THE LAST GLACIATION MAXIMUM IN THE SEA OF JAPAN/EAST SEA

LIU Yanguang; ZOU Jianjun; LI Chaoxin; ZHANG Weibin; SHI Xuefa; Suk Bong-Chool

doi:10.3724/SP.J.1140.2009.04053

Marine Geology & Quaternary Geology > 2009 > 29(4): 53-63. > DOI: 10.3724/SP.J.1140.2009.04053

LIU Yanguang, ZOU Jianjun, LI Chaoxin, ZHANG Weibin, SHI Xuefa, Suk Bong-Chool. THE LAST GLACIATION MAXIMUM IN THE SEA OF JAPAN/EAST SEA[J]. Marine Geology & Quaternary Geology, 2009, 29(4): 53-63. DOI: 10.3724/SP.J.1140.2009.04053

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THE LAST GLACIATION MAXIMUM IN THE SEA OF JAPAN/EAST SEA

1 Key Laboratory of Marine Sedimentology and Environmental Geology, First Institute of Oceanography, SOA, Qingdao 266061, China;
2 South Sea Research Institute, Korea Ocean Research & Development Institute, Geoje 656-830, Korea

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Received Date: May 29, 2009
Revised Date: June 09, 2009

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Abstract

Abstract

Hemipelagic sediments in the Sea of Japan (East Sea) during the last glaciation maximum (LGM) were characterized by centimeter-to decimeter-scale alternations of organic-poor light-gray layers, organic-rich dark-gray layers and homogenous layers. In association with the sedimentary characteristics, the alkenone sea surface temperatures (U^k'37-SSTs) of the central and southern Japan Sea were estimated and the results enabled us to understand the paleoceanographic evolutions in the study area during the LGM and its linkage with the East Asian monsoon (EAM). During 24.2~17.8 cal kaBP,deposition of the laminated layers had good relationship with the strengthening summer EAM,indicating that the EAM precipitation was the main cause for the oxygen-level variation of bottom water in the Japan Sea. The low U^k'37-SSTs in the northern Okinawa Trough during 24.2~17.8 cal kaBP further implied that the strong influx of East China Sea Coastal Water (ECSCW), which was regarded as lower-salinity and nutrient-enriched watermass and derived from the precipitation of summer EAM, had influence on the northern part of the East China Sea. Under the influence of weakened summer EAM or intensified winter EAM, the ventilation of deep water was reinforced and the suboxic or oxic bottom water dominated in the basins of Japan Sea during 30~24.2 and 17.8~15cal kaBP.Why there was the anomaly of high U^k'37-SSTs in the Japan Sea during 23~17.5 cal kaBP was not fully understood so far. It was generally accepted that the ventilation of deep water was blocked during this period by the density stratification of the water column as a result of excessive EAM precipitation, the surface salinity was low and the bottom was filled with static, anoxic water.
- sea level,
- East Asian monsoon,
- last glaciation maximum,
- Japan Sea

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References (54)

References

[1]	Oba T, Kato, M, Kitazato, H,et al.Paleoenvironmental changes in the Japan Sea during the last 85000 years[J]. Paleoceanography,1991,6:499-518.
[2]	Yamada K, Ishiwatari R.Carbon isotope compositions of long-chain n-alkanes in the Japan Sea sediments:implication for paleoenvironmental changes over the past 85 kyr[J]. Organic Geochemistry,1999,30:367-377.
[3]	Itaki T, Ikehara K, Motoyama I,et al.Abrupt ventilation changes in the Japan Sea over the last 30 ky:evidence from deep-dwelling radiolarians[J]. Palaeogeography, Palaeoclimatology, Palaeoecology,2004,208, 263-278.
[4]	Gorbarenko S A,Southon J R.Detailed Japan Sea paleoceanography during the last 25 kyr:constraints from AMS ¹⁴C dating and δ¹⁸O of planktonic foraminifera[J]. Palaeogeography, Palaeoclimatology, Palaeoecology,2000,156:177-193.
[5]	Tada R, Irino T, Koizumi I.Land ocean linkages over orbital and millennial timescales recorded in late Quaternary sediments of the Japan Sea[J]. Paleoceanography,1999,14(2):236-247.
[6]	Bahk J J, Chough S K, Han S J.Origins and paleoceanographic significance of laminated muds from the Ulleung Basin, East Sea (Sea of Japan)[J]. Marine Geology,2000,162, 459-477.
[7]	Watanabe S, Tada R, Ikehara K.et al.Sediment fabrics, oxygenation history, and circulation modes of Japan Sea during the Late Quaternary[J]. Palaeogeography, Palaeoclimatology, Palaeoecology,2007,247:50-64.
[8]	Wang L J, Oba T.Tele-connections between East Asian monsoon and the high-latitude climate:a comparison between the GISP2 ice core record and the high resolution marine records from the Japan and the South China seas[J]. Quaternary Research,1998,37(3):221-219.
[9]	Wang P X.Response of western Pacific marginal seas to glacial cycles:Paleoceanographic and sedimentological features[J]. Marine Geology 1999,156:5-39.
[10]	Lee K E.Surface water changes recorded in late Quaternary marine sediments of the Ulleung Basin, East Sea (Japan Sea)[J].Palaeogeography,Palaeoclimatology, Palaeoecology,2007,247:18-31.
[11]	Ishiwatari R, Houtatsu M, Okada H.Alkenone-sea surface temperature in the Japan Sea over the past 36 kyr:warm temperature at the last glacial maximum[J]. Marine Geology,2001,32:57-67
[12]	Fujine K, Yamamoto M, Tada R, Kido Y.A salinity related occurrence of a novel alkenone and alkenoate in late Pleistocene sediments from the Japan Sea[J]. Organic Geochemistry, 2006,37:1074-1084.
[13]	Lee K E, Bahk J J, Choi J Y.Alkenone temperature estimates for the East Sea during the last 190,000 years[J]. Organic Geochemistry,2008,39:741-753.
[14]	Liu Y G, Shi X F, Xing L, et al.Associated sea surface temperature in the East Sea (Sea of Japan) with the East Asia climatic changes since the last 170 ka. Submitted.2009.
[15]	Oba T, Murayama M, Matsumoto E,et al. AMS ¹⁴C ages of Japan Sea from the Oki Ridge[J]. Quaternary Research (Jpn),1995,34(4):289-296.
[16]	Kato M.Japan Sea since the last glacial age:foraminifera mainly based on analysis of core KH-793, C-3[J].Chikyu 1984,6:529-536.
[17]	Nakajima T,Kikkawa K,Ikehara K,et al.Marine sediments and late Quaternary stratigraphy in the southeastern part of the Japan Sea-concerning the timing of dark layer deposition[J]. Journal of the Geological Society of Japan,1996,102(2):125-138.
[18]	Crusius J, Pedersen T F, Calvert S E.A 36 kyr geochemical record from the Sea of Japan organic matter flux variations and changes in intermediate water oxygen concentrations[J]. Paleoceanography,1999.14(2):248-259.
[19]	Yokoyama Y, Kido Y, Tada R,et al.Japan Sea oxygen isotope stratigraphy and global sea-level changes for the last 50000 years recorded in sediment cores from the Oki Ridge[J]. Palaeogeography, Palaeoclimatology, Palaeoecology,2007,247:5-17.
[20]	Khim B K, Bahk J J, Hyun S,et al.Late Pleistocene dark laminated mud layers from the Korea Plateau, western East Sea/Japan Sea, and their paleoceanographic implications[J]. Palaeogeography, Palaeoclimatology, Palaeoecology,2007,247:74-87.
[21]	Chun J H, Cheong D, Ikehara K,et al.Age of the SKP-I and SKP-Ⅱ tephras from the southern East Sea/Japan Sea:Implications for interstadial events recorded in sediment from marine isotope stages 3 and 4[J]. Palaeogeography, Palaeoclimatology, Palaeoecology,2007,247:100-114.
[22]	Itaki T, Komatsu N, Motoyama I.Orbital and millennial-scale changes of radiolarian assemblages during the last 220 kyrs in the Japan Sea[J]. Palaeogeography, Palaeoclimatology, Palaeoecology,2007,247:115-130.
[23]	Khim B K, Ikehara K, Shin Y.Unstable Holocene climate in the northeastern East Sea (Sea of Japan):evidence from a diatom record[J]. Palaeogeography, Palaeoclimatology, Palaeoecology,2005,216:251-265.
[24]	Kido Y, Ikue M, Tada R, Orbital-scale stratigraphy and high-resolution analysis of biogenic components and deep-water oxygenation conditions in the Japan Sea during the last 640 kyr[J]. Palaeogeography, Palaeoclimatology,Palaeoecology,2007,247:32-49.
[25]	Hayashida A, Hattori S, Oda H.Diagenetic modification of magnetic properties observed in a piston core (MD01-2407) from the Oki Ridge, Japan Sea[J]. Palaeogeography, Palaeoclimatology, Palaeoecology,2007,247:65-73.
[26]	Ikeda M, Suzuki F, Oba T.A box model of glacial-interglacial variability in the Japan Sea[J]. Journal of Oceanography,1999,55:483-492.
[27]	Kumamoto Y, Yoneda M, Shibata Y,et al.Direct observation of the rapid turnover of the Japan Sea bottom water by means of AMS radiocarbon measurement[J].Geophysical Research Letters,1998:25(5):651-654.
[28]	Gamo T, Horibe Y.Abyssal circulation in the Japan Sea[J]. Journal of Oceanographic Society of Japan,1983,39:220-230.
[29]	Isobe A.On the origin of the Tsushima Warm Current and it seasonality[J]. Continental Shelf Research,1999,19:117-133.
[30]	Liu Y G, Shi X F, Suk B C, et al.Paleoceanographic evolution of southern Ulleung Basin, East Sea (Sea of Japan), during the last 48000 yrs. Submitted,2009.
[31]	Arthur M A, Sageman B B.Marine black shale:depositional environments of ancient deposits[J]. Ann. Rev. Earth. Planet. Sci.,1994,22:499-551.
[32]	Behl R J, Kennett J P.Brief interstadial events in the Santa Barbara basin, NE Pacific, during the past 60 kyr[J]. Nature,1996,379:243-246.
[33]	Diego T D, Douglas R G.Oxygen-related sediment microfabrics in modern "black shales", Gulf of California, Mexico[J].Journal of Foraminifera Research,1999,29(4):453-464.
[34]	Peterson L C, Hang G H, Hughen K A,et al.Rapid changes in the hydrologic cycle of the tropical Atlantic during the last glacial[J]. Science,2000,290, 1947-1950.
[35]	Schulz H, von Rad U, Erlenkauser H.Correlation between Arabian Sea and Greenland climate oscillations of the past 110,000 years[J]. Nature,1998,393:54-57.
[36]	Ijiri A, Wang L, Oba T.Paleoenvironmental changes in the northern area of the East China Sea during the past 42,000 years[J]. Palaeogeography, Palaeoclimatology, Palaeoecology,2005,219:239-261.
[37]	Yokoyama Y, De Deckker P, Lambeck K,et al.Sea-level at the Last Glacial Maximum:evidence from northwestern Australia to constrain ice volumes for oxygen isotope stage 2[J]. Palaeogeography, Palaeoclimatology, Palaeoecology,2001,165:281-297.
[38]	Yokoyama Y, Esat T M, Lambeck K.Coupled climate and sea-level changes deduced from Huon Peninsula coral terraces of the Last Ice Age[J]. Earth and Planetary Science Letters,2001,193:579-587.
[39]	Lambeck K, Yokoyama Y, Purcell T.Into and out of the Last Glacial Maximum:sea-level change during oxygen isotope stages 3 and 2[J]. Quaternary Science Reviews,21:2002,21:343-360.
[40]	LIU J P, Milliman J D, Gao S,et al. Holocene development of the Yellow River's subaqueous delta, North Yellow Sea[J]. Marine Geology,2004,209:45-67.
[41]	Wang Y J, Hai C, Edwards R L,et al.Millennial and orbital-scale changes in the East Asian monsoon over the past 224000 years[J]. Nature,451:1090-1093.
[42]	Irino T, Tada R.High-resolution reconstruction of variation in aeolian dust (Kosa) deposition at ODP site 797, the Japan Sea, during the last 200 ka[J]. Global and Planetary Change,2002,35:143-156.
[43]	Seki O, Kawamura K, Ikehara M,et al.Variation of alkenone sea surface temperature in the Sea of Okhotsk over the last 85 kyrs[J]. Organic Geochemistry,2004,35:347-354.
[44]	Okumura S, Minagawa M, Oba T,et al.Paleoenvironmental analysis of two sediment cores off Akita city in the Japan Sea based on oxygen, carbon and nitrogen isotopes[J]. Quaternary Research (Jpn),1996,35:349-358.
[45]	Matsui H, Tada R, Oba T.Low salinity isolation event in the Japan Sea in response to eustatic sea-level drop during LGM:reconstruction based on salinity-balance model[J]. Quaternary Research (Jpn),1998.37(3):221-223.
[46]	Tanimura Y, Shimada C, Haga M.Migration of continental mixed-waters preserved in abundance of a diatom species Paralia sulcata:paleoceanography of the northeastern East China Sea from the Last Glacial through the Postglacial[J]. Quaternary Research (Jpn),2002,41(2):85-93.
[47]	Prahl F G, Wolfe G V, Sparrow M A.Physiological impacts on alkenone paleothermometry[J]. Paleoceanography,2003,18(2):1025, doi: 10.1029/2002PA000803.
[48]	Bendle J, Rosell-Melé A, Ziveri P.Variability of unusual distribution of alkenones in the surface waters of the Nordic seas[J]. Paleoceanography,2005.20. doi: 10.1029/2004PA001025.
[49]	Brassell S C, Eglinton G, Marlowe I T,et al.Molecular stratigraphy:a new tool for climatic assessment[J]. Nature,1986,320:129-133.
[50]	Volkman J K, Barrett S M, Blackburn S I, et al.Alkenones in Gephyrocapsa oceanica:implications for studies of paleoclimate[J]. Geochimica et Cosmochimica Acta,1995,59:513-520.
[51]	Li J, Philp R P, Pu F, et al.Long-chain alkenones in Qinghai Lake sediments[J]. Geochimica et Cosmochimica Acta, 1996,60:235-241.
[52]	Sonzogni C, Bard E, Rostek F, et al.Temperature and salinity effects on alkenone ratios measured in surface sediments from the Indian Ocean[J]. Quaternary Research,1997,47:344-355.
[53]	Sikes E L, Farrington J W, Keigwin L D.Use of the alkenone unsaturation ratio U₃₇ to determine past sea surface temperatures:core-top SST calibrations and methodology considerations[J].Earth Planetary Scientific Letters, 1991,104:36-47.
[54]	Seki O, Kawamura K, Sakamoto T,et al.Decreased surface salinity in the Sea of Okhotsk during the last glacial period estimated from alkenones[J]. Geophysical Research Letters,2005.32, L08710. doi: 10.1029/2004GL022177.

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