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湖南澧县彭头山遗址是1988年发掘的一处新石器早期遗址。同年,我们对遗址有关地层的孢粉进行了分析。下面将分析结果予以介绍,并对当时的自然环境略作探讨。一遗址自然环境及采样地层综合剖面彭头山遗址位于北纬29°40′、东经110°45′,地处澧水冲积平原——澧阳平原的低岗上。东临洞庭湖,西倚武陵山,北有涔水,南为澧水。这里虽处于亚热带北部,但平原地区由于人类长期活动,原生植被已不复存在,只是在丘陵和村落附近还常见到苦槠、青冈栎、樟树、冬青等树种组成的常绿阔叶林片
Peng County, Hunan Pixian site was excavated in 1988 a Neolithic ruins. In the same year, we analyzed the sporopollen of the related strata of the site. The following analysis of the results to be introduced, and the natural environment of the time a little discussion. A Site Natural Environment and Comprehensive Profile of Sampling Stratum Pengtoushan site is located at 29 ° 40’N and 110 ° 45’E and is located on a low hillock in the alluvial plain of the Shuiyang Plain. Dongting Lake in the east, West Hill Wuling, Lushui north, south Lishui. Although the area is located in the northern part of the subtropics, native vegetation no longer exists in the plains due to long-term human activities, except for the evergreen broad-leaved forests consisting of bitter gourd, oak tree, camphor tree and holly tree near the hills and villages