Deposition and termination of Neoproterozoic iron formations (NIFs): New insights from NIFs in China

H Ye, CZ Wu, W Li, RX Lei, X Sun, W Hao… - Earth-Science …, 2024 - Elsevier
Over the past two decades, advancements in geochronological, sedimentary, and
geochemical studies have considerably deepened our understanding of the links between …

[HTML][HTML] Environmental controls on very high δ238U values in reducing sediments: Implications for Neoproterozoic seawater records

MO Clarkson, TC Sweere, CF Chiu, R Hennekam… - Earth-Science …, 2023 - Elsevier
Uranium isotopes (δ 238 U) are a widely applied tool for tracing global changes in oceanic
anoxia. Interpretation of seawater values and trends, often reconstructed from carbonates …

Environmental drivers of the first major animal extinction across the Ediacaran White Sea-Nama transition

SD Evans, C Tu, A Rizzo… - Proceedings of the …, 2022 - National Acad Sciences
The Ediacara Biota—the oldest communities of complex, macroscopic fossils—consists of
three temporally distinct assemblages: the Avalon (ca. 575–560 Ma), White Sea (ca. 560 …

Impact of global climate cooling on Ordovician marine biodiversity

DE Ontiveros, G Beaugrand, B Lefebvre… - Nature …, 2023 - nature.com
Global cooling has been proposed as a driver of the Great Ordovician Biodiversification
Event, the largest radiation of Phanerozoic marine animal Life. Yet, mechanistic …

Spatial pattern of marine oxygenation set by tectonic and ecological drivers over the Phanerozoic

X Wang, TJ Algeo, C Li, M Zhu - Nature Geoscience, 2023 - nature.com
Marine redox conditions (that is, oxygen levels) impact a wide array of biogeochemical
cycles, but the main controls of marine redox since the start of the Phanerozoic about 538 …

Chemical–to–reverse weathering triggered a pronounced positive carbon isotope excursion in a forced regressive to transgressive dolostone succession during the …

Y Zhang, G Zhu, X Li, Y Ai, P Duan, M Li… - Global and Planetary …, 2024 - Elsevier
Abstract The terminal Ediacaran (∼ 551–541 Ma) was a critical period in Earth's history
witnessing the coupled evolution of tectonism, climate, marine environment, and …

[HTML][HTML] Early diagenetic mobilization of rare earth elements and implications for the Ce anomaly as a redox proxy

K Zhang, GA Shields - Chemical Geology, 2023 - Elsevier
Abstract The Rare Earth Elements (REE) archived in carbonate rocks retain a wealth of
information on paleo-seawater chemistry and local-regional redox conditions. However …

Sedimentary, climatic, and provenance controls of mineral and chemical composition of the Ediacaran and Cambrian mudstones from the East European Craton

K Jewuła, J Środoń, A Kędzior, M Paszkowski… - Precambrian …, 2022 - Elsevier
Mineralogical and geochemical compositions of mudstones were used for untangling
provenance and climatic signals preserved in the upper Ediacaran-lower Cambrian strata …

[HTML][HTML] Temporal evolution of shallow marine diagenetic environments: Insights from carbonate concretions

SJ Loyd, P Meister, B Liu, K Nichols, FA Corsetti… - … et Cosmochimica Acta, 2023 - Elsevier
Early diagenesis of marine organic matter dramatically impacts Earth's surface chemistry by
changing the burial potential of carbon and promoting the formation of authigenic mineral …

Spatiotemporal variation of dissolved oxygen in the Ediacaran surface ocean and its implication for oceanic carbon cycling

Z Zhang, M Cheng, H Wang, X Chen, W Guo… - Science China Earth …, 2023 - Springer
Abstract The Ediacaran Period (635–539 Ma) witnessed the largest negative excursion in
inorganic carbon isotope (δ13Ccarb) over the Earth's geological history, also known as the …