Mercury in Hair of Mammoth and Other Prehistorical Mammals As a Proxy of Hg Level in the Environment Associated with Climate Changes
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Evolution and Extinction of the Giant Rhinoceros Elasmotherium Sibiricum Sheds Light on Late Quaternary Megafaunal Extinctions
ARTICLES https://doi.org/10.1038/s41559-018-0722-0 Evolution and extinction of the giant rhinoceros Elasmotherium sibiricum sheds light on late Quaternary megafaunal extinctions Pavel Kosintsev1, Kieren J. Mitchell2, Thibaut Devièse3, Johannes van der Plicht4,5, Margot Kuitems4,5, Ekaterina Petrova6, Alexei Tikhonov6, Thomas Higham3, Daniel Comeskey3, Chris Turney7,8, Alan Cooper 2, Thijs van Kolfschoten5, Anthony J. Stuart9 and Adrian M. Lister 10* Understanding extinction events requires an unbiased record of the chronology and ecology of victims and survivors. The rhi- noceros Elasmotherium sibiricum, known as the ‘Siberian unicorn’, was believed to have gone extinct around 200,000 years ago—well before the late Quaternary megafaunal extinction event. However, no absolute dating, genetic analysis or quantita- tive ecological assessment of this species has been undertaken. Here, we show, by accelerator mass spectrometry radiocarbon dating of 23 individuals, including cross-validation by compound-specific analysis, that E. sibiricum survived in Eastern Europe and Central Asia until at least 39,000 years ago, corroborating a wave of megafaunal turnover before the Last Glacial Maximum in Eurasia, in addition to the better-known late-glacial event. Stable isotope data indicate a dry steppe niche for E. sibiricum and, together with morphology, a highly specialized diet that probably contributed to its extinction. We further demonstrate, with DNA sequencing data, a very deep phylogenetic split between the subfamilies Elasmotheriinae and Rhinocerotinae that includes all the living rhinoceroses, settling a debate based on fossil evidence and confirming that the two lineages had diverged by the Eocene. As the last surviving member of the Elasmotheriinae, the demise of the ‘Siberian unicorn’ marked the extinction of this subfamily. -
Vast Atmospheric Cold Traps Within the Large Ringed Topographic Features in Ne Siberia: Implication for Mars
Third Mars Polar Science Conference (2003) 8117.pdf VAST ATMOSPHERIC COLD TRAPS WITHIN THE LARGE RINGED TOPOGRAPHIC FEATURES IN NE SIBERIA: IMPLICATION FOR MARS. G. A. Burba, Vernadsky Institute of Geochemistry and Analytical Chemistry, 19 Kosygin St., Moscow 119991, Russia e-mail: [email protected] Introduction: The ridges within the vast mountain plained that each of these “cold poles” is located country of the NE Siberia have been revealed recently within the lower areas at the central parts of the large to comprise two giant ring structures (RS), 500 and ring structures (intermountain basins), which works as 400 km in diameter [1] . Such evidence is a new look a giant cold traps being enclosed within a ring wall of on the general topographic structure of the area and mountain ridges. Such situation could lead to the cir- could be of importance for climatic consequences.The cumstances of the temperature inversion in the near- central lower areas of these structures, which are en- surface layer of the atmosphere. closed within a ring wall of mountain ridges, work as Implication for Mars: Couldn’t the similar situa- giant “cold traps” for the atmospheric air. During the tion with the air temperature take place during the win- winter seasons the temperature inversion in the near- ter season within the craters and large basins in the surface layer of the atmosphere take place there. polar regions of Mars? Topographic description: The highest area of the References: [1] Burba G. A. (1995) LPSC XXVI, North-East Siberia, Russia, consists of the mountain 189-190. [2] Atlas SSSR (1984) Map “Air tempera- ridges arranged as the two adjacent RS. -
Matheus Souza Lima Ribeiro
Palaeogeography, Palaeoclimatology, Palaeoecology 392 (2013) 546–556 Contents lists available at ScienceDirect Palaeogeography, Palaeoclimatology, Palaeoecology journal homepage: www.elsevier.com/locate/palaeo Climate and humans set the place and time of Proboscidean extinction in late Quaternary of South America Matheus Souza Lima-Ribeiro a,b,⁎, David Nogués-Bravo c,LeviCarinaTerribilea, Persaram Batra d, José Alexandre Felizola Diniz-Filho e a Departamento de Ciências Biológicas, Universidade Federal de Goiás, Campus Jataí, Cx. Postal 03, 75804-020 Jataí, GO, Brazil b Programa de Pós-graduação em Ecologia e Evolução, Universidade Federal de Goiás, Cx. Postal 131, 74001-970 Goiânia, GO, Brazil c Centre for Macroecology, Evolution and Climate, University of Copenhagen, Universitetsparken 15, 2100, Denmark d Department of Geology, Greenfield Community College, Greenfield, MA 01301, USA e Departamento de Ecologia, ICB, Universidade Federal de Goiás, Cx. Postal 131, 74001-970 Goiânia, GO, Brazil article info abstract Article history: The late Quaternary extinctions have been widely debated for a long time, but the varying magnitude of Received 18 April 2013 human vs. climate change impacts across time and space is still an unresolved question. Here we assess Received in revised form 7 October 2013 the geographic range shifts in response to climate change based on Ecological Niche Models (ENMs) and Accepted 21 October 2013 modeled the timing for extinction under human hunting scenario, and both variables were used to explain Available online 30 October 2013 the extinction dynamics of Proboscideans during a full interglacial/glacial cycle (from 126 ka to 6 ka) in South America. We found a large contraction in the geographic range size of two Proboscidean species stud- Keywords: Late Quaternary extinctions ied (Cuvieronius hyodon and Notiomastodon platensis) across time. -
Distinguishing Extant Elephants Ivory from Mammoth Ivory Using a Short
www.nature.com/scientificreports OPEN Distinguishing extant elephants ivory from mammoth ivory using a short sequence of cytochrome b gene Jacob Njaramba Ngatia1, Tian Ming Lan2,3,4, Yue Ma1,5, Thi Dao Dinh1, Zhen Wang1,5, Thomas D. Dahmer6 & Yan Chun Xu1,5,7* Trade in ivory from extant elephant species namely Asian elephant (Elephas maximus), African savanna elephant (Loxodonta africana) and African forest elephant (Loxodonta cyclotis) is regulated internationally, while the trade in ivory from extinct species of Elephantidae, including woolly mammoth, is unregulated. This distinction creates opportunity for laundering and trading elephant ivory as mammoth ivory. The existing morphological and molecular genetics methods do not reliably distinguish the source of ivory items that lack clear identifcation characteristics or for which the quality of extracted DNA cannot support amplifcation of large gene fragments. We present a PCR-sequencing method based on 116 bp target sequence of the cytochrome b gene to specifcally amplify elephantid DNA while simultaneously excluding non-elephantid species and ivory substitutes, and while avoiding contamination by human DNA. The partial Cytochrome b gene sequence enabled accurate association of ivory samples with their species of origin for all three extant elephants and from mammoth. The detection limit of the PCR system was as low as 10 copy numbers of target DNA. The amplifcation and sequencing success reached 96.7% for woolly mammoth ivory and 100% for African savanna elephant and African forest elephant ivory. This is the frst validated method for distinguishing elephant from mammoth ivory and it provides forensic support for investigation of ivory laundering cases. -
Spiders (Aranei) from Oymyakon, the Cold Pole of the Northern Hemisphere (Yakutia, Siberia)
Arthropoda Selecta 13 (12): 6975 © ARTHROPODA SELECTA, 2004 Spiders (Aranei) from Oymyakon, the cold pole of the northern hemisphere (Yakutia, Siberia) Ïàóêè (Aranei) Îéìÿêîíà, ïîëþñà õîëîäà ñåâåðíîãî ïîëóøàðèÿ (ßêóòèÿ) Yuri M. Marusik1, Seppo Koponen2 & Nadezhda K. Potapova3 Þ.Ì. Ìàðóñèê, Ñ. Êîïîíåí, Í.Ê. Ïîòàïîâà 1Institute for Biological Problems of the North, Russian Academy of Sciences, Portovaya Str. 18, Magadan 685000 Russia; E-mail: [email protected] 1 Èíñòèòóò áèîëîãè÷åñêèõ ïðîáëåì Ñåâåðà ÄÂÎ ÐÀÍ, Ïîðòîâàÿ 18, Ìàãàäàí 685000 Ðîññèÿ. 2Zoological Museum, Centre for Biodiversity, University of Turku, FI-20014 Turku, Finland; E-mail: [email protected] 3Institute for Biological Problems of Cryolithozone, Siberian Division of the Russian Academy of Sciences, Prospect Lenina 41, Yakutsk 677891, Russia; E-mail: [email protected] 3 Èíñòèòó áèîëîãè÷åñêèõ ïðîáëåì êðèîëèòîçîíû ÑÎ ÐÀÍ, ïð. Ëåíèíà 41, ßêóòñê 677891 Ðîññèÿ. KEY WORDS: Araneae, spiders, faunistic records, distribution patterns, Yakutia. ÊËÞ×ÅÂÛÅ ÑËÎÂÀ: Araneae, ïàóêè, ôàóíèñòè÷åñêèå íàõîäêè, ðàñïðîñòðàíåíèå, ßêóòèÿ. ABSTRACT: Fifty-five species of spiders were col- Introduction lected in the Oymyakon area (ca 64.565°N, 142 145°E), eastern Yakutia, 2003. The vast majority of Yakutia (or Republic of Sakha) is the largest admin- species found are boreal and hypoarctic spiders. The istrative unit of Russia, about 3 100 000 km2, consisting material include some steppe species, e.g. Zelotes bal- of taiga, steppe, forest tundra, tundra and mountain tistanus Caporiacco, 1935, Pellenes gobiensis Schen- ecosystems. This wide area is reaching from the Amur kel, 1936 and P. limbatus Kulczyñski, 1895, at the region to the Arctic Ocean. northern limits of their range. -
Late Quaternary Environment of Central Yakutia (NE' Siberia
Late Quaternary environment of Central Yakutia (NE’ Siberia): Signals in frozen ground and terrestrial sediments Spätquartäre Umweltentwicklung in Zentral-Jakutien (NO-Sibirien): Hinweise aus Permafrost und terrestrischen Sedimentarchiven Steffen Popp Steffen Popp Alfred-Wegener-Institut für Polar- und Meeresforschung Forschungsstelle Potsdam Telegrafenberg A43 D-14473 Potsdam Diese Arbeit ist die leicht veränderte Fassung einer Dissertation, die im März 2006 dem Fachbereich Geowissenschaften der Universität Potsdam vorgelegt wurde. 1. Introduction Contents Contents..............................................................................................................................i Abstract............................................................................................................................ iii Zusammenfassung ............................................................................................................iv List of Figures...................................................................................................................vi List of Tables.................................................................................................................. vii Acknowledgements ........................................................................................................ vii 1. Introduction ...............................................................................................................1 2. Regional Setting and Climate...................................................................................4 -
Straight-Tusked Elephant (Palaeoloxodon Antiquus) and Other Megafauna in Europe
The World of Elephants - International Congress, Rome 2001 The Late Quaternary extinction of woolly mammoth (Mammuthus primigenius), straight-tusked elephant (Palaeoloxodon antiquus) and other megafauna in Europe A.J. Stuart, A.M. Lister Department of Biology, University College, London, UK [email protected] We are engaged in a research project (funded at present, it is apparent that these range changes by the Natural Environment Research Council - were not the same for each species; for example NERC) on megafaunal extinctions throughout the “last stands” of Mammuthus primigenius, Europe within the period ca. 50,000 to 9000 14C Megaloceros giganteus and Palaeoloxodon years BP. The work involves a survey of strati- antiquus appear to have been made in very dif- graphic information and available 14C dates, and ferent regions of Europe. Tracking these changes also sampling crucial material for a major involves firstly gathering data from the literature programme of AMS 14C dating. Both of the and from colleagues in each region. By these elephant species present in the European Late means we are building up an approximate pic- Pleistocene: Mammuthus primigenius and ture and specifying the likely latest material of Palaeoloxodon antiquus are included in the our target species for each region. In order to project. obtain a much more accurate database, we are Our target species include most of those that sampling the putatively latest material and sub- became extinct, or regionally extinct, after mitting it for 14C dating. ca. 15,000 BP: woolly mammoth Mammuthus Late Quaternary extinctions have been vari- primigenius, woolly rhinoceros Coelodonta ously attributed to overkill by human hunters antiquitatis; giant deer Megaloceros giganteus; (Martin 1984; Martin & Steadman 1999), to lion Panthera leo; and spotted hyaena Crocuta environmental changes (Graham & Lundelius crocuta. -
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. -
Neanderthal Hunting Activity Pack
Insights into Neanderthal hunting An activity pack for 3-6 year olds Authors: Dr Karen Ruebens & Dr Geoff M Smith Illustrations: Dr Anna Goldfield This activity pack is aimed at children between 3 and 6 years old (preliteracy, Early Years Foundation Stage up to Early Years 3). It can be used in the classroom as well as at home. It aims to introduce kids to the lifeways and hunting strategies of Neanderthals based on the most recent scientific discoveries through a series of hands-on activities (colouring, cutting, connect the dots, memory game). About the authors: Dr. Karen Ruebens About the illustrator: reconstructs Neanderthal behaviour by studying the Dr. Anna Goldfield is an archaeologist, different types of stone tools illustrator, and science communicator they made across Europe. who loves thinking about life in the past. She writes about archaeology and the human story for Sapiens.org and Dr. Geoff M Smith identifies hosts The Dirt, a podcast bringing the animal bones found at stories from anthropology and Neanderthal sites and looks archaeology to listeners of all ages and for traces of hunting and backgrounds. butchery activities. Watch Karen and Geoff talk about Neanderthal hunting: https://neanderthalseminars.wixsite.com/home/videos 1 Today we are the only type of humans alive. In the past there were many different types of humans living at the same time. One of these, the Neanderthals, lived a long, long time ago (300,000 to 40,000 years ago to be exact), long before there were even houses, shops and cars. Colour this group of Neanderthals. -
The Woolly Mammoth
The Woolly Mammoth The Woolly Mammoth by Edward I. Maxwell The closest relative of the woolly mammoth is the Asian elephant. The main difference between the two is that the mammoth had an incredible coat of fur, made up of an outer layer of coarse "guard hair" with an inner layer of curly wool. The last known group of mammoths died off, or became extinct, around 4,000 years ago. The mammoth roamed the northern lands of the world during a period known as the Ice Age. It was among the largest land mammals to roam the earth. The mammoth was a tough beast and was able to endure extreme weather conditions and frigid temperatures. The mammoth shared these northern territories with other mammals during the Ice Age. The most important mammal to interact with the mammoth, however, was the human. When the mammoths were at their greatest numbers, humans mainly hunted animals and foraged for food. These hunters would follow herds of animals over incredibly long distances in order to hunt them. The woolly mammoth provided a great amount of food and other important things for these humans. The fur, for example, could be used to make coats and blankets that would help keep out the cold in the icy environment. Bones from the mammoth could be used to make tools and weapons. Because one mammoth provided so many useful things to a large group of people, early humans would follow the herds wherever they went. There is even a theory that the humans followed the mammoth over a land-bridge from Asia into the Americas. -
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. -
Columbian Mammoths: Giants of the Ice Age
Name: __________________________________________________ Date: ______________ Columbian Mammoths: Giants of the Ice Age Did you know not all mammoths were woolly mammoths? The woolly mammoth was just one of nearly a dozen different species of mammoths. Another species was the Columbian (pronounced “cuh-LUM-be-un”) mammoth. Columbian mammoths lived during the Pleistocene Epoch (“PLY-stuh-SEEN EP-uck”), sometimes called the Ice Age. The Pleistocene Epoch started 2.5 million years ago and ended about 10,000 years ago. Even though people call it the Ice Age, not all the world was covered in ice. Sheets of ice called glaciers (“GLAY-shurs”) covered most of what is now Canada and the northern United States, but the lands that became the southern United States and Mexico were not under ice. Columbian mammoths were grazers, or animals that eat mostly grass. To make sure they had enough to eat, they lived in savannas (“suh-VAN-uhs”). Savannas are warm grasslands with scattered trees, and they were away from the glaciers. This was different from the woolly mammoths, which lived closer to the glaciers in lands called steppes (“STEPS”), cool plains with shrubs, herbs, and a little grass. How big was a Columbian mammoth? Huge! They were about 14 feet tall, or 4.3 meters. They also weighed as much as 10 tons, the same as a school bus. This made them much bigger than woolly mammoths, which were about 10 feet tall (3 meters) and weighed 6 tons. So why were they called Columbian mammoths? Scientists use New Latin to name animals. In New Latin, “Columbia” means “land of Columbus”, or North America.