Alves, Tiago Marcos ![]() |
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Abstract
Three-dimensional (3D) seismic-reflection data from the Barents Sea show geometric similarities between Permian cool-water mounds and older carbonate build-ups. In detail, the Samson Dome area records the development of polygonal mounds in Upper Permian strata, at the same time a gradual drowning event took place in the Barents Sea. The presence of these polygonal mounds is interpreted to reflect: i) shallower conditions around the Samson Dome when compared to other parts of the Barents Sea; ii) earlier drowning of Upper Permian mounds towards the west and northwest into the Ottar Basin. Based on the recognition of mounds ~20 metres below the PermianTriassic stratigraphic boundary, this paper proposes for the first time that shallow areas of the Barents Sea, such as the Samson Dome, witnessed sustained organic productivity until the onset of the P-T extinction event.
Item Type: | Article |
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Date Type: | Publication |
Status: | Published |
Schools: | Earth and Environmental Sciences |
Subjects: | Q Science > QE Geology |
Uncontrolled Keywords: | Pangaea; Barents Sea; carbonate build-ups; Upper Permian mounds; P-T boundary. |
Additional Information: | Article first published online: 27 DEC 2015 Pdf uploaded in accordance with publisher's policy at http://www.sherpa.ac.uk/romeo/issn/0954-4879/ (accessed 10/03/2016) |
Publisher: | Wiley-Blackwell |
ISSN: | 1365-3121 |
Date of First Compliant Deposit: | 30 March 2016 |
Date of Acceptance: | 10 November 2015 |
Last Modified: | 26 Nov 2024 00:00 |
URI: | https://orca.cardiff.ac.uk/id/eprint/81014 |
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