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引用本文:韩有松,孟广兰,王少青,宋怀龙.中国东部沿海第四纪古环境的探讨 Ⅰ.试论“生物环境容忍带”与生物气候界线[J].海洋科学,1988,12(5):15-18.
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中国东部沿海第四纪古环境的探讨 Ⅰ.试论“生物环境容忍带”与生物气候界线
韩有松1, 孟广兰1, 王少青1, 宋怀龙1
中国科学院海洋研究所
摘要:
本文提出“生物环境容忍带”概念,讨论生物对气候环境的适应性和一定条件下的容忍性,以此为据,论证了中国东部沿海23000年以来的生物气候界线、冰缘外围环境和气候环境变迁轮廓。
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基金项目:
ON“ENVIRONMENTAL TOLERANCE ZONE OF ORGANISMS”ANDBIOCLIMATIO FRONTIER——DISCUSSION ON THE PALEOENVIRON-MENT OF EASTERN CHINA COAST (No.1)
Abstract:
Organisms are related closely to climate environment. The environment is called "Environmental tolerance zone of organisms", in which organism groups or individual could tolerate but not adapt thoroughly. The environment is a transitional type characterized mainly by transitional condition of climate and mixed-symbiosis. Based on the concept of "Environmental tolerance zone of organisms", the ancient Bohai Sea, continental shelf plain of north Yellow Sea and North China plain were "outer enviroment of the ice edge" 23,000-13,000a B.P., and the south frontier of the ice edge was roughly in 36-37°N, i. e. the north side of the hills-land in middle Shangdong. Mixed-symbiosis occurred in the temperate zone and subtropic zone in the north Chinaplain in the middle of the Holecene, when the temperature rose and the environment ofwarm-zone shifted towards the northern China. But that does not mean the plain of North China was subtropic climate environment at that time.
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