Search engine for discovering works of Art, research articles, and books related to Art and Culture
ShareThis
Javascript must be enabled to continue!

Platyspermic seeds from the Early Permian of Parana Basin, Brazil

View through CrossRef
This paper results from a taxonomic study of platyspermic seeds from taphofloristic assemblage of the "Toca do Indio Ranch", belonging to the upper portion of the Itarare Subgroup, Municipality of Cerquilho (SP) and a revision of material collected by Millan (1977) from the same area which is deposited in the National Museum of Rio de Janeiro. The assemblage comprises the Transitional Taphoflora (A-B) or the Gangamopteris-Rubidgea-Stephanophyllites association from the type-locality of Northeastern Parana Basin. This taphoflora is Early Permian (Asselian- Early Sakmarian) in age and records the beginning of the colonization of the Parana Basin by the proto-glossopterid and gangamopterid elements of the Glossopteris flora. It is, probably, correlated to the Argentinean "Lubeckense A" Floristic Stage or even a little older. The platyspermic seeds are assigned to the genera Samaropsis and Cordaicarpus. The assemblage is diversified and includes the taxa Cordaicarpus brasilianus n. sp., Samaropsis dolianitii Millan, S. rigbyi Millan, S. tietensis Millan, S cerquilhensis (Millan) comb. nov., S moreirana (White) Millan, S. goraiensis Surange & Lele, S. rugata sp. nov. and S rohnii sp.nov. The record of S. moreirana (White) Millan in the present study is the oldest from the Parana Basin and S. goraiensis Surange & Lele is recognized for the first time outside India. The wide variety of detached seeds reflect the diversification of the gymnosperms in this assemblage, putatively related to the last interglacial event of the Lower Gondwana glaciation in the Parana Basin. Biostratigraphic correlation based on seeds is not possible due to apparent endemic nature of the assemblage and further work in this field is required.
Title: Platyspermic seeds from the Early Permian of Parana Basin, Brazil
Description:
This paper results from a taxonomic study of platyspermic seeds from taphofloristic assemblage of the "Toca do Indio Ranch", belonging to the upper portion of the Itarare Subgroup, Municipality of Cerquilho (SP) and a revision of material collected by Millan (1977) from the same area which is deposited in the National Museum of Rio de Janeiro.
The assemblage comprises the Transitional Taphoflora (A-B) or the Gangamopteris-Rubidgea-Stephanophyllites association from the type-locality of Northeastern Parana Basin.
This taphoflora is Early Permian (Asselian- Early Sakmarian) in age and records the beginning of the colonization of the Parana Basin by the proto-glossopterid and gangamopterid elements of the Glossopteris flora.
It is, probably, correlated to the Argentinean "Lubeckense A" Floristic Stage or even a little older.
The platyspermic seeds are assigned to the genera Samaropsis and Cordaicarpus.
The assemblage is diversified and includes the taxa Cordaicarpus brasilianus n.
sp.
, Samaropsis dolianitii Millan, S.
rigbyi Millan, S.
tietensis Millan, S cerquilhensis (Millan) comb.
nov.
, S moreirana (White) Millan, S.
goraiensis Surange & Lele, S.
rugata sp.
nov.
and S rohnii sp.
nov.
The record of S.
moreirana (White) Millan in the present study is the oldest from the Parana Basin and S.
goraiensis Surange & Lele is recognized for the first time outside India.
The wide variety of detached seeds reflect the diversification of the gymnosperms in this assemblage, putatively related to the last interglacial event of the Lower Gondwana glaciation in the Parana Basin.
Biostratigraphic correlation based on seeds is not possible due to apparent endemic nature of the assemblage and further work in this field is required.

Related Results

Tectono-thermal evolution of the Junggar Basin, NW China: constraints from R o and apatite fission track modelling
Tectono-thermal evolution of the Junggar Basin, NW China: constraints from R o and apatite fission track modelling
The thermal evolution of the Junggar Basin, northwest China, was evaluated based on the thermal modelling results of 59 wells by using vitrinite reflectance (R o ...
Palynostratigraphy of Permian and Lower Triassic rocks, Sverdrup Basin, Canadian Arctic Archipelago
Palynostratigraphy of Permian and Lower Triassic rocks, Sverdrup Basin, Canadian Arctic Archipelago
Nine outcrop sections of Permian and Lower Triassic rocks were studied in the basin-margin and basin-centre facies of the Sverdrup Basin. Abundant, well preserved palynomorphs occu...
Mercury (Hg) anomalies and carbon isotope excursions as a stratigraphic marker for the Permian – Triassic mass extinction
Mercury (Hg) anomalies and carbon isotope excursions as a stratigraphic marker for the Permian – Triassic mass extinction
Mercury concentration anomalies in sedimentary successions are widely considered as proxies for volcanism and together with negative carbon isotope (δ13C) excursions, are ...
The Genetic Mechanism of the Sequence Stratigraphy of the Rift Lacustrine Basin in Jiyang Depression, East China
The Genetic Mechanism of the Sequence Stratigraphy of the Rift Lacustrine Basin in Jiyang Depression, East China
Abstract Through the studies of sequence stratigraphy of early Tertiary in the east part of Jiyang depression, the characteristics of sequence evolution in contin...
Successor Characteristics of the Mesozoic and Cenozoic Songliao Basins
Successor Characteristics of the Mesozoic and Cenozoic Songliao Basins
Abstract: The Songliao basin is a complex successor basin that was initiated in the Mesozoic and experienced multiple periods of reactivation. Based on seismic and drilling data, a...
Phase States of Hydrocarbons in Chinese Marine Carbonate Strata and Controlling Factors for Their Formation
Phase States of Hydrocarbons in Chinese Marine Carbonate Strata and Controlling Factors for Their Formation
Chinese marine strata were mainly deposited before the Mesozoic. In the Tarim, Sichuan and Ordos Basins, the marine source rocks are made of sapropelic dark shale, and calcareous s...
Permian rifting and detachment faults and their role in Alpine collisional tectonics
Permian rifting and detachment faults and their role in Alpine collisional tectonics
<p>The Permian was a time of strong crustal extension in the area of the later-formed Alpine orogen. This involved extensional detachment faulting and the formation o...
Pennsylvanian Rocks of Southwestern New Mexico and Southeastern Arizona
Pennsylvanian Rocks of Southwestern New Mexico and Southeastern Arizona
Abstract Pennsylvanian strata in southwestern New Mexico and southeastern Arizona range from Morrowan? to Virgilian in age, are disconformable to angularly unconform...

Back to Top