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Cambrian-recent Very abundant: Palaeozoic K/T made them less abundant |
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Middle Cambrian-recent Palaeozoic overshadowed by brachiopods |
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Late-Cambrian Present Abundant in Palaeozoic, Mesozoic, before Silurian: top predators |
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extermally shelled currently living in the West-Pacific |
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extinct now, Jura-Creataceous internal support of a squid like creature |
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U. Cam-Recent: extrenally shelled, straight or curved |
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L.Devon-Upper Cretaceous, K/T extinction |
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Cambrian-Recent rare till Ordovician |
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Rugose and tabulate coral time |
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Ordovician - Recent In Palaeozoic dominated shallow marine (especially Carboniferous) |
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Early Cambrian – Late Permian |
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Mid Cambrian to Carboniferous |
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Graptolite fossils are often found in shales and mud rocks where sea-bed fossils are rare, this type of rock having formed from sediment deposited in relatively deep water that had poor bottom circulation, was deficient in oxygen, |
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