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DOI | 10.1016/j.palaeo.2020.109988 |
Early Oligocene vegetation and climate of southwestern China inferred from palynology | |
Tang H.; Li S.-F.; Su T.; Spicer R.A.; Zhang S.-T.; Li S.-H.; Liu J.; Lauretano V.; Witkowski C.R.; Spicer T.E.V.; Deng W.-Y.-D.; Wu M.-X.; Ding W.-N.; Zhou Z.-K. | |
发表日期 | 2020 |
ISSN | 0031-0182 |
卷号 | 560 |
英文摘要 | The early Oligocene represents the beginning of the modern icehouse world. To better understand how vegetation and climate changed during this period, we reconstruct quantitively the early Oligocene vegetation and climate by analyzing fossil spore and pollen assemblages from Lühe basin, Yunnan Province, in southwestern China. The reconstructed paleoclimate using Bioclimatic Analysis shows that the mean annual temperature (MAT) ranged from 14.4 to 15.4 °C, the mean annual precipitation (MAP) was 1070.1–1297.8 mm, and the range of mean temperature of coldest quarter (MTCQ) was 6.7 to 7 °C, lower than that of the present day (9.3 °C). The reconstructed regional vegetation indicates a deciduous broadleaved forest mixed with evergreen broadleaved elements. Considering other Paleogene floras in Yunnan, deciduous broadleaved elements dominated in this area from the late Eocene to the early Oligocene. The paleoclimate reconstruction suggests that this vegetation composition may have been controlled mainly by cold winter temperatures. © 2020 Elsevier B.V. |
英文关键词 | Asia monsoon; Eocene-Oligocene boundary; Mean coldest month temperature; Nearest living relative; Paleoclimate; Paleovegetation |
语种 | 英语 |
scopus关键词 | broad-leaved forest; climate variation; deciduous tree; Oligocene; paleoclimate; Paleogene; palynology; spore; winter; China; Yunnan |
来源期刊 | Palaeogeography, Palaeoclimatology, Palaeoecology
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文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/150300 |
作者单位 | CAS Key Laboratory of Tropical Forest Ecology, Xishuangbanna Tropical Botanical Garden, Chinese Academy of Sciences, Mengla, Yunnan 666303, China; University of Chinese Academy of Sciences, Beijing, 100049, China; Center of Plant Ecology, Core Botanical Gardens, Chinese Academy of Sciences, Mengla, Yunnan 666303, China; School of Environment, Earth and Ecosystem Sciences, The Open University, Milton Keynes, MK76AA, United Kingdom; Faculty of Land Resource Engineering, Kunming University of Science and Technology, Kunming, 650093, China; Lancaster Environment Centre, Lancaster University, Lancaster, LA1 4YQ, United Kingdom; Schools of Chemistry and Earth Sciences, University of Bristol, Bristol, United Kingdom; Key Laboratory for Plant Diversity and Biogeography of East Asia, Kunming Institute of Botany, Chinese Academy of Sciences, Kunming, 650201, China |
推荐引用方式 GB/T 7714 | Tang H.,Li S.-F.,Su T.,et al. Early Oligocene vegetation and climate of southwestern China inferred from palynology[J],2020,560. |
APA | Tang H..,Li S.-F..,Su T..,Spicer R.A..,Zhang S.-T..,...&Zhou Z.-K..(2020).Early Oligocene vegetation and climate of southwestern China inferred from palynology.Palaeogeography, Palaeoclimatology, Palaeoecology,560. |
MLA | Tang H.,et al."Early Oligocene vegetation and climate of southwestern China inferred from palynology".Palaeogeography, Palaeoclimatology, Palaeoecology 560(2020). |
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