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Communication Dans Un Congrès Année : 2016

Can eustatic charts go beyond first-order? Insights from the Permo-Triassic

Résumé

To the first order, eustatic charts are in accord with our understanding of the geodynamic processes that controlsea level. By extrapolation, second-order features are also thought to obey to the same rules, and are thus oftentaken for granted. But this assumption may be jeopardized by a close examination of a characteristic example.The Permo-Triassic period is characteristic for both its purported eustatic signal and its geodynamic and climaticsetting are well defined and contrasted. Both the fragmentation of the Pangean supercontinent and the late Paleozoicmelting of ice sheets argue for a rise of the eustatic sea level (ESL) whereas eustatic charts show the opposite. Herewe review the possible mechanisms that could explain the apparent sea level low, and find that some of them dolower the ESL while others instead only modify the referential, either uplifting continents or tilting the marginswhere the control points are located. In the first category, we find that (i) dynamic deflections of the Earth surfaceabove subduction zones and their location with respect to continents primarily control absolute sea level while thePangean supercontinent forms and breaks up, (ii) endorheism that ubiquitously developed at the time of Pangeanaggregation also contributed to lowering the ESL by storing water out of the oceanic reservoir. In the secondcategory, we show that (i) the thermal uplift associated to supercontinental insulation and (ii) the dynamic upliftassociated with the emplacement of a superplume both give rates of change in the range of long-term changesof ESL. We also show that (iii) the dynamic tilting of continental margins not only produces apparent sea levelchanges, but also modifies the absolute sea level, which in turn may end up in the paradoxical situation whereinfingerprints of ESL drop are found in the geological record whereas ESL is actually rising. We conclude that theestablishment of second to third order absolute sea level changes may stay for a while a chimera.

Domaines

Tectonique
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Dates et versions

insu-01309247 , version 1 (29-04-2016)

Identifiants

  • HAL Id : insu-01309247 , version 1

Citer

Benjamin Guillaume, Julien Monteux, Stéphane Pochat, Laurent Husson, Gael Choblet. Can eustatic charts go beyond first-order? Insights from the Permo-Triassic. European Geosciences Union General Assembly 2016, European Geosciences Union, Apr 2016, Vienne, Austria. pp.EGU2016-9339. ⟨insu-01309247⟩
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