Award Abstract # 1039365
COLLABORATIVE RESEARCH: The Permian -Triassic Transition in Antarctica: Evaluating the Rates and Variability of Carbon Isotope Fluctuatios in Terrestrial Organic Matter

NSF Org: OPP
Office of Polar Programs (OPP)
Recipient: BOARD OF TRUSTEES OF SOUTHERN ILLINOIS UNIVERSITY
Initial Amendment Date: May 7, 2010
Latest Amendment Date: May 7, 2010
Award Number: 1039365
Award Instrument: Standard Grant
Program Manager: Alexandra Isern
OPP
 Office of Polar Programs (OPP)
GEO
 Directorate for Geosciences
Start Date: August 28, 2009
End Date: February 29, 2012 (Estimated)
Total Intended Award Amount: $41,015.00
Total Awarded Amount to Date: $41,015.00
Funds Obligated to Date: FY 2007 = $41,015.00
History of Investigator:
  • Susan Rimmer (Principal Investigator)
    srimmer@siu.edu
Recipient Sponsored Research Office: Southern Illinois University at Carbondale
900 S NORMAL AVE
CARBONDALE
IL  US  62901-4302
(618)453-4540
Sponsor Congressional District: 12
Primary Place of Performance: Southern Illinois University at Carbondale
900 S NORMAL AVE
CARBONDALE
IL  US  62901-4302
Primary Place of Performance
Congressional District:
12
Unique Entity Identifier (UEI): Y28BEBJ4MNU7
Parent UEI:
NSF Program(s): ANT Earth Sciences
Primary Program Source: 0100CYXXDB NSF RESEARCH & RELATED ACTIVIT
Program Reference Code(s): 0000, 9150, OTHR
Program Element Code(s): 511200
Award Agency Code: 4900
Fund Agency Code: 4900
Assistance Listing Number(s): 47.078

ABSTRACT

This project studies the Permian-Triassic extinction event as recorded in sedimentary rocks from the Transantarctic Mountains of Antarctica. Two hundred and fifty million years ago most life on Earth was wiped out in a geologic instant. The cause is a subject of great debate. Researchers have identified a unique stratigraphic section near Shackleton glacier laid down during the extinction event. Organic matter from these deposits will be analyzed by density gradient centrifugation (DGC), which will offer detailed information on the carbon isotope composition. The age of these layers will be precisely dated by U/Pb-zircon-dating of intercalated volcanics. Combined, these results will offer detailed constraints on the timing and duration of carbon isotope excursions during the extinction, and offer insight into the coupling of marine and terrestrial carbon cycles.
The broader impacts of this project include graduate and undergraduate student research, K12 outreach and teacher involvement, and societal relevance of the results, since the P/T extinction may have been caused by phenomena such as methane release, which could accompany global warming.

PUBLICATIONS PRODUCED AS A RESULT OF THIS RESEARCH

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McPherson, M., Rimmer, S.M., and Rowe, H., "Geochemistry and petrography of thermally metamorphosed Antarctic coal: Implications for 13C-depleted methane release" GSA Annual Meeting Abtracts and Program , 2011 , p.1
McPherson, M., Sanders, J., Rimmer, S.M., Rowe, H. "Geochemical, isotopic and petrographic analysis of Permian coal and carbonaceous shales from Antarctica: Importance of rank and maceral composition." GSA NC-SC Annual Meeting Abstracts with Program , 2010 , p.1
Sanders, M.M.,Rimmer, S.M., Rowe, H., and Crelling, J.C. "Unique organic petrography of high-rank Antarctic coal and black shale." 2012 Annual Meeting Geological Society of America, November 4-7, 2012, Charlotte, NC, Abstracts with Programs , v.44 , 2012 , p.569

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