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Article: Fish and tetrapod communities across a marine to brackish salinity gradient in the Pennsylvanian (early Moscovian) Minto Formation of New Brunswick, Canada, and their palaeoecological and palaeogeographical implications

Palaeontology Cover Image - Volume 59 Part 5
Publication: Palaeontology
Volume: 59
Part: 5
Publication Date: September 2016
Page(s): 689 724
Author(s): Aodhán Ó Gogáin, Howard J. Falcon‐Lang, David K. Carpenter, Randall F. Miller, Michael J. Benton, Peir K. Pufahl, Marcello Ruta, Thomas G. Davies, Steven J. Hinds, and Matthew R. Stimson
Addition Information

How to Cite

Ó GOGÁIN, A., FALCON‐LANG, H.J., CARPENTER, D.K., MILLER, R.F., BENTON, M.J., PUFAHL, P.K., RUTA, M., DAVIES, T.G., HINDS, S.J., STIMSON, M.R. 2016. Fish and tetrapod communities across a marine to brackish salinity gradient in the Pennsylvanian (early Moscovian) Minto Formation of New Brunswick, Canada, and their palaeoecological and palaeogeographical implications. Palaeontology, 59, 5, 689-724. DOI: 10.1111/pala.12249

Author Information

  • Aodhán Ó Gogáin - University of Bristol School of Earth Sciences Bristol UK (Email: ogogaina@tcd.ie)
  • Howard J. Falcon‐Lang - Royal Holloway Department of Earth Sciences Egham Surrey UK (Email: h.falcon-lang@es.rhul.ac.uk)
  • David K. Carpenter - University of Southampton Waterfront Campus Ocean and Earth Science National Oceanography Centre Southampton Southampton UK (Email: dkc1g12@soton.ac.uk)
  • Randall F. Miller - New Brunswick Museum Natural Science Department Saint John New Brunswick Canada (Email: Randall.Miller@nbm-mnb.ca)
  • Michael J. Benton - University of Bristol School of Earth Sciences Bristol UK (Email: mike.benton@bristol.ac.uk)
  • Peir K. Pufahl - Acadia University Department of Earth and Environmental Science Wolfville Nova Scotia Canada (Email: peir.pufahl@acadiau.ca)
  • Marcello Ruta - University of Lincoln School of Life Sciences Lincoln UK (Email: mruta@lincoln.ac.uk)
  • Thomas G. Davies - University of Bristol School of Earth Sciences Bristol UK (Email: thomas.davies@bristol.ac.uk)
  • Steven J. Hinds - Geological Surveys Branch New Brunswick Department of Energy and Mines Fredericton New Brunswick Canada (Email: steven.hinds@gnb.ca)
  • Matthew R. Stimson - New Brunswick Museum Natural Science Department Saint John New Brunswick Canada (Email: mstimson29@gmail.com)
  • Matthew R. Stimson - Geological Surveys Branch New Brunswick Department of Energy and Mines Fredericton New Brunswick Canada

Publication History

  • Manuscript Accepted: 28 June 2016
  • Manuscript Received: 22 June 2016

Funded By

Bob Savage Memorial Fund (University of Bristol)
New Brunswick Museum Creative Futures Fund
Geological Surveys Branch of the New Brunswick Department of Energy and Mines
NERC Advanced Fellowship. Grant Number: NE/F014120/2
Natural Sciences and Engineering Research Council of Canada

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Wiley Online Library
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Abstract

Euryhaline adaptations in Pennsylvanian vertebrates allowed them to inhabit the marine to freshwater spectrum. This is illustrated by new assemblages of fish and tetrapods from the early Moscovian Minto Formation of New Brunswick, Canada. Fish include chondrichthyans (xenacanthids and the enigmatic Ageleodus), acanthodians (gyracanthids and acanthodiforms), sarcopterygians (rhizodontids, megalichthyids and dipnoans), and actinopterygians (eurynotiforms). Tetrapods include small‐ to medium‐sized, and largely aquatic, stem tetrapods (colosteids) and anthracosaurs (embolomeres). A key finding is that the parautochthonous fossil assemblages are preserved across a salinity gradient, with diversity (measured by the Simpson Index) declining from open marine environments, through brackish embayments, and reaching a nadir in tidal estuaries. Chondrichthyans dominate the entire salinity spectrum (65% of fossils), a distribution that demonstrates a euryhaline mode of life, and one large predatory chondrichthyan, Orthacanthus, may have practised filial cannibalism in coastal nurseries because its heteropolar coprolites contain juvenile xenacanthid teeth. In contrast, other fish communities were more common in open marine settings while tetrapods were more common in coastal brackish waters. While all these faunas were also likely to have been euryhaline, their osmoregulation was, perhaps, less versatile. The demonstration of widespread euryhalinity among fish and aquatic tetrapods explains why Pennsylvanian faunas generally show a cosmopolitan biogeography because taxa were able to disperse via seaways. It also resolves the paradox of enriched strontium isotopic signatures observed in these faunas because organisms would have been, at times, exposed to continental water bodies as well. Therefore, our new findings contribute to the long‐running debate about the ecology of Pennsylvanian fishes and tetrapods.

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