Abstract
Antarctica is not a single ecological model. Substantial differences in the temperature, precipitation (which combine to affect the available water) and radiation determine the distribution and the habit of primary producers that in turn structure the trophic. Because terrestrial primary production is operating at environmental extremes in some parts of Antarctica, particularly in continental Antarctica, the spatial and temporal subsidies to the terrestrial stock of organic carbon make proportionately larger contributions to contemporary carbon cycling.
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Acknowledgments
We are grateful to Antarctica New Zealand and the New Zealand Foundation for Research in Science and Technology, the Royal Society (of London), the Carnegie Trust for the Universities of Scotland, the UK Natural Environment Research Council, which supports the British Antarctic Survey, and the UK Biotechnology and Biological Sciences Research Council with supports Rothamsted Research.
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Hopkins, D.W., Newsham, K.K., Dungait, J.A.J. (2014). Primary Production and Links to Carbon Cycling in Antarctic Soils. In: Cowan, D. (eds) Antarctic Terrestrial Microbiology. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-45213-0_12
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DOI: https://doi.org/10.1007/978-3-642-45213-0_12
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