SREL Reprint #2958
Thermophilic Temperature Optimum for Crenarchaeol Synthesis and Its Implication for Archaeal Evolution


Chuanlun L. Zhang,1* Ann Pearson,2 Yi-Liang Li,1† Gary Mills,1 and Juergen Wiegel3

Savannah River Ecology Laboratory, University of Georgia, Aiken, South Carolina 298021
Department of Earth and Planetary Sciences, Harvard University, Cambridge, Massachusetts 021382
Department of Microbiology, University of Georgia, Athens, Georgia 306053



Abstract
The isoprenoid lipid crenarchaeol is widespread in hot springs of California and Nevada. Terrestrial and marine data together suggest a maximum relative abundance of crenarchaeol at 40°C. This warm temperature optimum may have facilitated colonization of the ocean by (hyper)thermophilic Archaea and the major marine radiation of Crenarchaeota.

 

Keywords: Ambystoma opacum, catastrophic reproductive failure, extinction, larval density dependence, pond-breeding salamander, population model, storage effects, terrestrial survival

 

* Corresponding author. Mailing address: Savannah River Ecology Laboratory, University of Georgia, Aiken, SC 29802. Phone: (803) 725-5299. Fax: (803) 725-3309. E-mail: zhang@srel.edu

†Present address: Center for Biomarker Analysis, University of Tennessee, Knoxville, TN 37932-2575.

 

SREL Reprint #2958

 

Zhang, C. L., A. Pearson, Y. Li, G. Mills, J. Wiegel. 2006. Thermophilic Temperature Optimum for Crenarchaeol Synthesis and Its Implication for Archaeal Evolution. Appl. Environ. Microbiol. 72(6): 4419-4422.

 

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