Microsite conditions in retrogressive thaw slumps may facilitate increased seedling recruitment in the Alaskan Low Arctic

In Low Arctic tundra, thermal erosion of ice‐rich permafrost soils (thermokarst) has increased in frequency since the 1980s. Retrogressive thaw slumps (RTS) are thermokarst disturbances forming large open depressions on hillslopes through soil wasting and vegetation displacement. Tall (>0.5 m) de...

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Detalles Bibliográficos
Autores principales: Huebner, Diane Christine, Bret‐Harte, Marion Syndonia
Formato: Online Artículo Texto
Lenguaje:English
Publicado: John Wiley and Sons Inc. 2019
Materias:
Original Research
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6392365/
https://www.ncbi.nlm.nih.gov/pubmed/30847079
http://dx.doi.org/10.1002/ece3.4882

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6392365/
https://www.ncbi.nlm.nih.gov/pubmed/30847079
http://dx.doi.org/10.1002/ece3.4882

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