New palaeoscolecidan worms from the lower Cambrian : Siriuis Fossil-Lagerstatte (North Greenland), Latham Shale (California), and Kinzers Shale (Pennsylvania)
Palaeoscolecidan worms are an important component of many Lower Palaeozoic marine assemblages, with notable occurrences in a number of Burgess Shale-type Fossil-Lagerstätten. In addition to material from the lower Cambrian Kinzers Formation and Latham Shale, we also describe two new palaeoscolecidan...
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Polish Academy of Sciences
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ftucambridgeesc:oai:eprints.esc.cam.ac.uk:1217 2023-05-15T16:27:45+02:00 New palaeoscolecidan worms from the lower Cambrian : Siriuis Fossil-Lagerstatte (North Greenland), Latham Shale (California), and Kinzers Shale (Pennsylvania) Conway Morris, S Peel, J 2010-01 application/pdf http://eprints.esc.cam.ac.uk/1217/ http://eprints.esc.cam.ac.uk/1217/1/Conway_Morris_Acta_Palaeo_Polo_2009.PDF en eng Polish Academy of Sciences http://eprints.esc.cam.ac.uk/1217/1/Conway_Morris_Acta_Palaeo_Polo_2009.PDF Conway Morris, S and Peel, J (2010) New palaeoscolecidan worms from the lower Cambrian : Siriuis Fossil-Lagerstatte (North Greenland), Latham Shale (California), and Kinzers Shale (Pennsylvania). Acta Palaeontologica Polonica, 51 (1). pp. 141-156. ISSN ISSN: 0567-7920. EISSN: 1732-2421 04 - Palaeobiology Article PeerReviewed 2010 ftucambridgeesc 2020-08-27T18:08:48Z Palaeoscolecidan worms are an important component of many Lower Palaeozoic marine assemblages, with notable occurrences in a number of Burgess Shale-type Fossil-Lagerstätten. In addition to material from the lower Cambrian Kinzers Formation and Latham Shale, we also describe two new palaeoscolecidan taxa from the lower Cambrian Sirius Passet Fossil-Lagerstätte of North Greenland: Chalazoscolex pharkus gen. et sp. nov and Xystoscolex boreogyrus gen. et sp. nov. These palaeoscolecidans appear to be the oldest known (Cambrian Series 2, Stage 3) soft-bodied examples, being somewhat older than the diverse assemblages from the Chengjiang Fossil-Lagerstätte of China. In the Sirius Passet taxa the body is composed of a spinose introvert (or proboscis), trunk with ornamentation that includes regions bearing cuticular ridges and sclerites, and a caudal zone with prominent circles of sclerites. The taxa are evidently quite closely related; generic differentiation is based on degree of trunk ornamentation, details of introvert structure and nature of the caudal region. The worms were probably infaunal or semi-epifaunal; gut contents suggest that at least X. boreogyrus may have preyed on the arthropod Isoxys. Comparison with other palaeoscolecidans is relatively straightforward in terms of comparable examples in other Burgess Shale-type occurrences, but is much more tenuous with respect to the important record of isolated sclerites. These finds from Greenland provide further evidence that palaeoscolecidans possessed a complex anterior introvert directly comparable to a number of priapulid-like taxa from other Burgess Shale-type assemblages. Although these palaeoscolecidans have been allied with the nematomorphs, molecular data in conjunction with our observations suggest that this hypothesis is untenable. Palaeoscolecidans and similar priapulid-like taxa are probably primitive cycloneuralians and as such may indicate the original bodyplan of this important group of ecdysozoans. In addition, we describe another sclerite-bearing fossil from the Sirius Passet Fossil-Lagerstätte that may be related to the cambroclaves. Article in Journal/Newspaper Greenland North Greenland University of Cambridge, Department of Earth Sciences: ESC Publications Burgess ENVELOPE(76.128,76.128,-69.415,-69.415) Greenland Sirius ENVELOPE(163.250,163.250,-84.133,-84.133) |
institution |
Open Polar |
collection |
University of Cambridge, Department of Earth Sciences: ESC Publications |
op_collection_id |
ftucambridgeesc |
language |
English |
topic |
04 - Palaeobiology |
spellingShingle |
04 - Palaeobiology Conway Morris, S Peel, J New palaeoscolecidan worms from the lower Cambrian : Siriuis Fossil-Lagerstatte (North Greenland), Latham Shale (California), and Kinzers Shale (Pennsylvania) |
topic_facet |
04 - Palaeobiology |
description |
Palaeoscolecidan worms are an important component of many Lower Palaeozoic marine assemblages, with notable occurrences in a number of Burgess Shale-type Fossil-Lagerstätten. In addition to material from the lower Cambrian Kinzers Formation and Latham Shale, we also describe two new palaeoscolecidan taxa from the lower Cambrian Sirius Passet Fossil-Lagerstätte of North Greenland: Chalazoscolex pharkus gen. et sp. nov and Xystoscolex boreogyrus gen. et sp. nov. These palaeoscolecidans appear to be the oldest known (Cambrian Series 2, Stage 3) soft-bodied examples, being somewhat older than the diverse assemblages from the Chengjiang Fossil-Lagerstätte of China. In the Sirius Passet taxa the body is composed of a spinose introvert (or proboscis), trunk with ornamentation that includes regions bearing cuticular ridges and sclerites, and a caudal zone with prominent circles of sclerites. The taxa are evidently quite closely related; generic differentiation is based on degree of trunk ornamentation, details of introvert structure and nature of the caudal region. The worms were probably infaunal or semi-epifaunal; gut contents suggest that at least X. boreogyrus may have preyed on the arthropod Isoxys. Comparison with other palaeoscolecidans is relatively straightforward in terms of comparable examples in other Burgess Shale-type occurrences, but is much more tenuous with respect to the important record of isolated sclerites. These finds from Greenland provide further evidence that palaeoscolecidans possessed a complex anterior introvert directly comparable to a number of priapulid-like taxa from other Burgess Shale-type assemblages. Although these palaeoscolecidans have been allied with the nematomorphs, molecular data in conjunction with our observations suggest that this hypothesis is untenable. Palaeoscolecidans and similar priapulid-like taxa are probably primitive cycloneuralians and as such may indicate the original bodyplan of this important group of ecdysozoans. In addition, we describe another sclerite-bearing fossil from the Sirius Passet Fossil-Lagerstätte that may be related to the cambroclaves. |
format |
Article in Journal/Newspaper |
author |
Conway Morris, S Peel, J |
author_facet |
Conway Morris, S Peel, J |
author_sort |
Conway Morris, S |
title |
New palaeoscolecidan worms from the lower Cambrian : Siriuis Fossil-Lagerstatte (North Greenland), Latham Shale (California), and Kinzers Shale (Pennsylvania) |
title_short |
New palaeoscolecidan worms from the lower Cambrian : Siriuis Fossil-Lagerstatte (North Greenland), Latham Shale (California), and Kinzers Shale (Pennsylvania) |
title_full |
New palaeoscolecidan worms from the lower Cambrian : Siriuis Fossil-Lagerstatte (North Greenland), Latham Shale (California), and Kinzers Shale (Pennsylvania) |
title_fullStr |
New palaeoscolecidan worms from the lower Cambrian : Siriuis Fossil-Lagerstatte (North Greenland), Latham Shale (California), and Kinzers Shale (Pennsylvania) |
title_full_unstemmed |
New palaeoscolecidan worms from the lower Cambrian : Siriuis Fossil-Lagerstatte (North Greenland), Latham Shale (California), and Kinzers Shale (Pennsylvania) |
title_sort |
new palaeoscolecidan worms from the lower cambrian : siriuis fossil-lagerstatte (north greenland), latham shale (california), and kinzers shale (pennsylvania) |
publisher |
Polish Academy of Sciences |
publishDate |
2010 |
url |
http://eprints.esc.cam.ac.uk/1217/ http://eprints.esc.cam.ac.uk/1217/1/Conway_Morris_Acta_Palaeo_Polo_2009.PDF |
long_lat |
ENVELOPE(76.128,76.128,-69.415,-69.415) ENVELOPE(163.250,163.250,-84.133,-84.133) |
geographic |
Burgess Greenland Sirius |
geographic_facet |
Burgess Greenland Sirius |
genre |
Greenland North Greenland |
genre_facet |
Greenland North Greenland |
op_relation |
http://eprints.esc.cam.ac.uk/1217/1/Conway_Morris_Acta_Palaeo_Polo_2009.PDF Conway Morris, S and Peel, J (2010) New palaeoscolecidan worms from the lower Cambrian : Siriuis Fossil-Lagerstatte (North Greenland), Latham Shale (California), and Kinzers Shale (Pennsylvania). Acta Palaeontologica Polonica, 51 (1). pp. 141-156. ISSN ISSN: 0567-7920. EISSN: 1732-2421 |
_version_ |
1766017261758316544 |