Analysis of an ancient global warming event, the Paleocene-Eocene thermal maximum, under examination from ODP Holes 113-689B and 113-690B

Spatiotemporal patterns of carbonate dissolution provide a critical constraint on carbon input during an ancient (~55.5 Ma) global warming event known as the Paleocene-Eocene thermal maximum (PETM), yet the magnitude of lysocline shoaling in the Southern Ocean is poorly constrained due to limited sp...

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Bibliographic Details
Main Authors: Kelly, Daniel Clay, Nielsen, Tina M J, Schellenberg, Stephen A
Format: Other/Unknown Material
Language:English
Published: PANGAEA 2012
Subjects:
Ocean Drilling Program
ODP
Antarc*
Antarctic
Ocean acidification
Southern Ocean
Weddell Sea
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.787773
https://doi.org/10.1594/PANGAEA.787773

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