Contribution of deep-sourced carbon from hydrocarbon seeps to sedimentary organic carbon: Evidence from radiocarbon and stable isotope geochemistry

2021 ◽  
pp. 120572
Author(s):  
Dong Feng ◽  
John W. Pohlman ◽  
Jörn Peckmann ◽  
Yuedong Sun ◽  
Yu Hu ◽  
...  
1992 ◽  
Vol 29 (8) ◽  
pp. 1662-1673 ◽  
Author(s):  
Harald Strauss ◽  
Stefan Bengtson ◽  
Paul M. Myrow ◽  
Gonzalo Vidal

A sequence of clastic sediments in southeastern Newfoundland straddling the Precambrian–Cambrian boundary has been investigated for its stable isotope geochemistry of carbon and sulfur and acid-resistant organic-walled microfossils. A detailed study of the Chapel Island Formation, which includes the boundary interval, has revealed fluctuations in the isotopic composition of organic carbon. These are largely interpreted as caused by differences in the depositional environments. Highly variable sulfur isotopic compositions indicate bacterial sulfate reduction as a pyrite-forming process, sometimes under sulfate-limited conditions. Palynological results are quite limited with respect to diagnostic microfossils.


2021 ◽  
Author(s):  
MOHAMMAD ASIF ◽  
Lei Wang ◽  
Randy Hazlett ◽  
Yu-Shu Wu ◽  
Keka Ojha

Lithos ◽  
2019 ◽  
Vol 324-325 ◽  
pp. 640-660 ◽  
Author(s):  
Allen K. Andersen ◽  
Peter B. Larson ◽  
Michael A. Cosca

Geologos ◽  
2016 ◽  
Vol 22 (1) ◽  
pp. 79-80
Author(s):  
Karina Apolinarska

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