Vegetation structure in gullies developed by the melting of ice wedges along Kolyma River, northern Siberia

• Published in: Ecological Research
• Main Authors: Tsuyuzaki, Shiro, Ishizaki, Takeshi, Sato, Toshiyuki
• Format: Article in Journal/Newspaper
• Language: English
• Published: Wiley 1999
• Subjects: Kolyma; The Gully; kolyma river; Siberia
• Online Access: http://dx.doi.org/10.1046/j.1440-1703.1999.00316.x; https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1046%2Fj.1440-1703.1999.00316.x; http://onlinelibrary.wiley.com/wol1/doi/10.1046/j.1440-1703.1999.00316.x/fullpdf

Vegetation structure was surveyed in gullies developed by the melting of ice wedges along the Kolyma River, northern Siberia, using 72 50 × 50 cm plots. The mean total plant cover was approximately 50% on gley soils, which were only distributed in the gullies. Based on TWINSPAN cluster analysis, four vegetation types were recognized: (i) Agrostis purpurascens grassland with Ceratodon purpureus moss carpet; (ii) Matricaria matricarioides forbland; (iii) Chamaenerium angustifolium and M. matricarioides forbland; and (iv) Descurainia sophia grassland. Species that produce seeds capable of long‐distance dispersal established well. Of the environmental factors surveyed, the gully scales (height and width) and elevational difference within a plot were primarily related to the vegetation development. The gully height was correlated with soil pH and compaction that might be related to intensities of ground surface disturbances. Agrostis purpurascens established in large gullies, while Equisetum arvense and Salix alaxensis established in small gullies. Soil compaction was also related to the vegetation establishment patterns (e.g. Rumex sibirica did not establish on hard soils). We concluded that the gully scales primarily determine soil conditions, including ground surface instability as a function of slope and soil compaction, and subsequent community structure.