Clausinella Fasciata
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Clausinella Fasciata
''Clausinella fasciata'', the banded venus, is a marine bivalve mollusc in the family Veneridae. Fossil record Fossils of ''Clausinella fasciata'' are found in marine strata from the Miocene until the Quaternary The Quaternary ( ) is the current and most recent of the three periods of the Cenozoic Era in the geologic time scale of the International Commission on Stratigraphy (ICS). It follows the Neogene Period and spans from 2.58 million years ... (age range: from 20.43 to 0.012 million years ago). Fossils are known from various localities in Cyprus, Italy, Germany, United Kingdom, Morocco and Spain. Description This species has a solid, flat, sub-triangular shell which grows to in length. Surface colour is variable; red, pink, purple, yellow or brown with radiating bands and colourful streaks. It may have up to fifteen broad concentric ridges on older specimens. The interior is dull white. Distribution and habitat The banded venus has a recorded distrib ...
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Miocene
The Miocene ( ) is the first geological epoch of the Neogene Period and extends from about (Ma). The Miocene was named by Scottish geologist Charles Lyell; the name comes from the Greek words (', "less") and (', "new") and means "less recent" because it has 18% fewer modern marine invertebrates than the Pliocene has. The Miocene is preceded by the Oligocene and is followed by the Pliocene. As Earth went from the Oligocene through the Miocene and into the Pliocene, the climate slowly cooled towards a series of ice ages. The Miocene boundaries are not marked by a single distinct global event but consist rather of regionally defined boundaries between the warmer Oligocene and the cooler Pliocene Epoch. During the Early Miocene, the Arabian Peninsula collided with Eurasia, severing the connection between the Mediterranean and Indian Ocean, and allowing a faunal interchange to occur between Eurasia and Africa, including the dispersal of proboscideans into Eurasia. During the ...
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