Abstract
Although the mid-late Holocene cold and dry event about 4000 years ago (the 4 ka event) has been observed almost globally, it was most prominent in terrestrial climate proxies from the lower latitudes. Here we evaluate the oceanic response to this event in terms of a Holocene sea surface temperature (SST) record reconstructed using the U K′37 index for Core B3 on the continental shelf of the East China Sea. The record reveals a large temperature drop of about 5°C from the mid-Holocene (24.7°C at 5.6 ka) to the 4 ka event (19.2°C at 3.8 ka). This mid-late Holocene cooling period in Core B3 correlated with (i) decreases in the East Asia summer monsoon intensity and (ii) the transition period with increased El Niño/Southern Oscillation activities in the Equatorial Pacific. Our SST record provides oceanic evidence for a more global nature of the mid-late Holocene climate change, which was most likely caused by a southward migration of the Intertropical Converge Zone in response to the decreasing summer solar insolation in the Northern Hemisphere. However, the large SST drop around Core B3 indicates that the mid-late Holocene cooling was regionally amplified by the initiation/strengthening of eddy circulation/cold front which caused upwelling and resulted in additional SST decrease. Upwelling during the mid-late Holocene also enhanced with surface productivity in the East China Sea as reflected by higher alkenone content around Core B3.
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An, Z., Porter, S. C., Kutzback, J. E., Wu, X., Wang, S., Liu, X., Li, X., and Zhou, W., 2000. Asynchronous Holocene optimum of the East Asian monsoon. Quaternary Science Reviews, 19(8): 743–762.
Chen, Y., Hu, D., and Wang, F., 2004. Long-term variabilities of thermodynamic structure of the East China Sea Cold Eddy in summer. Chinese Journal of Oceanology and Limnology, 22(3): 224–230.
Drysdale, R., Zanchetta, G., Hellstrom, J., Maas, R., Fallick, A., Pickett, M., Cartwright, I., and Piccini, L., 2006. Late Holocene drought responsible for the collapse of Old World civilizations is recorded in an Italian cave flowstone. Geology, 34(2): 101–104.
Dykoski, C. A., Edwards, R. L., Cheng, H., Yuan, D., Cai, Y., Zhang, M., Lin, Y., Qing, J., An, Z., and Revenaugh, J., 2005. A high-resolution, absolute-dated Holocene and deglacial Asian monsoon record from Dongge Cave, China. Earth and Planetary Science Letters, 233(1–2): 71–86.
Ge, H., Zhang, C. L., Li, J., Versteegh, G. J. M., Hu, B., Zhao, J., and Dong, L., 2014. Tetraether lipids from the southern Yellow Sea of China: Implications for the variability of East Asia Winter Monsoon in the Holocene. Organic Geochemistry, 70: 10–19.
Haug, G. H., Hughen, K. A., Sigman, D. M., Peterson, L. C., and Röhl, U., 2001. Southward migration of the Intertropical Convergence Zone through the Holocene. Science, 293(5533): 1304–1308.
He, Y., Theakstone, W. H., Zhang, Z., Zhang, D., Yao, T., Chen, T., Shen, Y., and Pang, H., 2004. Asynchronous Holocene climatic change across China. Quaternary Research, 61(1): 52–63.
Ijiri, A., Wang, L., Oba, T., Kawahata, H., Huang, C. Y., and Huang, C.-Y., 2005. Paleoenvironmental changes in the northern area of the East China Sea during the past 42 000 years. Palaeogeography, Palaeoclimatology, Palaeoecology, 219(3–4): 239–261.
Ji, J., Shen, J., Balsam, W., Chen, J., Liu, L., and Liu, X., 2005. Asian monsoon oscillations in the northeastern Qinghai-Tibet Plateau since the late glacial as interpreted from visible reflectance of Qinghai Lake sediments. Earth and Planetary Science Letters, 233(1–2): 61–70.
Jian, Z., Wang, P., Saito, Y., Wang, J., Pflaumann, U., Oba, T., and Cheng, X., 2000. Holocene variability of the Kuroshio Current in the Okinawa Trough, northwestern Pacific Ocean. Earth and Planetary Science Letters, 184(1): 305–319.
Kim, J. M., and Kennett, J. P., 1998. Paleoenvironmental changes associated with the Holocene marine transgression, Yellow Sea (Hwanghae). Marine Micropaleontology, 34(1–2): 71–89.
Kim, J. M., and Kucera, M., 2000. Benthic foraminifer record of environmental changes in the Yellow Sea (Hwanghae) during the last 15,000 years. Quaternary Science Reviews, 19(11): 1067–1085.
Koutavas, A., deMenocal, P. B., Olive, G. C., and Lynch-Stieglitz, J., 2006. Mid-Holocene El Niño-Southern Oscillation (ENSO) attenuation revealed by individual foraminifera in eastern tropical Pacific sediments. Geology, 34(12): 993–996.
Levitus, S., and Boyer, T. P., 1994. World Ocean Atlas 1994, vol. 4, Temperature. U. S. Department of Commer., Washington, D. C.
Li, G. X., Sun, X. Y., Liu, Y., Bickert, T., and Ma, Y. Y., 2009. Sea surface temperature record from the north of the East China Sea since late Holocene. Chinese Science Bulletin, 54(23): 4507–4513.
Li, T., Liu, Z., Hall, M. A., Berne, S., Saito, Y., Cang, S., and Cheng, Z., 2001. Heinrich event imprints in the Okinawa Trough: Evidence from oxygen isotope and planktonic foraminifera. Palaeogeography, Palaeoclimatology, Palaeoecology, 176(1–4): 133–146.
Lin, Y. S., Wei, K. Y., Lin, I. T., Yu, P. S., Chiang, H. W., Chen, C. Y., Shen, C. C., Mii, H. S., and Chen, Y. G., 2006. The Holocene Pulleniatina Minimum Event revisited: Geochemical and faunal evidence from the Okinawa Trough and upper reaches of the Kuroshio current. Marine Micropaleontology, 59(3–4): 153–170.
Liu, J. P., Milliman, J. D., Gao, S., and Cheng, P., 2004. Holocene development of the Yellow River subaqueous delta, North Yellow Sea. Marine Geology, 209(1–4): 45–67.
Liu, J. P., Xu, K. H., Li, A. C., Milliman, J. D., Velozzi, D. M., Xiao, S. B., and Yang, Z. S., 2007. Flux and fate of Yangtze River sediment delivered to the East China Sea. Geomorphology, 85(3–4): 208–224.
Müller, P. J., Kirst, G., Ruhland, G., von Storch, I., and Rosell-Melé, A., 1998. Calibration of the alkenone paleotemperature index U K′37 based on core-tops from the eastern South Atlantic and the global ocean (60°N–60°S). Geochimica et Cosmochimica Acta, 62(10): 1757–1772.
Mayewski, P. A., Rohling, E. E., Stager, J. C., Karlen, W., Maasch, K. A., Meeker, L. D., Meyerson, E. A., Gasse, F., van Kreveld, S., Holmgren, K., Lee-Thorp, J., Rosqvist, G., Rack, F., Staubwasser, M., Schneider, R. R., and Steig, E. J., 2004. Holocene climate variability. Quaternary Research, 62(3): 243–255.
Staubwasser, M., Sirocko, F., Grootes, P. M., and Segl, M., 2003. Climate change at the 4.2 ka BP termination of the Indus valley civilization and Holocene south Asian monsoon variability. Geophysical Research Letters, 30(8): 1425.
Staubwasser, M., and Weiss, H., 2006. Holocene climate and cultural evolution in late prehistoric-early historic West Asia. Quaternary Research, 66(3): 372–387.
Su, J. L., 2005. Hydrography of the Coastal Oceans Near China Ocean Press, Beijing, 174–181 (in Chinese).
Wang, L., Sarnthein, M., Erlenkeuser, H., Grimalt, J., Grootes, P., Heilig, S., Ivanova, E., Kienast, M., Pelejero, C., and Pflaumann, U., 1999. East Asian monsoon climate during the Late Pleistocene: high-resolution sediment records from the South China Sea. Marine Geology, 156(1–4): 245–284.
Wang, L. B., Yang, Z. S., Zhang, R. P., Fan, D. J., Zhao, M. X., and Hu, B. Q., 2011. Sea surface temperature records of core ZY2 from the central mud area in the South Yellow Sea during last 6200 years and related effect of the Yellow Sea Warm Current. Chinese Science Bulletin, 56(15): 1588–1595.
Wanner, H., Beer, J., Bütikofer, J., Crowley, T. J., Cubasch, U., Flückiger, J., Goosse, H., Grosjean, M., Joos, F., Kaplan, J. O., Küttel, M., Müller, S. A., Prentice, I. C., Solomina, O., Stocker, T. F., Tarasov, P., Wagner, M., and Widmann, M., 2008. Mid- to Late Holocene climate change: An overview. Quaternary Science Reviews, 27(19–20): 1791–1828.
Wu, W., and Liu, T., 2004. Possible role of the ‘Holocene Event 3’ on the collapse of neolithic cultures around the Central Plain of China. Quaternary International, 117(1): 153–166.
Xiang, R., Yang, Z., Saito, Y., Fan, D., Chen, M., Guo, Z., and Chen, Z., 2008. Paleoenvironmental changes during the last 8400 years in the southern Yellow Sea: Benthic foraminiferal and stable isotopic evidence. Marine Micropaleontology, 67(1–2): 104–119.
Xiao, J., Wu, J., Si, B., Liang, W., Nakamura, T., Liu, B., and Inouchi, Y., 2006. Holocene climate changes in the monsoon/arid transition reflected by carbon concentration in Daihai Lake of Inner Mongolia. Holocene, 16(4): 551–560.
Xing, L., Jiang, Y., Yuan, Z., Zhang, H., Li, L., Zhou, L., and Zhao, M., 2013. Holocene temperature records from the East China sea mud area southwest of the Cheju Island reconstructed by the U K′37 and TEX86 paleothermometers. Journal of Ocean University of China, 12(4): 599–604.
Yancheva, G., Nowaczyk, N. R., Mingram, J., Dulski, P., Schettler, G., Negendank, J. F. W., Liu, J., Sigman, D. M., Peterson, L. C., and Haug, G. H., 2007. Influence of the intertropical convergence zone on the East Asian monsoon. Nature, 445(7123): 74–77.
Yang, S., and Youn, J. S., 2007. Geochemical compositions and provenance discrimination of the central south Yellow Sea sediments. Marine Geology, 243(1–4): 229–241.
Yuan, Z., Xing, L., Li, L., Zhang, H., Xiang, R., and Zhao, M., 2013. Biomarker records of phytoplankton productivity and community structure changes during the last 14000 years in the mud area southwest off Cheju Island, East China Sea. Journal of Ocean University of China, 12(4): 611–618.
Zhao, M., Beveridge, N. A. S., Shackleton, N. J., Sarnthein, M., and Eglinton, G., 1995. Molecular stratigraphy of cores off northwest Africa: Sea surface temperature history over the last 80 ka. Paleoceanography, 10(3): 661–675.
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Zhao, M., Ding, L., Xing, L. et al. Major mid-late Holocene cooling in the East China Sea revealed by an alkenone sea surface temperature record. J. Ocean Univ. China 13, 935–940 (2014). https://doi.org/10.1007/s11802-014-2641-2
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DOI: https://doi.org/10.1007/s11802-014-2641-2