Arid
DOI10.1639/0044-7447(2000)029[0002:THHOLV]2.0.CO;2
The holocene history of Lake Victoria
Johnson, TC; Kelts, K; Odada, E
通讯作者Johnson, TC
会议名称50th Scientific Advisory Council Meeting of the International-Geosphere-Biosphere-Programme
会议日期SEP, 1998
会议地点NAIROBI, KENYA
英文摘要

Recent investigations by the International Decade for the East African Lakes (IDEAL) have significantly advanced our knowledge on the history of Lake Victoria. Seismic reflection profiles confirm the origin of the lake as a result of regional tilting and provide an estimated age of 400 000 years for the lake basin. Three major desiccation events are recorded in the seismic records that may reflect the 100 000 year Milankovitch cycle of climate forcing. The most recent arid period resulted in complete desiccation of the pre-existing lake. Lake Victoria arose from a dry landscape 14 600 calendar years ago (14.6 ka). Primary production was extremely high as lake level rose in its first 500 years, nourished by the high input of nutrients from the flooded landscape. A few species of cichlids and other fish swam out of their fluvial refugia to colonize the new lake, generating hundreds of new endemic species over the ensuing 14 000 years. Lake level rose until a brief overflow event at about 14.2 ka to 13.6 ka. Closed-basin conditions returned during the Younger Dryas until 11.2 ka, when major outflow and open-basin conditions were permanently established. The lake experienced progressively stronger stratification and water-column stability through the first half of the Holocene, and diatom productivity dropped to a minimum from 9.8 to about 7.5 ka. This period coincides with, but is much longer than, the 8.2 ka climatic event that has been observed in many Holocene records from throughout the world. The degree of water-column mixing appears to have steadily increased over the last 6000 years. Short cores from the open lake, document a shift in lake conditions beginning in the 1930s that progressed to the major ecosystem collapse of the early 1980s. The coincidence of the shift in sediment properties in the 1930s with the beginning of rapid expansion of human population and agricultural activity suggests cause and effect. It is conceivable that the lake experienced similar conditions due to natural causes between about 9800 and 7500 years ago.


来源出版物AMBIO
ISSN0044-7447
EISSN1654-7209
出版年2000
卷号29
期号1
页码2-11
出版者SPRINGER
类型Article;Proceedings Paper
语种英语
国家USA;Kenya
收录类别SCI-E ; CPCI-S
WOS记录号WOS:000087739500002
WOS关键词LATE PLEISTOCENE DESICCATION ; CICHLID FISHES ; EAST-AFRICA ; EVENT ; MALAWI
WOS类目Engineering, Environmental ; Environmental Sciences
WOS研究方向Engineering ; Environmental Sciences & Ecology
资源类型会议论文
条目标识符http://119.78.100.177/qdio/handle/2XILL650/292907
作者单位(1)Univ Minnesota, Large Lakes Observ, Duluth, MN 55812 USA;(2)Univ Minnesota, Limnol Res Ctr, Minneapolis, MN 55455 USA;(3)Univ Nairobi, PASS, Dept Geol, Nairobi, Kenya
推荐引用方式
GB/T 7714
Johnson, TC,Kelts, K,Odada, E. The holocene history of Lake Victoria[C]:SPRINGER,2000:2-11.
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