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Anomalous drip in the Punkva caves (Moravian Karst): relevant implications for paleoclimatic proxies
Autoři | |
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Rok publikování | 2016 |
Druh | Článek v odborném periodiku |
Časopis / Zdroj | Hydrological Processes |
Fakulta / Pracoviště MU | |
Citace | |
www | Odkaz na článek na webu časopisu |
Doi | http://dx.doi.org/10.1002/hyp.10731 |
Obor | Geochemie |
Klíčová slova | cave dripwater;stable isotope 13C and 18O;Mg/Ca and Sr/Ca ratios;prior calcite precipitation;karst water mixing |
Popis | The drips in the Punkva caves have been investigated using several methods. There was an anomalous drip, which differed from regular drips in several parameters including mineralization and isotopic values. It has been interpreted as a consequence of prior calcite precipitation above the caves. This behavior has implications for the use of speleothems as climatic archives. |