Large excursions in δ^(13)C and δ^(34)S are found in sedimentary rocks from the Ediacaran Period that may provide detailed mechanistic information about oxidation of Earth’s surface. However, poor stratigraphic resolution and diagenetic concerns have thus far limited the interpretation of these records. Here, we present a high-resolution record of carbon and sulfur isotopes from the Khufai Formation, leading up to and including the onset of the Shuram carbon isotope excursion. We document large coherent excursions in the sulfur isotope composition and concentration of carbonate-associated sulfate (CAS) that occur both independently and synchronously with the carbon isotope excursion. Isotopic changes appear decoupled from major stratigraphi...
The terminal Neoproterozoic Era (850-542 Ma) is characterized by the most pronounced positive sulfur...
International audienceThe terminal Neoproterozoic Era (850–542 Ma) is characterized by the most pron...
International audienceThe terminal Neoproterozoic Era (850–542 Ma) is characterized by the most pron...
Large excursions in δ^(13)C and δ^(34)S are found in sedimentary rocks from the Ediacaran Period tha...
We report new sulfur isotope compositions (δ34S) in carbonate associated sulfate (CAS) and pyrite fr...
We report new sulfur isotope compositions (δ34S) in carbonate associated sulfate (CAS) and pyrite fr...
We report new sulfur isotope compositions (δ34S) in carbonate associated sulfate (CAS) and pyrite fr...
We report new sulfur isotope compositions (δ³⁴S) in carbonate associated sulfate (CAS) and pyrite fr...
We report new sulfur isotope compositions (δ34S) in carbonate associated sulfate (CAS) and pyrite fr...
The Ediacaran–Cambrian (E–C) transition was a critical period in Earth’s history, and it was charact...
Dynamics of &sigma34S and &sigma33S of oceanic sulfate and sedimentary pyrite over geologic time has...
© 2019 Elsevier B.V. The Proterozoic Eon spans Earth\u27s middle age during which many important tr...
High amplitude positive carbon isotope excursions in the Late Devonian, the punctata and Kellwasser ...
High amplitude positive carbon isotope excursions in the Late Devonian, the punctata and Kellwasser ...
High amplitude positive carbon isotope excursions in the Late Devonian, the punctata and Kellwasser ...
The terminal Neoproterozoic Era (850-542 Ma) is characterized by the most pronounced positive sulfur...
International audienceThe terminal Neoproterozoic Era (850–542 Ma) is characterized by the most pron...
International audienceThe terminal Neoproterozoic Era (850–542 Ma) is characterized by the most pron...
Large excursions in δ^(13)C and δ^(34)S are found in sedimentary rocks from the Ediacaran Period tha...
We report new sulfur isotope compositions (δ34S) in carbonate associated sulfate (CAS) and pyrite fr...
We report new sulfur isotope compositions (δ34S) in carbonate associated sulfate (CAS) and pyrite fr...
We report new sulfur isotope compositions (δ34S) in carbonate associated sulfate (CAS) and pyrite fr...
We report new sulfur isotope compositions (δ³⁴S) in carbonate associated sulfate (CAS) and pyrite fr...
We report new sulfur isotope compositions (δ34S) in carbonate associated sulfate (CAS) and pyrite fr...
The Ediacaran–Cambrian (E–C) transition was a critical period in Earth’s history, and it was charact...
Dynamics of &sigma34S and &sigma33S of oceanic sulfate and sedimentary pyrite over geologic time has...
© 2019 Elsevier B.V. The Proterozoic Eon spans Earth\u27s middle age during which many important tr...
High amplitude positive carbon isotope excursions in the Late Devonian, the punctata and Kellwasser ...
High amplitude positive carbon isotope excursions in the Late Devonian, the punctata and Kellwasser ...
High amplitude positive carbon isotope excursions in the Late Devonian, the punctata and Kellwasser ...
The terminal Neoproterozoic Era (850-542 Ma) is characterized by the most pronounced positive sulfur...
International audienceThe terminal Neoproterozoic Era (850–542 Ma) is characterized by the most pron...
International audienceThe terminal Neoproterozoic Era (850–542 Ma) is characterized by the most pron...