Loi, A. et al. (2010). The Late Ordovician glacio-eustatic record from a
high-latitude storm-dominated shelf succession: The Bou Ingarf
section (Anti-Atlas, Southern Morocco). Palaeogeography Palaeoclimatology Palaeoecology, 296(3–4), 332–358.
McElwain, J. C., Wade-Murphy, J., Hesselbo, S. P. (2005). Changes in
carbon dioxide during an oceanic anoxic event linked to intrusion
into Gondwana coals. Nature, 435(7041), 479–482.
McInerney, F. A., & Wing, S. L. (2011). The paleocene-eocene thermal
maximum: A perturbation of carbon cycle, climate, and biosphere
with implications for the future. Annual Review of Earth and
Planetary Sciences, 39, 489–516.
Mountanez, I. P., & Poulsen, C. J. (2013). The late paleozoic ice age:
An evolving paradigm. Annual Review of Earth and Planetary
Sciences, 41, 629–656.
Nardin, E., et al. (2011). Modeling the early paleozoic long-term
climatic trend. Geological Society of America Bulletin, 123, 1181–
1192.
Nelsen, M. P. et al. (2016). Delayed fungal evolution did not cause the
Paleozoic peak in coal production. Proceedings of the National
Academy of Science, 113(9), 2442–2447.
Pagani, M., Zachos, J. C., Freeman, K. H., Tipple, B., & Bohaty, S.
(2005). Marked decline in atmospheric carbon dioxide concentrations during the Paleogene. Science, 309, 600–603.
Page, A. A. et al. (2007). Were transgressive black shales a negative
feedback modulating glacioeustasy in the Early Palaeozoic icehouse? In Deep-time perspectives on climate change: marrying the
signal from computer models and biological proxies. pp. 123–156.
Pohl, A. et al. (2016). Glacial onset predated Late Ordovician climate
cooling. Paleoceanography, 31(6), 800–821
Pucéat, E., et al. (2010). Revised phosphate-water fractionation
equation reassessing paleotemperatures derived from biogenic
apatite. Earth and Planetary Science Letters, 298, 135–142.
Pucéat, E. et al. (2003). Thermal evolution of Cretaceous Tethyan
marine waters inferred from oxygen isotope composition of fish
tooth enamels. Paleoceanography, 18,(2), Article Number: 1029.
Rasmussen, C. M. O. et al. (2016). Onset of main Phanerozoic marine
radiation sparked by emerging Mid Ordovician icehouse. Scientific
Reports, 6, Article Number: 18884.
Raymo, M. E. (1991). Geochemical evidence supporting T.C. chamberlin’s theory of glaciation. Geology, 19, 344–347.
Royer, D. L. (2006). CO 2 -forced climate thresholds during the
phanerozoic. Geochimica and Cosmochimica Acta, 70, 5665–5675.
Royer, D. L., Berner, R. A., & Beerling, D. J. (2001). Phanerozoic
atmospheric CO 2 change: Evaluating geochemical and paleobiological approaches. Earth-Science Reviews, 54, 349–392.
Rubinstein, C. V. et al. (2010). Early middle ordovician evidence for
land plants in Argentina (eastern Gondwana). New Phytologist, 188
(2), 365–369.
Scher, H. D., & Martin, E. E. (2006). Timing and climatic
consequences of the opening of drake passage. Science, 312,
428–431.
Scott, A. C., & Glasspool, J. (2006). The diversification of Paleozoic
fire systems and fluctuations in atmospheric oxygen concentration.
Proceedings of the National Academy of Science, 103(29), 10861–
10865.
Shaviv, N. J., & Veizer, J. (2003). Celestial driver of phanerozoic
climate? GSA Today, 13(7), 4–10.
Sluijs, H. et al. (2006). Subtropical arctic ocean temperatures during the
Palaeocene/Eocene thermal maximum. Nature, 441(7093), 610–
613.
Stein, W. E. et al. (2007). Giant cladoxylopsid trees resolve the enigma
of the Earth’s earliest forest stumps at Gilboa. Nature, 446(7138),
904–907.
Thomas, D. J. et al. (1999). New evidence for subtropical warming
during the late Paleocene thermal maximum: stable isotopes from
the Deep Sea Drilling Project Site 527, Walvis Ridge. Paleoceanography, 14, 561–570.
Trotter, J. A. et al. (2008). Did cooling oceans trigger Ordovician
biodiversification? Evidence from conodont thermometry. Science,
321, 550–554
Veizer, J., et al. (1999).
87
Sr/
86
Sr, d
13
C and d
18
O evolution of
phanerozoic seawater. Chemical Geology, 161, 59–88.
Veizer, J., Goddéris, Y., & François, L. M. (2000). Evidence for
decoupling of atmospheric CO 2 and global climate during the
phanerozoic eon. Nature, 408, 698–701.
Zachos, J. C. et al. (2003). A transient rise in tropical sea surface
temperature during the Paleocene-Eocene Thermal Maximum.
Science, 302(5650), 1551–1554.
Zachos, J. C., Dickens, G. R., & et Zeebe, R. E. (2008). An early
Cenozoic perspective on greenhouse warming and carbon-cycle
dynamics. Nature, 451(17). https://doi.org/10.1038/nature.
Zhuravlev, A. Y., & Riding, R., (2001). The ecology of the Cambrian
radiation - Introduction. Perspectives in paleobiology and Earth
history series, pp. 1–7.
27 The Phanerozoic Climate
383
high-latitude storm-dominated shelf succession: The Bou Ingarf
section (Anti-Atlas, Southern Morocco). Palaeogeography Palaeoclimatology Palaeoecology, 296(3–4), 332–358.
McElwain, J. C., Wade-Murphy, J., Hesselbo, S. P. (2005). Changes in
carbon dioxide during an oceanic anoxic event linked to intrusion
into Gondwana coals. Nature, 435(7041), 479–482.
McInerney, F. A., & Wing, S. L. (2011). The paleocene-eocene thermal
maximum: A perturbation of carbon cycle, climate, and biosphere
with implications for the future. Annual Review of Earth and
Planetary Sciences, 39, 489–516.
Mountanez, I. P., & Poulsen, C. J. (2013). The late paleozoic ice age:
An evolving paradigm. Annual Review of Earth and Planetary
Sciences, 41, 629–656.
Nardin, E., et al. (2011). Modeling the early paleozoic long-term
climatic trend. Geological Society of America Bulletin, 123, 1181–
1192.
Nelsen, M. P. et al. (2016). Delayed fungal evolution did not cause the
Paleozoic peak in coal production. Proceedings of the National
Academy of Science, 113(9), 2442–2447.
Pagani, M., Zachos, J. C., Freeman, K. H., Tipple, B., & Bohaty, S.
(2005). Marked decline in atmospheric carbon dioxide concentrations during the Paleogene. Science, 309, 600–603.
Page, A. A. et al. (2007). Were transgressive black shales a negative
feedback modulating glacioeustasy in the Early Palaeozoic icehouse? In Deep-time perspectives on climate change: marrying the
signal from computer models and biological proxies. pp. 123–156.
Pohl, A. et al. (2016). Glacial onset predated Late Ordovician climate
cooling. Paleoceanography, 31(6), 800–821
Pucéat, E., et al. (2010). Revised phosphate-water fractionation
equation reassessing paleotemperatures derived from biogenic
apatite. Earth and Planetary Science Letters, 298, 135–142.
Pucéat, E. et al. (2003). Thermal evolution of Cretaceous Tethyan
marine waters inferred from oxygen isotope composition of fish
tooth enamels. Paleoceanography, 18,(2), Article Number: 1029.
Rasmussen, C. M. O. et al. (2016). Onset of main Phanerozoic marine
radiation sparked by emerging Mid Ordovician icehouse. Scientific
Reports, 6, Article Number: 18884.
Raymo, M. E. (1991). Geochemical evidence supporting T.C. chamberlin’s theory of glaciation. Geology, 19, 344–347.
Royer, D. L. (2006). CO 2 -forced climate thresholds during the
phanerozoic. Geochimica and Cosmochimica Acta, 70, 5665–5675.
Royer, D. L., Berner, R. A., & Beerling, D. J. (2001). Phanerozoic
atmospheric CO 2 change: Evaluating geochemical and paleobiological approaches. Earth-Science Reviews, 54, 349–392.
Rubinstein, C. V. et al. (2010). Early middle ordovician evidence for
land plants in Argentina (eastern Gondwana). New Phytologist, 188
(2), 365–369.
Scher, H. D., & Martin, E. E. (2006). Timing and climatic
consequences of the opening of drake passage. Science, 312,
428–431.
Scott, A. C., & Glasspool, J. (2006). The diversification of Paleozoic
fire systems and fluctuations in atmospheric oxygen concentration.
Proceedings of the National Academy of Science, 103(29), 10861–
10865.
Shaviv, N. J., & Veizer, J. (2003). Celestial driver of phanerozoic
climate? GSA Today, 13(7), 4–10.
Sluijs, H. et al. (2006). Subtropical arctic ocean temperatures during the
Palaeocene/Eocene thermal maximum. Nature, 441(7093), 610–
613.
Stein, W. E. et al. (2007). Giant cladoxylopsid trees resolve the enigma
of the Earth’s earliest forest stumps at Gilboa. Nature, 446(7138),
904–907.
Thomas, D. J. et al. (1999). New evidence for subtropical warming
during the late Paleocene thermal maximum: stable isotopes from
the Deep Sea Drilling Project Site 527, Walvis Ridge. Paleoceanography, 14, 561–570.
Trotter, J. A. et al. (2008). Did cooling oceans trigger Ordovician
biodiversification? Evidence from conodont thermometry. Science,
321, 550–554
Veizer, J., et al. (1999).
87
Sr/
86
Sr, d
13
C and d
18
O evolution of
phanerozoic seawater. Chemical Geology, 161, 59–88.
Veizer, J., Goddéris, Y., & François, L. M. (2000). Evidence for
decoupling of atmospheric CO 2 and global climate during the
phanerozoic eon. Nature, 408, 698–701.
Zachos, J. C. et al. (2003). A transient rise in tropical sea surface
temperature during the Paleocene-Eocene Thermal Maximum.
Science, 302(5650), 1551–1554.
Zachos, J. C., Dickens, G. R., & et Zeebe, R. E. (2008). An early
Cenozoic perspective on greenhouse warming and carbon-cycle
dynamics. Nature, 451(17). https://doi.org/10.1038/nature.
Zhuravlev, A. Y., & Riding, R., (2001). The ecology of the Cambrian
radiation - Introduction. Perspectives in paleobiology and Earth
history series, pp. 1–7.
27 The Phanerozoic Climate
383