Carbonate fluxes and calcareous nannoplankton

  • William W. Hay


Coccolithophores first became significant participants in the carbonate cycle in the Jurassic, but throughout the Jurassic they were largely restricted to shelf and epeiric sea environments. They spread into the open ocean in the Cretaceous, and with this became a major factor in governing the carbonate cycle in the sea. With the development of dissolution-resistant forms, such as Watznaueria barnesae, the coccolithophores perturbed the carbonate system and switched the major site of carbonate deposition from shallow seas to the deep ocean. Several major evolutionary steps in the development of the coccolithophores have forced further changes in the carbon cycle, favoring the deep sea as a site of carbonate deposition. Samples of recent coccolith assemblages from bottom sediments differ from those of living coccolithophores in surface waters. Many of the coccoliths of more delicate species, particularly holococcoliths, are dissolved in the water column or at the sediment surface and are only rarely preserved as fossils. They, along with the pteropods, form an important part of the shallow carbonate cycle. There appears to be a continuous gradation in the level of susceptibility of coccoliths to dissolution, from forms that dissolve in the near-saturated waters of the surface ocean to those that are among the most dissolution-resistant forms of calcite. This continuous dissolution spectrum is in contrast to the planktic foraminifera, in which dissolution of the tests also occurs in a sequence, but through a much more restricted depth range, the lysocline. Whereas the order of dissolution of planktic foraminifera follows their habitat, with warm-water species being most susceptible and cold-water forms most resistant to dissolution, the order of dissolution of coccoliths appears to be related to phylogeny. The steepness of the coccolith carbonate dissolution gradient appears to have changed over time. In the Oligocene almost pure nannofossil carbonate oozes devoid of terrigenous material were widespread, perhaps reflecting unusual climatic conditions on land. The overall effect of coccolithophore evolution has been to move carbonate deposition to the deep sea, where coccolith oozes accumulate on ocean crust and will ultimately be subducted. Only a fraction of the carbon in the subducted carbonate is returned to the surface through volcanic activity. If their activity were to continue for several hundreds of millions of years the coccolithophores would remove much of the carbon from the surface of the Earth to be emplaced in the mantle.


Carbonate Flux Continental Block Accommodation Space Calcareous Nannofossil Planktic Foraminifera 
These keywords were added by machine and not by the authors. This process is experimental and the keywords may be updated as the learning algorithm improves.


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  1. Alt JC, Teagle DAH (1999) The uptake of carbon during alteration of oceanic crust. Geochim Cosmochim Ac 63: 1527–1536CrossRefGoogle Scholar
  2. Berger WH (1967) Foraminiferal ooze: solution at depth. Science 156: 383–385CrossRefGoogle Scholar
  3. Berger WH (1968) Planktic foraminifera: selective solution and paleoclimatic interpretation. Deep-Sea Res 15: 31–43Google Scholar
  4. Berger WH (1970) Planktic foraminifera: selective solution and the lysocline. Mar Geol 8: 111–138CrossRefGoogle Scholar
  5. Berger WH, Winterer EL (1974) Plate stratigraphy and the fluctuating carbonate line. In: Hsü KJ, Jenkyns H (eds) Pelagic sediments on land and under the sea. Special Publication of the International Association of Sedimentologists 1: 11–48Google Scholar
  6. Berner RA (1991) A model for atmospheric CO2 over Phanerozoic time. Am J Sci 291: 339–376CrossRefGoogle Scholar
  7. Berner RA (1994) GEOCARB II: A revised model of atmospheric CO2 over Phanerozoic time. Am J Sci 294: 56–91CrossRefGoogle Scholar
  8. Berner RA (1997) The rise of plants and their effect on weathering and atmospheric CO2. Science 276: 544–546CrossRefGoogle Scholar
  9. Berner RA, Kothavala Z (2001) GEOCARB III: A revised model of atmospheric CO2 over Phanerozoic time. Am J Sci 301: 182–204CrossRefGoogle Scholar
  10. Berner RA, Lasaga AC, Garrrels RM (1983) The carbonate-silicate geochemical cycle and its effect on atmospheric carbon dioxide over the 100 million years. Am J Sci 283: 641–683CrossRefGoogle Scholar
  11. Berry JP, Wilkinson BH (1994) Paleoclimatic and tectonic control on the accumulation of North American cratonic sediment. Geol Soc Am Bull 106: 855–865CrossRefGoogle Scholar
  12. Budyko MI, Ronov AB (1979) Chemical evolution of the atmosphere in the Phanerozoic. Geochem Int 15: 1–9Google Scholar
  13. Budyko MI, Ronov AB, Yanshin AL (1987) History of the Earth’s atmosphere. Springer Verlag, New YorkCrossRefGoogle Scholar
  14. Cook TD, Bally AW (1975) Stratigraphie Atlas of North and Central America. Princeton University Press, Princeton, N.J.Google Scholar
  15. Floegel S, Wold CN, Hay WW (2000) Evolution of sediments and ocean salinity. Abstracts Volume, 31st International Geological Congress, Rio de Janeiro, Brazil, August 6–17, 2000, CD-ROM, 4 p.Google Scholar
  16. Gilluly J (1969) Geological perspective and the completeness of the geologic record. Geol Soc Am Bull 80: 2303–2312CrossRefGoogle Scholar
  17. Glaser KS, Droxler AW (1991) Holocene high stand shedding, producing a periplatform wedge in the surroundings of “drowned” shallow carbonate bank and shelf. Walton Basin, Northern Nicaragua Rise. J Sed Pet 61: 126–142Google Scholar
  18. Hay WW (1985) Potential errors in estimates of carbonate rock accumulating through geologic time. In: Sundquist ET, Broecker WS (eds) The carbon cycle and atmospheric CO2: Natural variations, Archaean to Present. Am Geophys Union, Geophys Monograph 32: 573–583CrossRefGoogle Scholar
  19. Hay WW (1994) Pleistocene-Holocene fluxes are not the Earth’s norm. In: Hay W, Usselman T (eds) Material Fluxes on the Surface of the Earth: Studies in Geophysics. National Academy Press, Washington, D.C.: 15–27Google Scholar
  20. Hay WW (1999) Carbonate sedimentation through the late Precambrian and Phanerozoic. Zentralblatt für Geologie und Paläontologie, Teil 1, 1998, Heft 5–6: 435–145Google Scholar
  21. Hay WW, Southam JR (1977) Modulation of marine sedimentation by the continental shelves. In: Anderson NR, Malahoff A (eds) The fate of fossil fuel CO2 in the oceans. Marine Science Series, Plenum Press, New York, 6: 569–604Google Scholar
  22. Hay WW, Sloan JL II, Wold CN (1988) The mass/age distribution of sediments on the ocean floor and the global rate of loss of sediment. J Geophys Res 93: 14933–14940CrossRefGoogle Scholar
  23. Hay WW, Wold CN, Söding E, Flögel S (2001) Evolution of sediment fluxes and ocean salinity. In: Merriam DF, Davis JC (eds) Geologic modeling and simulation: Sedimentary systems. Kluwer Academic/Plenum Publishers: 153–167CrossRefGoogle Scholar
  24. Hay WW, Söding E, DeConto RM, Wold CN (2002) The Late Cenozoic uplift – climate change paradox. Internat J Earth Sciences (Geologische Rundschau) 91: 746–774CrossRefGoogle Scholar
  25. Hoffman PF, Kaufman AJ, Halverson GP, Schräg DP (1998) A Neoproterozoic snowball earth. Science 281: 1342–1346CrossRefGoogle Scholar
  26. Iglesias-Rodríguez MD, Armstrong R, Feely R, Hood R, Kleypas J, Milliman JD, Sabine C, Sarmiento J (2002) Progress made in study of ocean’s calcium carbonate budget. EOS 83: 374–375CrossRefGoogle Scholar
  27. Khain VE, Ronov AB, Balukhovsky AN (1975) Cretaceous lithologic associations of the world. Sovietskaya Geologiya 11: 10–39 (in Russian) [English translation in Int Geol Rev 18: 1269–1295(1976)]Google Scholar
  28. Khain VE, Ronov AB, Seslavinskiy KB (1977) Silurian lithologic associations of the world. Sovietskaya Geologiya 5: 21–43 (in Russian) [English translation in Int Geol Rev 20: 249–268 (1978)]Google Scholar
  29. Khain VE, Ronov AB, Balukhovsky AN (1979) Neogene lithologic associations of the world. Sovietskaya Geologiya 10: 15–23 (in Russian) [English translation in Int Geol Rev 23: 426–454 (1981)]Google Scholar
  30. Khain VE, Levin LE, Tuliani LI (1982) Some quantitative parameters of global structure of the Earth. Geotectonics 16: 443–453Google Scholar
  31. Kunin NY (1987) Distribution of sedimentary basins of Eurasia and the volume of the Earth’s sedimentosphere. Int Geol Rev 29: 1257–1264CrossRefGoogle Scholar
  32. McArthur JM, Howarth RJ, Bailey TR (2001) Strontium isotope stratigraphy: LOWESS Version 3. Best-fit line to the marine Sr-isotope curve for 0 to 509 Ma and accompanying look-up table for deriving numerical age. J Geol 109: 155–169CrossRefGoogle Scholar
  33. Milliman JD (1993) Production and accumulation of calcium carbonate in the ocean: budget of a nonsteady state. Global Biogeochem Cy 7: 927–957CrossRefGoogle Scholar
  34. Milliman JD, Droxler AW (1996) Neritic and pelagic carbonate sedimentation in the marine environment: ignorance is not bliss. Internat J Earth Sci (Geol Rundsch) 85: 496–504Google Scholar
  35. Nicolas A, Elthon D, Moores E, Dilek Y (eds) (2001) Ophiolites and Ocean Crust. Geol Soc Am Special Paper 349: 1–560Google Scholar
  36. Pilskaln CH, Neumann AC, Bane JM (1989) Periplatform carbonate flux in the northern Bahamas. Deep-Sea Res 36: 1371–1406CrossRefGoogle Scholar
  37. Ramsay ATS (1974) The distribution of calcium carbonate in deep sea sediments. In: Hay WW (ed) Studies in Paleo-Oceanography. Soc Econ Paleont Miner Special Publication 20: 58–76Google Scholar
  38. Ronov AB (1980) The earth’s sedimentary shell (quantitative patterns of its structure, compositions, and evolution). – The 20th V. I. Vernadski Lecture, March 12, 1978 (in Russian). In: Yaroshevskii AA (ed) The Earth’s sedimentary shell (Quantitative patterns of its structure, compositions, and evolution). Nauka, Moscow, USSR: 1–80 [English translation in Int Geol Rev 24: 1313–1388 (1982); also American Geological Institute Reprint Series 5: 1–73 (1983)]Google Scholar
  39. Ronov AB (1993) Stratisfera – Hi Osadochnaya Obolochka Zemli (Kolichestvennoe Issledovanie). In: Yaroshevskii AA (ed) Nauka, Moscow, USSR: 1–144Google Scholar
  40. Ronov AB, Khain VY (1954) Devonian lithologic associations of the world. Sovetskaya Geologiya, 41: 47–76 (in Russian)Google Scholar
  41. Ronov AB, Khain VY (1955) Carboniferous lithologic associations of the world. Sovetskaya Geologiya, 48: 92–117 (in Russian)Google Scholar
  42. Ronov AB, Khain VY (1956) Permian lithologic associations of the world. Sovetskaya Geologiya, 54: 20–36 (in Russian)Google Scholar
  43. Ronov AB, Khain VY (1961) Triassic lithologic associations of the world. Sovetskaya Geologiya, 1: 27–48 (in Russian)Google Scholar
  44. Ronov AB, Khain VY (1962) Jurassic lithologic associations of the world. Sovietskaya Geologiya, 1: 9–34 (in Russian) [English translation in Int Geol Rev 1: 9–34 (1962)]Google Scholar
  45. Ronov AB, Seslavinskiy KB, Khain VY (1974) Cambrian lithologic associations of the world. Sovietskaya Geologiya, 12: 10–33 (in Russian) [English translation in Int Geol Rev 19: 373–394 (1977)]Google Scholar
  46. Ronov AB, Seslavinskiy KB, Khain VY (1976) Ordovician lithologic associations of the world. Sovietskaya Geologiya, 1: 7–27 (in Russian) [English translation in Int Geol Rev 18: 1395–1412(1976)]Google Scholar
  47. Ronov AB, Migdisov AA, Lobachzhuchenko SB (1977) Problems of evolution of chemical composition of sedimertary-rocks and regional metamorphism. Geokhimiya 2: 163–186Google Scholar
  48. Ronov AB, Khain VY, Balukhovsky AN (1978) Paleogene lithologic associations of the world. Sovietskaya Geologiya, 3: 142 (in Russian) [English translation in Int Geol Rev 21:415–446(1979)]Google Scholar
  49. Roth PH (1986) Mesozoic paleoceanography of the North Atlantic and Tethys oceans. In: Summerhayes CP, Shackleton NJ (eds) North Atlantic paleoceanography. Geological Society Special Publication 21: 299–320Google Scholar
  50. Schlager W, Reijmer J, Droxler AW (1994) Highstand shedding of carbonate platforms. J Sed Res B64: 270–281Google Scholar
  51. Schneidermann N (1977) Selective dissolution of recent coccoliths in the Atlantic Ocean: In: Ramsay ATS (ed) Oceanic micropaleontology 2: 1009–1053Google Scholar
  52. Scotese CR, Golonka J (1992) Paleogeographic Atlas. PALEOMAP Progress Report 20–0692, Department of Geology, University of Texas at Arlington, Arlington, Texas, USA, 34 ppGoogle Scholar
  53. Southam JR, Hay WW (1981) Global sedimentary mass balance and sea level changes. In: Emiliani C (ed) The Sea, 7, The Oceanic Lithosphere. Wiley-Interscience, New York, pp 1617–1684Google Scholar
  54. Van Andel TJH, Heath GR, Moore TC Jr. (1975) Cenozoic History and Paleoceanography of the Central Equatorial Pacific Ocean: A Regional Synthesis of Deep Sea Drilling Project Data. Geol Soc Am Memoir 143: 1–134Google Scholar
  55. Vaughan TW (1919) Corals and the formation of coral reefs. Smithsonian Institution Annual Report for 1917: 189–276Google Scholar
  56. Walker LJ, Wilkinson BH, Ivany LC (2002) Continental drift and Phanerozoic carbonate accumulation in shallow-shelf and deep-marine settings. J Geol 110: 75–87CrossRefGoogle Scholar
  57. Wallmann K (1999) Die Rolle der Subduktionszonen im globalen Wasser- und Kohlenstoffkreislauf. Habilitationsschrift, Christian-Albrechts-Universität, Kiel, GermanyGoogle Scholar
  58. Wallmann K (2001) Controls on the Cretaceous and Cenozoic evolution of seawater composition, atmospheric CO2 and climate. Geochim Cosmochim Ac 65: 3005–3025CrossRefGoogle Scholar
  59. Wold CN, Hay WW (1990) Reconstructing ancient sediment fluxes. Am J Sci 290: 1069–1089CrossRefGoogle Scholar
  60. Wold CN, Hay WW (1993) Reconstructing the age and lithology of eroded sediment. Geoinformatics 4: 137–144Google Scholar

Copyright information

© Springer-Verlag Berlin Heidelberg 2004

Authors and Affiliations

  • William W. Hay
    • 1
  1. 1.GEOMARKielGermany

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