Variability in oceanographic and ecological processes in the Canadian Arctic Archipelago

被引:134
|
作者
Michel, C.
Ingram, R. G.
Harris, L. R.
机构
[1] Fisheries & Oceans Canada, Inst Freshwater, Winnipeg, MB R3T 2N6, Canada
[2] Univ British Columbia, Dept Earth & Ocean Sci, Vancouver, BC V6T 1Z4, Canada
[3] Fisheries & Oceans Canada, Bedford Inst Oceanog, Dartmouth, NS B2Y 4A2, Canada
基金
加拿大自然科学与工程研究理事会;
关键词
Arctic; Canadian Archipelago; climate; sea ice; ice algae; phytoplankton; primary production; sedimentation; copepod grazing; pelagic-benthic coupling;
D O I
10.1016/j.pocean.2006.09.006
中图分类号
P7 [海洋学];
学科分类号
0707 ;
摘要
This paper brings together unpublished historical data sets and published literature to review the role of climatic, oceanographic and ecological processes in the marine ecosystem of the eastern Canadian Archipelago. Physical data include characteristics of the water masses, circulation patterns, sea ice conditions, and climatic records from 1950s onward. Biological data include unpublished data sets on nutrients, primary and secondary production, and sedimentation, which were collected during the 1980-1990s in the eastern Canadian Archipelago. These results show high year-to-year variability in nutrient inventories and ratios, the magnitude of the ice algae and phytoplankton bloom, the timing of ice algae sedimentation in the spring, and the composition of the zooplankton community. The significance of this high interannual variability and its effect on pelagic-benthic coupling processes is discussed in the context of climatic and oceanographic forcing, with emphasis on recent (past decade) Arctic changes. An estimate of total primary production in the Archipelago is also presented, along with published production estimates for other Arctic shelves, showing that the Archipelago may support up to 32% of the total primary production of Arctic shelves. The high year-to-year variability in production and carbon transfer pathways (e.g. pelagic versus benthic) in the Archipelago suggest that the system might be resilient to the increased variability in climatic conditions occurring in the past decade. However, this increased variability combined with directional change in climatic and oceanographic conditions might also modify the existing balance of ecological processes. For example, shifts in the timing of events appear to have already occurred in the past decade, with potential cascading effects throughout the ecosystem. Crown Copyright (c) 2006 Published by Elsevier Ltd. All rights reserved.
引用
收藏
页码:379 / 401
页数:23
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