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Fossil plant evidence for Early and Middle Jurassic paleoenvironmental changes in Lanzhou area, Northwest China

✍ Scribed by Bai-Nian Sun; San-Ping Xie; De-Fei Yan; Pei-Yun Cong


Book ID
103878210
Publisher
Elsevier Science
Year
2008
Tongue
English
Weight
627 KB
Volume
17
Category
Article
ISSN
1871-174X

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✦ Synopsis


Estimating the paleoclimate changes through CO 2 levels has become a promising area of geological research. This paper focuses on analysis of fossil Ginkgo in continuous sedimentary series in northwestern China using plant anatomy and organic geochemistry approaches. The CO 2 variation curve during Early and Middle Jurassic is reconstructed based on the stomatal ratio method, which is consistent with the estimated results of GEOCARB III. In comparison with the carbon isotopic composition measured from the fossil leaves of Ginkgo, we suggest that the stomata-based CO 2 concentrations for the Jurassic are generally consistent with the predictions of the geochemical model, ranging from 1000 to 1600 ppmv. Measurements of carbon isotope values demonstrate that the water use efficiency of the fossil Ginkgo in a "green house" world is higher than that of the living Ginkgo. Investigations of physiological responses of plants to the increasing CO 2 level at the present and in the future should help demonstrate this effect. The cause of the carbon isotopic shift at the boundary between Aalenian and Bajocian for the Yaojie Basin is unclear and therefore needs further investigation.