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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
ISSN0034-6667
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
DOI10.1016/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
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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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