Secrospiroxylon tolgoyensis gen. nov. et sp. nov., a unique coniferous stem from the uppermost Permian of the South Gobi Basin, Mongolia, and its palaeoclimatic, palaeoecophysiological, and palaeoecological implications

被引:1
|
作者
Cai, Yao-Feng [1 ]
Zhang, Hua [1 ]
Feng, Zhuo [2 ]
Zhang, Yi-Chun
Yuan, Dong-Xun
Xu, Hai-Peng [4 ]
Byambajav, Uugantsetseg [1 ,5 ]
Yarinpuil, Ariunchimeg [5 ]
Shen, Shu-Zhong [3 ,4 ]
机构
[1] Chinese Acad Sci, Nanjing Inst Geol & Palaeontol, State Key Lab Palaeobiol & Stratig, 39 East Beijing Rd, Nanjing 210008, Peoples R China
[2] Yunnan Univ, Yunnan Key Lab Palaeobiol, MEC Int Joint Lab Palaeobiol & Palaeoenvironm, Inst Palaeontol,Yunnan Key Lab Earth Syst Sci, Kunming 650500, Peoples R China
[3] Nanjing Univ, Sch Earth Sci & Engn, State Key Lab Mineral Deposits Res, 163 Xianlin Ave, Nanjing 210023, Peoples R China
[4] Nanjing Univ, Frontiers Sci Ctr Crit Earth Mat Cycling, 163 Xianlin Ave, Nanjing 210023, Jiangsu, Peoples R China
[5] Mongolian Acad Sci, Inst Paleontol, POB 46-650,S Danzan St 3-1, Ulaanbaatar 15160, Mongolia
基金
中国国家自然科学基金;
关键词
fossil wood; fungus-plant-arthropod interactions; ecophysiological response; Angara; Permian; TYLOSIS FORMATION; WOOD-DECAY; BOGDA MOUNTAINS; CRUSTAL GROWTH; FOSSIL; PLANTS; RECONSTRUCTION; ARTHROPOD; EVOLUTION; COLLISION;
D O I
10.1127/palb/2023/0080
中图分类号
Q91 [古生物学];
学科分类号
0709 ; 070903 ;
摘要
A permineralised tree stem, Secrospiroxylon tolgoyensis Y.CAI, H.ZHANG et FENG gen. nov et sp. nov., is described from the uppermost Permian in the Tsaagan Tolgoy section of the South Gobi Basin, Mongolia. The coniferous stem is unique for combining a heterocellular pith, an endarch primary xylem, and a Prototaxoxylon-type secondary xylem. Growth rings are inconspicuously present in the studied stem, whereas false rings are commonly present throughout the secondary xylem, indicating ecophysiological anatomical responses to continuous environmental turbulence under indistinctive seasonal climatic conditions during the latest Permian. Arthropod wood borings with two coprolite classes are recognised, speculated to originate from detritivorous oribatid mites. In addition, fungal hyphae and white-rot decay structures are commonly identified in the stem. Our study provides novel information on the diversity of the Angaran flora and additional information on climatic and environmental fluctuations, as well as fungus-plant-arthropod interactions in the terrestrial ecosystems of the latest Permian of southern Mongolia.
引用
收藏
页码:93 / 119
页数:27
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