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Microfacies, diagenesis and hydrocarbon potential of the Neoproterozoic cap  carbonate of the southern Amazon Craton - ScienceDirect
Microfacies, diagenesis and hydrocarbon potential of the Neoproterozoic cap carbonate of the southern Amazon Craton - ScienceDirect

Geochemistry of Ediacaran cap dolostones across the Yangtze Platform, South  China: implications for diagenetic modification and seawater chemistry in  the aftermath of the Marinoan glaciation | Journal of the Geological Society
Geochemistry of Ediacaran cap dolostones across the Yangtze Platform, South China: implications for diagenetic modification and seawater chemistry in the aftermath of the Marinoan glaciation | Journal of the Geological Society

Geochronological and geochemical constraints on the origin of highly  13Ccarb-depleted calcite in basal Ediacaran cap carbonate | Geological  Magazine | Cambridge Core
Geochronological and geochemical constraints on the origin of highly 13Ccarb-depleted calcite in basal Ediacaran cap carbonate | Geological Magazine | Cambridge Core

The Ediacaran record of glaciogenic dropstones, diamictites and cap  carbonates associated with non-metamorphosed banded iron formations (BIFs)  in Iran - ScienceDirect
The Ediacaran record of glaciogenic dropstones, diamictites and cap carbonates associated with non-metamorphosed banded iron formations (BIFs) in Iran - ScienceDirect

The Marinoan cap carbonate of Svalbard: Syngenetic marine dolomite with  17O‐anomalous carbonate‐associated sulphate - Fairchild - The Depositional  Record - Wiley Online Library
The Marinoan cap carbonate of Svalbard: Syngenetic marine dolomite with 17O‐anomalous carbonate‐associated sulphate - Fairchild - The Depositional Record - Wiley Online Library

PDF) Geochronological and geochemical constraints on the origin of highly  13 C carb -depleted calcite in basal Ediacaran cap carbonate
PDF) Geochronological and geochemical constraints on the origin of highly 13 C carb -depleted calcite in basal Ediacaran cap carbonate

Open Research Online oro.open.ac.uk
Open Research Online oro.open.ac.uk

An early diagenetic deglacial origin for basal Ediacaran "cap dolostones" |  Request PDF
An early diagenetic deglacial origin for basal Ediacaran "cap dolostones" | Request PDF

Minerals | Free Full-Text | Chemically Oscillating Reactions during the  Diagenetic Formation of Ediacaran Siliceous and Carbonate Botryoids
Minerals | Free Full-Text | Chemically Oscillating Reactions during the Diagenetic Formation of Ediacaran Siliceous and Carbonate Botryoids

An early diagenetic deglacial origin for basal Ediacaran “cap dolostones”
An early diagenetic deglacial origin for basal Ediacaran “cap dolostones”

Cryptic terrestrial fungus-like fossils of the early Ediacaran Period |  Nature Communications
Cryptic terrestrial fungus-like fossils of the early Ediacaran Period | Nature Communications

A ubiquitous hydrothermal episode recorded in the sheet-crack cements of a  Marinoan cap dolostone of South China: Implication for the origin of the  extremely 13C-depleted calcite cement - ScienceDirect
A ubiquitous hydrothermal episode recorded in the sheet-crack cements of a Marinoan cap dolostone of South China: Implication for the origin of the extremely 13C-depleted calcite cement - ScienceDirect

Testing models for post-glacial 'cap dolostone' deposition: Nuccaleena  Formation, South Australia
Testing models for post-glacial 'cap dolostone' deposition: Nuccaleena Formation, South Australia

The tempo of Ediacaran evolution | Science Advances
The tempo of Ediacaran evolution | Science Advances

Localities of studied cap dolostone sections on the Yangtze Platform.... |  Download Scientific Diagram
Localities of studied cap dolostone sections on the Yangtze Platform.... | Download Scientific Diagram

Geochemistry of Ediacaran cap dolostones across the Yangtze Platform, South  China: implications for diagenetic modification and seawater chemistry in  the aftermath of the Marinoan glaciation | Journal of the Geological Society
Geochemistry of Ediacaran cap dolostones across the Yangtze Platform, South China: implications for diagenetic modification and seawater chemistry in the aftermath of the Marinoan glaciation | Journal of the Geological Society

Figure 2 from Are basal Ediacaran (635 Ma) post-glacial “cap dolostones”  diachronous? | Semantic Scholar
Figure 2 from Are basal Ediacaran (635 Ma) post-glacial “cap dolostones” diachronous? | Semantic Scholar

Karstic features and subsequent barite precipitation in cap dolostones....  | Download Scientific Diagram
Karstic features and subsequent barite precipitation in cap dolostones.... | Download Scientific Diagram

A transient peak in marine sulfate after the 635-Ma snowball Earth | PNAS
A transient peak in marine sulfate after the 635-Ma snowball Earth | PNAS

Figure 2 from Are basal Ediacaran (635 Ma) post-glacial “cap dolostones”  diachronous? | Semantic Scholar
Figure 2 from Are basal Ediacaran (635 Ma) post-glacial “cap dolostones” diachronous? | Semantic Scholar

Chapter 18. The Ediacaran Period
Chapter 18. The Ediacaran Period

Frontiers | New Facies Model and Carbon Isotope Stratigraphy for an  Ediacaran Carbonate Platform From South America (Tamengo Formation—Corumbá  Group, SW Brazil)
Frontiers | New Facies Model and Carbon Isotope Stratigraphy for an Ediacaran Carbonate Platform From South America (Tamengo Formation—Corumbá Group, SW Brazil)

Geochronological and geochemical constraints on the origin of highly  13Ccarb-depleted calcite in basal Ediacaran cap carbonate | Geological  Magazine | Cambridge Core
Geochronological and geochemical constraints on the origin of highly 13Ccarb-depleted calcite in basal Ediacaran cap carbonate | Geological Magazine | Cambridge Core

A hydrothermal origin for isotopically anomalous cap dolostone cements from  south China | Nature
A hydrothermal origin for isotopically anomalous cap dolostone cements from south China | Nature

PDF) Geochronological and geochemical constraints on the origin of highly  13 C carb -depleted calcite in basal Ediacaran cap carbonate
PDF) Geochronological and geochemical constraints on the origin of highly 13 C carb -depleted calcite in basal Ediacaran cap carbonate