, Kevin G; Kennett, James P (2005): Structure of the penultimate deglaciation along the California margin and implications for Milankovitch theory. Geology, 33(2), 157-160

The detailed structure and timing of the penultimate deglaciation are insufficiently defined yet critical for understanding mechanisms responsible for abrupt climate change. Here we present oxygen isotope records (from planktonic and benthic foraminifera) at unprecedented resolution encompassing lat...

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Bibliographic Details
Main Authors: Cannariato, Kevin G, Kennett, James P
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA - Data Publisher for Earth & Environmental Science 2005
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.721804
https://doi.pangaea.de/10.1594/PANGAEA.721804