Note to users. If you're seeing this message, it means that your browser cannot find this page's style/presentation instructions -- or possibly that you are using a browser that does not support current Web standards. Find out more about why this message is appearing, and what you can do to make your experience of our site the best it can be.


Science 10 May 2002:
Vol. 296. no. 5570, pp. 1066 - 1068
DOI: 10.1126/science.1071184

Viewpoint

Life and the Evolution of Earth's Atmosphere

James F. Kasting,1* Janet L. Siefert2

Harvesting light to produce energy and oxygen (photosynthesis) is the signature of all land plants. This ability was co-opted from a precocious and ancient form of life known as cyanobacteria. Today these bacteria, as well as microscopic algae, supply oxygen to the atmosphere and churn out fixed nitrogen in Earth's vast oceans. Microorganisms may also have played a major role in atmosphere evolution before the rise of oxygen. Under the more dim light of a young sun cooler than today's, certain groups of anaerobic bacteria may have been pumping out large amounts of methane, thereby keeping the early climate warm and inviting. The evolution of Earth's atmosphere is linked tightly to the evolution of its biota.

1 Department of Geosciences, 443 Deike, The Pennsylvania State University, University Park, PA 16802, USA.
2 Department of Statistics, Rice University, Houston, TX 77251-1892, USA.
*   To whom correspondence should be addressed. E-mail: kasting{at}essc.psu.edu


Read the Full Text


THIS ARTICLE HAS BEEN CITED BY OTHER ARTICLES:
Evolutionary roots of iodine and thyroid hormones in cell-cell signaling.
S. J. Crockford (2009)
Integr. Comp. Biol. 49, 155-166
   Abstract »    Full Text »    PDF »
Mineral evolution.
R. M. Hazen, D. Papineau, W. Bleeker, R. T. Downs, J. M. Ferry, T. J. McCoy, D. A. Sverjensky, and H. Yang (2008)
American Mineralogist 93, 1693-1720
   Abstract »    Full Text »    PDF »
Syntrophic Growth on Formate: a New Microbial Niche in Anoxic Environments.
J. Dolfing, B. Jiang, A. M. Henstra, A. J. M. Stams, and C. M. Plugge (2008)
Appl. Envir. Microbiol. 74, 6126-6131
   Abstract »    Full Text »    PDF »
Methyl Sulfide Production by a Novel Carbon Monoxide Metabolism in Methanosarcina acetivorans.
J. J. Moran, C. H. House, J. M. Vrentas, and K. H. Freeman (2008)
Appl. Envir. Microbiol. 74, 540-542
   Abstract »    Full Text »    PDF »
A system's view of the evolution of life.
R. J.P Williams (2007)
J R Soc Interface 4, 1049-1070
   Abstract »    Full Text »    PDF »
Late Archean rise of aerobic microbial ecosystems.
J. L. Eigenbrode and K. H. Freeman (2006)
PNAS 103, 15759-15764
   Abstract »    Full Text »    PDF »
Cell evolution and Earth history: stasis and revolution.
T. Cavalier-Smith (2006)
Phil Trans R Soc B 361, 969-1006
   Abstract »    Full Text »    PDF »
Chemical and biological evolution of early Earth: Constraints from banded iron formations.
H. Ohmoto, Y. Watanabe, K. E. Yamaguchi, H. Naraoka, M. Haruna, T. Kakegawa, K.-i. Hayashi, and Y. Kato (2006)
Geological Society of America Memoirs 198, 291-331
   Abstract »    Full Text »    PDF »
The Enigmatic Planctomycetes May Hold a Key to the Origins of Methanogenesis and Methylotrophy.
L. Chistoserdova, C. Jenkins, M. G. Kalyuzhnaya, C. J. Marx, A. Lapidus, J. A. Vorholt, J. T. Staley, and M. E. Lidstrom (2004)
Mol. Biol. Evol. 21, 1234-1241
   Abstract »    Full Text »    PDF »
The Natural History of Nitrogen Fixation.
J. Raymond, J. L. Siefert, C. R. Staples, and R. E. Blankenship (2004)
Mol. Biol. Evol. 21, 541-554
   Abstract »    Full Text »    PDF »
The Interface Between the Biological and Inorganic Worlds: Iron-Sulfur Metalloclusters.
D. C. Rees and J. B. Howard (2003)
Science 300, 929-931
   Abstract »    Full Text »    PDF »
Geomicrobiology: How Molecular-Scale Interactions Underpin Biogeochemical Systems.
D. K. Newman and J. F. Banfield (2002)
Science 296, 1071-1077
   Abstract »    Full Text »    PDF »



To Advertise     Find Products


Science. ISSN 0036-8075 (print), 1095-9203 (online)