摘要
研究了北京天竺TZ01钻孔岩心孢粉样品239块,孢粉组合反映了北京天竺晚上新世以来(约3.580MaBP)植被演替和气候变迁大致经历了10个发展阶段:(1)3.580～3.050MaBP:以针叶林植被为主,气候寒冷偏湿;(2)3.050～2.555MaBP:植被为落叶阔叶和常绿阔叶混交林—草原类型,该阶段开始升温,但气候较为温暖湿润;(3)2.555～2.300MaBP:植被为温凉偏干的疏林草原,湿度开始下降;(4)2.300～1.770MaBP:植被类型仍为疏林草原,该阶段温度上升,但幅度并不大,湿度基本不变,气候温凉干爽;(5)1.770～1.070MaBP:植被类型为针阔混交林—草原,气候温暖湿润;(6)1.070～0.922MaBP:植被演替为较暖湿略干的针阔混交林—草原;(7)0.922～0.800MaBP:植被为较寒冷干燥的疏林草原,温度降低,降水减少;(8)0.800～0.650MaBP:植被为温暖偏干的以松为主的疏林草原,温度有所上升,但湿度变化较小;(9)0.650～0.160MaBP:植被为温凉湿润的针阔叶混交林—草原;(10)0.160MaBP至今:植被以针阔叶混交林—草原为主,前期气候冷湿,后期较为温暖湿润。
Totally 239 palynological samples from TZ01 borehole in Tianzhu Region in Beijing were studied. The palynological assemblages show that the vegetation succession and the changing pattern of climate in Tianzhu Region in Beijing during the past 3. 580 million years experienced ten stages ： （ 1 ） From 3.580 to 3.050 Ma BP, the vegetation was dominated by needle-leaved forest with the cold and humid climate conditions; （2） From 3. 050 to 2. 555 Ma BP, the vegetation changed into deciduous and evergreen broad-leaved mixed forests and grassland, and climate became warm and humid ; （ 3 ） From 2. 555 to 2. 300 Ma BP, the vegetation was arid grassland with sparse forest, and humidity began to decline; （4） From 2. 300 to 1. 770 Ma BP, the vegetation was grassland with sparse forest, but temperature began to rise and humidity changed little; （5） From 1. 770 to 1. 070 Ma BP, the vegetation transferred into grassland along with needle and broad-leaved mixed forests with the warm and humid climate conditions; （6） From 1. 070 to 0. 922 Ma BP, the vegetation had the same type as the previous stage, but climate was a bit arid; （7） From 0. 922 to 0. 800 Ma BP, the vegetation was grassland with sparse forest in cold and arid climate, while temperature declined and precipitation decreased; （8） From 0. 800 to 0. 650 Ma BP, the vegetation was arid grassland with sparse forest, and temperature rose again, but humidity changed little ; （9） From 0. 650 to 0. 160 Ma BP, the vegetation was grassland along with mixed needle and broad-leaved forest; （10） From 0. 160 Ma BP to present, the vegetation was dominated by needle and broad-leaved foreats, while climate was warmer and more humid during the late phase of this stage.
出处
《古地理学报》
CAS
CSCD
2007年第1期45-58,共14页
Journal of Palaeogeography：Chinese Edition
基金
中国科学院地球环境研究所黄土与第四纪地质国家重点实验室开放基金(SKLLQG0410)
北京市自然科学基金(8052009)
北京市优秀人才培养专项(20041D130018)资助项目
关键词
北京天竺
晚上新世
第四纪
植被演替
气候变迁
孢粉
Tianzhu Region in Beijing, Late Pliocene, Quaternary, vegetation succession, climate changing, sporo-pollen
