摘要
根据位于策勒绿洲与荒漠交错带的塔格勒剖面孢粉记录的初步研究表明，近700aB．P．来此地区气候的干旱状况持续求变，但期间仍有几次相对湿润期，即在剖面距顶2．7－2．0m段、1．8－1．9m段和0．8－0．6m段孢粉组合特征显示出当时植被生长条件较好，生长环境相对湿润的特征，地层沉积物特征也有相应体现。初步的研究表明，干旱区绿洲内部的地质沉积记录可能能够较为详细地记录到气候环境演变的细节。
?The spore - pollen study of the Tagle section, which locates in the inner Cele oasisshow that since about 700aBP, the dry regiem consectively existed, but three revealed relative wet periodspunctuated in the period, which appearred from about 630 to 3(X)aB - P., 200 to l70aB. P. and from 70- 30aB. P., imposed on the general desertification. Two important tindng boundaries of paleoclimaicevolution can be identified, i. e. at about 630aB. P., the wetting environmental transition was identicalwith the phase of 'Abrupt climaic change'took place at about l230A. D., which was deduced from thehistoric references since 2000aB. P. obtained in eastem China; Another short climatic shift perhaps ap-Pearred at about 200aB. P., aller which desertification agglavated intensively.
出处
《干旱区研究》
CSCD
1998年第3期14-18,共5页
Arid Zone Research
基金
新疆大学与日本东京理科大学合作研究项目
国家自然科学基金!49741003
新疆大学自然科学基金
关键词
土壤
策勒绿洲
塔格勒剖面
孢粉
沉积地层
southern fringe of Takelamagan desert, cele oasis, Tagele section, spore - pollen
