Environmental anomalies in the northeastern East China Sea during the last 3 000 years: implications for El Niño activity in the Holocene

Fengming Chang; Tiegang Li; Lihua Zhuang; Jun Yan

doi:10.1007/s00343-010-9066-6

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Environmental anomalies in the northeastern East China Sea during the last 3 000 years: implications for El Niño activity in the Holocene

OriginalPaper | Updated：2023-05-16

- Environmental anomalies in the northeastern East China Sea during the last 3 000 years: implications for El Niño activity in the Holocene
- Environmental anomalies in the northeastern East China Sea during the last 3 000 years: implications for El Niño activity in the Holocene
- 海洋湖沼学报（英文） 2010年28卷第1期页码：190-200
- Affiliations：
  
  Key Laboratory of Marine Geology and Environment Institute of Oceanology Chinese Academy of Sciences
- Author bio：
- Funds：
  
  Supported by the Knowledge Innovation Program of Chinese Academy of Sciences (Project No. KZCX2-YW-221), the State Key Basic Research and Development Plan of China (Project No2007CB815903) and the National Natural Science Foundation of China (Project No. 40506015).
- DOI：10.1007/s00343-010-9066-6
  中图分类号：
- 网络首发：2010-01-27，
  
  纸质出版：2010
- Accepted：
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Environmental anomalies in the northeastern East China Sea during the last 3 000 years: implications for El Niño activity in the Holocene[J]. 海洋湖沼学报（英文）, 2010,28(1):190-200.

Chang, F., Li, T., Zhuang, L. et al. Environmental anomalies in the northeastern East China Sea during the last 3 000 years: implications for El Niño activity in the Holocene., Chin. J. Ocean. Limnol. 28, 190–200 (2010). https://doi.org/10.1007/s00343-010-9066-6
Environmental anomalies in the northeastern East China Sea during the last 3 000 years: implications for El Niño activity in the Holocene[J]. 海洋湖沼学报（英文）, 2010,28(1):190-200. DOI： 10.1007/s00343-010-9066-6.

Chang, F., Li, T., Zhuang, L. et al. Environmental anomalies in the northeastern East China Sea during the last 3 000 years: implications for El Niño activity in the Holocene., Chin. J. Ocean. Limnol. 28, 190–200 (2010). https://doi.org/10.1007/s00343-010-9066-6 DOI：

摘要

Abstract

To reconstruct the productivity changes for the last 10 500 a in the northeastern East China Sea (ECS)

biogenic compounds (such as carbonate

organic carbon and opal)

marine micropaleontological fossils (planktonic foraminifera

benthic foraminifera

radiolarian and silicoflagellate) and the compositional characters of benthic foraminifera fauna analyses were carried out on a sediment core DOC082 obtained from the western slope of Okinawa Trough (29°13.93′N

128°08.53′E; 1 128 m water depth). The long-term changes of biogenic and micropaleontological proxies display some similarities through the last 10 500 a

which show three different phases: lower values are recorded during the early and middle Holocene (before about 4 000 a BP)

followed by an abrupt and remarkable increase at about 4 000 a BP

the late Holocene (after about 3 000 a BP) is characterized by continuously high values. The multi-proxy data of paleoproductivity and percents of benthic foraminifera genera (Uvigerina and Bulimina) show that during the early and middle Holocene (10 500–4 000 a BP) productivity was relatively low with a sudden and distinct increase at about 4 000 a BP

and the late Holocene (3 400–0 a BP) is marked by significantly higher productivity. Also

the radiolarian-based sea surface temperature (SST) records reveal a distinct decline in SST in the late Holocene after 3 200 a BP

very different from the early and middle Holocene. For the last 3 000 a

the enhanced biological productivity and distinctly lower SST indicate a major change of oceanographic conditions in the northeastern ECS. These marine environmental anomalies are consistent with other paleoclimatic records for the late Holocene in the Chinese continent and its surrounding regions. After analyzing the mechanisms of modern productivity and SST changes in the northeastern ECS

and based on the climatic anomalies in the Chinese continent and variations in the Kuroshio Current during modern El Niño periods

we suggest that the anomalous environmental conditions in the northeastern ECS may imply intensified El Niño activity during the late Holocene.

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references

Abbott M B, Binford M W, Kelts K R. 1997. A 3500 14C yr high resolution record of water-level changes in Lake Titicaca, Bolivia/Peru. Quaternary Research, 47: 169–180.

Altenbach A, Sarnthein M. 1989. Productivity in Benthic Foraminifera. In: Berger, W. H., V. S. Smetacek and G. Wefer eds. Productivity of the ocean: present and past. John Wiley & Sons Press, New York. p. 255–270.

Athanasios K, Lynch-Stieglitz J, Marchitto J et al. 2002. El Niño-like pattern in Ice Age Tropical Pacific Sea Surface Temperature. Science, 297: 226–230.

Bard E. 1988. Correction of accelerator mass spectrometry 14C ages measured in planktonic foraminifer: paleoceanographic implications. Paleoceanography, 3: 635–645.

Barron J A, Bukry D, Bischo J L. 2003. High resolution paleoceanography of the Guaymas Basin, Gulf of California, during the past 15000 years. Marine Micropaleontology, 949: 1–23.

Beardsley R C, Limeburner R, Yu H et al. 1985. Discharge of the Changjiang (Yangtze River) into the East China Sea. Cont. Shelf Res., 4(1–2): 57–76.

Bush A. 1999. Assessing the impact of mid-Holocene insolation on the atmosphere-ocean system. Geophysical Research Letters, 26: 99–102.

Chang F M, Li T G, Zhuang L H et al. 2008. A Holocene paleotemperature record based on radiolaria from the northern Okinawa Trough (East China Sea). Quaternary International, 183: 115–122.

Charles C, Hunter D, Fairbanks R. 1997. Interaction between the ENSO and the Asian Monsoon in a coral record of tropical climate. Science, 277: 925–928.

Chen R, Meng Y, Li B et al. 1999. Variations in the lysocline of carbonate in the southern Okinawa trough during the last 20 000 years. Maine Geology & Quaternary Geology, 19: 25–30. (in Chinese)

Chen W. 2002. Impacts of El Niño and La Niña on the cycle of the East Asian winter and summer monsoon. Chinese Journal of Atmospheric Sciences, 26: 595–610. (in Chinese with English abstract)

Chen Y L, Wang F, Bai X Z et al. 2004. Relationship between Hairtail (Trichiurus haumela) catches and marine hydrologic environment in the East China sea. Oceanologia et Limnologia Sinica, 35(5): 404–412. (in Chinese with English abstract)

Clement A C, Seager R, Cane M A. 2000. Suppression of El Niño during the mid-Holocene by changes in the Earth’s orbit. Paleoceanography, 15: 731–737.

Correge T, Delcroix T, Recy J et al. 2000. Evidence for stronger El Niño-Southern Oscillation (ENSO) events in a mid-Holocene massive coral. Paleoceanography, 14: 465–470.

Fei Z, Li B, Kuroda K. 1993. Primary Productivity in the Northern East China Sea. In: Su J, Cheng Z, Yu, G. eds. Proceeding of China-Japan Joint Symposium of the Cooperative Study on the Kuroshio 5. Ocean Press, Beijing, p. 47–159. (in Chinese)

Fontugne M, Usselmann P, Lavalle D et al. 1999. El Niño variability in the coastal desert of Southern Peru during the mid-Holocene. Quaternary Research, 52: 171–179.

Gagan M, Hendya E, Haberleb S et al. 2004. Post-glacial evolution of the Indo-Pacific Warm Pool and El Niño-Southern oscillation. Quaternary International, 118-119: 127–143.

Gagan M K, Ayliffe L K, Hopley D et al. 1998. Temperature and surface-ocean water balance of the mid-Holocene tropical western Pacific. Science, 279: 1014–1018.

Gong D, Wang S. 1998. Impact of ENSO on the seasonal rainfall in China. Journal of Natural Disasters, 7: 44–52. (in Chinese)

Guo B H, Li X Z, Lee J H. 1998. Interaction of Kuroshio water and shelf water in the Tsushima Current region in summer. ACTA Oceanologica Sinica, 20(5): 1–12. (in Chinese with English abstract)

Haberle S, Hope G, van der Kaars S. 2001a. Biomass burning in Indonesia and Papua New Guinea: natural and human induced fire events in the fossil record. Palaeogeography, Palaeoclimatology, Palaeoecology, 171: 259–268.

Haberle S, Ledru M. 2001b. Correlations among charcoal records of fires from the past 16,000 years in Indonesia, Papua New Guinea, and Central and South America. Quaternary Research, 55: 97–104.

Hama T, Shin H, Handa N. 1997. Spatial variability in the primary productivity in the East China Sea and its adjacent waters. Journal of Oceanography, 53: 41–51.

Haug G, Hughen K, Sigman D et al. 2001. Southward migration of the inter-tropical convergence zone through the Holocene. Science, 293: 1 304–1 308.

He F X. 1998. Relationship between El Niño phenomenon and the catch of navodon septentrionalis gunther in the Huanghai Sea, the East China Sea and the Tsushima Sea area. Transactions of Oceanology and Limnology, 1: 13–22. (in Chinese with English abstract)

He F X, Hong H. 1999. Variation of hydrologic structure and circulation in relation to ENSO events in the Kuroshio area in the East China Sea and its adjacent seas. Transactions of Oceanology and Limnology, 4: 16–24. (in Chinese with English abstract)

Jian Z, Wang P, Saito Y et al. 2000. Holocene variability of the Kuroshio Current in the Okinawa Trough, northwestern Pacific Ocean. Earth and Planetary Science Letters, 184: 305–319.

Kaiho K. 1994. Benthic foraminiferal dissolved-oxygen index and dissolved-oxygen levels in the modern ocean. Geology, 22: 719–722.

Kawahata H, Ohshimac H, Shimadad C et al. 2003. Terrestrial-oceanic environmental change in the southern Okhotsk Sea during the Holocene. Quaternary International, 108: 67–76.

Keefer D, Moseley M, DeFrance S D. 2003. A 38 000-year record of floods and debris flows in the region of southern Peru and its relation to El Niño events and great earthquakes. Palaeogeography, Palaeoclimatology, Palaeoecology, 194: 41–77.

Keefer D K, DeFrance S D, Moseley M E et al. 1998. Early maritime economy and El Niño events at Quebrada Tacahuay, Peru. Science, 281: 1 833–1 835.

Kim H C, Yamaguchi H, Yoo S et al. 2009. Distribution of Changjiang Diluted Water Detected by Satellite Chlorophyll- a and Its Interannual Variation during 1998–2007. Journal of Oceanography, 65: 129–135.

Labeyrie L, Cole J, Alverson K et al. 2003. The History of Climate Dynamics in the Late Quaternary. In: Alverson K, Bradley R and Pedersen T ed. Paleoclimate, Global Change and the Future. Springer, p. 33–61.

Lee H, Chao S. 2003. A climatological description of circulation in and around the East China Sea. Deep-Sea Research II, 50: 1 065–1 084.

Li C, Mu M. 2000. Relationship between East-Asian winter monsoon, warm pool situation and EVSO cycle. Chinese Science Bulletin, 45: 1 448–1 455. (in Chinese with English abstract)

Li F., 2000. Study of relationship between East Asian monsoon and Meiyu or heavy rainfall over Yangtze and Huaihe River basin in China. Journal of Chengdu Institute of Meteorology, 15: 72–77. (in Chinese with English abstract)

Liao M G, Qin Z, Zhao H. 1999. The impact of El Niño and La Niña phenomena on the global climate, Chinese climate and navigation. Navigation China, 45: 55–59.

Lie H J, Cho C H. 2002. Resent advances in understanding the circulation and hydrography of the East China Sea. Fisheries Oceanography, 11: 318–328.

Lie H J, Cho C H, Lee J H et al. 2003. Structure and eastward extension of the Changjiang River plume in the East China Sea. J. Geophys. Res., 108(C3): 3 077, doi:3010.1029/2001JC001194.

Liu K, Sun S, Jiang X. 1992. Environmental change in the Yangtze River Delta since 12 000 years BP. Quaternary Research, 38: 32–42.

Liu K B, Fearn M L. 2000a. Reconstruction of prehistoric landfall frequencies of catastrophic hurricanes in northwestern Florida from lake sediment records. Quaternary Research, 54: 238–245.

Liu Z, Kutzbach J, Wu L. 2000b. Modeling climate shift of El Niño variability in the Holocene. Geophysical Research Letters, 27: 2 265–2 268.

Liu X Q, Yin B S, Hou Y J. 2008. The dynamic of circulation and temperature. Salinity structure in the Changjiang mouth and its adjacent marine area II: major characteristics of the circulation. Oceanologia et Limnologia Sinica, 39(4): 312–320. (in Chinese with English abstract)

Lu S. 1992. Transversal Transport of Nutrient Salts in the Kuroshio Frontal Zone of the East China Sea. In: Su J, Cheng Z, Yu G eds. Proceeding of China-Japan Joint Symposium of the Cooperative Study on the Kuroshio 4. Ocean Press, Beijing, p. 134–141. (in Chinese)

Marchant M, Hebbeln D, Wefer G. 1999. High resolution planktic foraminiferal record of the last 13,300 years from the upwelling area off Chile. Marine Geology, 161: 115–128.

McGlone M S, Kershaw A P, Markgraf V. 1992. El Niño/Southern Oscillation climatic variability in Australasian and South American paleoenvironmental records. In: Dıaz H F and Markgraf V eds. El Niño—Historical and Paleoclimatic Aspects of the Southern Oscillation. Cambridge University Press, p. 435–462.

McGregor H V, Gagan M K. 2004. Western Pacific coral °18O records of anomalous Holocene variability in the El Niño-Southern Oscillation. Geophysical Research Letters, 31: L11204, doi:10.1029/GL019972.

Mortlock R, Froelich P. 1989. A simple method for the rapid determination of biogenic opal in pelagic marine sediments. Deep-Sea Research, 36: 1 415–1 426.

Mu M, Li C. 1999. ENSO signals in the interannual variability of East Asian Winter Monsoon. Part I: observed data analyses. Chinese Journal of Atmospheric Sciences, 23: 276–285. (in Chinese with English abstract)

Qiu B, Lukas R. 1996. Seasonal and interannual variability of the North Equatorial Current, the Mindanao Current, and the Kuroshio along the Pacific western boundary. Journal of Geophysical Research, 101: 12 315–12 330.

Rodbell D, Geoffrey O, David M A et al. 1999. A 15, 000-year record of El Niño-driven alluviation in southwestern Ecuador. Science, 283: 516–520.

Rosenthal Y, Broccoli A. 2004. In search of paleo-ENSO. Science, 304: 219–221.

Sandweiss D, Maasch K, Burger R et al. 2001. Variation in Holocene El Niño frequencies: climate records and cultural consequences in ancient Peru. Geology, 29: 603–606.

Sandweiss D, Richardson J, Reitz E et al. 1996. Geoarchaeological evidence from Peru for a 5 000 years B.P. onset of El Niño. Science, 273: 1 531–1 533.

Sawada K, Handa N. 1998. Variability of the path of the Kuroshio ocean current over the past 25 000 years. Nature, 392: 592–595.

Shi Y, Kong Z, Wang S. 1992. The important climatic fluctuations and events in China during the Holocene Megathermal. Science in China (Series B), 22: 1 300–1 308. (in Chinese with English abstract)

Shulmeister J, Lees B. 1995, Pollen evidence from tropical Australia for the onset of an ENSO-dominated climate at cal. 4000 BP. The Holocene, 5: 10–18.

Song C, Sun X., Saito Y. 2001. The paleoenvironmental information recorded by the pollen in the core B-3GC from the Okinawa Trough. Chinese Science Bulletin, 46: 153–158.

Stott L, Poulsen C, Lund S. 2002. Super ENSO and global climate oscillations at millennial time scales. Science, 297: 222–226.

Stuiver M, Reimer P. 1993. Extended 14C database and revised CALIB radiocarbon calibration program. Radiocarbon, 35: 215–230.

Stuiver M, Reimer P, Bard E et al. 1998. INTCAL98 Radiocarbon age calibration 24, 000–0 cal BP. Radiocarbon, 40: 1 041–1 083.

Tammy M R, Julie B G, Michael E M. 2000. El Niño-like climate teleconnections in New England during the Late Pleistocene. Science, 288: 1 039–1 042.

Tang Y X, Li X Z, Lie H J et al. 1997. Some important hydrographic structures in the Northeastern East China Sea in spring. Donghai Marine Science, 15(4): 1–10. (in Chinese with English abstract)

Tseng C, Lin C, Chen S et al. 2000. Temporal and spatial variations of sea surface temperature in the East China Sea. Continental Shelf Research, 20: 373–387.

Tudhope A, Chilcott C, McCulloch M et al. 2001. Variability in the El Niño-Southern Oscillation through a glacial-interglacial cycle. Science, 291: 1 511–1 517.

Walker D, Head M, Hancock G et al. 2000. Establishing a chronology for the last 1000 years of laminated mud accumulation at Lake Barrine, a tropical upland Maar lake, northeastern Australia. The Holocene, 10: 415–427.

Wang H. 2002. In stability of the East Asian Summer monsoon-ENSO relations, Advances in Atmospheric Sciences, 19: 1–11

Wang H, Van Strydonck M. 1997. Chronology of Holocene cheniers and oyster reefs on the coast of Bohai Bay, China. Quaternary Research, 47: 192–205.

Wang J, Saito Y, Oba T et al. 2000. High-resolution records of thermocline in the Okinawa Trough since about 10 000 yr BP. Science in China (Series D), 43: 551–560. (in Chinese with English abstract)

Webster P, Yang S. 1992. Monsoon and ENSO: Selectively Interactive Systems. Quarterly Journal of the Royal Meteorological Society, 118: 877–926.

Woodroffe C, Beech M, Gagan M. 2003. Mid-late Holocene El Niño variability in the equatorial Pacific from coral microatolls. Geophysical Research Letters, 30: 1 358, doi:10.1029/2002GL015868.

Wu S, Wei F. 2003. Analysis on the environment change in the early period of the late Holocene in Hebei Province. Geography and Geo-information Science, 19: 97–101. (in Chinese)

Xu Q, Wang Z, Liu Q. 1993. The variation of wind stress in northern Pacific and its relationship to Kuroshio meander and El Niño event. Journal of Ocean University of Qingdao, 23: 21–28. (in Chinese with English abstract)

Yu T. 1996. Distributional features and seasonal variations of temperature fronts in the East China Sea. Oceanologia et. Limnologia Sinica, 27: 12–29. (in Chinese with English abstract)

Yuan Y, Liu Y, Su J. 2001. Variability of the Kuroshio in the East China Sea during the El Niño to La Niña phenomenon of 1997 and 1998. Chinese Journal of geophysics, 44: 199–210. (in Chinese with English abstract)

Zhang D, Xue Z. 1994. Relationship between the El Niño and precipitation patterns in China since 1500 AD. Quarterly Journal of Applied Meteorology, 5: 168–175. (in Chinese with English abstract)

Zhang J, Liu S M, Ren J L et al.2007. Nutrient gradients from the eutrophic Changjiang (Yangtze River) Estuary to the oligotrophic Kuroshio waters and reevaluation of budgets for the East China Sea shelf. Prog. Oceanogr., doi:10.1016/j.pocean.2007.1004.1019.

Zhao H, Peng B, Dong M et al. 2003. Analysis of correlation between El Niño event and flood disasters in Dongting Lake area. Journal of Changde Teachers University (Natural Science Edition), 15: 68–71. (in Chinese with English abstract)

Zheng Q, Klemas V. 1982. Determination of winter temperature patterns, fronts, and surface currents in the Yellow Sea and East China Sea from satellite imagery. Remote Sensing of Environment, 12: 201–218.

Zheng X Q, Ding P X, Hu K L. 2008. Numerical analysis of characteristics of temperature-salinity distributions at the Changjiang Estuary and its adjacent areas in summer. Journal of East China Normal University (Natural Science), 6(6): 14–23. (in Chinese with English abstract)

Zhu K. 1972. The primary study on climatic changes in China since the last 5000 years. Journal of Archaeology, 1: 15–28. (in Chinese in English abstract)

Zhu S, Wang Y, Hu L. 1998. Study on climate variations in the region of Guanzhong in the historical period. Quaternary Sciences, 1: 1–11. (in Chinese with English abstract)

Zou E M, Guo B H, Tang Y X et al. 2001. An analysis of summer hydrographic features and circulation in the southern Yellow Sea and the northern East China Sea. Oceanologia et Limnologia Sinica, 32(2): 340–348. (in Chinese with English abstract)

Zou L, Ni Y. 1997. Impact of ENSO on the variability of the summer monsoon over Asian and the summer rainfall in China. Journal of Tropical Meteorology, 13: 306–314. (in Chinese with English abstract)

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