Morphological record of oxygenic photosynthesis in conical stromatolites

Conical stromatolites are thought to be robust indicators of the presence of photosynthetic and phototactic microbes in aquatic environments as early as 3.5 billion years ago. However, phototaxis alone cannot explain the ubiquity of disrupted, curled, and contorted laminae in the crests of many Meso...

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Veröffentlicht in:Proceedings of the National Academy of Sciences - PNAS 2009-07, Vol.106 (27), p.10939-10943
Hauptverfasser: Bosak, Tanja, Liang, Biqing, Sim, Min Sub, Petroff, Alexander P
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container_issue 27
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container_title Proceedings of the National Academy of Sciences - PNAS
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creator Bosak, Tanja
Liang, Biqing
Sim, Min Sub
Petroff, Alexander P
description Conical stromatolites are thought to be robust indicators of the presence of photosynthetic and phototactic microbes in aquatic environments as early as 3.5 billion years ago. However, phototaxis alone cannot explain the ubiquity of disrupted, curled, and contorted laminae in the crests of many Mesoproterozoic, Paleoproterozoic, and some Archean conical stromatolites. Here, we demonstrate that cyanobacterial production of oxygen in the tips of modern conical aggregates creates contorted laminae and submillimeter-to-millimeter-scale enmeshed bubbles. Similarly sized fossil bubbles and contorted laminae may be present only in the crestal zones of some conical stromatolites 2.7 billion years old or younger. This implies not only that cyanobacteria built Proterozoic conical stromatolites but also that fossil bubbles may constrain the timing of the evolution of oxygenic photosynthesis.
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subjects Aquatic ecosystems
Archaea - metabolism
Bacteria
Biofilms
Biological Sciences
Bubbles
Carbonates
Cyanobacteria
Fossils
Geologic Sediments - microbiology
Molecular evolution
Morphology
Oxygen
Oxygen - metabolism
Photosynthesis
Physical Sciences
Sediments
Stromatolites
title Morphological record of oxygenic photosynthesis in conical stromatolites
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