Fossil woods with coniferalean affinities from the Upper Cretaceous (Campanian–Maastrichtian) Puntudo Chico Formation, Chubut Province, Argentina

The Puntudo Chico Formation is a continental sequence overlying the Chubut Group at the central-East of the Cañadón Asfalto Basin in Patagonia (Chubut Province, Argentina). The age of this unit, Campanian–Maastrichtian, makes it comparable with other Patagonian units, such as the Allen (Río Negro Pr...

Descripción completa

Guardado en:
Detalles Bibliográficos
Publicado: 2019
Materias:
Acceso en línea:https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_01956671_v99_n_p321_Vera
http://hdl.handle.net/20.500.12110/paper_01956671_v99_n_p321_Vera
Aporte de:
id paper:paper_01956671_v99_n_p321_Vera
record_format dspace
spelling paper:paper_01956671_v99_n_p321_Vera2023-06-08T15:20:24Z Fossil woods with coniferalean affinities from the Upper Cretaceous (Campanian–Maastrichtian) Puntudo Chico Formation, Chubut Province, Argentina Agathoxylon Brachyoxylon Kawas Sea Podocarpoxylon Agathoxylon Aves Brachyoxylon Coniferales Coniferophyta Dinosauria Mammalia Petriella Podocarpoxylon The Puntudo Chico Formation is a continental sequence overlying the Chubut Group at the central-East of the Cañadón Asfalto Basin in Patagonia (Chubut Province, Argentina). The age of this unit, Campanian–Maastrichtian, makes it comparable with other Patagonian units, such as the Allen (Río Negro Province) and La Colonia Formation (Chubut Province), well-known by their paleontological content, including plants, mammals, and non-avian dinosaurs. Contrasting, the Puntudo Chico Formation fossil content is almost unknown, and even if fossil woods were reported, detailed studies were lacking. In this contribution, fossil woods collected from the Puntudo Chico Formation are studied, and three different conifer taxa are identified: Podocarpoxylon mazzonii (Petriella) Müller-Stoll & J. Schultze-Motel 1990, Brachyoxylon sp. cf. B. currumilii Bodnar, Escapa, Cúneo & Gnaedinger, 2013, and Agathoxylon antarcticus (Poole et Cantrill) Pujana, Santillana & Marenssi, 2014. This flora seems to be part of a distinctive Late Cretaceous–Danian floristic assemblages that inhabited a warm region located approximately at 38–42°S, that were probably linked and somewhat nearby the Kawas Sea, an inland sea that flooded the Neuquén and Río Colorado basins during the first Atlantic Transgressive Event in Patagonia. © 2019 Elsevier Ltd 2019 https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_01956671_v99_n_p321_Vera http://hdl.handle.net/20.500.12110/paper_01956671_v99_n_p321_Vera
institution Universidad de Buenos Aires
institution_str I-28
repository_str R-134
collection Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA)
topic Agathoxylon
Brachyoxylon
Kawas Sea
Podocarpoxylon
Agathoxylon
Aves
Brachyoxylon
Coniferales
Coniferophyta
Dinosauria
Mammalia
Petriella
Podocarpoxylon
spellingShingle Agathoxylon
Brachyoxylon
Kawas Sea
Podocarpoxylon
Agathoxylon
Aves
Brachyoxylon
Coniferales
Coniferophyta
Dinosauria
Mammalia
Petriella
Podocarpoxylon
Fossil woods with coniferalean affinities from the Upper Cretaceous (Campanian–Maastrichtian) Puntudo Chico Formation, Chubut Province, Argentina
topic_facet Agathoxylon
Brachyoxylon
Kawas Sea
Podocarpoxylon
Agathoxylon
Aves
Brachyoxylon
Coniferales
Coniferophyta
Dinosauria
Mammalia
Petriella
Podocarpoxylon
description The Puntudo Chico Formation is a continental sequence overlying the Chubut Group at the central-East of the Cañadón Asfalto Basin in Patagonia (Chubut Province, Argentina). The age of this unit, Campanian–Maastrichtian, makes it comparable with other Patagonian units, such as the Allen (Río Negro Province) and La Colonia Formation (Chubut Province), well-known by their paleontological content, including plants, mammals, and non-avian dinosaurs. Contrasting, the Puntudo Chico Formation fossil content is almost unknown, and even if fossil woods were reported, detailed studies were lacking. In this contribution, fossil woods collected from the Puntudo Chico Formation are studied, and three different conifer taxa are identified: Podocarpoxylon mazzonii (Petriella) Müller-Stoll & J. Schultze-Motel 1990, Brachyoxylon sp. cf. B. currumilii Bodnar, Escapa, Cúneo & Gnaedinger, 2013, and Agathoxylon antarcticus (Poole et Cantrill) Pujana, Santillana & Marenssi, 2014. This flora seems to be part of a distinctive Late Cretaceous–Danian floristic assemblages that inhabited a warm region located approximately at 38–42°S, that were probably linked and somewhat nearby the Kawas Sea, an inland sea that flooded the Neuquén and Río Colorado basins during the first Atlantic Transgressive Event in Patagonia. © 2019 Elsevier Ltd
title Fossil woods with coniferalean affinities from the Upper Cretaceous (Campanian–Maastrichtian) Puntudo Chico Formation, Chubut Province, Argentina
title_short Fossil woods with coniferalean affinities from the Upper Cretaceous (Campanian–Maastrichtian) Puntudo Chico Formation, Chubut Province, Argentina
title_full Fossil woods with coniferalean affinities from the Upper Cretaceous (Campanian–Maastrichtian) Puntudo Chico Formation, Chubut Province, Argentina
title_fullStr Fossil woods with coniferalean affinities from the Upper Cretaceous (Campanian–Maastrichtian) Puntudo Chico Formation, Chubut Province, Argentina
title_full_unstemmed Fossil woods with coniferalean affinities from the Upper Cretaceous (Campanian–Maastrichtian) Puntudo Chico Formation, Chubut Province, Argentina
title_sort fossil woods with coniferalean affinities from the upper cretaceous (campanian–maastrichtian) puntudo chico formation, chubut province, argentina
publishDate 2019
url https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_01956671_v99_n_p321_Vera
http://hdl.handle.net/20.500.12110/paper_01956671_v99_n_p321_Vera
_version_ 1768541559286923264