Stability and Fragility in Arctic Ecosystems

The conclusions reached in this paper, concerning the "Fragile Arctic" are the following: 1) Two definitions of ecological stability are in use, and it is essential to keep them separate and explicitly stated. "Type-l stability" is the condition of non-oscillation, or nearly non-...

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Published in:ARCTIC
Main Author: Dunbar, M.J.
Format: Article in Journal/Newspaper
Language:English
Published: The Arctic Institute of North America 1973
Subjects:
Online Access:https://journalhosting.ucalgary.ca/index.php/arctic/article/view/65966
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spelling ftunivcalgaryojs:oai:journalhosting.ucalgary.ca:article/65966 2023-05-15T14:19:19+02:00 Stability and Fragility in Arctic Ecosystems Dunbar, M.J. 1973-01-01 application/pdf https://journalhosting.ucalgary.ca/index.php/arctic/article/view/65966 eng eng The Arctic Institute of North America https://journalhosting.ucalgary.ca/index.php/arctic/article/view/65966/49880 https://journalhosting.ucalgary.ca/index.php/arctic/article/view/65966 ARCTIC; Vol. 26 No. 3 (1973): September: 177–268; 178-185 1923-1245 0004-0843 Active layer info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion article-commentary 1973 ftunivcalgaryojs 2022-03-22T21:22:54Z The conclusions reached in this paper, concerning the "Fragile Arctic" are the following: 1) Two definitions of ecological stability are in use, and it is essential to keep them separate and explicitly stated. "Type-l stability" is the condition of non-oscillation, or nearly non-oscillation and steady state found in certain tropical situations, the result of continued evolution toward greater economy of energy and involving high information content and low production/biomass ratio. This type of stability is highly vulnerable to serious perturbation, to which it cannot adapt. Such systems may thus be called "fragile" and they are found in the tropics and perhaps in certain parts of high latitude systems, such as lakes, subarctic forests and perhaps the tundra vegetation itself. "Type-2 stability" is the condition of ability to absorb serious perturbation and return to a stable state, usually the status quo ante. This involves system oscillation, smaller information content, higher production/biomass ratios, and lesser economy of energy use. This type is found in mid and high latitudes, in which the physical environment itself oscillates considerably. 2) In tundra environments, extreme ecosystem simplicity in the animal communities leads to extreme oscillation, and it is suggested that such oscillations can be tolerated only if the geographic scale is large, which it is in the Arctic. 3) "Thermokarst", or damage to tundra terrain by damage to, or removal of, the active layer, is a serious hazard which is well understood and can be easily avoided. It is upon this that the "fragile Arctic" reputation is founded. 4) Oil in arctic sea water constitutes a serious hazard, probably more serious than in warmer waters. Article in Journal/Newspaper Arctic Arctic Subarctic Thermokarst Tundra University of Calgary Journal Hosting Arctic ARCTIC 26 3
institution Open Polar
collection University of Calgary Journal Hosting
op_collection_id ftunivcalgaryojs
language English
topic Active layer
spellingShingle Active layer
Dunbar, M.J.
Stability and Fragility in Arctic Ecosystems
topic_facet Active layer
description The conclusions reached in this paper, concerning the "Fragile Arctic" are the following: 1) Two definitions of ecological stability are in use, and it is essential to keep them separate and explicitly stated. "Type-l stability" is the condition of non-oscillation, or nearly non-oscillation and steady state found in certain tropical situations, the result of continued evolution toward greater economy of energy and involving high information content and low production/biomass ratio. This type of stability is highly vulnerable to serious perturbation, to which it cannot adapt. Such systems may thus be called "fragile" and they are found in the tropics and perhaps in certain parts of high latitude systems, such as lakes, subarctic forests and perhaps the tundra vegetation itself. "Type-2 stability" is the condition of ability to absorb serious perturbation and return to a stable state, usually the status quo ante. This involves system oscillation, smaller information content, higher production/biomass ratios, and lesser economy of energy use. This type is found in mid and high latitudes, in which the physical environment itself oscillates considerably. 2) In tundra environments, extreme ecosystem simplicity in the animal communities leads to extreme oscillation, and it is suggested that such oscillations can be tolerated only if the geographic scale is large, which it is in the Arctic. 3) "Thermokarst", or damage to tundra terrain by damage to, or removal of, the active layer, is a serious hazard which is well understood and can be easily avoided. It is upon this that the "fragile Arctic" reputation is founded. 4) Oil in arctic sea water constitutes a serious hazard, probably more serious than in warmer waters.
format Article in Journal/Newspaper
author Dunbar, M.J.
author_facet Dunbar, M.J.
author_sort Dunbar, M.J.
title Stability and Fragility in Arctic Ecosystems
title_short Stability and Fragility in Arctic Ecosystems
title_full Stability and Fragility in Arctic Ecosystems
title_fullStr Stability and Fragility in Arctic Ecosystems
title_full_unstemmed Stability and Fragility in Arctic Ecosystems
title_sort stability and fragility in arctic ecosystems
publisher The Arctic Institute of North America
publishDate 1973
url https://journalhosting.ucalgary.ca/index.php/arctic/article/view/65966
geographic Arctic
geographic_facet Arctic
genre Arctic
Arctic
Subarctic
Thermokarst
Tundra
genre_facet Arctic
Arctic
Subarctic
Thermokarst
Tundra
op_source ARCTIC; Vol. 26 No. 3 (1973): September: 177–268; 178-185
1923-1245
0004-0843
op_relation https://journalhosting.ucalgary.ca/index.php/arctic/article/view/65966/49880
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