Applied and Environmental Microbiology, June 2006, p. 4419-4422, Vol. 72, No. 6
0099-2240/06/$08.00+0 doi:10.1128/AEM.00191-06
Copyright © 2006, American Society for Microbiology. All Rights Reserved.
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 29802,1
Department of Earth and Planetary Sciences, Harvard University, Cambridge, Massachusetts 02138,2
Department of Microbiology, University of Georgia, Athens, Georgia 306053
Received 24 January 2006/
Accepted 20 March 2006
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.
* 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{at}srel.edu.
Present address: Center for Biomarker Analysis, University of Tennessee, Knoxville, TN 37932-2575.
Applied and Environmental Microbiology, June 2006, p. 4419-4422, Vol. 72, No. 6
0099-2240/06/$08.00+0 doi:10.1128/AEM.00191-06
Copyright © 2006, American Society for Microbiology. All Rights Reserved.
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