Charred wood of Prototaxoxylon from the Wuchiapingian Wutonggou Formation (Permian) of Dalongkou, northern Bogda Mountains, northwestern China | |
Wan, Ming-Li1,2; Zhou, Wei-Ming3; Yang, Wan4,5; Wang, Jun1,2 | |
刊名 | PALAEOWORLD |
2016 | |
卷号 | 25期号:1页码:21-31 |
关键词 | Charcoal Prototaxoxylon Angara Flora Spiral Thickenings Wuchiapingian |
DOI | 10.1016/j.palwor.2015.06.003 |
文献子类 | Article |
英文摘要 | Charred wood occurs sporadically in sedimentary rocks in China. A marcroscopic charcoal with well-preserved anatomical structure is described from the Wuchiapiangian Wutonggou Formation in the southern part of Dalongkou section, northern Bogda Mountains in the Junggar Basin, northwestern China. It is characterized by uniseriate radial tracheidal pitting, taxaceous tertiary spiral thickenings in the tracheidal walls, uniseriate tangential tracheidal pitting, homogeneous, uniseriate, 2-10 cells high xylem rays, and 1-2 pits in each cross-field. It is assigned to Prototaxoxylon uniseriale Prasad. The uniseriate, bordered, contiguous, rarely separate tangential pitting of P uniseriale is evidenced clearly for the first time. The features of this species show a close affinity with conifers. The coniferous charred wood may have been derived from an extrabasinal forest, perhaps from upland environment deep within the hinterland, according to results of modern taphonomic research. (C) 2015 Elsevier B.V. and Nanjing Institute of Geology and Palaeontology, CAS. All rights reserved. |
WOS关键词 | CORDAITALEAN SEED PLANTS ; PARANA BASIN ; CHARCOAL REMAINS ; MASS EXTINCTION ; INNER-MONGOLIA ; SOUTH-AMERICA ; WILDFIRES ; RECONSTRUCTION ; ARGENTINA ; DEPOSITS |
WOS研究方向 | Paleontology |
语种 | 英语 |
WOS记录号 | WOS:000371910500003 |
资助机构 | National Basic Research Program of China (973 Program)(2012CB821901) ; National Basic Research Program of China (973 Program)(2012CB821901) ; National Natural Science Foundation of China(41372011 ; National Natural Science Foundation of China(41372011 ; University of Missouri Research Board ; University of Missouri Research Board ; Institute of Geology and Geophysics of Chinese Academy of Sciences(2011ZX05008-004-053) ; Institute of Geology and Geophysics of Chinese Academy of Sciences(2011ZX05008-004-053) ; 41372010 ; 41372010 ; 41472005) ; 41472005) ; National Basic Research Program of China (973 Program)(2012CB821901) ; National Basic Research Program of China (973 Program)(2012CB821901) ; National Natural Science Foundation of China(41372011 ; National Natural Science Foundation of China(41372011 ; University of Missouri Research Board ; University of Missouri Research Board ; Institute of Geology and Geophysics of Chinese Academy of Sciences(2011ZX05008-004-053) ; Institute of Geology and Geophysics of Chinese Academy of Sciences(2011ZX05008-004-053) ; 41372010 ; 41372010 ; 41472005) ; 41472005) |
内容类型 | 期刊论文 |
源URL | [http://ir.iggcas.ac.cn/handle/132A11/62030] |
专题 | 地质与地球物理研究所_中国科学院油气资源研究重点实验室 |
作者单位 | 1.Chinese Acad Sci, Nanjing Inst Geol & Palaeontol, Dept Palaeobot & Palynol, Nanjing 210008, Peoples R China 2.Chinese Acad Sci, Nanjing Inst Geol & Palaeontol, State Key Lab Palaeobiol & Stratig, Nanjing 210008, Peoples R China 3.Nanjing Univ, Sch Earth Sci & Engn, Nanjing 210023, Jiangsu, Peoples R China 4.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Petr Resources Res, Beijing 100029, Peoples R China 5.Missouri Univ Sci & Technol, Geol & Geophys Program, Rolla, MO 65409 USA |
推荐引用方式 GB/T 7714 | Wan, Ming-Li,Zhou, Wei-Ming,Yang, Wan,et al. Charred wood of Prototaxoxylon from the Wuchiapingian Wutonggou Formation (Permian) of Dalongkou, northern Bogda Mountains, northwestern China[J]. PALAEOWORLD,2016,25(1):21-31. |
APA | Wan, Ming-Li,Zhou, Wei-Ming,Yang, Wan,&Wang, Jun.(2016).Charred wood of Prototaxoxylon from the Wuchiapingian Wutonggou Formation (Permian) of Dalongkou, northern Bogda Mountains, northwestern China.PALAEOWORLD,25(1),21-31. |
MLA | Wan, Ming-Li,et al."Charred wood of Prototaxoxylon from the Wuchiapingian Wutonggou Formation (Permian) of Dalongkou, northern Bogda Mountains, northwestern China".PALAEOWORLD 25.1(2016):21-31. |
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