Paleoproductivity in the Equatorial Indian Ocean for the last 260,000 yr: A transfer function based on planktonic foraminifera

Quaternary Science Reviews

Volumn 18, Issue 6, 1999, Pages 839-857

  Cayre, Olivia ^b   Beaufort, Luc ^b   Vincent, Edith ^a,b  

^a CNRS   (France)

^b STATION MARINE D ENDOUME   (France)

Author keywords

[No Author keywords available]

Indexed keywords

PALEOPRODUCTIVITY; PLANKTONIC FORAMINIFERA; QUATERNARY; TRANSFER FUNCTION;

INDIAN OCEAN;

GLOBIGERINA BULLOIDES; GLOBIGERINA FALCONENSIS; GLOBIGERINITA GLUTINATA; GLOBIGERINOIDES RUBER; GLOBIGERINOIDES SACCULIFER; GLOBIYERINELLA AEQUILATERALIS; GLOBOQUADRINA CONGLOMERATA; GLOBOROTALIA CRASSAFORMIS; GLOBOROTALIA MENARDII; NEOGLOBOQUADRINA DUTERTREI;

EID: 0033135214     PISSN: 02773791     EISSN: None     Source Type: Journal    
DOI: 10.1016/S0277-3791(98)00036-5     Document Type: Article

References (77)

1. Andersen, D. M., & Prell, L. W. (1991). Coastal upwelling gradient during the late Pleistocene. In W. L. Prell, N. Nitsuma et al. (Eds.), Proceedings of the Ocean Drilling Program. Scientific Results, 117 (pp. 265-273). TX: College Station. Ocean Drilling Program.
2. Anderson, D. M., & Prell, L. W. (1993). A 300 kyr record of upwelling off oman during the late quarternary: Evidence of the Asian southwest monsoon. Paleoceanography, 8, 193-208.
3. Antoine, D., & Morel, A. (1996). Oceanic primary production. 1. Adaptation of a spectral light-photosynthesis model in view of application to satellite chlorophyll observations. Global Biogeochemical Cycles, 10, 43-55.
4. Antoine, D., André, J. M., & Morel, A. (1996). Oceanic primary production. 2. Estimation at global scale from satellite (coastal zone color scanner) chlorophyll. Global Biogeochemical Cycles, 10, 57-96.
5. Barnett, T. P., Dümenil, L., Schlese, U., Roeckner, E., & Latif, M. (1989). The effect of Eurasian snow cover on regional and global climate variations. Journal of the Atmospheric Sciences, 46, 261-285.
6. Bassinot, F. C., Labeyrie, L. D., Vincent, E., Quidelleur, X., Shackleton, N. J., & Lancelot, Y. (1994). The astronomical theory of climate and the age of the Brunhes-Matuyama magnetic reversal. Earth and Planetary Science Letters, 126, 91-108.
7. Bé, A. W. H. (1982). Biology of planktonic foraminifera. In T. W. Broadheat (Ed.), Foraminifera. Notes for a Short Course: Studies in Geology (Vol. 6, pp. 51-92). Knoxville, Tennessee: University of Tennessee.
8. Bé, A. W. H., & Hutson, W. H. (1977). Ecology of planktonic foraminifera and biogeographic patterns of life and fossil assemblages in the Indian Ocean. Micropaleontology, 23, 369-414.
9. Bé, A. W. H., & Tolderlund, D. S. (1971). Distribution and ecology of living planktonic foraminifera in surface waters of the Atlantic and Indian Oceans. In B. M. Funnel & W. R. Riedel (Eds.), The Micropaleontology of Oceans (pp. 105-149). Cambridge: Cambridge University Press.
10. Beaufort, L. (1996). Dynamics of the monsoon in the equatorial indian Ocean over the last 260,000 years. Quaternary International, 31, 13-18.
11. Beaufort, L., Lancelot, Y., Camberlin, P., Cayre, O., Vincent, E., Bassinot, F., & Labeyrie, L. (1997). Insolation cycles as a major control of equatorial Indian Ocean primary production, Science, 278, 1451-1454.
12. Berger, W. H. (1971). Sedimentation of planktonic foraminifera, Marine Geology, 11, 325-358.
13. Berger, A., & Loutre, M. F. (1991). Insolation values for the climate of the last 10 million years. Quaternary Science Reviews, 10, 297-317.
14. Bijma, J., Faber, W. W., & Hemleben, Ch. (1990). Temperature and salinity limits for growth and survival of some planktonic foraminifers in laboratory cultures. Journal of Foraminiferal Research, 20, 95-116.
15. Bottero, J. S. (1969). An Analysis of Upwelling Off the Southeast Arabian Coast during the Summer Monsoon. M.S. thesis, pp. 70. Corvallis: Oregon State University.
16. Brock, J. C., McClain, Ch. R., Anderson, D. M., Prell, W. L., & Hay, W. W. (1992). Southwest monsoon circulation and environment of recent planktonic foraminifera in the Northwestern Arabian Sea. Paleoceanography, 7, 799-813.
17. Caulet, J. P., Vénec-Peyré, M. T., Vergnaud-Grazzini, C., & Nigrini, C. A. (1992). Variation of south Somalian upwelling during the last 160 ka: Radiolarian and foraminifera records in Core MD 85674. In C. P. Summerhayes, W. L. Prell, K. C. Emeis (Eds.), Upwelling System: Evolution since the Early Miocene (Vol. 64, pp. 379-390). Geological Society Special Publication of London.
18. Clemens, S., & Prell, W. L. (1990). Late pleistocene variability of Arabian Sea Summer Monsoon winds and continental aridity: eolian records from the lithogenic component of deep-sea sediments. Paleoceanography, 5, 109-145.
19. Clemens, S., & Prell, W. L. (1991). Late Quaternary forcing of Indian Ocean summer-monsoon winds. A Comparison of Fourier model and General Circulation Model results. Journal of Geophyphysical Research, 96, 22683-22700.
20. Clemens, S., Prell, W. L., Murray, D., Shimmield, G., & Weedon, G. (1991). Forcing mechanisms of Indian Ocean Monsoon. Nature, 353, 720-725.
21. Crowley, T. J., & North, G. R. (1990). Paleoclimatology (pp. 414), New York: Oxford University Press.
22. Cullen, J. L. (1981). Microfossil evidence for changing salinity in the bay of Bengal over the last 20,000 years. Palaeogeography, Palaeoclimatology, Palaeoecology, 35, 315-356.
23. Cullen, J. L., & Prell, W. L. (1984). Planktonic foraminifera of the northern Indian Ocean. Distribution and preservation in surface sediments. Marine Micropaleontology, 9, 1-52.
24. Dietrich, G. (1973). The unique situation in the environment of the Indian Ocean. In B. Zeitzschel (Ed.) The Biology of the Indian Ocean (pp. 1-6). New York: Springer.
25. Düing, W. (1969). The Monsoon Regime of the Currents in the Indian Ocean (pp. 65). Honolulu: East-West Center Press.
26. Duplessy, J. C. (1982). Glacial to interglacial contrasts in the northern Indian Ocean. Nature, 295, 494-498.
27. Emerson, S., & Bender, M. (1981). Carbon fluxes at the sediment-water interface of the deep-sea. Calcium carbonate preservation. Journal of Marine Research, 39, 139-162.
28. Fontugne, M. R., & Duplessy, J. C. (1986). Variation of the monsoon regime during the upper Quaternary: Evidence from carbon isotopic record of organic matter in North Indian Ocean sediment cores. Palaeogeography, Palaeoclimatology, Palaeoecology, 56, 69-88.
29. Hahn, D., & Shukla, J. (1976). An apparent relationship between eurasian snow cover and Indian monsoon rainfall. Journal of the Atmospheric Sciences, 33, 2461-2463.
30. Hastenrath, S., Nicklis, A., & Greischar, L. (1993). Atmospheric-hydrospheric mechanisms of climate anomalies in the western Equatorial Indian Ocean, Journal of Geophysical Research, 98, 20219-20235.
31. Hemleben, Ch., Spindler, M., & Anderson, O. R. (1988). Modern Planktonic Foraminifera (pp. 363). New York: Springer.
32. Hutson, W. H. (1977). Transfer functions under no-analog conditions: Experiments with Indian Ocean planktonic foraminifera. Quaternary Research, 8, 355-367.
33. Hutson, W. H. (1978). Application of transfer function to Indian Ocean planktonic foraminifera. Quaternary Research, 9, 87-112.
34. Hutson, W. H. (1979). The Agulhas current during the late pleistocene: Analysis of modern faunal analogs. Science, 207, 64-66.
35. Hutson, W. H., & Prell, W. L. (1980). A paleocological transfer function, F1-2, for indian planktonic foraminifera. Journal of Paleontology, 54, 381-399.
36. Imbrie, J., & Kipp, N. G. (1971). A new micropaleontological method for quantitative paleoclimatology: Application to a late Pleistocene Caribean core. In K. K. Turekian (Ed.), The Late Cenozoic Glacial Ages (pp. 71-181). New Haven: Yale University Press.
37. Jenkins, G. M., & Watts, D. G. (1968). Spectral Analysis and its Applications (pp. 552). Oakland, California: Holden-Day.
38. Kallel, N., Labeyrie, L., Juillet-Leclerc, A., & Duplessy, J. C. (1988). A deep hydrological front between intermediate and deep water masses in the glacial Indian Ocean. Nature, 333, 651-655.
39. Kipp, N. G. (1976). New transfer function for estimating past sea-surface condition from sea-bed distribution of planktonic foraminiferal assemblages in North Atlantic. In R. M. Cline & J. D. Hays (Eds.), Investigation of Late Quarternary Paleoceanography and Paleoclimatology. Geological Society of America, Memoir, (Vol. 145, pp. 3-41).
40. Knox, R. A. (1987). The Indian Ocean: Interaction with the monsoon. In J. S. Fein & P. L. Stephens (Eds.), Monsoons (pp. 632) NewYork: Wiley.
41. Kroon, D. (1988). Distribution of extant planktic foraminiferal assemblages in Red Sea and Northern Indian Ocean surface waters. In G. J. A. Brummer, & D. Kroon (Eds.), Planktonic Foraminifers as Tacers of Ocean-climate History (pp 229-270). Amsterdam, The Netherlands: Free University Press.
42. Kroon, D., Beets, K., Mowbray, S., Shimmield, G., & Steens, T. (1990). Changes in northern Indian Ocean monsoonal wind activity during the last 500KA. Memorie Della Societa Geologica Italiana, 44, 189-207.
43. Kutzbach, J. E., & Guetter, P. J. (1986). The influence of changing orbital parameters and surface boundary conditions on climate simulations for the past 18000 years. Journal of the Atmospheric Sciences, 43, 1726-1759.
44. Kutzbach, J. E., & Otto-Bliesner B. L. (1982). The sensitivity of the African-Asian monsoonal climate to orbital parameter changes for 9000 years B.P. In a low-resolution general circulation model. Journal of the Atmospheric Sciences, 39, 1177-1188.
45. Le, J. & Shackleton, N. J. (1992). Carbonate dissolution fluctuations in the western equatorial Pacific during the late Quaternary. Paleoceanography, 7, 21-42.
46. Lancelot, Y., Balut, Y., & the shipboard scientific party (1992). 50-m piston cores taken in the tropical Indian Ocean (SEYMAMA/ SHIVA Expedition). 4th International Congress on Paleo-oceanography, Kiel, p176.
47. Levitus, S. (1982). Climatological atlas of the World Oceans. NOAA Prof. Pap. 13. pp. 173. US. govt. Printing office.
48. Lorentz, S., Grieger, B., Helbig, Ph., & Herterich, K. (1996). Investigating sensitivity of the Atmospheric General Circulation Model ECHAM 3 to paleoclimatic boundary conditions. Geologisches Rundschau, 85, 513-524.
49. Mix, A. C. (1989a). Pleistocene paleoproductivity: Evidence from organic carbon and foraminiferal species. In W. H. Berger, V. S. Smetacek & G. Wefer (Eds.), Productivity of the Ocean: Present and Past (pp. 313-340), New York: Wiley.
50. 2. Nature, 337, 541-544.
51. Mléneck Vautravers, M. (1997). Sédimentation et dissolution des carbonates biogéniques aux moyennes latitudes nord et sud. Approche Quantitative et Relations Avec les Paléocirculations Océan-Ques des Derniers 150000 Ans. Thèse de l' Université de Bordeaux I, pp 288.
52. Müller, P. J., & Suess, E. (1979). Productivity, sedimentation rate and sedimentary organic matter in the oceans, I. Organic carbon preservation. Deep-Sea Research, 26, 1347-1362.
53. Naidu, P. D., Babu, C. P., & Rao, Ch. M. (1992). The upwelling record in the sediments of the western continental margin of India. Deep-Sea Research, 39, 715-723.
54. Naidu, P. D., & Malmgren, B. A. (1996) A high-resolution record of late Quaternary upwelling along the Oman Margin, Arabian Sea based on planktonic foraminifera. Paleoceanography, 11, 129-140.
55. Ottens, J. J. (1992). Planktonic Foraminifera as Indicators of Ocean Environments in the Northest Atlantic (pp. 189) Amsterdam: Urije Universiteit.
56. Parker, F. L., & Berger, W. H. (1971). Faunal and solution patterns of planktonic foraminifera in surface sediments of the South Pacific. Deep-Sea Research, 18, 73-107.
57. Pflaumann, U., Duprat, J., Pujol, C., & Labeyrie, L. D. (1996). SimMAX: A modern analog technic to deduce Atlantic sea surface temperatures from planktonic foraminifera in deep-sea sediments. Paleoceanography, 11, 15-35.
58. Prahl, F. G., & Muehlhausen, L. A. (1989). Lipid Biomarkers as Geochemical Tools for Paleoceanographic Study. In W. H. Berger, V. S. Smetacek & G. Wefer (Eds.), Productivity of the Ocean: Present and Past (pp. 271-289) NewYork: Wiley.
59. Prell, W. L. (1985). The stability of low-latitude sea-surface temperatures: An evaluation of the CLIMAP reconstruction with emphasis on the positive SST anomalies. Technical Report, U.S. Dept. of Energy, pp. 60. Brown University, Dept. of Applied Sciences.
60. Prell, W. L., & Curry, W. B. (1981). Faunal and isotopic indices of monsoonal upwelling: Western Arabian Sea. Oceanologica Acta, 4, 91-98.
61. Prell, W. L., & Hutson, W. H. (1979). Zonal temperature-anomaly maps of Indian Ocean surface waters: Modern and ice-age patterns. Science, 206, 454-456.
62. Prell, W. L., Hutson, W. H., Williams, D. F., Bé, A. W. H., Geitzenauer, K., & Molfino, B. (1980). Surface circulation of the Indian Ocean during the last glacial maximum, approximately 18,000 yr B.P. Quaternary Research, 14, 309-336.
63. Prell, W. H., Flannery, B. P., Teukolsky, S. A., & Vetterling, W. T. (1986). Numerical Recipes: The Art of the Scientific Computing (pp. 618). Cambridge: Cambridge University Press.
64. Rao, K. K., Jayalakshmy, K. V., Kumaran, S., Balasubramanian, T., & Kutti, M. K. (1989). Planktonic foraminifera in waters off the Coromandel coast, Bay of Bengal. Indian Journal of Marine Sciences, 18, 1-7.
65. Rostek, F., Ruhland, G., Bassinot, F., Beaufort, L., Müller, P. J., & Bard, E. (1994). Fluctuations of the Indian monsoon regime during the last 170,000 years. Evidence from sea surface temperature, salinity and organic carbon records. In M. Desbois & F. Désalmand (Eds.), Global Precipitations and Climate Change, NATO ASI Series I 26 (pp. 27-51). Heidelberg: Springer.
66. Rostek, F., Bard, E., Beaufort, L., Sonzogni, C., & Ganssen, G. (1997). Sea surface temperature and productivity records for the past 240 kyr in the Arabian Sea. Deep Sea Research 2, 44, 1461-1480.
67. Sirocko, F., Sarnthein, M., Lange, H., & Erlenkeuser, H. (1991) Atmospheric summer circulation and coastal upwelling in the Arabian Sea during the holocene and the last glaciation. Quaternary ReSearch, 36, 72-93.
68. Smith, R. L., & Bottero, J. S. (1977). On upwelling in the Arabian Sea. In M. Angel (Ed.), A Voyage of Discovery (pp. 291-304). NewYork: Pergamon.
69. Thioulouse, J. (1990). Macmul and graphmu: Two Macintosh programs for the display and analysis of multivariate data. Computers and Geosciences, 16, 1235-1240.
70. Thunell, R. C. (1976). Optimum indices of calcium carbonate dissolution in deep-sea sediments. Geology, 4, 525-527.
71. Thunell, R. C., & Honjo, S. (1981). Calcite dissolution and modification of planktonic foraminiferal assemblages. Marine Micropaleontology, 6, 169-182.
72. Toggweiller, J. R., Dixon, K., & Bryan, K. (1989). Simulations of radiocarbon in a coarse-resolution world ocean model 2. Distributions of bomb-produced carbon 14. Journal of Geophysical Research, 94, 8243-8264.
73. Vénec-Peyré, M. T., Caulet, J. P., & Vergnaud Grazzini, C. (1995). Paleohydrographic changes in the Somali Basin (5°n upwelling and equatorial areas) during the last 160 kyr, based on correspondence analysis of foraminiferal and radiolarian assemblages. Paleoceanography, 10, 473-491.
74. Woodruff, S. D., Slutz, R. J., Jenne, R. L., & Steurer, P. M. (1987). A comprehensive Ocean-Atmosphere Data Set, Bulletin of American Meteorogical Society, 68, 1239-1250.
75. Wyrtki, K. (1971). Oceanographic Atlas of the International Indian Ocean Expedition (pp. 531). Washington DC: National Science Foundation.
76. Wyrtki, K. (1973). Physical oceanography of the indian ocean. In B. Zeitzschel (Ed.), The Biology of the Indian Ocean (pp. 18-36). NewYork: Springer.
77. Zhang, J. (1985). Living planktonic foraminifera from the eastern Arabian Sea. Deep-Sea Research, 32, 789-798.