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作 者:QUAN Cheng FU Qiong Yao SHI Gong Le LIU Yu Sheng LI Long LIU Xiao Yan JIN Jian Hua
机构地区:[1]Research Center of Paleontology and Stratigraphy, Jilin University [2]State Key Laboratory of Biocontrol and Guangdong Provincial Key Laboratory of Plant Resources, School of Life Sciences,Sun Yat-sen University [3]Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences [4]Office of Research and Graduate Studies, Prairie View A & M University
出 处:《Science China Earth Sciences》2016年第3期445-448,共4页中国科学(地球科学英文版)
基 金:the National Natural Science Foundation of China (Grant Nos. 41210001, 41372002 & 41528201);National Basic Research Program of China (Grant No. 2012CB822003)
摘 要:Mummified fossils are extraordinarily important for understanding both biotic evolution and ecology in the geological time,by uniquely providing a far more detailed source of information in comparison to impression materials.However,mummified fossils are extremely rare because of the inevitable requirement of unusual preservation conditions during fossilization,including the lithological features and deposition rate of surrounding rocks,and moisture and temperature conditions(Taylor et al.,2009).To date,only a few Cenozoic sites have been reported to yield mummified plant fossils around the world,Mummified fossils are extraordinarily important for understanding both biotic evolution and ecology in the geological time,by uniquely providing a far more detailed source of information in comparison to impression materials.However,mummified fossils are extremely rare because of the inevitable requirement of unusual preservation conditions during fossilization,including the lithological features and deposition rate of surrounding rocks,and moisture and temperature conditions(Taylor et al.,2009).To date,only a few Cenozoic sites have been reported to yield mummified plant fossils around the world,such as the middle
关 键 词:fossilization preservation inevitable Cenozoic uniquely ecology extremely moisture providing Miocene
分 类 号:Q914[天文地球—古生物学与地层学] P534.614[生物学—古生物学]
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