CLIMATIC OPTIMUM DURING THE HOLOCENE AND THE DISTRIBUTION OF WARM-WATER MOLLUSKS IN THE SEA OF JAPAN

被引：22

作者：

LUTAENKO, KA ^{[1
]}

机构：

[1] RUSSIAN ACAD SCI, INST MARINE BIOL, FAR E BRANCH, VLADIVOSTOK 690032, RUSSIA

来源：

PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY | 1993年 / 102卷 / 3-4期

关键词：

D O I：

10.1016/0031-0182(93)90071-P

中图分类号：

P9 [自然地理学];

学科分类号：

0705 ; 070501 ;

摘要：

The geographical distribution of warm-water mollusks has been analyzed and the paleobiogeographical significance of the climatic optimum during the Holocene in the formation of the shallow-water malacofauna in the Sea of Japan has been assessed. The shift of the southern boundary of the Pacific boreal region was 700-800 km to the north compared to its present-day position (based on bivalve mollusks). On the continental coast of the Sea of Japan this boundary is observed in Peter the Great Bay (approximately 43-degrees-N) and on the Japanese side it seems to be at the central part of Hokkaido. It can be concluded that a temperature increase of the surface water mass of 0.1-0.2-degrees-C can cause a shift of about 100 km of the northern boundary of the area of warm-water mollusks.

引用

页码：273 / 281

页数：9

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