(Table S1) Boron isotope and trace element data and reconstructed carbonate system parameters, ODP Holes 122-761B and 154-926A

The middle Miocene Climatic Optimum (17-15 Ma; MCO) is a period of global warmth and relatively high CO2 and is thought to be associated with a significant retreat of the Antarctic Ice Sheet (AIS). We present here a new planktic foraminiferal d11B record from 16.6 to 11.8 Ma from two deep ocean site...

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Bibliographic Details
Main Authors: Foster, Gavin L, Lear, Caroline H, Rae, James W B
Format: Dataset
Language:English
Published: PANGAEA 2012
Subjects:
AGE
ODP
pH
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.815855
https://doi.org/10.1594/PANGAEA.815855