Chaboureau, A. C., Sepulchre, P., Donnadieu, Y., & Franc, A. (2014).
Tectonic-driven climate change and the diversification of angiosperms. Proceedings of the National Academy of Sciences, 111(39),
14066–14070. https://doi.org/10.1073/pnas.1324002111.
Charney, J. G., & Eliassen, A. (1949). A numerical method for
predicting the perturbations of the Middle Latitude Westerlies.
Tellus, 1(2): 38–54. https://doi.org/10.1111/j.2153-3490.1949.
tb01258.x.
Chen, G.-S., Liu, Z., & Kutzbach, J. E. (2014). Reexamining the barrier
effect of the Tibetan Plateau on the South Asian Summer Monsoon.
Climate of the Past, 10(3),1269–1275. https://doi.org/10.5194/cp10-1269-2014.
Cogné, J. P., & Humler, E. (2006). Trends and rhythms in global
seafloor generation rate. Geochemistry, Geophysics, Geosystems, 7,
Q03011. https://doi.org/10.1029/2005GC001148.
Copper, P., & Scotese, C. R. (2003). Megareefs in Middle Devonain
super greenhouse climates. Special Publications - Geological
Society of America, 370, 209–230.
Daëron, M., Drysdale, R. N., Peral, M., Huyghe, D., Blamart, D.,
Coplen, T. B., et al. (2019). Most Earth-surface calcites precipitate
out of isotopic equilibrium. Nature Communications, 10(1), 429.
https://doi.org/10.1038/s41467-019-08336-5.
De Wit, M. J., & Furnes, H. (2016). 3.5-Ga hydrothermal fields and
diamictites in the Barberton Greenstone Belt—Paleoarchean crust in
cold environments. Science Advances, 2, e1500368. https://doi.org/
10.1126/sciadv.1500368.
Dodd, M. S., Papineau, D., Grenne, T., Slack, J. F., Rittner, M., Pirajno,
F., et al. (2017). Evidence for early life in Earth’s oldest
hydrothermal vent precipitates. Nature, 543(7643), 60–64. https://
doi.org/10.1038/nature21377.
Donnadieu, Y., Goddéris, Y., Ramstein, G., Nédélec, A., Meert,
J. (2004). A ‘snowball Earth’climate triggered by continental
break-up through changes in runoff.Nature, 428(6980), 303–306.
Donnadieu, Y., Pucéat, E., Moiroud, M., Guillocheau, F., & Deconinc,.
J. F. (2016). A better-ventilated ocean triggered by late Cretaceous
changes in continental configuration. Nature Communications, 7
(janvier), 10316. https://doi.org/10.1038/ncomms10316.
Dromart, G., Garcia, J.-P., Picard, S., Atrops, F., Lécuyer, C., &
Sheppard, S. M. F. (2003). Ice Age at the Middle–Late Jurassic
Transition? Earth and Planetary Science Letters, 213(3–4), 205–
220. https://doi.org/10.1016/S0012-821X(03)00287-5.
Dubiel, R. F., Parrish, J. T., Parrish, J. M., & Good, S. C. (1991). The
Pangaean megamonsoon: Evidence from the Upper Triassic Chinle
Formation, Colorado Plateau. Palaios, 6, 347–370.
Eiler, J. M. (2007). “Clumped-isotope” geochemistry—the study of
naturally-occurring, multiply-substituted isotopologues. Earth and
Planetary Science Letters, 262, 309–327.
Erwin, D. H. (1994). The Permo-Triassic extinction. Nature, 367, 231–
236. https://doi.org/10.1038/367231a0.
Flohn, H. (1950). Neue Anschauungen über die allgemeine Zirkulation
der Atmosphäre und ihre klimatische Bedeutung. Erdkunde, 4(3/4),
141–162.
Fluteau, F., Besse, J., Broutin, J., Ramstein, G. (2001). The Late
Permian climate. What can be inferred from climate modelling
concerning Pangea scenarios and Hercynian range altitude? Palaeogeography, Palaeoclimatology, Palaeoecology, 167, 39–71.
Fluteau, F., Ramstein, G., Besse J. (1999). Simulating the evolution of
the Asian and African Monsoons during the past 30 Myr using an
atmospheric general circulation model. Journal of Geophysical
Research, 104(D10), 11995–12018.
Fluteau, F., et al. (2006). The impacts of the Paleogeography and sea
level changes on the Mid Cretaceous climate. Palaeogeography,
Palaeoclimatology, Palaeoecology, 247(3–4), 357–381. https://doi.
org/10.1016/j.palaeo.2006.11.016
Fluteau, F., Ramstein, G., Besse, J., Guiraud, R., & Masse. J. P. (2007).
Impacts of Palaeogeography and sea level changes on the Mid
Cretaceous climate. Palaeogeography, Palaeoclimatology,
Palaeoecology, 247, 357–381.
Ghienne, J-F., Moreau, J., Degermann, L. et al. (2013). Lower
Palaeozoic unconformities in an intracratonic platform setting:
Glacial erosion versus tectonics in the eastern Murzuq Basin
(southern Libya). International Journal of Earth Sciences, 102(2),
455–482.
Goddéris, Y., Donnadieu, Y., Carretier, S., Aretz, M., Dera, G.,
Macouin, M., & Regard, V. (2017). Onset and ending of the late
Palaeozoic ice age triggered by tectonically paced rock weathering.
Nature Geoscience, 10(5): 382–386. https://doi.org/10.1038/
ngeo2931.
Granot, R., & Dyment, J. (2015). The Cretaceous opening of the South
Atlantic Ocean. Earth and Planetary Science Letters, 414(mars),
156–163. https://doi.org/10.1016/j.epsl.2015.01.015.
Haq, B. U., et al. (1987). Chronology of fluctuating sea levels since the
Triassic (250 million years ago to present). Science, 235,
1156–1166.
Haqq-Misra, J. D., et al. (2008). A revised, Hazy methane greenhouse
for the Archean Earth. Astrobiology, 8, 1127–1137.
Haug, G. H., & Tiedemann, R. (1998). Effect of the formation of the
Isthmus of Panama on Atlantic Ocean Thermohaline circulation.
Nature, 393, 673–676.
Hoareau, G., Bomou, B., van Hinsbergen, D. J. J., Carry, N., Marquer,
D. et al. (2015). Did high Neo-Tethys subduction rates contribute to
early Cenozoic warming? Climate of the Past, 11(12), 1751–1767.
Hoffman, et al. (2017). Snowball Earth climate dynamics and
Cryogenian geology-geobiology. Science Advances, 3, e1600983.
Hren, M. T., Sheldon, N. D., Grimes, S. T., Collinson, M. E, Hooker,
J. J., Bugler, M., Lohmann, K. C. (2013). Terrestrial cooling in
Northern Europe during the Eocene–Oligocene transition, PNAS,
110, 7562–7567.
Hu, S., & Boos, W. R. (2017). Competing effects of surface Albedo and
Orographic elevated heating on regional climate: Albedo-Elevation
compensation. Geophysical Research Letters, 4(13), 6966–6973.
https://doi.org/10.1002/2016GL072441.
Jaramillo, C. (2018). Evolution of the Isthmus of Panama: Biological,
Paleoceanographic and Paleoclimatological implications. In C.
Hoorn, A. Perrigo, & A. Antonelli (Eds.), Mountains, climate and
biodiversity (1st ed.). Wiley.
Jung, G., Prange, M., & Schulz, M. (2014). Uplift of Africa as a
potential cause for Neogene Intensification of the Benguela
upwelling system. Nature Geoscience, 7(10), 741–747. https://doi.
org/10.1038/ngeo2249.
Kasting, J., & Howard, M. T. (2006). Atmospheric composition and
climate on the early Earth. Philosophical Transactions of the Royal
Society B, 361, 1733–1742.
Kennett, J. P. (1977). Cenozoic evolution of Antarctic Glaciation, the
Circum-Antarctic Ocean, and their impact on global Paleoceanography. Journal of Geophysical Research, 82(27), 3843–3860.
https://doi.org/10.1029/JC082i027p03843.
Kiehl, J. T., & Shields, C. A. (2005). Climate simulation of the latest
Permian: Implications for mass extinction. Geology, 33(9), 757–
760. https://doi.org/10.1130/G21654.1.
Kutzbach, J. E., Prell, W. L., & Ruddiman, W. F. (1993). Sensitivity of
Eurasian climate to surface uplift of the Tibetan Plateau. The
Journal of Geology, 101(2), 177–190. https://doi.org/10.1086/
648215.
Knauth, L. P., & Lowe, D. R. (2003). High Archean climatic
temperature inferred from oxygen isotope geochemistry of cherts
in the 3.5 Ga Swaziland Supergroup, South Africa. Geological
Society of America Bulletin, 115, 566–580 (2003).
22 Climate Evolution on the Geological Timescale and the Role …
267
Tectonic-driven climate change and the diversification of angiosperms. Proceedings of the National Academy of Sciences, 111(39),
14066–14070. https://doi.org/10.1073/pnas.1324002111.
Charney, J. G., & Eliassen, A. (1949). A numerical method for
predicting the perturbations of the Middle Latitude Westerlies.
Tellus, 1(2): 38–54. https://doi.org/10.1111/j.2153-3490.1949.
tb01258.x.
Chen, G.-S., Liu, Z., & Kutzbach, J. E. (2014). Reexamining the barrier
effect of the Tibetan Plateau on the South Asian Summer Monsoon.
Climate of the Past, 10(3),1269–1275. https://doi.org/10.5194/cp10-1269-2014.
Cogné, J. P., & Humler, E. (2006). Trends and rhythms in global
seafloor generation rate. Geochemistry, Geophysics, Geosystems, 7,
Q03011. https://doi.org/10.1029/2005GC001148.
Copper, P., & Scotese, C. R. (2003). Megareefs in Middle Devonain
super greenhouse climates. Special Publications - Geological
Society of America, 370, 209–230.
Daëron, M., Drysdale, R. N., Peral, M., Huyghe, D., Blamart, D.,
Coplen, T. B., et al. (2019). Most Earth-surface calcites precipitate
out of isotopic equilibrium. Nature Communications, 10(1), 429.
https://doi.org/10.1038/s41467-019-08336-5.
De Wit, M. J., & Furnes, H. (2016). 3.5-Ga hydrothermal fields and
diamictites in the Barberton Greenstone Belt—Paleoarchean crust in
cold environments. Science Advances, 2, e1500368. https://doi.org/
10.1126/sciadv.1500368.
Dodd, M. S., Papineau, D., Grenne, T., Slack, J. F., Rittner, M., Pirajno,
F., et al. (2017). Evidence for early life in Earth’s oldest
hydrothermal vent precipitates. Nature, 543(7643), 60–64. https://
doi.org/10.1038/nature21377.
Donnadieu, Y., Goddéris, Y., Ramstein, G., Nédélec, A., Meert,
J. (2004). A ‘snowball Earth’climate triggered by continental
break-up through changes in runoff.Nature, 428(6980), 303–306.
Donnadieu, Y., Pucéat, E., Moiroud, M., Guillocheau, F., & Deconinc,.
J. F. (2016). A better-ventilated ocean triggered by late Cretaceous
changes in continental configuration. Nature Communications, 7
(janvier), 10316. https://doi.org/10.1038/ncomms10316.
Dromart, G., Garcia, J.-P., Picard, S., Atrops, F., Lécuyer, C., &
Sheppard, S. M. F. (2003). Ice Age at the Middle–Late Jurassic
Transition? Earth and Planetary Science Letters, 213(3–4), 205–
220. https://doi.org/10.1016/S0012-821X(03)00287-5.
Dubiel, R. F., Parrish, J. T., Parrish, J. M., & Good, S. C. (1991). The
Pangaean megamonsoon: Evidence from the Upper Triassic Chinle
Formation, Colorado Plateau. Palaios, 6, 347–370.
Eiler, J. M. (2007). “Clumped-isotope” geochemistry—the study of
naturally-occurring, multiply-substituted isotopologues. Earth and
Planetary Science Letters, 262, 309–327.
Erwin, D. H. (1994). The Permo-Triassic extinction. Nature, 367, 231–
236. https://doi.org/10.1038/367231a0.
Flohn, H. (1950). Neue Anschauungen über die allgemeine Zirkulation
der Atmosphäre und ihre klimatische Bedeutung. Erdkunde, 4(3/4),
141–162.
Fluteau, F., Besse, J., Broutin, J., Ramstein, G. (2001). The Late
Permian climate. What can be inferred from climate modelling
concerning Pangea scenarios and Hercynian range altitude? Palaeogeography, Palaeoclimatology, Palaeoecology, 167, 39–71.
Fluteau, F., Ramstein, G., Besse J. (1999). Simulating the evolution of
the Asian and African Monsoons during the past 30 Myr using an
atmospheric general circulation model. Journal of Geophysical
Research, 104(D10), 11995–12018.
Fluteau, F., et al. (2006). The impacts of the Paleogeography and sea
level changes on the Mid Cretaceous climate. Palaeogeography,
Palaeoclimatology, Palaeoecology, 247(3–4), 357–381. https://doi.
org/10.1016/j.palaeo.2006.11.016
Fluteau, F., Ramstein, G., Besse, J., Guiraud, R., & Masse. J. P. (2007).
Impacts of Palaeogeography and sea level changes on the Mid
Cretaceous climate. Palaeogeography, Palaeoclimatology,
Palaeoecology, 247, 357–381.
Ghienne, J-F., Moreau, J., Degermann, L. et al. (2013). Lower
Palaeozoic unconformities in an intracratonic platform setting:
Glacial erosion versus tectonics in the eastern Murzuq Basin
(southern Libya). International Journal of Earth Sciences, 102(2),
455–482.
Goddéris, Y., Donnadieu, Y., Carretier, S., Aretz, M., Dera, G.,
Macouin, M., & Regard, V. (2017). Onset and ending of the late
Palaeozoic ice age triggered by tectonically paced rock weathering.
Nature Geoscience, 10(5): 382–386. https://doi.org/10.1038/
ngeo2931.
Granot, R., & Dyment, J. (2015). The Cretaceous opening of the South
Atlantic Ocean. Earth and Planetary Science Letters, 414(mars),
156–163. https://doi.org/10.1016/j.epsl.2015.01.015.
Haq, B. U., et al. (1987). Chronology of fluctuating sea levels since the
Triassic (250 million years ago to present). Science, 235,
1156–1166.
Haqq-Misra, J. D., et al. (2008). A revised, Hazy methane greenhouse
for the Archean Earth. Astrobiology, 8, 1127–1137.
Haug, G. H., & Tiedemann, R. (1998). Effect of the formation of the
Isthmus of Panama on Atlantic Ocean Thermohaline circulation.
Nature, 393, 673–676.
Hoareau, G., Bomou, B., van Hinsbergen, D. J. J., Carry, N., Marquer,
D. et al. (2015). Did high Neo-Tethys subduction rates contribute to
early Cenozoic warming? Climate of the Past, 11(12), 1751–1767.
Hoffman, et al. (2017). Snowball Earth climate dynamics and
Cryogenian geology-geobiology. Science Advances, 3, e1600983.
Hren, M. T., Sheldon, N. D., Grimes, S. T., Collinson, M. E, Hooker,
J. J., Bugler, M., Lohmann, K. C. (2013). Terrestrial cooling in
Northern Europe during the Eocene–Oligocene transition, PNAS,
110, 7562–7567.
Hu, S., & Boos, W. R. (2017). Competing effects of surface Albedo and
Orographic elevated heating on regional climate: Albedo-Elevation
compensation. Geophysical Research Letters, 4(13), 6966–6973.
https://doi.org/10.1002/2016GL072441.
Jaramillo, C. (2018). Evolution of the Isthmus of Panama: Biological,
Paleoceanographic and Paleoclimatological implications. In C.
Hoorn, A. Perrigo, & A. Antonelli (Eds.), Mountains, climate and
biodiversity (1st ed.). Wiley.
Jung, G., Prange, M., & Schulz, M. (2014). Uplift of Africa as a
potential cause for Neogene Intensification of the Benguela
upwelling system. Nature Geoscience, 7(10), 741–747. https://doi.
org/10.1038/ngeo2249.
Kasting, J., & Howard, M. T. (2006). Atmospheric composition and
climate on the early Earth. Philosophical Transactions of the Royal
Society B, 361, 1733–1742.
Kennett, J. P. (1977). Cenozoic evolution of Antarctic Glaciation, the
Circum-Antarctic Ocean, and their impact on global Paleoceanography. Journal of Geophysical Research, 82(27), 3843–3860.
https://doi.org/10.1029/JC082i027p03843.
Kiehl, J. T., & Shields, C. A. (2005). Climate simulation of the latest
Permian: Implications for mass extinction. Geology, 33(9), 757–
760. https://doi.org/10.1130/G21654.1.
Kutzbach, J. E., Prell, W. L., & Ruddiman, W. F. (1993). Sensitivity of
Eurasian climate to surface uplift of the Tibetan Plateau. The
Journal of Geology, 101(2), 177–190. https://doi.org/10.1086/
648215.
Knauth, L. P., & Lowe, D. R. (2003). High Archean climatic
temperature inferred from oxygen isotope geochemistry of cherts
in the 3.5 Ga Swaziland Supergroup, South Africa. Geological
Society of America Bulletin, 115, 566–580 (2003).
22 Climate Evolution on the Geological Timescale and the Role …
267