Hostname: page-component-78c5997874-g7gxr Total loading time: 0 Render date: 2024-11-08T08:27:29.578Z Has data issue: false hasContentIssue false

The mammoth “cemeteries” of north-east Siberia

Published online by Cambridge University Press:  27 October 2009

Extract

The north of Yakutia has long been known to be an immense storehouse of frozen disjointed bones of many hundreds of thousands of large Pleistocene mammals—mammoths, horses, woolly rhinoceroses, bison, musk-oxen— “horned cattle”, as the first Russian travellers called them. Such knowledge had a commercial value, of whichmore will be said below, for the quarrying of mammoth ivory has gone on for many centuries. In quality these tusks, which have lain in frozen ground for tens of millennia, are as good as those of modern African and Indian elephants and are sometimes two or three times larger. For naturalists, the greatest interest lies in the discovery of whole frozen bodies or of skulls and complete skeletons. Study of the position of these bodiesand their morphology and of the contents of their stomachs and intestines may answer the age-old question of why the mammoth (or woolly elephant), together with this rich assemblage of large herbivores, died out. Would even a partial restoration of such previously abundant life be possible there today?

Type
Articles
Copyright
Copyright © Cambridge University Press 1974

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

Gusev, A. I. 1956. Mamontovyy gorizont [The mammoth horizon]. Materialy po Chetvertichnoy Geologii i Geomorfologii SSSR, Novaya Seriya, No 1, p 169–77.Google Scholar
Karta chetvertichnykh otlozeniy Arktiki i Subarktiki [Map of Quaternary deposits of the Arctic and sub-Arctic]. 1965. Leningrad, Nauchno-Issledovatel'skiy Institut Geologii Arktiki, Masshtab 1:5 000000.Google Scholar
Lindberg, G. U. 1972. Krupniye kolebaniya urovnya okeana v chetvertichyy period. [Big Quaternary changes of the ocean level]. Leningrad.Google Scholar
Pfizenmayer, E. M. 1926. Mammutleichen und Urwaldmenschen in Nordost Sibirien. Leipzig.Google Scholar
Popov, A. I. 1950. Taymyrskiy mamont [The Taymyr mammoth]. Voprosy Geografii, No 23, p 296305.Google Scholar
Tomirdiaro, S. V. 1972. Vechnaya merzlota i osvoyeniye gornykh stran i nizmennostey [Permafrost and the utilization of mountainous and lowland areas]. Magadan.Google Scholar
Vereshchagin, N. K. 1967. Primitive hunters and Pleistocene extinction in the Soviet Union. In: Martin, P. S. and Wright, H. E. Jr, eds. Pleistocene extinctions: the search for a cause. New Haven and London, Yale University Press, p 365–97.Google Scholar
Vereshchagin, N. K. 1971. Raskopki mamontova kladbishcha na r Berelekh [Excavation of a mammoth cemetery on the river Berelekh]. Vestnik Akademii Nauk SSSR, No 8, p 8593.Google Scholar
Vollosovich, K. A. 1915. Mamont iz Novosibirskikh ostrovov [A mammoth from Novosibirskiye Ostrova]. Priroda, No 4, p 604–07.Google Scholar
Yermolayev, M. M. 1932. Geologicheskiy i geomorfologicheskiy ocherk ostrova Bol'shogo Lyakhovskogo [Geological and geomorphological outline of Ostrov Bol'shoy Lyakhovskiy]. Sovet po Izucheniyu Proizvoditel'nykh Sil. Seriya Yakutskaya. Trudy, Vypusk 7, p 147228.Google Scholar
Zenzinov, V. M. 1915 Dobycha mamontovoy kosti na Novosibirskikh ostrovakh [Quarrying mammoth ivory in the Novosibirskiye Ostrova]. Priroda, 0708, p 979–92.Google Scholar