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InternatIonal UnIon for QUaternary research (InQUa) sectIon on eUropean QUaternary stratIgraphy (seQs) InstItUte of plant & anImal ecology Ural Branch of the rUssIan academy of scIences (IPAE) Ural federal UnIversIty named after the fIrst presIdent of rUssIa B. n. yeltsIn InstItUte of natUral scIences THE QUATERNARY OF THE URALS: global trends and Pan-European Quaternary records International conference INQUA-SEQS 2014 Ekaterinburg, Russia September 10–16, 2014 ekaterInBUrg UrfU 2014 Международный союз по изучению четвертичного периода секция европейской четвертичной стратиграфии институт экологии растений и животных уро РАН уральский федеральный университет иМени первого президента россии Б. н. ельцина институт естественных наук ЧЕТВЕРТИЧНЫЙ ПЕРИОД УРАЛА: глобальные тенденции и их отражение в общеевропейской четвертичной летописи Материалы международной конференции INQUA-SEQS Екатеринбург, Россия, 10–16 сентября 2014 года eкатеринБург урФУ 2014 Publication is supported by INQUA, RFBR (grant 14-05-20211 г) and the Program for enhancing the global competitiveness of UrFU (grant 6.1.3.5.b-14). Editorial Board: A. V. BORODIN, E. A. MARKOva, T. V. STRUKOva The Quaternary of the Urals: global trends and Pan-European Quaternary records : International conference INQUA-SEQS 2014 (Ekaterinburg, Russia, September 10–16, 2014). – Ekaterinburg, 2014. – 228 p. ISBN The book presents the proceedings of the International Conference INQUA-SEQS 2014 held in Ekaterinburg, Russia. Reports concern a wide spectrum of issues connected to the study of the Quaternary Epoch (2.6 Ma) in Europe and Asia. Based on the results of local and regional Quaternary studies the authors focus on Quaternary stratigraphy and correlations across the Ural region and Europe and discuss the integration of pan- European and pan-Eurasian stratigraphical frameworks. The special attention is given to palaeontological, palaeoclimatological and palaeoenvironmental issues from the Quaternary of Europe and Asia. Materials are published with the maximal preservation of the authors’ text. ISBN 978-5-321-02398-3 © Ural Federal University, 2014 © Institute of Plant and Animal Ecology UrB RAS, 2014 УДК "624/627"(470.5)=111(06) ББК 63.3(235.55)я431+81.2АнглЯ431 Ч52 Материалы конференции изданы при финансовой поддержке INQUA, РФФИ (грант 14-05-20211 г) и программы повышения конкурентоспособности УрФУ (грант 6.1.3.5.b-14). Рецензенты: С. Л. Вотяков, академик РАН, доктор геолого-минералогических наук, директор Института геологии и геохимии УрО РАН; С. А. Шавнин, доктор биологических наук, профессор, директор Ботанического сада УрО РАН Редакционная коллегия: А. В. Бородин, доктор Биологических наук, зав. лаБораторией филогенетики и Биохронологии иэриж уро РАН, профессор кафедры экологии иен урФУ; Е. А. Маркова, кандидат Биологических наук, старший научный сотрудник лаБоратории филогенетики и Биохронологии иэриж уро РАН; Т. В. Струкова, кандидат Биологических наук, ученый секретарь иэриж уро РАН Четвертичный период Урала: глобальные тенденции и их отражение Ч52 в общеевропейской четвертичной летописи : материалы международной конференции INQUA-SEQS (Екатеринбург, Россия, 10–16 сентября 2014 г.). – Екатеринбург : УрФУ, 2014. – 228 с. ISBN 978-5-321-02398-3 В книге представлены материалы международной конференции INQUA- SEQS 2014, проводившейся в Екатеринбурге (Россия). Сообщения касаются широкого спектра вопросов, связанных с исследованиями четвертичного периода (2,6 млн лет) в Европе и Азии. На основании результатов локальных и региональных исследований авторы рассматривают проблемы стратиграфии и корреляции четвертичных отложений Уральского региона и Европы и обсуждают вопросы интеграции общеевропейских и евразийских стратиграфических схем. Особое внимание уделено вопросам палеонтологии, палеоклимата и палеосреды четвертичного периода Европы и Азии. Библиографические ссылки в статьях оформлены в соответствии с ISO 690:2010. УДК "624/627"(470.5)=111(06) ББК 63.3(235.55)я431+81.2АнглЯ431 Ответственность за содержание предоставленных материалов несут авторы статей. ISBN 978-5-321-02398-3 © Уральский федеральный университет, 2014 © Институт экологии растений и животных УрО РАН, 2014 УДК 556.3.01(1-925.11/.16)(282.256.14) L. AgAfonov Institute of Plant and Animal Ecology, Ural Branch, Russian Academy of Sciences Ekaterinburg, Russia E-mail: [email protected] THE OB RIVER DISCHARGE FOR THE LAST 300 YEARS: RECONSTRUCTION FROM TREE RINGS Key words: climate change, hydrological cycle, streamflow, Ob River, West Siberia Much attention has been paid to research on river runoff in the context of global climate change (SWIPA, 2011). Such attention is deserved because river runoff is an important component of hydrological cycle, a main constituent of the climate system. Terrestrial water-cycle processes regulating evaporation, runoff and changes in the hydrological cycle are directly linked with atmospheric processes (Chahine, 1992; Rawlins, 2010; Shiklomanov et al., 2011). Changes in the terrestrial hydrologic budget of the Northern Hemisphere influence the freshwater inflow to the Arctic Ocean (Peterson et al., 2002, 2006; McClelland et al., 2004; Mauritzen, 2012). Annual river discharge is the dominant part (38 %) of freshwater input to the Arctic Ocean (Serreze et al., 2006), and the export of river freshwater to the Arctic Ocean is about 11 % of the global river discharge (Shiklomanov, 2000). The Ob River is one of the world’s greatest rivers. Its basin (2.9x10 6 km2) is the fourth largest over the world and is about the size of Western Europe. Estimates of annual discharge from the Ob Basin range from 400 km 3 to 429 km3 and it is to 12 % or more of the annual freshwater inflow to the Arctic Ocean. Approximately 70 % of annual discharge occurs in the ice- free period from May to October, and 80 % of the annual runoff originates southward of 61º N (1152 km from the Ob estuary). Ob River discharge has the highest autocorrelation coefficient (r = 0.38) for discharge in the Northern Hemisphere for a one-year lag and there is a reliable quasi-periodicity of many- year variations in runoff (Simonov, Khristoforov, 2005). The Ob catchment basin can therefore provide great insight into global scale perturbations to the climate system. We developed tree-ring width chronologies (larch and Siberian stone pine) for the 9 test sites (285 trees in total) along the Lower Ob River valley (64º49’ N – 66º06’ N). Response of tree-ring chronologies to hydro-climatic conditions were analyzed using program SEASCORR (Meko et al., 2011) to identify the seasonal hydrological and climatic signals in an annual tree-ring time series for 1936–2009. Modern interaction between the Ob discharge and air temperature over the Ob floodplain was used for understanding hydro- climatic conditions as a background. © Agafonov L., 2014 5 Fig. 1. Reconstruction of the Ob River discharge (1) for the period from August of previous year to July of current year and actual discharge records (2) for Salekhard gauge (287 km from the Ob River estuary). Bold line is 11-years smoothing filter for the reconstructed data Using tree-ring chronologies we reconstructed the Ob River discharge for period from previous August to current July (that is nearly the same as hydrological year) for the last 300 years (Fig. 1). Developed reconstruction of the Ob River discharge has good correlation (r = 0.67, p < 0.05) with records from gage of “Salekhard” for 1936–1996. Our approach and results demonstrate the high potential of tree-ring chronologies to reconstruct river discharge in this region and allow interpreting hydro-climatic interactions over the Ob catchment basin. This study was supported by Russian Foundation for Basic Researches, grant № 13–04–01964. REFERENCES Chahine M. T. 1992. The hydrological cycle and its influence on climate. Nature. Vol. 359. P. 374–380. Mauritzen C. 2012. Arctic freshwater. Nature Geoscince. Vol. 5. 163–165. doi:10.1038/ngeo1409 McClelland J. W., Holmes R. M., Peterson B. J., Stieglitz M. 2004. Increasing river discharge in the Eurasian Arctic: Consideration of dams, permafrost thaw, and fires as potential agents of change. J. of Geophysical Research. V.109. D18102, doi:10.1029/2004JD004583. Meko D. M., Touchan R., Anchukaitis K. J. Seascorr: A MATLAB program for identifying the seasonal climate signal in an annual tree-ring time series. Computers & Geosciences. 2011. Vol. 37. P. 1234–1241. Peterson B. J., Holmes R. M., McClelland J. W., Vörösmarty C. J., Lammers R. B., Shiklomanov A. I., Shiklomanov I. A., Rahmstorf S. 2002. Increase river discharge to the Arctic Ocean. Science. Vol. 298. P. 2171–2173. Peterson B. J., McClelland J. W., Curry R. Holmes R. M., Walsh J. E, Aagaard K. 2006. Trajectory shifts in the Arctic and Subarctic freshwater cycle. Science. Vol. 313. P. 1061–1066. Rawlins M. A., Steele M., Holland M. M. et al. 2010. Analysis of the Arctic System for Freshwater Cycle Intensification: Observations and Expectations. J. of Climate. V. 23. P. 5715–5737. Serreze, M. C., Walsh, J. E., Chapin III, F. S., Ostercamp, T., Dyurgerov, M., Romanovsky, V., Oechel, W. C., Morison, J., Zhang, T., Barry R.G. 2000. Observational evidence of recent change in the northern high-latitude environment. Climatic Change. Vol. 46. P. 159–207. 6 Simonov Yu. A., Khristoforov A.V. 2005. Analysis of Many-Year Variations in River Runoff into the Arctic Ocean. Water Resources. Vol. 32: 6, 587–593. DOI: 10.1007/s11268–005–0076–2 Shiklomanov I. A. 2000. Appraisal and Assessment of World Water Resources. Water Int. Vol. 25, 1:11–32.
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    ISSN2541–9293 ЖУРНАЛ О ПЕРМСКОМ КРАЕ 2 (7) лето-осень/2018 to Perm Пермь Кунгур Хохловка Оса Юго-Камский Кудымкар Автор фото: П. Семянников Автор www.permkrai.ru Пермский край 2.0 Пермский край 2.0 permkrai_2.0 reshetnikovmg г. Пермь, ул. Ленина, 39 г. Кунгур, ул. Октябрьская, 19 А Тел. +7 (342) 214-10-80 Тел. +7 (34271) 2-29-62 e-mail: [email protected] e-mail: [email protected] Посетив наш центр, вы можете: ■ узнать о самых интересных местах города Перми и края, культурных мероприятиях, развлечениях; ■ получить бесплатные туристические карты и издания о Пермском крае; ■ приобрести сувенирную и полиграфическую продукцию; ■ выбрать наилучшее место для ночлега, получить полезные советы о том, где можно сделать покупки или перекусить; ■ заказать всевозможные экскурсии по Перми и Пермскому краю с лучшими экскурсоводами. www.visitperm.ru facebook.com/visitperm vk.com/ticperm instagram.com/visitperm 1 №2 (7) лето-осень/2018 Фото и иллюстрации: Дирекция фестиваля KAMWA Константин Долгановский Григорий Скворцов Павел Семянников Александр Болгов Агентство «Стиль-МГ» Туроператор «Северный Урал» Перевод: Агентство переводов «Интер-Контакт» Издатель, редакция, типография: Агентство «Стиль-МГ» (ООО «Редакция (агентство) …Часто вспоминаем, что Пермский край — начало «Молодая гвардия – Стиль») Российская Федерация, 614070, Европы. Здесь первые лучи восходящего солнца каждое г. Пермь, бульвар Гагарина, 44а, утро золотят вершины вековечного Урала, прозванного офис 1 века назад Каменным Поясом необъятной России, опор- www.stmg.ru ным краем державы. Рерайт: Юлия Баталина Отсюда по Европе шествует новый день, открывая Рецензент: Наталья Аксентьева гостям и жителям Пермского края все новые и новые Редактор выпуска: свои грани. Яков Азовских События в регионе словно бьют ключом: фестивали Директор агентства: и встречи, события культуры и целого мира искусства Юрий Анкушин соприкасаются с живой природой, звенящим горным Учредитель: Министерство культуры воздухом и широкими реками.
  • European Bison in Russia – Past, Present and Future

    European Bison in Russia – Past, Present and Future

    European Bison Conservation Newsletter Vol 2 (2009) pp: 148–159 European bison in Russia – past, present and future Taras P. Sipko Institute of Problems Ecology and Evolution RAS, Moscow, Russia Abstract The area of the European bison during historical time Holocene is discussed with addition of new information published in last years. Northern border of an area corresponds 60 0 N. The area included average and southern Urals Mountains, the south of Western Siberia. On the east the European bison lived up to the Altay Mountains and Lake Baikal. The same area at a red deer having similar ecological needs. Increase of inbreeding level considerably and negatively influences adaptable and reproductive opportunities of a bison. This circumstance is especially shown in case of its reintroduction in mountain areas. The basic projects on cultivation of the European bison in Russia are discussed. Keywords : European bison, geographical range, inbreeding, reintroduction Bison Habitat The studies on historical changes of European bison habitat are important both theoretically and practically. Historical geographical range of a species is the most favorable area for reintroduction and creation new free populations. In Pleistocene, the European bison range covered the most part of Eurasia (Flerov 1979). From the beginning of Holocene natural conditions changed (especially in the western part of the region). Glacier shield and vast pre-glacier lakes shortened and disappeared. Forest boundary migrated to the North. Humans occupied the area. Snow cover became deeper and lasted longer and become a limiting factor of European bison distribution at the Russian plain. All factors mentioned above served in drawing of northeastern boundary of European bison range in historic time (Heptner et al.
  • D. Palaeozoological Research

    D. Palaeozoological Research

    Eiszeitalter u. Gegenwart Band 23/24 Seite 333-339 Öhringen/Württ., 15. Oktober 1973 D. Palaeozoological Research by HORST REMY, Bonn translated by U. BUREK, S. CHRULEV and R. THOMAS, Tübingen 1. Molluscs Comprehensive studies of Pleistocene land- and freshwater molluscs have so far been largely restricted to the faunas of interglacial and Würmian glacial deposits, and to the history of postglacial faunas. ANT has reconstructed the postglacial history of changes in landsnail distributions in NW-Germany and Westphalia (ANT 1963a, 1967). The present day fauna consists of a preexisting fauna ("Urfauna") together with postglacial immi­ grants. The elements of the "Urfauna" are eurythermal species, which were already living in NW-Germany during Würm Glaciation. These species comprise about 24 °/o of the present day fauna. In the South German periglacial region this portion is rather higher. Microclimatic conditions must have been more favourable in this region, presumably because the influence of the alpine ice mass was not as strong as that of the continental ice sheet to the north. There were many ecological niches whose local climates were more favourable for the survival of such species. Along the south coast of England, SW of the land connection with the continent, several migrant species survived (Atlanto-Britannic Fauna). In the forested region west of the Urals, the species wich today constitute the Siberio-Asiatic Fauna survived, while the immigrant species of the Mediterranean Fauna survived on the E-coast of Spain, on the W-coast of Italy and SE-Europe. It is not yet certain where some of the immigrant species lived during the glaciation; possibly these forms survived the ice age in S-Germany and the adjoining regions.