Plant species with predominantly tropical and subtropical modern distributions (or meso-megathermal species) penetrated into the highest southern latitudes of the American continent during the global warmest periods of the Cenozoic. These species – usually phylogenetically unrelated – became fossilized typically as dispersed spores and pollen grains. Here, we describe and illustrate fossil spores and pollen grains preserved during the Middle Eocene Climatic Optimum (MECO) in Patagonian southernmost latitudes (Río Turbio Formation). We study those species that today occurred in lower latitudes (e.g. northern Argentina and Brazil) and became locally extinct from Patagonia during the subsequent cooling episodes. We also estimate their frequenc...
A major climate shift took place about 40 Myr ago—the Middle Eocene Climatic Optimum or MECO—trigger...
The cycads pose classic problems in evolutionary biogeography, owing to their far-flung extant distr...
The statistical analysis of published Paleocene–Late Miocene palynological data from Patagonia suppo...
Myrtaceae, the gum tree family, is a large angiosperm clade of 5671 species mostly distributed in tr...
The Río Turbio Formation (Eocene–?Oligocene) is of particular paleobotanical interest owing to its c...
The statistical analysis of published Paleocene-Late Miocene palynological data from Patagonia suppo...
Premise of research. Cenozoic macrofloras from South America are fundamental for understanding extan...
Here I describe and illustrate 19 leaf morphospecies from the Paleogene Río Turbio Formation, Santa ...
A major reorganization of Patagonian ecosystems occurred when permanent ice sheets appeared in Antar...
Patagonia contains a rich and fairly continuous paleobotanical record from the late Maastrichtian to...
Patagonia contains a rich and fairly continuous paleobotanical record from the late Maastrichtian to...
Premise of research: Cenozoic macrofloras from South America are fundamental for understanding extan...
The beech-oak family Fagaceae dominates forests from the northern temperate zone to tropical Asia an...
Climate-driven changes in terrestrial environments and biomes after the Early Eocene Climatic Optimu...
Premise: Eocene floras of Patagonia document biotic response to the final separation of Gondwana. Th...
A major climate shift took place about 40 Myr ago—the Middle Eocene Climatic Optimum or MECO—trigger...
The cycads pose classic problems in evolutionary biogeography, owing to their far-flung extant distr...
The statistical analysis of published Paleocene–Late Miocene palynological data from Patagonia suppo...
Myrtaceae, the gum tree family, is a large angiosperm clade of 5671 species mostly distributed in tr...
The Río Turbio Formation (Eocene–?Oligocene) is of particular paleobotanical interest owing to its c...
The statistical analysis of published Paleocene-Late Miocene palynological data from Patagonia suppo...
Premise of research. Cenozoic macrofloras from South America are fundamental for understanding extan...
Here I describe and illustrate 19 leaf morphospecies from the Paleogene Río Turbio Formation, Santa ...
A major reorganization of Patagonian ecosystems occurred when permanent ice sheets appeared in Antar...
Patagonia contains a rich and fairly continuous paleobotanical record from the late Maastrichtian to...
Patagonia contains a rich and fairly continuous paleobotanical record from the late Maastrichtian to...
Premise of research: Cenozoic macrofloras from South America are fundamental for understanding extan...
The beech-oak family Fagaceae dominates forests from the northern temperate zone to tropical Asia an...
Climate-driven changes in terrestrial environments and biomes after the Early Eocene Climatic Optimu...
Premise: Eocene floras of Patagonia document biotic response to the final separation of Gondwana. Th...
A major climate shift took place about 40 Myr ago—the Middle Eocene Climatic Optimum or MECO—trigger...
The cycads pose classic problems in evolutionary biogeography, owing to their far-flung extant distr...
The statistical analysis of published Paleocene–Late Miocene palynological data from Patagonia suppo...