The photosynthesizing cyanobacteria can be found in a wide range of environments including rivers, soils, lakes, and shallow shelves. We also note that hydrogen-based anoxygenic photosynthesis would take up H2 and CO2, thereby reducing the local concentration of gases needed to form bubbles. We collected pieces of 2.72-billion-year-old stromatolites from the pre-oxygen world by drilling into an ancient reefs in the Outback of Australia. Click to Shop ourfossils, minerals, educational materials! This was tantalizing, but we wanted more proof: a modern analog to help prove our arsenic theory. In 2014, our team found the first clue that stromatolites were produced by arsenic-assisted photosynthesis and respiration. The process of photosynthesis uses Gas-bubble entrapment has been suggested as the origin of axial porosity in the central zone of some Proterozoic stromatolites (13). This picture shows modern stromatolites (columns and mounds) in Shark The COVID crisis has cut advertising rates in half, and we need your help. Make a one-time contribution to Raw Story Investigates, or click here to become a subscriber. Triassic, Paleozoic Era evolved yet). They needed another chemical to do this. Morphogenesis of modern cone-forming cyanobacteriala The antiquity of oxygenic photosynthesis: Evidence from stromatolites in sulphate-deficient Archaean lakes, A reconstruction of Archean biological diversity based on molecular fossils from the 2.78 to 2.45 billion-year-old Mount Bruce Supergroup, Hamersley Basin, Western Australia, The paleoproterozoic snowball Earth: A climate disaster triggered by the evolution of oxygenic photosynthesis, Reassessing the first appearance of eukaryotes and cyanobacteria, Late Archean molecular fossils from the Transvaal Supergroup record the antiquity of microbial diversity and aerobiosis, Methylhopane biomarker hydrocarbons in Hamersley Province sediments provide evidence for Neoarchean aerobiosis, Late Archean rise of aerobic microbial ecosystems, Atmospheric influence of Earth's earliest sulfur cycle, Stromatolite reef from the Early Archaean era of Australia, A case for biotic morphogenesis of coniform stromatolites, Microbial biofacies in hot-spring sinters: A model based on Ohaaki Pool, North Island, New Zealand, Methane bubbles in Lake Kinneret: Quantification and temporal and spatial heterogeneity, Hydrocarbon seep and hydrothermal vent paleoenvironments and paleontology: Past developments and future research directions, Precambrian marine carbonate isotope database: Version 1.1, Inhibition of methanogens increases photo-dependent nitrogenase activities in anoxic paddy soil amended with rice straw, Stromatolites from the Paleoproterozoic Earaheedy Group, Earaheady Basin, Western Australia, Biostratigraphic Studies of Stromatolites from the Proterozoic Earaheedy Group, Naberru Basin, Western Australia, Microfossils in Conophyton from the Soviet Union and their bearing on Precambrian biostratigraphy, Archean stromatolites from Abitibi greenstone belt, Quebec, Canada, Archean stromatolites in Michipicoten Group siderite ore at Wawa, Ontario, The Pilbara Drilling Project: c. 2.72 Ga Tumbiana Formation and c. 3.49 Ga Dresser Formation Pilbara Craton, Western Australia, Facies relations, depositional environments and diagenesis in a major early Proterozoic stromatolitic carbonate platform to basinal sequence, Campbellrand subgroup, Transvaal Supergroup, Southern Africa, Accretion, Trapping and binding of sediment in Archean stromatolites—Morphological expression of the antiquity of life, Molecular diversity of cyanobacteria inhabiting coniform structures and surrounding mat in a Yellowstone hot spring, Uncultivated cyanobacteria, Chloroflexus-like inhabitants, and spirochete-like inhabitants of a hot spring microbial mat, An oxygen microsensor with a guard cathode, Diffusive boundary layers and the oxygen uptake of sediments and detritus, Effect of oxygen concentration on photosynthesis and respiration in two hypersaline microbial mats, Photosynthesis of benthic microflora measured with high spatial resolution by the oxygen microprofile method: Capabilities and limitations of the method, Primary production of microalgae in sediments measured by oxygen microprofile, H, 3.43 billion-year-old stromatolite reef from the Pilbara Craton of Western Australia: Ecosystem-scale insights to early life on Earth, Origin of 3.45 Ga coniform stromatolites in Warrawoona Group, Western Australia, Stromatolites 3,400-Myr old from the Archean of Western Australia, Environmental control on diverse stromatolite morphologies in the 3000 Myr Pongola Supergroup, South Africa, Evolution of Archean Supracrustal Sequences, Special Paper, Archaean stromatolites from the Steep Rock Group, northwestern Ontario, Canada, Archaean quartz arenites in the Canadian Shield: Examples from the Superior and Churchill Provinces, Facies architecture and sequence-stratigraphic features of the Tumbiana Formation in the Pilbara Craton, northwestern Australia: Implications for depositional environments of oxygenic stromatolites during the Late Archean, Annual Report of Geological Survey of Western Australia, Small conical stromatolites from the Archean near Kanowna, Western Australia, Geological Survey of Western Australia, Perth, Archean shelf-facies and stromatolites proliferation in Dharwar supergoup, North Karnataka, District Karnataka, Archaean stromatolites from the Ngesi Group, Belingwe greenstone belt, Zimbabwe; 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