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Obtusum Zone
Malachite forms through the weathering of copper ore deposits and is renowned for its distinctive green concentric banding and layered fibrous structure
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Promicroceras Planicosta (Reynès, 1879) – Calcite Ammonite Fossil lightweight chakra board Obtusum ZoneA beautifully preserved specimen of Promicroceras planicosta, fully replaced by calcite. This ammonite displays fine ribbing and its characteristic planispiral coiling. As a key index fossil of the Lower Jurassic Sinemurian, Promicroceras is highly significant for ammonite biostratigraphy in the UK. An excellent choice for collectors, researchers, or curated display. Stratigraphic Context Lower Lias Group, Obtusum Zone Chronostratigraphy Lower
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