Abstract
To investigate the relationship between volcanic activity and sediment record on regional and temporal scales, 158 surface sediment samples were collected from the East China Sea Shelf to the northern Okinawa Trough (OT), and two cores recovered in the northern and southern OT, respectively. Mineralogy, grain-size, and geochemical analyses of those samples show that: 1) volcanic glass, volcanic-type pyroxene, hypersthenes, and magnetite increase in sediment influenced by volcanic activity; 2) sediment grain sizes (and also silt content) increase in ash layers; and 3) the contents of Na2O and Zr are higher, while terrigenous elements, e.g., TFe2O3 and K2O, and biogenous compositions, e.g., CaO and Sr, are relatively lower in ash layers than those of non-ash layers. The distribution of volcanic ash has three distinguishing characteristics: 1) volcanic ash is more abundant in the northern and central OT than the southern OT; 2) volcanic ash increases from continental shelf to the trough; 3) the sediment during the last 12 000 a suggests stronger volcanic events than during 15 000–12 000 a. The eruptive locations, frequency, and volume of calderas are among the most important factors controlling the distributions of volcanic ash. In addition, the main Kuroshio warm current that extends northward probably impeded the diffusion of volcanic ash to the west and south in the OT. However, a southward current probably carried some volcanic ash toward southern OT.
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References
Aoki K. 2008. Revised age and distribution of ca. 87 ka Aso-4 tephra based on new evidence from the northwest Pacific Ocean. Quatern. Int., 178: 100–118.
Arai F, Oba T, Kitazato H. 1981. Late Quaternary tephrochronology and palaeo-oceanography of the sediments of the Japan Sea. Quatern. Res. Jpn., 20: 209–230.
Cang S X, Qin Y S, Xiang R. 1999. Paleoenvironmental evolution of the Bohai Sea and the Yellow Sea: Millennial-scale changes of the large meanders of kuroshio and ENSO. Kor. J. Quatern. Res., 55–63.
Chen L R, Zhai S K, Shen S X. 1993. Isotopic characteristics and chronological dating of pumice in Okinawa Trough. Sci. Chin, Ser. B., 24(3): 324–329. (in Chinese with English abstract)
Gao S, Jia J J. 2002. Grain Size Characteristics of Core Top Sediment in the Central Northern Okinawa Trough and Adjacent Continental Slope. In: Gao S, Li J B, eds. The Formation and Evolution of Chinese Marginal Sea. China Ocean Press, Beijing, China. p.125–139. (in Chinese)
Gao S L, Wang H Y, Xin C Y. 1998. Cause of formation of sediment and sedimentary environment in the central and west margin of the Okinawa Trough. J. Oceanogr. Huanghai and Bohai Seas, 16(3): 39–46. (in Chinese with English abstract)
Hans-Joachim W-A, Lackschewitz K S. 2003. Chemical composition, distribution, and origin of silicic volcanic ash layers in the Greenland-Iceland-Norwegian Sea: explosive volcanism from 10 to 300 ka as recorded in deep-sea sediments. Mar. Geol., 193(3-4): 273–293.
Jian Z, Wang P X, Satio Y, et al. 2000. Holocene variability of the Kuroshio Current in the Okinawa Trough, northwestern Pacific Ocean. Earth Planet. Sci. Lett., 184(1): 305–319.
Jiang F Q, Li A C. 2002. Geochemical characteristics and their implications to provenance and environment of surface sediments from the southern Okinawa Trough. Acta Sedimentologica Sinica, 20(4): 680–686. (in Chinese with English abstract)
Kamata H, Hayashida A, Danhara T. 1997. Identification of a pair of co-ignimbrite ash and underlying distal plinian ash in the Early Pleistocene widespread tephra in Japan. J. Volcanol. Geotherm. Res., 78(1–2): 51–64.
Kawahata H, Ohshima H. 2004. Vegetation and environmental record in the northern East China Sea during the late Pleistocene. Global Planet. Change, 41(3–4): 251–273.
Letouzey J, Kimura M. 1986. The Okinawa Trough: Genesis of a back-arc basin developing along a continental margin. Tectonophysics, 125(1–3): 209–230.
Li B H, Zhao Q H, Wang Y J. 1997. Planktonic foraminifera and paleo-oceanography events in the southern Okinawa Trough since the last 20ka. Acta Oceanologica Sinica, 19(4): 90–98. (in Chinese with English abstract)
Li T G, Li A C, Chen L R et al. 2002. Environmental response of volcanic activity in the Okinawa Trough since 150 ka B. P. In: Gao S, Li J B, eds. Formation and Evolution of China Marginal Sea. China Ocean Press, Beijing, China. p.118–124. (in Chinese)
Li T G, Liu Z X, Hall M et al. 2001. Heinrich event imprints in the Okinawa Trough: evidence from oxygen isotope and planktonic foraminifera. Palaeogeogr. Palaeoclimatol. Palaeoecol, 176(1–4): 133–146.
Liu Y G, Cao D L, Zhang D Y. 2007. Holocene tephra deposits in the northern Okinawa Trough. Adv. Mar. Sci., 25(1): 34–45. (in Chinese with English abstract)
Liu Y G, Meng X W, Li T G. 2003. The elementary stratigraphy of the middle Okinawa Trough since the last deglaciation. Acta Oceanologica Sinica, 25(4): 50–58 (in Chinese, with English abstract).
Liu Z X, Li P Y, Li T. 2001. Discussion on the paleoclimatic events and cause in the Okinawa Trough during 50ka BP. Chin. Sci. Bull, 46(2): 153–159.
Machida H, 1999. The stratigraphy, chronology and distribution of distal marker-tephras in and around Japan. Global Planet. Change, 21(1–3): 71–94.
Machida H, Arai F. 1983. Extensive ash falls in and around the sea of Japan from large late quaternary eruptions. J. Volcanol. Geotherm. Res., 18(1–4): 151–164.
Machida H, Arai F. 1994. Implications of the time marker Aso-3 tephra to the significant lowering of sea level in the marine isotope stage 5d. J. Geography. Jpn., 103: 749–759.
Meng X W, Wang Y J, Lu C G. 1997. Precincts of sediments with different element associations and the sources indications in the central Okinawa Trough. Mar. Geol. Quatern. Geol., 17(3): 37–43. (in Chinese with English abstract)
Nakada M, Yokose H. 1992. Ice age as a trigger of active Quaternary volcanism and tectonism. Tectonophysics, 212: 321–329.
Park M H, Kim I S, Shin J B. 2003. Characteristics of the late Quaternary tephra layers in the East/Japan Sea and their new occurrences in western Ulleung Basin sediments. Mar. Geol., 202(3–4): 135–142.
Park Y A. 1992. The changes of sea level and climate during the late Pleistocene and Holocene in the Yellow Sea Region. Kor. J. Quatern. Res., 6: 13–19.
Qin Y S, Zhao Y Y, Chen L R. 1987. Geology of East China Sea. Science Press, Beijing, China. p.250–255.
Sibuet J C, Letouzey J, Barbier F. 1987. Back arc extension in the Okinawa Trough. J. Geophys. Res., 92: 14 041–14 063.
Sun Y B, Gao S, Li J. 2003. Preliminary analysis of grain-size populations with environmentally sensitive terrigenous components in marginal sea setting. Chin. Sci. Bull., 48(2): 184–187.
Takai A, Shibuya H, Yoshihara A et al. 2002. Paleointensity measurements of pyroclastic flow deposits co-born with widespread tephras in Kyushu Island, Japan. Phys. Earth Planet. In., 133(1–4): 159–179.
Ujiie H, Hatakeyama Y, Gu X X et al. 2001. Upward decrease of organic C/N ratios in the Okinawa Trough cores: proxy for tracing the post-glacial retreat of the continental shore line. Palaeogeogr. Palaeoclimatol. Palaeoecol, 165(1–2): 129–140.
Wang S L, Arthur Chen C T, Hong G H et al. 2000. Carbon dioxide and related parameters in the East China Sea. Cont. Shelf Res., 20(4-5): 525–544.
Wu Y H, Chen Z B, Shi X F. 2004. Stratigraphic and carbonate sediment characteristics of core CSH1 from the northern Okinawa Trough. Adv. Mar. Sci., 22(2): 163–169. (in Chinese with English abstract)
Xu X, Oda M. 1999. Surface-water evolution of the eastern East China Sea during the last 36,000 years. Mar. Geol., 156(1–4): 285–304.
Zhai S K, Chen L R, Zhang H Q. 2001. Magmatism and Seafloor Hydrothermal Activity in the Okinawa Trough. China Ocean Press, Beijing, China. p. 1–98. (in Chinese)
Zhai S K, Zhang J, He L B et al. 1997. Study on geochemistry of seafloor surface sediments in the North Okinawa Trough. Acta Sedimentologica Sinica, 15(suppl): 8–15. (in Chinese with English abstract)
Zhao Y Y, Yan M. 1994. Geochemistry of Sediment of the China Shelf Sea. Science Press, Beijing, China. p. 1–200. (in Chinese)
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Supported by the Pilot Project of the National Knowledge Innovation Program of the Chinese Academy of Science (No. KZCX2-YW-221), the National Natural Science Foundation of China (No. 40506016, 90411014 and 40976026), and National Basic Research Program of China (No. 2007CB815903).
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Jiang, F., Li, A. & Li, T. Sedimentary response to volcanic activity in the Okinawa Trough since the last deglaciation. Chin. J. Ocean. Limnol. 28, 171–182 (2010). https://doi.org/10.1007/s00343-010-9272-2
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DOI: https://doi.org/10.1007/s00343-010-9272-2