Item type |
紀要論文(ELS) / Departmental Bulletin Paper(1) |
公開日 |
2001-03-01 |
タイトル |
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言語 |
en |
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タイトル |
Biological characteristics of dark colored material (cryoconite) on Canadian Arctic glaciers (Devon and Penny ice caps) (scientific paper) |
言語 |
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言語 |
eng |
資源タイプ |
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資源タイプ識別子 |
http://purl.org/coar/resource_type/c_6501 |
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資源タイプ |
departmental bulletin paper |
ページ属性 |
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内容記述タイプ |
Other |
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内容記述 |
P(論文) |
著者名(英) |
Takeuchi, Nozomu
Kohshima, Shiro
Goto-Azuma, Kumiko
Koerner, Roy M.
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著者所属(英) |
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en |
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Frontier Observational Research System for Global Change, International Arctic Research Center, University of Alaska |
著者所属(英) |
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en |
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Biological Laboratory, Faculty of Bioscience and Biotechnology, Tokyo Institute of Technology |
著者所属(英) |
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en |
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National Institute of Polar Research |
著者所属(英) |
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en |
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Terrain Sciences Division, Geological Survey of Canada |
抄録(英) |
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内容記述タイプ |
Other |
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内容記述 |
Biological characteristics of dark colored material (cryoconite) collected from Canadian Arctic glaciers (Devon and Penny ice caps) are described. The cryoconite consists of mineral particles and organic matter. The amount of organic matter was 0.8-13.8% dry weight. Seven taxa of snow algae (Chlorophyta and Cyanophyta) were observed in the cryoconite. The mineral particles, the algae, the bacteria, and amorphous organic matter formed small dark colored granules (cryoconite granules). The size of the granules was approximately 0.4mm in diameter. Microscopy of the granules revealed that the granules contain bacteria with mucus like substance, and that the surface of the granules was covered with filamentous blue-green algae. These observations suggest that the granules are formed by algal and bacterial activity on the glaciers, and that the cryoconite includes a large amount of biological products. The amount of the cryoconite per unit area on the glacier surface was generally small (mean 48g m^<-2> in dry weight). In contrast, a large amount of the cryoconite was deposited at the bottom of cryoconite holes. The small amount of cryoconite on the glacier surface means that the effect of the cryoconite on albedo reduction of the glacier surface is small. |
雑誌書誌ID |
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収録物識別子タイプ |
NCID |
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収録物識別子 |
AA00733561 |
書誌情報 |
Memoirs of National Institute of Polar Research. Special issue
巻 54,
p. 495-505,
発行日 2001-03
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