Three stages in the Late Paleozoic to Triassic magmatism of southwestern Gondwana, and the relationships with the volcanogenic events in coeval basins

AM Sato, EJ Llambías, MAS Basei, CE Castro - Journal of South American …, 2015 - Elsevier
The intermediate to acid Choiyoi Magmatic Province is the most conspicuous feature along
the Late Paleozic continental margin of southwestern Gondwana, and is generally regarded …

Impacts of global warming on Permo-Triassic terrestrial ecosystems

MJ Benton, AJ Newell - Gondwana Research, 2014 - Elsevier
Geologists and palaeontologists have expressed mixed views about the effects of the end-
Permian mass extinction on continental habitats and on terrestrial life. Current work …

[HTML][HTML] On the causes of mass extinctions

DPG Bond, SE Grasby - Palaeogeography, Palaeoclimatology …, 2017 - Elsevier
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 …

Phanerozoic concentrations of atmospheric oxygen reconstructed from sedimentary charcoal

IJ Glasspool, AC Scott - Nature Geoscience, 2010 - nature.com
Variations of the Earth's atmospheric oxygen concentration (p O2) are thought to be closely
tied to the evolution of life, with strong feedbacks between uni-and multicellular life and …

Recovery from the most profound mass extinction of all time

S Sahney, MJ Benton - … of the Royal Society B: Biological …, 2008 - royalsocietypublishing.org
The end-Permian mass extinction, 251 million years (Myr) ago, was the most devastating
ecological event of all time, and it was exacerbated by two earlier events at the beginning …

A paleoclimatic review of southern South America during the late Paleozoic: a record from icehouse to extreme greenhouse conditions

CO Limarino, SN Césari, LA Spalletti, AC Taboada… - Gondwana …, 2014 - Elsevier
This paper provides a review of the Late Mississippian to Permian paleoclimatic history for
southern South America based on lithologic indicators, biostratigraphic information, and …

Climate changes caused by degassing of sediments during the emplacement of large igneous provinces

C Ganino, NT Arndt - Geology, 2009 - pubs.geoscienceworld.org
Most mass extinctions during the last 500 my coincide with eruptions of large igneous
provinces (LIPs). The Cretaceous-Tertiary extinction was synchronous with the Deccan flood …

How contact metamorphism can trigger global climate changes: Modeling gas generation around igneous sills in sedimentary basins

I Aarnes, H Svensen, JAD Connolly… - … et Cosmochimica Acta, 2010 - Elsevier
Large volumes of greenhouse gases such as CH4 and CO2 form by contact metamorphism
of organic-rich sediments in aureoles around sill intrusions in sedimentary basins …

When and how did the terrestrial mid-Permian mass extinction occur? Evidence from the tetrapod record of the Karoo Basin, South Africa

MO Day, J Ramezani, SA Bowring… - … of the Royal …, 2015 - royalsocietypublishing.org
A mid-Permian (Guadalupian epoch) extinction event at approximately 260 Ma has been
mooted for two decades. This is based primarily on invertebrate biostratigraphy of …

Tectonic evolution of the Cape and Karoo basins of South Africa

A Tankard, H Welsink, P Aukes, R Newton… - Marine and Petroleum …, 2009 - Elsevier
The Cape and Karoo basins formed within the continental interior of Gondwana. Subsidence
resulted from the vertical motion of rigid basement blocks and intervening crustal faults …