Abstract
Previous descriptions of soils in the McMurdo Dry Valleys, Antarctica, have focused on the dominance of abiotic controls rather than on nutrient cycling. Although free-living N2-fixing and nitrifying microorganisms have been isolated in Antarctic soils, little is known about in situ nitrogen (N) cycling. We measured KCl-extractable NH4 + and NO3 –, as well as anion resin exchangeable NO3 –, across sediment–soil transects and in two positions on a hill slope in Taylor Valley, Antarctica. These landscapes provide gradients of soil moisture, salinity, and texture that influence invertebrate communities and organic matter dynamics. Assuming an N cycle dominated by abiotic inputs, we hypothesized that inorganic N content would be predominantly comprised of NO3 – and most strongly correlated to soil salinity, while NO3 – flux (estimated by resin adsorption) would be most influenced by soil water content, salinity, and total soil NO3 – concentrations. Our results were inconsistent with a physically dominated N cycle. In contrast to previous studies of Dry Valley soils, we found that NH4 + made up a large proportion of inorganic N. Total KCl-extractable N was correlated most strongly with total soil N and soil moisture. The most saline soils in the swale of a hill slope had the highest concentrations of NO3 –, but we found no overall correlation between soil salinity and resin-exchangeable NO3 – or KCl-extractable N. Resin-extractable NO3 – was most strongly correlated with total soil N, soil water content, and KCl-extractable NH4 +, suggesting that accumulation of NO3 – in resins was influenced by the mineralization of organic matter and not strictly by ionic migration, as an abiotic-based model may have predicted. We conclude that biological N cycling is significant in some Dry Valley soils and that the dominance of biological vs physical influences over N cycling is controlled in part by the availability of soil moisture and organic matter.
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Received 2 January 2001; accepted 30 October 2001.
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Barrett, J., Virginia, R. & Wall, D. Trends in Resin and KCl-extractable Soil Nitrogen Across Landscape Gradients in Taylor Valley, Antarctica. Ecosystems 5, 289–299 (2002). https://doi.org/10.1007/s10021-001-0072-6
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DOI: https://doi.org/10.1007/s10021-001-0072-6