Hostname: page-component-586b7cd67f-rcrh6 Total loading time: 0 Render date: 2024-11-20T17:38:16.790Z Has data issue: false hasContentIssue false
  • English
  • Français

800-yr-long records of annual air temperature and precipitation over southern Siberia inferred from Teletskoye Lake sediments

Published online by Cambridge University Press:  20 January 2017

Ivan Kalugin ,
Andrei Daryin ,
Lyubov Smolyaninova ,
Andrei Andreev ,
Bernhard Diekmann  and
Oleg Khlystov
Ivan Kalugin*
Affiliation:
Institute of Geology and Mineralogy SB RAS, Pr. Ak. Koptyuga 3, RU 630090, Novosibirsk, Russia
Andrei Daryin
Affiliation:
Institute of Geology and Mineralogy SB RAS, Pr. Ak. Koptyuga 3, RU 630090, Novosibirsk, Russia
Lyubov Smolyaninova
Affiliation:
Institute of Geology and Mineralogy SB RAS, Pr. Ak. Koptyuga 3, RU 630090, Novosibirsk, Russia
Andrei Andreev
Affiliation:
Alfred-Wegener-Institute for Polar and Marine Research, Telegrafenberg A43, D-14473 Potsdam, Germany
Bernhard Diekmann
Affiliation:
Alfred-Wegener-Institute for Polar and Marine Research, Telegrafenberg A43, D-14473 Potsdam, Germany
Oleg Khlystov
Affiliation:
Institute of Limnology SB RAS, Ulan-Batorskaya 3, RU 664033 Irkutsk, Russia
*
*Corresponding author. Fax: +7 383 333 2792. E-mail address:[email protected] (I. Kalugin).
Get access Rights & Permissions [Opens in a new window]

Abstract

A unique 800-yr-long record of annual temperatures and precipitation over the south of western Siberia has been reconstructed from the bottom sediments of Teletskoye Lake, Altai Mountains using an X-ray fluorescence scanner (XRF) providing 0.1-mm resolution timeseries of elemental composition and X-ray density (XRD). Br content appears to be broadly correlative with mean annual temperature variations because of changes in catchment vegetation productivity. Sr/Rb ratio reflects the proportion of the unweathered terrestrial fraction. XRD appears to reflect water yield regime and sediment flux. Sedimentation is rather continuous because annual clastic supply and deposited mass are the same. The artificial neural networks method was applied to convert annual sedimentary time-series of XRD, Br content, and Sr/Rb ratio to annual records of temperature and precipitation using a transfer function. Comparison of these reconstructed Siberian records with the annual record of air temperature for the Northern Hemisphere shows similar trends in climatic variability over the past 800 yr. Estimated harmonic oscillations of temperature and precipitation values for both historical and reconstructed periods reveal subdecadal cyclicity.

Keywords

Teletskoye LakeXRF scannerSub-millimeter time seriesTemperature and precipitation records
Type
Research Article
Information
Quaternary Research , Volume 67 , Issue 3 , May 2007 , pp. 400 - 410
Copyright
University of Washington

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

Antti, E.K., Ojala, T., and Teija, A. 10000 years of interannual sedimentation recorded in the Lake Nautajarvi (Finland) clastic-organic varves. Palaeogeography, Palaeoclimatology, Palaeoecology 219, (2005). 285–302.Google Scholar
Atlas USSR Publ.House of Central administrative board of a geodesy and cartography. Moscow (1969). 1–200. (in Russian) Google Scholar
Baryshev, V.B., Gavrilov, N.G., Daryin, A.V., Zolotarev, K.V., Kulipanov, G.N., Mezentsev, N.A., and Terekhov, Ya.V. Scanning X-ray fluorescent microanalysis of rock samples. Review of Scientific Instruments 60, 7 Pt. II (1989). 2456–2457.Google Scholar
Belgrano, A., Malmgren, B.A., and Lindahl, O. Application of Artificial Neural Networks (ANN) to Primary Production Time-series Data. Journal of Plankton Research 23, 6 (2001). 651–658.Google Scholar
Berri, B.L. Periodicity of geophysical processes and its influence on lithosphere development. Evolution of geological processes in Earth history. (1993). Nauka, Moscow. 53–62. (in Russian) Google Scholar
Bobrov, V.A., Kalugin, I.A., Klerkx, J., Duchkov, A.D., Sherbov, B.L., and Stepin, A.S. Rate of recent sedimentation in the Teletskoye Lake based on gamma-spectrometry ( 137Cs) data. Russian Geology and Geophysics 40, 4 (1999). 530–536.Google Scholar
Briffa, K.R. Annual climate variability in the Holocene: interpreting the message of ancient trees. Quaternary Science Reviews 19, (2000). 87–105.Google Scholar
Cook, E.R., and Kairiukstis, L.A. Methods of Dendrochronology. (1990). Kluwer Academic, 394 Google Scholar
Cook, E.R., D'Arrigo, R.D., and Briffa, K.R. A reconstruction of the North Atlantic Oscillation using tree-ring chronology from North America and Europe. The Holocene 8, (1998). 9–17.Google Scholar
Crowley, T. Causes of climate change over the past 1000 years. Science 289, (2000). 270–277. (14 July) CrossRefGoogle ScholarPubMed
Daryin, A.V., Kalugin, I.A., Maksimova, N.V., Smolyaninova, L.G., and Zolotarev, K.V. Use of a scanning XRF analysis on SR beams from VEPP-3 storage ring for research of core bottom sediments from Teletskoe Lake with the purpose of high resolution quantitative reconstruction of the last millennium paleoclimate. Nuclear Instruments and Methods in Physics Research A 543, (2005). 255–258.Google Scholar
Dehandschutter, B., Vysotsky, E., Delvaux, D., Klerkx, J., Buslov, M.M., Seleznev, V.V., and de Batist, M. Structural evolution of the Teletsk Graben (Russian Altai). Tectonophysics 351, (2002). 139–167.CrossRefGoogle Scholar
Fernandez, P., and Grimalt, J.O. On the global distribution of persistent organic pollutants. Chimia 57, 9 (2003). 514–521.Google Scholar
Gavshin, V.M., Scherbov, B.L., Melgunov, M.S., Strakhovenko, V.D., Bobrov, V.A., and Tsibulchik, V.M. 137Cs and 210Pb in lacustrine sediments from Steppe Altai as indices of dynamics of anthropogenic geochemical background change during the XX century. Russian Geology and Geophysics 40, 9 (1999). 1331–1341.Google Scholar
Goldberg, E.L., Grachev, M.A., Chebykin, E.P., Phedorin, M.A., Kalugin, I.A., Khlystov, O.M., and Zolotarev, K.V. Scanning SRXF analysis and isotopes of uranium series from bottom sediments of Siberian lakes for high-resolution climate reconstructions. Nuclear Instruments and Methods in Physics Research A 543, (2005). 250–254.CrossRefGoogle Scholar
Guiot, J., Keller, T., and Tessier, L. Relational database in dendroclimatology and new non-linear methods to analyze the tree response to climate and pollution. Ohta, S., Fujii, T., Okada, N., Hughes, M.K., and Eckstein, D. Tree rings: from the past to the future, Proceedings of the International Workshop on Asian and Pacific Dendrochronology. Forestry and Forest Products Research Institute Scientific Meeting Report 1. (1995). 17–23.Google Scholar
Inman, D.L., Jenkins, S.A., (1999). Climate change and the episodicity of sediment flux of small California rivers. J. Geol. , Center for Coastal Studies, Scripps Institution of Oceanography, University of California, San Diego, La Jolla, California. 92093–0209, U.S.A., 107, N 3, 251–270.CrossRefGoogle Scholar
Jones, P.D., Briffa, K.R., Barnett, T.P., and Tett, S.F.B. High-resolution palaeoclimatic records for the last millennium: interpretation, integration and comparison with general circulation model control-run temperatures. The Holocene 8, 4 (1998). 455–471.Google Scholar
Kalugin, I. Recent bottom fill of the Teletsk basin. Selegei, V., Dehandschutter, B., Klerkx, J., and Vysotsky, E. The physical and geological environment of Lake Teletskoye. Royal Museum of Central Africa, Ann. Sc. Geol. vol. 105, (2001). Tervuren, Belgium. 263–282.Google Scholar
Kalugin, I., Selegei, V., Goldberg, E., and Seret, G. Rhythmic fine-grained sediment deposition in Lake Teletskoye, Altai, Siberia, in relation to regional climate change. Quaternary International 136, (2005). 5–13.Google Scholar
Keller, T., Guiot, J., and Tessier, L. Climatic effect of atmospheric CO2 doubling on radial tree growth in southeastern France. Journal of Biogeography 24, (1997). 857–864.CrossRefGoogle Scholar
Klimenko, V.V. Climate of Medieval Warm Epoch in Northern Hemisphere. Moscow Energy Institute, Moscow. (2001). 87 (in Russian) Google Scholar
Kumke, T., Scholzel, C., and Hense, A. Transfer Functions for Paleoclimate Reconstructions—Theory and Methods. Fischer, H., Kumke, T., Lohmann, G., Froser, G., Miller, H., von Storch, H., and Negendank, J.F.W. The climate in historical times. Towards a synthesis of Holocene proxy data and climate models. (2004). Springer-Verlag, Berlin- Heidelberg, Germany. 229–244.Google Scholar
Lotter, A.F., Sturm, M., Teranes, J.L., and Wehrli, B. Varve formation since 1885 and high-resolution varve analyses in hypertrophic Baldeggersee (Switzerland). Aquatic Sciences 59, (1997). 304–325.CrossRefGoogle Scholar
Lottermoser, B.G., Schütz, U., Boenecke, J., Oberhänsli, R., Zolitschka, B., and Negendank, J.F.W. Natural and anthropogenic influences on the geochemistry of Quaternary lake sediments from Holzmaar, Germany. Environmental Geology 31, 3/4 (1997). 236–247. (June 7, Q Springer-Verlag) CrossRefGoogle Scholar
Mann, M.E., Bradley, R.S., and Hughes, M.K. Global-scale temperature patterns and climate forcing over the past six centuries. Nature 392, (1998). 779–781.CrossRefGoogle Scholar
Neumann, T., Stogbauer, A., Walpersdorf, E., Stuben, D., Schaller, T., Moor, H. Ch., Wehrli, B., (1997). Sedimentary profiles of Fe, Mn, V, Cr, As and Mo as indicators of benthic redox conditions in Baldeggersee. Aquatic sciences 59, 345–361., 1015–1621., Birkhäuser Verlag, Basel.Google Scholar
Oldfield, F., Crooks, P.R.J., Harkness, D.D., and Petterson, G. AMS radiocarbon dating of organic fractions from varved lake sediments: an empirical test of reliability. Journal of Paleolimnology 18, (1997). 87–91.Google Scholar
Racca, J.M.J., Philibert, A., Racca, R., and Prairie, Y.T. A comparison between diatom-based pH inference models using Artificial Neural Networks (ANN), Weighted Averaging (WA) and Weighted Averaging Partial Least Squares (WA-PLS) regressions. Journal of Paleolimnology 26, (2001). 411–422.CrossRefGoogle Scholar
Ramrath, A., Nowaczyk, N.R., and Negendank, J.F.W. Sedimentological evidence for environmental changes since 34,000 years BP from Lago di Mezzano, central Italy. Journal of Paleolimnology 21, (1999). 423–435.Google Scholar
Rumelhart, D.E., Hinton, G.E., and Williams, R.J. Learning representations by back-propagating errors. Nature 323, (1986). 533 Google Scholar
Selegei, V.V., and Selegei, T.V. Teletskoye Lake. Gydrometeoizdat, Leningrad. (1978). 1–142. (in Russian) Google Scholar
Selegei, V., Dehandschutter, B., Klerkx, J., and Vysotsky, E. The physical and geological environment of Lake Teletskoye, 2001. Royal Museum of Central Africa, Tervuren, Belgium. Ann. Sc. Geol. 105, (2001). 310 Google Scholar
Skabichevskaya, N.A. Diatom algae in the bottom sediments of the Teletstkoye Lake. Problems of paleoclimatic reconstructions in Pleistocene and Holocene 1. (1998). Publ. Institute of Archaeology and Ethnography of SB RAS, Novosibirsk. 270–276. (in Russian) Google Scholar
Smolyaninova, L.G., Kalugin, I.A., and Daryin, A.V. Technique of receiving empiri-mathematical interdependence models between climatic parameters and litologi-geochemical character of bottom deposits. Computer technology 9: Mathematic, Mechanic, Computing 3, 42 (2004). 43–46.Google Scholar
Veelenturf, L.P.J. Analysis and applications of artificial neural networks. Computer Science (1995). 259 Google Scholar
Werbos, P.J. Backpropagation through time: what it does and how to do it. Proceedings of the IEEE 78, 10 (1990). 1550–1560. (October) Google Scholar
Woodhouse, C.A. Artificial neural networks and dendroclimatic reconstructions: an example from the Front Range, Colorado, USA. The Holocene 9, (1999). 521–529.CrossRefGoogle Scholar
Yang, B., Braeuning, A., Johnson, K.R., and Yafeng, S. General characteristics of temperature variation in China during the last two millennia. Geophysical Research Letters 29, (2002). 1324 Google Scholar
Zolotarev, K.V., Goldberg, E.L., and Kondratyev, V.I. Scanning SR-XRF beamline for analysis of bottom sediments. Nuclear Instruments and Methods in Physics Research A 470, (2001). 376–379.Google Scholar