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桂林甑皮岩洞穴遗址第四纪孢粉分析
引用本文:王丽娟.桂林甑皮岩洞穴遗址第四纪孢粉分析[J].人类学学报,1989,8(1):T001-T002.
作者姓名:王丽娟
作者单位:地质矿产部岩溶地质研究所
摘    要:本文对桂林甑皮岩洞穴古人类遗址的文化层堆积物和钙华板系统采样进行孢粉分析研究,分析了当时的植被演替和气候变化、古人类的生活环境以及文化层和钙华板形成的地质时代。

关 键 词:甑皮岩  孢子  花粉  全新世  洞穴遗址  桂林  孢粉分析

A QUATERNARY SPORO-POLLEN ANALYSIS OF ZENGPIYAN CAVE SITE, GUILIN
Wang Lijuan.A QUATERNARY SPORO-POLLEN ANALYSIS OF ZENGPIYAN CAVE SITE, GUILIN[J].Acta Anthropologica Sinica,1989,8(1):T001-T002.
Authors:Wang Lijuan
Abstract:Zengpiyan Cave, a neolithic site, is situated about 9km south of Guilin city. A great number of pollen grains of ligneous plant, herbal plant and spores of pteridophyta have been found in the cultural bed and the calctufas' plate. Mainly they are: Pinus, Carya, Quercus, Ulmus, Celtis, Corylopsis, Liquidambar, Euphorbiaceae, Sapium, Alchornea, Myrica, Magnoli-aceae, Palmae, Betula, Carpinus, Rutaceae, Rosaceae, Gramineae, Artemisia, Ranunculaceae, La-biatae, Gesneriaceae, Pteris, Polypodiaceae, Adiantaceae, Onychium, and Hicriopteris etc. The results of sporo-pollen analysis show that the process from accumulating of the cultural bed to forming the calctufas' plate may be divided by three phases of vegetation. They are rare forest vegetation phase, coniferous-broad leaf mixed forest phase with dominative broad leaf plant and coniferous-broad leaf mixed forest phase with dominative coniferous plant. The climates corresponding to three phases are mild-humid, warm-humid and warm-drier. The geological age of the cultural bed is described as the early Holocene-early middle Holocene, while the age of the calctufas' plate is late middle Holocene-late Holocene.
Keywords:Zengpiyan  Spore  Pollen  Holocene
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