Award Abstract # 0739583
Collaborative Research: Linking Modern Benthic Communities and Taphonomic Processes to the Stratigraphic Record of Antarctic Cores

NSF Org: OPP
Office of Polar Programs (OPP)
Recipient: HEALTH RESEARCH, INC.
Initial Amendment Date: July 29, 2008
Latest Amendment Date: July 19, 2010
Award Number: 0739583
Award Instrument: Continuing Grant
Program Manager: Alexandra Isern
OPP
 Office of Polar Programs (OPP)
GEO
 Directorate for Geosciences
Start Date: September 1, 2008
End Date: August 31, 2012 (Estimated)
Total Intended Award Amount: $160,268.00
Total Awarded Amount to Date: $160,268.00
Funds Obligated to Date: FY 2008 = $75,879.00
FY 2009 = $8,201.00

FY 2010 = $76,188.00
History of Investigator:
  • Samuel Bowser (Principal Investigator)
    samuel.bowser@health.ny.gov
Recipient Sponsored Research Office: Health Research Incorporated/New York State Department of Health
150 BROADWAY, SUITE 280
MENANDS
NY  US  12204-2732
(518)431-1200
Sponsor Congressional District: 20
Primary Place of Performance: Wadsworth Center
P.O. Box 509
Albany
NY  US  12201-0509
Primary Place of Performance
Congressional District:
20
Unique Entity Identifier (UEI): G9H6SUM59YC4
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 answers a simple question: why are there so few fossils in sediment cores from Antarctica?s continental shelf? Antarctica?s benthos are as biologically rich as those of the tropics. Shell-secreting organisms should have left a trail throughout geologic time, but have not. This trail is particularly important because these organisms record regional climate in ways that are critical to interpreting the global climate record. This study uses field experiments and targeted observations of modern benthic systems to examine the biases inflicted by fossil preservation. By examining a spectrum of ice-affected habitats, this project provides paleoenvironmental insights into carbonate preservation, sedimentation rates, and burial processes; and will provide new approaches to reconstructing the Cenozoic history of Antarctica. Broader impacts include graduate and undergraduate research and education, development of undergraduate curricula to link art and science, K12 outreach, public outreach via the web, and societal relevance through improved understanding of records of global climate change.

PUBLICATIONS PRODUCED AS A RESULT OF THIS RESEARCH

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Habura, "High-throughput sequencing of Astrammina rara: Sampling the giant genome of a giant foraminiferan protist" BMC Genomics , v.12 , 2011 , p.169 16910.1186/1471-2164-12-169
McClintock, J.B., Tackett, L.B., Bowser, S.S. "Video observations on non-swimming valve-claps in the Antarctic scallop Adamussium colbecki" Antarctic Science , v.22 , 2010 , p.173 10.1017/S0954102009990757
Miller, M.F., S.S. Bowser, and S.E. Walker "Diving for the sedimentary record of multiyear sea ice" Oceanography , v.25 , 2012 , p.118 http://dx.doi.org/10.5670/oceanog.2012.83.
MURRAY, K. T., MILLER, M. F. and BOWSER, S. S. "Depositional processes beneath coastal multi-year sea ice" Sedimentology , 2012 doi: 10.1111/j.1365-3091.2012.01345.x

PROJECT OUTCOMES REPORT

Disclaimer

This Project Outcomes Report for the General Public is displayed verbatim as submitted by the Principal Investigator (PI) for this award. Any opinions, findings, and conclusions or recommendations expressed in this Report are those of the PI and do not necessarily reflect the views of the National Science Foundation; NSF has not approved or endorsed its content.

As earth climate warms and ice sheets melt, more and more land cover will be exposed along the Antarctic continent. What influence will greater imput of terrestrial materials have on near shore marine environments? Can we better recognize similar episodes in earth history from the fossil record? This research project identified key aspects of "fossilization" processes in a setting associated with such an ice-free landscape, namely the Taylor Dry Valley in McMurdo Sound. In 2006 and again in 2008, research divers collected numerous sediment cores, deployed/retrieved experimental arrays, and conducted photo/video transects at primary research site, Explorers Cove, which is one of the few places in Antarctica that is readily accessible for such research. Our group helped determine the fate of wind-swept and meltwater-deposited sediment to the seafloor and identified the role of various organisms in disturbing surface sediment and thus influencing the fossil record. We also developed molecular markers for one key group of fossil-producing unicellular organisms (i.e., foraminiferan protists), which can now be used in future studies of "ancient DNA" in this and other Antarctic marine environments. During the course of this work, approximately 1,000 students and adults were directly addressed by participating scientists through school visits and public outreach talks.


Last Modified: 11/29/2012
Modified by: Samuel S Bowser

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