黄河流域全新世遗址区土壤研究进展

Progress of Soil Research in Holocene Site Area of Yellow River Basin

黄河流域是古文明孕育、产生、发展的重要区域之一,其中下游地区普遍覆盖着第四纪的松散堆积物。已有研究表明该区域曾经历过多次气候剧烈变化。对黄河流域遗址区土壤研究,有助于弄清全新世时期该区域的环境演变和古人类活动等信息。近年来,对古文化遗址区的土壤研究日益成为国内外研究的热点。该文从土壤特性与环境变化、土壤特性与人类活动2个方面,简述了黄河流域遗址区古土壤的理化性质、微型态、年代学、孢粉、陶器、土壤遗存物等方面的研究进展,指出当前研究存在的问题,期望能够丰富该区域古环境、古文明的相关研究,为协调人地关系提供方向。

The Yellow River basin is one of the important regions for the breeding,generation and development of ancient civilization.Previous studies have shown that this region has experienced many severe climate changes.Through the study of the soil of the Yellow River basin site area,it is helpful to find out the information of the environmental evolution and paleoanthropic activities of this region in the holocene.In recent years,the study of soil in the ancient cultural sites has become a hot topic at home and abroad.From the aspects of soil characteristics,environmental changes,soil characteristics and human activities,the research progress on the physical and chemical properties,micro-states,chronology,palynology,pottery and soil remains of ancient soils in the Yellow River basin site areas was briefly reviewed.This paper points out the problems existing in the current research and hopes to enrich the related studies on the ancient environment and ancient civilization in the region and provide a direction for the coordination of human-earth relations.