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Mercury spikes at the Devonian-Carboniferous boundary in the eastern part of the Rhenohercynian Zone (central Europe) and in the South China Block
Autoři | |
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Rok publikování | 2019 |
Druh | Článek v odborném periodiku |
Časopis / Zdroj | Palaeogeography, Palaeoclimatology, Palaeoecology |
Fakulta / Pracoviště MU | |
Citace | |
www | https://www.sciencedirect.com/science/article/pii/S003101821930077X |
Doi | http://dx.doi.org/10.1016/j.palaeo.2019.05.043 |
Klíčová slova | Famennian-Tournaisian boundary;Hangenberg events;Trace element geochemistry;Volcanic activity;Hydrothermal activity |
Popis | Distribution of Hg and other trace elements from Devonian-Carboniferous boundary The highest Hg, Hg/TOC, Hg/Al, and Hg/Fe values bellow and in the Hangenberg Events Anomalous Hg was not simply derived from the increased deposition of organic carbon. Both sections were influenced by widespread hydrothermal and volcanic activity. Hg enrichment caused by local hydrothermal and volcanic activity and redox variations |
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