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First record of Brachyoxylon wood from Upper Jurassic of Sichuan Basin, Southwest China and its paleoenvironmental significance
被引:0
|作者:
Xie, Ao-Wei
[1
]
Wang, Yong-Dong
[2
]
Tian, Ning
[3
]
Jiang, Zi-Kun
[4
]
Xie, Xiao-Ping
[5
]
Xi, Shu-Na
[6
]
Bai, Shi-Hui
[6
]
Uhl, Dieter
[1
]
机构:
[1] Senckenberg Forsch Inst & Naturmuseum, Senckenberganlage 25, D-60325 Frankfurt, Germany
[2] Chinese Acad Sci, State Key Lab Palaeobiol & Stratig, Nanjing Inst Geol & Palaeontol, Nanjing 210008, Peoples R China
[3] Shenyang Normal Univ, Coll Palaeontol, Shenyang 110034, Peoples R China
[4] Chinese Acad Geol Sci, Beijing 100037, Peoples R China
[5] Qufu Normal Univ, Sch Geog & Tourism, Rizhao 276826, Peoples R China
[6] 11th Geol Brigade Sichuan, Dazhou 635000, Peoples R China
来源:
关键词:
xylology;
Brachyoxylon sp;
Penglaizhen Formation;
paleoclimate;
Shehong;
FOSSIL WOOD;
BIODIVERSITY;
REAPPRAISAL;
GENERA;
ASIA;
D O I:
10.1016/j.palwor.2024.11.007
中图分类号:
Q91 [古生物学];
学科分类号:
0709 ;
070903 ;
摘要:
Diverse and abundant foliage fossils are well known and well documented from the Upper Triassic to the Lower and Middle Jurassic of the Sichuan Basin in Southwest China. Yet, the fossil record of Upper Jurassic plants in this region is sparse. Decades ago, hundreds of fossil wood specimens were unearthed from the Upper Jurassic in the central part of the Sichuan Basin, offering important insights into the region's past terrestrial ecosystems and paleoclimate. Despite their significance, systematic studies of these fossils have been limited. Here, we describe the anatomy of a fossil wood specimen from the Upper Jurassic Penglaizhen Formation in Shehong City, Sichuan Province. The specimen displays key Brachyoxylon features, including mixed radial tracheid pitting in conjunction with araucarioid cross-field pitting. This is the first record of the coniferous wood Brachyoxylon in the central Sichuan Basin. Paleoclimatic evidence from associated leaves, pollen, and sediments, suggests that these trees thrived under generally warm and semi-arid to arid conditions, likely in riparian and lacustrine environments with local water abundance, as indicated by the growth rings with narrow latewood bands. (c) 2024 Elsevier B.V. and Nanjing Institute of Geology and Palaeontology, CAS. This is an open access article under the CC BY license (http://
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