Septomedullopitys szei sp nov., a new gymnospermous wood from Lower Wuchiapingian (Upper Permian) continental deposits of NW China, and its implication for a weakly seasonal humid climate in mid-latitude NE Pangaea
Wan, Mingli1,2; Yang, Wan3,4; Wang, Jun1
刊名PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY
2014-08-01
卷号407页码:1-13
关键词Septomedullopitys szei sp nov. Coprolites Fossil wood Palaeoclimate Late Permian China
ISSN号0031-0182
DOI10.1016/j.palaeo.2014.04.011
文献子类Article
英文摘要Septomedullopitys szei sp. nov. is described from the Wuchiapingian Wutonggou Formation of Tarlong Valley, southern Bogda Mountains, Xinjiang, in northwestern China. The stem has a heterogeneous pith ca 15-20 mm in diameter, and containing numerous linear secretory ducts and parenchymatous bands. Primary xylem is endarch and the tracheids contain scalariform thickenings. Secondary xylem is of the Protophyllocladoxylon type. Comparisons with contemporaneous gymnospermous woods containing either heterogeneous pith with ducts or Protophyllocladoxylon-type secondary xylem from the Angara palaeocontinent indicate that the Tarlong stem represents a new Permian morphotaxon for the region. The presence of coprolites, borings, and spindle-shaped cavities within the stem suggests well-developed animal-plant-fungi interactions. The occurrence of numerous growth interruptions and absence of true growth rings within the stem suggest weak seasonality of annual precipitation.-The interruptions suggest a humid climate with short-term, nonperiodic droughts. (C) 2014 Elsevier B.V. All rights reserved.
WOS关键词CORDAITALEAN SEED PLANTS ; ENVIRONMENTAL-FACTORS ; NORTHEASTERN BRAZIL ; PARNAIBA BASIN ; CONIFER WOODS ; GROWTH RINGS ; RECONSTRUCTION ; ANTARCTICA ; TREES ; STEM
WOS研究方向Physical Geography ; Geology ; Paleontology
语种英语
出版者ELSEVIER SCIENCE BV
WOS记录号WOS:000337777500001
资助机构Chinese Academy of Sciences(KZCX2-EW-120) ; Chinese Academy of Sciences(KZCX2-EW-120) ; National Basic Research Program of China (973 Program)(2012CB821901) ; National Basic Research Program of China (973 Program)(2012CB821901) ; National Nature Science Foundation of China ; National Nature Science Foundation of China ; 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) ; Chinese Academy of Sciences(KZCX2-EW-120) ; Chinese Academy of Sciences(KZCX2-EW-120) ; National Basic Research Program of China (973 Program)(2012CB821901) ; National Basic Research Program of China (973 Program)(2012CB821901) ; National Nature Science Foundation of China ; National Nature Science Foundation of China ; 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) ; Chinese Academy of Sciences(KZCX2-EW-120) ; Chinese Academy of Sciences(KZCX2-EW-120) ; National Basic Research Program of China (973 Program)(2012CB821901) ; National Basic Research Program of China (973 Program)(2012CB821901) ; National Nature Science Foundation of China ; National Nature Science Foundation of China ; 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) ; Chinese Academy of Sciences(KZCX2-EW-120) ; Chinese Academy of Sciences(KZCX2-EW-120) ; National Basic Research Program of China (973 Program)(2012CB821901) ; National Basic Research Program of China (973 Program)(2012CB821901) ; National Nature Science Foundation of China ; National Nature Science Foundation of China ; 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)
内容类型期刊论文
源URL[http://ir.iggcas.ac.cn/handle/132A11/85896]  
专题中国科学院地质与地球物理研究所
通讯作者Wang, Jun
作者单位1.Chinese Acad Sci, State Key Lab Palaeobiol & Stratig, Nanjing Inst Geol & Palaeontol, Nanjing 210008, Jiangsu, Peoples R China
2.Univ Chinese Acad Sci, Beijing 100049, Peoples R China
3.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Petr Resources Res, Beijing 100029, Peoples R China
4.Missouri Univ Sci & Technol, Geol & Geophys Program, Rolla, MO 65409 USA
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Wan, Mingli,Yang, Wan,Wang, Jun. Septomedullopitys szei sp nov., a new gymnospermous wood from Lower Wuchiapingian (Upper Permian) continental deposits of NW China, and its implication for a weakly seasonal humid climate in mid-latitude NE Pangaea[J]. PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY,2014,407:1-13.
APA Wan, Mingli,Yang, Wan,&Wang, Jun.(2014).Septomedullopitys szei sp nov., a new gymnospermous wood from Lower Wuchiapingian (Upper Permian) continental deposits of NW China, and its implication for a weakly seasonal humid climate in mid-latitude NE Pangaea.PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY,407,1-13.
MLA Wan, Mingli,et al."Septomedullopitys szei sp nov., a new gymnospermous wood from Lower Wuchiapingian (Upper Permian) continental deposits of NW China, and its implication for a weakly seasonal humid climate in mid-latitude NE Pangaea".PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY 407(2014):1-13.
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