D
David J. P. Ferguson
Researcher at University of Technology, Sydney
Publications - 7
Citations - 236
David J. P. Ferguson is an academic researcher from University of Technology, Sydney. The author has contributed to research in topics: Migmatite & Batholith. The author has an hindex of 5, co-authored 7 publications receiving 184 citations. Previous affiliations of David J. P. Ferguson include John Radcliffe Hospital & La Trobe University.
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Journal ArticleDOI
Oocyst wall formation and composition in coccidian parasites
Kelly Mai,Philippa A Sharman,Robert A. Walker,Marilyn Katrib,David P De Souza,Malcolm J. McConville,Michael Wallach,Sabina I. Belli,David J. P. Ferguson,Nicholas Smith +9 more
TL;DR: The oocyst wall of coccidian parasites is a robust structure that is resistant to a variety of environmental and chemical insults and has high levels of dityrosine bonds, which may provide a structural matrix for assembly of the oocySt wall and contribute to its resilience.
Journal ArticleDOI
Conservation of proteins involved in oocyst wall formation in Eimeria maxima, Eimeria tenella and Eimeria acervulina.
Sabina I. Belli,David J. P. Ferguson,Marilyn Katrib,Iveta Slapetova,Kelly Mai,Jan Šlapeta,Sarah A. Flowers,K. B. Miska,Fiona M. Tomley,M W Shirley,Michael Wallach,Nicholas Smith +11 more
TL;DR: This study confirms the conservation of the roles of GAM56 and GAM82 in oocyst wall formation and shows that antibodies to gametocyte antigens of E. maxima cross-react with homologous proteins in other species, helping to explain cross-species maternal immunity.
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Sex and Eimeria: a molecular perspective
TL;DR: The molecular events that underpin sexual reproduction in Eimeria are piece together and additional details from analogous events in Plasmodium are used to fill current knowledge gaps.
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Delamerian Glenelg tectonic zone, western Victoria: characterisation and synthesis of igneous rocks
TL;DR: In this paper, the authors grouped the Cambro-Ordovician plutonic rocks of the Glenelg River Complex (western Victoria) into three structural associations based on intrusion timing relative to Delamerian deformational episodes.
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Delamerian Glenelg tectonic zone, western Victoria: Geology and metamorphism of stratiform rocks
C. M. Gray,Anthony I.S. Kemp,J. A. C. Anderson,D. J. Bushell,David J. P. Ferguson,J. A. Fitzherbert,M. D. Stevenson +6 more
TL;DR: The Cambro-Ordovician Glenelg tectonic zone of western Victoria is a distinctive metamorphic-igneous segment of the Delamerian Orogenic Belt comprising two northweststriking regional metamorphics segments of andalusite-sillimanite type prograding towards an axial granitic batholith.