Diagenetically-enhanced trilobite obrution deposits in concretionary limestones: The paradox of “rhythmic events beds”
Certain offshore facies with extraordinarily well preserved fossils, particularly trilobites, display distinctive motifs of rhythmically bedded, decimeter-scale, concretionary limestone and dark gray shale. Examples are known from Cambrian to Neogene age, but are especially common in the lower-middl...
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Veröffentlicht in: | Palaeogeography, palaeoclimatology, palaeoecology palaeoclimatology, palaeoecology, 2012-12, Vol.367-368, p.30-43 |
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