浙东中新世<i>Cinnamomum</i> cf. <i>bejolghota</i>微细构造及其古环境意义

何文龙; 何雨栗; 陈军林; 肖良; 刀克群; 吴靖宇; 李相传; 孙柏年

doi:10.3799/dqkx.2013.046

Volume 38 Issue 3

May 2013

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Article Navigation > Earth Science > 2013 > 38(3): 461-470

HE Wen-long, HE Yu-li, CHEN Jun-lin, XIAO Liang, DAO Ke-qun, WU Jing-yu, LI Xiang-chuan, SUN Bai-nian, 2013. Microstructures of Cinnamomum cf. bejolghota from the Miocene of Eastern Zhejiang and Its Palaeoenvironmental Significance. Earth Science, 38(3): 461-470. doi: 10.3799/dqkx.2013.046

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HE Wen-long, HE Yu-li, CHEN Jun-lin, XIAO Liang, DAO Ke-qun, WU Jing-yu, LI Xiang-chuan, SUN Bai-nian, 2013. Microstructures of Cinnamomum cf. bejolghota from the Miocene of Eastern Zhejiang and Its Palaeoenvironmental Significance. Earth Science, 38(3): 461-470. doi: 10.3799/dqkx.2013.046

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Microstructures of Cinnamomum cf. bejolghota from the Miocene of Eastern Zhejiang and Its Palaeoenvironmental Significance

doi: 10.3799/dqkx.2013.046

1.
School of Earth Sciences, Lanzhou University, Lanzhou 730000, China
2.
State Key Laboratory of Palaeobiology and Stratigraphy, Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences, Nanjing 210008, China
3.
The School of Earth Science and Resources, Chang'an University, Xi'an 710064, China

Received Date: 2012-04-20
Publish Date: 2013-05-15

Abstract

Abstract

Leaf fossils are collected for this study from the Shengxian Formation in Tiantai, Zhejiang Province. There are abundant compressed angiosperm fossils and a few gymnosperm fossils in the Shengxian Formation. Based on steady macromorphology of leaf including the base, the apex, the vein and so on, one species of Lauraceae plant fossils is studied in detail by analyzing the leaf architecture and cuticle characteristics in this paper. The fossil leaves and living Cinnamomum bejolghota (Buch-Ham.) Sweet are found sharing resemblance on the leaf shape, leaf vein, vein cell, stomata type and the features of trichomes. So the fossil leaves are identified as Cinnamomum bejolghota. Based on cuticle characteristics of fossil leaves and the distribution area and survival environment of living Cinnamomum bejolghota, we come to the following conclusions on the paleoclimate and paleoenviroment in eastern Zhejiang, that it was hotter and moister than present, and the distribution area of Cinnamomum bejolghota moved southward from Miocene.
- plant fossils,
- cuticular microstructure,
- eastern Zhejiang,
- Miocene,
- Shengxian Formation,
- stratigraphy

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致谢: 朱胜睿参与了化石采集工作，在此表示感谢.

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Microstructures of Cinnamomum cf. bejolghota from the Miocene of Eastern Zhejiang and Its Palaeoenvironmental Significance

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