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| 1 | Cenozoic plant diversity of Yunnan: A review显示文摘Yunnan in southwestern China is renowned for its high plant diversity.To understand how this modern botanical richness formed,it is critical to investigate the past biodiversity throughout the geological time.In this review,we present a summary on plant diversity,floristics and climates in the Cenozoic of Yunnan and document their changes,by compiling published palaeobotanical sources.Our review demonstrates that thus far a total of 386 fossil species of ferns,gymnosperms and angiosperms belonging to 170 genera within 66 families have been reported from the Cenozoic,particularly the Neogene,of Yunnan.Angiosperms display the highest richness represented by 353 species grouped into 155 genera within 60 families,with Fagaceae,Fabaceae,Lauraceae and Juglandaceae being the most diversified.Most of the families and genera recorded as fossils still occur in Yunnan,but seven genera have disappeared,including Berryophyllum,Cedrelospermum,Cedrus,Palaeocarya,Podocarpium,Sequoia and Wataria.The regional extinction of these genera is commonly referred to an aridification of the dry season associated with Asian monsoon development.Floristic analyses indicate that in the late Miocene,Yunnan had three floristic regions:a northern subtropical floristic region in the northeast,a subtropical floristic region in the east,and a tropical floristic region in the southwest.In the late Pliocene,Yunnan saw two kinds of floristic regions:a subalpine floristic region in the northwest,and two subtropical floristic regions separately in the southwest and the eastern center.These floristic concepts are verified by results from our areal type analyses which suggest that in the Miocene southwestern Yunnan supported the most Pantropic elements,while in the Pliocene southwestern Yunnan had abundant Tropical Asia(Indo e Malaysia)type and East Asia and North America disjunct type that were absent from northwestern Yunnan.From the late Miocene to late Pliocene through to the present,floristic composition and vegetation types changed markedly,presumably in response to altitude changes and coeval global cooling.An integration of palaeoclimate data suggests that during the Neogene Yunnan was warmer and wetter than today.Moreover,northern Yunnan witnessed a pronounced temperature decline,while southern Yunnan experienced only moderate temperature changes.Summer precipitation was consistently higher than winter precipitation,suggesting a rainfall seasonality.This summary on palaeoclimates helps us to understand under what conditions plant diversity occurred and evolved in Yunnan throughout the Cenozoic. | Yongjiang Huang Linbo Jia QiongWang Volker Mosbrugger Torsten Utescher Tao Su Zhekun Zhou | 2016 | Plant Diversity2016，38，6： | 8 |
| 2 | The coexistence approach-a met-hod for quantitative reconstructions of Tertiary terrestrial pal-aeoclimate data using plant fossils 显示文摘 | Mosbrugger V Utescher T | 1997 | Palaeogeography Pal-aeoclimatology Palaeoecology1997，134，1： | 1 |
| 3 | Late Mioceneclimate in the circnm-AIpine realm-a quantitative analysis ofterrestrial palaeofloras显示文摘 | Bruch A A Utescher T Mosbrugger V | 2006 | Palaeogeography Palaeoclimatolo-gy Palaeoecology2006，238，： | 1 |
| 4 | Early to Middle Jurassic vegetation and climatic events in the Qaidam Basin,Northwest China显示文摘 | YONGDONG WANG VOLKER MOSBRUGGER HONG ZHANG | 2005 | Palaeogeography Palaeoclimatology Palaeoecology2005，224，： | 1 |
| 5 | Quantitative reconstruction of Miocene climate patterns and evolution in Southern China based on plant fossils显示文摘 | Yi-Feng Yao Angela A. Bruch Volker Mosbrugger Cheng-Sen Li | 2010 | Palaeogeography Palaeoclimatology Palaeoecology2010，，3： | 1 |
| 6 | Quantitativereconstruction of Miocene climate patterns and evolution inSouthern China based on plant fossils 显示文摘 | YAO Y F BRUCH A A MOSBRUGGER V | 2011 | Palaeogeography Palaeoclimatology Palaeoecology2011，304，34： | 1 |
| 7 | The coexistence approach: a method for quantitative reconstruction of Tertiary terrestrial paleoclimate data using plant fossils显示文摘 | Mosbrugger Utescher | 1997 | Palaeogeogr Palaeoclimatol Palaeoecol1997，134，： | 1 |
| 8 | Cenozoic continental climatic evolution of central Europe显示文摘 | MOSBRUGGER V UTESCHER T DILCHER D L | 2005 | Proceedings of the National Academy of Sciences2005，102，14： | 1 |
| 9 | Third pole environment (TPE) 显示文摘 | Yao T D Thompson L G Mosbrugger V | 2012 | Environmental Development2012，3，： | 1 |
| 10 | Reconstructing Holocene vegetation and climate history of Nam Co area (Tibet), using pollen and other palynomorphs显示文摘 | Mark Herrmann Xinmiao Lu Jonas Berking Brigitta Schütt Tandong Yao Volker Mosbrugger | 2009 | Quaternary International2009，，1： | 1 |
| 11 | Evolution and function of leaf venation architecture: A review 显示文摘 | Roth-Nebelsick A Uhl D Mosbrugger V | 2001 | Annal Bot2001，87，5： | 1 |
| 12 | Evolution and function of leaf venation architecture, a review 显示文摘 | Roth-nebelsick A Uhl D Mosbrugger V | 2001 | Anm Bot2001，87，： | 1 |
| 13 | Evolution and function of leaf venation architecture: A review显示文摘 | Roth-Nebelsick A Uhl D Mosbrugger V | 2001 | Annals of Botany2001，87，5： | 1 |
| 14 | The coexistence approach-a method for quantitative reconstructions of Tertiary terrestrial palaeoclimate data using plant fossils显示文摘 | MOSBRUGGER V UTESCHER T | 1997 | Palaeogeography Palaeoclimatology Palaeoecology1997，134，： | 1 |
| 15 | The coexistence approach-a method for quantitative reconstructions of Tertiary terrestrial palaeoclimate data using plant fossils显示文摘 | MOSBRUGGER V UTESCHER T | 1997 | Palaeogeography Palaeoclimatology Palaeoecology1997，134，： | 1 |
| 16 | l_~afvenation density as a climate and environmental proxy: a critical review and new data 显示文摘 | Uhl D Mosbrugger V | 1999 | Palaeogeography Palaeoclimatology Palaeoecology1999，149，14： | 1 |
| 17 | The coexistence approach: a method for quantitative reconstruction of Tertiary terrestrial paleoclimate data using plant fossils显示文摘 | Mosbrugger Utescher | 1997 | Pala ogeogr Palaeoclimatol Palaeoecol1997，，134： | 1 |
| 18 | A review of char- coal analysis as a tool for assessing Quaternary and Tertiary environments:achievements and limits显示文摘 | Figueiral I Mosbrugger V | 2000 | Palaeogeography Palaeoclimatology Palaeoecology2000，164，： | 1 |
| 19 | Reconstructing palaeotemperatures using leaf floras-ease studies for a comparison of leaf margin analysis and the coexistence approach 显示文摘 | Uhl D Mosbrugger V Bruch A | 2003 | Rev Palaeobot Palynol2003，126，： | 1 |
| 20 | The coexistence approach: a method for quantitative reconstruction of Tertiary terrestrial palaeoclimate data using plant fossils 显示文摘 | Mosbrugger Utescher | 1997 | Pala ogeogr Palaeoclimatol palaeoecol1997，，134： | 1 |
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