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1989
Fox, A. J., Mattison B. W., & Pemberton S. G. (1989).  The Lower Cretaceous McMurray Fm. In the subsurface of the Syncrude Mine area, Athabasca Oil Sands : an integrated paleontological and physical sedimentological examination.
Mattison, B. W., & Pemberton S. G. (1989).  The McMurray Formation in the Athabasca oil sands area : an ichnological and paleontological perspective. In : Fourth UNITAR/UNDP International Conference on Heavy Crude and Tar Sands, Meyer, R. F. and Wiggins, E. J. (eds.). 2, 37-52.
Mattison, B. W., Fox A. J., & Pemberton S. G. (1989).  Sedimentogic, paleontologic and ichnologic criteria for the recognition of ancient estuarine deposits: an example from Lower Cretaceous McMurray Formation in the Athabasca oil sands area of northeastern Alberta. 66-79.
1988
Mattison, B. W., & Pemberton S. G. (1988).  Trends in trace fossil assemblages within estuary-associated tidal flat sediments : an example from the Athabasca Oil Sands of northeastern Alberta.
1987
Mattison, B. W., & Pemberton S. G. (1987).  Ichnocoenoses and fossil biocoenoses of the McMurray Formation, Athabasca Oil Sands mining area, northeastern Alberta : implications for paleoenvironmental reconstruction and depositional modelling.
Mattison, B. W., & Pemberton S. G. (1987).  Ichnological assemblages as depositional environmental indicators in McMurray Formation - Athabasca oil sands of northeastern Alberta. 71(5), 590-.
Pemberton, G. S., Ranger M. J., Mattison B. W., & Fox A. J. (1987).  Ichnological microdynamics of the Athabasca Oil Sands : an integrated surface and subsurface study : Third Progress Report. 239.
1986
Pemberton, G. S., Ranger M. J., Mattison B. W., & Fox A. J. (1986).  Ichnological microdynamics of the Athabasca Oil Sands : an integrated surface and subsurface study : Second Progress Report. 107.
Pemberton, G. S., Mattison B. W., Fox A., & Ranger M. J. (1986).  Ichnology of the Lower Cretaceous McMurray Formation, Athabasca Oil Sands, area. In : Canadian Society of Petroleum Geologists, Reserves 21, National Meeting.

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