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首页> 外文期刊>Chinese Geographical Science >RECONSTRUCTION OF PALEOVEGETATION AND PALEOCLIMATE OF HOLOCENE HYPSITHERMAL IN THE HEMUDU REGION
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RECONSTRUCTION OF PALEOVEGETATION AND PALEOCLIMATE OF HOLOCENE HYPSITHERMAL IN THE HEMUDU REGION

机译:河姆渡地区全新世地温的古植被和古气候的重建。

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摘要

In this pater, the paleovegetation and paleoclimate in the Hemudu region of Zhejiang Province during 7000 to 6000 a B. P. are reconstructed. Firstly , using Andersen's method, a correction is made for the percentage of pollens of various plants excavated at Hemudu Site. Secondly, on the basis of the results , the dominant species and constructive species and types of zonal forest vegetation are identified, then the paleovegetation of Holocene Hypsithermal is reconstructed. Finally, by contrasting the above mentioned paleovegetation with the vegetation of Wuyanling Natural Reserve (WYLNR) in south Zhejiang and Dinghushan Natural Reserve (DHSNR) in Guangdong today, and on the analogy of above results, the paleoclimate is also reconstructed.
机译:在该模式中,重建了河南省河姆渡地区7000至6000 a B. P.的古植被和古气候。首先,使用安徒生方法,对河姆渡遗址出土的各种植物的花粉百分比进行校正。其次,根据研究结果,确定了地带性森林植被的优势种,建设性种和类型,进而重建了全新世的超高温古植被。最后,通过将上述古植被与今天浙江南部的五言岭自然保护区(WYLNR)和广东的鼎湖山自然保护区(DHSNR)的植被进行对比,并根据上述结果,也重建了古气候。

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