The Hirnantian Isotopic Carbon Excursion (HICE) is a constructive carbon isotope excursion which happened at the end of the Ordovician period, throughout the Hirnantian Age from around 445.2 Ma to 443.Eight Ma (million years ago).
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The Hirnantian Isotopic Carbon Excursion (HICE) is a constructive carbon isotope excursion which happened at the end of the Ordovician period, throughout the Hirnantian Age from around 445.2 Ma to 443.Eight Ma (million years ago). https://www.4shared.com/u/-tImha8Q/ivankonovalovrd9418.html