Photosynthesis Research

, Volume 88, Issue 2, pp 109–117

Photosynthesis in the Archean Era

Authors

    • Department of Biochemistry and Molecular Biology, 913 Lederle GRT Tower-BUniversity of Massachusetts Amherst
Minireview

DOI: 10.1007/s11120-006-9040-5

Cite this article as:
Olson, J.M. Photosynth Res (2006) 88: 109. doi:10.1007/s11120-006-9040-5

Abstract

The earliest reductant for photosynthesis may have been H2. The carbon isotope composition measured in graphite from the 3.8-Ga Isua Supercrustal Belt in Greenland is attributed to H2-driven photosynthesis, rather than to oxygenic photosynthesis as there would have been no evolutionary pressure for oxygenic photosynthesis in the presence of H2. Anoxygenic photosynthesis may also be responsible for the filamentous mats found in the 3.4-Ga Buck Reef Chert in South Africa. Another early reductant was probably H2S. Eventually the supply of H2 in the atmosphere was likely to have been attenuated by the production of CH4 by methanogens, and the supply of H2S was likely to have been restricted to special environments near volcanos. Evaporites, possible stromatolites, and possible microfossils found in the 3.5-Ga Warrawoona Megasequence in Australia are attributed to sulfur-driven photosynthesis. Proteobacteria and protocyanobacteria are assumed to have evolved to use ferrous iron as reductant sometime around 3.0 Ga or earlier. This type of photosynthesis could have produced banded iron formations similar to those produced by oxygenic photosynthesis. Microfossils, stromatolites, and chemical biomarkers in Australia and South Africa show that cyanobacteria containing chlorophyll a and carrying out oxygenic photosynthesis appeared by 2.8 Ga, but the oxygen level in the atmosphere did not begin to increase until about 2.3 Ga.

Keywords

anoxygenic photosynthesisbacteriochlorophyllbanded iron formationBuck Reef Chertchemical biomarkerschlorophyllcyanobacteriaFortesque Groupevaporitesferrous ironhydrogenisotope fractionationIsua Supercrustal Beltmicrofossilsoxygenic photosynthesisproteobacteriareaction centerreductants for CO2 fixationstromatolitesSwaziland SequenceWarrawoona Megasequence

Abbreviations

Bchl

bacteriochlorophyll

BIF

banded iron formation

Chl

chlorophyll

Ga

billion years

PDB

Peedee belemnite standard

RC

reaction center

Rubisco

ribulose bisphosphate carboxylase

WM

Warrawoona Megasequence

Copyright information

© Springer Science+Business Media, Inc. 2006