Stable carbon and oxygen isotope ratios of benthic and planktonic foraminifera of ODP Hole 171-1049C

Ocean anoxic events were periods of high carbon burial that led to drawdown of atmospheric carbon dioxide, lowering of bottom-water oxygen concentrations and, in many cases, significant biological extinction (Arthur et al., 1990; Erbacher et al., 1996, doi:10.1130/0091-7613(1996)024<0499:EPORAO&g...

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Bibliographic Details
Main Authors: Erbacher, Jochen, Huber, Brian T, Norris, Richard D, Markey, Molly
Format: Dataset
Language:English
Published: PANGAEA 2000
Subjects:
ODP
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.769750
https://doi.org/10.1594/PANGAEA.769750