Acta Scientiarum Naturalium Universitatis Pekinensis

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A Preliminary Study on Mid-Holocene Paleoclimate and Paleoenvi-ronment along the Coast of Zhejiang Province

JIANG Dayong, YANG Shouren   

  1. Department of Geology, Peking University, Beijing, 100871, dyjiang@geoms. geo.pku. edu.cn
  • Received:1995-04-18 Online:1996-03-20 Published:1996-03-20

浙江沿海中全新世古气候、古环境初步分析

江大勇, 杨守仁   

  1. 北京大学地质学系,北京,100871

Abstract: Paleoclimate and paleoenvironment are discussed on the basis of faunas and14C dating,δ18O values, etc. of Mid Holocene beachrocks in Zhejiang province in the paper. Results of the study indicate that Zhejiang province belonged to the tropical zone in Mid-Holocene. This period can be divided into three epochs: (1) before 6040 aBP, (2) 5860-3210 aBP, (3) 2875-2770 aBP. In the second epoch, it was warmmer, especially the period of 5490-4110 aBP with megathermal maximum, the paleotemperature calculated by δ18O was 5-6℃ higher than that of the present.

Key words: paleoclimate, paleoenvironment, fauna, MidHolocene, Zhejiang Province

摘要: 首次通过对浙江象山爵溪镇下沙、大岙和岱山大长涂岛小沙河3个中全新世海滩岩剖面进行以动物群分析为基础,应用δ18O和14C等手段相结合的综合研究,初步分析了浙江沿海中全新世的古气候、古环境。认为海滩岩中热带贝类的出现是中全新世时气候变暖的结果。当时热带向北扩展到了浙江中北部地区,可分为3个暖期:6 040 aBP前、5 860~3 218 aBP和2 875~2 770 aBP,其中5 860~3 210 aBP较暖,它又可分为:5 860~5 490 aBP,5 490~4 110 aBP和3 765~3 210 aBP3个阶段,以5 490~4 110 aBP为最暖期,由δ18O计算的古气温约比现今当地高5~6℃。还由微量元素等特征推测了当时的古环境。

关键词: 古气候, 古环境, 动物群, 中全新世, 浙江

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