Articles | Volume 11, issue 12
Clim. Past, 11, 1751–1767, 2015
https://doi.org/10.5194/cp-11-1751-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Clim. Past, 11, 1751–1767, 2015
https://doi.org/10.5194/cp-11-1751-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Research article
18 Dec 2015
Research article
| 18 Dec 2015
Did high Neo-Tethys subduction rates contribute to early Cenozoic warming?
G. Hoareau et al.
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Cited
11 citations as recorded by crossref.
- Geochemical characterization of ophiolites in the Alpine-Himalayan Orogenic Belt: Magmatically and tectonically diverse evolution of the Mesozoic Neotethyan oceanic crust H. Furnes et al. 10.1016/j.earscirev.2020.103258
- Potential links between continental rifting, CO2 degassing and climate change through time S. Brune et al. 10.1038/s41561-017-0003-6
- A sink- or a source-driven carbon cycle at the geological timescale? Relative importance of palaeogeography versus solid Earth degassing rate in the Phanerozoic climatic evolution Y. GODDÉRIS & Y. DONNADIEU 10.1017/S0016756817001054
- Magmatic Forcing of Cenozoic Climate? P. Sternai et al. 10.1029/2018JB016460
- Ophiolites of the Central Asian Orogenic Belt: Geochemical and petrological characterization and tectonic settings H. Furnes & I. Safonova 10.1016/j.gsf.2018.12.007
- Sediment control on subduction plate speeds W. Behr & T. Becker 10.1016/j.epsl.2018.08.057
- High-temperature overprint in (U)HPM rocks exhumed from subduction zones; A product of isothermal decompression or a consequence of slab break-off (slab rollback)? S. Faryad & S. Cuthbert 10.1016/j.earscirev.2020.103108
- Tectonic evolution and geodynamics of the Neo-Tethys Ocean R. Zhu et al. 10.1007/s11430-021-9845-7
- Subtropical climate conditions and mangrove growth in Arctic Siberia during the early Eocene G. Suan et al. 10.1130/G38547.1
- A warm or a cold early Earth? New insights from a 3-D climate-carbon model B. Charnay et al. 10.1016/j.epsl.2017.06.029
- Towards interactive global paleogeographic maps, new reconstructions at 60, 40 and 20 Ma F. Poblete et al. 10.1016/j.earscirev.2021.103508
11 citations as recorded by crossref.
- Geochemical characterization of ophiolites in the Alpine-Himalayan Orogenic Belt: Magmatically and tectonically diverse evolution of the Mesozoic Neotethyan oceanic crust H. Furnes et al. 10.1016/j.earscirev.2020.103258
- Potential links between continental rifting, CO2 degassing and climate change through time S. Brune et al. 10.1038/s41561-017-0003-6
- A sink- or a source-driven carbon cycle at the geological timescale? Relative importance of palaeogeography versus solid Earth degassing rate in the Phanerozoic climatic evolution Y. GODDÉRIS & Y. DONNADIEU 10.1017/S0016756817001054
- Magmatic Forcing of Cenozoic Climate? P. Sternai et al. 10.1029/2018JB016460
- Ophiolites of the Central Asian Orogenic Belt: Geochemical and petrological characterization and tectonic settings H. Furnes & I. Safonova 10.1016/j.gsf.2018.12.007
- Sediment control on subduction plate speeds W. Behr & T. Becker 10.1016/j.epsl.2018.08.057
- High-temperature overprint in (U)HPM rocks exhumed from subduction zones; A product of isothermal decompression or a consequence of slab break-off (slab rollback)? S. Faryad & S. Cuthbert 10.1016/j.earscirev.2020.103108
- Tectonic evolution and geodynamics of the Neo-Tethys Ocean R. Zhu et al. 10.1007/s11430-021-9845-7
- Subtropical climate conditions and mangrove growth in Arctic Siberia during the early Eocene G. Suan et al. 10.1130/G38547.1
- A warm or a cold early Earth? New insights from a 3-D climate-carbon model B. Charnay et al. 10.1016/j.epsl.2017.06.029
- Towards interactive global paleogeographic maps, new reconstructions at 60, 40 and 20 Ma F. Poblete et al. 10.1016/j.earscirev.2021.103508
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Short summary
The impact of Neo-Tethys closure on early Cenozoic warming has been tested. First, the volume of subducted sediments and the amount of CO2 emitted along the northern Tethys margin has been calculated. Second, corresponding pCO2 have been tested using the GEOCLIM model. Despite high CO2 production, maximum pCO2 values (750ppm) do not reach values inferred from proxies. Other cited sources of excess CO2 such as the NAIP are also below fluxes required by GEOCLIM to fit with proxy data.
The impact of Neo-Tethys closure on early Cenozoic warming has been tested. First, the volume of...
