Extensive non-marine depositional setting evidenced by carbonate minerals in the Ediacaran clastic series of the western East European Craton - ScienceDirect
PDF) The Marinoan cap carbonate of Svalbard: Syngenetic marine dolomite with 17 O ‐anomalous carbonate‐associated sulphate
PDF) Global marine redox changes drove the rise and fall of the Ediacara biota
Extensive non-marine depositional setting evidenced by carbonate minerals in the Ediacaran clastic series of the western East European Craton - ScienceDirect
Massive formation of early diagenetic dolomite in the Ediacaran ocean: Constraints on the “dolomite problem”
A) Dolomite abundance versus genus richness of marine benthic... | Download Scientific Diagram
Massive formation of early diagenetic dolomite in the Ediacaran ocean: Constraints on the “dolomite problem” | PNAS
Cross-plot of δ 18 O vs. δ 13 C of the analysed dolomites. The isotope... | Download Scientific Diagram
Fracture dolomite as an archive of continental palaeo-environmental conditions | Communications Earth & Environment
Upper Ediacaran fibrous dolomite versus Ordovician fibrous calcite cement: Origin and significance as a paleoenvironmental archive - ScienceDirect
Upper Ediacaran fibrous dolomite versus Ordovician fibrous calcite cement: Origin and significance as a paleoenvironmental archive - ScienceDirect
Massive formation of early diagenetic dolomite in the Ediacaran ocean: Constraints on the “dolomite problem” | PNAS
Extensive non-marine depositional setting evidenced by carbonate minerals in the Ediacaran clastic series of the western East European Craton - ScienceDirect
Massive formation of early diagenetic dolomite in the Ediacaran ocean: Constraints on the “dolomite problem” | PNAS
Formation, diagenesis and palaeoenvironmental significance of upper Ediacaran fibrous dolomite cements - Hu - 2020 - Sedimentology - Wiley Online Library
Extensive non-marine depositional setting evidenced by carbonate minerals in the Ediacaran clastic series of the western East European Craton - ScienceDirect
PDF) Extensive marine anoxia during the terminal Ediacaran Period