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Division of Geological and Planetary Sciences, California Institute of Technology and the Howard Hughes Medical Institute Pasadena, California, 91125, U.S.A., dkn@gps.caltech.edu
Department of Microbiology and The BioTechnology Institute, University of Minnesota, St. Paul, Minnesota, 55108, U.S.A., gralnick@umn.edu
| The first 20% of the full text of this article appears below. |
| INTRODUCTION |
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As for the players of "Clue," scientists seeking to understand the co-evolution of life and Earth are often confronted with the dilemma of having to parse multiple solutions to an ancient biogeochemical event. For example, in trying to explain the genesis of Archean Banded Iron Formations, we must ask whether it was cyanobacteria in the near shore-environment producing O2, or anoxygenic phototrophs in the oceans directly oxidizing iron (Kappler et al. 2005)? Again, in parallel to "Clue," typically all we have to work with are isolated scraps of evidencemetamorphosed pieces of rock collected from remote locales on Earth, that contain morphological and/or chemical fossils whose origin and/or meaning is enigmatic. Nevertheless, the legacies of billions of years of evolutiongenetic rolls of the dice, subject to natural selectionprovide us with a means to interpret these putative biosignatures. By applying the principle of uniformitarianism, we assume that the study of modern organisms can provide us with insights into the composition and behavior of their ancient relatives, thereby allowing us to reconstruct ancient events. This, of course, is a necessary assumption that may not be true, so in the end, all we can really claim is to
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