In this report, we analyze the angiosperm fossil record (micro- and megafossil) from the central and southern basins of Argentina, southern South America, deposited between the late Barremian (128.3 Ma) to the end of the Coniacian (85.8 Ma). Based on this analysis, three major stages in the evolution of the angiosperms in the southernmost region of South America are established as follows: the late Barremian-Aptian, the latest Aptian-earliest Albian, and the middle Albian- Coniacian. The comparison between our fossil data set and those from Australia, North America, Asia and Europe suggest that the evolution and diversification of the angiosperms at mid and high latitudes in both hemispheres occurred roughly synchronously.Fil: Archangelsky,...
The study of plant material from localities of Late Cretaceous age from southern latitudes is fundam...
The South American Transition Zone (SATZ) is a biogeographic area in which not only orogeny (Andes u...
The oldest seed occurrences in Western Gondwana have been recognized in a new stratigraphic section ...
The angiosperm pollen record from the Anfiteatro de Ticó and Punta del Barco formations (Baqueró Gro...
This paper describes the diversity, taphonomy and palaeoecology of angiosperm leaves that dominate a...
The Baqueró Group is one of the most relevant units regarding the study of the early diversification...
The critical climatic changes that occurred during the Albian–Turonian Cretaceous interval led to a ...
The Río Turbio Formation (Eocene–?Oligocene) is of particular paleobotanical interest owing to its c...
The revision of the stratigraphy of the Cerro Bayo in the Bajo Grande area (Argentinean Patagonia) a...
Floodplain deposits of the Anfiteatro de Ticó Formation (Baqueró Group, Aptian), in Patagonia (Argen...
Se describen ejemplares de Rochipteris copiapensis (Solms-Laubach) Herbst, Troncoso & Gnaedinger y d...
Six angiosperm pollen types studied with SEM are recorded in the Cretaceous (early Aptian) Tico´ flo...
The mid-Cretaceous greenhouse period in the southern Patagonia Argentina (Austral Basin) is represen...
The first palynologic record in a Lower Cretaceous sequence at the Cañadón Calcáreo locality of Extr...
An anatomical and ecological study of a Late Pennsylvanian-early Permian assemblage of silicified tr...
The study of plant material from localities of Late Cretaceous age from southern latitudes is fundam...
The South American Transition Zone (SATZ) is a biogeographic area in which not only orogeny (Andes u...
The oldest seed occurrences in Western Gondwana have been recognized in a new stratigraphic section ...
The angiosperm pollen record from the Anfiteatro de Ticó and Punta del Barco formations (Baqueró Gro...
This paper describes the diversity, taphonomy and palaeoecology of angiosperm leaves that dominate a...
The Baqueró Group is one of the most relevant units regarding the study of the early diversification...
The critical climatic changes that occurred during the Albian–Turonian Cretaceous interval led to a ...
The Río Turbio Formation (Eocene–?Oligocene) is of particular paleobotanical interest owing to its c...
The revision of the stratigraphy of the Cerro Bayo in the Bajo Grande area (Argentinean Patagonia) a...
Floodplain deposits of the Anfiteatro de Ticó Formation (Baqueró Group, Aptian), in Patagonia (Argen...
Se describen ejemplares de Rochipteris copiapensis (Solms-Laubach) Herbst, Troncoso & Gnaedinger y d...
Six angiosperm pollen types studied with SEM are recorded in the Cretaceous (early Aptian) Tico´ flo...
The mid-Cretaceous greenhouse period in the southern Patagonia Argentina (Austral Basin) is represen...
The first palynologic record in a Lower Cretaceous sequence at the Cañadón Calcáreo locality of Extr...
An anatomical and ecological study of a Late Pennsylvanian-early Permian assemblage of silicified tr...
The study of plant material from localities of Late Cretaceous age from southern latitudes is fundam...
The South American Transition Zone (SATZ) is a biogeographic area in which not only orogeny (Andes u...
The oldest seed occurrences in Western Gondwana have been recognized in a new stratigraphic section ...