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A study of kudurs used by wild animals located on the water sources high in REE content in the Caucasus Nature Reserveстатья
Статья опубликована в высокорейтинговом журнале
Статья опубликована в журнале из списка Web of Science и/или Scopus- Авторы: Panichev A.M., Trepet S.A., Chekryzhov I.Yu, Seryodkin I.V., Vakh E.A., Makarevich R.A., Eskina T.G., Bibina K.V., Stolyarova T.A., Mitina E.I., Ivanov V.V., Ostapenko D.S., Kholodov K.S., Golokhvast A.S.
- Журнал: Environmental Geochemistry and Health
- Год издания: 2021
- Издательство: Springer Nature
- Местоположение издательства: Switzerland
- DOI: 10.1007/s10653-020-00670-8
- Аннотация: One of the theories explaining the reasons for geophagy, which was proposed earlier by the authors of the article, consists in the assumption that animals need rare-earth elements (REE). In order to test this hypothesis, we studied the chemical composition of spring waters in the territory of the Caucasus Nature Reserve at three kudurs along the Achipsta River, as well as at the Mamaevsky kudur (southwestern slope of the Pshekish mountain). At the Mamaevsky kudur, we also studied the chemical composition of earth consumed by animals, and the species, age and gender composition, seasonal and daily activity of ungulate animals–visitors of the kudur. It was determined that the most active visitors of the Mamaevsky kudur were European bison (Bison bonasus) with one activity peak during the rut, in July. The frequency of visits to the kudur by red deer (Cervus elaphus) was 4 times lower with the highest peak activity in April and a lower peak in August. Only in one of four water sources at the Mamaevsky kudur there was an elevated concentration of Na (by 7 times). In the other three the concentration was comparable to the local river water. The waters of two “sodium-free” springs had increased concentrations of REE (by 5–8 times). Geophagic earths near the Mamaevsky springs are decomposition products of siltstone and sandstone shale rocks of the Jurassic age consisting of clay minerals (illite mixed with smectite, and chlorites)—from 42 to 45%, and quartz and feldspar (in total up to 50%) mixed with Fe and Ca carbonates. The chemical composition of acid extracts (0.1 N HCl, pH = 1.0) from consumed earth showed the highest extractability of Ca and Fe. In trace elements, Sr, Ba, Zn, Cu, Ni, Co, V, light lanthanides, and Y are most actively extracted. Na is extracted at 0.03–0.1 g/kg. The sodium bicarbonate spring water consumed by animals at kudurs on the Achipsta River had Na contents 70–300 times, and REE contents 25–40 times higher than that in the river water. The revealed facts do not contradict the hypothesis that the desire for geophagy in animals in the Caucasus (in addition to the long-known “urge” for Na) can be also related to the properties of lanthanides group elements exchange in the body.
- Добавил в систему: Подчасова (Столярова) Татьяна Андреевна