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A possible anomalocaridid from the Cambrian Sirius Passet Lagerstätte, North Greenland

Published online by Cambridge University Press:  14 July 2015

Allison C. Daley
Affiliation:
Department of Earth Sciences, Paleobiology, Uppsala University, Villavägen 16, SE-752 36 Uppsala, Sweden
John S. Peel
Affiliation:
Department of Earth Sciences, Paleobiology, Uppsala University, Villavägen 16, SE-752 36 Uppsala, Sweden

Abstract

The Sirius Passet biota of North Greenland is one of the oldest Cambrian lagerstätten, and although it is dominated by non-mineralized arthropods and lobopods, anomalocaridids have never been identified. Based on a single specimen, we herein describe for the first time an appendage with possible anomalocaridid affinities as suggested by an overall gross morphology similar to that of the frontal appendage of Anomalocaris from other localities. Tamisiocaris borealis n. gen. and n. sp. has an elongated appendage with paired spines along one margin, and differs from the frontal appendage of Anomalocaris in that segment boundaries are absent and ventral spines are relatively long and spineless. These differences may be taphonomic, but the entire surface of the appendage is covered in a fine fabric, making it unlikely that this appendage was originally segmented or sclerotized. the taxon is tentatively placed within Radiodonta, but this systematic placement cannot be confirmed while complete body specimens are lacking.

Type
Paleontological Notes
Copyright
Copyright © The Paleontological Society 

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References

Babcock, L. E. and Peel, J. S.. 2007. Palaeobiology, taphonomy, and stratigraphic significance of the trilobite Buenellus from the Sirius Passet Biota, Cambrian of North Greenland. Memoirs of the Association of Australasian Palaeontologists, 34:401418.Google Scholar
Briggs, D. E. G. 1979. Anomalocaris, the largest known Cambrian arthropod. Palaeontology, 22:631663.Google Scholar
Briggs, D. E. G., Lieberman, B. S., Hendricks, J. R., Halgedahl, S. L., and Jarrard, R. D.. 2008. Middle Cambrian arthropods from Utah. Journal of Paleontology, 82:238254.CrossRefGoogle Scholar
Briggs, D. E. G. and Robison, R. A.. 1984. Exceptionally preserved nontrilobite arthropods and Anomalocaris from the Middle Cambrian of Utah. University of Kansas Paleontological Contributions, 111:123.Google Scholar
Budd, G.E. 1993. A Cambrian Gilled Lobopod from Greenland. Nature, 364:709711.CrossRefGoogle Scholar
Budd, G. E. 1996. The morphology of Opabinia regalis and the reconstruction of the arthropod stem-group. Lethaia, 29:114.CrossRefGoogle Scholar
Budd, G. E. 1998. Stem group arthropods from the Lower Cambrian Sirius Passet fauna of North Greenland, p. 125138. In Fortey, R. A. and Thomas, R. H. (eds.), Arthropod Relationships, Systematics Assocation Special Volume Series. Chapman and Hall, London, UK.Google Scholar
Budd, G. E. 1999. The morphology and phylogenetic significance of Kerygmachela kierkegaardi Budd (Buen Formation, Lower Cambrian, N Greenland). Transactions of the Royal Society of Edinburgh-Earth Sciences, 89:249290.CrossRefGoogle Scholar
Chen, J. Y., Ramsköld, L., and Zhou, G. Q.. 1994. Evidence for Monophyly and Arthropod Affinity of Cambrian Giant Predators. Science, 264:13041308.CrossRefGoogle ScholarPubMed
Chen, J. Y. and Zhou, G. Q.. 1997. Biology of the Chengjiang fauna. Bulletin of the National Museum of Natural Sciences, 10:11106.Google Scholar
Chen, J. Y., Waloszek, D., and Maas, A.. 2004. A new “great-appendage” arthropod from the Lower Cambrian of China and homology of chelicerate chelicerae and raptorial antero-ventral appendages. Lethaia, 37:320.CrossRefGoogle Scholar
Collins, D. 1996. The “evolution” of Anomalocaris and its classification in the arthropod class Dinocarida (nov) and order Radiodonta (nov). Journal of Paleontology, 70:280293.CrossRefGoogle Scholar
Conway Morris, S. and Peel, J. S.. 2008. The earliest annelids: Lower Cambrian polychaetes from the Sirius Passet Lagerstätte, Peary Land, North Greenland. Acta Paleontologica Polonica, 53:137148.CrossRefGoogle Scholar
Conway Morris, S. and Peel, J. S.. In press. New palaeoscolecidan worms from the lower Cambrian: Sirius Passet Fossil-Lagerstätte (North Greeland), Latham Shale (California) and Kinzers Shale (Pennsylvania). Acta Palaeontologica Polonica.Google Scholar
Conway Morris, S., Peel, J. S., Higgins, A. K., Soper, N. J., and Davis, N. C.. 1987. A Burgess Shale-Like Fauna from the Lower Cambrian of North Greenland. Nature, 326:181183.CrossRefGoogle Scholar
Cotton, T. J. and Braddy, S. J.. 2004. The phylogeny of arachnomorph arthropods and the origin of the Chelicerata. Transactions of the Royal Society of Edinburgh-Earth Sciences, 94:169193.CrossRefGoogle Scholar
Daley, A. C., Budd, G. E., Caron, J. B., Edgecombe, G. D., and Collins, D.. 2009. The Burgess Shale Anomalocaridid Hurdia and Its Significance for Early Euarthropod Evolution. Science, 323:15971600.CrossRefGoogle Scholar
Daley, A.C. and Budd, G. E.. In press. New anomalocaridid appendages from the Burgess Shale, Canada. Palaeontology.Google Scholar
Dewel, R. A. and Dewel, W. C.. 1998. The place of tardigrades in arthropod evolution, p. 109123. In Fortey, R. A. and Thomas, R. H. (eds.), Arthropod Relationships, Systematics Assocation Special Volume Series. Chapman and Hall, London, UK.Google Scholar
Dzik, J. and Lendzion, K.. 1988. The Oldest Arthropods of the East European Platform. Lethaia, 21:2938.CrossRefGoogle Scholar
Fletcher, T. P. and Collins, D.. 1998. The Middle Cambrian Burgess Shale and its relationship to the Stephen Formation in the southern Canadian Rocky Mountains. Canadian Journal of Earth Sciences, 35:413436.CrossRefGoogle Scholar
Hou, X. and Bergström, J.. 2006. Dinocarids–anomalous arthropods or arthropod-like worms?, p. 139158, 847–850. In Rong, J., Fang, Z., Zhou, Z., Zhan, R., Wang, X., and Yuan, X. (eds.), Originations, Radiations and Biodiversity changes—Evidences from the Chinese Fossil Record. Science Press, Beijing, China.Google Scholar
Hou, X., Aldridge, R. J., Bergström, J., Siveter, David. J., Siveter, Derek. J., and Feng, X.. 2004. The Cambrian Fossils of Chengjiang, China. The Flowering of Early Animal Life. Blackwell, Oxford, 1233 p.Google Scholar
Hou, X., Bergström, J., and Ahlberg, P.. 1995. Anomalocaris and Other Large Animals in the Lower Cambrian Chengjiang Fauna of Southwest China. GFF, 117:163183.Google Scholar
Lagebro, L., Stein, M., and Peel, J. S.. 2009. A new ?Lamellipedian arthropod from the Early Cambrian Sirius Passet fauna of North Greenland. Journal of Paleontology, 83:820825.CrossRefGoogle Scholar
Lendzion, K. 1975. Fauna of the Mobergella Zone in the Polish Lower Cambrian. Kwartalnik geologiczny, 19:237242.Google Scholar
Lendzion, K. 1977. Cassubia—a new generic name for Pomerania Lendzion 1975. Kwartalnik geologiczny, 21:211.Google Scholar
Lieberman, B. S. 2003. A new soft-bodied fauna: The Pioche Formation of Nevada. Journal of Paleontology, 77:674690.2.0.CO;2>CrossRefGoogle Scholar
Masiak, M. and Zylinska, A.. 1994. Burgess Shale-type fossils in Cambrian sandstones of the Holy Cross Mountains. Acta Palaeontologica Polonica, 39:329340.Google Scholar
Nedin, C. 1995. The Emu Bay Shale, a Lower Cambrian fossil Lagerstätten, Kangaroo Island, South Australia. Memoirs of the Association of Australasian Palaeontologists, 18:3140.Google Scholar
Resser, C. E. 1929. New Lower and Middle Cambrian Crustacea. Proceedings of the United States National Museum, 76:118.CrossRefGoogle Scholar
Van Roy, P. and Tetlie, O. E.. 2006. A spinose appendage fragment of a problematic arthropod from the Early Ordovician of Morocco. Acta Palaeontologica Polonica, 52:239246.Google Scholar
Whiteaves, J. F. 1892. Description of a new genus and species of Phyllocarid Crustacea from the Middle Cambrian of Mount Stephen, B.C. Canadian Record of Science, 5:205208.Google Scholar
Whittington, H. B. and Briggs, D. E. G.. 1985. The Largest Cambrian Animal, Anomalocaris, Burgess Shale, British-Columbia. Philosophical Transactions of the Royal Society of London Series B-Biological Sciences, 309:569609.Google Scholar
Zhang, X. and Briggs, D. E. G.. 2007. The nature and significance of the appendages of Opabinia from the Middle Cambrian Burgess Shale. Lethaia, 40:161173.CrossRefGoogle Scholar