2009
DOI: 10.1111/j.1462-2920.2008.01830.x
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Isotopic evidence for the provenance and turnover of organic carbon by soil microorganisms in the Antarctic dry valleys

Abstract: SummaryThe extremely cold and arid Antarctic dry valleys are one of the most environmentally harsh terrestrial ecosystems supporting organisms in which the biogeochemical transformations of carbon are exclusively driven by microorganisms. The natural abundance of 13 C and 15 N in source organic materials and soils have been examined to obtain evidence for the provenance of the soil organic matter and the C loss as CO2 during extended incubation (approximately 1200 days at 10°C under moist conditions) has been … Show more

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Cited by 64 publications
(82 citation statements)
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References 71 publications
(121 reference statements)
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“…Therefore, we propose that they act as a reservoir for terrestrial microbiota. This notion is supported by recent isotopic evidence indicating that some organic matter in Dry Valleys soils remote from sources of liquid water has an endolithic origin (36). Weathering of sandstone is accelerated by endolithic colonization (10), and therefore, can be envisaged to disperse endolithic taxa, although in a relatively slow manner.…”
Section: Discussionmentioning
confidence: 82%
“…Therefore, we propose that they act as a reservoir for terrestrial microbiota. This notion is supported by recent isotopic evidence indicating that some organic matter in Dry Valleys soils remote from sources of liquid water has an endolithic origin (36). Weathering of sandstone is accelerated by endolithic colonization (10), and therefore, can be envisaged to disperse endolithic taxa, although in a relatively slow manner.…”
Section: Discussionmentioning
confidence: 82%
“…We further propose expansion and extension of isotope approaches, which have been used in both High Arctic and Antarctic environments previously (Hopkins et al 2009;Lyons et al 2013), in order to shed light on the biogeochemical responses of Arctic and Antarctic cyanobacteria. Simulation studies, testing how changes in atmospheric CO 2 and temperature affect cyanobacterial populations, would help us to understand how these phyla may evolve in situ.…”
Section: Discussionmentioning
confidence: 99%
“…However, studies on the role of this large bacterial community in biogeochemical cycles are necessary to determine which of these microorganisms are really active in this extreme environment. In a recent report, Hopkins et al (2009) described evidence of a contribution of microorganisms to organic carbon turnover in the soil in Antarctic dry valleys, which make up one of the most environmentally harsh terrestrial ecosystems. Such information is essential to help us predict the possible consequences of microbial disturbances and their consequent impacts on biogeochemical transformations in Antarctic ecosystems.…”
Section: Discussionmentioning
confidence: 99%