
NSF Org: |
EAR Division Of Earth Sciences |
Recipient: |
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Initial Amendment Date: | August 30, 2010 |
Latest Amendment Date: | July 27, 2011 |
Award Number: | 1024614 |
Award Instrument: | Standard Grant |
Program Manager: |
Enriqueta Barrera
EAR Division Of Earth Sciences GEO Directorate for Geosciences |
Start Date: | September 1, 2010 |
End Date: | August 31, 2014 (Estimated) |
Total Intended Award Amount: | $300,667.00 |
Total Awarded Amount to Date: | $300,667.00 |
Funds Obligated to Date: |
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History of Investigator: |
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Recipient Sponsored Research Office: |
310 E CAMPUS RD RM 409 ATHENS GA US 30602-1589 (706)542-5939 |
Sponsor Congressional District: |
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Primary Place of Performance: |
623 BOYD GRADUATE RESEARCH CTR ATHENS GA US 30602-0001 |
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): |
ECOSYSTEM STUDIES, Geobiology & Low-Temp Geochem, EMERGING TOPICS, Global Systems Science |
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
Microorganisms from the Kingdom Archaea produce novel membrane lipids of the class isoprenoidal diethers and glycerol dialkyl glycerol tetraethers (GDGTs). In particular, crenarchaeol was recognized to be the key biomarker for low temperature crenarchaeota and known to be associated with ammonia-oxidizing archaea (AOA). AOA and crenarchaeol have recently been found in Great Basin hot springs and in a thermophilic culture ("Candidatus N. yellowstonii") enriched from springs in Yellowstone National Park. "Candidatus N. yellowstonii"-like species were also present in some of the Great Basin hot springs. The goal of this research is 1) to seek the linkage between crenarchaeol production and distribution of "Candidatus N. yellowstonii"-like species and 2) to determine the factors controlling the distribution of crenarchaeol and other archaeal lipid biomarkers in Great Basin hot springs. The PIs hypothesize that crenarchaeol is actively produced in situ by these microbes and can serve as a proxy for archaeal ammonia oxidation. This hypothesis will be tested by quantifying of archaeal biomarkers (particularly crenarchaeol) and "Candidatus N. yellowstonii"-like archaea in hot springs of different temperatures and chemical compositions and evaluation of soil contamination to the hot spring environment. The production of crenarchaeol will be linked to specific archaeal populations from natural environments using stable isotope probing (SIP) of RNA/DNA and lipids. Finally, the PI will evaluate the role of ammonia-oxidizing archaea in carbon fixation using in situ CO2 fixation experiments. These objectives will be achieved by using advanced molecular approaches and innovative chemical tracer studies (hydrogen isotopes of archaeal biomarkers and 13C-labeling of carbon substrates). The major phylogenetic and functional groups of archaea will be characterized using standard protocols for DNA/RNA extraction, amplification, cloning, and sequencing. Statistical analysis will be employed to link differences in aqueous geochemistry, lipid biomarkers, and predominant 16S rRNA or functional gene phylogenies among springs with diverse lipid profiles.
The crenarchaeol isomer is an important part of a paleothermometer (TEX86) based on tetraether lipids. Thus, understanding the source and distribution of crenarchaeol and its isomers has evolutionary implications and contributes to a better understanding of how this molecule's distribution relates to paleotemperature. This project will be closely linked to studies of geothermal features in China and will coordinate efforts with colleagues who are actively doing archaeal research in Yellowstone National Park and other countries to promote the establishment of an archaeal research network on phylogeny, biogeography and ecological functions of archaea in terrestrial hot springs. In addition to training undergraduate and graduate students, Zhang will bring high school teachers and students to the field each year and incorporate this research into his community seminars on life in extreme environments in Augusta, GA, which has interested both children and adults.
PUBLICATIONS PRODUCED AS A RESULT OF THIS RESEARCH
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PROJECT OUTCOMES REPORT
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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.
The initial report on the presence of GDGTs (crenarchaeol in particular) in terrestrial hot springs was published 10 years ago (Pearson et al., 2004). It was soon followed by a number of reports that focused on specific geothermal environments with the goal to correlate the composition and abundance of GDGTs with individual ecosystem variables (e.g., pH, temperature, dissolved oxygen, nutrients, microbial community composition). This research included a great diversity of terrestrial hot springs and their immediate soil environments and provided valuable insights into the dynamic interactions between environmental and biological variables affecting the distribution of GDGTs in these environments. Integrating the data from hot springs located in Yellowstone, the Great Basin, Kamchataka, and Tengchong (ranging in temperature from less than 40°C to 85°C and in pH from ~2.0 to 9.2) facilitated the following observations: 1) the major GDGTs (iGDGTs and bGDGTs) that were initially observed in marine or soil environments can form in situ in hot springs, 2) pH is the primary factor affecting the composition of GDGTs in global hot spring environments while growth temperature plays a secondary role, and 3) the composition of GDGTs is strongly linked to the composition of microbial communities in hot springs indicating their integral role in adaptation to physicochemical gradients. These results might help us to better evaluate GDGT-based indices as proxies for the characterization of marine or lacustrine aquatic environments or terrestrial soils. Furthermore, the ubiquity of GDGTs in terrestrial hot springs has stimulated research addressing whether some of the GDGTs have a thermophilic origin.
References
Pearson, A., et al. 2004. Non-marine crenarchaeol in Nevada hot springs. Appl. Environ. Microbiol. 70:52...
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