Cambrian stem-group annelids and a metameric origin of the annelid head
The oldest fossil annelids come from the Early Cambrian Sirius Passet and Guanshan biotas and Middle Cambrian Burgess Shale. While these are among the best preserved polychaete fossils, their relationship to living taxa is contentious, having been interpreted either as members of extant clades or as...
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pubmed-46501892015-12-02 Cambrian stem-group annelids and a metameric origin of the annelid head Parry, Luke Vinther, Jakob Edgecombe, Gregory D. Palaeontology The oldest fossil annelids come from the Early Cambrian Sirius Passet and Guanshan biotas and Middle Cambrian Burgess Shale. While these are among the best preserved polychaete fossils, their relationship to living taxa is contentious, having been interpreted either as members of extant clades or as a grade outside the crown group. New morphological observations from five Cambrian species include the oldest polychaete with head appendages, a new specimen of Pygocirrus from Sirius Passet, and an undescribed form from the Burgess Shale. We propose that the palps of Canadia are on an anterior segment bearing neuropodia and that the head of Phragmochaeta is formed of a segment bearing biramous parapodia and chaetae. The unusual anatomy of these taxa suggests that the head is not differentiated into a prostomium and peristomium, that palps are derived from a modified parapodium and that the annelid head was originally a parapodium-bearing segment. Canadia, Phragmochaeta and the Marble Canyon annelid share the presence of protective notochaetae, interpreted as a primitive character state subsequently lost in Pygocirrus and Burgessochaeta, in which the head is clearly differentiated from the trunk. The Royal Society 2015-10 /pmc/articles/PMC4650189/ /pubmed/26445984 http://dx.doi.org/10.1098/rsbl.2015.0763 Text en © 2015 The Authors. http://creativecommons.org/licenses/by/4.0/ Published by the Royal Society under the terms of the Creative Commons Attribution License http://creativecommons.org/licenses/by/4.0/, which permits unrestricted use, provided the original author and source are credited. |
repository_type |
Open Access Journal |
institution_category |
Foreign Institution |
institution |
US National Center for Biotechnology Information |
building |
NCBI PubMed |
collection |
Online Access |
language |
English |
format |
Online |
author |
Parry, Luke Vinther, Jakob Edgecombe, Gregory D. |
spellingShingle |
Parry, Luke Vinther, Jakob Edgecombe, Gregory D. Cambrian stem-group annelids and a metameric origin of the annelid head |
author_facet |
Parry, Luke Vinther, Jakob Edgecombe, Gregory D. |
author_sort |
Parry, Luke |
title |
Cambrian stem-group annelids and a metameric origin of the annelid head |
title_short |
Cambrian stem-group annelids and a metameric origin of the annelid head |
title_full |
Cambrian stem-group annelids and a metameric origin of the annelid head |
title_fullStr |
Cambrian stem-group annelids and a metameric origin of the annelid head |
title_full_unstemmed |
Cambrian stem-group annelids and a metameric origin of the annelid head |
title_sort |
cambrian stem-group annelids and a metameric origin of the annelid head |
description |
The oldest fossil annelids come from the Early Cambrian Sirius Passet and Guanshan biotas and Middle Cambrian Burgess Shale. While these are among the best preserved polychaete fossils, their relationship to living taxa is contentious, having been interpreted either as members of extant clades or as a grade outside the crown group. New morphological observations from five Cambrian species include the oldest polychaete with head appendages, a new specimen of Pygocirrus from Sirius Passet, and an undescribed form from the Burgess Shale. We propose that the palps of Canadia are on an anterior segment bearing neuropodia and that the head of Phragmochaeta is formed of a segment bearing biramous parapodia and chaetae. The unusual anatomy of these taxa suggests that the head is not differentiated into a prostomium and peristomium, that palps are derived from a modified parapodium and that the annelid head was originally a parapodium-bearing segment. Canadia, Phragmochaeta and the Marble Canyon annelid share the presence of protective notochaetae, interpreted as a primitive character state subsequently lost in Pygocirrus and Burgessochaeta, in which the head is clearly differentiated from the trunk. |
publisher |
The Royal Society |
publishDate |
2015 |
url |
https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4650189/ |
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1613502987725963264 |