Now showing items 1-8 of 8

    • Application of the Blue-Intensity Method for Dating Wooden Buildings in Siberia 

      Myglan, V. S.; Zharnikov, Z. Y.; Sidorova, M. O.; Barinov, V. V.; Tainik, A. V. (2018-12)
      Despite the success achieved in the tree-ring dating of wood samples from archaeological excavations over the recent years, attempts to apply this method to relatively recent wooden constructions in central Siberia run ...
    • Archaeological Sites as Markers of Neopleistocene-Holocene Hydrological System Transformation in the Kurai and Chuya Basins, Southeastern Altai: Results of Geomorphological and Geoarchaeological Studies 

      Agatova, A. R.; Nepop, R. K.; Slyusarenko, I. Y.; Myglan, V. S.; Barinov, V. V. (2016-12)
      Multidisciplinary studies using geomorphological, geoarchaeological, and geochronological approaches indicate contrasting environmental changes in Southeastern Altai, beginning in the Late Pleistocene. 29 new radiocarbon dates ...
    • Diverse growth trends and climate responses across Eurasia’s boreal forest 

      Hellmann, L.; Agafonov, L.; Ljungqvist, F. Ch.; Churakova, O.; Düthorn, E.; Esper, Jan; Hülsmann, L.; Kirdyanov, A. V.; Moiseev, P.; Myglan, V. S.; Nikolaev, A. N.; Reinig, F.; Schweingruber, F. H.; Solomina, O.; Tegel, W.; Büntgen, Ulf (2016-07)
      The area covered by boreal forests accounts for ∼16%of the global and 22% of theNorthern Hemisphere landmass. Changes in the productivity and functioning of this circumpolar biome not only have strong effects on species ...
    • Extreme climatic events in the Altai Republic according to dendrochronological data 

      Barinov, V. V.; Myglan, V. S.; Nazarov, A. N.; Vaganov, E. A.; Agatova, A. R.; Nepop, R. K. (2016-03)
      The results of dating of extreme climatic events by damage to the anatomical structure and missing tree rings of the Siberian larch in the upper forest boundary of the Altai Republic are given. An analysis of the spatial ...
    • Extreme Climatic Events in the Altai-Sayan Region as an Indicator of Powerful Volcanic Eruptions 

      Barinov, V. V.; Myglan, V. S.; Taynik, A. V.; Oidupaa, O. Ch.; Agatova, A. R. (2018-12)
      Analytic data on anomalies of the tree-ring structure of Siberian larch on the transect, passing through the Russian part of the Altai-Sayan Mountain Region from the west to the east along the top forest limit, are given ...
    • Growth coherency and climate sensitivity of Larix sibirica at the upper treeline in the Russian Altai-Sayan Mountains 

      Taynik, A. V.; Barinov, V. V.; Oidupaa, Orlan Ch.; Myglan, V. S.; Reinig, Frederick; Ulf, Büntgen (2016-09)
      Tree-ring research in the Altai-Sayan Mountains so far only considered a limited number of wellreplicated site chronologies. The dendroecological and palaeoclimatological potential and limitations of large parts of ...
    • Last millennium northern hemisphere summer temperatures from tree rings: Part I: The long term context 

      Wilson, Rob; Anchukaitis, Kevin; Briffa, Keith R.; Büntgen, Ulf; Cook, Edward; D'Arrigo, Rosanne; Davi, Nicole; Esper, Jan; Frank, Dave; Gunnarson, Bjorn; Hegerl, Gabi; Helama, Samuli; Klesse, Stefan; Krusic, Paul J.; Linderholm, Hans W.; Myglan, V. S.; Osborn, Timothy J.; Rydval, Milos; Schneider, Lea; Schurer, Andrew; Wiles, Greg; Zhang, Peng; Zorita, Eduardo (2016-02)
      Large-scale millennial length Northern Hemisphere (NH) temperature reconstructions have been progressively improved over the last 20 years as new datasets have been developed. This paper, and its companion (Part II, ...
    • Reply to 'Limited Late Antique cooling' 

      Büntgen, U.; Myglan, V. S.; Ljungqvist, F. C.; Mccormick, M.; Di, Cosmo N.; Sigl, M.; Jungclaus, J.; Wagner, S.; Krusic, P. J.; Esper, J.; Kaplan, J. O.; de Vaan M.A.C.; Luterbacher, J.; Wacker, L.; Tegel, W.; Solomina, O. N.; Nicolussi, K.; Oppenheimer, C.; Reinig, F.; Kirdyanov, A. V. (2017-04)
      We discuss the combined efficacy of environmental, archaeological and historical indicators in establishing a prolonged period of cold summers across much of the Northern Hemisphere landmass between 536 and about 660 AD, ...