The terrestrial end-Permian mass extinction in the paleotropics postdates the marine extinction
The end-Permian mass extinction was the most severe ecological event during the
Phanerozoic and has long been presumed contemporaneous across terrestrial and marine …
Phanerozoic and has long been presumed contemporaneous across terrestrial and marine …
The expansion of land plants during the Late Devonian contributed to the marine mass extinction
The evolution and expansion of land plants brought about one of the most dramatic shifts in
the history of the Earth system—the birth of modern soils—and likely stimulated massive …
the history of the Earth system—the birth of modern soils—and likely stimulated massive …
[HTML][HTML] Evidence for variable provenance of Mercury anomalies during the Smithian–Spathian (Olenekian)
Mercury (Hg) enrichment recorded in Smithian to Spathian (Olenekian) marine sedimentary
successions has been used to link putative renewed Siberian Traps Large Igneous Province …
successions has been used to link putative renewed Siberian Traps Large Igneous Province …
[HTML][HTML] 二叠纪-三叠纪转折期升温事件与陆地生态系统
张华， 蔡垚峰， 角升林， 沈树忠 - 第四纪研究, 2024 - dsjyj.com.cn
张华, 蔡垚峰, 角升林, 沈树忠. 2024. 二叠纪-三叠纪转折期升温事件与陆地生态系统.
第四纪研究, 44 (5): 1093-1107. doi: 10.11928/j. issn. 1001-7410.2024. 05.02引用本文: 张华 …
第四纪研究, 44 (5): 1093-1107. doi: 10.11928/j. issn. 1001-7410.2024. 05.02引用本文: 张华 …
Volcanogenic mercury and plant mutagenesis during the end-Permian mass extinction: Palaeoecological perturbation in northern Pangaea
NW Paterson, VM Rossi, E Schneebeli-Hermann - Gondwana Research, 2024 - Elsevier
The end-Permian extinction (EPE)(∼ 251.9 Ma) is considered the most severe biotic crisis in
Earth's history. Rapid climatic change and oceanic acidification triggered by Siberian Traps …
Earth's history. Rapid climatic change and oceanic acidification triggered by Siberian Traps …
Diachronous end-Permian terrestrial crises in North and South China
Climate breakdown driven by massive volcanic eruptions was the likely cause of the
terrestrial Permian–Triassic mass extinction (ca. 252 Ma). However, establishing the …
terrestrial Permian–Triassic mass extinction (ca. 252 Ma). However, establishing the …
Spatiotemporal disparity of volcanogenic mercury records in the southwestern Neo-Tethys Ocean during the Permian–Triassic transition
J Chen, Y Zhou, W Liu, B Lu, J Wu, G Sun… - Global and Planetary …, 2024 - Elsevier
Abstract The Permian–Triassic (P-Tr) transition marks a vital period in Earth's history,
characterized by major environmental perturbations and the largest mass extinction event of …
characterized by major environmental perturbations and the largest mass extinction event of …
Middle Neoproterozoic (Tonian) polar wander of South China: Paleomagnetism and ID‐TIMS U‐Pb geochronology of the Laoshanya Formation
Paleomagnetic records of middle Neoproterozoic (820 to 780 Ma) rocks display high
amplitude directional variations that lead to large discrepancies in paleogeographic …
amplitude directional variations that lead to large discrepancies in paleogeographic …
[HTML][HTML] Global warming event and the changeover of terrestrial ecosystems during the Permian-Triassic Transition
Z Hua, CAI Yaofeng, J Shenglin, S Shuzhong - Quaternary Sciences, 2024 - dzkx.org
At the end of the Permian, ca. 252 million years ago, intense volcanic activities released a
massive amount of CO 2, CH 4 and other greenhouse gases, resulting the surface seawater …
massive amount of CO 2, CH 4 and other greenhouse gases, resulting the surface seawater …