摘要
中国黄土沉积纪录了最近2.6Ma以来黄土高原及全球自然环境演变的历史。重建其演变历史以预测未来气候环境的变化趋势是指导该地区经济、生态环境建设的重要基础。黄土的地球化学指标是重建该地区环境演变历史的重要途径之一。基于进一步研究的目的,总结了黄土地球化学指标在环境演变研究中的应用和近年来取得的进展。
Loess deposition in China has recorded the histories of the environmental evolution in the Loess Plateau and other areas of the world since the recent 2.6 Ma. It is very important to reconstruct the history of environmental evolution for forecasting the climatic changing trend and to guide economical construction and environmental restoration in these areas. Loess geochemical indicator is an important way to recon- struct the history qf climate-environment evolution. Based on the purpose of further study, the paper tries to sum the application and progress of loess geochemical indicators in the study of environmental evolution' in recent years.
出处
《安徽农业科学》
CAS
北大核心
2011年第17期10426-10431,共6页
Journal of Anhui Agricultural Sciences
基金
国家自然科学基金项目(40801008)
北方民族大学引进人员科研项目
关键词
黄土
地球化学指标
古气候环境
Loess
Geochemical indicator
Paleoclimate and paleoenvironment