A new genus of Sphenopsida from the Lower Permian of the Parana Basin, Southern Brazil

被引:3
作者
Boardman, Daiana Rockenbach [1 ]
Iannuzzi, Roberto [1 ]
Dutra, Tania Lindner [2 ]
机构
[1] Univ Fed Rio Grande do Sul, Dept Paleontol & Estratig, Inst Geociencias, Ave Bento Goncalves 9500, BR-91509900 Porto Alegre, RS, Brazil
[2] Univ Vale Rio Sinos UNISINOS, Programa Posgrad Geol, Ave Unisinos 950, BR-93022000 Sao Leopoldo, RS, Brazil
关键词
Taxonomy; Paragiridia taioensis nov gen. et sp; Sphenopsida; Lower Permian; Rio Bonito Formation; Parana Basin; FOREST;
D O I
10.1016/j.revpalbo.2016.07.004
中图分类号
Q94 [植物学];
学科分类号
071001 ;
摘要
This study presents a new taxon of Sphenopsida, Paragiridia taioensis nov. gen. et sp. The specimens were recovered from the Bruno Peiker Outcrop, municipality of Taki, state of Santa Catarina in southern Brazil, and are preserved as impressions or compressions. They represent an autochthonous monospecific assemblage constituted of delicate plant parts, some of them still connected to each other, allowing a reconstruction of the whole plant. The root system of P. taioensis is composed of unbranched, non-articulate and continuously striated axes, covered with thin rootlets irregularly on the entire surface, sometimes dichotomized; Paracalamites-like articulated axes; and Phyllotheca-like leaf whorls. The reproductive structure is represented by fertile internodes, without bracts or foliar whorls between them. The sporangiophores are bifurcated at least once, non-peltate, with terminal clavate sporangia, densely but loosely arranged on the main axes, occurring in the middle to upper portion of the inter nodes. The natural new taxon, as reconstituted, lived in transitional environments that were exposed for relatively short periods, when the vegetation became established. These marginal areas were occasionally flooded and covered with large amounts of sediment that buried part or all of the community; when the water naturally receded, the plant individuals would have recolonized these marginal areas, probably using their continuously growing root systems for vegetative reproduction. In evolutionary terms, the group that includes Paragiridia and closely similar forms must have descended directly from Carboniferous Archaeocalamitaceae, in view of their simplified structure and lack of a pelta on their sporangiophores. Therefore, they probably represent a separate sphenopsid lineage, which evolved toward the development of a peltate sporangiophore organized in strobili. (C) 2016 Elsevier B.V. All rights reserved.
引用
收藏
页码:44 / 55
页数:12
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