Add to ORKGAfter the severe glaciation that finished at about 630 million years ago, during the late Neoproterozoic, the central region of Brazil was the site of extensive deposition of platformal carbonates of Araras Group
One of the main questions on Neoproterozoic geology regards the extent and dynamics of the glacial s...
One of the main questions on Neoproterozoic geology regards the extent and dynamics of the glacial s...
The stable isotope record of marine carbon indicates that the Proterozoic Eon began and ended with e...
International audienceOcean and atmosphere oxidation in the Ediacaran Period paved the way for the d...
We present carbon and oxygen isotopic data on carbonates along three profiles of the Neoproterozoic ...
Carbon isotope fluctuations in Precambrian sedimentary carbonates between 2.8 Ga and 0.60 Ga in Braz...
International audienceThe snowball Earth hypothesis postulates that the planet was entirely covered ...
This paper addresses the carbon isotope variations observed on Mesoproterozoic and Neoproterozoic ca...
After the late Cryogenian glaciation the central region of Brazil was the site of extensive depositi...
Life on Earth transitioned from being mainly dominated by bacteria prior to the Cryogenian Snowball ...
Neoproterozoic carbonate rocks comprise different stratigraphic units in the southern part of the Es...
texto completo: acesso restrito. p. 143–167The Neoproterozoic successions of South America largely ...
Although the pre-glacial Proterozoic isotopic record is poorly constrained, it is apparent that the ...
Shallow intracratonic basins developed across a large area of the central part of the Australian cra...
ABSTRACT: This report reviews and incorporates new elemental and isotope chemostratigraphic data for...
One of the main questions on Neoproterozoic geology regards the extent and dynamics of the glacial s...
One of the main questions on Neoproterozoic geology regards the extent and dynamics of the glacial s...
The stable isotope record of marine carbon indicates that the Proterozoic Eon began and ended with e...
International audienceOcean and atmosphere oxidation in the Ediacaran Period paved the way for the d...
We present carbon and oxygen isotopic data on carbonates along three profiles of the Neoproterozoic ...
Carbon isotope fluctuations in Precambrian sedimentary carbonates between 2.8 Ga and 0.60 Ga in Braz...
International audienceThe snowball Earth hypothesis postulates that the planet was entirely covered ...
This paper addresses the carbon isotope variations observed on Mesoproterozoic and Neoproterozoic ca...
After the late Cryogenian glaciation the central region of Brazil was the site of extensive depositi...
Life on Earth transitioned from being mainly dominated by bacteria prior to the Cryogenian Snowball ...
Neoproterozoic carbonate rocks comprise different stratigraphic units in the southern part of the Es...
texto completo: acesso restrito. p. 143–167The Neoproterozoic successions of South America largely ...
Although the pre-glacial Proterozoic isotopic record is poorly constrained, it is apparent that the ...
Shallow intracratonic basins developed across a large area of the central part of the Australian cra...
ABSTRACT: This report reviews and incorporates new elemental and isotope chemostratigraphic data for...
One of the main questions on Neoproterozoic geology regards the extent and dynamics of the glacial s...
One of the main questions on Neoproterozoic geology regards the extent and dynamics of the glacial s...
The stable isotope record of marine carbon indicates that the Proterozoic Eon began and ended with e...