UPPSALA UNIVERSITET : Department of Earth Sciences: Palaeobiology : personal

Palaeobiology

Personal
John S. Peel

Professor of Historical Geology and Palaeontology
Department of Earth Sciences
Palaeobiology program
Uppsala University
Villavägen 16
SE-752 36 Uppsala
SWEDEN

Phone: +46 18 471 27 47
Mobile: +46 79 425 06 34

e-mail: John.Peel@pal.uu.se

John Peel, Fimbuldal, Peary Land, North Greenland (82°18´N)

Photo: Fimbuldal, Peary Land, North Greenland (82°18´N):     2006-08-07

Research interests
  • Cambrian molluscs (especially helcionelloids) and Small Shelly Fossils
  • Lower Palaeozoic gastropods and monoplacophoran molluscs
  • Sirius Passet Lagerstätte (Lower Cambrian) of Greenland
  • Lower Palaeozoic (especially Cambrian) palaeontology and stratigraphy of Greenland
Eotebenna arctica, Henson Gletscher Fm. Photo: Eotebenna arctica, Henson Gletscher Fm. (Lower Cambrian), North Greenland
  

Recent publications

Conway Morris, S. & Peel, J. S.  2008:  The earliest annelids: Lower Cambrian polychaetes from the Sirius Passet Lagerstätte, Peary Land, North Greenland. Acta Palaeontologica Polonica 53, 137-148.   

    Abstract: Apart from the Phyllopod Bed of the Burgess Shale (Middle Cambrian) polychaete annelids are practically unknown from any of the Cambrian Lagerstätten. This is surprising both because their diversity in the Burgess Shale is considerable, while to date the Chengjiang Lagerstätte which is equally impressive in terms of faunal diversity has no reliable records of any annelids. Here we describe, on the basis of about 40 specimens, Phragmochaeta canicularis new genus, new species from the Lower Cambrian Sirius Passet Lagerstätte of Peary Land, North Greenland. This makes it by far the oldest known polychaete, with a likely age of lower to middle Atdabanian, The body consists of approximately 20 segments, each bearing notochaetae and neurochaetae. The former appeared to have formed a felt-like covering on the dorsum, whilst the neurochaetae projected obliquely to the longitudinal axis. Apart from minor differences in chaetal size at either end there is no other tagmosis. Details of the head are obscure, and presence of palps, tentacles and eyes are conjectural.  Jaws appear to have been absent. The gut was straight, and flanked by massive longitudinal musculature. P. canicularis was evidently benthic, propelling itself on the neurochaetae, with the dorsal neurochaetae conferring protection.  Its stratigraphic position and generalized appearance are consistent with P. canicularis being primitive, but the phylogenetic relationships within the polychaetes remain problematic, principally because of paucity of relevant morphological information.

Atkins, C.J. & Peel, J.S. 2008: Yochelcionella (Mollusca, Helcionelloida) from the lower Cambrian of North America. Bulletin of Geosciences 83(1), 23-38.

Stein, M. & Peel, J.S.  2008
: The trilobite Perrisopyge from the Lower Cambrian of Laurentia. GFF 130(2), 71-78.

Babcock, L.E. & 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, 331-348.

Isakar, M. & Peel, J.S. 2007: Lower Cambrian helcionelloid molluscs from Estonia. GFF 129, 255-262.

Peel, J.S. & Berg-Madsen, V. 2007: Eobucania (Mollusca) from the Furongian (late Cambrian) of Sweden. GFF 129, 235-237.

Skovsted, C.B. & Peel, J.S. 2007: Small shelly fossils from the argillaceous facies of the Lower Cambrian Forteau Formation of western Newfoundland. Acta Palaeontologica Polonica 52, 729-748.

Skovsted, C.B., Brock, G.A., Lindström, A., Peel, J.S., Paterson, J.R. & Fuller, M.F. 2007: Early Cambrian record of failed durophagy and shell repair in an epibenthic mollusc. Biology letters (2007) 3, 314-317.
 

Current Ph.D projects

Christian J. Atkins: Lower Cambrian Small Shelly Fossils (especially molluscs) from North Greenland
Martin Stein: Cambrian arthropods from Greenland, including the Sirius Passet biota

Complete list of publications


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