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The Importance and Measurement of New Production

  • Trevor Platt
  • Pratima Jauhari
  • Shubba Sathyendranath
Part of the Environmental Science Research book series (ESRH, volume 43)

Abstract

Public concern about the inadvertent interference by man in the processes that conspire to produce the earth’s climate — the general problem of “global change” — has emphasised the need for scientists to gain a deeper understanding of the planet as a compound biogeochemical system. In particular it has become recognised that we must improve our knowledge of the global carbon cycle, including the part of it that lies in the oceans. It is in this context that a rather obscure concept in biological oceanography has been projected into the scientific limelight and has given a household word (“new production”) to those institutions where research on global-change issues is carried out, written about, read about, or worried about. For understanding the oceanic carbon cycle, and the role of the oceans in the planetary carbon cycle, the concept of new production is central and fundamental.

Keywords

Regenerate Production Photic Zone Pelagic Ecosystem Annual Time Scale Biological Pump 
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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References

  1. Altabet, M. A., and Deuser, W. G., 1985, Seasonal variations in natural abundance of 15N in particles sinking to the deep Sargasso Sea, Nature, 315:218.CrossRefGoogle Scholar
  2. Andrews, J., Friedrich, C., Pautot, G., Pluger, W., Renard, V., Melguen, M., Cronan, D., Craig, J., Hoffert, M., Stoffers, P., Shearme, S., Thijssen, T., Glasby, G., Note, L., and Saget, P., 1983, The Hawaii-Tahiti transect. The oceanographic environments of manganese nodule deposits in the Central Pacific, Mar. Geol., 54:109.CrossRefGoogle Scholar
  3. Barnola, J. M., Reynaud, D., Korotkevich, Y.C., and Lorius, C., 1987, Vostok ice core provides 160,000-year record of atmospheric CO2, Nature, 329:408.CrossRefGoogle Scholar
  4. Bender, M. L., Grande, K., Johnson, J., Marra, J., Williams, J. LeB., Sieburth, J., Pilson, M., Langdon, C., Hitchcock, G., Orchardo, J., Hunt, C., Donaghay, P., and Heinemann, K., 1987, A comparison of four methods for determining planktonic community production, Limnol. Oceanogr., 32:1085.CrossRefGoogle Scholar
  5. Berger, W. H., Smetacek, V. S., and Wefer, G., 1989, Ocean productivity and paleoproductivity — an overview, in: “Productivity of the Ocean: Present and Past,” W. H. Berger, V. S. Smetacek, and G. Wefer, eds., John Wiley and Sons Limited.Google Scholar
  6. Coale, K. H., and Bruland, K. W., 1987, Oceanic stratified euphotic zone as elucidated by 234Th:238U disequilibria, Limnol. Oceanogr., 32:189.CrossRefGoogle Scholar
  7. Codispoti, L. A., 1989, Phosphorus vs. nitrogen limitation of new and export production, in: “Productivity of the Ocean: Present and Past,” W. H. Berger, V. S. Smetacek, and G. Wefer, eds., John Wiley and Sons Limited.Google Scholar
  8. Dugdale, R. C., 1967, Nutrient limitation in the sea: dynamics, identification, and significance, Limnol. Oceanogr., 12:685.CrossRefGoogle Scholar
  9. Dugdale, R. C., and Goering, J. J., 1967, Uptake of new and regenerated forms of nitrogen in primary productivity, Limnol. Oceanogr., 12:196.CrossRefGoogle Scholar
  10. Eppley, R. W., and Peterson, B. J., 1979, Particulate organic matter flux and planktonic new production in the deep ocean, Nature, 282:677.CrossRefGoogle Scholar
  11. Home, E. P. W., Loder, J. W., Harrison, W. G., Mohn, R., Lewis, M. R., Irwin, B., and Platt, T., 1989, Nitrate supply and demand at the Georges Bank tidal front, Scient. Mar., 53:145.Google Scholar
  12. Jenkins, W. J., 1982, Oxygen utilization rates in North Atlantic subtropical gyre and primary production in oligotrophic systems, Nature, 300:246.CrossRefGoogle Scholar
  13. Jenkins, W. J., 1988, Nitrate flux into the euphotic zone near Bermuda, Nature, 331:521.CrossRefGoogle Scholar
  14. Lewis, M. R., Harrison, W. G., Oakey, N. S., Herbert, D., and Platt, T., 1986, Vertical nitrate fluxes in the oligotrophic ocean, Science, 234:870.PubMedCrossRefGoogle Scholar
  15. McElroy, M. B., 1983, Marine biological controls on atmospheric CO2 and climate, Nature, 302:328.CrossRefGoogle Scholar
  16. Platt, T., 1984, Primary productivity in the central North Pacific: comparison to oxygen and carbon fluxes, Deep Sea Res., 31:1311.CrossRefGoogle Scholar
  17. Platt, T., and Harrison, W. G., 1985, Biogenic fluxes of carbon and oxygen in the ocean, Nature, 318:55.CrossRefGoogle Scholar
  18. Platt, T., and Harrison, W. G., 1986, Reconciliation of carbon and oxygen fluxes in the upper ocean, Deep Sea Res., 33:273.CrossRefGoogle Scholar
  19. Platt, T., and Sathyendranath, S., 1988, Oceanic primary production: Estimation by remote sensing at local and regional scales, Science, 1613:1620.Google Scholar
  20. Platt, T., Lewis, M. R., and Geider, R., 1984, Thermodynamics of the pelagic ecosystem: Elementary closure conditions for biological production in the open ocean, in: “Flows of Energy and Materials in Marine Ecosystems,” M. J. R. Fasham, ed., Plenum Publishing Corporation, New York.Google Scholar
  21. Platt, T., Harrison, W. G., Lewis, M. R., Li, W. K. W., Sathyendranath, S., Smith, R. E., and Vézina, A. F., 1989, Biological production of the oceans: The case for a consensus, Mar. Ecol. Prog. Ser., 52:77.CrossRefGoogle Scholar
  22. Quinones, R. A., and Platt, T., 1991, The relationship between the f-ratio and the P:R ratio in the pelagic ecosystem, Limnol. Oceanogr., 36:211.CrossRefGoogle Scholar
  23. Sarnthein, M., Winn, K., and Zahn, R., 1987, Paleoproductivity or oceanic upwelling and the effect on atmospheric CO2 and climate change during déglaciation times, in: “Abrupt Climatic Change — Evidence and Implications,” W. H. Berger and L. D. Labeyrie, eds., Reidel, Dordrecht.Google Scholar
  24. Sathyendranath, S., Platt, T., Home, E. P. W., Harrison, W. G., Ulloa, O., Outerbridge, R., and Hoepffner, N., 1991, New production in the ocean: estimation by compound remote sensing, Nature, in press.Google Scholar
  25. Smith, S.V., 1984, Phosphorus versus nitrogen limitation in the marine environment, Limnol Oceanogr., 29:1149.CrossRefGoogle Scholar
  26. Vézina, A., and Platt, T., 1987, Small-scale variability of new production and particulate fluxes in the ocean, Can. J. Fish. Aquat. Sci., 44:198.CrossRefGoogle Scholar

Copyright information

© Springer Science+Business Media New York 1992

Authors and Affiliations

  • Trevor Platt
    • 1
  • Pratima Jauhari
    • 2
  • Shubba Sathyendranath
    • 1
    • 3
  1. 1.Biological Oceanography DivisionBedford Institute of OceanographyDartmouthCanada
  2. 2.Geological Oceanography DivisionNational Institute of OceanographyDona PaulaIndia
  3. 3.Department of OceanographyDalhousie UniversityHalifaxCanada

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