The Carnian Pluvial Episode (CPE) has been recognized as a time of plant radiations and originations, likely related to observed swift changes from xerophytic to more hygrophytic floras. This suggests that the increasing humidity causally resulting from LIP volcanismwas the trigger for these changes in the terrestrial realm. Understanding the cause and effects of the CPE on the plant realm, requires study of well-preserved floras that are precisely aligned with the CPE. We therefore focus on the best age-constrained section within the CPE for the terrestrial to marginal marine environment to understand the floristic composition at the early CPE. This is found in the Dolomites, Italy, and is remarkable for the preservation of the oldest foss...
The Le Fraine fossil locality, near the Tregiovo village (Trento Province, northern Italy) yields tw...
Amber from the Carnian succession of the Dolomites and Julian Alps (northeastern Italy) represents o...
The Carnian Pluvial Episode (CPE) was a perturbation of the Late Triassic climate that had a strong ...
The Carnian Pluvial Episode (CPE) was a perturbation of the Late Triassic climate that had a strong ...
The Carnian Pluvial Episode (CPE; c. 234–232 million years ago) is characterized by an accelerated h...
The Carnian Pluvial Episode (CPE; c. 234–232 million years ago) is characterized by an accelerated h...
Among the most significant global climate changes recorded in the Mesozoic, the Carnian Pluvial Epis...
Among the most significant global climate changes recorded in the Mesozoic, the Carnian Pluvial Epis...
The Carnian Pluvial Event is an Upper Triassic swing toward increased rainfall best documented in th...
The generally arid Late Triassic climate was interrupted by a wet phase during the mid-Carnian terme...
The Late Triassic Carnian Pluvial Episode (CPE; ca. 234–232 Ma) was characterized by dramatic global...
The Carnian Pluvial Event is an Upper Triassic swing toward increased rainfall best documented in th...
The Carnian Pluvial Event is an Upper Triassic swing toward increased rainfall best documented in th...
A major global change, the transition from an icehouse to a greenhouse world, took place during the ...
The fossil record of amber dates back to the Palaeozoic, but it is only since the Mesozoic that ambe...
The Le Fraine fossil locality, near the Tregiovo village (Trento Province, northern Italy) yields tw...
Amber from the Carnian succession of the Dolomites and Julian Alps (northeastern Italy) represents o...
The Carnian Pluvial Episode (CPE) was a perturbation of the Late Triassic climate that had a strong ...
The Carnian Pluvial Episode (CPE) was a perturbation of the Late Triassic climate that had a strong ...
The Carnian Pluvial Episode (CPE; c. 234–232 million years ago) is characterized by an accelerated h...
The Carnian Pluvial Episode (CPE; c. 234–232 million years ago) is characterized by an accelerated h...
Among the most significant global climate changes recorded in the Mesozoic, the Carnian Pluvial Epis...
Among the most significant global climate changes recorded in the Mesozoic, the Carnian Pluvial Epis...
The Carnian Pluvial Event is an Upper Triassic swing toward increased rainfall best documented in th...
The generally arid Late Triassic climate was interrupted by a wet phase during the mid-Carnian terme...
The Late Triassic Carnian Pluvial Episode (CPE; ca. 234–232 Ma) was characterized by dramatic global...
The Carnian Pluvial Event is an Upper Triassic swing toward increased rainfall best documented in th...
The Carnian Pluvial Event is an Upper Triassic swing toward increased rainfall best documented in th...
A major global change, the transition from an icehouse to a greenhouse world, took place during the ...
The fossil record of amber dates back to the Palaeozoic, but it is only since the Mesozoic that ambe...
The Le Fraine fossil locality, near the Tregiovo village (Trento Province, northern Italy) yields tw...
Amber from the Carnian succession of the Dolomites and Julian Alps (northeastern Italy) represents o...
The Carnian Pluvial Episode (CPE) was a perturbation of the Late Triassic climate that had a strong ...