Trend of Santonian (Late Cretaceous) atmospheric CO_2 and global mean land surface temperature: Evidence from plant fossils

查看全文 作　　者：WAN [1]ChuanBiao;WANG [2]DeHai;ZHU [2]ZhanPing;QUAN [3]Cheng

机构地区：[1]Exploration and Development Research Institute, Daqing Oilfield Company Ltd., Daqing 163712, China;[2]College ofGeoseiences, Jilin University, Changchun 130061, China;[3]Key Laboratory for Evolution of Past Life and Environment in Northeast China, MOE, Jilin University, Changchun 130026, China

出　　处：《Science China Earth Sciences》索引2011年第54卷第9期,共8页

基　　金：supported by the National Basic Research Pro-gram of China (Grant No. 2006CB701401);the National Natural Science Foundation of China (Grant No. 41002004);China Postdoctoral Science Foundation (Grant No. 20090451258);the Fund of LPS, Nanjing Insti-tute of Geology and Palaeontology, CAS (Grant No. 103107) 关键词：二氧化碳排放量晚白垩世植物化石地表温度温度趋势证据平均大气

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Trend of Santonian (Late Cretaceous) atmospheric CO_2 and global mean land surface temperature: Evidence from plant fossils

参考文献(13)

引证文献(8)

耦合文献(39)

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