[Keyword='GLOBAL WARMING']
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Paleocene-Eocene Thermal Maximum Isotope and Mg/Ca Data
Entry ID:
NOAA_NCDC_PALEO_2005-058
Summary
Abstract:
A rapid increase in greenhouse gas levels is thought to have fueled global
warming at the Paleocene-Eocene Thermal Maximum (PETM). Foraminiferal magnesium/calcium ratios indicate that bottom waters warmed by 4 to 5C, similar to tropical and subtropical surface ocean waters, implying no amplification of warming in high-latitude regions of deep-water formation under ice-free conditions. Intermediate waters warmed before the carbon isotope excursion, in association with downwelling in the North Pacific and reduced Southern Ocean convection, supporting changing circulation as the trigger for methane hydrate release. A switch to deep convection in the North Pacific at the PETM onset could have amplified and sustained warming. Geographic Coverage
(Click for Interactive Map)
Spatial coordinates
Data Set Citation
Dataset Originator/Creator:
Tripati, A. and H. Elderfield
Dataset Title:
Paleocene-Eocene Thermal Maximum Isotope and Mg/Ca Data
Dataset Series Name:
IGBP PAGES/WDCA CONTRIBUTION SERIES NUMBER: 2005-058
Dataset Release Date:
2005-08
Dataset Release Place:
Boulder, CO
Dataset Publisher:
IGBP PAGES/World Data Center for Paleoclimatology
Issue Identification:
2005-058
Other Citation Details:
NOAA/NCDC Paleoclimatology Program
Online Resource:
ftp://ftp.ncdc.noaa.gov/pub/data/paleo/paleocean/by_contributor/tri...
Paleo Temporal Coverage
Paleo Start Date:
55 Ma
Paleo Stop Date: 0 Ma Chrono Unit: Chrono Unit: Location Keywords
Science Keywords
ISO Topic Category
Ancillary Keywords
Data Set Progress
COMPLETE
Originating Center
Data Center
Distribution
Distribution Media:
ftp
Fees:
none
Personnel
Publications/References
Tripati, A. and H. Elderfield. 2005. Deep-Sea Temperature and Circulation
Changes at the Paleocene-Eocene Thermal Maximum. Science, Vol. 308, pp. 1894, 24 June 2005. Creation and Review Dates
DIF Creation Date:
2006-12-28
Last DIF Revision Date:
2007-08-03
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