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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Main Authors: Parry, Luke, Vinther, Jakob, Edgecombe, Gregory D.
Format: Online
Language:English
Published: The Royal Society 2015
Online Access:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4650189/
id pubmed-4650189
recordtype oai_dc
spelling 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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