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in 1854, 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. Subsequently, E. Ehlers, a specialist on recent polychaetes, recorded them from the Jurassic Solenhofen Stone of Bavaria,
347:
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,
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of material from
England, Wales, Canada and Sweden 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.
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EHLERS, E. 1868a. 12Iber eine fossile
Funicee aus Solenhofen (Eunicites aritus), nebst Bemerkungenvtiber fossile Wtirmer tiberhaupt. Zeitschrifl ftir wissenschaftliche Zoologie, 18, 421–443.
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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.
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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.
31:
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EICHWALD, E. 1854. Die
Grauwackenschichten von Lieu-und Esthland. Bulletin de la Société Impériale des Naturalistes de Moscou, 27, 1–111.
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379:) from the Lower Carboniferous of Halkin Mountain, Flintshire. Quarterly Journal of the Geological Society of London, 52, 438–450.
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Hints, O.; Eriksson, M. (2007). "Diversification and biogeography of scolecodont-bearing polychaetes in the
Ordovician".
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EHLERS, E. 1868b. Ueber fossiler WĂĽrmer aus dem lithographischen
Schiefer in Bayern. Palaeontographica, 17, 145–175.
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Segments of the fossil jaw of a polychaete worm were first reported from
Silurian strata on the Estonian island of
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including complete scientific bibliography, lists of fossil genera and species, and selection of images
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MASSALONGO, A. 1855. Monografica delle Nereidi fossili del Monte Bolca. Antonelli, Verona, 55 pp.
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Germany, demonstrating their affinity and proposing the generic names
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rocks in Scotland. Scolecodonts representing the present-day families
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period (around half a billion years ago at the start of the
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HINDE, G. J. 1896. On the jaw-apparatus of an annelid (
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Since the other classes of annelids (specifically, the
287:Palaeogeography, Palaeoclimatology, Palaeoecology
263:. Extensive studies in the late 19th century by
226:(which includes the Arabellidae) are known from
146:teeth and their dwelling tubes made of durable
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401:Piotr Mierzejewski's page on microfossils
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115:Hills of southern Australia and in mid-
61:. Scolecodonts are common and diverse
34:An Ordovician scolecodont from Estonia
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107:have been described in even older,
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170:Scolecodonts belonging to the
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299:10.1016/j.palaeo.2006.02.029
138:. Polychaetes are commonly
99:Relatedly, more problematic
158:(a.k.a. parchment), and/or
27:Jaw of a polychaete annelid
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377:Eunicites reidiae sp. nov.
59:invertebrate paleontology
420:Fossil record of animals
65:, which range from the
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123:in British Columbia.
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111:era deposits in the
49:, a common type of
238:first appeared in
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212:Symmetroprionidae
152:calcium carbonate
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393:scolecodonts.net
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196:Polychaetaspidae
176:Atraktoprionidae
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184:Kalloprionidae
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119:deposits of
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73:era) to the
63:microfossils
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18:Scolecodonts
53:-producing
40:scolecodont
409:Categories
272:References
140:fossilized
128:earthworms
79:Ordovician
57:useful in
44:polychaete
257:Eunicites
232:Onuphidae
224:Oenonidae
174:families
144:chitinous
113:Ediacaran
94:Paleozoic
71:Paleozoic
415:Annelids
348:370–389.
252:Saaremaa
240:Mesozoic
228:Silurian
166:Taxonomy
117:Cambrian
87:Devonian
83:Silurian
67:Cambrian
246:History
172:extinct
148:calcite
132:leeches
105:fossils
75:present
47:annelid
293:: 95.
220:extant
160:chitin
103:-like
90:marine
51:fossil
156:mucus
96:era.
259:and
234:and
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101:worm
85:and
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