Phanerozoic paleotemperatures: The earth's changing climate during the last 540 million years
This study provides a comprehensive and quantitative estimate of how global temperatures
have changed during the last 540 million years. It combines paleotemperature …
have changed during the last 540 million years. It combines paleotemperature …
Extinction and dawn of the modern world in the Carnian (Late Triassic)
The Carnian Pluvial Episode (Late Triassic) was a time of global environmental changes
and possibly substantial coeval volcanism. The extent of the biological turnover in marine …
and possibly substantial coeval volcanism. The extent of the biological turnover in marine …
[HTML][HTML] On the causes of mass extinctions
The temporal link between large igneous province (LIP) eruptions and at least half of the
major extinctions of the Phanerozoic implies that large scale volcanism is the main driver of …
major extinctions of the Phanerozoic implies that large scale volcanism is the main driver of …
Triassic climates—state of the art and perspectives
The climate of the Triassic period was characterized by a non-zonal pattern, dictated by a
strong global monsoon system with effects that are most evident in the Tethys realm. This …
strong global monsoon system with effects that are most evident in the Tethys realm. This …
Production and preservation of resins–past and present
Amber is fossilised plant resin. It can be used to provide insights into the terrestrial
conditions at the time the original resin was exuded. Amber research thus can inform many …
conditions at the time the original resin was exuded. Amber research thus can inform many …
The triassic period
The Triassic is bound by two mass extinctions that coincide with vast outpourings of volcanic
flood basalts. The Mesozoic begins with a gradual recovery of plant and animal life after the …
flood basalts. The Mesozoic begins with a gradual recovery of plant and animal life after the …
Climate warming, euxinia and carbon isotope perturbations during the Carnian (Triassic) Crisis in South China
Abstract The Carnian Humid Episode (CHE), also known as the Carnian Pluvial Event, and
associated biotic changes are major enigmas of the Mesozoic record in western Tethys. We …
associated biotic changes are major enigmas of the Mesozoic record in western Tethys. We …
Multiple negative carbon-isotope excursions during the Carnian Pluvial Episode (Late Triassic)
Abstract The Carnian Pluvial Episode was a phase of global climatic change and biotic
turnover that occurred during the early Late Triassic. In marine sedimentary basins, the …
turnover that occurred during the early Late Triassic. In marine sedimentary basins, the …
Discovery of a major negative δ13C spike in the Carnian (Late Triassic) linked to the eruption of Wrangellia flood basalts
Major climate changes and mass extinctions are associated with carbon isotope anomalies
in the atmosphere-ocean system and have been shown to coincide with the onset of large …
in the atmosphere-ocean system and have been shown to coincide with the onset of large …
The Carnian Humid Episode of the late Triassic: a review
From 1989 to 1994 a series of papers outlined evidence for a brief episode of climate
change from arid to humid, and then back to arid, during the Carnian Stage of the late …
change from arid to humid, and then back to arid, during the Carnian Stage of the late …