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• W237788508 endingPage "188" @default.
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• W237788508 abstract "Abstract During the last decades, numerous local reconstructions based on field geology were developed at the University of Lausanne (UNIL). Team members of the UNIL participated in the elaboration of a 600 Ma to present global plate tectonic model deeply rooted in geological data, controlled by geometric and kinematic constraints and coherent with forces acting at plate boundaries. In this paper, we compare values derived from the tectonic model (ages of oceanic floor, production and subduction rates, tectonic activity) with a combination of chemical proxies (namely CO 2 , 87 Sr/ 86 Sr, glaciation evidence, and sea-level variations) known to be strongly influenced by tectonics. One of the outstanding results is the observation of an overall decreasing trend in the evolution of the global tectonic activity, mean oceanic ages and plate velocities over the whole Phanerozoic. We speculate that the decreasing trend reflects the global cooling of the Earth system. Additionally, the parallel between the tectonic activity and CO 2 together with the extension of glaciations confirms the generally accepted idea of a primary control of CO 2 on climate and highlights the link between plate tectonics and CO 2 in a time scale greater than 10 7 yr. Last, the wide variations observed in the reconstructed sea-floor production rates are in contradiction with the steady-state model hypothesized by some." @default.
• W237788508 created "2016-06-24" @default.
• W237788508 creator A5017353282 @default.
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• W237788508 creator A5031418470 @default.
• W237788508 creator A5060482065 @default.
• W237788508 creator A5081234776 @default.
• W237788508 date "2015-04-01" @default.
• W237788508 modified "2023-10-16" @default.
• W237788508 title "Geodynamic evolution of the Earth over the Phanerozoic: Plate tectonic activity and palaeoclimatic indicators" @default.
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• W237788508 doi "https://doi.org/10.3724/sp.j.1261.2015.00072" @default.

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