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    中国百强科技报刊

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    Volume 37 Issue 1
    Jan.  2012
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    DING Su-ting, SUN Bai-nian, WU Jing-yu, LI Xiang-chuan, 2012. Machilus Fossil from Miocene in Tiantai, Zhejiang Province, China, and Its Paleoenvironmental Implications. Earth Science, 37(1): 35-46. doi: 10.3799/dqkx.2012.004
    Citation: DING Su-ting, SUN Bai-nian, WU Jing-yu, LI Xiang-chuan, 2012. Machilus Fossil from Miocene in Tiantai, Zhejiang Province, China, and Its Paleoenvironmental Implications. Earth Science, 37(1): 35-46. doi: 10.3799/dqkx.2012.004

    Machilus Fossil from Miocene in Tiantai, Zhejiang Province, China, and Its Paleoenvironmental Implications

    doi: 10.3799/dqkx.2012.004
    • Received Date: 2011-07-26
    • Publish Date: 2012-01-15
    • Six fossil leaves with fine venation and well-preserved cuticles of Machilus tiantaiensis Ding S. T. et Sun B. N. sp. nov. (Lauraceae) were discovered from the Late Miocene Xiananshan Formation of Tiantai County, eastern Zhejiang Province, China. The fossils were characterized by elliptic shape with entire margin, acuminate apex, cuneate base and pinnate venation; the anticlinal walls of epidermal cells are undulated, the unicellular trichome bases are mostly found on the veins; leaves hypostomatic, stomata paracytic with two embedded guard cells and one or two subsidiary cells. The leaf cuticular and architectural features of these fossil leaves suggest the affinity within the genus Machilus. The quantitative traits of leaf morphology were studied here, and a free data analysis package (palaeontological statistics) is utilized for cluster analysis. The leaf morphologic and cuticular features show that the fossil is similar to the modern leaves of M. pingii mostly. The paleoatmospheric CO2 concentration is estimated through the stomatal ratio between the fossil species and the extant M. pingii Cheng ex Yang (nearest living relative of the fossil species), and the result shows that the level of atmospheric CO2 in the Late Miocene of Tiantai is about 407.9×10-6. The modern trees of Machilus are distributed in tropical and subtropical regions of South and Southeast Asia, which indicates that the Miocene climate of eastern China was warm and humid.

       

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