دورية أكاديمية

Eurydesma-Lyonia fauna (Early Permian) from the Itararé group, Paraná Basin (Brazil): A paleobiogeographic W-E trans-Gondwanan marine connection

التفاصيل البيبلوغرافية
العنوان: Eurydesma-Lyonia fauna (Early Permian) from the Itararé group, Paraná Basin (Brazil): A paleobiogeographic W-E trans-Gondwanan marine connection
المؤلفون: Taboada, Arturo César, Neves, Jacqueline Peixoto, Weinschütz, Luiz Carlos, Pagani, Maria Alejandra, Simões, Marcello Guimarães
المساهمون: Universidade Estadual Paulista (UNESP)
سنة النشر: 2016
المجموعة: Universidade Estadual Paulista São Paulo: Repositório Institucional UNESP
مصطلحات موضوعية: Biocorrelation, Early Permian, Eurydesma, Itararé group, Lyonia, W-E Gondwana marine connection
الوصف: Here, the biocorrelation of the marine invertebrate assemblages of the post-glacial succession in the uppermost portion of the Late Paleozoic Itararé Group (Paraná Basin, Brazil) is for the first time firmly constrained with other well-dated Gondwanan faunas. The correlation and ages of these marine assemblages are among the main controversial issues related to Brazilian Gondwana geology. In total, 118 brachiopod specimens were analyzed, and at least seven species were identified: Lyonia rochacamposi sp. nov., Langella imbituvensis (Oliveira),? Streptorhynchus sp.,? Cyrtella sp., Tomiopsis sp. cf. T. harringtoni Archbold and Thomas, Quinquenella rionegrensis (Oliveira) and Biconvexiella roxoi Oliveira. The presence of Tomiopsis sp. cf. T. harringtoni and the bivalve Atomodesma (Aphanaia) orbirugata (Harrington) in the Teixeira Soares beds plus Myonia argentinensis (Harrington) and Heteropecten paranaensis Neves et al., both of which recorded in deposits in the Teixeira Soares and Mafra beds (Butiá), suggests a biocorrelation with the Eurydesma fauna from the Bonete Formation, Sauce Grande-Colorado Basin, Argentina. Furthermore, the presence of Lyonia Archbold and Praeundulomya cf. subelongata Dickins in the Taciba Formation indicates affinities with deposits in the Lyons Group, Carnarvon Basin, and the Fossil Cliff Member, Perth Basin (Western Australia), suggesting a late Asselian-early Sakmarian age. Even more importantly, the collected data suggest the existence of an W-E trans-Gondwanan marine seaway between the Paraná (Brazil), Sauce Grande-Colorado (Argentina), Huab (Hardap shale of the Dwyka Group, Aranos area, Namibia, southwest Africa), the Carnavon (Western Australia) basins, and beyond eastward to the Cimmerian region. A V proto-rift system through two major axes of extensional basin development facilitated the W-E marine connection. Main axes formed by a north-northwesterly trending axis paralleling the future South Atlantic and a broadly north-northeasterly trending line of separation related to the ...
نوع الوثيقة: article in journal/newspaper
وصف الملف: 431-454
اللغة: English
ردمك: 978-3-9521630-1-6
3-9521630-1-5
تدمد: 0031-0182
العلاقة: Palaeogeography, Palaeoclimatology, Palaeoecology; 1,285; http://dx.doi.org/10.1016/j.palaeo.2016.02.022Test; Palaeogeography, Palaeoclimatology, Palaeoecology, v. 449, p. 431-454.; http://hdl.handle.net/11449/172653Test; 2-s2.0-84960154857; 2-s2.0-84960154857.pdf; 3952163015625103
DOI: 10.1016/j.palaeo.2016.02.022
الإتاحة: https://doi.org/10.1016/j.palaeo.2016.02.022Test
http://hdl.handle.net/11449/172653Test
حقوق: openAccess
رقم الانضمام: edsbas.31C9DD83
قاعدة البيانات: BASE
الوصف
ردمك:9783952163016
3952163015
تدمد:00310182
DOI:10.1016/j.palaeo.2016.02.022