Husson, L. (2006). Dynamic topography above retreating subduction
zones. Geology, 34(9), 741–744.
Irving, E. (1964). Paleomagnetism and its application to geological
and geophysical problems. Hoboken: Wiley.
Irving, E. (1977). Drift of the major continental blocks since the
Devonian. Nature, 270, 304–309.
Jagoutz, O., Royden, L., Holt, A. F., & Becker, T. W. (2015).
Anomalously fast convergence of India and Eurasia caused by
double subduction. Nature Geoscience, 8, 475–479.
Jakobsson, M., Backman, J., Rudels, B., Nycander, J., Frank, M.,
Mayer, L., et al. (2007). The early Miocene onset of a ventilated
circulation regime in the Arctic Ocean. Nature, 447, 986–990.
Kim, S. T., & O’Neil, J. R. (1997). Equilibrium and nonequilibrium
oxygen isotope effects in synthetic carbonates. Geochimica et
Cosmochimica Acta, 61, 3461–3475.
Kirschvink, J. L., Ripperdan, R. L., & Evans, D. A. (1997). Evidence
for a large-scale reorganization of early cambrian continental
masses by inertial interchange true polar wander. Science, 277
(5325), 541–545.
Le Pichon, X. (1968). Sea-floor spreading and continental drift. Journal
Geophysical Research, 73, 3661–3697.
Li, L., & Garzione, C. (2017). Spatial distribution and controlling
factors of stable isotopes in meteoric waters on the Tibetan Plateau:
Implications for paleoelevation reconstructions. Earth and Planetary Science Letters, 460, 302–314.
Li, Z. X., Bogdanova, S. V., Collins, A. S., Davidson, A., De Waele,
B., Ernst, R. E., et al. (2008). Assembly, configuration, and
break-up history of Rodinia: A synthesis. Precambrian Research,
160, 179–210.
Matte, P. (1986). Tectonics and plate tectonics model for the Variscan
Belt of Europe. Tectonophysics, 126, 329–374.
McElhinny, M. W., Powell, C. M., & Pisarevsky, S. A. (2003).
Paleozoic Terranes of Eastern Australia and the drift history of
Gondwana. Tectonophysics, 362, 41–65.
McKenzie, D., & Sclater, J. G. (1971). The evolution of the Indian
Ocean since the Late Cretaceous. Geophysical Journal International, 24, 437–528.
Meert, J. G., & Santosh, M. (2017). The Columbia supercontinent
revisited. Gondwana Research, 50, 67–83.
Metcalfe, I. (2002). Permian tectonic framework and palaeogeography
of SE Asia. Journal of Asian Earth Sciences, 20, 551–566.
Miller, K. G., Kominz, M. A., Browning, J. V., Wright, J. D.,
Mountain, G. S., Katz, M. E., et al. (2005). The Phanerozoic record
of global sea-level change. Science, 310, 1293–1298.
Moreau, M.-G., Besse, J., Fluteau, F., & Greff-Lefftz, M. (2007). A new
global Paleocene-Eocene apparent polar wandering path loop by
“stacking” magnetostratigraphies: Correlations with high latitude
climatic data. Earth and Planetary Science Letters, 260, 152–165.
Morgan, W. J. (1968). Rises, trenches, great faults and crustal blocks.
Journal Geophysical Research, 73(308), 1959–1982.
Morgan, W. J. (1972). Deep mantle convection plumes and plate
motions. AAPG Bulletin, 56, 203–213.
Mulch, A. (2016). Stable isotope paleoaltimetry and the evolution of
landscapes and life. Earth and Planetary Science Letters, 433, 180–
191. https://doi.org/10.1016/j.epsl.2015.10.034.
Müller, R. D., Seton, M., Zahirovic, S., Williams, S. E., Matthews, K.
J., Wright, N. M., et al. (2016). Ocean basin evolution and
global-scale plate reorganization events since Pangea
breakup. Annual Review of Earth and Planetary Sciences, 44(1),
107–138.
Nance, R. D., Gutierrez-Alonso, G., Duncan Keppie, J., Linnemann,
U., Brendan Murphy, J., Quesada, C., et al. (2012). A brief history
of the Rheic Ocean. Geosciences Frontiers, 3(2), 125–135.
Oriolo, S., Oyhantçabal, P., Wemmer, K., & Siegesmund, S. (2017).
Contemporaneous assembly of Western Gondwana and final
Rodinia break-up: Implications for the supercontinent cycle.
Geoscience Frontiers, 8, 1431–1445.
Otto-Bliesner, B. L., & Upchurch, G. R. Jr. (1997). Vegetation-induced
warming of high-latitude regions during the Late Cretaceous period.
Nature, 385, 804–807.
Otto-Bliesner, B. L., Brady, E. C., & Shields, C. (2002). Late
Cretaceous Ocean: Coupled simulations with the National Center
for Atmospheric Research climate system model. Journal of
Geophysical Research: Atmospheres, 107(D2), ACL 11-1–ACL
11-14.
Peppe, D. J., Royer, D. L., Wilf, P., & Kowalski, E. A. (2010).
Quantification of large uncertainties in fossil leaf paleoaltimetry.
Tectonics, 29(3). https://doi.org/10.1029/2009TC002549.
Pirouz, M., Avouac, J. P., Hassanzadeh, J., Kirschvink, J. L., &
Bahroudi, A. (2017). Early Neogene foreland of the Zagros,
implications for the initial closure of the Neo-Tethys and kinematics
of crustal shortening. Earth and Planetary Science Letters, 477,
168–182.
Poirier, A., & Hillaire-Marcel, C. (2011). Improved Os-isotope
stratigraphy of the Arctic Ocean. Geophysical Research Letters,
38, L14607.
Poulsen, C. J., Ehlers, T. A., & Insel, N. (2010). Onset of convective
rainfall during gradual Late Miocene rise of the Central Andes.
Science, 328, 490–493.
Quade, J., Garzione, C., & Eiler, J. (2007). Paleoelevation reconstruction using pedogenic carbonates. Reviews in Mineralogy and
Geochemistry, 66, 53–87.
Raff, A. D., & Mason, R. G. (1961). Magnetic survey off the west coast
of North America, 40° n. latitude to 52° n. latitude. GSA Bulletin,
72, 1267–1270.
Robert, B., Besse, J., Blein, O., Greff-Lefftz, M., Baudin, T., Lopes, F.,
et al. (2017). Constraints on the Ediacaran inertial interchange true
polar wander hypothesis: A new paleomagnetic study in Morocco
(West African Craton). Precambrian Research, 295, 90–116.
Rogers, J. J. W., & Santosh, M. (2002). Configuration of Columbia, a
Mesoproterozoic supercontinent. Gondwana Research, 5, 5–22.
Romm, J. (1994). A new forerunner for continental drift. Nature
367, 407.
Rowley, D. B., & Garzione, C. N. (2007). Stable isotope-based
paleoaltimetry. Annual Review of Earth and Planetary Sciences, 35,
463–508.
Sarr, A. C., Husson, L., Sepulchre, P., Pastier, A. M., Pedoja, K., Elliot,
M., et al. (2019). Subsiding Sundaland. Geology, 47(2), 119–122.
https://doi.org/10.1130/G45629.1.
Seton, M., Müller, R. D., Zahirovic, S., Gaina, C., Torsvik, T.,
Shephard, G., et al. (2012). Global continental and ocean basin
reconstructions since 200 Ma. Earth Science Reviews, 113,
212–270.
Su, T., Farnsworth, A., Spicer, R. A., Huang, J., Wu, F.-X., Liu, J.,
et al. (2019). No high Tibetan Plateau until the Neogene. Science
Advances, 5(3), eaav2189. https://doi.org/10.1126/sciadv.aav2189.
Tapponnier, P., Zhiqin, X., Roger, F., Meyer, B., Arnaud, N.,
Wittlinger, G., & Jingsui, Y. (2001). Oblique, stepwise rise and
growth of the Tibet Plateau. Science, 294, 1671–1677.
2 The Changing Face of the Earth Throughout the Ages
47
zones. Geology, 34(9), 741–744.
Irving, E. (1964). Paleomagnetism and its application to geological
and geophysical problems. Hoboken: Wiley.
Irving, E. (1977). Drift of the major continental blocks since the
Devonian. Nature, 270, 304–309.
Jagoutz, O., Royden, L., Holt, A. F., & Becker, T. W. (2015).
Anomalously fast convergence of India and Eurasia caused by
double subduction. Nature Geoscience, 8, 475–479.
Jakobsson, M., Backman, J., Rudels, B., Nycander, J., Frank, M.,
Mayer, L., et al. (2007). The early Miocene onset of a ventilated
circulation regime in the Arctic Ocean. Nature, 447, 986–990.
Kim, S. T., & O’Neil, J. R. (1997). Equilibrium and nonequilibrium
oxygen isotope effects in synthetic carbonates. Geochimica et
Cosmochimica Acta, 61, 3461–3475.
Kirschvink, J. L., Ripperdan, R. L., & Evans, D. A. (1997). Evidence
for a large-scale reorganization of early cambrian continental
masses by inertial interchange true polar wander. Science, 277
(5325), 541–545.
Le Pichon, X. (1968). Sea-floor spreading and continental drift. Journal
Geophysical Research, 73, 3661–3697.
Li, L., & Garzione, C. (2017). Spatial distribution and controlling
factors of stable isotopes in meteoric waters on the Tibetan Plateau:
Implications for paleoelevation reconstructions. Earth and Planetary Science Letters, 460, 302–314.
Li, Z. X., Bogdanova, S. V., Collins, A. S., Davidson, A., De Waele,
B., Ernst, R. E., et al. (2008). Assembly, configuration, and
break-up history of Rodinia: A synthesis. Precambrian Research,
160, 179–210.
Matte, P. (1986). Tectonics and plate tectonics model for the Variscan
Belt of Europe. Tectonophysics, 126, 329–374.
McElhinny, M. W., Powell, C. M., & Pisarevsky, S. A. (2003).
Paleozoic Terranes of Eastern Australia and the drift history of
Gondwana. Tectonophysics, 362, 41–65.
McKenzie, D., & Sclater, J. G. (1971). The evolution of the Indian
Ocean since the Late Cretaceous. Geophysical Journal International, 24, 437–528.
Meert, J. G., & Santosh, M. (2017). The Columbia supercontinent
revisited. Gondwana Research, 50, 67–83.
Metcalfe, I. (2002). Permian tectonic framework and palaeogeography
of SE Asia. Journal of Asian Earth Sciences, 20, 551–566.
Miller, K. G., Kominz, M. A., Browning, J. V., Wright, J. D.,
Mountain, G. S., Katz, M. E., et al. (2005). The Phanerozoic record
of global sea-level change. Science, 310, 1293–1298.
Moreau, M.-G., Besse, J., Fluteau, F., & Greff-Lefftz, M. (2007). A new
global Paleocene-Eocene apparent polar wandering path loop by
“stacking” magnetostratigraphies: Correlations with high latitude
climatic data. Earth and Planetary Science Letters, 260, 152–165.
Morgan, W. J. (1968). Rises, trenches, great faults and crustal blocks.
Journal Geophysical Research, 73(308), 1959–1982.
Morgan, W. J. (1972). Deep mantle convection plumes and plate
motions. AAPG Bulletin, 56, 203–213.
Mulch, A. (2016). Stable isotope paleoaltimetry and the evolution of
landscapes and life. Earth and Planetary Science Letters, 433, 180–
191. https://doi.org/10.1016/j.epsl.2015.10.034.
Müller, R. D., Seton, M., Zahirovic, S., Williams, S. E., Matthews, K.
J., Wright, N. M., et al. (2016). Ocean basin evolution and
global-scale plate reorganization events since Pangea
breakup. Annual Review of Earth and Planetary Sciences, 44(1),
107–138.
Nance, R. D., Gutierrez-Alonso, G., Duncan Keppie, J., Linnemann,
U., Brendan Murphy, J., Quesada, C., et al. (2012). A brief history
of the Rheic Ocean. Geosciences Frontiers, 3(2), 125–135.
Oriolo, S., Oyhantçabal, P., Wemmer, K., & Siegesmund, S. (2017).
Contemporaneous assembly of Western Gondwana and final
Rodinia break-up: Implications for the supercontinent cycle.
Geoscience Frontiers, 8, 1431–1445.
Otto-Bliesner, B. L., & Upchurch, G. R. Jr. (1997). Vegetation-induced
warming of high-latitude regions during the Late Cretaceous period.
Nature, 385, 804–807.
Otto-Bliesner, B. L., Brady, E. C., & Shields, C. (2002). Late
Cretaceous Ocean: Coupled simulations with the National Center
for Atmospheric Research climate system model. Journal of
Geophysical Research: Atmospheres, 107(D2), ACL 11-1–ACL
11-14.
Peppe, D. J., Royer, D. L., Wilf, P., & Kowalski, E. A. (2010).
Quantification of large uncertainties in fossil leaf paleoaltimetry.
Tectonics, 29(3). https://doi.org/10.1029/2009TC002549.
Pirouz, M., Avouac, J. P., Hassanzadeh, J., Kirschvink, J. L., &
Bahroudi, A. (2017). Early Neogene foreland of the Zagros,
implications for the initial closure of the Neo-Tethys and kinematics
of crustal shortening. Earth and Planetary Science Letters, 477,
168–182.
Poirier, A., & Hillaire-Marcel, C. (2011). Improved Os-isotope
stratigraphy of the Arctic Ocean. Geophysical Research Letters,
38, L14607.
Poulsen, C. J., Ehlers, T. A., & Insel, N. (2010). Onset of convective
rainfall during gradual Late Miocene rise of the Central Andes.
Science, 328, 490–493.
Quade, J., Garzione, C., & Eiler, J. (2007). Paleoelevation reconstruction using pedogenic carbonates. Reviews in Mineralogy and
Geochemistry, 66, 53–87.
Raff, A. D., & Mason, R. G. (1961). Magnetic survey off the west coast
of North America, 40° n. latitude to 52° n. latitude. GSA Bulletin,
72, 1267–1270.
Robert, B., Besse, J., Blein, O., Greff-Lefftz, M., Baudin, T., Lopes, F.,
et al. (2017). Constraints on the Ediacaran inertial interchange true
polar wander hypothesis: A new paleomagnetic study in Morocco
(West African Craton). Precambrian Research, 295, 90–116.
Rogers, J. J. W., & Santosh, M. (2002). Configuration of Columbia, a
Mesoproterozoic supercontinent. Gondwana Research, 5, 5–22.
Romm, J. (1994). A new forerunner for continental drift. Nature
367, 407.
Rowley, D. B., & Garzione, C. N. (2007). Stable isotope-based
paleoaltimetry. Annual Review of Earth and Planetary Sciences, 35,
463–508.
Sarr, A. C., Husson, L., Sepulchre, P., Pastier, A. M., Pedoja, K., Elliot,
M., et al. (2019). Subsiding Sundaland. Geology, 47(2), 119–122.
https://doi.org/10.1130/G45629.1.
Seton, M., Müller, R. D., Zahirovic, S., Gaina, C., Torsvik, T.,
Shephard, G., et al. (2012). Global continental and ocean basin
reconstructions since 200 Ma. Earth Science Reviews, 113,
212–270.
Su, T., Farnsworth, A., Spicer, R. A., Huang, J., Wu, F.-X., Liu, J.,
et al. (2019). No high Tibetan Plateau until the Neogene. Science
Advances, 5(3), eaav2189. https://doi.org/10.1126/sciadv.aav2189.
Tapponnier, P., Zhiqin, X., Roger, F., Meyer, B., Arnaud, N.,
Wittlinger, G., & Jingsui, Y. (2001). Oblique, stepwise rise and
growth of the Tibet Plateau. Science, 294, 1671–1677.
2 The Changing Face of the Earth Throughout the Ages
47