PALEOCEANOGRAPHIC RECORDS OF INDONESIAN THROUGHFLOW AT ITS EXIT SINCE THE LAST GLACIAL AND THEIR SIGNIFICANCE

ZHANG Peng; XU Jian; YANG Ce; GAO Lianfeng; ZHANG Zhenguo; NIU Yao

doi:10.16562/j.cnki.0256-1492.2017.03.013

Marine Geology & Quaternary Geology > 2017 > 37(3): 129-137. > DOI: 10.16562/j.cnki.0256-1492.2017.03.013

ZHANG Peng, XU Jian, YANG Ce, GAO Lianfeng, ZHANG Zhenguo, NIU Yao. PALEOCEANOGRAPHIC RECORDS OF INDONESIAN THROUGHFLOW AT ITS EXIT SINCE THE LAST GLACIAL AND THEIR SIGNIFICANCE[J]. Marine Geology & Quaternary Geology, 2017, 37(3): 129-137. DOI: 10.16562/j.cnki.0256-1492.2017.03.013

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PALEOCEANOGRAPHIC RECORDS OF INDONESIAN THROUGHFLOW AT ITS EXIT SINCE THE LAST GLACIAL AND THEIR SIGNIFICANCE

ZHANG Peng^1,2,,
XU Jian^1,2, ,,
YANG Ce^1,2,
GAO Lianfeng³,
ZHANG Zhenguo³,
NIU Yao⁴

1.
Institute of Cenozoic Geology and Environment, Department of Geology, Northwest University Xi'an 710069
2.
State Key Laboratory of Continental Dynamics and Department of Geology, Northwest University, Xi'an 710069
3.
School of Mining Engineering, North China University of Science and Technology, Tangshan 063009
4.
The Fifth Geological Team, Henan Province Non-ferrous Metals Geological Mineral Resources Bureau, Zhengzhou 450016

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Received Date: June 21, 2016
Revised Date: September 05, 2016

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Abstract

Abstract

The Indonesian Throughflow (ITF), sole conduit between the Pacific and Indian Oceans, plays an important role in regulating heat and fresh water budgets between the two oceans, and in controlling the tropical and global climate. In this study, we investigated records from the Core SO18460 that was drilled at the exit of the ITF into the Timor Sea to reexamine their significance in reflecting the ITF since the last glacial. Records of temperature and salinity of surface and subsurface seawaters, and depth of thermocline (DOT) were reconstructed from δ¹⁸O and Mg/Ca ratio of the planktonic foraminifera of Globigerinoides ruber and Pulleniatina obliquiloculata and were then compared with regional paleoclimatic indices. The results show that salinity of both surface and thermocline seawaters co-varied with regional precipitation over the last glacial cycle, likely indicating transmission of precipitation signal by means of seawater salinity from sea surface to thermocline through upper ocean mixing. Sea surface temperature at the coring site of Core SO18460 oscillated centering at 28 ℃, possibly under influence of the Western Pacific Warm Pool since the early Holocene. In contrast, thermcoline seawater temperature (TWT) was always below 22 ℃, probably indicating that El Niño-Southern Oscillation was located in El Niño-like episodes. Decline of TWT and shoal of DOT might be, on the one hand, in response to more frequent El Niño-like events; and on the other hand, resulted from depression of ITF surface flow caused by increased precipitation due to southward shift of the Intertropical Convergence Zone, and/or by intensification of South China Sea surface flow driven by enhanced East Asian winter monsoon during Holocene. On glacial-interglacial timescale, TWT co-varied with the boreal summer insolation, possibly due to influence of North Pacific Tropical Water sourced waters that were carried by the Mindanao Current to the Sulawesi Sea and merged into the ITF.
- Indonesian Throughflow,
- salinity,
- Western Pacific Warm Pool,
- El Niño-Southern Oscillation,
- North Pacific Tropical Water

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References (45)

References

[1]	Gordon A L, Susanto R D, Vranes K. Cool Indonesian throughflow as a consequence of restricted surface layer flow[J]. Nature, 2003, 425(6960): 824-828. doi: 10.1038/nature02038
[2]	Gordon A L. Oceanography of the Indonesian seas and their throughflow[J]. Oceanography, 2005, 18(4): 14-27. doi: 10.5670/oceanog.2005.01
[3]	Sprintall J, Wijffels S E, Molcard R, et al. Direct estimates of the Indonesian throughflow entering the Indian Ocean: 2004-2006[J]. Journal of Geophysical Research, 2009, 114(C7): C07001. doi: 10.1029/2008JC005257
[4]	Trenberth K E. Recent observed interdecadal climate changes in the northern hemisphere[J]. Bulletin of the American Meteorological Society, 1990, 71(7): 988-993. doi: 10.1175/1520-0477(1990)071<0988:ROICCI>2.0.CO;2
[5]	Gordon A L, Huber B A, Metzger E J, et al. South China Sea throughflow impact on the Indonesian throughflow[J]. Geophysical Research Letters, 2012, 39(11): L11602, doi: 10.1029/2012GL052021.
[6]	Lee T, Fukumori I, Menemenlis D, et al. Effects of the Indonesian throughflow on the Pacific and Indian oceans[J]. Journal of Physical Oceanography, 2002, 32(5): 1404-1429. doi: 10.1175/1520-0485(2002)032<1404:EOTITO>2.0.CO;2
[7]	Song Q, Vecchi G A, Rosati A J. The role of the indonesian throughflow in the Indo-Pacific climate variability in the GFDL coupled climate model[J]. Journal of Climate, 2007, 20(11): 2434-2451. doi: 10.1175/jcli4133.1
[8]	Qu T D, Du Y, Strachan J, et al. Sea surface temperature and its variability in the Indonesian region[J]. Oceanography, 2005, 18(4): 50-61. doi: 10.5670/oceanog.2005.05
[9]	Holbourn A, Kuhnt W, Xu J. Indonesian throughflow variability during the last 140 Ka: the Timor sea outflow[J]. Geological Society, London, Special Publications, 2011, 355(1): 283-303, doi: 10.1144/SP355.14.
[10]	Martin P A, Lea D W. A simple evaluation of cleaning procedures on fossil benthic foraminiferal Mg/Ca[J]. Geochemistry, Geophysics, Geosystems, 2002, 3(10): 8401, doi: 10.1029/2001GC000280.
[11]	Fairbanks R G, Mortlock R A, Chiu T C, et al. Marine radiocarbon calibration curve spanning 0 to 50, 000 years BP based on paired ²³⁰Th/²³⁴U/²³⁸U and ¹⁴C dates on pristine corals[J]. Quaternary Science Reviews, 2005, 24(16-17): 1781-1796. doi: 10.1016/j.quascirev.2005.04.007
[12]	Xu J, Kuhnt W, Holbourn A, et al. Indo-Pacific Warm Pool variability during the Holocene and Last Glacial Maximum[J]. Paleoceanography, 2010, 25(4): PA4230, doi: 10.1029/2010PA001934.
[13]	Anand P, Elderfield H, Conte M H. Calibration of Mg/Ca thermometry in planktonic foraminifera from a sediment trap time series[J]. Paleoceanography, 2003, 18(2): 1050, doi: 10.1029/2002PA000846.
[14]	Bemis B E, Spero H J, Bijma J, et al. Reevaluation of the oxygen isotopic composition of planktonic foraminifera: experimental results and revised paleotemperature equations[J]. Paleoceanography, 1998, 13(2): 150-160. doi: 10.1029/98PA00070
[15]	Waelbroeck C, Labeyrie L, Michel E, et al. Sea-level and deep water temperature changes derived from benthic foraminifera isotopic records[J]. Quaternary Science Reviews, 2002, 21(1-3): 295-305, doi: 10.1016/S0277-3791(01)00101-9.
[16]	Locarnini R A, Mishonov A V, Antonov J I, et al. World ocean atlas 2009, volume 1: temperature[M]//Levitus S. NOAA Atlas NESDIS 68. Washington, DC: U.S. Government Printing Office, 2010: 184.
[17]	Antonov J I, Seidov D, Boyer T P, et al. World ocean atlas 2009, volume 2: salinity[M]//Levitus S. NOAA Atlas NESDIS 69. Washington, DC: U.S. Government Printing Office, 2010: 184.
[18]	Schlitzer R. Ocean data view: Version 4.6.2[CP/OL]. (2014-03-31). http://odv.awi.de.
[19]	Xu J, Holbourn A, Kuhnt W, et al. Centennial changes in the thermocline structure of the Indonesian outflow during terminations Ⅰ and Ⅱ[J]. Earth and Planetary Science Letters, 2008, 273(1-2): 152-162, doi: 10.1016/j.epsl.2008.06.029.
[20]	Labeyrie L D, Duplessy J C, Blanc P L. Variations in mode of formation and temperature of oceanic deep waters over the past 1250, 000 years[J]. Nature, 1987, 327(6122): 477-482. doi: 10.1038/327477a0
[21]	Visser K, Thunell R, Stott L. Magnitude and timing of temperature change in the Indo-Pacific warm pool during deglaciation[J]. Nature, 2003, 421(6919): 152-155. doi: 10.1038/nature01297
[22]	Sagawa T, Yokoyama Y, Ikehara M, et al. Shoaling of the western equatorial Pacific thermocline during the last glacial maximum inferred from multispecies temperature reconstruction of planktonic foraminifera[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2012, 346-347: 120-129. doi: 10.1016/j.palaeo.2012.06.002
[23]	Lea D W, Pak D K, Spero H J. Climate impact of late quaternary equatorial Pacific sea surface temperature variations[J]. Science, 2000, 289(5485): 1719-1724. doi: 10.1126/science.289.5485.1719
[24]	Yan X H, Ho C R, Zheng Q A, et al. Temperature and size variabilities of the western Pacific warm pool[J]. Science, 1992, 258(5088): 1643-1645. doi: 10.1126/science.258.5088.1643
[25]	Ayliffe L K, Gagan M K, Zhao J X, et al. Rapid interhemispheric climate links via the Australasian monsoon during the last deglaciation[J]. Nature Communications, 2013, 4: 2908, doi: 10.1038/ncomms3908.
[26]	Sprintall J, Gordon A L, Koch-Larrouy A, et al. The Indonesian seas and their role in the coupled ocean-climate system[J]. Nature, 2014, 7(7): 487-492. doi: 10.1038/ngeo2188
[27]	Xu J. Change of Indonesian throughflow outflow in response to east asian monsoon and ENSO activities since the Last Glacial[J]. Science China Earth Sciences, 2014, 57(4): 791-801, doi: 10.1007/s11430-014-4845-0.
[28]	Carton J A, Giese B S. A reanalysis of ocean climate using simple ocean data assimilation (SODA)[J]. Monthly Weather Review, 2008, 136(8): 2999-3017. doi: 10.1175/2007MWR1978.1
[29]	Rodbell D T, Seltzer G O, Anderson D M, et al. A ~15, 000-year record of El Ni o-driven alluviation in southwestern Ecuador[J]. Science, 1999, 283(5401): 516-520. doi: 10.1126-science.283.5401.516/
[30]	Moy C M, Seltzer G O, Rodbell D T, et al. Variability of El Ni o/southern oscillation activity at millennial timescales during the Holocene epoch[J]. Nature, 2002, 420(6912): 162-165. doi: 10.1038/nature01194
[31]	Koutavas A, deMenocal P B, Olive G C, et al. Mid-Holocene El Ni o-Southern Oscillation (ENSO) attenuation revealed by individual foraminifera in eastern tropical Pacific sediments[J]. Geology, 2006, 34(12): 993-996. doi: 10.1130/G22810A.1
[32]	Conroy J L, Overpeck J T, Cole J E, et al. Holocene changes in eastern tropical Pacific climate inferred from a Galápagos lake sediment record[J]. Quaternary Science Reviews, 2008, 27(11-12): 1166-1180.
[33]	Liu Z Y, Lu Z Y, Wen X Y, et al. Evolution and forcing mechanisms of El Ni o over the past 21, 000 years[J]. Nature, 2014, 515(7528): 550-553, doi: 10.1038/nature13963.
[34]	Qu T D, Mitsudera H, Yamagata T. A climatology of the circulation and water mass distribution near the Philippine coast[J]. Journal of Physical Oceanography, 1999, 29(7): 1488-1505, doi: 10.1175/1520-0485(1999)029<1488:ACOTCA>2.0.CO; 2.
[35]	Fine R A, Lukas R, Bingham F M, et al. The western equatorial Pacific: a water mass crossroads[J]. Journal of Geophysical Research, 1994, 99(C12): 25063-25080, doi: 10.1029/94JC02277.
[36]	Fine R A, Maillet K A, Sullivan K F, et al. Circulation and ventilation flux of the Pacific Ocean[J]. Journal of Geophysical Research, 2001, 106(10): 22159-22178, doi: 10.1029/1999JC000184.
[37]	Gordon A L. Interocean exchange of thermocline water[J]. Journal of Geophysical Research, 1986, 91(C4): 5037-5046. doi: 10.1029/JC091iC04p05037
[38]	Mohtadi M, Oppo D W, Lückge A, et al. Reconstructing the thermal structure of the upper ocean: insights from planktic foraminifera shell chemistry and alkenones in modern sediments of the tropical eastern Indian Ocean[J]. Paleoceanography, 2011, 26(3): PA3219, doi: 10.1029/2011PA002132.
[39]	Dang H W, Jian Z M, Bassinot F, et al. Decoupled Holocene variability in surface and thermocline water temperatures of the Indo-Pacific Warm Pool[J]. Geophysical Research Letters, 2012, 39(1): L01701. doi: 10.1029/2011gl050154
[40]	Fan W J, Jian Z M, Bassinot F, et al. Holocene centennial-scale changes of the Indonesian and South China Sea throughflows: evidences from the Makassar Strait[J]. Global and Planetary Change, 2013, 111: 111-117, doi: 10.1016/j.gloplacha.2013.08.017.
[41]	Haug G H, Hughen K A, Sigman D M, et al. Southward migration of the intertropical convergence zone through the Holocene[J]. Science, 2001, 293(5533): 1304-1308. doi: 10.1126/science.1059725
[42]	Linsley B K, Rosenthal Y, Oppo D W. Holocene evolution of the Indonesian throughflow and the western Pacific warm pool[J]. Nature Geoscience, 2010, 3(8): 578-583. doi: 10.1038/ngeo920
[43]	Griffiths M L, Drysdale R N, Gagan M K, et al. Abrupt increase in east Indonesian rainfall from flooding of the Sunda Shelf ~9500 years ago[J]. Quaternary Science Reviews, 2013, 74: 273-279. doi: 10.1016/j.quascirev.2012.07.006
[44]	Wang Y J, Cheng H, Edwards R L, et al. A high-resolution absolute-dated late Pleistocene monsoon record from Hulu Cave, China[J]. Science, 2001, 294(5550): 2345-2348. doi: 10.1126/science.1064618
[45]	Yuan D X, Cheng H, Edwards R L, et al. Timing, duration, and transitions of the last interglacial Asian monsoon[J]. Science, 2004, 304(5670): 575-578. doi: 10.1126/science.1091220

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PALEOCEANOGRAPHIC RECORDS OF INDONESIAN THROUGHFLOW AT ITS EXIT SINCE THE LAST GLACIAL AND THEIR SIGNIFICANCE

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