Evolution of sedimentation on the continental slope of the Kronotskii Peninsula (Eastern Kamchatka) over the last 20 ka

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• 作者：M. A. Levitan ; T. G. Kuz’mina ; V. L. Luksha…
• 刊名：Lithology and Mineral Resources
• 出版年：2015
• 出版时间：July 2015
• 年：2015
• 卷：50
• 期：4
• 页码：249-269
• 全文大小：2,766 KB
• 参考文献：Bigg, G.R., Clark, C.D., and Hughes, A.L.C., A last glaciation sheet on the Pacific Russian coast and catastrophic change arising from coupled ice-volcanic interaction, Earth Planet. Sci. Lett., 2008, vol. 265, pp. 559-70.View Article
  Biscaye, P., Mineralogy and sedimentation of recent deepsea clay in the Atlantic Ocean and adjacent seas and oceans, Geol. Soc. Am. Bull., 1965, vol. 76, pp. 803-32.View Article
  Diekmann, B., Fütterer, D.K, Grobe, H., et al. Terrigenous sediment supply in the polar to temperate South Atlantic: landocean links of environmental changes during the late Quaternary, The South Atlantic in the late Quaternary: reconstruction of material budgets and current systems, Wefer, G., Mulitza, S., and Ratmeyer, Y., Eds., Berlin: Springer, 2003.
  Fairbanks, R.G., A 17,000-year glacio-eustatic sea level record: influence of glacial melting rates on the Younger Dryas event and deep ocean circulation, Nature, 1989, vol. 342, pp. 637-42.View Article
  Frolov, V.T., Geneticheskaya tipizatsiya morskikh otlozhenii (Genetic Typification of Marine Sediments), Moscow: Nauka, 1984.
  Gallego-Torres, D., Martinez-Ruiz, F., Paytan, A., et al., Pliocene-Holocene evolution of depositional conditions in the eastern Mediterranean: role of anoxia vs. productivity at time of sapropel deposition, Palaeogeogr., Palaeoclimat., Palaeoecol., 2004, vol. 209, pp. 424-39.
  Gorbarenko, S., Stable isotope and lithological evidence of late-glacial and Holocene oceanography of the north-western Pacific and its marginal seas, Quat. Res., 1996, vol. 46, pp. 230-50.View Article
  Gorbarenko, S.A., Harada, N., Malakhov, M.I., et al., Orbital and millennial-scale environmental and sedimentological changes in the Okhotsk Sea during the last 350 kyr, Gl. Planet. Change, 2010, vol. 72, pp. 79-5.View Article
  Keigwin, L.D., Glacialage hydrography of the far north-west Pacific Ocean, Paleoceanography, 1998, vol. 13, no. (4), pp. 323-39.View Article
  Khotinskii, N.A., Golotsen severnoi Evrazii (Holocene in North Eurasia), Moscow: Nauka, 1977.
  Khubunaya, S.A., Formational affiliation of Cretaceous and Paleogene basalts of the Kronotskii Eocene basalts of the Kamchatka Peninsulas (eastern Kamchatka) based on geochemical properties, Extended Abstract of PhD (Geol.–Miner.) Dissertation, Moscow: Geochem. Inst. Russ. Acad. Sci., 1983.
  Levitan, M.A., Lavrushin, Yu.A., and Stein, R., Ocherki istorii osadkonakopleniya v Severnom Ledovitom okeane i moryakh Subarktiki v poslednie 130 tys. let (Essays on the History of Sedimentation in the North Arctic Ocean and Subarctic Seas during the Last 130 ka), Moscow: GEOS, 2007.
  Levitan, M.A., Roshchina, I.A., and Tolmacheva, A.V., Geochemical Features of Sediments on the Continental Slope of the Weddell Sea and Their Paleoceano-graphic Interpretation, Lithol. Miner. Resour., 2008, no. 2, pp. 111-24.View Article
  Levitan, M.A., Kuz’mina, T.G., Luksha, V.L., et al., Late Pleistocene Sedimentation History of the Shirshov Ridge, Bering Sea, Geochem. Int., 2013, no. 3, pp. 173-04.View Article
  Malakhov, M.I., Gorbarenko, S.A., Nürnberg, D., et al., Variations in the relative strain of the geomagnetic field in bottom sediments of the Bering Sea and SW Pacific during the last 380 ka, in Kvarter vo vsem ego mnogoobrazii (Quaternary in Its Entire Diversity), Kol’ka, V.V., Ed., Apatity, 2011, pp. 61-3.
  Matishov, G.G., Dno okeana v lednikovyi period (Ocean Floor in the Glacial Period), Moscow: Nauka, 1980.
  Max, L., Riethdorf, J.-R., Tiedemann, R., et al., Sea surface temperature variability and seaice extent in the subarctic northwest Pacific during the past 15,000 years, Paleoceanography, 2012, vol. 27, p. A3213.View Article
  Müller, C., Rekonstruktion der Pal?o-Umweltbedingungen am Laptev-See-Kontinentalalrand w?hrend der Beiden Letzten Glazial/Interglazial-Zyclen anhand Sedimentologischer und Mineralogischer Untersuchungen, Ber. Polarforsch., 1999, no. 328.
  Nürnberg, D. and Tiedemann, R., Environmental change in the Sea of Okhotsk during the last 1.1 million years, Paleoceanography, 2004, vol. 19, PA4011.
  Nürnberg, D. and Tiedemann, R., Sediment Sampling, in SO201-KALMAR Leg 2 Cruise Rep., Dullo, C., Baranov, B., and van den Bogaard, C. Eds., 2009, Kiel: IFM-GEOMAR, pp. 67-4.
  Okazaki, Y., Timmermann, A., Menviel, L., et al., Deepwater formation in the North Pacific during the last glacial termination, Science, 2010, vol. 329, no. 5988, pp. 200-04.View Article
  Ronov, A.B., Yaroshevskii, A.A., and Migdisov, A.A., Khimicheskii sostav zemnoi kory i geokhimicheskii balans glavnykh elementov (Chemical Composition of the Earth’s Crust and Geochemical Balance of Major Elements), Moscow: Nauka, 1990.
  Sancetta, C., Heusser, L., Labeyrie, L., et al., Wisconsin-Holocene paleoenvironment of the Bering Sea: evidence from diatoms, pollen, oxygen isotopes and clay minerals, Mar. Geol., 1985, vol. 62, pp. 55-8.View Article
  Sarnthein, M., Stattegger,
• 作者单位：M. A. Levitan (1)
  T. G. Kuz’mina (1)
  V. L. Luksha (2)
  I. A. Roshchina (1)
  K. V. Syromyatnikov (1)
  L. Max (3)
  D. Nürnberg (4)
  J.-R. Riethdorf (4)
  
  1. Vernadsky Institute of Geochemistry and Analytical Chemistry, Russian Academy of Sciences, ul. Krasikova 19, Moscow, 119991, Russia
  2. Faculty of Geology, Lomonosov Moscow State University, Moscow, 119991, Russia
  3. Alfred Wegener Institute for Polar and Marine Research, Columbusstrasse, D-27568, Bremerhaven, Germany
  4. IFM-GEOMAR, Leibnitz-Institute für Meereswissenschaften, Wischhofstr. 1-3, D-24148, Kiel, Germany
  
• 刊物类别：Earth and Environmental Science
• 刊物主题：Earth sciences
  Mineral Resources
  Mineralogy
  Sedimentology
  Russian Library of Science
  
• 出版者：MAIK Nauka/Interperiodica distributed exclusively by Springer Science+Business Media LLC.
• ISSN：1608-3229

文摘

Different genetic types of marine sediments that were deposited on the continental slope of the Kronotskii Peninsula with the rate of several tens of centimeters per thousand years during the last 20 ka have been investigated. It is established that their lithological, mineral, and chemical compositions were determined by climate changes.