Life and the Evolution of Earth's Atmosphere

Author:

Kasting James F.1,Siefert Janet L.2

Affiliation:

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.

Abstract

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.

Publisher

American Association for the Advancement of Science (AAAS)

Subject

Multidisciplinary

Reference23 articles.

1. The relative influences of nitrogen and phosphorus on oceanic primary production

2. I. Berman-Frank et al. Science 294 1534 (2001).

3. H. D. Holland in Early Life on Earth S. Bengtson Ed. (Columbia Univ. Press New York 1994) pp. 237–244.

4. Atmospheric Influence of Earth's Earliest Sulfur Cycle

5. L. Margulis Symbiosis in Cell Evolution: Microbial Communities in the Archean and Proterozoic Eons (Freeman San Francisco ed. 2 1993) chap. 7 pp. 327–343.

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