Arid
DOI10.5194/cp-16-2255-2020
Aridification signatures from fossil pollen indicate a drying climate in east-central Tibet during the late Eocene
Yuan, Qin; Barbolini, Natasha; Rydin, Catarina; Gao, Dong-Lin; Wei, Hai-Cheng; Fan, Qi-Shun; Qin, Zhan-Jie; Du, Yong-Sheng; Shan, Jun-Jie; Shan, Fa-Shou; Vajda, Vivi
通讯作者Barbolini, N
来源期刊CLIMATE OF THE PAST
ISSN1814-9324
EISSN1814-9332
出版年2020
卷号16期号:6页码:2255-2273
英文摘要Central Asia experienced a number of significant elevational and climatic changes during the Cenozoic, but much remains to be understood regarding the timing and driving mechanisms of these changes as well as their influence on ancient ecosystems. Here, we describe the palaeoecology and palaeoclimate of a new section from the Nangqian Basin in Tibet, north-western China, dated as Bartonian (41.2-37.8 Ma; late Eocene) based on our palynological analyses. Located on the east-central part of what is today the Tibetan Plateau, this section is excellently placed for better understanding the palaeoecological history of Tibet following the Indo-Asian collision. Our new palynological record reveals that a strongly seasonal steppe-desert ecosystem characterized by drought-tolerant shrubs, diverse ferns, and an underlying component of broad-leaved forests existed in east-central Tibet during the Eocene, influenced by a southern monsoon. A transient warming event, possibly the middle Eocene climatic optimum (MECO; 40 Ma), is reflected in our record by a temporary increase in regional tropical taxa and a concurrent decrease in steppe-desert vegetation. In the late Eocene, a drying signature in the palynological record is linked to proto-Paratethys Sea retreat, which caused widespread long-term aridification across the region. To better distinguish between local climatic variation and farther-reaching drivers of Central Asian palaeoclimate and elevation, we correlated key palynological sections across the Tibetan Plateau by means of established radioisotopic ages and biostratigraphy. This new palynozonation illustrates both intra- and inter-basinal floral response to Qinghai-Tibetan uplift and global climate change during the Paleogene, and it provides a framework for the age assignment of future palynological studies in Central Asia. Our work highlights the ongoing challenge of integrating various deep time records for the purpose of reconstructing palaeoelevation, indicating that a multi-proxy approach is vital for unravelling the complex uplift history of Tibet and its resulting influence on Asian climate.
类型Article
语种英语
开放获取类型gold, Green Submitted
收录类别SCI-E
WOS记录号WOS:000592950700001
WOS关键词WESTERN QAIDAM BASIN ; HOH XIL BASIN ; PALYNOLOGICAL RECORD ; ASIAN MONSOONS ; NANGQIAN BASIN ; TECTONIC EVOLUTION ; NORTHWEST CHINA ; STABLE-ISOTOPE ; PLATEAU UPLIFT ; XINING BASIN
WOS类目Geosciences, Multidisciplinary ; Meteorology & Atmospheric Sciences
WOS研究方向Geology ; Meteorology & Atmospheric Sciences
资源类型期刊论文
条目标识符http://119.78.100.177/qdio/handle/2XILL650/327671
作者单位[Yuan, Qin; Gao, Dong-Lin; Wei, Hai-Cheng; Fan, Qi-Shun; Qin, Zhan-Jie; Du, Yong-Sheng; Shan, Jun-Jie; Shan, Fa-Shou] Chinese Acad Sci, Qinghai Inst Salt Lakes, Key Lab Comprehens & Highly Efficient Utilizat Sa, Xining, Peoples R China; [Yuan, Qin; Gao, Dong-Lin; Wei, Hai-Cheng; Fan, Qi-Shun; Qin, Zhan-Jie; Du, Yong-Sheng; Shan, Jun-Jie; Shan, Fa-Shou] Chinese Acad Sci, Qinghai Inst Salt Lakes, Qinghai Prov Key Lab Geol & Environm Salt Lakes, Xining, Peoples R China; [Yuan, Qin; Shan, Jun-Jie] Univ Chinese Acad Sci, Beijing, Peoples R China; [Yuan, Qin; Vajda, Vivi] Swedish Museum Nat Hist, Dept Palaeobiol, Stockholm, Sweden; [Barbolini, Natasha; Rydin, Catarina] Stockholm Univ, Dept Ecol Environm & Plant Sci, Stockholm, Sweden; [Barbolini, Natasha; Rydin, Catarina] Stockholm Univ, Bolin Ctr Climate Res, Stockholm, Sweden; [Barbolini, Natasha] Univ Amsterdam, Inst Biodivers & Ecosyst Dynam, Dept Ecosyst & Landscape Dynam, Amsterdam, Netherlands; [Rydin, Catarina] Royal Swedish Acad Sci, Bergius Fdn, Stock...
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GB/T 7714
Yuan, Qin,Barbolini, Natasha,Rydin, Catarina,et al. Aridification signatures from fossil pollen indicate a drying climate in east-central Tibet during the late Eocene[J],2020,16(6):2255-2273.
APA Yuan, Qin.,Barbolini, Natasha.,Rydin, Catarina.,Gao, Dong-Lin.,Wei, Hai-Cheng.,...&Vajda, Vivi.(2020).Aridification signatures from fossil pollen indicate a drying climate in east-central Tibet during the late Eocene.CLIMATE OF THE PAST,16(6),2255-2273.
MLA Yuan, Qin,et al."Aridification signatures from fossil pollen indicate a drying climate in east-central Tibet during the late Eocene".CLIMATE OF THE PAST 16.6(2020):2255-2273.
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