Changes in the vertical profile of Indonesian Throughflow during Termination II: Evidence from the Timor Sea

Paleoceanography

Volumn 21, Issue 4, 2006, Pages

  Xu, Jian ^a   Kuhnt, Wolfgang ^a   Holbourn, Ann ^a   Andersen, Nils ^a   Bartoli, Gretta ^a  

^a UNIVERSITY OF KIEL   (Germany)

Author keywords

[No Author keywords available]

Indexed keywords

CLIMATE CHANGE; GLACIAL-INTERGLACIAL CYCLE; MARINE ISOTOPE STAGE; MONSOON; PALEOTEMPERATURE; PLANKTONIC FORAMINIFERA; PRECIPITATION ASSESSMENT; SEA LEVEL; SEA SURFACE TEMPERATURE; THERMOCLINE; THROUGHFLOW; TIMESCALE; VERTICAL PROFILE; WIND PROFILE;

ASIA; EURASIA; INDIAN OCEAN; INDONESIA; SOUTHEAST ASIA; TIMOR SEA;

FORAMINIFERA;

EID: 34547992480     PISSN: 08838305     EISSN: None     Source Type: Journal    
DOI: 10.1029/2006PA001278     Document Type: Article

References (70)

1. Anand, P., H. Elderfield, and M. H. Conte (2003), Calibration of Mg/Ca thermometry in planktonic foraminifera from a sediment trap time series, Paleoceanography, 18(2), 1050, doi:10.1029/2002PA000846.
2. Andreasen, D. J., and A. C. Ravelo (1997), Tropical Pacific Ocean thermocline depth reconstructions for the last glacial maximum, Paleoceanography, 12(3), 395-413.
3. Ashkenazy, Y., and E. Tziperman (2006), Scenarios regarding the lead of equatorial sea surface temperature over global ice volume, Paleoceanography, 21, PA2006, doi:10.1029/2005PA001232.
4. Bassinot, F., et al. (2002), Scientific report of the WEPAMA cruise, MD122/RAAGES VII, 453 pp., Inst. Fr. pour la Rech. et la Technol., Polaires, France.
5. Bé, A. W. H. (1977), An ecological, zoogeographical and taxonomic review of recent planktonic foraminifera, in Oceanic Micropaleontology, edited by A. T. S. Ramsay, pp. 1-100, Elsevier, New York.
6. Bemis, B. E., H. J. Spero, J. Bijma, and D. W. Lea (1998), Reevaluation of the oxygen isotopic composition of planktonic foraminifera: Experimental results and revised paleotemperature equations, Paleoceanography, 13(2), 150-160.
7. Cane, M. A., and A. Clement (1999), A Role for the tropical Pacific coupled ocean-atmosphere system on Milankovitch and millennial timescales. part II: Global impacts, in Mechanisms of Global Climate Change at Millennial Time Scales, Geophys. Monogr. Ser, vol. 112, edited by P. U. Clark, R. S. Webb, and L. D. Keigwin, pp. 373-383, AGU, Washington D. C.
8. Conan, S. M.-H., E. M. Ivanova, and G.J. A. Brummer (2002), Quantifying carbonate dissolution and calibration of foraminiferal dissolution indices in the Somali Basin, Mar. Geol., 182, 325-349.
9. Conkright, M. E., et al. (2002), World Ocean Atlas 2001: Objective analyses, data statistics, and figures, CD-ROM documentation, Internal Rep. 17, 17 pp., Natl. Oceanogr. Data Cent., Silver Spring, Md.
10. Cortese, G., and A. Abelmann (2002), Radiolarian-based paleotemperatures during the last 160 kyr at ODP Site 1089 (Southern Ocean, Atlantic sector), Palaeogeogr. Palaeoclimatol. Palaeoecol., 182, 259-286.
11. Cresswell, G., A. Frische, J. Peterson, and D. Quadfasel (1993), Circulation in the Timor Sea, J. Geophys. Res., 98(C8), 14,379-14,389.
12. De Deckker, P., N. J. Tapper, and S. van der Kaars (2002), The status of the Indo-Pacific Warm Pool and adjacent land at the Last Glacial Maximum, Global Planet. Change, 35, 25-35.
13. Dekens, P. S., D. W. Lea, D. K. Pak, and H. J. Spero (2002), Core top calibration of Mg/Ca in tropical foraminifera: Refining paleotemperature estimation, Geochem. Geophys. Geosyst., 3(4), 1022, doi:10.1029/ 2001GC000200.
14. de Villiers, S., M. Greaves, and H. Elderfield (2002), An intensity ratio calibration method for the accurate determination of Mg/Ca and Sr/ Ca of marine carbonates by ICP-AES, Geochem. Geophys. Geosyst., 3(1), 1001, doi:10.1029/2001GC000169.
15. Esat, T. M., M. T. McCulloch, J. Chappel, B. Pillans, and A. Omura (1999), Rapid fluctuations in sea level recorded at Huon Peninsula during the penultimate deglaciation, Science, 283, 197-209.
16. Godfrey, J. S. (1996), The effect of the Indonesian Throughflow on ocean circulation and heat exchange with the atmosphere: A review, J. Geophys. Res., 101(C5), 12,217-12,237.
17. Gordon, A. L., and R. A. Fine (1996), Pathways of water between the Pacific and Indian oceans in the Indonesian seas, Nature, 379, 146-149.
18. Gordon, A. L., R. D. Susanto, and A. L. Ffield (1999), Throughflow within Makassar Strait, Geophys. Res. Lett., 26, 3325-3328.
19. Gordon, A. L., R. D. Susanto, and K. Vranes (2003), Cool Indonesian Throughflow as a consequence of restricted surface layer flow, Nature, 425, 824-828.
20. Hastings, D., M. Kienast, S. Steinke, and A. Whitko (2001), A comparison of three independent paleotemperature estimates from a high resolution record of deglacial SST records in the tropical South China Sea, Eos Trans. AGU, 82, Fall Meet. Suppl., Abstract PP12B-10.
21. Hemleben, C., M. Spindler, and O. R. Anderson (1989), Modern Planktonic Foraminifera, 363 pp., Springer, New York.
22. Herguera, J. C., and W. H. Berger (1991), Paleoproductivity from benthic foraminifera abundance: Glacial to postglacial change in the west-equatorial Pacific, Geology, 19, 1173-1176.
23. Holboum, A., W Kuhnt, H. Kawamura, Z. Jian, P. Grootes, H. Erlenkeuser, and J. Xu (2005), Orbitally paced paleoproductivity variations in the Timor Sea and Indonesian Throughflow variability during the last 460 kyr, Paleoceanography, 20(3), PA3002, doi:10.1029/2004PA001094.
24. Jian, Z., B. Huang, W. Kuhnt, and H. Lin (2001), Late Quaternary upwelling intensity and east Asian monsoon forcing in the South China Sea, Quat. Res., 55, 363-370.
25. Kienast, M., S. Steinke, K. Stattegger, and S. E. Calvert (2001), Synchronous tropical South China Sea SST change and Greenland warming during deglaciation, Science, 297, 226-230.
26. Koutavas, A., J. Lynch-Stieglitz, T. M. Marchitto Jr., and J. P. Sachs (2002), El Niño-like pattern in ice age tropical Pacific sea surface temperature, Science, 297, 226-230.
27. Kuhnt, W., S. Hess, and Z. Jian (1999), Quantitative composition of benthic foraminiferal assemblages as a proxy indicator for organic carbon flux rates in the South China Sea, Mar. Geol., 156, 123-158.
28. Kuhnt, W., A. Holbourn, R. Hall, M. Žuvela, and R. Käse (2004), Neogene history of the Indonesian Throughflow, in Continent-Ocean Interactions Within East Asia Marginal Seas, Geophys. Monogr. Ser., vol. 149, edited by P. Clift et al., pp. 299-320, AGU, Washington, D. C.
29. Kuhnt, W., et al. (2006), Cruise report SONNE-185 "Variability of the Indonesian Throughflow and Australasian climate history of the last 150 000 years (VITAL)", report, Inst. für Geowiss., Christian-Albrechts-Univ. zu Kiel, Kiel, Germany, in press.
30. Lambeck, K., and J. Chappell (2001), Sea level change through the last glacial cycle, Science, 292, 679-686.
31. Laskar, J. (1990), The chaotic motion of the solar system: A numerical estimate of the size of the chaotic zones, Icarus, 88, 266-291.
32. Le, J., and N. J. Shackleton (1992), Carbonate dissolution fluctuations in the western equatorial Pacific during the late Quaternary, Paleoceanography, 7(1), 21-42.
33. Lea, D. W., D. K. Pak, and H. J. Spero (2000), Climate impact of late Quaternary equatorial Pacific sea surface temperature variations, Science, 289, 1719-1724.
34. Lea, D. W., D. K. Pak, L. C. Peterson, and K. A. Hughen (2003), Synchroneity of tropical and high-latitude Atlantic temperatures over the last glacial termination, Science, 301, 1361-1364.
35. Lee, T., I. Fukumori, D. Menemenlis, Z. Xing, and L.-L. Fu (2002), Effects of the Indonesian Throughflow on the Pacific and Indian oceans, J. Phys. Oceanogr., 32(5), 1404-1429.
36. Liu, Z. H., and T. D. Herbert (2004), High-latitude influence on the eastern equatorial Pacific climate in the early Pleistocene epoch, Nature, 427, 720-723.
37. Lohmann, G. P. (1995), A model for variation in the chemistry of planktonic foraminifera due to secondary calcification and selective dissolution, Paleoceanography, 10(3), 445-457.
38. Longhurst, A. (1998), Ecological Geography of the Sea, Elsevier, New York.
39. Martin, P. A., and D. W. Lea (2002), A simple evaluation of cleaning procedures on fossil benthic foraminiferal Mg/Ca, Geochem. Geophys. Geosyst., 3(10), 8401, doi:10.1029/2001GC000280.
40. Martinson, D. G., et al. (1987), Age dating and the orbital theory of the ice ages: Development of a high-resolution 0 to 300,000 year chronostratigraphy, Quat. Res., 27, 1-29.
41. Medina-Elizalde, M., and D. W. Lea (2005), The mid-Pleistocene transition in the tropical Pacific, Science, 310, 1009-1012, doi:10.1126/science.1115933.
42. Molcard, R., M. Fieux, and F. Syamsudin (2001), The throughflow within Ombai Strait, Deep Sea Res., Part I, 48, 1237-1253.
43. Murray, S. P., and D. Arief (1988), Throughflow into the Indian Ocean through the Lombok Strait, January 1985-January 1986, Nature, 333, 444-447.
44. North Greenland Ice Core Project Members (2004), High-resolution record of Northern Hemisphere climate extending into the last interglacial period, Nature, 431, 147-151.
45. Oppo, D. W., and Y. Sun (2005), Amplitude and timing of sea-surface temperature change in the northern South China Sea: Dynamic link to the east Asian monsoon, Geology, 33, 785-788, doi:10.1130/G21867.1.
46. Paillard, D., L. Laberyrie, and P. Yiou (1996), Macintosh program performs time-series analysis, Eos Trans. AGU, 77, 39.
47. Potemra, J. T., S. L. Hautala, and J. Sprintall (2003), Vertical structure of Indonesian Throughflow in a large-scale model, Deep Sea Res., Part II, 50, 2143-2161.
48. Ravelo, A. C., and R. G. Fairbanks (1992), Oxygen isotopic composition of multiple species of planktonic foraminifera: Recorders of the modern photic zone temperature gradient, Paleoceanography, 7(6), 815-831.
49. Ravelo, A. C., R. G. Fairbanks, and S. G. H. Philander (1990), Reconstructing tropical Atlantic hydrography using planktonic foraminifera and an ocean model, Paleoceanography, 5(3), 409-431.
50. Rosenthal, Y., and G. P. Lohmann (2002), Accurate estimation of sea surface temperatures using dissolution-corrected calibrations for Mg/Ca paleothermometry, Paleoceanography, 17(3), 1044, doi:10.1029/ 2001PA000749.
51. 16O of seawater, Paleoceanography, 15(1), 135-145.
52. Russell, A. D., B. Hönisch, H. J. Spero, and D. W. Lea (2004), Effects of seawater carbonate ion concentration and temperature on shell U, Mg, and Sr in cultured planktonic foraminifera, Geochim. Cosmochim. Acta, 68(21), 4347-4361.
53. Saito, T., P. R. Thompson, and D. Breger (1981), Systematic Index of Recent and Pleistocene Planktonic Foraminifera, 190 pp., Univ. of Tokyo Press, Tokyo.
54. Sarnthein, M., and K. Winn (1990), Reconstruction of low and middle latitude export productivity, 30,000 years B. P. to present: Implication for control of global carbon reservoirs, in Climate-Ocean Interaction, edited by M. E. Schlesinger, pp. 319-342, Springer, New York.
55. Schiller, A., J. S. Godfrey, P. C. McIntosh, G. Meyers, and S. E. Wijffels (1998), Seasonal near-surface dynamics and thermodynamics of the Indian Ocean and Indonesian Throughflow in a global ocean general circulation model, J. Phys. Oceanogr., 28(11), 2288-2312.
56. Schmidt, M. W., H. J. Spero, and D. W. Lea (2004), Links between salinity variation in the Caribbean and North Atlantic thermocline circulation, Nature, 428, 160-163.
57. Shackleton, N. J., M. Chapman, M. F. Sánchez-Goñi, D. Pailler, and Y. Lancelot (2002), The classic marine isotope substage 5e, Quat. Res., 58, 14-16.
58. Shackleton, N. J., M. F. Sánchez-Goñi, D. Pailler, and Y. Lancelot (2003), Marine isotope sub-stage 5e and the Eemian interglacial, Global Planet. Change, 36, 151-155.
59. Sirocko, F., K. Seelos, K. Schaber, B. Rein, F. Dreher, M. Diehl, R. Lehne, K. Jäger, M. Krbetschek, and D. Degering (2005), A late Eemian aridity pulse in central Europe during the last glacial inception, Nature, 436, 833-836, doi:10.1038/nature03905.
60. Song, Q., and A. L. Gordon (2004), Significance of the vertical profile of the Indonesian Throughflow transport to the Indian Ocean, Geophys. Res. Lett., 31, L16307, doi:10.1029/2004GL020360.
61. Speich, S., B. Blanke, and G. Madec (2001), Warm and cold water routes of an O.G.C.M. thermohaline conveyor belt, Geophys. Res. Lett., 28(2), 311-314.
62. Tapper, N. (2002), Climate, climatic variability and atmospheric circulation patterns in the maritime continent region, in Bridging Wallace's Line: The Environmental and Cultural History and Dynamics of the SE-Asian-Australian Region, edited by P. Kershaw et al., Adv. Geoecol., 34, 5-38.
63. Ter Braak, C. J. F. (1995), Ordination, Chapter 5 in: Data Analysis in Community Landscape Ecology, edited by R. H. G. Jongman, C. J. F. Ter Braak, and O. F. R. Van Tongeren, pp. 91-173, Cambridge Univ. Press, New York.
64. Thunell, R., E. Tappa, C. Pride, and E. Kincaid (1999), Sea-surface temperature anomalies associated with the 1997-1998 El Niño recorded in the oxygen isotope composition of planktonic foraminifera, Geology, 27, 843-846.
65. Visser, K., R. Thunell, and L. Stott (2003), Magnitude and timing of temperature change in the Indo-Pacific warm pool during deglaciation, Nature, 421, 152-155.
66. Waelbroeck, C., L. Labeyrie, E. Michel, J.-C. Duplessy, J. F. McManus, K. Lambeck, E. Balbon, and M. Labracherie (2002), Sea-level and deep water temperature changes derived from benthic foraminifera isotopic records, Quat. Sci. Rev., 21, 295-305, doi:10.1016/ S0277-3791(01)00101-9.
67. Wang, P., S. Clemens, L. Beaufort, P. Braconnot, G. Ganssen, Z. Jian, P. Kershaw, and M. Sarnthein (2005), Evolution and variability of the Asian monsoon system: State of the art and outstanding issues, Quat. Sci. Rev., 24, 595-629.
68. Wollenburg, J., and W. Kuhnt (2000), The response of benthic foraminifers to carbon flux and primary production in the Arctic Ocean, Mar. Micropaleontol., 40, 189-231.
69. You, Y., and M. Tomczak (1993), Thermocline circulation and ventilation in the Indian Ocean derived from water mass analysis, Deep Sea Res., Part I, 40, 13-56.
70. Žuvela, M. (2005), Modelling of the Indonesian Throughflow on glacial-interglacial timescales, Ph.D thesis, Math. -Naturwiss. Fak., Christian-Albrechts-Univ. Kiel, Kiel, Germany.