A new Protophyllocladoxylon stem from the Xishanyao Formation (Middle Jurassic) in the Santanghu Basin, Xinjiang, Northwest China

被引:8
|
作者
Gou, Xu-Dong [1 ]
Feng, Zhuo [1 ,2 ]
Wei, Hai-Bo [1 ]
Lv, Yong [2 ]
Yang, Shi-Ling [3 ,4 ,5 ]
机构
[1] Yunnan Univ, MEC Int Joint Lab Palaeobiol & Palaeoenvironm, Yunnan Key Lab Palaeobiol, Yunnan Key Lab Earth Syst Sci,Inst Palaeontol, Kunming 650500, Yunnan, Peoples R China
[2] Chinese Acad Geol Sci, Inst Karst Geol, Guilin 541004, Peoples R China
[3] Chinese Acad Sci, Inst Geol & Geophys, Key Lab Cenozo Geol & Environm, Beijing 100029, Peoples R China
[4] CAS Ctr Excellence Life & Paleoenvironm, Beijing 100044, Peoples R China
[5] Univ Chinese Acad Sci, Coll Earth & Planetary Sci, Beijing 100049, Peoples R China
基金
中国国家自然科学基金;
关键词
Protophyllocladoxylon yiwuense Gou et Feng sp. nov; Plant-fungal interaction; Growth-ring analysis; Middle Jurassic; China; NORTHERN BOGDA MOUNTAINS; MESOZOIC FOSSIL WOOD; JUNGGAR BASIN; SP NOV; CONIFER WOOD; GROWTH RINGS; SELECTIVE DELIGNIFICATION; WUTONGGOU FORMATION; PETRIFIED FOREST; DECAYING FUNGI;
D O I
10.1016/j.revpalbo.2021.104474
中图分类号
Q94 [植物学];
学科分类号
071001 ;
摘要
A new permineralized stem, Protophyllocladoxylon yiwuense Gou et Feng sp. nov., is described from the Middle Jurassic Xishanyao Formation in Naomaohu Town of Yiwu County, Hami City, Xinjiang Uygur Autonomous Region, Northwest China. The stem is only preserved with secondary xylem, which is pycnoxylic and exclusively composed of tracheids and parenchymatous rays. The tracheids have uniseriate or biseriate, alternately arranged bordered pits on their radialwalls, and uniseriate bordered pits on the tangentialwalls. The rays are uniseriate or partially biseriate, up to 34 cells high. There are one or two large, simple pits in each cross field. A branch trace horizontally passes through the secondary xylem showing anatomical structures identical to the secondary xylem. Analyses of the growth-ringwidth and mean sensitivity values indicate that P. yiwuense had long growing seasons with readily available water supplies and favorable paleoclimatic conditions. White-rot decay features are commonly recognized in the stem, including pocket-like cavities, complete removal of the middle lamellae, thickened corners and separation of the secondary walls of tracheids, as well as septa-like structures in the tracheid lumens due to the cell's reactions to fungal activity. Our study sheds new light into the plant diversity and paleoenvironmental and paleoecological conditions of the Middle Jurassic. (C) 2021 The Authors. Published by Elsevier B.V.
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页数:13
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