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The redox structure of Ediacaran and early Cambrian oceans and its controls
The rapid diversification of early animals during the Ediacaran (635–541 Ma) and early
Cambrian (ca. 541–509 Ma) has frequently been attributed to increasing oceanic …
Cambrian (ca. 541–509 Ma) has frequently been attributed to increasing oceanic …
Carbon pools and fluxes in the China Seas and adjacent oceans
Abstract The China Seas include the South China Sea, East China Sea, Yellow Sea, and
Bohai Sea. Located off the Northwestern Pacific margin, covering 4700000 km 2 from …
Bohai Sea. Located off the Northwestern Pacific margin, covering 4700000 km 2 from …
Extensive primary production promoted the recovery of the Ediacaran Shuram excursion
Member IV of the Ediacaran Doushantuo Formation records the recovery from the most
negative carbon isotope excursion in Earth history. However, the main biogeochemical …
negative carbon isotope excursion in Earth history. However, the main biogeochemical …
Chemical–to–reverse weathering triggered a pronounced positive carbon isotope excursion in a forced regressive to transgressive dolostone succession during the …
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 …
witnessing the coupled evolution of tectonism, climate, marine environment, and …
The hidden role of dissolved organic carbon in the biogeochemical cycle of carbon in modern redox-stratified lakes
The dissolved organic carbon (DOC) reservoir plays a critical role in the C cycle of marine
and freshwater environments because of its size and implication in many biogeochemical …
and freshwater environments because of its size and implication in many biogeochemical …
Dynamic interplay of biogeochemical C, S and Ba cycles in response to the Shuram oxygenation event
Compared with Phanerozoic strata, sulfate minerals are relatively rare in the Precambrian
record; this is probably due to the lower concentrations of sulfate in dominantly anoxic …
record; this is probably due to the lower concentrations of sulfate in dominantly anoxic …
Deep carbon cycle in subduction zones
The carbon cycle between the deep Earth and the atmosphere (ie, the deep carbon cycle)
can significantly affect the global climate on both long and short time scales. Although …
can significantly affect the global climate on both long and short time scales. Although …
A deep marine organic carbon reservoir in the non-glacial Cryogenian ocean (Nanhua Basin, South China) revealed by organic carbon isotopes
The late-Cryogenian warm (non-glacial) interval (c. 660− c. 650 Ma) is potentially of great
significance to the co-evolution between life and the surface environment during the …
significance to the co-evolution between life and the surface environment during the …
Astronomical time scale for the lower Doushantuo Formation of early Ediacaran, South China
Abstract Nearly 90% of the Ediacaran Period (635–541 Ma) of the Neoproterozoic is
represented by the Doushantuo Formation (DST Fm) in South China. Its lowest Member I is …
represented by the Doushantuo Formation (DST Fm) in South China. Its lowest Member I is …
Making sense of massive carbon isotope excursions with an inverse carbon cycle model
The beginning and end of the Proterozoic Eon are marked by extreme variations in
carbonate carbon isotope values that have been interpreted to record massive perturbations …
carbonate carbon isotope values that have been interpreted to record massive perturbations …