Floristic similarities of the Artinskian Siderópolis Member macroflora, Rio Bonito formation (Paraná Basin, Brazil) with Cisuralian paleofloras of India

• Main Authors: Mary Elizabeth Cerruti Bernardes-de-Oliveira, Pauline Sabina Kavali, Sandra Eiko Mune, Maria Judite Garcia, Mahesh Shivanna, Roberto Iannuzzi, Karoline Gonçalves Pereira
• Format: Article
• Language: English
• Published: Universidade de São Paulo 2016-12-01
• Series: Geologia USP. Série Científica
• Subjects: Glossopteris; Western Gondwana; Eastern Gondwana; Artinskian.
• Online Access: http://www.revistas.usp.br/guspsc/article/view/124470

This contribution focuses on the relationship between the Siderópolis Member paleoflora and Indian Gondwanan paleofloras, especially with those of the Cisuralian stages, thus providing additional criteria for the correlation of Western and Eastern Gondwanan coal successions in the lower Permian interval. Despite the large number of species in common with the Karharbari Stage (Sakmarian) flora, the Siderópolis paleoflora exhibits a higher percentage and diversification of the genus Glossopteris, which is less expressive in the Karharbari Stage floras, while the declining Gangamopteris-Noeggerathiopsis complex in Siderópolis Member paleoflora still dominates the associations of Karharbari Stage. However, the floristic composition of the lower level of the Barakar Stage (Artinskian), despite having fewer species in common with the Siderópolis paleoflora, exhibits the characters of the latter vis-à-vis the dominance and diversity of the genus Glossopteris over the Gangamopteris‑Noeggerathiopsis complex, which decreases both in diversity as well as in abundance in the lower Barakar, similar to what occurs in the Brazilian paleoflora. The decline of the icehouse stage and the similar latitudinal position of the Gondwanan regions compared in the present study seem to have acted as important factors to the development of similar vegetation patterns in coal floras from Western (Brazilian) and Eastern (Indian) Gondwana during the Artinskian.