Abstract The Upper Triassic Chinle Formation is a critical non-marine archive of low- paleolatitude biotic and environmental change in southwestern North America. The well …
The end-Triassic mass extinction is often linked to environmental and climate change triggered by the activity of the Central Atlantic Magmatic Province ca. 201 Mya. In the …
Abstract Uranium–lead (U–Pb) geochronology was conducted by laser ablation–inductively coupled plasma mass spectrometry (LA-ICPMS) on 7175 detrital zircon grains from 29 …
YD Sun, MJ Orchard, ÁT Kocsis… - Earth and Planetary …, 2020 - Elsevier
Abstract The Carnian–Norian (C–N) transition (Late Triassic) has long been postulated as an interval of major climatic changes, though the nature of such changes and their …
Geodiversity treaties have multiplied and given rise to geological heritage as a singular value of protection and preservation for territories. The Puyango Petrified Forest (PPF) is a …
Abstract The Norian Stage (Late Triassic) has long been regarded as an interval of stable climates, but, in fact, there are only sparse studies of the paleoclimate variations during this …
Building on an earlier study that confirmed the stability of the 405‐kyr eccentricity climate cycle and the timing of the Newark‐Hartford astrochronostratigraphic polarity time scale …
MS Garcia, RT Müller, ÁAS Da-Rosa… - Journal of South …, 2019 - Elsevier
Late Triassic deposits from south Pangea (Argentina and Brazil) bear the oldest (so far) and most informative unequivocal records of dinosaurs worldwide. Herein we describe a new …
Abstract The Sonsela Sandstone bed was first named as an informal unit in the lower part of the Chinle Formation in northern Arizona, USA, and it was later assigned a type section near …