In marine sediments, formation of pyrite (FeS 2) is promoted by both organoclastic sulfate
reduction (OSR) and sulfate-driven anaerobic oxidation of methane (SD-AOM), and these …

Molybdenum (Mo) is a trace element sensitive to oceanic redox conditions. The fidelity of
sedimentary Mo as a paleoredox proxy of coeval seawater depends on the extent of Mo …

Methane seepage has been extensively observed in various continental margin settings. It
has profound effects on the marine redox environment and the molybdenum (Mo) cycles in …

Abstract The Kuroshio Current, originating from the West Pacific Warm Pool and flowing
through the Okinawa Trough, connects the equator and the subtropical West Pacific and …

The evolution of Jurassic carbonates is globally significant for understanding the
depositional framework, diagenetic phases and sedimentary characteristics of shallow …

Methane release from marine sediments strongly influences the local seafloor environment
and ecosystems, and may impact Earth's climate system. Recent studies revealed …

Paleoenvironmental reconstructions of coastal areas during geological history are critical for
understanding past responses to marine transgression. Identifying transgressive layers in …

The formation of authigenic pyrite in marine sediments involves multiple reactions between
ferrous iron (Fe 2+) and hydrogen sulfide (H 2 S). Ferrous iron is commonly provided …

Copper-zinc isotopic excursions in carbonate sedimentary successions are used to trace
oceanic chemistry fluctuations that occurred in the geological past. However, whether …

Sulphate deficiency makes lake environments a key source of atmospheric methane
because sulphate-driven anaerobic oxidation of methane (SD-AOM) is hindered. Miocene to …