
Palaeogeography Palaeoclimatology Palaeoecology, Journal Year: 2024, Volume and Issue: unknown, P. 112654 - 112654
Published: Dec. 1, 2024
Language: Английский
Palaeogeography Palaeoclimatology Palaeoecology, Journal Year: 2024, Volume and Issue: unknown, P. 112654 - 112654
Published: Dec. 1, 2024
Language: Английский
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
0Earth-Science Reviews, Journal Year: 2025, Volume and Issue: unknown, P. 105100 - 105100
Published: March 1, 2025
Language: Английский
Citations
0Chemical Geology, Journal Year: 2025, Volume and Issue: unknown, P. 122715 - 122715
Published: March 1, 2025
Language: Английский
Citations
0Elsevier eBooks, Journal Year: 2025, Volume and Issue: unknown
Published: Jan. 1, 2025
Language: Английский
Citations
0Scientific 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
0Earth-Science Reviews, Journal Year: 2024, Volume and Issue: 258, P. 104912 - 104912
Published: Oct. 7, 2024
Language: Английский
Citations
3Earth-Science Reviews, Journal Year: 2024, Volume and Issue: 255, P. 104851 - 104851
Published: June 27, 2024
Language: Английский
Citations
0Earth-Science Reviews, Journal Year: 2024, Volume and Issue: 259, P. 104904 - 104904
Published: Aug. 31, 2024
Language: Английский
Citations
0Proceedings 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
0Palaeogeography Palaeoclimatology Palaeoecology, Journal Year: 2024, Volume and Issue: unknown, P. 112654 - 112654
Published: Dec. 1, 2024
Language: Английский
Citations
0