DOCSLIB.ORG

Pleistocene Climate Change, Natural Environments

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
Pleistocene Climate Change, Natural Environments Quaternary International 80–81 (2001) 131–167 Pleistocene climate change, natural environments and palaeolithic occupation of the Altai area, west-central Siberia Jiri Chlachula Laboratory for Palaeocology, University Zlin, 762 72 Zlin, Czech Republic Abstract Diversity of the relief and the Pleistocene environments of the mountain areas of SW Siberia played a major role in the history of the palaeolithic peopling of this territory. The geographical and contextual distribution of the cultural records reflects a climatic instability in the Altai area. Palaeoenvironmental proxy data indicate that the natural conditions during the earlier stages were generally more favourable for early human occupation than during the later stages. The cyclic nature of the glacial and interglacial periods led to periodic landscape transformations and generation of specific ecosystems adjusted to particular topographic settings and responding to climatic variations. The initial occupation of the broader Altai region associated with ‘‘pebble-tool’’ industries from alluvial formations likely occurred during some of the Middle Pleistocene interglacials accompanying the northern expansion of the temperate zone and biota. Mixed coniferous and broadleaf forests established in the tectonically active mountain zone with elevations of 1500–2000 m and parklands in the adjacent plains and continental basins provided a wide range of occupation habitats. There is limited evidence for persistence of Early Palaeolithic inhabitation during glacial stages due to inhospitable periglacial conditions. The last interglacial warming, indicated by re-colonization of southern Siberia by coniferous taiga forests, is linked with the appearance of the Mousterian tradition. Changes in the relief configuration influenced the local climate regime and opened new habitats for the Middle Palaeolithic population concentrated in the transitional zones of 500–1000 m elevation in the karstic area of the NW Altai foothills. Occupation of the central and southern Altai during the early last glacial was impeded by harsh, ice-marginal environments and expansion of glaciers in the valleys filled by large proglacial lakes. Progressive warming during the early mid-last glacial interstadial stage (59–35 ka BP) caused wasting of the ice fields accompanied by cataclysmic releases of ice-dammed lakes and large-scale erosional processes. Periodic outbursts of the glacial basins had a dramatic impact on the regional ecosystems, also obliterating the earlier cultural records. Appearance of the transitional early Late Palaeolithic stone industries reflects adaptation to mosaic interstadial habitats, including sub-alpine forest, dark coniferous forest, mixed parklands and open steppe. The identical geographical distribution of the Middle and Late Palaeolithic sites and the time-transgressive lithic technologies suggest a regional cultural (and biological?) continuity in the broader Altai area during the Late Pleistocene. Re-establishment of cold tundra–steppe and tundra–forest habitats correlates with the Late Palaeolithic horizon with developed stone industries dominated by blade-flaking techniques. These techniques possibly survived in more protected locations characterized by warm microclimates in the northern Altai throughout the last glacial maximum (20–18 ka BP). Emergence of the microlithic assemblages with wedge-shape cores is linked with a new cultural adjustment in the final stage of the Palaeolithic development responding to transformations of the former periglacial ecosystems towards the end of the Pleistocene. r 2001 Published by Elsevier Science Ltd. 1. Introduction remainder of Siberia from the southern regions of Central Asia. Study of the Pleistocene occupation of the Geoarchaeological investigations of human occupa- Altai was initiated by discovery of the Ulalinka Site in tion dating to the Pleistocene have a long tradition in the Gorno Altaisk in 1961 by A.P. Okladnikov following Altai region. A particular significance of the local the find of isolated palaeolithic artefacts in the vicinity Palaeolithic research lies in the geographical location of the city of Biysk (Okladnikov, 1964; Okladnikov of the Altai area on the margin of SW Siberia, believed and Adamenko, 1966). Despite the controversial age of to be the main gateway for the initial peopling of the the former site, this discovery started systematic 1040-6182/01/$ - see front matter r 2001 Published by Elsevier Science Ltd. PII: S 1040-6182(01)00023-4 132 J. Chlachula / Quaternary International 80–81 (2001) 131–167 investigations that eventually resulted in locating other The current study objectives of geoarchaeological palaeolithic sites in the broader Altai region, the adjacent research relate to particular site-specific problems, as Gorna Shoria Mountains and in the Kuznetsk Basin. By well as to general aspects of the Pleistocene peopling of the late 1980s, geoarchaeological surveys gradually north Asia. These include implementation of new expanded from the northern foothills into the central approaches aimed at site location in diverse topographic and southern Altai, mapping a number of open-air sites settings and geological contexts, the chronological (Tyumechin I and II, Tytkesken’, Ust’-Sema, Ust’- classification of the cultural records, the complex Karakol, Ust’-Kuyum, Anui I-III) as well as cave sites palaeoenvironmental reconstruction, the technological (Okladnikova, Denisova, Strashnaya, Kaminnaya, analysis of stone industries and comparative studies Razboinichia, Iskra, Maloyalomanskaya, Dmitrievka, leading to a broader territorial correlation. Apart from Tytkesken’ Caves) (Shunkov, 1982; Lapshin, 1982; the principal cultural evidence, some multistratified Kungurov, 1984, 1993; Derevianko and Markin, 1990, open-air sites (e.g., Kara-bom, Ust’-Karakol), and 1992; Derevianko and Zenin, 1990; Derevianko and particularly cave sites (the Denisova, Okladnikova, Petrin, 1990; Derevianko and Shunkov, 1992; Shunkov Kaminnaya Caves) have provided important biostrati- et al., 1994; Derevianko et al., 1995, 1999). The principal graphic and climatological records of the Quaternary long-term investigations have focused on three areas: the history and the Pleistocene climate change in south- Anui River Basin in the NW Altai foothills, the middle western Siberia. Katun River basin in Central Altai and the Chuya River Reconstruction of the Pleistocene climate dynamics basin in the southern part of the Altai Mountains that shaped the configuration of the topographic relief (Fig. 1). The recorded occupation/workshop sites, de- and ultimately governed the past ecosystems is essential scribed as Middle or Late Palaeolithic, can be classified for understanding the process and timing of the initial in respect to a particular geological context as buried peopling of the territory of north-central Asia. This sites (both open-air and cave sites) and sites exposed on study presents an up-to-date overview of the geological, the present surface; and in terms of preservation as intact biotic and archaeological evidence concerning past sites and sites re-deposited in secondary positions. climatic variations of the broader area of the Altai and Fig. 1. Geography of the Altai area with location of the principal Quaternary geology sections and the palaeolithic sites discussed in the text. Geology sections: 1FBachat, 2FBelovo, 3FBiysk, 4FChernyy Anui, 5FIniya, 6FChuya, 7FTeleckoye Ozero. Archaeological sites: 1FMokhovo, 2FUlalinka, 3FOkladnikova Cave, 4FDenisova Cave, 5FKaminnaya Cave, 6FUst’-Kanskaya Cave, 7FUst’-Karakol, 8FKara-Bom, 9FKara Tenesh, 10FTyumechin I, II; 11FMaloyalomanskaya Cave, 12FBarburghazy, 13FBigdon, 14FYustyd I, II; 15FUst’-Sema, 16FMaima, 17FIskra. J. Chlachula / Quaternary International 80–81 (2001) 131–167 133 the natural conditions during the palaeolithic occupa- higher elevations. Semi-desert communities with admix- tion of this part of Siberia. ture of taxa characteristic of the Mongolian steppes are found in the upland depressions of the southern Altai. The present soil cover corresponds to the zonal 2. Geographical location and natural setting vegetation distribution. In the northern lowland basins and plains, steppe chernozems prevail with luvisolic soils South-western Siberia, including the Altai and the formed in more humid locations in the river valleys. Kuzbass regions, is characterized by a rather diverse Kastanozems and podzolic forest soils prevail in the physiography with high mountain massifs in the south lower mountain zone; thin brunisols and tundra regosols and east, and open lowlands in the north and west are found in the (sub)-alpine zone; and kastanozems, (Fig. 1). The Altai Mountains (maximum elevation brown calcareous soils or solonets appear in the high- 4506 m asl) and the Kuznetskiy Alatau (2171 m asl) mountain basin (Chuya and Kuray Depression) and on form a natural barrier to the south and east, respec- the upland plateaus (Ukok) (Rudoy et al., 2000). tively, connected by the Gornaya Shoria Mountains (1560 m). The Salair Range (590 m) separates the adjacent continental depression in the north: the upper 3. Pre-Quaternary history of the Altai area Ob Basin and the Kuznetsk Basin (150–300 m), repre- senting the marginal parts of the Western Siberian Geological history of the broader Altai region is Lowland. Hydrologically, the area belongs to the Ob closely linked with the formation of the major central River drainage system, with the Katun, Biya, Irtysh and Asian mountain system. The Caledonian orogenesis
Load more

Recommended publications
  • Download Tour Program In
    Ethnographic tour Golden Ring of Altai Day 1. Sunday. Barnaul Morning arrival in Barnaul. Meeting at the airport. Accommodation at the Barnaul hotel (twin rooms). Rest. Meeting with guides in the hotel's hall at 13:00. Excursion around the central and historical parts of Barnaul. Visit to Altai State Local History Museum. Nowadays museum collection contains more than 150 thousand exhibits; among them is the only model of steam engine in the world, which was invented by Ivan Polzunov in 1763 in Barnaul. Archeological finds are of a special interest, they tell about history of ancient Altai; home appliances, embodying ethnical and social features of local people, as well as historical and technical (including military remnants), numismatic and mineralogical collections, natural-science collecting, representing biodiversity and natural resources of Altai. Then visit the museum of pharmacy of the Altai mountains. The exhibition includes medical items, glassware, tools for the preparation of medicinal tinctures and pills. In the museum you can find also production of various biopharmaceutical Altai companies, medicine consists of the Altai honey, local herbs, sea buckthorn and products of reindeer antlers, which can be purchased. Return to the hotel. Accommodation at the Barnaul hotel 3* till 30 km by bus Meals independent Day 2. Monday. Manzherok, the spring Arzhan Suu Morning meeting with the guide in the lobby of the hotel. Transfer by a comfortable bus through the old town of Altai-Biysk which is the symbol of the gateway to the Altai Mountains, as well as the start of the main artery-an ancient trade route - Chuysky tract.
    [Show full text]
  • In Flora of Altai
    Ukrainian Journal of Ecology Ukrainian Journal of Ecology, 2018, 8(4), 362-369 ORIGINAL ARTICLE Genus Campanula L. (Campanulaceae Juss.) in flora of Altai A.I. Shmakov1, A.A. Kechaykin1, T.A. Sinitsyna1, D.N. Shaulo2, S.V. Smirnov1 1South-Siberian Botanical Garden, Altai State University, Lenina pr. 61, Barnaul, 656049, Russia, E-mails: [email protected], [email protected] 2Central Siberian Botanical Garden, Zolotodolinskaya st., 101, Novosibirsk, 630090, Russia. Received: 29.10.2018. Accepted: 03.12.2018 A taxonomic study of the genus Campanula L. in the flora of Altai is presented. Based on the data obtained, 14 Campanula species, belonging to 3 subgenera and 7 sections, grow in the territory of the Altai Mountain Country. The subgenus Campanula includes 4 sections and 8 species and is the most diverse in the flora of Altai. An original key is presented to determine the Campanula species in Altai. For each species, nomenclature, ecological and geographical data, as well as information about type material, are provided. New locations of Campanula species are indicated for separate botanical and geographical regions of Altai. Keywords: Altai; Campanula; distribution; diversity; ecology; species A taxonomic study of the genus Campanula L. in the flora of Altai is presented. Based on the data obtained, 14 Campanula species, belonging to 3 subgenera and 7 sections, grow in the territory of the Altai Mountain Country. The subgenus Campanula includes 4 sections and 8 species and is the most diverse in the flora of Altai. An original key is presented to determine the Campanula species in Altai. For each species, nomenclature, ecological and geographical data, as well as information about type material, are provided.
    [Show full text]
  • Pleistocene Glaciations of the Se Altai, Russia, Based on Geomorphological Data and Absolute Dating of Glacial Deposits in Chagan Reference Section
    GEOCHRONOMETRIA 44 (2017): 49–65 DOI 10.1515/geochr-2015-0059 Available online at http://www.degruyter.com/view/j/geochr Conference Proceedings of the 12th International Conference “Methods of Absolute Chronology” May 11-13th, 2016, Gliwice-Paniówki, Poland PLEISTOCENE GLACIATIONS OF THE SE ALTAI, RUSSIA, BASED ON GEOMORPHOLOGICAL DATA AND ABSOLUTE DATING OF GLACIAL DEPOSITS IN CHAGAN REFERENCE SECTION ANNA R AGATOVA1, 2 and ROMAN K NEPOP1, 2 1Sobolev Institute of Geology and Mineralogy, Russia, 630090 Novosibirsk, Ak. Koptyuga av., 3 2Ural Federal University, Russia, 620002 Yekaterinburg, Mira str., 19 Received 25 June 2016 Accepted 9 February 2017 Abstract: Geomorphological evidence of at least two Pleistocene glacial epochsis noted within the Chagan-Uzun river basin, SE Altai. A review and analysis of all available absolute dates for reference Chagan section is presented. The highest correlation amongst all TL dates is observed for the lens of glacio-lacustrine sediments – the most suitable among glacial deposits for luminescence dating, and indicates its possible Middle Pleistocene age. IRSL dates obtained from feldspar indicate a Middle Pleistocene age of moraines already in the upper part of the section. The small number of obtained IRSL dates does not allow making geochronological reconstructions of the Pleistocene glaciations, but gives the possibility for further experiments with different variation of OSL (IRSL) techniques. Strong low temperature peak in TL signal and strong response to IR stimulation are specific regional quartz features, which could be explained by combination of short transportation distance and low number of depositional cycles for mineral grains. Available radiocarbon dates of carbonate concre- tions from this section are not related to the age of moraine sedimentation and most likely indicate the period of the Chagan river incision into the ancient glacial deposits.
    [Show full text]
  • Siberia and India: Historical Cultural Affinities
    Dr. K. Warikoo 1 © Vivekananda International Foundation 2020 Published in 2020 by Vivekananda International Foundation 3, San Martin Marg | Chanakyapuri | New Delhi - 110021 Tel: 011-24121764 | Fax: 011-66173415 E-mail: [email protected] Website: www.vifindia.org Follow us on Twitter | @vifindia Facebook | /vifindia All Rights Reserved. No part of this publication may be reproduced, stored in a retrieval system, or transmitted in any form, or by any means electronic, mechanical, photocopying, recording or otherwise without the prior permission of the publisher Dr. K. Warikoo is former Professor, Centre for Inner Asian Studies, School of International Studies, Jawaharlal Nehru University, New Delhi. He is currently Senior Fellow, Nehru Memorial Museum and Library, New Delhi. This paper is based on the author’s writings published earlier, which have been updated and consolidated at one place. All photos have been taken by the author during his field studies in the region. Siberia and India: Historical Cultural Affinities India and Eurasia have had close social and cultural linkages, as Buddhism spread from India to Central Asia, Mongolia, Buryatia, Tuva and far wide. Buddhism provides a direct link between India and the peoples of Siberia (Buryatia, Chita, Irkutsk, Tuva, Altai, Urals etc.) who have distinctive historico-cultural affinities with the Indian Himalayas particularly due to common traditions and Buddhist culture. Revival of Buddhism in Siberia is of great importance to India in terms of restoring and reinvigorating the lost linkages. The Eurasianism of Russia, which is a Eurasian country due to its geographical situation, brings it closer to India in historical-cultural, political and economic terms.
    [Show full text]
  • New Data on Large Mammals of the Pleistocene Trlica Fauna, Montenegro, the Central Balkans I
    ISSN 00310301, Paleontological Journal, 2015, Vol. 49, No. 6, pp. 651–667. © Pleiades Publishing, Ltd., 2015. Original Russian Text © I.A. Vislobokova, A.K. Agadjanian, 2015, published in Paleontologicheskii Zhurnal, 2015, No. 6, pp. 86–102. New Data on Large Mammals of the Pleistocene Trlica Fauna, Montenegro, the Central Balkans I. A. Vislobokova and A. K. Agadjanian Borissiak Paleontological Institute, Russian Academy of Sciences, Profsoyuznaya ul. 123, Moscow, 117997 Russia email: [email protected], [email protected] Received September 18, 2014 Abstract—A brief review of 38 members of four orders, Carnivora, Proboscidea, Perissodactyla, and Artio dactyla, from the Pleistocene Trlica locality (Montenegro), based on the material of excavation in 2010–2014 is provided. Two faunal levels (TRL11–10 and TRL6–5) which are referred to two different stages of faunal evolution in the Central Balkans are recognized. These are (1) late Early Pleistocene (Late Villafranchian) and (2) very late Early Pleistocene–early Middle Pleistocene (Epivillafranchian–Early Galerian). Keywords: large mammals, Early–Middle Pleistocene, Central Balkans DOI: 10.1134/S0031030115060143 INTRODUCTION of the Middle Pleistocene (Dimitrijevic, 1990; Forsten The study of the mammal fauna from the Trlica and Dimitrijevic, 2002–2003; Dimitrijevic et al., locality (Central Balkans, northern Montenegro), sit 2006); the MNQ20–MNQ22 zones (Codrea and uated 2.5 km from Pljevlja, provides new information Dimitrijevic, 1997); terminal Early Pleistocene improving the knowledge of historical development of (CrégutBonnoure and Dimitrijevic, 2006; Argant the terrestrial biota of Europe in the Pleistocene and and Dimitrijevic, 2007), Mimomys savinipusillus biochronology. In addition, this study is of interest Zone (Bogicevic and Nenadic, 2008); or Epivillafran in connection with the fact that Trlica belongs to chian (Kahlke et al., 2011).
    [Show full text]
  • Deer from Late Miocene to Pleistocene of Western Palearctic: Matching Fossil Record and Molecular Phylogeny Data
    Zitteliana B 32 (2014) 115 Deer from Late Miocene to Pleistocene of Western Palearctic: matching fossil record and molecular phylogeny data Roman Croitor Zitteliana B 32, 115 – 153 München, 31.12.2014 Institute of Cultural Heritage, Academy of Sciences of Moldova, Bd. Stefan Cel Mare 1, Md-2028, Chisinau, Moldova; Manuscript received 02.06.2014; revision E-mail: [email protected] accepted 11.11.2014 ISSN 1612 - 4138 Abstract This article proposes a brief overview of opinions on cervid systematics and phylogeny, as well as some unresolved taxonomical issues, morphology and systematics of the most important or little known mainland cervid genera and species from Late Miocene and Plio-Pleistocene of Western Eurasia and from Late Pleistocene and Holocene of North Africa. The Late Miocene genera Cervavitus and Pliocervus from Western Eurasia are included in the subfamily Capreolinae. A cervid close to Cervavitus could be a direct forerunner of the modern genus Alces. The matching of results of molecular phylogeny and data from cervid paleontological record revealed the paleozoogeographical context of origin of modern cervid subfamilies. Subfamilies Capreolinae and Cervinae are regarded as two Late Miocene adaptive radiations within the Palearctic zoogeographic province and Eastern part of Oriental province respectively. The modern clade of Eurasian Capreolinae is significantly depleted due to climate shifts that repeatedly changed climate-geographic conditions of Northern Eurasia. The clade of Cervinae that evolved in stable subtropical conditions gave several later radiations (including the latest one with Cervus, Rusa, Panolia, and Hyelaphus) and remains generally intact until present days. During Plio-Pleistocene, cervines repeatedly dispersed in Palearctic part of Eurasia, however many of those lineages have become extinct.
    [Show full text]
  • Altai Peaks and Rivers
    ALTAI PEAKS AND RIVERS Welcome to the majestic Altai Republic, land of mountains, nomads and heart-stopping adventures. From remote villages TOUR DURATION to superb ski resorts to pristine caves and mountain lakes, this 13 days / 12 nights tour gives you a complete picture of Altai’s extraordinary GROUP SIZE diversity. 6 -12 people The Altai Republic spans a vast 92,500sqm at the junction of the Siberian taiga, the steppes of Kazakhstan and the semi-deserts of Mongolia. A quarter REGIONS VISITED Novosibirsk, Altai region of the Altai Republic is covered in forest, and the region is rich in rivers and lakes, with more than 20,000 tributaries winding their way through the mountains on their northward journey to the Arctic Ocean. The nearest large START CITY — END CITY Novosibirsk — Novosibirsk city is Novosibirsk, an important junction of the Trans-Siberian Railway. Novosibirsk is about 350km from the Altai border, which in Siberian terms, is not particularly far away! This city, the third largest in Russia, is where our SEASON Winter, December — April adventure begins. This tour takes place in late winter, the perfect time for enjoying skiing and TOUR CATEGORY Combination tour snowboarding on Altai’s pristine slopes. You’ll also get to experience adventurous winter activities like dog sledding and snowmobiling in eerily beautiful taiga forests and snow sprinkled meadows. Novosibirsk is a great PRICE jumping off point, with its superb restaurants and stately architecture. Our From US $3950* journey is a cultural discovery as well, as we experience both urban and rural Russian life, and the unique traditions of the indigenous Altay people.
    [Show full text]
  • THE GOLDEN MOUNTAINS of ALTAI a Treasure of Biodiversity and Culture Publisher: Altai Alliance
    THE GOLDEN MOUNTAINS OF ALTAI A Treasure of Biodiversity and Culture Publisher: Altai Alliance Produced by: Pacific Environment Written by: Jennifer Castner and Pacific Environment Senior Editor and Production Manager: Meerim Kylychbekova Contributors: Chagat Almashev, Matt Foley, Gleb Raygorodetsky, Don Weeden Editors: David Gordon, Leah Zimmerman, Michael Martin Contact: [email protected] Copyright 2009 Cover Photos: Carol Hiltner, World Wildlife Fund, Ashley Tindall (top), Flickrcc/Ilya Schurov (middle), Meerim Kylychbekova (bottom). Design: Design Action Collective THE GOLDEN MOUNTAINS OF ALTAI A Treasure of Biodiversity and Culture 1 THE GOLDEN MOUNTAINS OF ALTAI Introduction Nestled in the Golden Mountains of Altai in south - health, water quality, critical habitat, and the local ern Siberia, the Republic of Altai is a unique blend tourism-based economy. of ancient cultures, stunning landscapes, and extraordinarily high biodiversity. The republic bor - In this paper, we explore why the Altai is a high- ders Mongolia, China, and Kazakhstan, covering priority conservation area, what threats the region 93,000 square kilometers—an area roughly the size faces today, and where the most significant conser - of the state of Indiana. Sacred sites dot the repub - vation opportunities are located. The paper discusses lic’s varied terrain. Its lands include temperate and specific recommendations to engage in and advance boreal forests, dramatic alpine landscapes, rich agri - these conservation opportunities. It focuses on: cultural lands, the wild and scenic Katun River, and • Strengthening cultural and environmental the remote and fragile Ukok Plateau. activism; The republic’s relative isolation and lack of devel - • Promoting alternative energy and green-building opment mean that its landscape and habitats remain technologies; largely intact.
    [Show full text]
  • A Comprehensive Approach Towards the Systematics of Cervidae
    A peer-reviewed version of this preprint was published in PeerJ on 18 February 2020. View the peer-reviewed version (peerj.com/articles/8114), which is the preferred citable publication unless you specifically need to cite this preprint. Heckeberg NS. 2020. The systematics of the Cervidae: a total evidence approach. PeerJ 8:e8114 https://doi.org/10.7717/peerj.8114 A comprehensive approach towards the systematics of Cervidae Nicola S Heckeberg Corresp., 1, 2, 3 , Gert Wörheide 1, 2, 4 1 Department of Earth and Environmental Sciences, Palaeontology & Geobiology, Ludwig-Maximilians-Universität München, Munich, Germany 2 SNSB-Bayerische Staatssammlung für Paläontologie und Geologie, Munich, Germany 3 Leibniz Institute for Evolution and Biodiversity Science, Museum für Naturkunde, Berlin, Germany 4 Geobio-CenterLMU, Munich, Germany Corresponding Author: Nicola S Heckeberg Email address: [email protected] Systematic relationships of cervids have been controversial for decades. Despite new input from molecular systematics, consensus could only be partially reached. The initial, gross (sub)classification based on morphology and comparative anatomy was mostly supported by molecular data. The rich fossil record of cervids has never been extensively tested in phylogenetic frameworks concerning potential systematic relationships of fossil cervids to extant cervids. The aim of this work was to investigate the systematic relationships of extant and fossil cervids using molecular and morphological characters and make implications about their evolutionary history based on the phylogenetic reconstructions. To achieve these objectives, molecular data were compiled consisting of five nuclear markers and the complete mitochondrial genome of 50 extant and one fossil cervid species. Several analyses using different data partitions, taxon sampling, partitioning schemes, and optimality criteria were undertaken.
    [Show full text]
  • Era Glaciale Alla Memoria Di Alberto Carlo Blanc
    Studi Superiori NIS SCIENZE GEOLOGICHE Alberto Malatesta Geologia e paleobiologia del)' era glaciale Alla memoria di Alberto Carlo Blanc la edizione - maggio 1985 © copyright by La Nuova Italia Scientifica, Roma Finito di stampare nel maggio 1985 per i tipi delle Arti Grafiche Editoriali S.r.l., Urbino Prefazione Svolgendo da diversi anni il corso di Geologia e Paleontologia del Ouaternario presso l'Università La Sapienza di Roma è stata mia cura preparare per gli studenti una serie di appunti, che ho cercato di perfe­ zionare e rendere ogni anno più completi. Ouando fui interpellato dalla Nuova Italia Scientifica circa l'eventua­ lità di pubblicare un testo che coprisse i principali aspetti dello studio del Ouaternario, non potei che presentare un sommario degli argomenti trattati nelle lezioni del corso più recente da me tenuto. Il panorama prospettato fu accolto favorevolmente, con la raccomandazione di ag­ giungere un capitolo sugli aspetti applicativi della conoscenza delle for­ mazioni quaternarie. Anche se questo implicava un nuovo lavoro di rac­ colta e coordinamento di dati, non potei che aderire alla richiesta. Come attualmente il corso viene seguito oltre che dagli studenti di Scienze Geologiche anche da naturalisti, biologi e archeologi, così il pre­ sente testo è destinato anche a studiosi che non hanno una particolare preparazione in materia geologica e paleontologica. Pertanto ogni capito­ lo della storia del Ouaternario, dal glacialismo alle vicende faunistiche, è preceduto da un cenno sulle conoscenze di base indispensabili alla com­ prensione di quanto si espone e si discute nel contesto di ogni argo­ mento. A parte il glacialismo quaternario, del quale ritengo si debba fornire un quadro completo, anche se sintetico, nella trattazione delle diverse fenomenologie mi sono riferito essenzialmente all'Europa e alla nostra penisola.
    [Show full text]
  • Riddu Riddu, Joik Or Rock-N-Roll ?
    Riddu Riddu, joik or rock-n-roll ? A study of Riddu Riddu Festivála and its role as a cultural tool for ethnic revialization Anastassia Valerievna Leonenko Thesis submitted for the degree: Master of Philosophy in Indigenous Studies Faculty of Social Sciences, University of Tromsø April 2008 Riddu Riđđu, joik or rock-n-roll? A study of Riddu Riđđu Festivála and its role as a cultural tool for ethnic revitalization Anastassia Valerievna Leonenko Thesis submitted for the degree: Master of Philosophy in Indigenous Studies Faculty of Social Sciences, University of Tromsø Norway April 2008 To Alexandre Descomps and our baby II Acknowledgements This master thesis is a result of the contribution of different individuals and organisations. First, I am grateful to the University of Tromsø that opened my path to an international academic milieu by admitting me to the Indigenous Master Programme where I met my classmates from all over the world, Saami professors with personal experience in the indigenous self-determination movement, and other researchers on indigenous issues. Moreover, the Centre for Sámi Studies played an active role in my educational process, by organising seminars (at Skibotn) and conferences (the Forum for Development Cooperation with Indigenous Studies), trips to Finnmark (Karasjok, Kautokeino, Alta) and to Kåfjord (Manndalen) and finally, funding my research project. My gratitude goes as well to the Norwegian State Educational Loan Fund (Lånekassen) and the Centre for Environment and Development (SEMUT) for their financial support that made this research possible. My greatest gratitude and thanks go to my supervisor Bjørn Bjerkli, Associate Professor at the Department of Social Anthropology at the Tromsø University, who devoted a great deal of his time reading and commenting on my work.
    [Show full text]
  • Early and Middle Pleistocene of Northern Eurasia
    See discussions, stats, and author profiles for this publication at: https://www.researchgate.net/publication/262698534 Early and Middle Pleistocene of Northern Eurasia Chapter · December 2013 DOI: 10.1016/B978-0-444-53643-3.00249-1 CITATIONS READS 16 1,055 2 authors: I. A. Vislobokova Alexey Tesakov Russian Academy of Sciences Russian Academy of Sciences 99 PUBLICATIONS 1,635 CITATIONS 165 PUBLICATIONS 2,916 CITATIONS SEE PROFILE SEE PROFILE Some of the authors of this publication are also working on these related projects: Integrated approach to characterize the structural setting and the related fossil geothermal system along the northeastern boundary of the Quaternary Denizli Basin View project Entwicklung der Fauna und Flora im Oligozän und Miozän der Mongolei (FWF-Projekt: P-10505-GEO) View project All content following this page was uploaded by I. A. Vislobokova on 30 May 2018. The user has requested enhancement of the downloaded file. This article was originally published in the Encyclopedia of Quaternary Science published by Elsevier, and the attached copy is provided by Elsevier for the author's benefit and for the benefit of the author's institution, for non-commercial research and educational use including without limitation use in instruction at your institution, sending it to specific colleagues who you know, and providing a copy to your institution’s administrator. All other uses, reproduction and distribution, including without limitation commercial reprints, selling or licensing copies or access, or posting on open internet sites, your personal or institution’s website or repository, are prohibited. For exceptions, permission may be sought for such use through Elsevier's permissions site at: http://www.elsevier.com/locate/permissionusematerial Vislobokova I., and Tesakov A.
    [Show full text]