Abstract
The socio-economical importance of geological heritage (geoheritage) makes it a geological resource. New minerals are reported regularly, and their type specimens and localities are ex-situ and in-situ constituents of geoheritage, respectively. The present study focuses on the contemporary dynamics of these specific resources. For this purpose, the information about new minerals reported during the past five years is analyzed. The attention is paid to the distribution of the new mineral specimens (holotypes and cotypes) and their type localities by country; the transboundary replacement of new minerals is also considered. It is established that the new minerals-related geoheritage resources are accumulated in dozens of countries. The ex-situ geoheritage (specimens in museum collections) is represented twice narrower than the in-situ geoheritage (localities as geosites). About a half of new minerals are replaced to the other countries and often to the other parts of the world. The registered patterns are explained by the peculiarities of the contemporary mineralogical research. The outcomes of the present analysis permit to make recommendations for the development of the optimal geoheritage policy.
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