The paradox of drowned carbonate platforms and the origin of Cretaceous Pacific guyots
The paradox of drowned carbonate platforms and the origin of Cretaceous Pacific guyots
Geochemical, stratigraphic and palaeolatitudinal data from deep boreholes drilled through Pacific guyots—flat-topped seamounts—help to explain the drowning of these Cretaceous shallow-water carbonate platforms that once thrived through the accumulation of biogenic and inorganic calcium carbonate sediment in mid-oceanic regions. The platforms drowned sequentially over a 60-million-year interval while they were being transported northward by Pacific plate motion through a narrow equatorial zone (∼0–10° S). Such platforms were apparently resistant to the effects of Cretaceous oceanic anoxic events. Although the mechanism responsible for drowning remains unknown, the tropics have not always been the refuge for atolls that they are today
889–894
Wilson, Paul
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Jenkyns, Hugh C.
fff51099-4260-4b20-b72b-d5828994b2c5
Elderfield, Henry
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Larson, Roger L.
536f436a-1541-4342-bfc7-cbd49ec5a432
30 April 1998
Wilson, Paul
f940a9f0-fa5a-4a64-9061-f0794bfbf7c6
Jenkyns, Hugh C.
fff51099-4260-4b20-b72b-d5828994b2c5
Elderfield, Henry
f16b0e78-6878-4cf8-8e48-a449f9b84879
Larson, Roger L.
536f436a-1541-4342-bfc7-cbd49ec5a432
Wilson, Paul, Jenkyns, Hugh C., Elderfield, Henry and Larson, Roger L.
(1998)
The paradox of drowned carbonate platforms and the origin of Cretaceous Pacific guyots.
Nature, 392, .
(doi:10.1038/31865).
Abstract
Geochemical, stratigraphic and palaeolatitudinal data from deep boreholes drilled through Pacific guyots—flat-topped seamounts—help to explain the drowning of these Cretaceous shallow-water carbonate platforms that once thrived through the accumulation of biogenic and inorganic calcium carbonate sediment in mid-oceanic regions. The platforms drowned sequentially over a 60-million-year interval while they were being transported northward by Pacific plate motion through a narrow equatorial zone (∼0–10° S). Such platforms were apparently resistant to the effects of Cretaceous oceanic anoxic events. Although the mechanism responsible for drowning remains unknown, the tropics have not always been the refuge for atolls that they are today
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Published date: 30 April 1998
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Local EPrints ID: 468828
URI: http://eprints.soton.ac.uk/id/eprint/468828
ISSN: 0028-0836
PURE UUID: 65e99c3b-fbc3-4ed7-bfc7-cc85463c7de3
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Date deposited: 26 Aug 2022 16:52
Last modified: 17 Mar 2024 02:50
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Author:
Hugh C. Jenkyns
Author:
Henry Elderfield
Author:
Roger L. Larson
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