Previous Article |
Table of Contents
| Next Article
* Department of Geology and Geophysics, Yale University, New Haven,
CT 06520-8109; Edited by Karl K. Turekian, Yale University, New Haven, CT, and
approved December 29, 2000 (received for review October 29, 2000)
The distinctive relations between biological activity and isotopic
effect recorded in biomarkers (e.g., carbon and sulfur isotope ratios)
have allowed scientists to suggest that life originated on this planet
nearly 3.8 billion years ago. The existence of life on other planets
may be similarly identified by geochemical biomarkers, including the
oxygen isotope ratio of phosphate (
Special Feature
Geology
Oxygen isotope ratios of PO4: An inorganic indicator
of enzymatic activity and P metabolism and a new biomarker in the
search for life
,
, and
Department of Geology, University of
Michigan, Ann Arbor, MI 48109; and § Department of
Geology, Amherst College, Amherst, MA 01002
18Op)
presented here. At low near-surface temperatures, the exchange of
oxygen isotopes between phosphate and water requires enzymatic catalysis. Because enzymes are indicative of cellular activity, the
demonstration of enzyme-catalyzed PO4-H2O
exchange is indicative of the presence of life. Results of laboratory
experiments are presented that clearly show that
18OP values of inorganic phosphate can be
used to detect enzymatic activity and microbial metabolism of
phosphate. Applications of
18Op as a
biomarker are presented for two Earth environments relevant to the
search for extraterrestrial life: a shallow groundwater reservoir and a
marine hydrothermal vent system. With the development of in
situ analytical techniques and future planned sample return strategies,
18Op may provide an important
biosignature of the presence of life in extraterrestrial systems such
as that on Mars.
To whom reprint requests should be addressed. E-mail:
blake{at}geology.yale.edu
www.pnas.org/cgi/doi/10.1073/pnas.051515898
![]()
CiteULike
Complore
Connotea
Del.icio.us
Digg What's this?
This article has been cited by other articles in HighWire Press-hosted journals:
![]() |
A. S. Colman, R. E. Blake, D. M. Karl, M. L. Fogel, and K. K. Turekian Marine phosphate oxygen isotopes and organic matter remineralization in the oceans PNAS, September 13, 2005; 102(37): 13023 - 13028. [Abstract] [Full Text] [PDF] |
||||