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McIlroy, 2004 (eds)

The Application of ichnology to palaeoenvironmental and stratigraphic analysis

McIlroy, D.
DOI
DOI10.1144/gsl.sp.2004.228.01.01
Year2004
PublisherGeological Society of London
JournalGeological Society, London, Special Publications
Volume228
Number1
Typebook
LanguageEnglish
Id51641

Abstract

Extract Ichnology is the study of trace fossils, which preserve the activity of animals as recorded by their tracks, trails, burrows and borings. Rather than giving information about the taxonomic affinities of a given type of organism, trace fossils yield information about an animal’s behaviour in response to its environment. Trace fossils are almost always in situ, are commonly specific to a particular suite of environmental conditions, can be readily studied in core and may be common in strata devoid of body fossils. They are invaluable in thorough sedimentological analysis and are thus of great utility to petroleum geologists, sedimentologists and palaeontologists alike. Over the last 30 years or so, ichnology has been a rapidly developing branch of palaeontology that not only has important applications in classical palaeobiology (e.g. Donovan 1994; Bromley 1996), but is also of great value in the more applied disciplines of palaeoenvironmental and stratigraphical analysis. Much progress has been made in the development of this discipline, but there remain many fascinating and challenging issues, particularly in combining ichnology and sedimentology. This book aims to provide a summary of recent progress, with an up-to-date summary of most themes in modern ichnology. The volume stems from the 2003 Lyell Meeting sponsored by The Geological Society, The Palaeontological Association, BP, Shell, Exxon Mobil, Statoil, Total and Amerada Hess. The introductory paper by McIlroy (a) provides a condensed summary of some ichnological themes and frontiers, and outlines a practical approach for the description of trace fossils and identification of key stratigraphic

Contents

PagesTitleAuthor(s)
3-27Some ichnological concepts, methodologies, applications and frontiersMcIlroy, D.
29–62Stratigraphic applications of substrate-specific ichnofacies: Delineating discontinuities in the rock recordPemberton, S. G., McEachern, J. A.,Saunders, T.
63-76Recent and sub-recent microborings from the upwelling area off Mauritania (West Africa) and their implications for palaeoecologyGlaub, I.
77-92Climatic control of trace fossil distribution in the marine realmGoldring, R., Cadée, G. C., D’Alessandro, A., Gibert, J. M. de, Jenkins, R., Pollard, J. E.
93-123A new approach to the analysis and interpretation of tracks: examples from the dinosauriaManning, P. L.
125-139Phanerozoic history of deep-sea trace fossilsUchman, A.
141-156A re-evaluation of the relationship between trace fossils and dysoxiaMartin, D. K.
157-178Ichnology of Carboniferous tide-influenced environments and tidal flat variability in the North American MidcontinentMángano, M. G., Buatois, L. A.
179-211Differentiation of estuarine and offshore marine deposits using integrated ichnology and sedimentology: Permian Pebbley Beach Formation, Sydney Basin, AustraliaBann, K. L., Fielding, C. R., MacEachern, J. A., Tye, S. C.
213-236Palaeoecology of the Bright Angel Shale in the eastern Grand Canyon, Arizona, USA, incorporating sedimentological, ichnological and palynological dataBaldwin, C. T., Strother, P. K., Beck, J. H., Rose, E.
311-333Animal-substrate interactions in freshwater environments: applications of ichnology in facies and sequence stratigraphic analysis of fluvio-lacustrine successionsBuatois, L. A., Mángano, M. G.
335-354Trace fossil distribution in lacustrine deltas: examples from the Triassic rift lakes of the Ischigualasto-Villa Unión basin, ArgentinaMelchor, R. N.
397-418Trace fossils in the aftermath of mass extinction eventsTwitchett, R. J., Barras, C. G.
419-453Ichnotaxonomy and ichnostratigraphy of chambered trace fossils in palaeosols attributed to coleopterans, ants and termitesGenise, J. F.
455-479A stratigraphy of marine bioerosionBromley, R. G.
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