Abstract

Active layer detachment slides of different age were examined in the Central part of Yamal peninsula (West Siberian Arctic) in the subzone of northern hypoarctic tundra. Plant communities on the shear surface, on displaced blocks with preserved but degrading initial tundra vegetation and on undisturbed surroundings were described. In the processes of recovery pioneer grass-dominated communities on relatively dry surfaces and Equisetum-dominated communities in wet cracks were replaced by Salix reptans-graminoid communities. Vegetation on displaced blocks also transformed to the similar communities. On the oldest completely recovered landslides Salix reptans–graminoid communities with thin moss stratum occur both on former shear surface and on washed out remnants of blocks. Ancient landslides are indicated by willow copses and mesophytic herbaceous communities.

Full Text
Paper version not known

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call

Disclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.