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Carbon isotope evidence for the global physiology of Proterozoic cyanobacteria.

ABSTRACT: Ancestral cyanobacteria are assumed to be prominent primary producers after the Great Oxidation Event [?2.4 to 2.0 billion years (Ga) ago], but carbon isotope fractionation by extant marine cyanobacteria (?-cyanobacteria) is inconsistent with isotopic records of carbon fixation by primary producers in the mid-Proterozoic eon (1.8 to 1.0 Ga ago). To resolve this disagreement, we quantified carbon isotope fractionation by a wild-type planktic ?-cyanobacterium (Synechococcus sp. PCC 7002), an engineered Proterozoic analog lacking a CO₂-concentrating mechanism, and cyanobacterial mats. At mid-Proterozoic pH and pCO₂ values, carbon isotope fractionation by the wild-type ?-cyanobacterium is fully consistent with the Proterozoic carbon isotope record, suggesting that cyanobacteria with CO₂-concentrating mechanisms were apparently the major primary producers in the pelagic Proterozoic ocean, despite atmospheric CO₂ levels up to 100 times modern. The selectively permeable microcompartments central to cyanobacterial CO₂-concentrating mechanisms ("carboxysomes") likely emerged to shield rubisco from O₂ during the Great Oxidation Event.

SUBMITTER: Hurley SJ

PROVIDER: S-EPMC7787495 | biostudies-literature | 2021 Jan

REPOSITORIES: biostudies-literature

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Carbon isotope evidence for the global physiology of Proterozoic cyanobacteria.

Hurley Sarah J SJ Wing Boswell A BA Jasper Claire E CE Hill Nicholas C NC Cameron Jeffrey C JC

Science advances 20210106 2

Ancestral cyanobacteria are assumed to be prominent primary producers after the Great Oxidation Event [≈2.4 to 2.0 billion years (Ga) ago], but carbon isotope fractionation by extant marine cyanobacteria (α-cyanobacteria) is inconsistent with isotopic records of carbon fixation by primary producers in the mid-Proterozoic eon (1.8 to 1.0 Ga ago). To resolve this disagreement, we quantified carbon isotope fractionation by a wild-type planktic β-cyanobacterium (<i>Synechococcus</i> sp. PCC 7002), a ...[more]

PMID: 33523966

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Project description:Marine nitrogen fixation is a major source of new nitrogen to the ocean, which interacts with climate driven changes to physical nutrient supply to regulate the response of ocean primary production in the oligotrophic tropical ocean. Warming and changes in nutrient supply may alter the ecological niche of nitrogen-fixing organisms, or 'diazotrophs', however, impacts of warming on diazotroph physiology may also be important. Lab-based studies reveal that warming increases the nitrogen fixation-specific elemental use efficiency (EUE) of two prevalent marine diazotrophs, Crocosphaera and Trichodesmium, thus reducing their requirements for the limiting nutrients iron and phosphorus. Here, we coupled a new diazotroph model based upon observed diazotroph energetics of growth and resource limitation to a state-of-the-art global model of phytoplankton physiology and ocean biogeochemistry. Our model is able to address the integrated response of nitrogen fixation by Trichodesmium and Crocosphaera to warming under the IPCC high emission RCP8.5 scenario for the first time. Our results project a global decline in nitrogen fixation over the coming century. However, the regional response of nitrogen fixation to climate change is modulated by the diazotroph-specific thermal performance curves and EUE, particularly in the Pacific Ocean, which shapes global trends. Spatially, the response of both diazotrophs is similar with expansion towards higher latitudes and reduced rates of nitrogen fixation in the lower latitudes. Overall, 95%-97% of the nitrogen fixation climate signal can be attributed to the combined effect of temperature on the niche and physiology of marine diazotrophs, with decreases being associated with a reduced niche and increases resulting due to a combination of expanding niche and temperature driven changes to EUE. Climate change impacts on both the niche and physiology of marine diazotrophs interact to shape patterns of marine nitrogen fixation, which will have important implications for ocean productivity in the future.

Dataset Information

Carbon isotope evidence for the global physiology of Proterozoic cyanobacteria.

Publications

Carbon isotope evidence for the global physiology of Proterozoic cyanobacteria.

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