China's Beech Forests in the Pre-Quaternary

<i>Fagus</i> in China is never dominant in Late Cretaceous and Tertiary floras although it might reach its highest diversity in the Miocene. The genus <i>Fagus</i> was more widely distributed during the Palaeogene than in the Neogene. Furthermore, the ecological requirements...

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Main Authors: L. Yu-Sheng, W. Wei-Ming, A. Momohara
Format: Article
Language:English
Published: Copernicus Publications 1998-01-01
Series:Fossil Record
Online Access:http://www.foss-rec.net/1/151/1998/fr-1-151-1998.pdf
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spelling doaj-1a50a2baf0bc4642888107d205897c362020-11-24T23:18:08ZengCopernicus PublicationsFossil Record2193-00662193-00741998-01-011115116510.5194/fr-1-151-1998China's Beech Forests in the Pre-QuaternaryL. Yu-Sheng0W. Wei-Ming1A. Momohara2Museum of Natural History, Institute of Palaeontology, Invalidenstrasse 43, 10115 Berlin, GermanyDepartment of Palynology, Nanjing Institute of Geology & Palaeontology, Academia Sinica, Nanjing 210008, ChinaDepartment of Environmental Studies, Chiba University, 648 Matsudo, Matsudo City, Chiba, 271, Japan<i>Fagus</i> in China is never dominant in Late Cretaceous and Tertiary floras although it might reach its highest diversity in the Miocene. The genus <i>Fagus</i> was more widely distributed during the Palaeogene than in the Neogene. Furthermore, the ecological requirements of <i>Fagus</i> in the Palaeogene seem much broader than those in the Neogene onwards. This is because the Palaeogene floras containing <i>Fagus</i> lived in various conditions from an arid and hot climate to a humid and warm habitat. Additionally, <i>Fagus</i> then coexisted with many kinds of hygrophilous, thermophilous and xerophilous plants. However, the wide distribution, broad ecological adaptation and species composition changed greatly in the Neogene. The Neogene <i>Fagus</i>-containing floras are slightly more similar to the modern beech forests than the Palaeogene ones, although a big difference remains. Chinese fossil data document the post-Tertiary development of the modern beech forests. <br><br> doi:<a href="http://dx.doi.org/10.1002/mmng.19980010111" target="_blank">10.1002/mmng.19980010111</a>http://www.foss-rec.net/1/151/1998/fr-1-151-1998.pdf
collection DOAJ
language English
format Article
sources DOAJ
author L. Yu-Sheng
W. Wei-Ming
A. Momohara
spellingShingle L. Yu-Sheng
W. Wei-Ming
A. Momohara
China's Beech Forests in the Pre-Quaternary
Fossil Record
author_facet L. Yu-Sheng
W. Wei-Ming
A. Momohara
author_sort L. Yu-Sheng
title China's Beech Forests in the Pre-Quaternary
title_short China's Beech Forests in the Pre-Quaternary
title_full China's Beech Forests in the Pre-Quaternary
title_fullStr China's Beech Forests in the Pre-Quaternary
title_full_unstemmed China's Beech Forests in the Pre-Quaternary
title_sort china's beech forests in the pre-quaternary
publisher Copernicus Publications
series Fossil Record
issn 2193-0066
2193-0074
publishDate 1998-01-01
description <i>Fagus</i> in China is never dominant in Late Cretaceous and Tertiary floras although it might reach its highest diversity in the Miocene. The genus <i>Fagus</i> was more widely distributed during the Palaeogene than in the Neogene. Furthermore, the ecological requirements of <i>Fagus</i> in the Palaeogene seem much broader than those in the Neogene onwards. This is because the Palaeogene floras containing <i>Fagus</i> lived in various conditions from an arid and hot climate to a humid and warm habitat. Additionally, <i>Fagus</i> then coexisted with many kinds of hygrophilous, thermophilous and xerophilous plants. However, the wide distribution, broad ecological adaptation and species composition changed greatly in the Neogene. The Neogene <i>Fagus</i>-containing floras are slightly more similar to the modern beech forests than the Palaeogene ones, although a big difference remains. Chinese fossil data document the post-Tertiary development of the modern beech forests. <br><br> doi:<a href="http://dx.doi.org/10.1002/mmng.19980010111" target="_blank">10.1002/mmng.19980010111</a>
url http://www.foss-rec.net/1/151/1998/fr-1-151-1998.pdf
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