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,[1] 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.

Scolecodont ramphoprion
An Ordovician scolecodont from Estonia


Scolecodonts belonging to the extinct families Atraktoprionidae, Hadoprionidae, Kalloprionidae, Mochtyellidae, Paulinitidae, Polychaetaspidae, Ramphoprionidae, Rhytiprionidae, Skalenoprionidae, Symmetroprionidae, Xanioprionidae, and the still-extant (living) family Oenonidae (which includes the Arabellidae) are known from Silurian rocks in Scotland. Scolecodonts representing the present-day families Onuphidae and Dorvilleidae first appeared in Mesozoic era deposits.


Segments of the fossil jaw of a polychaete worm were first reported from Silurian strata on the Estonian island of Saaremaa in 1854,[2] but they were misinterpreted as fish teeth. A year later, impressions of whole polychaete worms with poorly preserved jaws were described from Italian Tertiary deposits.[3] Subsequently, E. Ehlers, a specialist on recent polychaetes, recorded them from the Jurassic Solenhofen Stone of Bavaria, Germany, demonstrating their affinity and proposing the generic names Eunicites and Lumbriconereites.[4][5] Extensive studies in the late 19th century by George J. Hinde of material from England, Wales, Canada and Sweden[6][7][8][9] established a basis for the nomenclature of what he regarded as isolated components of annelid jaws; but study of them lapsed thereafter for almost 50 years.


  1. ^ Hints, O.; Eriksson, M. (2007). "Diversification and biogeography of scolecodont-bearing polychaetes in the Ordovician". Palaeogeography, Palaeoclimatology, Palaeoecology. 245: 95. doi:10.1016/j.palaeo.2006.02.029.
  2. ^ EICHWALD, E. 1854. Die Grauwackenschichten von Lieu-und Esthland. Bulletin de la Societe Imperiale des Naturalistes de Moscou, 27, 1–111.
  3. ^ MASSALONGO, A. 1855. Monografica delle Nereidi fossili del Monte Bolca. Antonelli, Verona, 55 pp.
  4. ^ EHLERS, E. 1868a. 12Iber eine fossile Funicee aus Solenhofen (Eunicites aritus), nebst Bemerkungenvtiber fossile Wtirmer tiberhaupt. Zeitschrifl ftir wissenschaftliche Zoologie, 18, 421–443.
  5. ^ EHLERS, E. 1868b. Ueber fossiler Würmer aus dem lithographischen Schiefer in Bayern. Palaeontographica, 17, 145–175.
  6. ^ HINDE, G. J. 1879. On annelid jaws from the Cambro-Silurian, Silurian and Devonian Formations in Canada and from the Lower Carboniferous in Scotland. Quarterly Journal of the Geological Society of London, 35, 370–389.
  7. ^ HINDE, G. J. 1880. On annelid jaws from the Wenlock and Ludlow Formations of the west of England. Quarterly Journal of the Geological Society of London, 36, 368–378.
  8. ^ HINDE, G. J. 1882. On annelid remains from the Silurian strata of the Isle of Gotland. Geologiska Föreningen i Stockholm Förhandlingar, 6(6): 254–255.
  9. ^ HINDE, G. J. 1896. On the jaw-apparatus of an annelid (Eunicites reidiae sp. nov.) from the Lower Carboniferous of Halkin Mountain, Flintshire. Quarterly Journal of the Geological Society of London, 52, 438–450.

External links

  • including complete scientific bibliography, lists of fossil genera and species, and selection of images
  • Piotr Mierzejewski's page on microfossils

Belemnitida (or belemnites) is an extinct order of squid-like cephalopods that existed from the Late Triassic to Late Cretaceous. Unlike squid, belemnites had an internal skeleton that made up the cone. The parts are, from the arms-most to the tip: the tongue-shaped pro-ostracum, the conical phragmocone, and the pointy guard. The calcitic guard is the most common belemnite remain. Belemnites, in life, are thought to have had 10 hooked arms and a pair of fins on the guard. The chitinous hooks were usually no bigger than 5 mm (0.20 in), though a belemnite could have had between 100 and 800 hooks in total, using them to stab and hold onto prey.

Belemnites were an important food source for many Mesozoic marine creatures, both the adults and the planktonic juveniles, and likely played an important role in restructuring marine ecosystems after the Triassic–Jurassic extinction event. They may have laid between 100 and 1,000 eggs. Some species may have been adapted to speed and swam in the turbulent open ocean, whereas others resided in the calmer littoral zone (nearshore) and fed off the seafloor. The largest belemnite known, Megateuthis elliptica, had guards of 60 to 70 cm (24 to 28 in).

Belemnites are coleoids, a group that includes squid and octopuses, and are often grouped into the superorder Belemnoidea, though the higher classification of cephalopods is volatile and there is no clear consensus how belemnites are related to modern coleoids. Guards can give information on the climate, habitat, and the carbon cycle of the ancient waters they inhabited. Guards have been found since antiquity and have become part of folklore.


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