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Planktonic foraminiferal oxygen isotope analysis by ion microprobe technique suggests warm tropical...

Planktonic foraminiferal oxygen isotope analysis by ion microprobe technique suggests warm tropical...

https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_proquest_journals_883388461

Planktonic foraminiferal oxygen isotope analysis by ion microprobe technique suggests warm tropical sea surface temperatures during the Early Paleogene

About this item

Full title

Planktonic foraminiferal oxygen isotope analysis by ion microprobe technique suggests warm tropical sea surface temperatures during the Early Paleogene

Publisher

Washington: Blackwell Publishing Ltd

Journal title

Paleoceanography and paleoclimatology, 2011-09, Vol.26 (3)

Language

English

Formats

Publication information

Publisher

Washington: Blackwell Publishing Ltd

More information

Scope and Contents

Contents

Muricae largely preserve their original d18O value Robust SSTs can be reconstructed from frosty foraminifers using SIMS Muricae d18O values are in agreement with model predictions for the PETM event Cool tropical sea surface temperatures (SSTs) are reported for warm Paleogene greenhouse climates based on the 18O of planktonic foraminiferal tests. T...

Alternative Titles

Full title

Planktonic foraminiferal oxygen isotope analysis by ion microprobe technique suggests warm tropical sea surface temperatures during the Early Paleogene

Identifiers

Primary Identifiers

Record Identifier

TN_cdi_proquest_journals_883388461

Permalink

https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_proquest_journals_883388461

Other Identifiers

ISSN

2572-4517

E-ISSN

2572-4525

DOI

10.1029/2010PA002056

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