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Changes of Clay Mineral Assemblages in the Northern Part of the Aleutian Basin in the Bering Sea during the Last Glacial Period
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 Title & Authors
Changes of Clay Mineral Assemblages in the Northern Part of the Aleutian Basin in the Bering Sea during the Last Glacial Period
Kim, Sung-Han; Cho, Hyen-Goo; Khim, Boo-Keun;
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 Abstract
Clay mineral assemblages of core PC25A collected from the northern part of the Aleutian Basin in the Bering Sea were examined in order to investigate changes in sediment provenances and transport pathways. Ages of core PC25A were determined by both Last Appearance Datum of radiolaria (L. nipponica sakaii; ) and age control points obtained by the correlations of , and laminated sediment layers with the adjacent core PC23A, whose ages are well constrained. The corebottom age of core PC25A was calculated to be about 57,600 yr ago and core-top might be missing during coring execution. Average contents of smectite, illite, kaolinite, and chlorite during the last glacial period are 11% (5~24%), 47% (36~58%), 13% (9~19%), and 29% (21~40%), respectively. Clay mineral assemblages of the last glacial period are characterized by higher illite and lower smectite contents than those of core MC24 representing the modern values. Illite-rich clay sediments during the warm Early Holocene were transported from the northern part of Alaska continent (Province 1) through the ice-melt waters. During the deglacial period (Blling-Allrod) of MIS 2, clay-sized particles seemed to be also transported by ice-melt waters mainly from Province 2 and Province 3 located farther south than Province 1. Higher smectite content during the Last Glacial Maximum is attributed to increased amounts of clay particles from the adjacent Alaska Peninsula (Province 4). From the early to the middle MIS 3, illite and smectite contents decreased, whereas chlorite content increased. With the low sea level standing during MIS 3 the supply of clay sediments from Province 2 and Province 3 was most likely intensified. Changes in clay mineral assemblages of core PC25A located in the northern part of the Aleutian Basin in the Bering Sea are closely related to the change of surface current system caused by sea level variation during the last glacial period.
 Keywords
clay mineral;provenance;surface current;sea level;glacial period;Bering Sea;
 Language
Korean
 Cited by
1.
Clay mineral distribution and provenance in the Heuksan mud belt, Yellow Sea, Geo-Marine Letters, 2015, 35, 6, 411  crossref(new windwow)
 References
1.
김성한, 김부근, 신혜선, Uchida, M., Itaki, T., and Ohkushi, K. (2009) 베링해 중부 지역의 마지막 빙하 기 이후 고생산성의 고해상 변화. 한국해양학회지, 14, 133-144.

2.
Biscaye, P.E. (1964) Distribution between kaolinite and chlorite in recent sediments by x-ray diffraction. Am. Mineral., 49, 1281-1289.

3.
Biscaye, P.E. (1965) Mineralogy and sedimentation of recent deep-sea clay in the Atlantic Ocean and Adjacent Seas and Oceans. Geol. Soc. Am. Bull., 76, 803-832. crossref(new window)

4.
Bouquillon, A., France-Lanord, C., Michard, A., and Tiercelin, J.J. (1990) Sedimentology and isotopic chemistry of the Bengal Fan sediments: the denudation of the Himalaya. In: Cocharn, J.R., Stow, D.A.V., et al. (eds.), Proc. ODP: Sci. Results, Ocean Drilling Program Vol. 116, ODP: College Station, TX, 43-58.

5.
Brindley, G.W. (1980) Order-disorder in clay mineral structures. In: Brindley, G.W. and Brown, G. (eds.), Crystal structures of clay minerals and their X-ray identification. Mineralogical Society Monograph, 5, 125-195.

6.
Brunelle, B.G., Sigman, D.M., Cook, M.S., Keigwin, L.D., Haug, G.H., Plessen, B., Schettler, G., and Jaccard, S.L. (2007) Evidence from diatom-bound nitrogen isotopes for subarctic Pacific stratification during the last ice age and a link to North Pacific denitrification changes. Paleoceanography, 22, PA1215, doi:10.1029/ 2005PA001205.

7.
Brunton, G.D. (1955) Vapour pressure glycolation of oriented clay minerals. Am. Mineral., 40, 803-832.

8.
Chamley, H. (1989) Clay Sedimentology. Springer-Verlag, Berlin, 623p.

9.
Chamley, H. (1997) Clay mineral sedimentation in the ocean. In: Paquet, G. and Clauer, N. (eds), Soils and sediments, Mineralogy and Geochemistry. Springer, 269-302.

10.
Coachman, L.K., Aagaard, K., and Tripp, R.B. (1975) Bering Strait: The Regional Oceanography. University of Washington Press, Seattle, 172p.

11.
Cook, M.S., Keigwin, L.D., and Sancetta, C.A. (2005) The deglacial history of surface and intermediate water of the Bering Sea. Deep-Sea Res. II, 52, 2163-2173. crossref(new window)

12.
Damiani, D., Giorgetti, G., and Turbanti, I.M. (2006) Clay mineral fluctuations and surface textural analysis of quartz grains in Pliocene-Quaternary marine sediments from Wilkes Land continental rise (East- Antarctica): Paleoenvironmental significance. Mar. Geol., 226, 281-295. crossref(new window)

13.
Deer, W.A., Howie, R.A., and Zussaman, J. (1966) An introduction to the rock forming minerals. Longmans, London, 528p.

14.
Diekmann, B., Kuhn, G., Mackensen, A., Petschick, R., Futterer, D.K., Gersonde, R., Riuhlemann, C., and Niebler, H.S. (1999) Kaolinite and chlorite as tracers of modern and late Quaternary deep water circulation in the South Atlantic and the adjoining Southern Ocean. In: Fischer, G. and Wefer, G. (eds.), Use of Proxies in Paleoceanography: examples from the South Atlanic. Springer-Verlag, Berlin, Heidelberg, 1-29.

15.
Ehrmann, W.U., Melles, M., Kuhn, G., and Grobe, H. (1992) Significance of clay mineral assemblages in the Antarctic Ocean. Mar. Geol., 107, 249-273. crossref(new window)

16.
Fairbanks, R.G. (1989) A 17,000-year glacioeustatic sealevel record: influence of glacial melting rates on the Younger Dryas event and deep-ocean circulation. Nature, 342, 637-642. crossref(new window)

17.
France-Lanord, C., Derry, L., and Michard, A. (1993) Evolution of the Himalaya since Miocene times: isotopic and sedimentological evidence from the Bengal Fan. In: Treloar, P.J. and Searle, M. (eds.), Himalayan Tectonics. Spec. Publ. Geol. Soc. London, 7, 603-621.

18.
Gingele, F.X. (1996) Holocene climatic optimum in Southwest Africa - evidence from the marine clay mineral record. Paleogeogr. Palaeoclimatol. Palaeoecol. 122, 77-87. crossref(new window)

19.
Gorbarenko, S.A., Basov, I.A., Chekhovskaya, M.P., Southon, J., Khusid, T.A., and Artemova, A.V. (2005) Orbital and millennium scale environmental changes in the southern Bering Sea during the last glacial- Holocene: geochemical and paleontological evidence. Deep-Sea Res. II, 52, 2174-2185. crossref(new window)

20.
Grim, R.E. (1968) Clay Mineralogy. McGraw-Hill, New York, 596p.

21.
Itaki, T., Uchida, M., Kim, S., Shin, H.S., Tada, R., and Khim, B.K. (2009) Late Pleistocene stratigraphy and paleoceanographic implications in northern Bering Sea slope sediments: evidence from the radiolarian species Cycladophora davisiana. Jour. Quat. Sci., 24, 856-865. crossref(new window)

22.
Katsuki, K. and Takahashi, K. (2005) Diatoms as paleoenvironmental proxies for seasonal productivity, sea-ice and surface circulation in the Bering Sea during the late Quaternary. Deep-Sea Res. II, 52, 2110-2130. crossref(new window)

23.
Keigwin, L.D., Donnelly, J.P., Cook, M.S., Driscoll, N.W., and Brigham-Grette, J. (2006) Rapid sea-level rise and Holocene climate in the Chukchi Sea. Geology, 34, 861-864. crossref(new window)

24.
Khim, B.K. and Park, Y.A. (1992) Smectite as a possible source-indicative clay mineral in the Yellow Sea. Geo-Mar. Lett., 12, 228-231. crossref(new window)

25.
Morley, J.J., Hays, J.D., and Robertson, J.H. (1982) Stratigraphic framework for the late Pleistocene in the northwest Pacific Ocean. Deep-Sea Res., 29, 1485-1499. crossref(new window)

26.
Naidu, A.S., Creager, J.S., and Mowatt, T.C. (1982) Clay mineral dispersal patterns in the north Bering and Chukchi Seas. Mar. Geol., 47, 1-15. crossref(new window)

27.
Naidu, A.S. and Mowatt, T.C. (1983) Sources and dispersal patterns of clay minerals in surface sediments from the continental-shelf areas off Alaska. Geol. Soc. Am. Bull., 94, 841-854. crossref(new window)

28.
Niebauer, H.J., Bond, N.A., Yakunin, L.P., and Plotnikov, V.V. (1999) An update on the climatology and sea ice of the Bering Sea. In: Loughlin, T.R. and Ohtani, K. (eds.), Dynamics of the Bering Sea, Univ. Alaska Sea Grant, Fairbanks, 29-59.

29.
Park, Y.A. and Khim, B.K. (1992) Origin and dispersal of the recent clay minerals in the Yellow Sea. Mar. Geol., 104, 205-213. crossref(new window)

30.
Sancetta, C., Heusser, L., Labeyrie, L., Naidu, S.A., and Robinson, S.W. (1985) Wisconsin-Holocene paleoenvironment of the Bering Sea: evidence from diatoms, pollen, oxygen isotopes and clay minerals. Mar. Geol., 62, 55-68.

31.
Singer, A. (1984) The paleoclimatic interpretation of clay minerals in sediments - a review. Earth Sci. Rev., 21, 251-293. crossref(new window)

32.
Siroko, F. and Lange, H. (1991) Clay accumulation rates in the Arabian Sea during the late Quaternary. Mar. Geol., 97, 105-119. crossref(new window)

33.
Stabeno, P.J., Schumacher, J.D., and Ohtani, K. (1999) The physical oceanography of the Bering Sea. In: Loughlin, T.R. and Ohtani, K. (eds.), Dynamics of the Bering Sea, Univ. Alaska Sea Grant, Fairbanks, 1-28.

34.
Stephan, S., Hanebuth, T.J.J., Vogt, C., and Stattegger, K. (2008) Sea level induced variations in clay mineral composition in the southwestern South China over the past 17,000 yr. Mar. Geol., 250, 199-210. crossref(new window)

35.
Stokke, P.R. and Carson, B. (1973) Variation in clay mineral X-ray diffraction results with the quantity of sample mounted. Jour. Sediment. Petrol., 43, 957-964.

36.
Thamban, M., Rao, V.P., and Schneider, R.R. (2002) Reconstruction of late Quaternary monsoon oscillations based on clay mineral proxies using sediment cores from the western margin of India. Mar. Geol., 186, 527-539. crossref(new window)

37.
Trentesaux, A., Liu, Z., Colin, C., Clemens, S.C., Boulay, S., and Wang, P. (2003) Pleistocene paleoclimatic cyclicity of southern China: clay mineral evidence recorded in the South China Sea (ODP Site 1146). In: Prell, W.L. Wang, P., Blum, P., and Clemens, S., (eds.), Proc. ODP Sci. Res., Vol. 184, 1-10 (online).

38.
Vanderaveroet, P., Averbuch, O., Deconinck, J.F., and Chamley, H. (1999) A record of glacial/interglacial alternations in Pleistocene sediments off New Jersey expressed by clay mineral, grain size and magnetic susceptibility data. Mar. Geol., 159, 79-92. crossref(new window)