Effect of changes in δ18O content of the surface ocean on estimated sea surface temperatures in past warm climate

Paleoceanography

Volumn 21, Issue 2, 2006, Pages

  Roche, D M ^a,b   Donnadieu, Y ^a   Puceat E ^a   Paillard, D ^a  

^a CNRS   (France)

^b VU UNIVERSITY AMSTERDAM   (Netherlands)

Author keywords

[No Author keywords available]

Indexed keywords

OCEANIC CIRCULATION; PALEOCEANOGRAPHY; PALEOTEMPERATURE; SEA SURFACE TEMPERATURE;

EID: 33751260821     PISSN: 08838305     EISSN: None     Source Type: Journal    
DOI: 10.1029/2005PA001220     Document Type: Article

References (34)

1. Barrera, E., and S. Savin (1999), Evolution of late Campanian-Maastrichtian marine climates and oceans, Spec. Pap. Geol. Soc. Am., 332, 245-282.
2. Barrera, E., S. Savin, E. Thomas, and C. Jones (1997), Evidence for thermohaline circulation reversals controlled by sea-level change in the latest Cretaceous, Geology, 25, 715-718.
3. 2 extremes of the Middle Cretaceous (late Albian-Turonian), Paleoceanography, 17(4), 1070, doi:10.1029/2002PA000778.
4. 18O record at Deep Sea Drilling Project Site 511, Paleoceanography, 18(2), 1031, doi:10.1029/2002PA000848.
5. Brass, G., J. Southam, and W. Peterson (1982), Warm saline bottom water in the ancient ocean, Nature, 269, 620-623.
6. Crowley, T., and J. Zachos (2000), Warm Climates in Earth History, pp. 50-76, Cambridge Univ. Press, New York.
7. Delaygue, G., J. Jouzel, and J.-C. Dutay (2000), Oxygen-18 salinity relationship simulated by an oceanic general circulation model, Earth Planet. Sci. Lett., 178, 113-123.
8. Ditchfield, P., J. Marshall, and D. Pirrie (1994), High latitudes paleotemperatures variations: New data from the Tithonian to Eocene of James Ross Island, Palaeogeogr. Palaeoclimatol. Palaeoecol., 107, 70-101.
9. Epstein, S., R. Buchsbaum, H. Lowenstam, and H. Urey (1953), Revised carbonate-water isotopic temperature scale, Geol. Soc. Am. Bull., 64, 1315-1326.
10. Erez, J., and B. Luz (1983), Experimental paleotemperature equation for planktonic foraminifera, Geochim. Cosmochim. Acta, 47, 1025-1031.
11. Frank, T. D., D. Thomas, R. M. Leckie, M. A. Arthur, P. R. Bown, K. Jones, and J. A. Lees (2005), The Maastrichtian record from Shatsky Rise (northwest Pacific): A tropical perspective on global ecological and oceanographic changes, Paleoceanography, 20, PA1008, doi:10.1029/ 2004PA001052.
12. Huber, B., D. Hodell, and C. Hamilton (1995), Middle-Late Cretaceous climate of the southern high latitudes: Stable isotopic evidence for minimal equator-to-pole thermal gradients, Geol. Soc. Am. Bull., 107, 1164-1191.
13. Huber, B. T., R. D. Norris, and K. G. MacLeod (2002), Deep-sea paleotemperature record of extreme warmth during the Cretaceous, Geology, 30, 123-126.
14. Huber, M., and L. C. Sloan (1999), Warm climate transitions: A general circulation modeling study of the late Paleocene thermal maximum (∼56 Ma), J. Geophys. Res., 104, 16,633-16,656.
15. Huber, M., and L. Sloan (2001), Heat transport, deep waters, and thermal gradients: Coupled simulation of an Eocene greenhouse climate, Geophys. Res. Lett., 28, 3481-3484.
16. Jouzel, J., G. Hoffmann, R. Koster, and V. Masson (2000), Water isotopes in precipitation: Data/model comparison for present-day and past climates, Quat. Sci. Rev., 19, 363-379.
17. 4 on early Earth surface temperatures, J. Geophys. Res., 92, 2991-2998.
18. Manabe, S. (1997), Early development in the study of greenhouse warming: The emergence of climate models, Ambio, 26(1), 47-51.
19. Norris, R. D., K. Bice, E. Mango, and P. Wilson (2002), Jiggling the tropical thermostat during the Cenomanian "hothouse", Geology, 30, 299-302.
20. Paren, J., and J. Potter (1984), Isotopic tracers in polar seas and glacier ice, J. Geophys. Res., 89, 749-750.
21. Pearson, P., P. W. Ditchfield, J. Singano, K. G. Harcourt-Brown, C. Nicholas, R. K. Olsson, N. Shackleton, and M. A. Hall (2001), Warm tropical sea surface temperatures in the Late Cretaceous and Eocene epochs, Nature, 413, 481-487.
22. Petoukhov, V., A. Ganopolski, V. Brovkin, M. Claussen, A. Eliseev, C. Kubatzki, and S. Rahmstorf (2000), CLIMBER-2: A climate system model of intermediate complexity. part I: Model description and performance for present climate, Clim. Dyn., 16, 1-17.
23. Pierrehumbert, R. (2002), The hydrologic cycle in deep-time climate problems, Nature, 419, 191-198.
24. Pirrie, D., and J. Marshall (1990), High-paleolatitude Late Cretaceous paleotemperatures: New data from James Ross Island, Antarctica, Geology, 18, 31-34.
25. Pucéat, E., C. Lécuyer, S. M. F. Sheppard, G. Dromart, S. Reboulet, and P. Grandjean (2003), Thermal evolution of Cretaceous Tethyan marine waters inferred from oxygen isotope composition of fish tooth enamels, Paleoceanography, 18(2), 1029, doi:10.1029/2002PA000823.
26. Roche, D., D. Paillard, A. Ganopolski, and G. Hoffmann (2004), Oceanic oxygen-18 at the present day and LGM: Equilibrium simulations with a coupled climate model of intermediate complexity, Earth Planet. Sci. Lett., 218, 317-330.
27. Sellwood, B., G. Price, and P. Valdes (1994), Cooler estimates of Cretaceous temperatures, Nature, 370, 453-455.
28. Shackleton, N. (1974), Attainment of isotopic equilibrium between ocean water and the benthonic foraminifera genus Uvigerina: Isotopic changes in the ocean during the last glacial, in Les méthodes quantitatives d'étude des variations du climat au cours du pléistocène, pp. 203-210, Cent. Natl. de la Rech. Sci., Gifsur-Yvette.
29. Shackleton, N., and J. Kennett (1975), Paleotemperature history of the Cenozoic and the initiation of Antarctic glaciation: Oxygen and carbon isotope analyses in DSDP Sites 277, 279 and 281, Initial Rep. Deep Sea Drill. Proj., 29, 743-755.
30. Sloan, L. C., J. C. G. Walker, and T. C. Moore Jr. (1995), Possible role of oceanic heat transport in early Eocene climate, Paleoceanography, 10, 347-356.
31. Thomas, D. (2004), Evidence for deep-water production in the North Pacific Ocean during the early Cenozoic warm interval, Nature, 430, 65-68.
32. Wilson, P. A., and R. D. Norris (2001), Warm tropical ocean surface and global anoxia during the mid-Cretaceous period, Nature, 412, 425-428.
33. Wilson, P. A., R. D. Norris, and M. J. Cooper (2002), Testing the mid-Cretaceous "greenhouse hypothesis" using Turonian pristine foraminiferal calcite from Demerara Rise, Geology, 30, 607-610.
34. Zachos, J., and L. Stott (1994), Evolution of early cenozoic marine temperatures, Paleoceanography, 9, 353-387.