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首页> 外文期刊>Palaeobotanist >Pennsylvanian megaspores from northeastern border of the Paraná Basin, Brazil: Correlation with Indian Gondwana megaspores
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Pennsylvanian megaspores from northeastern border of the Paraná Basin, Brazil: Correlation with Indian Gondwana megaspores

机译:来自巴西巴拉那盆地东北边界的宾夕法尼亚州大孢子:与印度冈​​瓦纳大孢子的相关性

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摘要

Analysis of sediments from Campinas and Monte Mor, municipalities of the State of S?o Paulo, Brazil, has revealed the presence of new megaspores in addition to the known taxa. Trilete, alete, azonate and gulate dispersed fossil megaspores were recorded from the lower and middle levels of the Itararé Group from the northeastern border of the Paraná Basin (Lower Pennsylvanian) of Campinas municipality (Upper Bashkirian - Lower Moscovian) and of Monte Mor municipality (Kazimovian). Twenty-four species of megaspores recovered from one or both of these localities have been systematically analyzed and the synonymy of four previously described megaspores has been discussed. The present study of megaspores from Campinas reveals the presence of the taxa Banksisporites dijkstrae, B. endosporitiferus, B. utkalensis, Biharisporites spinosus, Bokarosporites psilatus, B. rotundus, Duosporites perversus, Duosporites sp. a, Lagenicula horrida, Lagenicula sp., L. nudus, L. rugosus, Lagenoisporites cf. L. hispanicus and Lagenoisporites. sp. The megaspores from Monte Mor includes the taxa Bokarosporites rotundus, Duosporites sp. b, Lagenoisporites nudus, L rugosus and L. cf. L. hispanicus. The taxa Bokarosporites rotundus, B. psilatus, Banksisporites utkalensis, B. endosporitiferus, B. dijkstrae and Biharisporites spinosus are also known from the Permian of India. Banksisporites tenuis previously detected in Campinas and Monte Mor localities is also a species which is shared with India. The presence of these taxa in the Pennsylvanian of the Paraná Basin, Brazil indicates their appearance in the Carboniferous. While all of them persisted up to the Permian, some like Biharisporites spinosus, Banksisporites tenuis and B. utkalensis extend up to Triassic and Early Cretaceous as well. The presence of these megaspores both in India and in Brazil indicates the occurrence of common ancestral heterosporous early land plants. An attempt has been made to interpret the palaeogeographic distribution pattern of some of the megaspores which appeared earlier in Brazil as compared to India, suggesting the floral migration from Brazil towards India.
机译:对巴西圣保罗州坎皮纳斯和蒙特莫尔的沉积物进行的分析表明,除了已知的分类群以外,还存在新的大孢子。在坎皮纳斯市(上Bashkirian-下莫斯科州)的Paraná盆地(下宾夕法尼亚州)东北边界的Itararé小组的中低层记录了由Triarae,etale,azonate和gulate分散的大孢子化石大孢子。 Kazimovian)。从一个或两个地点回收的二十四个大孢子已被系统地分析,并且已经讨论了四个先前描述的大孢子的同义词。目前对来自坎皮纳斯的大孢子的研究表明,存在以下类群:Banksisporites dijkstrae,B.endosporitiferus,B.utkalensis,Biharisporites spinosus,Bokarosporites psilatus,B.rotundus,Duosporites perversus,Duosporites sp。 a。Lagenicula horrida,Lagenicula sp。,L. nudus,L. rugosus,Lagenoisporites cf. L. hispanicus和Lagenoisporites。 sp。来自蒙特莫尔的大孢子包括圆形分类单元Bokarosporites,Duosporites sp.。 b,裸核孢子虫,皱纹L.和L。西班牙乳杆菌。从印度的二叠纪也已知类群Bokarosporites,B。psilatus,Banksisporites utkalensis,B.endosporitiferus,B.dijkstrae和Biharisporites spinosus。先前在坎皮纳斯(Campinas)和蒙特莫尔(Monte Mor)地区发现的班克斯银行(Banksisporites tenuis)也是印度共有的物种。这些类群在巴西巴拉那盆地的宾夕法尼亚州中的存在表明它们出现在石炭纪。尽管它们都一直持续到二叠纪,但像Biharisporites spinosus,Banksisporites tenuis和B. utkalensis一直延伸到三叠纪和早白垩世。在印度和巴西,这些大孢子的存在表明共同祖先异地早期陆地植物的出现。试图解释一些大孢子的古地理分布模式,这些大孢子在巴西比印度早出现,这表明花卉从巴西向印度迁移。

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