Kudurs (mineral licks) in the Belukha Mountain area, Altai Mountains, Russia; Arabian Journal of Geosciences; Vol. 15, iss. 14

Dettagli Bibliografici
Parent link:Arabian Journal of Geosciences.— .— New York: Springer Science+Business Media LLC.
Vol. 15, iss. 14.— 2022.— Article number 1284, 17 p.
Altri autori: Panichev A. M. Aleksandr Mikhaylovich, Baranovskaya N. V. Nataliya Vladimirovna, Seryodkin I. V. Ivan Vladimirovich, Chekryzhov I. Yu. Igor Yurjevich, Vakh E. A., Lutsenko T. N., Patrusheva O. V. Olga Vladimirovna, Makarevich R. A., Kholodov A. S. Aleksey Sergeevich, Golokhvast K. S. Kirill Sergeevich
Riassunto:Title screen
Studies were carried out in the upper reaches of the Akkem River aimed at explaining why the local ungulates consume clay rocks common in the basin of the Yarlu River, a tributary of the Akkem River. Chemical composition of river and spring waters and mineral and chemical composition of clay rocks consumed by wild and domestic ungulates at kudurs were studied. The waters in the local watercourses are ultra-fresh, hydro-carbonate-calcium. Increased concentrations of rare-earth elements (REE) were observed in waters of the Yarlu River. Consumed clayey rocks (kudurits) are represented by finely dispersed quartz-plagioclase-mica-chlorite mineral associations — the products of transformation of shale rocks of the Early Paleozoic age. The comparison of the chemical composition of kudurits and coprolites of red deer showed that when the rocks pass through the digestive tract, out of all macroelements, only Na is reliably assimilated in the body in amounts from 0.1 to 0.3 g per kg of kudurit. In addition, kudurits act as sorbents, removing P, K, Mg, and sometimes Ca from the body. As part of micronutrients, they are most active in sorbing and removing REE from the body
Текстовый файл
AM_Agreement
Lingua:inglese
Pubblicazione: 2022
Soggetti:
Accesso online:https://doi.org/10.1007/s12517-022-10478-8
Natura: Elettronico Capitolo di libro
KOHA link:https://koha.lib.tpu.ru/cgi-bin/koha/opac-detail.pl?biblionumber=685070

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330 |a Studies were carried out in the upper reaches of the Akkem River aimed at explaining why the local ungulates consume clay rocks common in the basin of the Yarlu River, a tributary of the Akkem River. Chemical composition of river and spring waters and mineral and chemical composition of clay rocks consumed by wild and domestic ungulates at kudurs were studied. The waters in the local watercourses are ultra-fresh, hydro-carbonate-calcium. Increased concentrations of rare-earth elements (REE) were observed in waters of the Yarlu River. Consumed clayey rocks (kudurits) are represented by finely dispersed quartz-plagioclase-mica-chlorite mineral associations — the products of transformation of shale rocks of the Early Paleozoic age. The comparison of the chemical composition of kudurits and coprolites of red deer showed that when the rocks pass through the digestive tract, out of all macroelements, only Na is reliably assimilated in the body in amounts from 0.1 to 0.3 g per kg of kudurit. In addition, kudurits act as sorbents, removing P, K, Mg, and sometimes Ca from the body. As part of micronutrients, they are most active in sorbing and removing REE from the body 
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461 1 |t Arabian Journal of Geosciences  |c New York  |n Springer Science+Business Media LLC. 
463 1 |t Vol. 15, iss. 14  |v Article number 1284, 17 p.  |d 2022 
610 1 |a электронный ресурс 
610 1 |a труды учёных ТПУ 
610 1 |a Kudurs 
610 1 |a Geophagy 
610 1 |a Ultrabasic rocks 
610 1 |a Geochemistry 
610 1 |a Altai Mountains 
701 1 |a Panichev  |b A. M.  |g Aleksandr Mikhaylovich 
701 1 |a Baranovskaya  |b N. V.  |c geochemist  |c Professor of Tomsk Polytechnic University, Doctor of biological sciences  |f 1970-  |g Nataliya Vladimirovna  |9 15240 
701 1 |a Seryodkin  |b I. V.  |g Ivan Vladimirovich 
701 1 |a Chekryzhov  |b I. Yu.  |g Igor Yurjevich 
701 1 |a Vakh  |b E. A. 
701 1 |a Lutsenko  |b T. N. 
701 1 |a Patrusheva  |b O. V.  |g Olga Vladimirovna 
701 1 |a Makarevich  |b R. A. 
701 1 |a Kholodov  |b A. S.  |g Aleksey Sergeevich 
701 1 |a Golokhvast  |b K. S.  |g Kirill Sergeevich 
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