Enzootic diseases and extinction of mammoths as a reflection of deep geochemical changes in ecosystems of Northern Eurasia

Λεπτομέρειες βιβλιογραφικής εγγραφής
Τίτλος: Enzootic diseases and extinction of mammoths as a reflection of deep geochemical changes in ecosystems of Northern Eurasia
Συγγραφείς: Leshchinskiy, Sergey V.
Πηγή: Archaeological and anthropological sciences. 2015. Vol. 7, № 3. P. 297-317
Στοιχεία εκδότη: Springer Science and Business Media LLC, 2014.
Έτος έκδοσης: 2014
Θεματικοί όροι: вымирание мамонтов, энзоотические заболевания, геохимические изменения, палеоэкологический анализ, Северная Евразия, 0601 history and archaeology, 06 humanities and the arts, 01 natural sciences, 0105 earth and related environmental sciences
Περιγραφή: The results of investigations performed on more than 23,500 mammoth bones and teeth in Northern Eurasia from 2003 to 2013 with the aim of revealing traces of enzootic diseases are presented here. The study focused on the Late Pleistocene “beast solonetz” sites (i.e. mineral licks/oases) of Western Siberia: Shestakovo-Kochegur (25.9–17.8 ka BP) in the Kemerovo region, Volchia Griva (17.8–11 ka BP) in the Novosibirsk region and Lugovskoye (16.5–10 ka BP) nearby Khanty-Mansiysk. Additional sites studies included sites (30–10 ka BP) from other regions of Northern Eurasia also with mass mammoth remains (Gari, Berelyokh, Krasnoyarskaya Kurya, Krakow Spadzista Street, Předmosti, Dolni Věstonice, Milovice and others). The results suggest that just at the end of the Pleistocene, large herbivorous mammals experienced a powerful geochemical stress which would manifest as mass destructive changes of bones due to enzootic diseases caused by mineral deficiency. Remains characterized by destructive changes are common and prevalent in all collections. Maximum damage was discovered in the bones and teeth of Mammuthus primigenius Blum. The most typical signs of osteodystrophy were osteoporosis, osteofibrosis, osteomalacia, osteolysis, cartilage atrophy, exostoses and fractures, resulting in the formation of false joints, ulcers and friction grooves on articular surfaces. The results of the paleoecological analysis suggest that the larger part of Northern Eurasia at the end of Pleistocene was extremely unfavourable for the existence of megafauna. The disruption of the abiotic relationships caused by the cardinal transformation of geochemical landscapes could have become the main reason for the wide-spread enzootia and, finally, the extinction of the mammoth.
Τύπος εγγράφου: Article
Γλώσσα: English
ISSN: 1866-9565
1866-9557
DOI: 10.1007/s12520-014-0205-4
Σύνδεσμος πρόσβασης: https://link.springer.com/content/pdf/10.1007%2Fs12520-014-0205-4.pdf
https://link.springer.com/article/10.1007/s12520-014-0205-4
https://rd.springer.com/article/10.1007%2Fs12520-014-0205-4
http://vital.lib.tsu.ru/vital/access/manager/Repository/vtls:000578438
Rights: Springer TDM
Αριθμός Καταχώρησης: edsair.doi.dedup.....04a5fc5d917bd5ae6a7f0e72c3c4b10c
Βάση Δεδομένων: OpenAIRE
Περιγραφή
ISSN:18669565
18669557
DOI:10.1007/s12520-014-0205-4