AMUR-HEILONG NATURAL HERITAGE |
All chapters: Species diversity and use of biological resources |
Song-Nen Plain - Sea of Reeds |
Related maps, pictures, links |
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Once upon a time the whole plain was a huge lake and fine sands were deposited from rivers and lakes throughout the Quaternary period. These tend to be poorly drained, creating swampy, sometimes saline conditions in the low-lying areas, some of which have boggy peat soils. Nowadays typical landscapes are flooded meadows and shallow, reed-filled lakes, rivers and old river courses undergoing ecological succession to grassland. Lakes may be either fresh or brackish, and salt concentrations are increasing in many areas as a result of freshwater diversions for irrigation. Meadows are dominated by tall grasses that are adapted to flooded soils. These often grow as dense tussocks that emerge from flooded areas. Lakes are often filled or lined at the margin by the salt-tolerant reed. Upland areas are dominated by grasslands, forest-grasslands with crooked elms, and shrub groves of wild-apricot on the hilltops. During the past 100 years the largest grassland-wetland of the Amur-Heilong basin, has been reduced by agriculture and other human encroachment to a series of isolated and shrinking wet grass habitats. There is no reliable regulatory mechanism to ensure sufficient and timely water supply to these remnant wetlands. This leads to degradation of habitat due to desiccation and agricultural encroachment. Siberian cranes in Lindian County (Photo by Guo Yumin)
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Maps:
Topography of Amur Heilong River basin
Photo: Introductory tour of Amur basin
GIS: Amur-Heilong Natural Heritage
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