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Published online on April 13, 2006, 10.1073/pnas.0510157103
PNAS | April 25, 2006 | vol. 103 | no. 17 | 6442-6447


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From the Cover
PHYSICAL SCIENCES / BIOLOGICAL SCIENCES / ENVIRONMENTAL SCIENCES / ECOLOGY
Quantifying archaeal community autotrophy in the mesopelagic ocean using natural radiocarbon

Anitra E. Ingalls*,{dagger},{ddagger}, Sunita R. Shah*,{dagger}, Roberta L. Hansman§, Lihini I. Aluwihare§, Guaciara M. Santos, Ellen R. M. Druffel, and Ann Pearson*,||

*Department of Earth and Planetary Sciences, Harvard University, Cambridge, MA 02138; §Scripps Institution of Oceanography, University of California at San Diego, La Jolla, CA 92093; and Department of Earth System Science, University of California, Irvine, CA 92697

Edited by John M. Hayes, Woods Hole Oceanographic Institution, Woods Hole, MA, and approved March 3, 2006 (received for review November 23, 2005)

An ammonia-oxidizing, carbon-fixing archaeon, Candidatus "Nitrosopumilus maritimus," recently was isolated from a salt-water aquarium, definitively confirming that chemoautotrophy exists among the marine archaea. However, in other incubation studies, pelagic archaea also were capable of using organic carbon. It has remained unknown what fraction of the total marine archaeal community is autotrophic in situ. If archaea live primarily as autotrophs in the natural environment, a large ammonia-oxidizing population would play a significant role in marine nitrification. Here we use the natural distribution of radiocarbon in archaeal membrane lipids to quantify the bulk carbon metabolism of archaea at two depths in the subtropical North Pacific gyre. Our compound-specific radiocarbon data show that the archaea in surface waters incorporate modern carbon into their membrane lipids, and archaea at 670 m incorporate carbon that is slightly more isotopically enriched than inorganic carbon at the same depth. An isotopic mass balance model shows that the dominant metabolism at depth indeed is autotrophy (83%), whereas heterotrophic consumption of modern organic carbon accounts for the remainder of archaeal biomass. These results reflect the in situ production of the total community that produces tetraether lipids and are not subject to biases associated with incubation and/or culture experiments. The data suggest either that the marine archaeal community includes both autotrophs and heterotrophs or is a single population with a uniformly mixotrophic metabolism. The metabolic and phylogenetic diversity of the marine archaea warrants further exploration; these organisms may play a major role in the marine cycles of nitrogen and carbon.

biomarkers | carbon isotopes | microbial ecology | nitrogen cycle | oceanography


See Commentary on page 6417.

{dagger}A.E.I. and S.R.S. contributed equally to this work.

{ddagger}Present address: School of Oceanography, University of Washington, Seattle, WA 98195.

Author contributions: A.P. and L.I.A. designed research; A.E.I., S.R.S., R.L.H., and A.P. performed research; G.M.S. and E.R.M.D. contributed new reagents/analytic tools; A.E.I., S.R.S., L.I.A., G.M.S., and A.P. analyzed data; and A.E.I., S.R.S., L.I.A., and A.P. wrote the paper.

Conflict of interest statement: No conflicts declared.

This paper was submitted directly (Track II) to the PNAS office.

||To whom correspondence should be addressed. E-mail: pearson{at}eps.harvard.edu

© 2006 by The National Academy of Sciences of the USA


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