Seawater pH and isotopic paleotemperatures of Cretaceous oceans

Palaeogeography, Palaeoclimatology, Palaeoecology

Volumn 170, Issue 1-2, 2001, Pages 49-57

  Zeebe, Richard E ^a,b  

^a ALFRED WEGENER INSTITUTE FOR POLAR AND MARINE RESEARCH   (Germany)

^b Doherty Earth Observatory of Columbia University   (United States)

Author keywords

Cool tropics; Cretaceous; Oxygen isotopes; Paleotemperatures; pH effect; SSTs

Indexed keywords

CRETACEOUS; FORAMINIFERA; OXYGEN ISOTOPE; PALEOCEANOGRAPHY; PALEOTEMPERATURE; PH; SEAWATER;

EID: 0035362612     PISSN: 00310182     EISSN: None     Source Type: Journal    
DOI: 10.1016/S0031-0182(01)00226-7     Document Type: Article

References (42)

1. Global environmental changes preceeding the Cretaceous-Tertiary boundary: Early-Late Maastrichtian transition
2. Evolution of the Cretaceous ocean-climate system
3. Evolution of late Campanian-Maastrichtian marine climates and oceans
4. A warm, equable Cretaceous: The nature of the problem
5. A 'simulation' of mid-Cretaceous climate
6. Reevaluation of the oxygen isotopic composition of planktonic foraminifera: Experimental results and revised paleotemperature equations
7. 2 over Phanerozoic time
8. Reassessing foraminiferal stable isotope geochemistry: Impact of the oceanic carbonate system (experimental results)
9. 2 police the rate of chemical weathering?
10. Carbon dioxide in the atmosphere: Evidence from Cenozoic and mesozoic paleosols
11. 2 changes and tropical sea surface temperatures
12. Comparison of zonal temperature profiles for past warm time periods
13. Late Cretaceous climate and vegetation interactions: Cold continental interior paradox
14. Late Cretaceous oceans and the cool tropic paradox
15. A 400 million year carbon isotope record of pedogenic carbonate: Implications for paleoatmospheric carbon dioxide
16. Estimating the global thermal state from Cretaceous sea surface and continental temperature data
17. 2 levels
18. Palaeoclimate and palaeovegetation in central India during the upper Cretaceous based on stable isotope composition of the palaeosol carbonates
19. Comparison of modern and late Cretaceous meridional energy transport and oceanology
20. Climate: Is the past the key to the future?
21. Middle-Late Cretaceous climate of the southern high-latitudes: Stable isotopic evidence for minimal equator-to-pole thermal gradients: Reply
22. Middle-Late Cretaceous climate of the southern high-latitudes: Stable isotopic evidence for minimal equator-to-pole thermal gradients
23. On the isotopic chemistry of carbonates and a paleotemperature scale
24. Low-latitude sea-surface temperatures for the mid-Cretaceous and the evolution of planktonic foraminifera
25. Low-latitude sea-surface temperatures for the mid-Cretaceous and the evolution of planktonic foraminifera: Reply
26. A reinterpretation of mid-Cretaceous shallow marine temperatures through model-data comparison
27. Low-latitude sea-surface temperatures for the mid-Cretaceous and the evolution of planktonic foraminifera: Comment
28. Middle-Late Cretaceous climate of the southern high-latitudes: Stable isotopic evidence for minimal equator-to-pole thermal gradients: Discussion
29. Isotopic evidence for palaeotemperatures and depth stratification of middle Cretaceous planktonic foraminifera from the Pacific Ocean
30. Cooler estimates of Cretaceous temperatures
31. Paleotemperature history of the Cenozoic and the initiation of Antarctic glaciation: Oxygen and carbon isotope analyses in DSDP sites 277, 279, and 281
32. Effect of seawater carbonate concentration on foraminiferal carbon and oxygen isotopes
33. Deconvolving glacial ocean carbonate chemistry from the planktonic foraminifera carbon isotope record
34. A review of terrestrial and marine climates in the Cretaceous with implications for modeling the greenhouse earth
35. Geologic analogs: Their value and limitations in carbon dioxide research
36. Evidence for extreme climatic warmth from late Cretaceous arctic vertebrates
37. Oxygen isotope exchange between carbonic acid, bicarbonate, carbonate, and water: A re-examination of the data of McCrea (1950) and an expression for the overall partitioning of oxygen isotopes between the carbonate species and water
38. Evolution of early Cenozoic marine temperatures
39. An explanation of the effect of seawater carbonate concentration on foraminiferal oxygen isotopes
40. A diffusion-reaction model of carbon isotope fractionation in foraminifera