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Miguel A. Torres-Martínez

Researcher at National Autonomous University of Mexico

Publications -  26
Citations -  114

Miguel A. Torres-Martínez is an academic researcher from National Autonomous University of Mexico. The author has contributed to research in topics: Permian & Carboniferous. The author has an hindex of 5, co-authored 21 publications receiving 64 citations.

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Permian (Leonardian) brachiopods from Paso Hondo Formation, Chiapas, southern Mexico. Paleobiogeographical implications

TL;DR: In this article, Dyoros (Lissosia ) maya and Hustedia shumardi are proposed as a new species of brachiopod from the Paso Hondo Formation.
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Response of the western proto-North Atlantic margin to the early Aptian oceanic anoxic event (OAE) 1a: an example from the Cupido platform margin-Gulf of Mexico, NE Mexico

TL;DR: In this paper, microfacies and geochemical analyses conducted on five stratigraphic sections in northeastern Mexico (ancentral western margin of the proto-North Atlantic) reveal major paleoenvironmental changes in shallow water and pelagic environments in the prelude and run-up of the early Aptian oceanic anoxic event (OAE) 1a.
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Permian brachiopods from Chiapas, Mexico: new stratigraphical and paleobiogeographical insights

TL;DR: In this paper, eleven brachiopod species from the Paso Hondo Formation in the Chicomuselo region of southern Chiapas, Mexico are described, including Dyoros (Tetragonetes) rectangulatus, Costispinifera rugatula, Echinosteges tuberculatus, Tropidelasma furcillatum, Acosarina rectimarginata, Tautosia transenna, Composita hapsida, and Neospirifer venezuelensis.
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Paleoecology of the first Devonian-like sclerobiont association on Permian brachiopods from southeastern Mexico

TL;DR: In this article, a sclerobiont association from the Paso Hondo Formation (Roadian, middle Permian), Chiapas, Mexico is described, which is similar to those recorded in different Devonian localities, especially by the cooccurrence of microconchids, hederelloids, and bryozoans.
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Depositional paleoenvironments of the Lower Permian (upper Cisuralian) carbonate succession of Paso Hondo Formation in Chiapas State, southeastern Mexico

TL;DR: A microfacies analysis carried out on the carbonate rocks of a stratigraphic section, allowed for the first time the recognition of the depositional conditions that prevailed in the Chicomuselo region at the end of the Cisuralian as mentioned in this paper.