Glaciers and ice sheets as a biome

被引:265
作者
Anesio, Alexandre M. [1 ]
Laybourn-Parry, Johanna [1 ]
机构
[1] Univ Bristol, Bristol Glaciol Ctr, Sch Geog Sci, Bristol BS8 1SS, Avon, England
关键词
HIGH ARCTIC GLACIER; LAKE VOSTOK; SNOW COVER; MICROBIAL BIOGEOGRAPHY; GLOBAL DISTRIBUTION; CRYOCONITE HOLES; ANTARCTIC ICE; MICROORGANISMS; SVALBARD; BACTERIA;
D O I
10.1016/j.tree.2011.09.012
中图分类号
Q14 [生态学(生物生态学)];
学科分类号
071012 ; 0713 ;
摘要
The tundra is the coldest biome described in typical geography and biology textbooks. Within the cryosphere, there are large expanses of ice in the Antarctic, Arctic and alpine regions that are not regarded as being part of any biome. During the summer, there is significant melt on the surface of glaciers, ice caps and ice shelves, at which point microbial communities become active and play an important role in the cycling of carbon and other elements within the cryosphere. In this review, we suggest that it is time to recognise the cryosphere as one of the biomes of Earth. The cryospheric biome encompasses extreme environments and is typified by truncated food webs dominated by viruses, bacteria, protozoa and algae with distinct biogeographical structures.
引用
收藏
页码:219 / 225
页数:7
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