Medical Geology Newsletter

Total Page:16

File Type:pdf, Size:1020Kb

Medical Geology Newsletter July 2012 MEDICAL GEOLOGY NEWSLETTER International Medical Geology Association Newsletter No. 20 ISSN 1651-5250 HIGH CHAPTER ACTIVITIES: THE LARGEST NEWSLETTER YET Inside this issue: MESSAGE FROM THE 2 CHAIRMAN MEDICAL GEOLOGY IN 3 THE NEWS: OLD AND NEW FROM THE EDITOR 4 CHAPTERS 5 REPORTS 10 AWAITING APPROVAL 26 POSSIBLE CHAPTERS 27 NOTICES 28 PAST EVENTS 29 UPCOMING EVENTS 32 SHORT ARTICLES 34 Participants of the first conference in medical geology in the Republic of Bel- arus. Minsk, BelNIGRI, February 28, 2012. ARITCLE: OPEN-PIT MIN- 50 ING IN ARGENTINA NEW IMGA CONFERENCE LOGO See page 4. MESSAGE FROM THE CHAIRMAN Dear Friends and Colleagues on Medical Geology: Welcome to the 20th edition of the International Medical Geology Association (IMGA) Newsletter, which marks a significant achievement on the development of medical geology worldwide. Since its inception in 1999, our Newsletter has aimed at keeping our global IMGA community informed about the most recent re- search advances on this emerging multidisciplinary field of medical geology. Today, our goals remain the same, as has been amply demonstrated by the increased number of publications, conference and educational activities, and research programs conducted by our Chapters worldwide; many of these activities are high- lighted throughout this 20th edition of our Newsletter. With over 15 IMGA Chapters worldwide, IMGA is continuously expanding its membership, reaching over 320 members during the first part of 2012. Today, we are proud to welcome our newly established chapters in South Africa (under the leadership of Prof. Hassina Maori, University of Johannesburg), Denmark (led by Dr. Peter Appel), N.I.S. (led by Dr. Iosif Volfson), United States (led by Ms Brittany Merola, Duke University), and Mexico (led by Prof. Hector Rubio, University of Chihuahua). Working together with our regional Chap- ters, IMGA will be contributing actively to several international upcoming conferences in 2012 including the 34th International Geological Congress to be held in Brisbane, Australia in August 2012, the 9th International Symposium on Environmental Geochemistry to be held in Aveiro, Portugal in August 2012, and the 2012 SINO-European Symposium on Environment and Health to be held in Galway, Ireland in July 2012. Addition- ally, plans for the organization of our 5th International Conference on Medical Geology (MEDGEO2013) are well underway. The dates for MEDGEO2013 have been announced for the week of August 25-29, 2013 in Washington, DC. Please visit our website for the most recent updates on our main conference. This year we extend a warm welcome to the International Registry of Pathology (IRP) as one of our affiliated organizations and sponsors of our MEDGEO International Conference Series. IMGA and IRP share a com- mon bond in our missions to pursue global education opportunities and outreach for the medical, earth sci- ences, environmental and public health communities. As part of this collaboration, we are proud to announce the establishment of a research grant program to be titled IMGA Gardner Research Grants (in honor and mem- ory of our good friend and IRP President, Dr. William A Gardner), to support research opportunities for gradu- ate students interested in medical geology. More information on this IMGA-IRP program will be posted soon in our website at http://www.medicalgeology.org . With these developments and successes in mind I want to express my appreciation and the appreciation of the As- sociation to Dr. Eduardo Santini (Argentina), our medical councilor for the last two years. Eduardo’s dedicated and committed service to our Association was outstanding in establishing the Argentine Chapter on Medical Geology and contributing to the development of medical geology in South America. At the same time I wish to welcome Dr. Diego Fridman (Argentina), as our incoming medical councilor who will join the Executive Committee and help to continue the upward trend of IMGA. Diego’s training as a physician with expertise in clinical and epidemi- ological research will certainly stimulate our interactions with the biomedical public health community. As we continue our trajectory for another successful decade of Medical Geology advances, I would like to thank each one of you for the opportunity that you have provided to me to serve as the Chairman of IMGA and to have had one of those rare opportunities in life to be part of something truly unique and genuinely special. Respectfully, Jose A. Centeno, Chairman, International Medical Geology Association Page 2 MEDICAL GEOLOGY NEWSLETTER MEDICAL GEOLOGY IN THE NEWS: OLD AND NEW! From: Karin Ljung Björklund, [email protected] For fun, I checked "Medical Geology" on Google's Ngram and found a reference to it from as early as 1834, in Vol. 25 of the Americal Journal of Medicine: “Medical Geology - At some future day I have no doubt that we shall discover that there is such a science as medical geology viz that certain strata are as foundation ground for human habitations much more liable to be affected with certain causes of diseases than others and we shall probably not only know the fact but ascertain the cause and the remedy. The county of Norfolk has long been famous or infamous for the astonishing num- ber of patients affected with the stone. nothing has hitherto been done to investigate the cause. The earth I have long since been persuaded contains within itself agents destined to affect future changes of the solid surface and also of the atmosphere .The pestilence and earthquake which reigned together for seventy years during the reign of Justinian and depopulated the fairest portion of the civilized world were doubtless the result of certain subterranean laws which regulate its internal economy laws known only to its creator.” http://books.google.se/books? id=gOhQAAAAYAAJ&hl=sv&hl=sv&pg=PA182&img=1&zoom=3&sig=ACfU3U1TOlzM7mA8SHWRUzVtj KRYa4qsvA&ci=159%2C581%2C749%2C486&edge=0 From: Bob Finkelman We made the cut! In the January 2012 issue of Earth magazine the readers were asked: How can geoscentists help society? The fifth most common response was: “By warning of health dangers from natural resources”. In my opinion this response represents a significant increase in the awareness and acceptance of Medical Geol- ogy by the geoscience community. By the way, the first four responses were predicting future climate change, finding and developing natural resources, predicting and warning about natural disasters, and mitigating cli- mate change through geoengineering. Two issue that have been central to geology for centuries and two deal- ing with the hot topic of climate change. Bob MEDICAL GEOLOGY ON FACEBOOK Members who use Facebook should become friends of Medical Geology. https://www.facebook.com/pages/International-Medical-Geology-Association-IMGA/217954944942790 This Facebook site will be used to provide information on MEDGEO2013 in Washington. Page 3 MEDICAL GEOLOGY NEWSLETTER FROM THE EDITOR A 20th edition of the Medical Geology newsletter may not be a major milestone, but it can probably be consid- ered to be significant. The newsletter has grown in size and this is the largest edition so far, much of the in- crease being due to the Chapter Reports, ably compiled by Fiona Fordyce. This edition has new section, Short Articles, that lets IMGA members know what others are doing. A Short Article does not have to be a completed piece of work and I encourage members to submit notes to say that “I am working on this …”. Reports of completed work and longer articles are also welcome. The Editorial Com- mittee has also discussed the idea of thematic newsletters and we are open to ideas. Anyone submitting material for the newsletter should read Section 8 on Newsletter Policy in the Medical Ge- ology Policy Book at: http://www.medicalgeology.org/pages/public/imga/Policy%20book.pdf. The Editor would like to note a couple of points from the policy: Although some review is carried out, the newsletter is, well … a newsletter, and does not claim to be, and is not a fully refereed journal. It is the author’s responsibility to ensure that material submitted is not under copyright or that a copyright holder has given formal permission to republish in the newsletter. Further information will be provided in the next newsletter. Published articles may be referenced using the IMGA Newsletter ISSN Number as “ISSN: 1651-5250”. The newsletter is scheduled to be published twice a year, in June and December, although publication may be delayed for various reasons. (for this issue, partly by the editor’s personal affairs following on his retirement!) Early submission is encouraged. Submission date for Publication date Articles Other material Newsletter March 15th April 15th June 15th Newsletter September 15th October 15th December 15th David Elliott, IMGA Newsletter Editor, [email protected] IMGA CONFERENCE LOGO IMGA is proud to announce the newly adapted logo for our International Confer- ence on Medical Geology. The logo was originally unveiled during the 4th Inter- national Conference on Medical Geology in Bari, Italy, and it is a contribution from the Italian Chapter on Medical Geology. The logo was designed based on an artistic expression from Giuseppe (Beppe) Fiore (right). The bottom part of the logo (in brown colour) symbolizes our planet Earth (Geology), the four semi- curved lines (in green) coming off the Earth symbolize the four elements (plants, water, animals and air), gaining their strength from the Earth. Symbolizing the medical side is the Rod of Asclepius (or the Aesculapius) displayed in the centre of the logo and demonstrating a direct and dynamic interaction with the Earth. Page 4 MEDICAL GEOLOGY NEWSLETTER CHAPTERS In order to expand and develop the IMGA community world-wide, IMGA is encouraging the establishment of Local Chapters (i.e. groups) within individual countries/regions.
Recommended publications
  • Message from the New Chairman
    Subcommission on Devonian Stratigraphy Newsletter No. 21 April, 2005 MESSAGE FROM THE NEW CHAIRMAN Dear SDS Members: This new Newsletter gives me the pleasant opportunity to thank you for your confidence which should allow me to lead our Devonian Subcommission successfully through the next four years until the next International Geological Congress in Norway. Ahmed El Hassani, as Vice-Chairman, and John Marshall, as our new Secretary, will assist and help me. As it has been our habit in the past, our outgoing chairman, Pierre Bultynck, has continued his duties until the end of the calendar year, and in the name of all the Subcommission, I like to express our warmest thanks to him for all his efforts, his enthusi- asm for our tasks, his patience with the often too slow progress of research, and for the humorous, well organized and skil- ful handling of our affairs, including our annual meetings. At the same time I like to thank all our outgoing Titular Members for their partly long-time service and I express my hope that they will continue their SDS work with the same interest and energy as Corresponding Members. The new ICS rules require a rather constant change of voting members and the change from TM to CM status should not necessarily be taken as an excuse to adopt the lifestyle of a “Devonian pensioner”. I see no reason why constantly active SDS members shouldn´t become TM again, at a later stage. On the other side, the rather strong exchange of voting members should bring in some fresh ideas and some shift towards modern stratigraphical tech- niques.
    [Show full text]
  • Geologists of Russian Origin in Latin America
    REVISTA DEL MUSEO DE LA PLATA 2018, Volumen 3, Número 2: 223-295 Geologists of Russian origin in Latin America P. Tchoumatchenco1 , A.C. Riccardi 2 , †M. Durand Delga3 , R. Alonso 4 , 7 8 M. Wiasemsky5 , D. Boltovskoy 6 , R. Charrier , E. Minina 1Geological Institute, Bulgarian Academy of Sciences Acad. G. Bonchev Str. Bl. 24, 1113 Sofia, Bulgaria, [email protected] 2Museo de La Plata, Facultad de Ciencias Naturales y Museo, Universidad Nacional de La Plata, Argentina, [email protected] 3Passed away August19, 2012 4Universidad Nacional de Salta, Argentina, [email protected] 581, Chemin du Plan de Charlet, F-74190 Passy, France, [email protected] 6Dep. Ecologia, Genetica y Evolucion, Fac. Ciencias Exactas y Naturales, Univ. de Buenos Aires, Argentina, [email protected] 7History of Geology Group, Sociedad Geológica de Chile, Santiago de Chile, [email protected] 8State Geological Museum “V.I.Vernadsky”, Mohovaya ul. 11/11, Moscow 125009, Russian Federation, [email protected] REVISTA DEL MUSEO DE LA PLATA / 2018, Volumen 3, Número 2: 223-295 / ISSN 2545-6377 ISSN 2545-6377 UNIVERSIDAD NACIONAL DE LA PLATA - FACULTAD DE CIENCIAS NATURALES Y MUSEO Revista del Museo de La Plata 2018 Volumen 3, Número 2 (Julio-Diciembre): 223-295 Geologists of Russian origin in Latin America P. Tchoumatchenco1, A.C. Riccardi2, †M. Durand Delga3, R. Alonso4, M. Wiasemsky5, D. Boltovskoy6, R. Charrier7, E. Minina8 1 Geological Institute, Bulgarian Academy of Sciences Acad. G. Bonchev Str. Bl. 24, 1113 Sofia, Bulgaria, [email protected] 2 Museo de La Plata, Facultad de Ciencias Naturales y Museo, Universidad Nacional de La Plata, Argentina, [email protected] 3 Passed away August19, 2012 4 Universidad Nacional de Salta, Argentina, [email protected] 5 81, Chemin du Plan de Charlet, F-74190 Passy, France, [email protected] 6 Dep.
    [Show full text]
  • A Viking-Age Settlement in the Hinterland of Hedeby Tobias Schade
    L. Holmquist, S. Kalmring & C. Hedenstierna-Jonson (eds.), New Aspects on Viking-age Urbanism, c. 750-1100 AD. Proceedings of the International Symposium at the Swedish History Museum, April 17-20th 2013. Theses and Papers in Archaeology B THESES AND PAPERS IN ARCHAEOLOGY B New Aspects on Viking-age Urbanism, c. 750-1100 AD. Proceedings of the International Symposium at the Swedish History Museum, April 17–20th 2013 Lena Holmquist, Sven Kalmring & Charlotte Hedenstierna-Jonson (eds.) Contents Introduction Sigtuna: royal site and Christian town and the Lena Holmquist, Sven Kalmring & regional perspective, c. 980-1100 Charlotte Hedenstierna-Jonson.....................................4 Sten Tesch................................................................107 Sigtuna and excavations at the Urmakaren Early northern towns as special economic and Trädgårdsmästaren sites zones Jonas Ros.................................................................133 Sven Kalmring............................................................7 No Kingdom without a town. Anund Olofs- Spaces and places of the urban settlement of son’s policy for national independence and its Birka materiality Charlotte Hedenstierna-Jonson...................................16 Rune Edberg............................................................145 Birka’s defence works and harbour - linking The Schleswig waterfront - a place of major one recently ended and one newly begun significance for the emergence of the town? research project Felix Rösch..........................................................153
    [Show full text]
  • Geothermal Field and Geothermal Resources, Country Update for Belarus
    European Geothermal Congress 2019 Den Haag, The Netherlands, 11-14 June 2019 Geothermal Field and Geothermal Resources, Country Update for Belarus Margarita Dubanevich1, Vladimir Zui2 1 Republican Unitary Enterprise “Research and Production Centre for Geology”, Kuprevich str, 7, 220141 Minsk, Republic of Belarus; 2 Belarusian State University, Nezavisimosti sq., 4, 220030 Minsk, Republic of Belarus [email protected] , [email protected] Keywords: Geothermics, geothermal energy, here. The maximal temperature recorded in the deepest terrestrial temperature distribution, heat flow, inclined Predrechitsa-1 borehole at the base of the geothermal resources, GSHP installations, country platform cover was around 135-140 ºC at the depth of update. 6.4 km in the Pripyat Trough. First heat pump installations were created in the middle of nineties of the past century and for the end of 2018, ABSTRACT around 250 geothermal installations were put into The geothermal investigations were started in Belarus operation in the country and a few similar geothermal since 50th of the previous century. The region belongs heating systems are under construction each year. All to the western part of the East European Platform. Its available installations are used for space heating and territory formed mostly by Precambrian crustal blocks simultaneously to produce warm water. The biggest with Paleozoic Pripyat Trough and the Podlaska-Brest geothermal installation of 1 MWth was put into Depression in southern part of the country. There are no operation at the Greenhouse Complex “Berestye” at the warm springs within the considered area. eastern suburb of Brest town in the west part of the country. All heat pump installations excluding the latter Since the time elapsed after the World Geothermal one use shallow depth intervals with low-enthalpy Congress 2016 the main efforts were directed to geothermal resources.
    [Show full text]
  • Middle Devonian Acanthodians from Belarus – New Data and Interregional Biostratigraphy
    Acta Geologica Polonica, Vol. XX (202X), No. X, pp. xxx–xxx DOI: 10.24425/agp.2020.134568 Middle Devonian acanthodians from Belarus – new data and interregional biostratigraphy DMITRY P. PLAX1 and MICHAEL NEWMAN2* 1 Belarusian National Technical University (BNTU), Nezavisimosti Avenue 65, 220013 Minsk, Republic of Belarus. 2 Vine Lodge, Vine Road, Johnston, Haverfordwest, SA62 3NZ Pembrokeshire, United Kingdom. Email: [email protected]. ORCID: 0000-0002-7465-3069 *Corresponding author ABSTRACT: Plax, D.P. and Newman, M. XXXX. Middle Devonian acanthodians from Belarus – new data and interregional biostratigraphy. Acta Geologica Polonica, XX (X), xxx–xxx. Warszawa. The Lower Devonian (Emsian) and Middle Devonian of Belarus contain assemblages of biostratigraphically useful faunal and floral microremains. Surface deposits are few, with most material being derived from bore- hole cores. Acanthodian scales are particularly numerous and comparison with scales from other regions of the Old Red Sandstone continent (Laurussia), specifically the Orcadian Basin of Scotland, the Baltic Region, Spitsbergen, and Severnaya Zemlya have demonstrated a lot of synonymy of acanthodian species between these areas. This is especially the case between Belarus, the Orcadian Basin and the Baltic Region, which has allowed us to produce an interregional biostratigraphic scheme, as well as to postulate marine connection routes between these areas. The acanthodian biostratigraphy of Belarus is particularly important as it is associated with spores and marine invertebrates, so giving the potential of more detailed correlations across not only the Old Red Sandstone continent, but elsewhere in the Devonian world. We also demonstrate that differences in preservation (e.g., wear and how articulated a specimen is) is one of the main reasons for synonymy.
    [Show full text]
  • Makhnach, A. A. Diagenetic Gypsum, Anhydrite and Halite in Non
    BALTICA Volume 21 Number 1-2 December 2008 : 25-39 Diagenetic gypsum, anhydrite and halite in non-evaporite deposits of Belarus Anatoliy A. Makhnach Makhnach, A. A., 2008. Diagenetic gypsum, anhydrite and halite in non-evaporite deposits of Belarus. Baltica, Vol. 21 (1-2), 25-39. Vilnius. ISSN 0067-3064. Abstract The location, morphology, geochemistry and genesis of diagenetic gypsum, anhydrite and halite spread in non-evaporite lithofacies in two different regions of Belarus are discussed in present paper. It is shown that diagenetic anhydrite, gypsum and halite could occur in normal marine, aqueoglacial, volcanogenic– sedimentary deposits in shallow or deep water environment and that the bearing rocks are not associated with the evaporating process. Mechanism of gypsum, anhydrite and halite formation in non–evaporite deposits has been studied in detail. Keywords Diagenetic gypsum, anhydrite, halite, Upper Proterozoic, Paleozoic, Northern and Middle Belarus, Prypiac’ Trough. Anatoliy A. Makhnach [[email protected]], Belarussian Research Geological Exploration Institute, Acad. V. Kuprevich Street 7, 220141 Minsk, Belarus. Manuscript submitted 4 August 2008; accepted 14 November 2008. INTRODUCTION sulfate is inherited from the sulfur composition of overlying parent evaporites, but is slightly heavier Diagenetic anhydrite, gypsum and halite are widespread due to the bacterial sulfate reduction in the course of in subevaporite and interevaporite strata of evaporite– the subsurface water–rock interaction. A wide range bearing basins. Two areas of the territory of Belarus of the 1,000 · Br/Cl ratio variations for the diagenetic were chosen to demonstrate that the above minerals halite testifies to repeated changing and mixing occur in shallow–water and deep–water normal marine brines of different salinities within subsaliferous and deposits, in aqueoglacial, volcanogenic–sedimentary intersaliferous formations.
    [Show full text]
  • Transboundary Sub Parts of Groundwater Bodies in the Pripyat and Dnieper River Basin of the Republic of Belarus
    European Union Water Initiative Plus for the Eastern Partnership Countries (EUWI+) Result 2 TRANSBOUNDARY SUB PARTS OF GROUNDWATER BODIES IN THE PRIPYAT AND DNIEPER RIVER BASIN OF THE REPUBLIC OF BELARUS Final report, December 2020 Transboundary sub parts of GWBs in Belarus Beneficiaries Ministry of Natural Resources and Environmental Protection of the Republic of Belarus Responsible EU member state consortium EUWI+ project leader Mr Alexander Zinke, Umweltbundesamt GmbH (AT) EUWI+ country representative in Belarus Mr Alexandr Stankevich Responsible international thematic lead expert Mr Andreas Scheidleder, Umweltbundesamt (AT) Responsible national thematic lead expert Ms Olga Vasneva, “The Institute of Geology” branch of the Republican Unitary Enterprise "Research and Production Center for Geology” Authors Ms Olga Berezko, Ms Olga Vasneva, Ms Elena Cherevach, Ms Olga Buinevich, Ms Tatiana Kononova, Mr Igor Vitsen, all “The Institute of Geology” branch of the Republican Unitary Enterprise "Research and Pro- duction Center for Geology" Disclaimer: The EU-funded program European Union Water Initiative Plus for Eastern Partnership Countries (EUWI+) is im- plemented by the United Nations Economic Commission for Europe (UNECE), the Organisation for Economic Co-operation and Development (OECD), both responsible for the implementation of Result 1, and an EU Mem- ber States Consortium comprising the Environment Agency Austria (UBA, Austria), the lead coordinator, and the International Office for Water (IOW, France), both responsible for the implementation of Results 2 and 3. The program is co-funded by Austria and France through the Austrian Development Agency and the French Artois-Picardie Water Agency. This document was produced with the financial assistance of the European Union.
    [Show full text]
  • New Findings of Cenozoic Marine Invertebrate Fauna
    Общая биология Выпуск 6/2018 UDК 563.1.+564.13 Yu. U. Zaika1, A. V. Krylov2, N. Yu. Anikina3 1Unitary Enterprise “Geoservice”, 53, Janki Maura str., 220036; Belarusian State Technical University, Minsk, Belarus +375(44)709 37 36, [email protected] 2Joint-Stock Company “Polargeo”, Vasiljevski Island, 24th Line, 3—7, Building 20-Б, 199106, St. Petersburg, Russia, +8 10 7(812)334 56 24; [email protected] 3Central Mining and Geological Laboratory Ltd., 167000, Komi Republic, Russian Federation, Syktyvkar, Оktiabrsky Ave, 131/6, [email protected] NEW FINDINGS OF CENOZOIC MARINE INVERTEBRATE FAUNA FROM У THE WESTERN PART OF THE EAST-EUROPEAN PLAIN Г New findings of marine faunal remains from Quaternary and possibly older Cenozoic strata from different regions of Belarus as well as of the European part of Russia are reported in the present article. Despite the prolonged discussion about the genesis of surficial deposits of the north-western part of the East European Plain,р in Belarus the concept of continental and predominantly glacial origin of unconsolidated sediments of the upper part of the sedimentary cover is usually considered as firmly established and is not disputed in regional-geological literature.а New paleontological evidence suggesting a marine nature of several kinds of these deposits was recently obtained. In some localities of varved and thin-bedded clays and silts, which are considered in the framework of the glacial theory as glacial-lacustrine, marine microfauna was discovered. The obtained results have the potential to become a basisБ for a revision of the common paleogeographic concept associating these sediments with Pleistocene glacial lakes.
    [Show full text]
  • Утверждено Постановление Бюро Президиума Национальной Академии Наук Беларуси 27.12.2017 № 489
    УТВЕРЖДЕНО Постановление Бюро Президиума Национальной академии наук Беларуси 27.12.2017 № 489 ПЕРАЛІК навуковых, навукова-тэхнічных і навукова-практычных мерапрыемстваў, плануемых да правядзення арганізацы- ямі Нацыянальнай акадэміі навук Беларусі ў 2018 годзе ПЕРЕЧЕНЬ научных, научно-технических и научно-практических мероприятий, планируемых к проведению организациями Национальной академии наук Беларуси в 2018 году LIST of Conferences, Symposia and Schools Planning to Carry Out by Organizations of the National Academy of Sciences of Belarus in 2018 Статус мероприятия; его наименование; организация(и), № ответственная(ые) за проведение; место и время проведения; п.п. контактные адрес, телефон, факс, e-mail Республиканские мероприятия 1 Рэспубліканскі навукова-практычны семінар «Любаншчына на гісторыка-культурнай карце Беларусі» Дзяржаўная навуковая ўстанова «Цэнтр даследаванняў беларускай культуры, мовы і літаратуры Нацыянальнай акадэміі навук Беларусі», 220072, г. Мінск, вул. Сурганава, 1, корп. 2 Мінская вобл., Любань, 24–25 красавіка Тэл.: +375 (17) 284-15-31; Факс:+375 (17) 284-18-85 E-mail: [email protected] Любанскі раённы выканаўчы камітэт 223812, г. Любань, вул. Першамайская, 24а Факс: +375 (17) 945-51-41; E-mail: [email protected] Республиканский научно-практический семинар «Любанщина на историко-культурной карте Беларуси» Государственное научное учреждение «Центр исследований белорусской культуры, языка и литературы Национальной академии наук Беларуси», 220072, г. Минск, ул. Сурганова, 1, корп. 2 2 Статус мероприятия, его наименование, организация(и), № п.п. ответственная(ые) за проведение, место и дата проведения, контактные телефон, факс, e-mail Минская обл., Любань, 24–25 апреля Тел.: +375 (17) 284-15-31; Факс:+375 (17) 284-18-85; E-mail: [email protected] Любанский районный исполнительный комитет 223812, г. Любань, ул.
    [Show full text]
  • Devonian Stratigraphy in Estonia: Current State and Problems
    Estonian Journal of Earth Sciences, 2012, 61, 1, 33–47 doi: 10.3176/earth.2012.1.03 Devonian stratigraphy in Estonia: current state and problems Elga Mark-Kurika and Anne Põldvereb a Institute of Geology at Tallinn University of Technology, Ehitajate tee 5, 19086 Tallinn, Estonia; [email protected] b Tartu Regional Department, Geological Survey of Estonia, Rõõmu tee 1, 51013 Tartu, Estonia; [email protected] Received 3 February 2011, accepted 7 November 2011 Abstract. An updated version of the Devonian stratigraphical chart of Estonia with comments is presented. Estonian regional stratigraphical units are correlated with the standard conodont zonation and miospore zonation, used in the western part of the East European Platform. The fossil fish zonations, largely accepted in the Main Devonian Field, are discussed. Differences in the position of series and stage boundaries and age determination of regional units in the Baltic area, Belarus and NW Russia are dealt with. Two key markers for the correlation of the Middle Devonian of the Baltic area and Scotland, based mainly on placoderms, are described. Special attention is paid to occurrences of inarticulate brachiopods and finds of rare articulate brachiopods in siliciclastic rocks of the Baltic area, indicating their marine origin. Key words: Devonian, biozones, regional stratigraphy, correlations, Estonia. INTRODUCTION some drill cores in South Estonia and the latter occurs only in a limited area of SE Estonia. In contrast, the Devonian deposits on the territory of Estonia form a Middle Devonian (Eifelian, Givetian) is well developed. comparatively minor part of the extensive Devonian It is exposed across a broad outcrop area in the whole of strata on the East European (Russian) Platform.
    [Show full text]
  • Palaeogeographic Reconstructions of the Natural Environment in Southeast Belarus During the Bathonian–Oxfordian Ages V
    ISSN 01458752, Moscow University Geology Bulletin, 2015, Vol. 70, No. 2, pp. 159–170. © Allerton Press, Inc., 2015. Original Russian Text © V.V. Makhnach, E.M. Tesakova, 2015, published in Vestnik Moskovskogo Universiteta. Geologiya, 2015, No. 2, pp. 85–97. Palaeogeographic Reconstructions of the Natural Environment in Southeast Belarus during the Bathonian–Oxfordian Ages V. V. Makhnacha and E. M. Tesakovab aBelarus State University, Department of Geography, Minsk, Belarus bMoscow State University, Department of Geology, Moscow, Russia email: [email protected], [email protected] Received October 8, 2014 Abstract—Palaeogeographic reconstructions of the natural environments in Southeast Belarus during the Bathonian–Oxfordian were carried out using the method of conjugate analysis of facies, sedimentology, pale ontology, and geochemistry. The results show the existence of lagoon environments at the end of the Batho nian with a gradually growing sea gulf in the Early Callovian and general marine regime developed by the end of Early Callovian that continued during the Middle–Late Callovian and Oxfordian. Transgression of the sea and intervention of marine faunas occurred in three directions: from Western Europe, Ukraine, and Central Russia. Mollusc and ostracod faunas had mixed characteristics with dominance of the Tethyan elements over the Arctic ones. In the Early Oxfordian the Eastern Paleobasin of Belarus had a stable connection with the Middle Russian Sea. Keywords: Jurassic, Mollusca, Ostracoda, palaeogeography, Belarus DOI: 10.3103/S0145875215020064 INTRODUCTION The modern understanding of the Jurassic paleo geography of the northwestern part of the Dniepr– Jurassic deposits remained poorly known in Donets Basin (East Belarus) was built via summaries on Belarus until 1955.
    [Show full text]
  • Revista Del Museo De La Plata
    REVISTA DEL MUSEO DE LA PLATA 2018, Volumen 3, Número 2: 223-295 Geologists of Russian origin in Latin America P. Tchoumatchenco1 , A.C. Riccardi 2 , †M. Durand Delga3 , R. Alonso 4 , 7 8 M. Wiasemsky5 , D. Boltovskoy 6 , R. Charrier , E. Minina 1Geological Institute, Bulgarian Academy of Sciences Acad. G. Bonchev Str. Bl. 24, 1113 Sofia, Bulgaria, [email protected] 2Museo de La Plata, Facultad de Ciencias Naturales y Museo, Universidad Nacional de La Plata, Argentina, [email protected] 3Passed away August19, 2012 4Universidad Nacional de Salta, Argentina, [email protected] 581, Chemin du Plan de Charlet, F-74190 Passy, France, [email protected] 6Dep. Ecologia, Genetica y Evolucion, Fac. Ciencias Exactas y Naturales, Univ. de Buenos Aires, Argentina, [email protected] 7History of Geology Group, Sociedad Geológica de Chile, Santiago de Chile, [email protected] 8State Geological Museum “V.I.Vernadsky”, Mohovaya ul. 11/11, Moscow 125009, Russian Federation, [email protected] REVISTA DEL MUSEO DE LA PLATA / 2018, Volumen 3, Número 2: 223-295 / ISSN 2545-6377 ISSN 2545-6377 UNIVERSIDAD NACIONAL DE LA PLATA - FACULTAD DE CIENCIAS NATURALES Y MUSEO Revista del Museo de La Plata 2018 Volumen 3, Número 2: 223-295 Geologists of Russian origin in Latin America P. Tchoumatchenco1, A.C. Riccardi2, †M. Durand Delga3, R. Alonso4, M. Wiasemsky5, D. Boltovskoy6, R. Charrier7, E. Minina8 1 Geological Institute, Bulgarian Academy of Sciences Acad. G. Bonchev Str. Bl. 24, 1113 Sofia, Bulgaria, [email protected] 2 Museo de La Plata, Facultad de Ciencias Naturales y Museo, Universidad Nacional de La Plata, Argentina, [email protected] 3 Passed away August19, 2012 4 Universidad Nacional de Salta, Argentina, [email protected] 5 81, Chemin du Plan de Charlet, F-74190 Passy, France, [email protected] 6 Dep.
    [Show full text]