Abstract
Riverine water and sediment discharge to the Arctic Ocean is among the most important parameters influencing Arctic climate. It is clear that the evaluation of Arctic paleoclimate requires information on the paleodischarge of major rivers entering the sedimentation basin. Presently, the water discharge of the Ob River accounts for about 12% of the total input of river water into the Arctic Ocean. During the investigation of the Kara Sea in the framework of the Russian-German SIRRO Project, the history of Yenisei discharge received much attention in a number of publications. This paper presents the results of lithological and geochemical investigations with application to the Holocene discharge of the Ob River. Qualitative (SiO2, Al2O3, K2O, and some modules) and quantitative (sedimentation rates and absolute masses of sedimentary material) parameters were used to characterize the history of the Ob sediment discharge. It was shown that the investigated paleochannels of the Ob were initiated at the Pleistocene-Holocene boundary, and during the first half of the Holocene, the river discharge decreased irregularly with decreasing age of sediments. The observed maxima are in fairly good agreement with the data for the Yenisei. We proposed a hypothesis on the influence of glacioisostatic movements in the marginal region of the former Kara ice sheet of late Valdai age on the cessation of marine-fluvial glaciation in the paleochannels of Ob and Yenisei in the periphery of the Ob-Yenisei shoal.
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References
L. P. Bobylev, K. Ya. Kondratyev, and O. M. Johannessen, Arctic Environment Variability in the Context of Global Change (Springer, Berlin, 2003).
R. Stein, “Arctic Paleo-River Discharge (APARD),” Ber. Polarforsch., No. 279 (1998).
V. V. Gordeev, J. M. Martin, I. S. Sidorov, and M. V. Sidorova, “A Reassessment of the Eurasian River Input of Water, Sediment, Major Elements, and Nutrients to the Arctic Ocean,” Am. J. Sci. 296, 664–691 (1996).
M. A. Levitan, M. V. Burtman, L. L. Demina, et al., “History of Holocene Sedimentation in the Southern Kara Sea,” Litol. Polezn. Iskop, No. 6, 651–666 (2004) [Lithol. Min. Res. 39, 566–579 (2004)].
M. A. Levitan, M. V. Burtman, L. L. Demina, et al., “Facies Variability of Surface Sediments from the Ob-Yenisei Shoal and the Ob and Yenisei Estuaries,” Litol. Polezn. Iskop, No. 5, 472–484 (2005) [Lithol. Min. Res. 39, 408–419 (2005)].
K. Dittmers and F. Schoster, “Acoustic Facies in the Southern Kara Sea: New Results by PARASOUND Echosounding,” Ber. Polarforsch., No. 479, 55–71 (2004).
M. A. Levitan, V. V. Krupskaya, E. A. Frolova, and L. N. Vlasova, “First Results of the Sediment Studies,” Ber. Polarforsch., No. 479, 44–54 (2004).
F. Schoster and M. A. Levitan, “Scientific Cruise Report of the Kara Sea Expedition with RV “Akademik Boris Petrov”; in 2003 within the Frames of the Russian-German Project ’sIRRO’ and the Russian-Norwegian Project ‘MAREAS’,” Ber. Polarforsch., No. 479 (2004).
V. P. Petelin, Grain-Size Analysis of Marine Bottom Sediments (Nauka, Moscow, 1967) [in Russian].
R. Stein, F. Niessen, K. Dittmers, et al., “Siberian River Run-Off and Late Quaternary Glaciation in the Southern Kara Sea, Arctic Ocean: Preliminary Results,” Polar Res. 21, 315–322 (2002).
M. Stuiver, P. J. Reimer, E. Bard, et al., “INTCAL 98 Radiocarbon Age Calibration, 24.000-0 Cal BP,” Radiocarbon 40, 1041–1083 (1998).
M. A. Levitan, M. V. Burtman, Z. N. Gorbunova, and E. G. Gurvich, “Quartz and Feldspars in the Surface Layer of Kara Sea Sediments,” Litol. Polezn. Iskop, No. 2, 115–125 (1998) [Lithol. Min. Res. 33, 99–108 (1998)].
F. Schoster and R. Stein, “Major and Minor Elements in Surface Sediments of Ob and Yenisei Estuaries and the Adjacent Kara Sea,” Ber. Polarforsch., No. 300, 196–207 (1999).
M. A. Levitan, T. A. Khusid, V. M. Kuptsov, et al., “Type Sections of the Upper Quaternary Deposits of the Kara Sea,” Okeanologiya, No. 5, 776–788 (1994).
L. A. Kodina, V. G. Tokarev, L. N. Vlasova, and G. S. Korobeinik, “Contribution of Biogenic Methane to Ikaite Formation in the Kara Sea: Evidence from the Stable Carbon Isotope Geochemistry,” in Siberian River Run-Off in the Kara Sea. Characterisation, Quantification, Variability and Environmental Significance, Ed. by R. Stein, K. Fahl, D. Futterer, et al. (Elsevier, Amsterdam, 2003), pp. 349–374.
I. Mardanian and L. Kodina, “Organic Carbon Distribution within Two Ikaite-Bearing Sediment Cores in the Kara Sea,” Ber. Polarforsch., No. 479, 72–76 (2004).
Ya. E. Yudovich and M. P. Ketris, Principles of Lithochemistry (Nauka, St. Petersburg, 2000) [in Russian].
L. Polyak, M. Levitan, T. Khusid, et al., “Variations in the Influence of Riverine Discharge on the Kara Sea during the Last Deglaciation and the Holocene,” Global Planet. Change 32, 291–309 (2002).
L. L. Demina, M. A. Levitan, and N. V. Politova, “Speciation of Metals in the Sediments of the Kara Sea,” Geokhimiya, (in press).
K. Dittmers, F. Niessen, and R. Stein, “Holocene Sediment Budget and Sedimentary History of the Ob and Yenisei Estuaries, in Siberian River Run-Off in the Kara Sea. Characterisation, Quantification, Variability and Environmental Significance, Ed. by R. Stein, K. Fahl, D. Futterer, et al. (Elsevier, Amsterdam, 2003), pp. 457–488.
K. V. Kremenetski, A. A. Velichko, O. K. Borisova, et al., “Peatlands of the Western Siberian Lowlands: Current Knowledge on Zonation, Carbon Content and Late Quaternary History,” Quatern. Sci. Rev. 22, 703–723 (2003).
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Original Russian Text © M.A. Levitan, I.A. Roshchina, A.V. Tolmacheva, 2007, published in Geokhimiya, 2007, No. 6, pp. 654–669.
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Levitan, M.A., Roshchina, I.A. & Tolmacheva, A.V. Holocene history of Ob River discharge according to lithological and geochemical data. Geochem. Int. 45, 590–605 (2007). https://doi.org/10.1134/S0016702907060079
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DOI: https://doi.org/10.1134/S0016702907060079