Duration and intensity of the Late Permian (early Wuchiapingian) cool climate episode: Sclerochemical evidence from brachiopod assemblages in Iran DOI Creative Commons
Marco Viaretti, Gaia Crippa, Valentina Brombin

et al.

Palaeogeography Palaeoclimatology Palaeoecology, Journal Year: 2024, Volume and Issue: unknown, P. 112654 - 112654

Published: Dec. 1, 2024

Language: Английский

Tellurium and Mercury in Late Cretaceous to Early Eocene Sediments as Proxies for Volcanic Activity in the Deccan and North Atlantic Large Igneous Provinces DOI Creative Commons
Nils Björn Baumann, Marcel Regelous, Thierry Adatte

et al.

Geochemistry Geophysics Geosystems, Journal Year: 2025, Volume and Issue: 26(2)

Published: Feb. 1, 2025

Abstract Late Maastrichtian to Early Eocene sediments from Wadi Nukhul, Egypt were deposited between about 67 and 55.5 Ma during the eruption of Deccan Traps North Atlantic Igneous Province (NAIP). We use Te Hg as proxies for volcanism constrain timing flood basalt relative environmental perturbations extinction events this period. find enrichment in latest earliest Danian Paleocene Eocene, which result enhanced volcanic input Te. An increase coincides with Warming Event. A second larger peak begins 120–80 kyr before Cretaceous/Paleogene boundary (KPB) continues into Danian, highest values 70–30 prior KPB, potentially related eruptions voluminous Wai subgroup. The Chicxulub impact, therefore, did not trigger these eruptions, likely led climate instability, may have amplified effects impact. 6 Myr period low is followed by an starting at 57.5 peaking Paleocene‐Eocene (PEB; 56 Ma) opening eruptive rates NAIP. In contrast, variations over same time are less systematic. Our results show that be a robust proxy, complementary Hg, large events.

Language: Английский

Citations

0

Correlation and cyclicity of stratigraphic sequence boundaries and chronostratigraphic stage boundaries of the last 253 My: Synchrony of tectonism, sea level, climate and biotic change DOI
Michael R. Rampino,

K. Caldeira

Earth-Science Reviews, Journal Year: 2025, Volume and Issue: unknown, P. 105100 - 105100

Published: March 1, 2025

Language: Английский

Citations

0

Platinum-group elements (PGEs) and rhenium in Permian-Triassic boundary sediments from southern China and Japan linked to concurrent eruptions of the Siberian Traps DOI

Monika Misztela,

Michael R. Rampino, I. H. Campbell

et al.

Chemical Geology, Journal Year: 2025, Volume and Issue: unknown, P. 122715 - 122715

Published: March 1, 2025

Language: Английский

Citations

0

Greatly increased CO2 DOI

Scott E. Elias

Elsevier eBooks, Journal Year: 2025, Volume and Issue: unknown

Published: Jan. 1, 2025

Language: Английский

Citations

0

Mechanisms of global climate change during the five major mass extinctions DOI Creative Commons
Kunio Kaiho

Scientific Reports, Journal Year: 2025, Volume and Issue: 15(1)

Published: May 12, 2025

Since the emergence of diverse animal phyla around 500 million years ago, five major mass extinction events have occurred, each coinciding with abnormal climate changes. We analyzed sedimentary organic molecules from first and least understood event at end Ordovician period. divided all extinctions into two phases each, totaling ten events, examined relationship between shifts "coronene index"-an indicator heating temperatures in rocks caused by volcanic activity or meteorite impacts. As a result, we found that four began global cooling ended warming, while one started an unknown anomaly also warming. During initial phases, showed low-temperature heating, high-temperature, moderate-temperature. All subsequent warming moderate-temperature heating. These findings suggest large-scale eruptions impacts heated sulfides, sulfates, hydrocarbons varying temperatures, releasing SO2 soot stratosphere, blocking sunlight, triggering extinction. This was followed moderate carbonates, increasing CO2 emissions driving long-term leading to secondary events.

Language: Английский

Citations

0

Global Eocene-Oligocene unconformity in clastic sedimentary basins DOI
Z. F. M. Burton,

Tim McHargue,

Stephan A. Graham

et al.

Earth-Science Reviews, Journal Year: 2024, Volume and Issue: 258, P. 104912 - 104912

Published: Oct. 7, 2024

Language: Английский

Citations

3

Statistical approaches for improved definition of carbon isotope excursions DOI Creative Commons
James S Eldrett, Steven C. Bergman, Daniel Minisini

et al.

Earth-Science Reviews, Journal Year: 2024, Volume and Issue: 255, P. 104851 - 104851

Published: June 27, 2024

Language: Английский

Citations

0

The impact catastrophism and Alvarez theory of mass extinctions in a retrospective, perspective and prospective: towards the Phanerozoic impact event stratigraphy DOI
Grzegorz Racki, Christian Koeberl

Earth-Science Reviews, Journal Year: 2024, Volume and Issue: 259, P. 104904 - 104904

Published: Aug. 31, 2024

Language: Английский

Citations

0

Correlation of sub-centennial-scale pulses of initial Central Atlantic Magmatic Province lavas and the end-Triassic extinctions DOI Creative Commons
Dennis V. Kent, Paul E. Olsen,

Huapei Wang

et al.

Proceedings of the National Academy of Sciences, Journal Year: 2024, Volume and Issue: 121(46)

Published: Oct. 28, 2024

The end-Triassic extinction (ETE) on land was synchronous with the initial lavas of Central Atlantic Magmatic Province (CAMP) and occurred just after brief 26 thousand year (kyr) reverse geomagnetic polarity Chron E23r that can be used for global correlation. Lava-by-lava paleomagnetic secular variation data, previously reported from Morocco northeastern United States combined our data North Mountain Basalt Fundy Basin Canada show phase CAMP volcanism in only five directional groups or pulses each occupying less than a century. first four occur during ~40 kyr period based available astrochronology U-Pb geochronology. coincidence major pulse ETE points to short-lived volcanic winters albedo-induced by sulfate aerosols as plausible key agent extinctions tropical continental realm, whereas looser correlations allow prolonged CO 2 emissions contribute more long-ranging effects marine realm via ocean acidification longer-term warming.

Language: Английский

Citations

0

Duration and intensity of the Late Permian (early Wuchiapingian) cool climate episode: Sclerochemical evidence from brachiopod assemblages in Iran DOI Creative Commons
Marco Viaretti, Gaia Crippa, Valentina Brombin

et al.

Palaeogeography Palaeoclimatology Palaeoecology, Journal Year: 2024, Volume and Issue: unknown, P. 112654 - 112654

Published: Dec. 1, 2024

Language: Английский

Citations

0