New fossil worms from the Lower Cambrian of the Kinzers Formation, Pennsylvania, with some comments on Burgess Shale-type preservation

Two new fossil worms are described from the Lower Cambrian Kinzers Formation of southeast Pennsylvania. Both are unique specimens. Kinzeria crinita new genus and species has a body divided into three regions. The head bears a prominent set of elongate tentacles, presumably employed for feeding. The...

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Published in:Journal of Paleontology
Main Authors: Capdevila, D. Garcia-Bellido, Morris, S. Conway
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1999
Subjects:
Online Access:http://dx.doi.org/10.1017/s0022336000027918
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022336000027918
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spelling crcambridgeupr:10.1017/s0022336000027918 2024-09-15T18:09:59+00:00 New fossil worms from the Lower Cambrian of the Kinzers Formation, Pennsylvania, with some comments on Burgess Shale-type preservation Capdevila, D. Garcia-Bellido Morris, S. Conway 1999 http://dx.doi.org/10.1017/s0022336000027918 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022336000027918 en eng Cambridge University Press (CUP) https://www.cambridge.org/core/terms Journal of Paleontology volume 73, issue 3, page 394-402 ISSN 0022-3360 1937-2337 journal-article 1999 crcambridgeupr https://doi.org/10.1017/s0022336000027918 2024-07-31T04:04:26Z Two new fossil worms are described from the Lower Cambrian Kinzers Formation of southeast Pennsylvania. Both are unique specimens. Kinzeria crinita new genus and species has a body divided into three regions. The head bears a prominent set of elongate tentacles, presumably employed for feeding. The elongate trunk tapers slightly in a posterior direction. It contains a prominent intestinal tract, the contents of which indicate a deposit feeding habit. The tail is an expanded structure, with either a spatulate or sagittate outline. The mode of life of K. crinita is uncertain, but the animal may have been semi-sedentary. Atalotaenia adela new genus and species is more poorly known, lacking the anterior. The preserved body is vermiform, with external annulations and a rounded posterior. There is a prominent internal strand, consisting of a probable intestine and an associated fibrous unit, possibly representing muscles. This worm may have been infaunal. These discoveries extend further our understanding of the ancient diversity of Laurentian Burgess Shale-type faunas. In common with the Burgess Shale itself and the Sirius Passet fauna (Peary Land, Greenland) the location of fossil-Lagerstätte [see Shields (1998) for a discussion of the terminology of Lagerstätten] of the Kinzers Formation adjacent to a prominent escarpment reinforces earlier evidence of the paleotopography exerting an important control on the distribution of Burgess Shale-type faunas. Whether this is a result of localized faunal abundances or taphonomic control is, however, uncertain. Article in Journal/Newspaper Greenland Peary Land Cambridge University Press Journal of Paleontology 73 3 394 402
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
description Two new fossil worms are described from the Lower Cambrian Kinzers Formation of southeast Pennsylvania. Both are unique specimens. Kinzeria crinita new genus and species has a body divided into three regions. The head bears a prominent set of elongate tentacles, presumably employed for feeding. The elongate trunk tapers slightly in a posterior direction. It contains a prominent intestinal tract, the contents of which indicate a deposit feeding habit. The tail is an expanded structure, with either a spatulate or sagittate outline. The mode of life of K. crinita is uncertain, but the animal may have been semi-sedentary. Atalotaenia adela new genus and species is more poorly known, lacking the anterior. The preserved body is vermiform, with external annulations and a rounded posterior. There is a prominent internal strand, consisting of a probable intestine and an associated fibrous unit, possibly representing muscles. This worm may have been infaunal. These discoveries extend further our understanding of the ancient diversity of Laurentian Burgess Shale-type faunas. In common with the Burgess Shale itself and the Sirius Passet fauna (Peary Land, Greenland) the location of fossil-Lagerstätte [see Shields (1998) for a discussion of the terminology of Lagerstätten] of the Kinzers Formation adjacent to a prominent escarpment reinforces earlier evidence of the paleotopography exerting an important control on the distribution of Burgess Shale-type faunas. Whether this is a result of localized faunal abundances or taphonomic control is, however, uncertain.
format Article in Journal/Newspaper
author Capdevila, D. Garcia-Bellido
Morris, S. Conway
spellingShingle Capdevila, D. Garcia-Bellido
Morris, S. Conway
New fossil worms from the Lower Cambrian of the Kinzers Formation, Pennsylvania, with some comments on Burgess Shale-type preservation
author_facet Capdevila, D. Garcia-Bellido
Morris, S. Conway
author_sort Capdevila, D. Garcia-Bellido
title New fossil worms from the Lower Cambrian of the Kinzers Formation, Pennsylvania, with some comments on Burgess Shale-type preservation
title_short New fossil worms from the Lower Cambrian of the Kinzers Formation, Pennsylvania, with some comments on Burgess Shale-type preservation
title_full New fossil worms from the Lower Cambrian of the Kinzers Formation, Pennsylvania, with some comments on Burgess Shale-type preservation
title_fullStr New fossil worms from the Lower Cambrian of the Kinzers Formation, Pennsylvania, with some comments on Burgess Shale-type preservation
title_full_unstemmed New fossil worms from the Lower Cambrian of the Kinzers Formation, Pennsylvania, with some comments on Burgess Shale-type preservation
title_sort new fossil worms from the lower cambrian of the kinzers formation, pennsylvania, with some comments on burgess shale-type preservation
publisher Cambridge University Press (CUP)
publishDate 1999
url http://dx.doi.org/10.1017/s0022336000027918
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022336000027918
genre Greenland
Peary Land
genre_facet Greenland
Peary Land
op_source Journal of Paleontology
volume 73, issue 3, page 394-402
ISSN 0022-3360 1937-2337
op_rights https://www.cambridge.org/core/terms
op_doi https://doi.org/10.1017/s0022336000027918
container_title Journal of Paleontology
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