Pre-Cenozoic cyclostratigraphy and palaeoclimate responses to astronomical forcing
D De Vleeschouwer, LME Percival… - Nature Reviews Earth & …, 2024 - nature.com
Astronomical insolation forcing is well established as the underlying metronome of
Quaternary ice ages and Cenozoic climate changes. Yet its effects on earlier eras …
Quaternary ice ages and Cenozoic climate changes. Yet its effects on earlier eras …
On the onset of Central Atlantic Magmatic Province (CAMP) volcanism and environmental and carbon-cycle change at the Triassic–Jurassic transition (Neuquén Basin …
Abstract The Triassic–Jurassic transition is characterized by the end-Triassic mass extinction
approximately synchronous with the onset of emplacement of the Central Atlantic Magmatic …
approximately synchronous with the onset of emplacement of the Central Atlantic Magmatic …
Organic carbon burial is paced by a~ 173-ka obliquity cycle in the middle to high latitudes
Earth's climate system is complex and inherently nonlinear, which can induce some
extraneous cycles in paleoclimatic proxies at orbital time scales. The paleoenvironmental …
extraneous cycles in paleoclimatic proxies at orbital time scales. The paleoenvironmental …
The Jurassic Period
Ammonites underwent an evolutionary diversification after the mass extinction of the end
Triassic induced by the formation of a Large Igneous province (LIP), and this group provides …
Triassic induced by the formation of a Large Igneous province (LIP), and this group provides …
The Triassic–Jurassic transition–A review of environmental change at the dawn of modern life
Abstract The Triassic–Jurassic transition, which is here broadly defined as extending from
the Late Triassic through the Early Jurassic (~ 237 Ma to 174 Ma), was an important interval …
the Late Triassic through the Early Jurassic (~ 237 Ma to 174 Ma), was an important interval …
Reduced plate motion controlled timing of Early Jurassic Karoo-Ferrar large igneous province volcanism
Past large igneous province (LIP) emplacement is commonly associated with mantle plume
upwelling and led to major carbon emissions. One of Earth's largest past environmental …
upwelling and led to major carbon emissions. One of Earth's largest past environmental …
Obliquity forcing of lake-level changes and organic carbon burial during the Late Paleozoic Ice Age
The linkages between the astronomical forcing of sea-level oscillations, the environment,
and climate change during the Late Paleozoic Ice Age (LPIA) add to our understanding of …
and climate change during the Late Paleozoic Ice Age (LPIA) add to our understanding of …
Early Jurassic large igneous province carbon emissions constrained by sedimentary mercury
Large igneous province eruptions and their carbon emissions often coincide with, and are
hypothesized to have driven, severe environmental perturbations in the geological past …
hypothesized to have driven, severe environmental perturbations in the geological past …
Determining the style and provenance of magmatic activity during the Early Aptian Oceanic Anoxic Event (OAE 1a)
LME Percival, LR Tedeschi, RA Creaser… - Global and Planetary …, 2021 - Elsevier
Large igneous province (LIP) volcanism has been proposed as a key trigger of several
major climate and environmental perturbations during the Phanerozoic Aeon. Large-scale …
major climate and environmental perturbations during the Phanerozoic Aeon. Large-scale …
The Jenkyns Event (early Toarcian OAE) in the Ordos Basin, North China
Abstract The early Toarcian (Early Jurassic) Oceanic Anoxic Event (T-OAE) or Jenkyns
Event (~ 183 Ma) was marked by a globally synchronous negative carbon-isotope …
Event (~ 183 Ma) was marked by a globally synchronous negative carbon-isotope …