@article{NazarovaRazjigaevaDiekmannetal.2019, author = {Nazarova, Larisa B. and Razjigaeva, N. G. and Diekmann, Bernhard and Grebennikova, T. A. and Ganzey, L. A. and Belyanina, N. I. and Arslanov, K. A. and Kaistrenko, V. M. and Gorbunov, A. O. and Kharlamov, A. A. and Golovatyuk, L. V. and Syrykh, Lydmila S. and Subetto, D. A. and Lisitsyn, A. P.}, title = {Reconstruction of Holocene Environmental Changes in North-Western Pacific in Relation to Paleorecord from Shikotan Island}, series = {Doklady earth sciences}, volume = {486}, journal = {Doklady earth sciences}, number = {1}, publisher = {Pleiades Publ.}, address = {New York}, issn = {1028-334X}, doi = {10.1134/S1028334X19050143}, pages = {494 -- 497}, year = {2019}, abstract = {Results of a paleolimnological investigation of a well-dated lake sediment section from Shikotan Island (Southern Kurils) showed that from ca 8.0 to 5.8 cal ka BP a warm and humid period corresponding to middle Holocene optimum took place. Cooling thereafter corresponds to Neoglacial. A reconstructed from ca 0.9 to ca 0.58 cal ka BP warm period can correspond to a Medieval Warm Period. Cooling after 0.58cal ka BP can be correlated with the LIA. Marine regression stages were identified at ca 6.2-5.9, 5.5-5.1 and 1.07-0.36 cal ka BP. The general chronology of major climatic events of Holocene in the island is in accordance with the climate records from the North Pacific region. Revealed spatial differences in timing and magnitude of the Late Holocene climatic episodes (LIA, MWP) in the region needs further investigations.}, language = {en} } @article{NazarovaGrebennikovaRazjigaevaetal.2017, author = {Nazarova, Larisa B. and Grebennikova, Tatiana A. and Razjigaeva, Nadezhda G. and Ganzey, Larisa A. and Belyanina, Nina I. and Arslanov, Khikmat A. and Kaistrenko, Victor M. and Gorbunov, Aleksey O. and Kharlamov, Andrey A. and Rudaya, Natalia and Palagushkina, Olga and Biskaborn, Boris and Diekmann, Bernhard}, title = {Reconstruction of Holocene environmental changes in Southern Kurils (North-Western Pacific) based on palaeolake sediment proxies from Shikotan Island}, series = {Global and planetary change}, volume = {159}, journal = {Global and planetary change}, publisher = {Elsevier}, address = {Amsterdam}, issn = {0921-8181}, doi = {10.1016/j.gloplacha.2017.10.005}, pages = {25 -- 36}, year = {2017}, abstract = {We investigated a well-dated sediment section of a palaeolake situated in the coastal zone of Shikotan Island (Lesser Kurils) for organic sediment-geochemistry and biotic components (diatoms, chironomids, pollen) in order to provide a reconstruction of the palaeoenvironmental changes and palaeo-events (tsunamis, sea-level fluctuations and landslides) in Holocene. During the ca 8000 years of sedimentation the changes in organic sediment-geochemistry and in composition of the diatoms and chironomids as well as the shifts in composition of terrestrial vegetation suggest that the period until ca 5800 cal yr BP was characterized by a warm and humid climate (corresponds to middle Holocene optimum) with climate cooling thereafter. A warm period reconstructed from ca 900 to at least ca 580 cal yr BP corresponds to a transition to a Nara-Heian-Kamakura warm stage and can be correlated to a Medieval Warm Period. After 580 cal yr PB, the lake gradually dried out and climatic signals could not be obtained from the declining lacustrine biological communities, but the increasing role of spruce and disappearance of the oak from the vegetation give evidences of the climate cooling that can be correlated with the LIA. The marine regression stages at the investigated site are identified for ca 6200-5900 (at the end of the middle Holocene transgression), ca 5500-5100 (Middle Jomon regression or Kemigawa regression), and ca 1070-360 cal yr BP (at the end of Heian transgression). The lithological structure of sediments and the diatom compositions give evidences for the multiple tsunami events of different strengths in the Island. Most remarkable of them can be dated at around ca 7000, 6460, 5750, 4800, 950 cal yr BP. The new results help to understand the Holocene environmental history of the Southern Kurils as a part of the Kuril-Kamchatka and Aleutian Marginal Sea-Island Arc Systems in the North-Western Pacific region.}, language = {en} } @article{PasechnikShmelevaSaidgazievetal.2022, author = {Pasechnik, Sergey V. and Shmeleva, Dina and Saidgaziev, Ayvr Sh. and Kharlamov, Semen and Vasilieva, Aleksandra A. and Santer, Svetlana}, title = {Shear flows induced by electro-osmotic pumps in optofluidic liquid crystal cell for modulation of visible light and THz irradiation}, series = {Liquid Crystals and their Application : Russian Journal}, volume = {22}, journal = {Liquid Crystals and their Application : Russian Journal}, number = {3}, publisher = {Nanomaterials Research Institute}, address = {Ivanovo}, issn = {1991-3966}, doi = {10.18083/LCAppl.2022.3.49}, pages = {49 -- 57}, year = {2022}, abstract = {The work is devoted to the use of electrokinetic phenomena in liquid crystals to create a new class of microfluidics devices - optofluidics, designed to control electromagnetic radiation, including the THz frequency range. To achieve the goal, an optical method is used to study changes in the orientational structure in LC layers caused by a shear flow generated by electroosmotic pumps. Simula-tion of LC behaviour in an experimental cell containing electroosmotic pumps and flat layers of a nematic liquid crystal is fulfilled. The experimental depend-ences of the intensity of polarized radiation passing through flat LC layers on the control voltage applied to the electroosmotic pump and the results of calcu-lations of the hydrodynamic and mechano-optical characteristics of the experi-mental LC cell are presented. The propagation of THz irradiation across the multilayer structure of the optofluidic cell is considered taking into account the minimum number of re-reflections of waves from different layers and the ab-sorption of THz irradiation in a propylene and a liquid crystal.}, language = {en} }