%0 Journal Article
%T A STUDY ON THE SPORO-POLLEN ASSEMBLAGE AND ITSPALEO-ENVIRONMENT AT THE PLANT-BEARINGCALCIC SINTER OF LATE CENOZOIC ERA ON NORTHERNSLOPE OF THE KUNLUN MOUNTAINS<br>昆仑山北坡晚新生代含植物化石石灰华的孢粉组合及其古环境
%A Huang Cixuan Zhang Qingsong
%A <br>黄赐璇
%A 张青松
%J 地理学报
%D 1991
%I 
%X In 1988, some plant-bearing calcic sinter were discovered and collected by the team of Scientific Expedition of Chinese Academy of Sciences to the Karakulun-Kunlun Mts. at 4600m. on the northern slope of middle Kunlun Mts. Its age is estimated to be from late Pliocene to early Pleistocene. Sporo-pollen assemblage of the plant-bearing calcic sinter is dominanted by angiospermous pollen (91.4%). Arboreal and shrubs pollen occupies 23.2% in the total pollen. Broad-leaf trees' pollen are mainly Salix, Ulmus> Quercus and Betula. Herbaceous pollen occupies 75.4%y in which Artemisia and Chenopodiaceae are abundant and Xerophyte pollens occupy a high percentages. Sporo-pollen analysis data support that the age of the plant-bearing calcic sitner is from middle-late Pliocene to early Pleistocene. In that time Paleovegetation was mainly represented by mountain steppe (Artemisia, Chenopodiaceae....) mixed with deciduous broad- Itaf forest (Salix, Quercus, Ulmus, Berula ...... in a warm and semidry climatic condition. Art annual mean temperature is estimated about 10?13?C. Altitude of the place where plant-bearing calcic sinter grew at that time was probably 1 500-2 000 m.
%K plant-bearing calcic sinter
%K sporo-pollen
%K paleo-environment<br>含植物化石石灰华
%K 孢子花粉
%K 古环境
%U http://www.alljournals.cn/get_abstract_url.aspx?pcid=E62459D214FD64A3C8082E4ED1ABABED5711027BBBDDD35B&cid=869B153A4C6B5B85&jid=F7B5B947C24B9D649491012214E4BEF4&aid=E512424D4AAA34C3A07CEC1B09891B0A&yid=116CB34717B0B183&iid=38B194292C032A66&journal_id=0375-5444&journal_name=地理学报&referenced_num=0&reference_num=0