SOIL INSTABILITY IN TUNDRA VEGETATION*
Movement of the substratum and thawing of perennially frozen ground are of primary importance in northern latitudes in controlling the microdistribution of tundra vegetation. In middle latitudes, however, soil movement receives only minor attention in studies of vegetation, except in specialized hab...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.607.354 2023-05-15T14:56:05+02:00 SOIL INSTABILITY IN TUNDRA VEGETATION* Sigafoos R. S Knowledge Bank Kb. Osu. Edu R. S. Sigafoos The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.607.354 en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.607.354 Metadata may be used without restrictions as long as the oai identifier remains attached to it. https://kb.osu.edu/dspace/bitstream/handle/1811/3870/V51N06_281.pdf;jsessionid=FCFB861D7A483CD9B32136AB82DEC97A?sequence=1 Four types of topography are represented on the Seward Peninsula coastal plain dissected uplands text ftciteseerx 2016-01-08T14:19:13Z Movement of the substratum and thawing of perennially frozen ground are of primary importance in northern latitudes in controlling the microdistribution of tundra vegetation. In middle latitudes, however, soil movement receives only minor attention in studies of vegetation, except in specialized habitats. Griggs (1934, pp. 168-170) drew an analogy between vegetation of rocky arctic slopes and weeds of plowed fields of temperate regions. Raup (1947, p. 50) classified the vegetation of the Brintnell Lake region and Polunin (1934, p. 346) classified the vegetation of Akpatok Island according to habitat, rather than according to recognized ecological schemes. Polunin (1935, pp. 192-194) stated that soil movement on Akpatok Island in eastern arctic Canada has retarded the develop-ment of the vegetation since the island was freed of continental ice. Thawing of perennially frozen ground under existing climates is unique to regions of high latitudes where it has a profound effect upon local water tables, thus upon vegetation. The effects of unstable soils upon vegetation were studied on Seward Peninsula Text Arctic Seward Peninsula Tundra Unknown Akpatok Island ENVELOPE(-68.131,-68.131,60.417,60.417) Arctic Brintnell Lake ENVELOPE(-114.717,-114.717,55.800,55.800) Canada Freed ENVELOPE(164.333,164.333,-71.483,-71.483) |
institution |
Open Polar |
collection |
Unknown |
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ftciteseerx |
language |
English |
topic |
Four types of topography are represented on the Seward Peninsula coastal plain dissected uplands |
spellingShingle |
Four types of topography are represented on the Seward Peninsula coastal plain dissected uplands Sigafoos R. S Knowledge Bank Kb. Osu. Edu R. S. Sigafoos SOIL INSTABILITY IN TUNDRA VEGETATION* |
topic_facet |
Four types of topography are represented on the Seward Peninsula coastal plain dissected uplands |
description |
Movement of the substratum and thawing of perennially frozen ground are of primary importance in northern latitudes in controlling the microdistribution of tundra vegetation. In middle latitudes, however, soil movement receives only minor attention in studies of vegetation, except in specialized habitats. Griggs (1934, pp. 168-170) drew an analogy between vegetation of rocky arctic slopes and weeds of plowed fields of temperate regions. Raup (1947, p. 50) classified the vegetation of the Brintnell Lake region and Polunin (1934, p. 346) classified the vegetation of Akpatok Island according to habitat, rather than according to recognized ecological schemes. Polunin (1935, pp. 192-194) stated that soil movement on Akpatok Island in eastern arctic Canada has retarded the develop-ment of the vegetation since the island was freed of continental ice. Thawing of perennially frozen ground under existing climates is unique to regions of high latitudes where it has a profound effect upon local water tables, thus upon vegetation. The effects of unstable soils upon vegetation were studied on Seward Peninsula |
author2 |
The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
Sigafoos R. S Knowledge Bank Kb. Osu. Edu R. S. Sigafoos |
author_facet |
Sigafoos R. S Knowledge Bank Kb. Osu. Edu R. S. Sigafoos |
author_sort |
Sigafoos R. S |
title |
SOIL INSTABILITY IN TUNDRA VEGETATION* |
title_short |
SOIL INSTABILITY IN TUNDRA VEGETATION* |
title_full |
SOIL INSTABILITY IN TUNDRA VEGETATION* |
title_fullStr |
SOIL INSTABILITY IN TUNDRA VEGETATION* |
title_full_unstemmed |
SOIL INSTABILITY IN TUNDRA VEGETATION* |
title_sort |
soil instability in tundra vegetation* |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.607.354 |
long_lat |
ENVELOPE(-68.131,-68.131,60.417,60.417) ENVELOPE(-114.717,-114.717,55.800,55.800) ENVELOPE(164.333,164.333,-71.483,-71.483) |
geographic |
Akpatok Island Arctic Brintnell Lake Canada Freed |
geographic_facet |
Akpatok Island Arctic Brintnell Lake Canada Freed |
genre |
Arctic Seward Peninsula Tundra |
genre_facet |
Arctic Seward Peninsula Tundra |
op_source |
https://kb.osu.edu/dspace/bitstream/handle/1811/3870/V51N06_281.pdf;jsessionid=FCFB861D7A483CD9B32136AB82DEC97A?sequence=1 |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.607.354 |
op_rights |
Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
_version_ |
1766328126756880384 |