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Postglacial sedimentation in the White Sea (northwestern Russia) reconstructed by integrated microfossil and geochemical data

Published online by Cambridge University Press:  22 October 2019

Dmitry F. Budko ,
Liudmila L. Demina ,
Ekaterina A. Novichkova ,
Yelena I. Polyakova ,
Marina D. Kravchishina  and
Vasily N. Melenevsky
Dmitry F. Budko*
Affiliation:
Shirshov Institute of Oceanology, Russian Academy of Sciences, 36 Nakhimovsky Prospect, Moscow 117997, Russia
Liudmila L. Demina
Affiliation:
Shirshov Institute of Oceanology, Russian Academy of Sciences, 36 Nakhimovsky Prospect, Moscow 117997, Russia
Ekaterina A. Novichkova
Affiliation:
Shirshov Institute of Oceanology, Russian Academy of Sciences, 36 Nakhimovsky Prospect, Moscow 117997, Russia
Yelena I. Polyakova
Affiliation:
Geographical Faculty, Lomonosov Moscow State University, GSP-1, Leninskie Gory, Moscow 119991, Russia
Marina D. Kravchishina
Affiliation:
Shirshov Institute of Oceanology, Russian Academy of Sciences, 36 Nakhimovsky Prospect, Moscow 117997, Russia
Vasily N. Melenevsky
Affiliation:
Sobolev Institute of Geology and Mineralogy, Siberian Branch Russian Academy of Sciences, 3 Academician Koptyug Avenue, Novosibirsk 630090, Russia
*
*Corresponding author e-mail address: [email protected] (D.F. Budko).
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Abstract

The White Sea being connected with the Arctic Ocean via the Barents Sea has an influence on its water temperature/salinity structures and biological processes and thus has an indirect impact on the Eurasian climate system. In this work, we have managed to find a correspondence between the climate fluctuation in the Holocene and changes in the geochemical and microfossil properties in the sediment core of the White Sea. For the first time, the element speciation in the sediment core covering about 10,000 cal yr BP period was investigated. The cooling periods (the early Holocene and the Subboreal stage) were characterized by a trend of increase in Si, Al, and Ti contents and Ti/Al ratios, which reflect lithogenous contribution, and decrease in geochemically labile forms of trace elements. A significant increase in the content of organic-bound trace elements and biogenic components (Сorg, BSi, and chlorin) was observed during periods of Holocene climatic optimums. The evident relationship between the metal speciation and indicators of the sedimentation paleoenvironment is observed at the stage of the active phase of early diagenesis after the slowing down of the biogeochemical processes. Down-core decrease in the Mn oxyhydroxide content exhibited a weakening of diagenesis processes at the ~130–150 cm depth.

Keywords

SedimentationMicrofossilsMajor and trace elementsChemical speciationWhite SeaDiagenesisClimate changes
Type
Research Article
Information
Quaternary Research , Volume 93 , January 2020 , pp. 110 - 123
Copyright
Copyright © University of Washington. Published by Cambridge University Press, 2019 

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References

REFERENCES

Aagard, K., Carmack, E.C., 1989. The role of sea ice and other fresh water in the Arctic circulation. Journal of Geophysical Research 94, 14485–14498.Google Scholar
Arar, E.J., Collins, G.B., 1997. Method 445.0: In Vitro Determination of Chlorophyll a and Pheophytin a in Marine and Freshwater Algae by Fluorescence. Revision 1.2. National Exposure Research Laboratory, Office of Research and Development, U.S. Environmental Protection Agency, Cincinnati, OH.Google Scholar
Battarbee, R.W., 1973. A new method for estimation of absolute microfossil numbers, with reference especially to diatoms. Limnology and Oceanography 18, 647–654.Google Scholar
Bauch, H.A., Mueller-Lupp, T., Taldenkova, E., Spielhagen, R.F., Kassens, H., Thiede, J., Grootes, P.M., Heinemeier, J., Petryashov, V.V. 2001. Chronology of the Holocene transgression at the North Siberian margin. Global and Planetary Change 31, 125–139.Google Scholar
Belyaev, N.A., 2015. Organic Matter and Hydrocarbon Markers of the White Sea. PhD dissertation. [In Russian.] Shirshov Institute of Oceanology, Moscow.Google Scholar
Bond, G., 1997. A pervasive millennial-scale cycle in North Atlantic Holocene and glacial climates. Science 278, 1257–1266.Google Scholar
Budko, D.F., 2017. Amorphous silica in the White Sea system. [In Russian.] In: Lisitzin, A.P. (Ed.), The White Sea System. Vol. IV, The Processes of Sedimentation, Geology and History. Scientific World, Moscow, pp. 337–370.Google Scholar
Budko, D.F., Demina, L.L., Lisitzin, A.P., Kravchishina, M.D., Politova, N.V., 2017. Occurrence forms of trace metals in recent bottom sediments from the White and Barents Seas. Doklady Earth Sciences 474, 552–556.Google Scholar
Calvert, S.E., Pedersen, T.F., 2007. Elemental proxies for palaeoclimatic and palaeoceanographic variability in marine sediments: interpretation and application. Development in Marine Geology 1, 568–643.Google Scholar
Chase, Z., Ellword, M.J., Van de Flierdt, T., 2018. Discovering the ocean's past through geochemistry. Elements 14, 397–402.Google Scholar
Сhester, R., Hughes, M.J., 1967. A chemical technique for separation of ferromanganese minerals and adsorbed trace metals from pelagic sediments. Chemical Geology 3, 249–262.Google Scholar
Demidov, I.N., Houmark-Nielsen, M., Kjaer, K.H., Larsen, E., 2006. The last Scandinavian Ice Sheet in northwestern Russia: ice flow patterns and decay dynamics. Boreas 35, 425–433.Google Scholar
Demina, L.L., Bud'ko, D.F., Alekseeva, T.N., Novigatsky, A.N., Filippov, A.S., Kochenkova, A.I., 2018a. Occurrence forms of heavy metals in the bottom sediments of the White Sea. In: Lisitsyn, A.P., Demina, L.L. (Eds.), Sedimentation Processes in the White Sea: The White Sea Environment Part II. Springer, Berlin, pp. 241–270.Google Scholar
Demina, L.L., Budko, D.F., Lisitzin, A.P., Novigatsky, A.N., 2018b. First data on the geochemical speciation of trace metals in the vertical fluxes of dispersed sedimentary matter in the White Sea. Doklady Earth Sciences 480, 689–693.Google Scholar
Demina, L.L., Budko, D.F., Alekseeva, T.N., Novigatsky, A.N., Filippov, A.S., Kochenkova, A.I., 2017. Partitioning of trace elements in the process of early diagenesis of bottom sediments in the White Sea. Geochemistry International 55, 144–149.Google Scholar
Demina, L.L., Levitan, M.A., Politova, N.V., 2006. Speciation of some heavy metals in bottom sediments of the Ob and Yenisei estuarine zones. Geochemistry International 44, 182–195.Google Scholar
Dzhinoridze, R.N., 1971. Diatom Algae from the Bottom Sediments of the White Sea in Connection with Its History in the Holocene. [In Russian.] PhD dissertation, Komarov Botanical Institute, Leningrad.Google Scholar
Dzhinoridze, R.N., Kirienko, E.A., Kalugin, L.V., Rybalko, A.E., Spiridonov, M.A., Spiridonova, E.A., 1979. Stratigraphy of the upper Quaternary deposits of the northern part of the White Sea. [In Russian.] In: Gershanovich, D.E. (Ed.), Late Quaternary History and Sedimentogenesis of Marginal and Inland Seas. Nauka, Moscow, pp. 34–39.Google Scholar
Fairbanks, R.G., 1989. A 17.000-year glacio-eustatic sea level record: influence of glacial melting rates on the Younger Dryas event and deep-ocean circulation. Nature 342, 637–642.Google Scholar
Fernandes, M.C., Nayak, G.N., 2015. Speciation of metals and their distribution in tropical estuarine mudflat sediments, southwest coast of India. Ecotoxicology and Environmental Safety 122, 68–75.Google Scholar
Gorbarenko, S.A., Derkachev, A.N., Astakhov, A.C., 2000. Lithostratigraphy and tephrochronology of upper quaternary sediments of the Sea of Okhotsk. [In Russian.] Russian Journal of Pacific Geology 19, 58–72.Google Scholar
Gordeev, V.V., Martin, J.M., Sidorov, I.S., Sidorova, M.V., 1996. A reassessment of the Eurasian river input of water, sediment, major elements and nutrients to the Arctic Ocean. American Journal of Science 296, 664–691.Google Scholar
Govberg, L.I., 1970. Distribution of molluscs in Holocene sediments from the White Sea. [In Russian.] Oceanology 10, 837–846.Google Scholar
Grotti, M., Soggia, F., Ianni, C., Magi, E., Udisti, R., 2013. Bioavailability of trace elements in surface sediments from Kongsfjorden, Svalbard. Marine Pollution Bulletin 77, 367–374.Google Scholar
Gurskii, Y.N., 2005. Particular features of the chemical composition of the interstitial waters of the White Sea. Oceanology 45, 208–221.Google Scholar
Gusakova, A.I., 2013. Mineral composition of the modern bottom sediments of the White Sea. Oceanology 53, 223–232.Google Scholar
Harris, P.G., Zhao, M., Rosell-Melé, A., Tiedemann, R., Sarnthein, M., Maxwell, J.R., 1996. Chlorin accumulation rate as a proxy for Quaternary marine primary production. Nature 383, 63–65.Google Scholar
Jakobsson, M., Mayer, L., Coakley, B., Dowdeswell, J.A., Forbes, S., Fridman, B., Hodnesdal, H., et al. , 2012. The International Bathymetric Chart of the Arctic Ocean (IBCAO) version 3.0. Geophysical Research Letters 39, L12609.Google Scholar
Kim, S., Takashashi, K., Khim, B.-K., Kanematsu, Y., Asahi, H., Ravelo, A.C., 2014. Biogenic opal production changes during the mid-Pleistocene transition in the Bering Sea (IODP Expedition 323 Site U1343). Quaternary Research 81, 151–157.Google Scholar
Kitano, Y., Fujiyoshi, R., 1980. Selective chemical leaching of Cd, Cu, Mn and Fe in marine sediments. Geochemistry Journal 14, 122–128.Google Scholar
Kolka, V.V., Korsakova, O.P., Shelekhova, T.S., Lavrova, N.B., Arslanov, K.A., 2013. Reconstruction of the relative level of the White Sea during the Holocene on the Karelian coast near Engozero settlement, northern Karelia. Doklady Earth Sciences 449, 434–438.Google Scholar
Kot, A., Namiesnik, J., 2000. The role of speciation in analytical chemistry. Trends in Analytical Chemistry 19, 69–79.Google Scholar
Koukina, S.E., Vetrov, A.A., 2013. Metal forms in sediments from Arctic coastal environments in Kandalaksha Bay, White Sea, under separation processes. Estuarine, Coastal and Shelf Science 130, 21–29.Google Scholar
Kuz'mina, T.G., Lein, A.Y., Luchsheva, L.N, Murdmaa, I.O., Novigatskii, A.S., Shevchenko, V.P., 2009. Chemical composition of surface sediments of the White Sea. Lithology and Mineral Resources 44, 103–119.Google Scholar
Laukert, G., Makhotin, M., Petrova, M.V., Frank, M., Hathorne, E.C., Bauch, D., Boning, P., Kassens, H., 2019. Water mass transformation in the Barents Sea inferred from radiogenic neodymium isotopes, rare earth elements and stable oxygen isotopes. Chemical Geology 511, 416–430.Google Scholar
Lein, A.Y., Novichkova, Y.A., Rybalko, A.Y., Ivanov, M.V., 2013. Carbon isotope composition of organic matter in Holocene sediments of the White Sea as one of the indicators of sedimentation conditions. Doklady Earth Science 452, 1056–1061.Google Scholar
Lisitsyn, A.P., 1994. A marginal filter of the oceans. [In Russian] Oceanology 34, 735–747.Google Scholar
Lisitsyn, A.P., Demina, L.L. (Eds.), 2018. Sedimentation Processes in the White Sea: The White Sea Environment Part II. The Handbook of Environmental Chemistry 82. Springer, Berlin.Google Scholar
Luoma, S.N., Bryan, G.W., 1981. A statistical assessment of the forms of trace metals in oxidized estuarine sediments employing chemical extractants. Science of the Total Environment 17, 165–196.Google Scholar
Main Service of Geodesy and Cartography at the Council of Ministers of the USSR, 1971. Atlas of Murmansk Region. Council of Ministers of the USSR, Moscow.Google Scholar
Malyasova, E.S., 1976. Palynology of the Bottom Sediments of the White Sea. [In Russian.] Leningrad University Press, Leningrad.Google Scholar
Mamindy-Pajany, Y., Hurel, C., Geret, F., Galgani, F., Bataglia-Brunet, F., Marmier, N., Romeo, M., 2013. Arsenic in marine sediments from French Mediterranean ports: geochemical partitioning, bioavailability and ecotoxicology. Chemosphere 90, 2730–2736.Google Scholar
Melenevskii, V.N., Leonova, G.A., Konyshev, A.S., 2011. The organic matter of the recent sediments of Lake Beloe, West Siberia (from data of pyrolytic studies). Russian Geology and Geophysics 56, 583–592.Google Scholar
Naeher, S., Gilli, A., North, R.P., Hamann, Y., Schubert, C.J., 2013. Tracing bottom water oxygenation with sedimentary Mn/Fe ratios in Lake Zurich, Switzerland. Chemical Geology 352, 125–133.Google Scholar
Nemati, K., Abu Bakar, N.K., Abas, M.R., Sobhanzadeh, E., 2011. Speciation of heavy metals by modified BCR sequential extraction procedure in different depths of sediments from Sungai Buloh, Selangor, Malaysia. Journal of Hazardous Materials 192, 402–410.Google Scholar
Nevessky, E.N., Medvedev, V.S., Kalinenko, V.V., 1977. The White Sea: Sediment Formation and Development History in Holocene. [In Russian.] Nauka, Moscow.Google Scholar
Novichkova, E.A., Polyakova, E.I., 2007. Dinoflagellate cysts in the surface sediments of the White Sea. Oceanology 47, 660–670.Google Scholar
Novichkova, E.A., Polyakova, E.I., 2013. Associations of microalgae in bottom sediments of marginal filters areas (White Sea bays). Doklady Earth Science 449, 413–417.Google Scholar
Novichkova, Y.A., Reikhard, L.Y., Lisitzin, A.P., Rybalko, A.Y., Vernal, A. de, 2017. New data on the Holocene evolution of the Dvina Bay (White Sea). Doklady Earth Science 474, 607–611.Google Scholar
Petelin, V.P., 1967. Grain-Size Analysis for Marine Bottom Sediments. [In Russian.] Nauka, Moscow.Google Scholar
Polyakova, Y.I., Dzhinoridze, R.N., Novichkova, T.S., Golovnina, E.A., 2003. Diatoms and palynomorphs in the White Sea sediments as indicators of ice and hydrological conditions. Oceanology 43. 144–158.Google Scholar
Polyakova, Y.I., Novichkova, Y.A., 2018. Diatoms and aquatic palynomorphs in the White Sea sediments as indicators of sedimentation processes and paleoceanography. In: Barcelo, D., Kostianoy, A.G. (Eds.), The Handbook of Environmental Chemistry. Springer, Berlin, pp. 67–104.Google Scholar
Polyakova, Y.I., Novichkova, Y.A., Lisitzin, A.P., Bauch, H.A., Rybalko, A.Y., 2014. Modern data on the biostratigraphy and geochronology of White Sea sediments. Doklady Earth Sciences 454, 169–174.Google Scholar
Poulton, S.W., Raiswell, R., 2002. The low-temperature geochemical cycle of iron: from continental fluxes to marine sediment deposition. American Journal of Science 302, 774–805.Google Scholar
Pueyo, M., Rauret, G., Luck, D., 2001. Certification of the extractable contents of Cd, Cr, Cu, Ni, Pb and Zn in a freshwater sediment following a collaboratively tested and optimized three-step sequential extraction procedure. Journal of Environmental Monitoring 3, 243–250.Google Scholar
Quevauviller, P., Ure, A., Muntau, H., Griepink, B., 1993. Improvement of analytical measurements within the BCR programme: single and sequential extraction procedures applied to soil and sediment analysis. International Journal of Environmental and Analytical Chemistry 51, 129–134.Google Scholar
Raiswell, R., Canfield, D.E., 2012. The iron biogeochemical cycle: past and present. Geochemical Perspectives 1, 1–2.Google Scholar
Regueneau, O., Gallinari, M., Corrin, L., Grandel, S., Hall, P., Hauvespre, A., Lampitt, R.S., et al. , 2001. The benthic silica cycle in the Northeast Atlantic: annual mass balance, seasonality, and importance of non-steady-state processes for the early diagenesis of biogenic opal in deep-sea sediments. Processes in Oceanology 50, 171–200.Google Scholar
Regueneau, O., Leynaert, A., Treguer, P., DeMaster, D.J., Anderson, R.F., 1996. Opal studied as a marker of paleoproductivity. Eos, Transactions American Geophysical Union 77, 491–493.Google Scholar
Rybalko, A.E., Zhuravlyov, V.A., Semyonova, L.R., Tokarev, M.Y., 2018. Development history and Quaternary deposits of the White Sea basin. In: Lisitsyn, A.P., Demina, L.L. (Eds.), Sedimentation Processes in the White Sea: The White Sea Environment Part II. Springer, Berlin, pp. 135–164.Google Scholar
Stein, R., Boucsein, B., Fahl, K., Garcia de Oteyza, T., Knies, J., Niessen, F., 2001. Accumulation of particulate organic carbon at the Eurasian continental margin during late Quaternary times: controlling mechanisms and paleoenvironmental significance. Global and Planetary Change 31, 87–104.Google Scholar
Stockmarr, J., 1971. Tablets with spores used in absolute pollen analysis. Pollen et Spores 13, 616–621.Google Scholar
Stuiver, M., Reimer, P.J., 1993. Extended 14C data base and revised CALIB 3.0 14C age calibration program. Radiocarbon 35, 215–230.Google Scholar
Sutherland, R.A., Tack, F.M.G., 2003. Fractionation of Cu, Pb and Zn in certified reference soils SRM 2710 and SRM 2711 using the optimized BCR sequential. Advances in Environmental Research 8, 37–50.Google Scholar
Ure, A.M., Quevauviller, P., Muntau, H., Griepink, B., 1993. Speciation of heavy metals in soils and sediments. An account of the improvement and harmonization of extraction techniques undertaken under the auspices of the BCR of the Commission of the European Community. International Journal of Environmental and Analytical Chemistry 51, 135–151.Google Scholar