Plate tectonic controls on atmospheric CO2levels since the Triassic
13. Climate action
Taverne
paleoclimate
carbon cycle
SDG 13 - Climate Action
geodynamic
01 natural sciences
0105 earth and related environmental sciences
DOI:
10.1073/pnas.1315657111
Publication Date:
2014-03-11T01:34:20Z
AUTHORS (6)
ABSTRACT
SignificanceAlthough plate tectonics is generally considered to be the main contributor of CO2production, despite decades of paleoproxy and solid-earth research, this very first-order assumption remains unproven. Based on estimates of total subduction-zone lengths, from a combined analysis of seismic tomography models and plate tectonic reconstructions, we have bridged a major gap between solid-earth sciences and the atmosphere and biosphere sciences by providing understanding of one of the most fundamental controls of climate: variation of plate tectonic activity of our planet. By using the subduction zone length input into the GEOCARBSULF climate model, we obtain a better fit with atmospheric CO2proxies compared with previously used plate tectonic assumptions.
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