variations in the Earth’s orbit, the role of which is explained
in Chap. 7.
One of the major challenges for the near future is
understanding the relationship between these climate and
geochemical evolutions on the one hand and biological
evolution on the other.
References
Ahlberg, A., Arndorff, L., & Guy-Ohlson, D. (2002). Onshore climate
change during the Late Triassic marine inundation of the Central
European Basin. Terra Nova, 14(4), 241–248.
Anderson, H. M., Hiller, N., & Gess, R. W. (1995). Archeopteris
(progymnospermopsida) from the Devonian of Southern Africa.
Journal of the Linnean Society, 117(4), 305–320.
Bergmann, K. D. et al. (2018). A 600-million-year carbonate
clumped-isotope record from the Sultanate of Oman. Journal of
Sedimentary Research, 88, 960–979
Berner, R. A. (2004). The phanerozoic carbon cycle (p. 150p). New
York: Oxford University Press.
Bice, K. L., & Norris, R. D. (2002). Possible atmospheric CO 2
extremes of the Middle Cretaceous (late Albian-Turonian). Paleoceanography, 17, 1070.
Boucot, A. J., Xu, C., & Scotese, C. R. (2004). Phanerozoic climatic
zones and paleogeography with a consideration of atmospheric CO 2
level. Paleontological Journal, 38, 115–122.
Breecker, D. O., Sharp, Z. D., & McFadden, L. D. (2010). Atmospheric
CO 2 concentrations during ancient greenhouse climates were
similar to those predicted for AD 2100. Proceedings of the
National Academy of Science, 107, 576–580.
Came, R. E., et al. (2007). Coupling of surface temperatures and
atmospheric CO 2 concentrations during the paleozoic era. Nature,
449, 198–201.
Caputo M. V. et al. (2008). Late devonian and early carboniferous
glacial records of South America. In Resolving the late Paleozoic
ice age in time and space (Vol. 441). Geological Society of
America Special Papers, (pp. 161–173).
Dabard M. P. et al. (2015). Sea-level curve for the Middle to early Late
Ordovician in the Armorican Massif (western France): icehouse
third-order glacio-eustatic cycles.Palaeogeography Palaeoclimatology Palaeoecology, 436, 96–111.
Davies N. S., & Gibling, M. R. (2013). The sedimentary record of
Carboniferous rivers: continuing influence of land plant evolution
on alluvial processes and Palaeozoic ecosystems. Earth-Science
Reviews, 120, 40–79.
DeConto, R. M., & Pollard, D. (2003). Rapid cenozoic glaciation of
antarctica induced by declining atmospheric CO 2 . Nature, 412,
245–248.
Dera, G. et al. (2011). Climatic ups and downs in a disturbed Jurassic
world. Geology, 39(3), 215–218.
Dessert, C., et al. (2001). Erosion of deccan traps determined by river
geochemistry: Impact on the global climate and the
87
Sr/
86
Sr ratio of
seawater. Earth and Planetary Science Letters, 188(3/4), 459–474.
Dickens, G. R. (2003). Rethinking the global carbon cycle with a large,
dynamic and microbially mediated gas hydrate capacitor. Earth and
Planetary Science Letters, 213(3–4), 169–183.
Donnadieu, Y., et al. (2011). A mechanism for brief glacial episodes in
the mesozoic greenhouse. Paleoceanography, 26. https://doi.org/10.
1029/2010pa002100.
Donnadieu, Y., et al. (2006). A GEOCLIM simulation of climatic and
biogeochemical consequences of Pangea breakup. Geochemistry
Geophysics
Geosystems,
7(11).
https://doi.org/10.1029/
2006gc001278.
Dromart, G., et al. (2003). Ice age at the middle-late jurassic transition?
Earth and Planetary Science Letters, 213, 205–220.
Elsworth, G. et al. (2017). Enhanced weathering and CO 2 drawdown
caused by the latest Eocene strengthening of the Atlantic meridional
overturning circulation. Nature Geoscience, 10(3), 213–216.
Finnegan, S., et al. (2011). The magnitude and duration of late
ordovician-early silurian glaciation. Science, 331, 903–906.
Foster, G. L., Royer, D. L., Lunt, D. J. (2017) Future climate forcing
potentially without precedent in the last 420 million years. Nature
Communications. https://doi.org/10.1038/ncomms14845.
Frakes, L. A., Francis, J. E., & Syktus, J. I. (1992). Climate modes of
the phanerozoic. Cambridge: Cambridge University Press.
France-Lanord, C., & Derry, L. A. (1997). Organic carbon burial
forcing of the carbon cycle from Himalaya erosion. Nature, 390,
65–67.
Friedrich, O. et al. (2012). Evolution of middle to Late Cretaceous
oceans - a 55 m.y. record of Earth’s temperature and carbon cycle.
Geology, 40(2), 107–110.
Galy, V., et al. (2007). Efficient organic carbon burial in the Bengal fan
sustained by the Himalayan erosional system. Nature, 450, 407–
410.
Ghosh, P., Garzione, C. N., & Eiler, J. M. (2006). Rapid uplift of the
Altiplano revealed through C-13-O-18 bonds in paleosol carbonates. Science, 311(5760), 511–515.
Goddéris, Y., et al. (2008). Causal of casual link between the rise of
nannoplankton calcification and a tectonically-driven massive
decrease in the Late Triassic Atmospheric CO 2 ? Earth and
Planetary Science Letters, 267, 247–255.
Goddéris, Y., & François, L. M. (1996). Balancing the cenozoic Carbon
and Alkalinity Cycles: Constraints from isotopic records. Geophysical research letters, 23(25), 3743–3746.
Goddéris, Y. et al. (2014). The role of palaeogeography in the
Phanerozoic history of atmospheric CO 2 and climate. Earth-Science
Reviews, 128, 122–138.
Goddéris, Y. et al. (2017). Onset and ending of the late Palaeozoic ice
age triggered by tectonically paced rock weathering. Nature
Geoscience, 10(5), 382–385.
Hayes, J. M., Strauss, H., & Kaufman, A. J. (1999). The abundance of
13
C in marine organic matter and isotopic fractionation in the global
biogeochemical cycle of carbon during the past 800 Ma. Chemical
Geology, 161, 103–125.
Hodel, F. et al. (2018). Fossil black smoker yields oxygen isotopic
composition of Neoproterozoic seawater. Nature Communications,
9, Article Number: 1453.
Huber, M., & Nof, D. (2006). The ocean circulation in the Southern
Hemisphere and its climatic impacts in the eocene. Palaeogeography, Palaeoclimatology, Palaeoecology, 231, 9–28.
Joachimski, M. M. et al. (2004). Oxygen isotope evolution of biogenic
calcite and apatite during the Middle and Late Devonian. International Journal of Earth Sciences,93(4): 542–553.
Katz, M. E. et al. (2005). Biological overprint of the geological carbon
cycle. Marine Geology, 217, 323–338.
Kump, L. R., et al. (1999). A weathering hypothesis for glaciation at
high atmospheric pCO 2 during the late ordovician. Palaeogeography, Palaeoclimatology, Palaeoecology, 152, 173–187.
Le Hir, et al. (2011). The climate change caused by the land plant
invasion in the Devonian. Earth and Planetary Science Letters, 310
(3–4), 203–212.
Lefebvre, V. et al. (2013). Was the Antarctic glaciation delayed by a
high degassing rate during the Early Cenozoic? Earth and
Planetary Science Letters, 371–372, 203–211.
Lenton, T. M. et al. (2012). First plants cooled the Ordovician. Nature
Geoscience, 5, 86–89.
382
Y. Goddéris et al.
in Chap. 7.
One of the major challenges for the near future is
understanding the relationship between these climate and
geochemical evolutions on the one hand and biological
evolution on the other.
References
Ahlberg, A., Arndorff, L., & Guy-Ohlson, D. (2002). Onshore climate
change during the Late Triassic marine inundation of the Central
European Basin. Terra Nova, 14(4), 241–248.
Anderson, H. M., Hiller, N., & Gess, R. W. (1995). Archeopteris
(progymnospermopsida) from the Devonian of Southern Africa.
Journal of the Linnean Society, 117(4), 305–320.
Bergmann, K. D. et al. (2018). A 600-million-year carbonate
clumped-isotope record from the Sultanate of Oman. Journal of
Sedimentary Research, 88, 960–979
Berner, R. A. (2004). The phanerozoic carbon cycle (p. 150p). New
York: Oxford University Press.
Bice, K. L., & Norris, R. D. (2002). Possible atmospheric CO 2
extremes of the Middle Cretaceous (late Albian-Turonian). Paleoceanography, 17, 1070.
Boucot, A. J., Xu, C., & Scotese, C. R. (2004). Phanerozoic climatic
zones and paleogeography with a consideration of atmospheric CO 2
level. Paleontological Journal, 38, 115–122.
Breecker, D. O., Sharp, Z. D., & McFadden, L. D. (2010). Atmospheric
CO 2 concentrations during ancient greenhouse climates were
similar to those predicted for AD 2100. Proceedings of the
National Academy of Science, 107, 576–580.
Came, R. E., et al. (2007). Coupling of surface temperatures and
atmospheric CO 2 concentrations during the paleozoic era. Nature,
449, 198–201.
Caputo M. V. et al. (2008). Late devonian and early carboniferous
glacial records of South America. In Resolving the late Paleozoic
ice age in time and space (Vol. 441). Geological Society of
America Special Papers, (pp. 161–173).
Dabard M. P. et al. (2015). Sea-level curve for the Middle to early Late
Ordovician in the Armorican Massif (western France): icehouse
third-order glacio-eustatic cycles.Palaeogeography Palaeoclimatology Palaeoecology, 436, 96–111.
Davies N. S., & Gibling, M. R. (2013). The sedimentary record of
Carboniferous rivers: continuing influence of land plant evolution
on alluvial processes and Palaeozoic ecosystems. Earth-Science
Reviews, 120, 40–79.
DeConto, R. M., & Pollard, D. (2003). Rapid cenozoic glaciation of
antarctica induced by declining atmospheric CO 2 . Nature, 412,
245–248.
Dera, G. et al. (2011). Climatic ups and downs in a disturbed Jurassic
world. Geology, 39(3), 215–218.
Dessert, C., et al. (2001). Erosion of deccan traps determined by river
geochemistry: Impact on the global climate and the
87
Sr/
86
Sr ratio of
seawater. Earth and Planetary Science Letters, 188(3/4), 459–474.
Dickens, G. R. (2003). Rethinking the global carbon cycle with a large,
dynamic and microbially mediated gas hydrate capacitor. Earth and
Planetary Science Letters, 213(3–4), 169–183.
Donnadieu, Y., et al. (2011). A mechanism for brief glacial episodes in
the mesozoic greenhouse. Paleoceanography, 26. https://doi.org/10.
1029/2010pa002100.
Donnadieu, Y., et al. (2006). A GEOCLIM simulation of climatic and
biogeochemical consequences of Pangea breakup. Geochemistry
Geophysics
Geosystems,
7(11).
https://doi.org/10.1029/
2006gc001278.
Dromart, G., et al. (2003). Ice age at the middle-late jurassic transition?
Earth and Planetary Science Letters, 213, 205–220.
Elsworth, G. et al. (2017). Enhanced weathering and CO 2 drawdown
caused by the latest Eocene strengthening of the Atlantic meridional
overturning circulation. Nature Geoscience, 10(3), 213–216.
Finnegan, S., et al. (2011). The magnitude and duration of late
ordovician-early silurian glaciation. Science, 331, 903–906.
Foster, G. L., Royer, D. L., Lunt, D. J. (2017) Future climate forcing
potentially without precedent in the last 420 million years. Nature
Communications. https://doi.org/10.1038/ncomms14845.
Frakes, L. A., Francis, J. E., & Syktus, J. I. (1992). Climate modes of
the phanerozoic. Cambridge: Cambridge University Press.
France-Lanord, C., & Derry, L. A. (1997). Organic carbon burial
forcing of the carbon cycle from Himalaya erosion. Nature, 390,
65–67.
Friedrich, O. et al. (2012). Evolution of middle to Late Cretaceous
oceans - a 55 m.y. record of Earth’s temperature and carbon cycle.
Geology, 40(2), 107–110.
Galy, V., et al. (2007). Efficient organic carbon burial in the Bengal fan
sustained by the Himalayan erosional system. Nature, 450, 407–
410.
Ghosh, P., Garzione, C. N., & Eiler, J. M. (2006). Rapid uplift of the
Altiplano revealed through C-13-O-18 bonds in paleosol carbonates. Science, 311(5760), 511–515.
Goddéris, Y., et al. (2008). Causal of casual link between the rise of
nannoplankton calcification and a tectonically-driven massive
decrease in the Late Triassic Atmospheric CO 2 ? Earth and
Planetary Science Letters, 267, 247–255.
Goddéris, Y., & François, L. M. (1996). Balancing the cenozoic Carbon
and Alkalinity Cycles: Constraints from isotopic records. Geophysical research letters, 23(25), 3743–3746.
Goddéris, Y. et al. (2014). The role of palaeogeography in the
Phanerozoic history of atmospheric CO 2 and climate. Earth-Science
Reviews, 128, 122–138.
Goddéris, Y. et al. (2017). Onset and ending of the late Palaeozoic ice
age triggered by tectonically paced rock weathering. Nature
Geoscience, 10(5), 382–385.
Hayes, J. M., Strauss, H., & Kaufman, A. J. (1999). The abundance of
13
C in marine organic matter and isotopic fractionation in the global
biogeochemical cycle of carbon during the past 800 Ma. Chemical
Geology, 161, 103–125.
Hodel, F. et al. (2018). Fossil black smoker yields oxygen isotopic
composition of Neoproterozoic seawater. Nature Communications,
9, Article Number: 1453.
Huber, M., & Nof, D. (2006). The ocean circulation in the Southern
Hemisphere and its climatic impacts in the eocene. Palaeogeography, Palaeoclimatology, Palaeoecology, 231, 9–28.
Joachimski, M. M. et al. (2004). Oxygen isotope evolution of biogenic
calcite and apatite during the Middle and Late Devonian. International Journal of Earth Sciences,93(4): 542–553.
Katz, M. E. et al. (2005). Biological overprint of the geological carbon
cycle. Marine Geology, 217, 323–338.
Kump, L. R., et al. (1999). A weathering hypothesis for glaciation at
high atmospheric pCO 2 during the late ordovician. Palaeogeography, Palaeoclimatology, Palaeoecology, 152, 173–187.
Le Hir, et al. (2011). The climate change caused by the land plant
invasion in the Devonian. Earth and Planetary Science Letters, 310
(3–4), 203–212.
Lefebvre, V. et al. (2013). Was the Antarctic glaciation delayed by a
high degassing rate during the Early Cenozoic? Earth and
Planetary Science Letters, 371–372, 203–211.
Lenton, T. M. et al. (2012). First plants cooled the Ordovician. Nature
Geoscience, 5, 86–89.
382
Y. Goddéris et al.