Ladant, J. B., Donnadieu, Y. (2016). Palaeogeographic regulation of
glacial events during the Cretaceous supergreenhous. Nature
communications, 7, Article number: 12771.
Lefebvre, V., Donnadieu, Y., Sepulchre, P., Swingedouw, D., &
Zhang, Z.-S. (2012). Deciphering the role of Southern Gateways
and carbon dioxide on the onset of the Antarctic circumpolar
current. Paleoceanography, 27(4), n/a–n/a. https://doi.org/10.1029/
2012PA002345.
Le Hir, G., Donnadieu, Y., Goddéris, Y., Meyer-Berthaud, B.,
Ramstein, G., & Blakey, R. C. (2011). The climate change caused
by the land plant invasion in the Devonian. Earth and Planetary
Science Letters, 310(3), 203–212. https://doi.org/10.1016/j.epsl.
2011.08.042.
Lowe, D. R., & Tice, M. M. (2004). Geologic evidence for Archean
atmospheric and climatic evolution: Fluctuating levels of CO 2 , CH 4 ,
and O 2 with an overriding tectonic control. Geology, 32, 493–496.
Lunt, D. J., et al. (2008). Closure of the Panama Seaway during the
Pliocene: Implications for climate and Northern Hemisphere
Glaciation. Climate Dynamics, 3, 1–18.
Maffre, P., Ladant, J. B., Donnadieu, Y., Sepulchre, P., & Goddéris, Y.
(2018). The influence of Orography on modern ocean circulation.
Climate Dynamics, 50(3–4), 1277–1289. https://doi.org/10.1007/
s00382-017-3683-0.
Matte, P. (1986). Tectonics and plate Tectonics model for the Variscan
Belt of Europe. Tectonophysics, 126, 329–374.
Meyer-Berthaud, B., Scheckler, S., Wendt, J. (1999). Archaeopteris is
the earliest known modern tree. Nature, 398, 700–701.
Molnar, P., Boos, W. R., & Battisti, D. S. (2010). Orographic controls on
climate and Paleoclimate of Asia: Thermal and mechanical roles for the
Tibetan Plateau. Annual Review of Earth and Planetary Sciences, 38
(1), 77–102. https://doi.org/10.1146/annurev-earth-040809-152456.
Montañez, I., & Poulsen, C. (2013). The late Paleozoic ice age: An
evolving paradigm. Annual Review of Earth and Planetary
Sciences, 41, 24.1–24.28.
Montañez, I. P., McElwain, J. C., Poulsen, C. J., White, J. D.,
DiMichele, W. A., Wilson, J. P., Griggs, G., & Hren, M. T. (2016).
Climate, pCO 2 and terrestrial carbon cycle linkages during late
Palaeozoic glacial–interglacial cycles. Nature Geoscience, 9(11),
824–828. https://doi.org/10.1038/ngeo2822.
Montes, C., Cardona, A., Jaramillo, C., Pardo, A., Silva, J. C.,
Valencia, V., et al. (2015). Middle Miocene closure of the Central
American Seaway. Science, 348(6231), 226–229. https://doi.org/10.
1126/science.aaa2815.
Murphy, D. P., & Thomas, D. J. (2013). The evolution of late
Cretaceous deep-ocean circulation in the Atlantic Basins: Neodymium isotope evidence from South Atlantic Drill Sites for Tectonic
controls: Cretaceous Atlantic deep circulation. Geochemistry,
Geophysics, Geosystems, 14(12), 5323–5340. https://doi.org/10.
1002/2013GC004889.
O’Dea, A., Lessios, H. A., Coates, A. G., Eytan, R. I.,
Restrepo-Moreno, S. A., Cione, A. L., et al. (2016). Formation of
the Isthmus of Panama. Science Advances, 2(8), e1600883. https://
doi.org/10.1126/sciadv.1600883.
Potter, S. F., Dawson, E. J., & Frierson, D. M. W. (2017). Southern
African Orography impacts on low clouds and the Atlantic ITCZ in
a coupled model: African Orography impacts on the ITCZ.
Geophysical Research Letters, 44(7), 3283–389. https://doi.org/
10.1002/2017GL073098.
Poulsen, C. J., Ehlers, T. A., & Insel, N. (2010). Onset of convective
rainfall during gradual late Miocene rise of the Central Andes.
Science, 328(5977): 490–493. https://doi.org/10.1126/science.
1185078.
Poulsen, C. J., Gendaszek, A. S., & Jacob, R. L. (2003). Did the rifting
of the Atlantic Ocean Cause the Cretaceous thermal maximum?
Geology, 31(2), 115–118. https://doi.org/10.1130/0091-7613(2003)
031%3c0115:DTROTA%3e2.0.CO;2.
Ramstein, G., Fluteau, F., Besse, J., Joussaume, S. (1997). Effects of
orogeny, sea-level change and tectonic drift on the monsoon over
the past 30 millions years. Nature, 386, 788–795.
Rind, D. G., Russell, G., & Ruddiman, W. F. (1997). The effects of
uplift on ocean‐atmosphere circulation. In W. F. Ruddiman (Ed.),
Tectonic uplift and climate change (pp. 123–147). New York:
Plenum.
Robert, F., & Chaussidon, M. (2006). A palaeotemperature curve for
the Precambrian oceans based on silicon isotopes in cherts. Nature,
443, 969–972.
Ruddiman, W. F., et al. (1997). The uplift-climate connection: A
synthesis. In W. F. Ruddiman (Ed.), Tectonic uplift and climate
change (pp. 471–515). New York: Plenum.
Sepulchre, P., Arsouze, T., Donnadieu, Y., Dutay, J-C., et al. (2014).
Consequences of shoaling of the Central American Seaway
determined from modeling Nd isotopes. Paleoceanography, 29(3),
176–189.
Sepulchre, P., Ramstein, G., Fluteau, F., Schuster, M., Tiercelin, J. J., &
Brunet, M. (2006). Tectonic Uplift and Eastern Africa Aridification.
Science, 313(5792), 1419–1423. https://doi.org/10.1126/science.
1129158.
Sepulchre, P., Sloan, L. C., Snyder, M., & Fiechter, J. (2009). Impacts
of Andean Uplift on the Humboldt current system: A climate model
sensitivity study. Paleoceanography, 24(4). https://doi.org/10.1029/
2008PA001668.
Shields, C. A., & Kiehl, J. T. (2018). Monsoonal precipitation in the
Paleo-Tethys warm pool during the latest Permian. Palaeogeography, Palaeoclimatology, Palaeoecology, 491(février), 123–136.
https://doi.org/10.1016/j.palaeo.2017.12.001.
Sijp, W. P., von der Heydt, A. S. Dijkstra, H. A. Flögel, S., Douglas,
P. M. J., & Bijl. P. K. (2014). The role of ocean gateways on
cooling climate on long time scales. Global and Planetary Change,
119(août), 1–22. https://doi.org/10.1016/j.gloplacha.2014.04.004.
Su, B., Jiang, D., Zhang, R., Sepulchre, P., & Ramstein, G. (2018).
Difference between the North Atlantic and Pacific Meridional
overturning circulation in response to the uplift of the Tibetan
Plateau. Climate of the Past, 14(6), 751–762. https://doi.org/10.
5194/cp-14-751-2018.
Tan, N., Ramstein, G., Dumas, C., Contoux, C., Ladant, J. B.,
Sepulchre, P., Zhang, Z., & De Schepper, S. (2017). Exploring the
MIS M2 glaciation occurring during a warm and high atmospheric
CO 2 Pliocene background climate. Earth and Planetary Science
Letters, 472, 266–276.
Tartèse, R., Chaussidon, M., Gurenko, A., Delarue, F., & Robert, F.
(2017). Warm Archaean Oceans reconstructed from oxygen isotope
composition of early-life Remnants. Geochemical Perspectives
Letters, 55–65. https://doi.org/10.7185/geochemlet.1706.
Valley, J. W. (2006). Early Earth. Elements 2(4), 201–204. https://doiorg.insu.bib.cnrs.fr/10.2113/gselements.2.4.201.
Veizer, J., & Prokoph, (2015). Temperatures and oxygen isotopic
composition of Phanerozoic oceans. Earth-Science Reviews, 146,
92–104. https://doi.org/10.1016/j.earscirev.2015.03.008.
Warner, T. (2004). Desert Meteorology. Cambridge: Cambridge
University Press. https://doi.org/10.1017/CBO9780511535789.
Young, G. M., Von Brunn, V., Gold, D. J. C., & Minter, W. E. L.
(1998). Earth’s oldest reported Glaciation: Physical and chemical
evidence from the Archean Mozaan Group (2.9 Ga) of South
Africa. Journal of Geology, 106, 523–538.
Zachos, J., et al. (2001). Trends, rhythms, and aberrations in global
climate 65 Ma to present. Science, 292, 686–693.
Zerkle, A. L., Claire, M. W., Domagal-Goldman, S. D., Farquhar J., &
Poulton, S. W. (2012). A bistable organic-rich atmosphere on the
268
F. Fluteau and P. Sepulchre
glacial events during the Cretaceous supergreenhous. Nature
communications, 7, Article number: 12771.
Lefebvre, V., Donnadieu, Y., Sepulchre, P., Swingedouw, D., &
Zhang, Z.-S. (2012). Deciphering the role of Southern Gateways
and carbon dioxide on the onset of the Antarctic circumpolar
current. Paleoceanography, 27(4), n/a–n/a. https://doi.org/10.1029/
2012PA002345.
Le Hir, G., Donnadieu, Y., Goddéris, Y., Meyer-Berthaud, B.,
Ramstein, G., & Blakey, R. C. (2011). The climate change caused
by the land plant invasion in the Devonian. Earth and Planetary
Science Letters, 310(3), 203–212. https://doi.org/10.1016/j.epsl.
2011.08.042.
Lowe, D. R., & Tice, M. M. (2004). Geologic evidence for Archean
atmospheric and climatic evolution: Fluctuating levels of CO 2 , CH 4 ,
and O 2 with an overriding tectonic control. Geology, 32, 493–496.
Lunt, D. J., et al. (2008). Closure of the Panama Seaway during the
Pliocene: Implications for climate and Northern Hemisphere
Glaciation. Climate Dynamics, 3, 1–18.
Maffre, P., Ladant, J. B., Donnadieu, Y., Sepulchre, P., & Goddéris, Y.
(2018). The influence of Orography on modern ocean circulation.
Climate Dynamics, 50(3–4), 1277–1289. https://doi.org/10.1007/
s00382-017-3683-0.
Matte, P. (1986). Tectonics and plate Tectonics model for the Variscan
Belt of Europe. Tectonophysics, 126, 329–374.
Meyer-Berthaud, B., Scheckler, S., Wendt, J. (1999). Archaeopteris is
the earliest known modern tree. Nature, 398, 700–701.
Molnar, P., Boos, W. R., & Battisti, D. S. (2010). Orographic controls on
climate and Paleoclimate of Asia: Thermal and mechanical roles for the
Tibetan Plateau. Annual Review of Earth and Planetary Sciences, 38
(1), 77–102. https://doi.org/10.1146/annurev-earth-040809-152456.
Montañez, I., & Poulsen, C. (2013). The late Paleozoic ice age: An
evolving paradigm. Annual Review of Earth and Planetary
Sciences, 41, 24.1–24.28.
Montañez, I. P., McElwain, J. C., Poulsen, C. J., White, J. D.,
DiMichele, W. A., Wilson, J. P., Griggs, G., & Hren, M. T. (2016).
Climate, pCO 2 and terrestrial carbon cycle linkages during late
Palaeozoic glacial–interglacial cycles. Nature Geoscience, 9(11),
824–828. https://doi.org/10.1038/ngeo2822.
Montes, C., Cardona, A., Jaramillo, C., Pardo, A., Silva, J. C.,
Valencia, V., et al. (2015). Middle Miocene closure of the Central
American Seaway. Science, 348(6231), 226–229. https://doi.org/10.
1126/science.aaa2815.
Murphy, D. P., & Thomas, D. J. (2013). The evolution of late
Cretaceous deep-ocean circulation in the Atlantic Basins: Neodymium isotope evidence from South Atlantic Drill Sites for Tectonic
controls: Cretaceous Atlantic deep circulation. Geochemistry,
Geophysics, Geosystems, 14(12), 5323–5340. https://doi.org/10.
1002/2013GC004889.
O’Dea, A., Lessios, H. A., Coates, A. G., Eytan, R. I.,
Restrepo-Moreno, S. A., Cione, A. L., et al. (2016). Formation of
the Isthmus of Panama. Science Advances, 2(8), e1600883. https://
doi.org/10.1126/sciadv.1600883.
Potter, S. F., Dawson, E. J., & Frierson, D. M. W. (2017). Southern
African Orography impacts on low clouds and the Atlantic ITCZ in
a coupled model: African Orography impacts on the ITCZ.
Geophysical Research Letters, 44(7), 3283–389. https://doi.org/
10.1002/2017GL073098.
Poulsen, C. J., Ehlers, T. A., & Insel, N. (2010). Onset of convective
rainfall during gradual late Miocene rise of the Central Andes.
Science, 328(5977): 490–493. https://doi.org/10.1126/science.
1185078.
Poulsen, C. J., Gendaszek, A. S., & Jacob, R. L. (2003). Did the rifting
of the Atlantic Ocean Cause the Cretaceous thermal maximum?
Geology, 31(2), 115–118. https://doi.org/10.1130/0091-7613(2003)
031%3c0115:DTROTA%3e2.0.CO;2.
Ramstein, G., Fluteau, F., Besse, J., Joussaume, S. (1997). Effects of
orogeny, sea-level change and tectonic drift on the monsoon over
the past 30 millions years. Nature, 386, 788–795.
Rind, D. G., Russell, G., & Ruddiman, W. F. (1997). The effects of
uplift on ocean‐atmosphere circulation. In W. F. Ruddiman (Ed.),
Tectonic uplift and climate change (pp. 123–147). New York:
Plenum.
Robert, F., & Chaussidon, M. (2006). A palaeotemperature curve for
the Precambrian oceans based on silicon isotopes in cherts. Nature,
443, 969–972.
Ruddiman, W. F., et al. (1997). The uplift-climate connection: A
synthesis. In W. F. Ruddiman (Ed.), Tectonic uplift and climate
change (pp. 471–515). New York: Plenum.
Sepulchre, P., Arsouze, T., Donnadieu, Y., Dutay, J-C., et al. (2014).
Consequences of shoaling of the Central American Seaway
determined from modeling Nd isotopes. Paleoceanography, 29(3),
176–189.
Sepulchre, P., Ramstein, G., Fluteau, F., Schuster, M., Tiercelin, J. J., &
Brunet, M. (2006). Tectonic Uplift and Eastern Africa Aridification.
Science, 313(5792), 1419–1423. https://doi.org/10.1126/science.
1129158.
Sepulchre, P., Sloan, L. C., Snyder, M., & Fiechter, J. (2009). Impacts
of Andean Uplift on the Humboldt current system: A climate model
sensitivity study. Paleoceanography, 24(4). https://doi.org/10.1029/
2008PA001668.
Shields, C. A., & Kiehl, J. T. (2018). Monsoonal precipitation in the
Paleo-Tethys warm pool during the latest Permian. Palaeogeography, Palaeoclimatology, Palaeoecology, 491(février), 123–136.
https://doi.org/10.1016/j.palaeo.2017.12.001.
Sijp, W. P., von der Heydt, A. S. Dijkstra, H. A. Flögel, S., Douglas,
P. M. J., & Bijl. P. K. (2014). The role of ocean gateways on
cooling climate on long time scales. Global and Planetary Change,
119(août), 1–22. https://doi.org/10.1016/j.gloplacha.2014.04.004.
Su, B., Jiang, D., Zhang, R., Sepulchre, P., & Ramstein, G. (2018).
Difference between the North Atlantic and Pacific Meridional
overturning circulation in response to the uplift of the Tibetan
Plateau. Climate of the Past, 14(6), 751–762. https://doi.org/10.
5194/cp-14-751-2018.
Tan, N., Ramstein, G., Dumas, C., Contoux, C., Ladant, J. B.,
Sepulchre, P., Zhang, Z., & De Schepper, S. (2017). Exploring the
MIS M2 glaciation occurring during a warm and high atmospheric
CO 2 Pliocene background climate. Earth and Planetary Science
Letters, 472, 266–276.
Tartèse, R., Chaussidon, M., Gurenko, A., Delarue, F., & Robert, F.
(2017). Warm Archaean Oceans reconstructed from oxygen isotope
composition of early-life Remnants. Geochemical Perspectives
Letters, 55–65. https://doi.org/10.7185/geochemlet.1706.
Valley, J. W. (2006). Early Earth. Elements 2(4), 201–204. https://doiorg.insu.bib.cnrs.fr/10.2113/gselements.2.4.201.
Veizer, J., & Prokoph, (2015). Temperatures and oxygen isotopic
composition of Phanerozoic oceans. Earth-Science Reviews, 146,
92–104. https://doi.org/10.1016/j.earscirev.2015.03.008.
Warner, T. (2004). Desert Meteorology. Cambridge: Cambridge
University Press. https://doi.org/10.1017/CBO9780511535789.
Young, G. M., Von Brunn, V., Gold, D. J. C., & Minter, W. E. L.
(1998). Earth’s oldest reported Glaciation: Physical and chemical
evidence from the Archean Mozaan Group (2.9 Ga) of South
Africa. Journal of Geology, 106, 523–538.
Zachos, J., et al. (2001). Trends, rhythms, and aberrations in global
climate 65 Ma to present. Science, 292, 686–693.
Zerkle, A. L., Claire, M. W., Domagal-Goldman, S. D., Farquhar J., &
Poulton, S. W. (2012). A bistable organic-rich atmosphere on the
268
F. Fluteau and P. Sepulchre