Recurrent photic zone euxinia limited ocean oxygenation and animal evolution during the Ediacaran

W Zheng, A Zhou, SK Sahoo, MR Nolan… - Nature …, 2023 - nature.com
Abstract The Ediacaran Period (~ 635–539 Ma) is marked by the emergence and
diversification of complex metazoans linked to ocean redox changes, but the processes and …

The role of LIPs in Phanerozoic mass extinctions: An Hg perspective

Y Zhou, Y Li, W Zheng, S Tang, S Pan, J Chen… - Earth-Science …, 2024 - Elsevier
Abstract All of the Big Five mass extinctions (BFMEs) of the Phanerozoic are postulated to
have been associated with eruptions of large igneous provinces (LIPs), although the role of …

Geochemical and hydrographic evolution of the Late Devonian Appalachian Seaway: linking sedimentation, redox, and salinity across time and space

GJ Gilleaudeau, W Wei, MN Remírez… - Geochemistry …, 2023 - Wiley Online Library
Continental interiors were flooded by epeiric seas during many intervals of the geologic
past. Few modern analogs exist for these environments, however, and basic variables such …

Mercury isotope evidence for Middle Ordovician photic-zone euxinia: Implications for termination of the Great Ordovician biodiversification event

M Liu, W Yuan, C Fang, X Wang, N Tan, M Zhao… - Gondwana …, 2025 - Elsevier
Abstract The Darriwilian (Middle Ordovician) is marked by a striking peak of the Great
Ordovician Biodiversification Event (GOBE) followed by an abrupt∼ 50% decline in …

The expansion of land plants during the Late Devonian contributed to the marine mass extinction

MS Smart, G Filippelli, WP Gilhooly III, K Ozaki… - … Earth & Environment, 2023 - nature.com
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 …

Applications of mercury stable isotopes for tracing volcanism in the geologic record

Q Gong, MX Ling, W Zheng - Science China Earth Sciences, 2024 - Springer
Mercury (Hg) enrichments in ancient sediments have been used as a proxy of volcanism,
especially large igneous province (LIP) eruptions. However, considering the existence of …

[HTML][HTML] Astronomically paced climate and carbon cycle feedbacks in the lead-up to the Late Devonian Kellwasser Crisis

NMA Wichern, OM Bialik, T Nohl, LME Percival… - Climate of the …, 2024 - cp.copernicus.org
Repeated carbon isotope excursions and widespread organic-rich shale deposition mark
the Middle and Upper Devonian series. Various explanations such as extensive volcanism …

Subaerial volcanism broke mid-Proterozoic environmental stasis

S Zhang, H Wang, X Wang, W Zheng, J Hao… - Science …, 2024 - science.org
The mid-Proterozoic, spanning 1.8 to 0.8 billion years ago, is recognized as a phase of
marine anoxia, low marine primary productivity (MPP), and constrained eukaryotic …

Climate-forced Hg-remobilization associated with fern mutagenesis in the aftermath of the end-Triassic extinction

R Bos, W Zheng, S Lindström, H Sanei… - Nature …, 2024 - nature.com
The long-term effects of the Central Atlantic Magmatic Province, a large igneous province
connected to the end-Triassic mass-extinction (201.5 Ma), remain largely elusive. Here, we …

Mercury isotopes record development and attenuation of photic zone euxinia during the earliest Cambrian

K Zhao, G Zhu, W Zheng, G Sun, T Li… - Global and Planetary …, 2023 - Elsevier
Abstract The Ediacaran-Cambrian transition period (ca. 550–521 Ma) witnessed the decline
of Ediacaran Biota and the rapid diversification of Cambrian biota. Numerous studies have …