
NSF Org: |
OCE Division Of Ocean Sciences |
Recipient: |
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Initial Amendment Date: | February 27, 2008 |
Latest Amendment Date: | February 27, 2008 |
Award Number: | 0751643 |
Award Instrument: | Standard Grant |
Program Manager: |
Bilal U. Haq
OCE Division Of Ocean Sciences GEO Directorate for Geosciences |
Start Date: | May 1, 2008 |
End Date: | April 30, 2010 (Estimated) |
Total Intended Award Amount: | $309,055.00 |
Total Awarded Amount to Date: | $309,055.00 |
Funds Obligated to Date: |
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History of Investigator: |
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Recipient Sponsored Research Office: |
266 WOODS HOLE RD WOODS HOLE MA US 02543-1535 (508)289-3542 |
Sponsor Congressional District: |
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Primary Place of Performance: |
266 WOODS HOLE RD WOODS HOLE MA US 02543-1535 |
Primary Place of
Performance Congressional District: |
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Unique Entity Identifier (UEI): |
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Parent UEI: |
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NSF Program(s): | Marine Geology and Geophysics |
Primary Program Source: |
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Program Reference Code(s): |
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Program Element Code(s): |
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Award Agency Code: | 4900 |
Fund Agency Code: | 4900 |
Assistance Listing Number(s): | 47.050 |
ABSTRACT
OCE-0751643
One of the most important and unexplained observations of the climate transition from the Last Glacial Maximum into the Holocene is the abrupt rise in atmospheric CO2 content and coincident decrease in the atmosphere's radiocarbon (14C) content that began about 16,000 years ago. It has been hypothesized that these changes reflect a sudden change in deep ocean circulation because the ocean is a much larger reservoir of carbon than the atmosphere. The strongest evidence for a deep ocean-atmosphere connection comes from a study by Marchitto et al., (2007) that showed the radiocarbon content of fossil benthic foraminifera from Baja California decreased dramatically starting 16,000 years ago. They hypothesized these data reflect the transit of 'old' carbon from the deep Southern Ocean to the north Pacific. In this project, the PI will confirm these published results and test the hypothesis that the increase in deglacial atmospheric CO2 was due to outgasing of the deep Southern Ocean via Antarctic Intermediate Water by studying the radiocarbon content of fossil benthic and planktic foraminifera in a suite of sediment cores along a depth transect from the Chilean margin. Because this region is very close to the presumed Southern Ocean source of the old deep water, and the cores span a range of intermediate ocean water depths, they are ideal for testing the Baja California observations and hypotheses. The PI will develop oxygen isotope stratigraphies and chronologies for the Chilean core suite to identify the deglacial interval, and will measure radiocarbon in benthic foraminifera from the cores to define the depth range and the extent of the radiocarbon ventilation changes during the deglaciation. The results of this research will test an important component of the evolving theory to explain how the land, the sea and the atmosphere interacted during the deglaciation to alter global climate. Broader impacts will include fundamental research to help explain the mechanisms of past climate change, K-12 outreach and international mentoring of a Chilean postdoctoral fellow, Dr. Ricardo dePol Holz.
PUBLICATIONS PRODUCED AS A RESULT OF THIS RESEARCH
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