A scolecodont is the jaw of a polychaete annelid, a common type of fossil-producing segmented worm useful in invertebrate paleontology. Scolecodonts are common and diverse microfossils, which range from the Cambrian period (around half a billion years ago at the start of the Paleozoic era) to the present. They diversified profusely in the Ordovician, and are most common in the Ordovician, Silurian and Devonian marine deposits of the Paleozoic era.
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| - Scolécodonte (fr)
- Scolecodont (en)
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| - Un scolécodonte (Scolodonta) est une pièce maxillaire de vers annélides connue sous forme de microfossiles dans le Paléozoïque. Le géologue et paléontologue britannique George Jennings Hinde (1839-1918) fit de nombreuses études de scolécodontes à partir d'échantillons d'Angleterre, du pays de Galles, du Canada et de Suède établissant une base pour la nomenclature de ce qu'il considérait comme des éléments isolés de mâchoires d'annélides. (fr)
- A scolecodont is the jaw of a polychaete annelid, a common type of fossil-producing segmented worm useful in invertebrate paleontology. Scolecodonts are common and diverse microfossils, which range from the Cambrian period (around half a billion years ago at the start of the Paleozoic era) to the present. They diversified profusely in the Ordovician, and are most common in the Ordovician, Silurian and Devonian marine deposits of the Paleozoic era. (en)
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| - Un scolécodonte (Scolodonta) est une pièce maxillaire de vers annélides connue sous forme de microfossiles dans le Paléozoïque. Le géologue et paléontologue britannique George Jennings Hinde (1839-1918) fit de nombreuses études de scolécodontes à partir d'échantillons d'Angleterre, du pays de Galles, du Canada et de Suède établissant une base pour la nomenclature de ce qu'il considérait comme des éléments isolés de mâchoires d'annélides. (fr)
- A scolecodont is the jaw of a polychaete annelid, a common type of fossil-producing segmented worm useful in invertebrate paleontology. Scolecodonts are common and diverse microfossils, which range from the Cambrian period (around half a billion years ago at the start of the Paleozoic era) to the present. They diversified profusely in the Ordovician, and are most common in the Ordovician, Silurian and Devonian marine deposits of the Paleozoic era. Relatedly, more problematic worm-like fossils have been described in even older, Neoproterozoic era deposits in the Ediacaran Hills of southern Australia and in mid-Cambrian deposits of Burgess shale in British Columbia. Since the other classes of annelids (specifically, the earthworms and leeches) lack hard parts, only the sea-dwelling polychaetes are frequently represented in the fossil record. Polychaetes are commonly fossilized due to their chitinous teeth and their dwelling tubes made of durable calcite (a calcium carbonate), hardened mucus (a.k.a. parchment), and/or chitin-like cement. (en)
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