KMS Nanjing Institute of Geology and Palaeonotology,CAS
Permian/Triassic megaspores of Otynisporites (Fuglewicz) Karasev et Turnau, 2015: Diversity, botanical affinity, and stratigraphic significance | |
通讯作者 | Zavialova, Natalia([email protected]) |
Zavialova, Natalia1; Karasev, Eugeny1,2; Schneebeli-Hermann, Elke3; Li, Wenben4 | |
2025-02-01 | |
发表期刊 | REVIEW OF PALAEOBOTANY AND PALYNOLOGY
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ISSN | 0034-6667 |
卷号 | 333页码:36 |
摘要 | Megaspores of Otynisporites eotriassicus, O. tuberculatus, and O. maculosus from the latest Changhsingian-early Induan of the Moscow Basin of Russia, O. eotriassicus from the Induan of the Kap Stosch subbasin of East Greenland, and O.? tarimensis, and Otynisporites? sp. from the Middle Triassic of the Tarim Basin of China were studied using light, scanning and transmission electron microscopy. The general morphology and sporoderm ultrastructure of all specimens prove their affinity with heterosporous lycopsids, but they are unexpectedly variable in details of the sculpture and ultrastructure. Megaspores of Otynisporites? sp. and O.? tarimensis differ significantly from the other studied megaspores and probably were produced by a different heterosporous lycopsid. Three morphological groups are distinguished within O. eotriassicus. Multilamellated zones are found only in O. tuberculatus and (much less distinct) in O. maculosus, that leads to the necessity to re-evaluate the phylogenetic value of this character. Analysis of morphology, stratigraphic and geographic ranges of earlier reports of Otynisporites shows that confirmed findings are confined to the latest Changhsingian-Induan, with O. tuberculatus and O. maculosus sharing the same stratigraphic range as O. eotriassicus. The geographic distribution shows that Otynisporites-producing plants grew under a moderately warm climate, in the middle latitudes. A comparison with the composition of palynological assemblages from megaspore-containing deposits implies that parent plants of O. eotriassicus, O. tuberculatus, and O. maculosus more probably produced trilete cavate microspores, Lundbladispora might be a counterpart for O. eotriassicus, whereas parent plants of O.? tarimensis and Otynisporites? sp. more probably produced monolete microspores. |
关键词 | Megaspores SEM TEM Permian/Triassic boundary Stratigraphic marker Heterosporous lycopsids |
DOI | 10.1016/j.revpalbo.2024.105232 |
收录类别 | SCI |
语种 | 英语 |
关键词[WOS] | PERMIAN-TRIASSIC BOUNDARY ; SPORE WALL ULTRASTRUCTURE ; KAP STOSCH ; MASS EXTINCTION ; MADHYA-PRADESH ; PLEUROMEIA ; MORPHOLOGY ; SUCCESSION ; ANNALEPIS ; EVOLUTION |
资助项目 | RFBR[19-04-00498] ; Federal University for the state[FZSM-2023-0023] ; Swiss NSF[20021-135446/1] |
WOS研究方向 | Plant Sciences ; Paleontology |
WOS类目 | Plant Sciences ; Paleontology |
WOS记录号 | WOS:001367001900001 |
项目资助者 | RFBR ; Federal University for the state ; Swiss NSF |
出版者 | ELSEVIER |
文献类型 | 期刊论文 |
条目标识符 | http://ir.nigpas.ac.cn/handle/332004/44624 |
专题 | 中国科学院南京地质古生物研究所 |
通讯作者 | Zavialova, Natalia |
作者单位 | 1.Russian Acad Sci, Borissiak Paleontol Inst, Moscow, Russia 2.Kazan Volga Reg Fed Univ, Kazan, Russia 3.Univ Zurich, Zurich, Switzerland 4.Chinese Acad Sci, Nanjing Inst Geol & Palaeontol, Nanjing, Peoples R China |
推荐引用方式 GB/T 7714 | Zavialova, Natalia,Karasev, Eugeny,Schneebeli-Hermann, Elke,et al. Permian/Triassic megaspores of Otynisporites (Fuglewicz) Karasev et Turnau, 2015: Diversity, botanical affinity, and stratigraphic significance[J]. REVIEW OF PALAEOBOTANY AND PALYNOLOGY,2025,333:36. |
APA | Zavialova, Natalia,Karasev, Eugeny,Schneebeli-Hermann, Elke,&Li, Wenben.(2025).Permian/Triassic megaspores of Otynisporites (Fuglewicz) Karasev et Turnau, 2015: Diversity, botanical affinity, and stratigraphic significance.REVIEW OF PALAEOBOTANY AND PALYNOLOGY,333,36. |
MLA | Zavialova, Natalia,et al."Permian/Triassic megaspores of Otynisporites (Fuglewicz) Karasev et Turnau, 2015: Diversity, botanical affinity, and stratigraphic significance".REVIEW OF PALAEOBOTANY AND PALYNOLOGY 333(2025):36. |
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