Размеры Тела Шерстистого Мамонта Mammuthus Primigenius (Blumenbach) Второй Половины Позднего Плейстоцена Севера Восточной Сибири Г.Г

Total Page:16

File Type:pdf, Size:1020Kb

Размеры Тела Шерстистого Мамонта Mammuthus Primigenius (Blumenbach) Второй Половины Позднего Плейстоцена Севера Восточной Сибири Г.Г ПРИРОДНЫЕ РЕСУРСЫ АРКТИКИ И СУБАРКТИКИ, 2021, Т. 26, № 1 УДК562/569:566/569 DOI10.31242/2618-9712-2021-26-1-4 Размеры тела шерстистого мамонта Mammuthus primigenius (Blumenbach) второй половины позднего плейстоцена севера Восточной Сибири Г.Г.Боескоров Институт геологии алмаза и благородных металлов СО РАН, Якутск, Россия [email protected] Аннотация. Проанализированы сведения о размерах тела шерстистого мамонта Mammuthus primigenius (Blumenbach) второй половины позднего плейстоцена севера Восточной Сибири (Яку- тия, п-ов Таймыр, западная Чукотка). Статья основана на оригинальных данных автора, прини- мавшего участие в исследовании морфологических особенностей замороженных останков мумий и скелетов мамонтов, найденных на территории Якутии за последние 30 лет: Чурапчинский, Максу- нуохский, Юкагирский мамонты; часть скелета мамонта с р. Зимовье (остров Большой Ляховс- кий). Отдельно измерен скелет Тирехтяхского мамонта. Кроме того, проанализированы литера- турные данные по размерам тела шерстистого мамонта второй половины позднего плейстоцена Восточной Сибири и других регионов. Предыдущими исследователями отмечалось, что высота в холке взрослых самцов M. primigenius с территории Якутии и Таймыра близка таковой самцов ази- атского (индийского) слона Elephas maximus L. Отсюда был сделан вывод, что и общие размеры тела у шерстистого мамонта схожи с таковыми азиатского слона. В данной статье, основанной на более обширном материале, показано, что хотя шерстистый мамонт действительно был очень схож по высоте в холке с современным E. maximus, в то же время тело у него было в среднем длин- нее, голова больше, т. е. пропорции тела у этих видов были разными. По-видимому, особенности пропорций тела шерстистого мамонта способствовали его лучшему выживанию в условиях ледни- кового периода. Ключевые слова:шерстистыймамонт,Mammuthus primigenius,позднийплейстоцен,размеры тела,ВосточнаяСибирь.. Благодарности. Работа выполнена в рамках проекта № 0381-2019-0002 по госзаданию ИГАБМ СО РАН. Введение кимобразом,шерстистыймамонтбылвысокоспе- Запоследниедесятилетияврезультатеизуче- циализированнымвидоммамонтовогобиома. нияновыхнаходокиприменениясовременных ОпираясьнаэкогеографическоеправилоБерг- методовисследованияполученфактическийма- мана,можнопредположить,чтомамонты,оби- териал,позволяющийболееобоснованносудить тавшиевусловияххолодногоклиматасеверных оприспособленияхшерстистогомамонтакусло- широт, были крупнее современных слонов. Так виямсуществованияварктическойисубаркти- считалинекоторыеспециалистыпохоботным[7]. ческой «тундростепи» позднего плейстоцена. Этосправедливовотношениигигантскоготрогон- Mummuthus primigeniusобладалкомплексомспе- териевогомамонтаMammuthus trogontherii(Pohlig, цифическиханатомо-морфологических(густая 1889),жившеговраннемисреднемплейстоцене, длиннаятрехъяруснаяшерсть,маленькиеуши, высотавхолкеукоторогодостигала4[8]идаже короткий хвост, жировой «горб», «капюшон- 4,5м[9,10].Болеепозднийшерстистыймамонт, ное»расширениенахоботе,широкиеподошвы существовавший во второй половине среднего ног)[1–5]ифизиологических(пониженнаячув- плейстоценаивпозднемплейстоцене,неимел ствительностькхолоду,своеобразныйлипидный столькрупныхразмеров.Ранееужеотмечалось, обмен)[6]идиоадаптаций,обеспечивавшихши- чтовысотавхолкевзрослыхсамцовM. primige- рокоераспространениеданноговидавСеверной niusстерриторииЯкутиииТаймыраварьирует Голарктикевтечениедлительноговремени.Та- от250до308см[1,5]иприближаетсяктаковой 38 ©БоескоровГ.Г.,2021 РАЗМЕРЫТЕЛАШЕРСТИСТОГОМАМОНТАMAMMUTHUS PRIMIGENIUS(BLUMENBACH) самцов азиатского (индийского) слона Elephas Результаты и обсуждение maximusL.,1758:250–320см[11].Высотавхол- Совокупные данные по размерам скелетов кесамцовафриканскогосаванновогослонаLox- (или их частей) взрослых самцов шерстистого odonta africana (Blum., 1797) намного больше, мамонтастерриторииВосточнойСибири(Яку- 310–442см[7].АфриканскийлеснойслонLox- тия,п-овТаймыр,западнаяЧукотка)представ- odonta cyclotis(Matschie,1900)наименьшийпо лены в табл. 1 и 2. Взрослые (старше 30 лет) размерам–высотавхолкевзрослыхсамцовэто- самцы M. primigenius, измеренные с достаточ- говидасоставляет240–300см[12].Однакодан- нойточностью,имеливысотувхолке260–320см ныепоразмерамтеламамонтоввуказанныхвыше (М = 284,5 см; n = 8). Дополняют эти данные работахбылиоснованынавесьмаограниченном остаткискелетов,накоторыхреконструирована материале,измерениитрехскелетовмамонтов– высота в холке: примерно от 270 до 300 см Адамса,БерезовскогоиТаймырского. (n=7).Этизначениясоответствуютпределамиз- Кнастоящемувременинайденыиисследова- менчивостивысотывхолкеазиатскогослона, ныновыеостаткискелетовизамороженныхму- указаннымДж.ШошанииДж.Айзенбергом[11]– мий шерстистого мамонта, измерения которых 250–320 см и сходны с нашими измерениями позволяютболееобоснованноохарактеризовать E. maximus –261–314см(М=295,0см;n=7). общиеразмерытелашерстистогомамонтавто- Р.Лайдеккер[17]приводилсведенияобазиат- ройполовиныпозднегоплейстоценасевераВос- скихслонахвысотойвхолке335,343и366см, точнойСибири. однако,эторедкиеисключения,рекордныераз- мерыдлявида.Остатковскелетовичастейтру- Материал и методы исследования повсамокмамонтовнайденогораздоменьше, Нами(илипринашемучастии)изученымор- чем самцов. По имеющимся данным [18–21] фологическиеособенностиостанковмамонтов, можноконстатировать,чтовысотавхолкеуса- найденныхнатерриторииЯкутиизапоследние мокшерстистогомамонтастерриториисевера 30лет:Чурапчинский[13];Максунуохский[14, ВосточнойСибирисоставлялаот216до240см, 15], Юкагирский [16] мамонты; часть скелета всреднем226,0см(n=5).Этотакжеоченьсход- мамонтасмягкимитканями,найденнаяв1994г. носвысотойвхолкевзрослыхсамокE. maximus вустьер.Зимовье(о.Бол.Ляховский).Отдельно (всреднем224см)[11]. измерен скелет Тирехтяхского мамонта, кратко Шерстистыймамонтстерриториисовремен- описанный П.А. Лазаревым [15], представлен- нойЕвропывторойполовиныпозднегоплейсто- ныйвэкспозицииЯкутскогообъединенногому- цена(вюрм)былвышеростом.Высотавхолке зеяисторииикультурынародовСевераим.Ем. скелетоввзрослыхсамцовизэтогорегионасо- Ярославского. ставляет: 290–295 см, Козлово, Пермская об- Крометого,намипроанализированыдоступ- ласть,Россия[22];340см,Климэуць,Молдо- ныелитературныеданныепоразмерамшерсти- ва[23];320см,Борна[24],Ален[25],Польх[26]. стогомамонтавторойполовиныпозднегоплей- 349см[27],Зигсдорф,все–Германия[27]. стоценаВосточнойСибири. Общаядлинатела(скелетов)взрослыхсам- Приисследованиитруповмамонтовисполь- цов шерстистого мамонта, измеренная по пря- зованыклассическиезоологическиеипалеонто- мой линии от рострума до основания хвоста, логические методы измерения крупных млеко- составляет 350–414 см (М = 381,0 см; n = 7). питающих. Аналогичныхизмеренийсовременныхслоновв Длясравнениянамиизученрядразмерныхосо- научной литературе нами не найдено, поэтому бенностейазиатскогослонанадомашнихособях мы использовали для сравнения оригинальные вТаиланде(2012и2013гг.;n=10)инамузей- измерения длины тела взрослых самцов азиат- ных чучелах, выставленных в Зоологическом скогослона,которыесоставилиот313до388см музее(г.Санкт-Петербург)ивМузееестествен- (М = 337,1 см; n = 7). Таким образом, хотя по нойисторииг.Пекин,Китай(n=2). высотевхолкешерстистыймамонтбылсходенс Исследованные скелеты и мумифицирован- азиатскимслоном,длинателаунегобылаболь- ныеостаткитруповмамонтовдатированырадио- ше. Для уточнения этих различий нами вычи- углеродным методом в различных геохроноло- слен индекс длины тела у мамонтов и слонов: гическихлабораторияхРоссиииЗарубежья. L(длинатела(скелета)попрямойлинииотро- 39 40 Таблица1 Размеры скелетов и бивней взрослых самцов шерстистого мамонта из Восточной Сибири каргинского интерстадиала позднего плейстоцена Table1 Sizes of skeletons and tusks in adult males of woolly mammoth from Eastern Siberia, Karginian interstadial, Late Pleistocene Длинаскелетапопрямой Названиескелетамамонта;место Высота Длинабивняпо Диаметрбивня линииотрострума находки;геологическийвозраст; вхолке,см большой(наружной) увыхода Радиоуглеродный Индивидуальный дооснованияхвоста,см источник Heightofthe кривизне,см изальвеолы,см возраст возраст Lengthoftheskeleton Thenameofthemammothskeleton; skeleton Thelengthofthetusk Thediameterofthe Radiocarbonage Individualage inastraightlinefrom placeofdiscovery;geologicalage; atwithers, alongthelarge(outer) tuskattheexitofthe therostrumtothebase asource incm curvature,incm alveoli,incm ofthetail,cm Хатангскиймамонт;р.Большая 45000±200, Старый, Неменее – По–видимому, 18–20 Рассоха,п-овТаймыр >53170лет 55–60лет 300 300–350 ПРИРОДНЫЕ KhatangaMammoth;Bolshaya назад Г.Г. RassokhaR.,TaimyrPeninsula[1] Березовскиймамонт; 31750±2500, Старый,около 265 385 Около160 12.2 БОЕСКОРОВ р.Березовка,притокр.Колыма, 44000±3500 50лет Якутия л.н. РЕСУРСЫ BerezovkaMammoth; BerezovkaR.,atributary oftheKolymaR.,Yakutia[1,5] АРКТИКИ Мамонтср.Зимовье, 42700±1300л.н. Взрослый Около300 – – – о.Бол.Ляховский,часть (ГИН-8813) скелета,1995г.Нашиданные MammothfromtheZimovyeR., И СУБАРКТИКИ, BolshoiLyakhovskyIsland, Yakutia,partoftheskeleton, 1995.Ourdata Шандринскиймамонт. 41170л.н. Старый,около Около300 Около400 – 18 Shandrinskymammoth[1,15] 60лет 2021, Тирехтяхскиймамонт;бассейн 32200; Взрослый 278 350 Около300 16 р.Индигирка 44540±1870л.н. Т. TirekhtyakhMammoth; 26, basinoftheIndigirkaR., № Yakutia[15,33] 1 МамонтКутоманова; 36950±4300; Взрослый, ~290 – – 19 р.Моховая,п-овТаймыр 35800±2700 40–50лет Kutomanov’sMammoth; MokhovayaR.,Taimyr Peninsula[22] Максунуохскиймамонт; >38500лет Вероятно, Около – – – р.Максунуоха,Якутия назад взрослый 270–280 MaksunuokhaMammoth; (ГИН-12720) MaksunuokhaR.,Yakutia[14] Энмынвеемскиймамонт; 32850±900л.н. Вероятно, Около300
Recommended publications
  • Complete Mitochondrial Genome of a Woolly Mammoth (Mammuthus Primigenius) from Maly Lyakhovsky Island (New Siberian Islands, Russia) and Its Phylogenetic Assessment
    Mitochondrial DNA Part B Resources ISSN: (Print) 2380-2359 (Online) Journal homepage: http://www.tandfonline.com/loi/tmdn20 Complete mitochondrial genome of a woolly mammoth (Mammuthus primigenius) from Maly Lyakhovsky Island (New Siberian Islands, Russia) and its phylogenetic assessment Igor V. Kornienko, Tatiana G. Faleeva, Natalia V. Oreshkova, Semyon E. Grigoriev, Lena V. Grigoreva, Evgeniy P. Simonov, Anna I. Kolesnikova, Yuliya A. Putintseva & Konstantin V. Krutovsky To cite this article: Igor V. Kornienko, Tatiana G. Faleeva, Natalia V. Oreshkova, Semyon E. Grigoriev, Lena V. Grigoreva, Evgeniy P. Simonov, Anna I. Kolesnikova, Yuliya A. Putintseva & Konstantin V. Krutovsky (2018) Complete mitochondrial genome of a woolly mammoth (Mammuthusprimigenius) from Maly Lyakhovsky Island (New Siberian Islands, Russia) and its phylogenetic assessment, Mitochondrial DNA Part B, 3:2, 596-598, DOI: 10.1080/23802359.2018.1473721 To link to this article: https://doi.org/10.1080/23802359.2018.1473721 © 2018 The Author(s). Published by Informa View supplementary material UK Limited, trading as Taylor & Francis Group. Published online: 18 May 2018. Submit your article to this journal Article views: 118 View Crossmark data Full Terms & Conditions of access and use can be found at http://www.tandfonline.com/action/journalInformation?journalCode=tmdn20 MITOCHONDRIAL DNA PART B: RESOURCES 2018, VOL. 3, NO. 2, 596–598 https://doi.org/10.1080/23802359.2018.1473721 MITOGENOME ANNOUNCEMENT Complete mitochondrial genome of a woolly mammoth (Mammuthus primigenius) from Maly Lyakhovsky Island (New Siberian Islands, Russia) and its phylogenetic assessment Igor V. Kornienkoa,b, Tatiana G. Faleevac, Natalia V. Oreshkovad,e, Semyon E. Grigorievf, Lena V. Grigorevaf, Evgeniy P.
    [Show full text]
  • Curriculum Vitae
    ADAM N ROUNTREY Research Museum Collection Manager University of Michigan Museum of Paleontology Research Museums Center 3600 Varsity Drive, Ann Arbor, MI 48108 +1 (734) 936 1385 [email protected] EDUCATION / ACADEMIC POSITIONS8 Research Museum Collection Manager, University of Michigan (2013-present) Research Assistant Professor, University of Western Australia (2012-2013) Postdoctoral Scholar, University of Michigan (2009-2012) PhD, Geology (2009) – University of Michigan “Life Histories of Juvenile Woolly Mammoths from Siberia: Stable Isotope and Elemental Analyses of Tooth Dentin” MS, Geology (2006) – University of Michigan BS (magna cum laude), Environmental Studies, (2003) – Randolph-Macon College PUBLICATIONS ( * = student paper) Moore, J., Rountrey, A., Scates Kettler, H. (2019). CS3DP: Developing Agreement for 3D Standards and Practices Based on Community Needs and Values. In Grayburn, J., Lischer-Katz, Z., Golubiewski-Davis, K., Ikeshoji-Orlati, V. (Eds.), 3D/VR in the Academic Library: Emerging Practices and Trends. Council on Library and Information Resources. Arlington, Virginia. *Ong, J.L., et al. (2018). A boundary current drives synchronous growth of marine fishes across tropical and temperate latitudes. Global Change Biology 24(5):1894-1903. DOI: 10.1111/gcb.14083. Holen, S.R., et al. (2018). Broken bones and hammerstones at the Cerutti Mastodon site: a reply to Haynes. PaleoAmerica 4(1):8-11. Holen, S.R., et al. (2018). Reply to Ferraro, J.V, et al. Contesting early archaeology in California. Nature 544:E3. DOI: 10.1038/nature25166. Holen, S.R., et al. (2017). Disparate Perspectives on Evidence from the Cerutti Mastodon Site: A Reply to Braje et al. PaleoAmerica DOI: 10.1080/20555563.2017.1396836.
    [Show full text]
  • LATE PLEISTOCENE and EARLY HOLOCENE WINTER AIR TEMPERATURES in KOTELNY ISLAND: RECONSTRUCTIONS USING STABLE ISOTOPES of ICE WEDGES Yu.K
    Kriosfera Zemli, 2019, vol. XXIII, No. 2, pp. 12–24 http://www.izdatgeo.ru DOI: 10.21782/EC2541-9994-2019-2(12-24) LATE PLEISTOCENE AND EARLY HOLOCENE WINTER AIR TEMPERATURES IN KOTELNY ISLAND: RECONSTRUCTIONS USING STABLE ISOTOPES OF ICE WEDGES Yu.K. Vasil’chuk1,2, V.M. Makeev3, A.A. Maslakov1, N.A. Budantseva1, A.C. Vasil’chuk1 1 Lomonosov Moscow State University, Faculty of Geography and Faculty of Geology, 1, Leninskie Gory, Moscow, 119991, Russia 2 Tyumen State University, 6, Volodarskogo str., Tyumen, 625003, Russia; [email protected] 3Russian State Hydrometeorological University, 98, Malookhtinsky prosp., St. Petersburg, 109017, Russia Late Pleistocene and Holocene winter air temperatures in Kotelny Island, northeastern Russian Arctic, have been reconstructed using oxygen isotope compositions of ice wedges and correlated with evidence of Late Pleistocene and Holocene climate variations inferred from pollen data. The δ18О values range exceeds 6 ‰ in Late Pleistocene ice wedges but is only 1.5 ‰ in the Holocene ones (–30.6 ‰ to –24.0 ‰ against –23.1 ‰ to –21.6 ‰, respectively). The Late Pleistocene mean January air temperatures in Kotelny Island were 10–12 °С lower than the respective present temperature. On the other hand, mean winter temperatures in cold substages during the Karga interstadial were colder than those during the Sartan glacial event. The Late Pleistocene– Holocene climate history included several warm intervals when air temperatures were high enough to maintain the existence of low canopy tree patches in Kotelny Island. Mean January air temperatures in the early Holocene were only 1.0–1.5 °С lower than now.
    [Show full text]
  • Quaternary International Xxx (2010) 1E23
    ARTICLE IN PRESS Quaternary International xxx (2010) 1e23 Contents lists available at ScienceDirect Quaternary International journal homepage: www.elsevier.com/locate/quaint Sedimentary characteristics and origin of the Late Pleistocene Ice Complex on north-east Siberian Arctic coastal lowlands and islands e A review L. Schirrmeister a,*, V. Kunitsky b, G. Grosse c, S. Wetterich a, H. Meyer a, G. Schwamborn a, O. Babiy b, A. Derevyagin d, C. Siegert a a Alfred Wegener Institute for Polar and Marine Research, Periglacial Research, Telegrafenberg A 43, 14471 Potsdam, Germany b Melnikov Permafrost Institute RAS SB, Merslotnaya Street, Yakutsk, Republic of Sakha, (Yakutia), 677010 Russia c Geophysical Institute, University of Alaska Fairbanks (UAF), 903 Koyukuk Drive, Fairbanks, AK 99775, USA d Moscow State University (MSU), Faculty of Geology Russia, Moscow 119899, Vorobievy Gory article info abstract Article history: The origin of Late Pleistocene ice-rich, fine-grained permafrost sequences (Ice Complex deposits) in arctic Available online xxx and subarctic Siberia has been in dispute for a long time. Corresponding permafrost sequences are frequently exposed along seacoasts and river banks in Yedoma hills, which are considered to be erosional remnants of Late Pleistocene accumulation plains. Detailed cryolithological, sedimentological, geochro- nological, and stratigraphical results from 14 study sites along the Laptev and East Siberian seacoasts were summarized for the first time in order to compare and correlate the local datasets on a large regional scale. The sediments of the Ice Complex are characterized by poorly-sorted silt to fine-sand, buried cryosols, TOC contents of 1.2e4.8 wt%, and very high ground ice content (40e60 wt% absolute).
    [Show full text]
  • Mammuthus Primigenius) Carcass from Maly Lyakhovsky Island (New Siberian Islands, Russian Federation
    Quaternary International 445 (2017) 89e103 Contents lists available at ScienceDirect Quaternary International journal homepage: www.elsevier.com/locate/quaint A woolly mammoth (Mammuthus primigenius) carcass from Maly Lyakhovsky Island (New Siberian Islands, Russian Federation) ** * Semyon E. Grigoriev a, , Daniel C. Fisher b, , Theodor Obada c, Ethan A. Shirley b, Adam N. Rountrey b, Grigory N. Savvinov d, Darima K. Garmaeva e, Gavril P. Novgorodov a, Maksim Yu. Cheprasov a, Sergei E. Vasilev f, Artemiy E. Goncharov g, h, i, Alexey Masharskiy i, Viktoriya E. Egorova e, Palmira P. Petrova e, Eya E. Egorova e, Yana A. Akhremenko e, Johannes van der Plicht j, Alexei A. Galanin k, Sergei E. Fedorov a, *** Evgeny V. Ivanov d, Alexei N. Tikhonov l, a, a Lazarev Mammoth Museum, Institute of Applied Ecology of the North, North-Eastern Federal University, Yakutsk, Russian Federation b Museum of Paleontology, University of Michigan, Ann Arbor, MI, USA c Institute of Zoology, Academy of Sciences of Moldova, Chis¸inau, Republic of Moldova d Institute of Applied Ecology of the North, North-Eastern Federal University, Yakutsk, Russian Federation e Medical Institute, North-Eastern Federal University, Yakutsk, Russian Federation f 3D Modelling and Virtual Reality Center, Institute of Physics and Technologies, North-Eastern Federal University, Yakutsk, Russian Federation g North-West State Medical University named after I.I. Mechnikov, Saint-Petersburg, Russian Federation h Institute of Experimental Medicine, Saint-Petersburg, Russian Federation i Saint
    [Show full text]
  • Rules for the Classification and Construction of Sea-Going Ships
    RUSSIAN MARITIME REGISTER OF SHIPPING RULES FOR THE CLASSIFICATION AND CONSTRUCTION OF SEA-GOING SHIPS PART I CLASSIFICATION Saint-Petersburg Edition 2019 Rules for the Classification and Construction of Sea-Going Ships of Russian Maritime Register of Shipping have been approved in accordance with the established approval procedure and come into force on 1 January 2019. The present edition of the Rules is based on the 2018 edition taking into account the amendments developed immediately before publication. The unified requirements, interpretations and recommendations of the International Association of Classification Societies (IACS) and the relevant resolutions of the International Maritime Organization (IMO) have been taken into consideration. The Rules are published in the following parts: Part I "Classification"; Part II "Hull"; Part III "Equipment, Arrangements and Outfit"; Part IV "Stability"; Part V "Subdivision"; Part VI "Fire Protection"; Part VII "Machinery Installations"; Part VIII "Systems and Piping"; Part IX "Machinery"; Part X "Boilers, Heat Exchangers and Pressure Vessels"; Part XI "Electrical Equipment"; Part XII "Refrigerating Plants"; Part XIII "Materials"; Part XIV "Welding"; Part XV "Automation"; Part XVI "Structure and Strength of Fiber-Reinforced Plastic Ships"; Part XVII "Distinguishing Marks and Descriptive Notations in the Class Notation Specifying Structural and Operational Particulars of Ships"; Part XVIII "Common Structural Rules for Bulk Carriers and Oil Tankers". The text of the Part is identical to that of the IACS Common Structural Rules; Part XIX "Additional Requirements for Structures of Container Ships and Ships, Dedicated Primarily to Carry their Load in Containers". The text of the Part is identical to IACS UR S11A "Longitudinal Strength Standard for Container Ships" (June 2015) and S34 "Functional Requirements on Load Cases for Strength Assessment of Container Ships by Finite Element Analysis" (May 2015).
    [Show full text]
  • 5.3.3 Onshore Coastal Studies - Coastal Dynamics at Key Sites of the New Siberian Lslands, Dmitry Laptev Strait, and Buor-Khaya Bay Mikhail N
    5 The New Siberian lslands The Ex~editionLENA 2002 5.3.3 Onshore coastal studies - coastal dynamics at key sites of the New Siberian lslands, Dmitry Laptev Strait, and Buor-Khaya Bay Mikhail N. Grigoriev, Feliks E. Are, Hans-W., Hubberten, Volker Rachold, Sergey 0. Razumov and Waldemar Schneider 5.3.3.1 lntroduction The main objective of the onshore coastal studies was to quantitatively assess coastal change rates (shoreline and cliff edge) focussing On erosive coasts. Twelve key sites along the coast of the Laptev and East-Siberian Seas were studied (Fig. 5.3.1-1): New Siberian Archipelago: north-eastern coast of Stolbovoy lsland (lce Complex and thermokarst deposits, ice-poor Pleistocene-Holocene coasts); northern coast of Kotelny lsland, Anisy Cape (lce Complex and thermokarst deposits, ice-poor Pleistocene-Holocene coasts); southern coast of Belkovsky Island, Skalisty Cape (rocky and other types of non-icy coasts); south-eastern coast of Kotelny Island, Khomurgunnakh River mouth area (lce Complex and thermokarst deposits, ice-poor Pleistocene-Holocene coasts); south-western coast of Bunge Land, Bunge polar station ("high sand" area, marine terrace); southern coast of Novoya Sibir Island, Wood Mountain Cape (rocky and other types of non-icy coasts, ice-poor Pleistocene coasts); south-western coast of Novoya Sibir Island (lce Complex and thermokarst deposits, ice-rich marine deposits, ice-poor Pleistocene- Holocene coasts); southern coast of Bunge Land ("low sand" area, marine terrace); north-western coast of Maly Lyakhovsky Island (lce Complex and thermokarst deposits, ice-poor Pleistocene-Holocene coasts); Dmitry Laptev Sfraif (mainland coasf): 10) Svyatoy Nos Cape (ice-poor and ice-rich Pleistocene-Holocene coasts, rocky and other types of non-icy coasts); II) Oyagossky Yar, mouth of Kondratev River area (lce Complex and thermokarst deposits); Buor-Khaya Bay: 12) north-western coast of Muostakh Island (lce Complex).
    [Show full text]
  • Supplement of the Genesis of Yedoma Ice Complex Permafrost – Grain-Size Endmember Modeling Analysis from Siberia and Alaska
    Supplement of E&G Quaternary Sci. J., 69, 33–53, 2020 https://doi.org/10.5194/egqsj-69-33-2020-supplement © Author(s) 2020. This work is distributed under the Creative Commons Attribution 4.0 License. Supplement of The genesis of Yedoma Ice Complex permafrost – grain-size endmember modeling analysis from Siberia and Alaska Lutz Schirrmeister et al. Correspondence to: Lutz Schirrmeister ([email protected]) The copyright of individual parts of the supplement might differ from the CC BY 4.0 License. Supplementary material Table S1: Overview of current hypotheses about the formation of Yedoma deposits during the last ~120 years of research. Origin Reference (1) Fluvial, alluvial and proluvial Fluvial and alluvial sediments of meandering rivers Katasonov (1975) Floodplain sediments Popov (1953, 1969) Proluvial slope sediments Romanovsky (1958) Slagoda (1991, 1993, 2004) Vtyurin et al.( 1957) (2) Aeolian Cryogenic-aeolian (“loess ice”) loess and Murton et al. (2015, 2017) retransported loess Péwé (1955, 1975) Péwé and Journaux (1983) Tomirdiaro (1982, 1996) Tomirdiaro et al. (1984) Tomirdiaro and Chernen’kiy (1987) Walter et al. (2007) (3) Lacustrine and palustrine Sediments of river deltas and swamps dammed by a Nagaoka (1994) shelf ice sheet Nagaoka et al. (1995) (4) Glacial and proglacial Buried remnants of glaciers Grosswald (1983, 1998) Proglacial deposits in basins dammed by a shelf Toll (1895) glacier Vollosowitch (1914) (5) Marine-estuarine-lagoon Near-shore marine and lagoon deposits Bol’shiyanov et al. (2013) (6) Polygenetic Polygenetic deposits as products of fluvial, lacustrine, Konishchev (1987) palustrine, slope, aeolian transport Sher (1997) Schirrmeister et al. (2011, 2013) (7) Nival -polygenetic Nival-polygenetic deposits as products of aeolian, Galabala (1997) fluvial, solifluction transport from melting extensive Kunitsky (1989), Kunitsky et al.
    [Show full text]
  • Jfossh Organic Matter Dnaracterftstncs Inn Permafrost
    JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 116, GOOM02, doi:IO.I02l)/2011JG001647, 2011 JFossH organic matter dnaracterftstncs inn permafrost deposits of tllne nortllneast Siberftan Arctic Lutz Schirrmeister, 1 Guido Grosse,2 Sebastian Wetterich, 1 Pier Paul Overduin, 1 Jens Strauss,' Edward A. G. Schuur,3 and Hans-Wolfgang Hubberten1 Received 7 January 2011; revised 15 May 2011; accepted I June 2011; published 13 September 2011. [1] Permafrost deposits constitute a large organic carbon pool highly vulnerable to degradation and potential carbon release due to global warming. Permafrost sections along coastal and river bank exposures in NE Siberia were studied for organic matter (OM) characteristics and ice content. OM stored in Quaternary permafrost grew, accumulated, froze, partly decomposed, and refroze under different periglacial environments, reflected in specific biogeochemical and cryolithological features. OM in permafrost is represented by twigs, leaves, peat, grass roots, and plant detritus. The vertical distribution of total organic carbon (TOC) in exposures varies from 0.1 wt % of the dry sediment in fluvial deposits to 45 wt% in Holocene peats. Variations in OM parameters are related to changes in vegetation, bioproductivity, pedogenic processes, decomposition, and sedimentation rates during past climate variations. High TOC, high C/N, and low 813C reflect less decomposed OM accumulated under wet, anaerobic soil conditions characteristic of interglacial and interstadial periods. Glacial and stadia! periods are characterized by less variable, low TOC, low C/N, and high 813C values indicating stable environments with reduced bioproductivity and stronger OM decomposition under dryer, aerobic soil conditions. Based on TOC data and updated information on bulk densities, we estimate average organic carbon inventories for ten different stratigraphic units in northeast Siberia, ranging from 7.2 kg C m-3 for Early Weichselian fluvial deposits, to 33.2 kg C m-3 for Middle Weichselian Ice Complex deposits, to 74.7 kg C m-3 for Holocene peaty deposits.
    [Show full text]
  • CV Theodor Obada
    Curriculum vitae Europass Personal information Last Name / First Name Obadă / Teodor Adress 96 Ialoveni Street, ap. 13, MD-2070, Chişinău, Republic of Moldova, Telephone +373 22284689 Mobile phone: +373 69572957 Fax E-mail address [email protected] Nationality Romanian Date of Birth 09. 12. 1961 Sex Male Position / Field of Activity Institute of Zoology, Republic of Moldova Zoology/Paleontology Work Experience Period 1987-1991 – higher specialist Position 1991-1993 – lower scientific researcher 1993-present – scientific researcher Main activities and responsibility The phylogeny, morphology and taxonomy of the Order Proboscidea during the Neogene and Quaternary; the taxonomy, paleobiogeography and phylogeny of large mammals from the Neogene and Quaternary of Europe; the principles of zoological nomenclature; conservation of paleontological specimens in museum collections. Employer name and address Institute of Zoology, Academy of Sciences of Moldova, 1 Academiei Street, Chişinău, MD-2028, Republic of Moldova; National Museum of Ethnography and Natural History of Moldova, 82 Mihail Kogălniceanu Street, Chişinău, MD-2029, Republic of Moldova. Business or sector Scientific research Education and training Period 1982-1987 Bachelor of Science in Geography and Biology Qualification / Diploma Pedagogical Institute „T.G. Şevcenco”, Tiraspol, Faculty of Geography, Geography and Biology teacher Main studied topics / professional skills 1991- 1994, The study of systematics and biostratigraphy of the Order Proboscidea acquired The name and type of education The Institute of Zoology, the Academy of Sciences of Moldova provider Level in national or international Research - teaching classification Teaching in higher academic Course of Anthropology at the Faculty of Psychology and Special Psychopedagogy, institutions Ion Creangă Pedagogical University, Chișinău, 1993. Period 1982-1987 Qualification / Diploma Geography and Biology teacher‚ Bachelor of Science Diploma Main studied topics / professional skills acquired Geology-paleontology/ Terrestrial Vertebrate Zoology.
    [Show full text]
  • Mercury in Hair of Mammoth and Other Prehistorical Mammals As a Proxy of Hg Level in the Environment Associated with Climate Changes
    applied sciences Article Mercury in Hair of Mammoth and Other Prehistorical Mammals as a Proxy of Hg Level in the Environment Associated with Climate Changes Stella Eyrikh 1,* , Gennady Boeskorov 2 , Tatyana Serykh 1, Marina Shchelchkova 3 and Tatyana Papina 1 1 Institute for Water and Environmental Problems, Siberian Branch of the Russian Academy of Science SB RAS, 656038 Barnaul, Russia; [email protected] (T.S.); [email protected] (T.P.) 2 Diamond and Precious Metals Geology Institute, Siberian Branch of the Russian Academy of Science, 677890 Yakutsk, Russia; [email protected] 3 Biological Department, Institute of Natural Sciences, M.K. Ammosov’s North-Eastern Federal University, 677000 Yakutsk, Russia; [email protected] * Correspondence: [email protected]; Tel.: +7-385-224-8007 Received: 5 October 2020; Accepted: 30 November 2020; Published: 3 December 2020 Abstract: The paper presents the first results of Hg determination in the hair of prehistorical animals (woolly mammoth, steppe bison, and woolly rhino). Hair of prehistorical mammals can be used as an archive that preserves changes of environmental pollution at the paleoscale. The aim of our study was to assess the levels of Hg exposure of ancient animals and to understand whether Hg concentration in hair could be used as a proxy indicating changes of mercury levels in the environment following global climate changes. We assessed changes of Hg exposure recorded in hairs of seven specimens of mammoth fauna mammals that inhabited the Yakutia region in the period from 45 to 10 ka yr BP. Hg concentrations in hair varied from 0.017 to 0.177 µg/g; the lowest Hg concentration were determined in older specimens (45–33 kyr yr BP).
    [Show full text]
  • Reproductive Life Histories of Mammoths by Joseph Jameel El Adli
    Reproductive Life Histories of Mammoths by Joseph Jameel El Adli A dissertation submitted in partial fulfillment of the requirements for the degree of Doctor of Philosophy (Earth and Environmental Sciences) in the University of Michigan 2018 Doctoral Committee: Professor Daniel C. Fisher, Chair Professor Catherine Badgley Professor Emeritus Philip D. Gingerich Professor Kyger C Lohmann Associate Professor Jeffery A. Wilson Joseph J. El Adli [email protected] ORCID iD: 0000-0002-3989-5409 © Joseph J. El Adli 2018 DEDICATION To all those I’ve met along the way. ii ACKNOWLEDGEMENTS Looking back on the five years of work that went into assembling this body of research, it is impossible (and would quite frankly be disingenuous) for me to treat this as anything but the result of a collective effort. Whether through discussions of methods and results, direct contributions to projects, or just sheer moral support, I have completed this document carried on the backs of many individuals whom I would like to thank here. My gratitude for your presence in my life is greater than you can know. First and foremost, I would like to thank my advisor, Dan Fisher, for giving me the chance to work on such fantastic material and teaching me new, creative methods of understanding past life. Dan’s guidance, insights, support, and discussions have immensely improved how I think about conducting scientific research and how I communicate my work to others. I am indebted to Dan for the many opportunities that he has provided for me to work in the field and travel to other countries to present my work.
    [Show full text]