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作 者:Yuting Zhong Magdalena H.Huyskens Qing-Zhu Yin Yaqiong Wang Qiang Ma Yi-Gang Xu
机构地区:[1]State Key Laboratory of Isotope Geochemistry,Guangzhou Institute of Geochemistry,Chinese Academy of Sciences,China [2]CAS Center for Excellence in Deep Earth Science,China [3]Department of Earth and Planetary Sciences,University of California at Davis,USA [4]State Key Laboratory of Palaeobiology and Stratigraphy,Nanjing Institute of Geology and Palaeontology and Center for Excellence in Life and Paleoenvironment,Chinese Academy of Sciences,China [5]State Key Laboratory of Geological Processes and Mineral Resources,School of Earth Sciences,China University of Geosciences,China
出 处:《National Science Review》2021年第6期111-113,共3页国家科学评论(英文版)
基 金:This work was supported by the National Natural Science Foundation of China(41688103 and41873018);the Strategic Priority Research Program(B)of the Chinese Academy of Sciences(XDB18000000)。
摘 要:The Early Cretaceous Jehol Biota,renowned for its exceptionally wellpreserved volcanic-influenced ecosystem, was buried in lacustrine and occasionally fluvial sediments. This includes, notably, the Huajiying, Yixian and Jiufotang Formations in northern Hebei and western Liaoning and equivalent ash-interbedding sediments in neighboring areas [1–3](Fig. 1). It harbors many evolutionarily significant taxonomies, e.g. feathered dinosaurs,early birds, mammals and flowering plants, representing one of the most diversified terrestrial biotas of the Mesozoic [1,2,4].
关 键 词:BEDDING VOLCANIC FLUVIAL
分 类 号:Q915[天文地球—古生物学与地层学]
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