Unusual fossil macrofloras from South America (Peru, Bolivia, Brazil), Africa (Niger), India, and Australia are distinctly different from both the Early and Late Carboniferous floras of Gondwana. These floras can be correlated with each other based on macrofloral and palynologic composition, and dated as Late Visean to earliest Serpukhovian through palynologic data from several floras and isotopic data from Australia. The floras are dominated by pteridosperm foliage and characterized by the occurrence of tree-lycopsids, and represent a warm-temperate, frost-free floral belt in Gondwana that reached from 30 8 to as far as 60 8 South that existed directly before the onset of the major episode of the Carboniferous glaciation. The plants lived ...
The statistical analysis of published Paleocene-Late Miocene palynological data from Patagonia suppo...
Two hypotheses have attempted to explain the development of Mixed Paleofloras during the Cenozoic in...
Diverse Cenozoic (possibly latest Oligocene to mid–late Miocene) macrofossils from the Lightning Rid...
Unusual fossil macrofloras from South America (Peru, Bolivia, Brazil), Africa (Niger), India, and Au...
Near the close of the Triassic the Dicroidum flora of Gondwanan regions underwent considerable modif...
Plant assemblages are described from the Talacasto and Punta Negra Formations, San Juan Province, th...
Plant assemblages are described from the Talacasto and Punta Negra Formations, San Juan Province, th...
Plant assemblages are described from the Talacasto and Punta Negra Formations, San Juan Province, th...
The Late Paleozoic in West Gondwana was a period of significant climatic changes, ranging from a gla...
Charting the broad patterns of vascular plant evolution for Gondwana against the major global enviro...
The past geographical positions and climates of the high latitude Southern Hemisphere land masses (N...
ABSTRACT: Tropical rainforests in the northeast of Australia have been interpreted as being either c...
Premise of research. Cenozoic macrofloras from South America are fundamental for understanding extan...
Patagonia contains a rich and fairly continuous paleobotanical record from the late Maastrichtian to...
The statistical analysis of published Paleocene–Late Miocene palynological data from Patagonia suppo...
The statistical analysis of published Paleocene-Late Miocene palynological data from Patagonia suppo...
Two hypotheses have attempted to explain the development of Mixed Paleofloras during the Cenozoic in...
Diverse Cenozoic (possibly latest Oligocene to mid–late Miocene) macrofossils from the Lightning Rid...
Unusual fossil macrofloras from South America (Peru, Bolivia, Brazil), Africa (Niger), India, and Au...
Near the close of the Triassic the Dicroidum flora of Gondwanan regions underwent considerable modif...
Plant assemblages are described from the Talacasto and Punta Negra Formations, San Juan Province, th...
Plant assemblages are described from the Talacasto and Punta Negra Formations, San Juan Province, th...
Plant assemblages are described from the Talacasto and Punta Negra Formations, San Juan Province, th...
The Late Paleozoic in West Gondwana was a period of significant climatic changes, ranging from a gla...
Charting the broad patterns of vascular plant evolution for Gondwana against the major global enviro...
The past geographical positions and climates of the high latitude Southern Hemisphere land masses (N...
ABSTRACT: Tropical rainforests in the northeast of Australia have been interpreted as being either c...
Premise of research. Cenozoic macrofloras from South America are fundamental for understanding extan...
Patagonia contains a rich and fairly continuous paleobotanical record from the late Maastrichtian to...
The statistical analysis of published Paleocene–Late Miocene palynological data from Patagonia suppo...
The statistical analysis of published Paleocene-Late Miocene palynological data from Patagonia suppo...
Two hypotheses have attempted to explain the development of Mixed Paleofloras during the Cenozoic in...
Diverse Cenozoic (possibly latest Oligocene to mid–late Miocene) macrofossils from the Lightning Rid...