中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Permian/Triassic megaspores of Otynisporites (Fuglewicz) Karasev et Turnau, 2015: Diversity, botanical affinity, and stratigraphic significance

文献类型:期刊论文

作者Zavialova, Natalia1; Karasev, Eugeny1,2; Schneebeli-Hermann, Elke3; Li, Wenben4
刊名REVIEW OF PALAEOBOTANY AND PALYNOLOGY
出版日期2025-02-01
卷号333页码:36
关键词Megaspores SEM TEM Permian/Triassic boundary Stratigraphic marker Heterosporous lycopsids
ISSN号0034-6667
DOI10.1016/j.revpalbo.2024.105232
通讯作者Zavialova, Natalia(zavial@mail.ru)
英文摘要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.
WOS关键词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
语种英语
WOS记录号WOS:001367001900001
出版者ELSEVIER
资助机构RFBR ; Federal University for the state ; Swiss NSF
源URL[http://ir.nigpas.ac.cn/handle/332004/44623]  
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
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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.

入库方式: OAI收割

来源:南京地质古生物研究所

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