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Vegetation development and carbon storage on a glacier foreland in the High Arctic, Ny-Ålesund, Svalbard
Authors:Shinpei Yoshitake  Masaki Uchida  Toshiyuki Ohtsuka  Hiroshi Kanda  Hiroshi Koizumi  Takayuki Nakatsubo
Institution:aFaculty of Science and Engineering, Waseda University, 2-2, Wakamatsucho, Shinjuku-ku, Tokyo 162-8480, Japan;bNational Institute of Polar Research, 10-3, Midoricho, Tachikawa, Tokyo 190-8518, Japan;cRiver Basin Research Center, Gifu University, 1-1,Yanagido, Gifu 501-1193, Japan;dFaculty of Education and Integrated Arts and Sciences, Waseda University, 2-2, Wakamatsucho, Shinjuku-ku, Tokyo 162-8480, Japan;eGraduate School of Biosphere Science, Hiroshima University, 1-7-1, Kagamiyama, Higashi-Hiroshima 739-8521, Japan
Abstract:The distribution of organic carbon and its relationship to vegetation development were examined on a glacier foreland near Ny-Ålesund, Svalbard (79°N). In a 0.72-km2 area, we established 43 study plots on three line transects along primary succession from recently deglaciated area to old well-vegetated area. At each plot, we measured the type and percent coverage of vegetation types. The organic carbon content of vegetation, organic soil, and mineral soil samples was determined based on their organic carbon concentration and bulk density. Cluster analysis based on vegetation coverage revealed five types of ground surfaces representing variations in the amounts and allocation patterns of organic carbon. In the later stages of succession, 7%–24% and 31%–40% of organic carbon was contained in the organic and deeper soil layers, respectively. Organic carbon storage in the later stages of succession ranged from 1.1 – 7.9 kg C m−2. A larger amount of organic carbon, including ancient carbon in a raised beach deposit, was expected to be contained in much deeper soil layers. These results suggest that both vegetation development and geological history affect ecosystem carbon storage and that a non-negligible amount of organic carbon is distributed in this High Arctic glacier foreland.
Keywords:Carbon storage  High arctic glacier foreland  Succession  Svalbard  Vegetation
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