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 …
New thoughts about the Cretaceous climate and oceans
WW Hay, S Floegel - Earth-Science Reviews, 2012 - Elsevier
Several new discoveries suggest that the climate of the Cretaceous may have been more
different from that of today than has been previously supposed. Detailed maps of climate …
different from that of today than has been previously supposed. Detailed maps of climate …
How Large Igneous Provinces affect global climate, sometimes cause mass extinctions, and represent natural markers in the geological record
Abstract Large Igneous Provinces (LIPs) can have a significant global climatic effect as
monitored by sedimentary trace and isotopic compositions that record paleo …
monitored by sedimentary trace and isotopic compositions that record paleo …
Initial pulse of Siberian Traps sills as the trigger of the end-Permian mass extinction
SD Burgess, JD Muirhead, SA Bowring - Nature Communications, 2017 - nature.com
Mass extinction events are short-lived and characterized by catastrophic biosphere collapse
and subsequent reorganization. Their abrupt nature necessitates a similarly short-lived …
and subsequent reorganization. Their abrupt nature necessitates a similarly short-lived …
[PDF][PDF] Carbon isotope stratigraphy
MR Saltzman, E Thomas, FM Gradstein - The geologic time scale, 2012 - academia.edu
Variations in the 13C/12C value of total dissolved inorganic carbon (DIC) in the world's
oceans through time have been documented through stratigraphic study of marine …
oceans through time have been documented through stratigraphic study of marine …
[HTML][HTML] Geology and paleontology of the upper cretaceous Kem Kem group of eastern Morocco
The geological and paleoenvironmental setting and the vertebrate taxonomy of the
fossiliferous, Cenomanian-age deltaic sediments in eastern Morocco, generally referred to …
fossiliferous, Cenomanian-age deltaic sediments in eastern Morocco, generally referred to …
Massive and prolonged deep carbon emissions associated with continental rifting
Carbon from Earth's interior is thought to be released to the atmosphere mostly via
degassing of CO2 from active volcanoes,,,. CO2 can also escape along faults away from …
degassing of CO2 from active volcanoes,,,. CO2 can also escape along faults away from …
Marine productivity changes during the end-Permian crisis and Early Triassic recovery
J Shen, SD Schoepfer, Q Feng, L Zhou, J Yu… - Earth-Science …, 2015 - Elsevier
The latest Permian mass extinction (LPME) coincided with major changes in the composition
of marine plankton communities, yet little is known about concurrent changes in primary …
of marine plankton communities, yet little is known about concurrent changes in primary …
[HTML][HTML] A volcanic scenario for the Frasnian–Famennian major biotic crisis and other Late Devonian global changes: More answers than questions?
G Racki - Global and Planetary Change, 2020 - Elsevier
Although the prime causation of the Late Devonian Frasnian–Famennian (F–F) mass
extinction remains conjectural, such destructive factors as the spread of anoxia and rapid …
extinction remains conjectural, such destructive factors as the spread of anoxia and rapid …
Environmental changes in the Late Ordovician–early Silurian: Review and new insights from black shales and nitrogen isotopes
MJ Melchin, CE Mitchell, C Holmden, P Štorch - Bulletin, 2013 - pubs.geoscienceworld.org
Abstract The Late Ordovician (Katian-Hirnantian) through earliest Silurian (Rhuddanian)
interval was a time of varying climate and sea level, marked by a peak glacial episode in the …
interval was a time of varying climate and sea level, marked by a peak glacial episode in the …