Isotopic evidences of past upwelling intensity in the Arabian Sea

Global and Planetary Change

Volumn 40, Issue 3-4, 2004, Pages 285-293

  Naidu, Pothuri Divakar ^a  

^a NATIONAL INSTITUTE OF OCEANOGRAPHY   (India)

Author keywords

Arabian Sea; Isotopes; Monsoon; Upwelling; Upwelling indices

Indexed keywords

CARBON ISOTOPE; MONSOON; OXYGEN ISOTOPE; PALEOCEANOGRAPHY; PLANKTONIC FORAMINIFERA; QUATERNARY; UPWELLING;

ARABIAN SEA; INDIAN OCEAN;

FORAMINIFERA; GLOBIGERINA; GLOBIGERINA BULLOIDES; GLOBIGERINOIDES SACCULIFER; NEOGLOBOQUADRINA DUTERTREI; PULLENIATINA OBLIQUILOCULATA;

EID: 0346333298     PISSN: 09218181     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.gloplacha.2003.09.002     Document Type: Article

References (34)

1. Andersen, D.M., Prell, W.L., 1993. A 300 kyr record of upwelling off Oman during the late Quaternary evidence of the Asian Southwest monsoon. Paleoceanography 8, 193-208.
2. Be, A.W.H., Tolderlund, D.S., 1971. Distribution and ecology of living planktonic foraminifera in surface waters of the Atlantic and Indian oceans. In: Funnell, B.M., Riedel, W.R. (Eds.), The Micropaleontology of Ocean. Cambridge Univ. Press, New York, pp. 105-149.
3. Be, A.W.H., Van Donk, J., 1971. Oxygen-18 studies of recent planktonic foraminifera. Science 173, 167-168.
4. Berger, W.H., Diester-Haass, L., Killingely, J.S., 1978. Upwelling off Northwest Africa. The Holocene decrease as seen in carbon isotopes and sedimentological indicators. Oceanologica Acta 1, 1-7.
5. Bruce, J.G., 1983. The wind field in the western Indian Ocean and the related ocean circulation. Monthly Weather Review 111, 1442-1452.
6. Clemens, S., Prell, W.L., Murray, D., Shimmield, G., Weedon, G., 1991. Forcing mechanisms of the Indian Ocean monsoon. Nature 353, 720-725.
7. Craig, H., 1957. Isotopic standards for carbon and oxygen and correction factors for mass-spectrometric analysis of carbon dioxide. Geochimica et Cosmochimica Acta 12, 133-149.
8. Curry, W.B., Ostermann, D.R., Guptha, M.V.S., Ittekkot, V., 1992. Foraminiferal production and monsoonal upwelling in the Arabian Sea, evidence from sediment traps. In: Summerhays, C.P., Prell, W.L., Emeis, K.C., et al. (Eds.), Upwelling Systems. Evolution since the Early Miocene. Geological Society Special Publication, vol. 64, pp. 93-106.
9. Deuser, W.G., Ross, E.H., 1989. Seasonally abundant foraminifera of the Sargasso Sea: succession, deep-water fluxes, isotopic composition, and paleoceanographic implications. Journal of Foraminiferal Research 19, 268-293.
10. Emiliani, E., 1955. Pleistocene temperatures. Journal of Geology 63, 538-578.
11. Epstein, S., Buchsbaum, R., Lowenstam, H.A., Urey, H.C., 1953. Revised carbonate-water isotopic temperature scale. Bulletin of the Geological Society of America 64, 1315-1325.
12. Hasternath, S., Lamb, P.J., 1979. Climatic Atlas of the Indian Ocean. University of Wisconsin Press, Madison, p. 97.
13. Honjo, S., Dymond, J., Prell, W.L., Ittekkot, V., 1999. Monsoon-controlled export fluxes to the interior of the Arabian Sea. Deep-Sea Research. Part 2. Topical Studies in Oceanography 46, 1859-1902.
14. Kroon, D., Ganssen, G., 1989. Northern Indian Ocean upwelling cells and the stable isotopic composition of living planktonic foraminifers. Deep-Sea Research 36, 1219-1236.
15. Labeyrie, L.D., Duplessy, J.-C, Blanc, PL., 1987. Variations in mode of formation and temperature of oceanic deep waters over the past 125,000 years. Nature 327, 477-482.
16. Madhupratap, M., Kumar, S.P, Bhattathiri, P.M.A., Kumar, R.D., Raghukumar, S., Nair, K.K.C., Ramaiah, N., 1996. Mechanism of the biological response to winter cooling in the northeastern Arabian Sea. Nature 384, 549-552.
17. McCrea, J.M., 1950. On the isotopic chemistry of carbonates and a paleotemperature scale. Journal of Chemical Physics 18, 849-859.
18. 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.
19. Naidu, P.D., Niitsuma, N., 2003. Carbon and oxygen isotope time series records of planktic and benthic foraminifera from the Arabian Sea: implications on upwelling processes. Paleogeography, Paleoclimatology, Paleoecology (in press).
20. Nair, R.R., Ittekkot, V., Manganini, S.J., Ramaswamy, V., Haake, B., Degens, E.T., Desai, B.N., Honjo, S., 1989. Increased particulate flux to the deep ocean related to monsoon. Nature 338, 749-751.
21. Niitsuma, N., Oba, T., Okada, M., 1991. Oxygen and carbon isotope stratigraphy at Site 723, Oman Margin. Proceedings of Ocean Drilling Program, Scientific Results 117, 321-341.
22. Peeters, F., 2000. The distribution and stable isotope composition of living planktic foraminifera in relation to seasonal changes in the Arabian Sea. PhD thesis, Free University, Amsterdam, The Netherlands, p. 184.
23. Prell, W.L., 1984. Monsoonal climate of the Arabian Sea during the late Quaternary: a response to changing solar radiation. In: Berger, A.L., et al. (Ed.), Milankovitch and Climate Part 1. Reidel, Dordrecht, pp. 349-366.
24. Prell, W.L., Curry, W.B., 1981. Faunal and isotopic indices of monsoonal upwelling: Western Arabian Sea. Oceanologica Acta 4, 91-98.
25. Prell, W.L., VanCampo, E., 1986. Coherent response of Arabian Sea upwelling and pollen transport to late Quaternary monsoonal winds. Nature 323, 526-528.
26. Prell, W.L., Murray, D.W., Clemens, S.C., Anderson, D.M., 1992. Evolution and variability of the Indian ocean summer monsoon: evidence from western Arabian sea drilling program. Geophysical Monograph 70, 447-469.
27. Shackleton, J., Wiseman, J.D.H., Buckley, H.A., 1973. Non-equilibrium isotopic fractionation between seawater and planktonic foraminiferal tests. Nature 242, 177-179.
28. Shi, W., Morrison, J.M., Bohm, E., Manghnani, V., 2000. The Oman upwelling zone during 1993, 1994 and 1995. Deep-Sea Research. Part 2. Topical Studies in Oceanography 47, 1227-1247.
29. Smith, S.L., Codispoti, L.A., Morrison, J.M., Barber, R.T., 1998. Arabian Sea expedition. An integrated, interdisciplinary investigation of the response of the northwestern Indian Ocean to Monsoonal forcing. Deep-Sea Research. Part 2. Topical Studies in Oceanography 45, 1905-1915.
30. Steens, T.N.F., Ganssen, G., Kroon, D., 1992. Oxygen and carbon isotopes in planktonic foraminifera as indicators of upwelling intensity and upwelling-induced high productivity in sediments from the northwestern Arabian Sea. In: Summerhays, C.P., et al. (Ed.), Upwelling Systems. Evolution since the Early Miocene. Geological Society Special Publication, vol. 64, pp. 107-119.
31. Thunell, R., Sautter, L.R., 1992. Planktonic foraminiferal faunal and stable isotopic indices of upwelling. A sediment trap study in the San Pedro Basin, Southern California Bight. In: Summerhays, C.P., et al. (Ed.), Upwelling Systems. Evolution since the Early Miocene. Geological Society Special Publication, vol. 64, pp. 77-91.
32. Urey, H.C., 1947. The thermodynamic properties of isotopic substances. Journal of Chemical Society, 562-581.
33. Wefer, G., Berger, W.H., 1991. Isotope paleontology: growth and composition of extant calcareous species. Marine Geology 100, 207-248.
34. Wiggert, J.D., Murtugudde, R.G., Mcclain, C.R., 2002. Processes controlling inter annual variations in wintertime (Northeast Monsoon) primary productivity in the central Arabian Sea. Deep-Sea Research. Part 2. Topical Studies in Oceanography 49, 2319-2343.