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Ichnology : organism-substrate interactions in space and time PDF

744 Pages·2011·33.407 MB·English
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This page intentionally left blank Ichnology Organism–substrate interactions in space and time Ichnology is the study of traces, such as burrows, trackways, and borings, created in the substrate by living organisms. It is an increasingly important field, having recently been transformed into a multifaceted science at the crossroads of many disciplines. This is the first book to systematically cover the conceptual framework of the discipline and the wide breadth of applica- tions in both paleobiology and sedimentology, bridging the gap between the two main facets of the field. It emphasizes the importance of understanding ecological controls on benthic fauna distribution and the role of burrowing organisms in chan- ging their environments. A detailed analysis of the ichnology of a full range of dep- ositional environments is presented using examples from the Precambrian to the Recent, and the use of trace fossils in facies analysis and sequence stratigraphy is discussed. By presenting ichnological information within a macroevolutionary perspec- tive, the authors provide an up-to-date overview of the subject and highlight the potential of biogenic structures to provide valu- able information and solve problems in a wide range of fields. An invaluable resource for researchers and graduate students in paleontology as well as in sedimentology and sequence stra- tigraphy, this book will also be of interest to oil industry profes- sionals working in reservoir and exploration geology. luis a. buatois is a Full Professor at the University of Saskatchewan, specializing in paleoenvironmental and strati- graphic aspects of ichnology. He has received awards from the Argentinean Paleontological Association, the Egidio Feruglio Foundation, and the Argentinean Academy of Sciences, and the Argentinean Secretary of Science and Technology. Currently President of the International Ichnological Association, and formerly Vice-President of the International Palaeontological Association, he has carried out field and subsurface work in many different countries. Professor Buatois has published four other books, edited three journal special issues, and is the author of over 150 scientific papers. He is also a member of the editorial board of a number of journals, including Lethaia and Ichnos. m. gabriela mángano is an Associate Professor at the University of Saskatchewan and works on ecological and evolu- tionary aspects of trace fossils. In addition to her research projects in paleontology and geology, she has a strong interest in philosophy and the history of science. Dr Mángano has done extensive inter- national fieldwork and, as a researcher for the National Research Council in Argentina, she obtained awards from the Argentinean Paleontological Association, the Mid-American Paleontological Society, and the Argentinean Federation of University Women. She is a member of the editorial board of a number of journals, includ- ing Journal of Paleontology, Palaios, Paleontologia Electronica, and Revista Brasilera de Paleontologia, has edited two special issues, and has published three other books and more than 100 scientific papers. Ichnology Organism–substrate interactions in space and time luis a. buatois m. gabriela mángano University of Saskatchewan, Canada CambriDge uniVersitY Press Cambridge, New York, Melbourne, Madrid, Cape Town, Singapore, São Paulo, Delhi, Tokyo, Mexico City Cambridge University Press The Edinburgh Building, Cambridge CB2 8RU, UK Published in the United States of America by Cambridge University Press, New York www.cambridge.org Information on this title: www.cambridge.org/9780521855556 © Luis A. Buatois and M. Gabriela Mángano 2011 This publication is in copyright. Subject to statutory exception and to the provisions of relevant collective licensing agreements, no reproduction of any part may take place without the written permission of Cambridge University Press. First published 2011 Printed in the United Kingdom at the University Press, Cambridge A catalog record for this publication is available from the British Library Library of Congress Cataloging in Publication data Buatois, Luis A. Ichnology: organism-substrate interactions in space and time/Luis A. Buatois, M. Gabriela Mángano. p. cm. ISBN 978-0-521-85555-6 (hardback) 1. Ichnology. 2. Paleoecology. I. Mánga no, M. Gabriela. II. Title. QE720.5.B83 2011 560’.43–dc22 2010051885 ISBN 978-0-521-85555-6 Hardback Cambridge University Press has no responsibility for the persistence or accuracy of URLs for external or third-party internet websites referred to in this publication, and does not guarantee that any content on such websites is, or will remain, accurate or appropriate. We dedicate this book to Melanie, Gabriel, Michelle, and also Sebastian and Milly v Contents Acknowledgments xi 1.4.4 Grazing traces or pascichnia 20 1.4.5 Feeding traces or fodinichnia 20 Introduction 1 1.4.6 Dwelling traces or domichnia 21 Part I Conceptual tools and methods 1.4.7 Traps and farming traces or agrichnia 21 1 The basics of ichnology 5 1.4.8 Escape traces or fugichnia 22 1.1 Basic concepts 5 1.4.9 Equilibrium traces or equilibrichnia 22 1.2 Characteristics of trace fossils 8 1.4.10 Predation traces or praedichnia 23 1.2.1 T race fossils represent evidence of 1.4.11 Nesting traces or calichnia 24 behavior 8 1.4.12 Pupation chambers or pupichnia 24 1.2.2 T he same organism may produce more 1.4.13 Fixation/anchoring traces or fixichnia 24 than one ichnotaxon 9 1.4.14 Bioclaustration structures or impedichnia 24 1.2.3 T he same ichnotaxon may be produced 1.4.15 Discussion: complex traces and extended by more than one organism 10 organisms 24 1.2.4 M ultiple architects may produce a single 2 Taxonomy of trace fossils 25 structure 10 2.1 Approach and philosophy 25 1.2.5 P roducers are commonly soft-bodied 2.2 Some problems and practical guidelines 26 animals that are rarely preserved 11 2.3 Ichnotaxobases 27 1.2.6 T race fossils are commonly preserved 2.3.1 General form 28 in rock units that are otherwise 2.3.2 Wall and lining 28 unfossiliferous 12 2.3.3 Branching 29 1.2.7 T he same biogenic structure may be 2.3.4 Fill 30 differentially preserved in various 2.3.5 Spreite 31 substrates 12 2.4 Compound and composite trace fossils 31 1.2.8 T race fossils commonly have long 2.4.1 Compound trace fossils 31 stratigraphic ranges 13 2.4.2 Composite trace fossils 33 1.2.9 T race fossils commonly have narrow 2.5 Hierarchies in ichnotaxonomy 34 environmental ranges 14 2.6 Vertebrate ichnotaxonomy 35 1.2.10 Trace fossils are rarely transported 14 2.7 The uncertainty principle in ichnotaxonomy 36 1.3 Preservation of trace fossils 14 2.8 Classification of trace fossils in outcrops and 1.3.1 Stratinomic classifications 14 cores 36 1.3.2 P hysiochemical processes of 3 Paleobiology of trace fossils 38 preservation and alteration 17 3.1 Modes of life 38 1.4 Ethology of trace fossils 17 3.1.1 Feeding strategy 38 1.4.1 Resting traces or cubichnia 18 3.1.2 Position with respect to the 1.4.2 Locomotion traces or repichnia 20 substrate–water interface 43 1.4.3 Death traces or mortichnia 20 3.1.3 Level of motility 43 vii Contents viii 3.2 Modes of interaction with the substrate 44 6.1.1 Hydrodynamic Energy 99 3.3 Locomotion and burrowing mechanisms 46 6.1.2 Substrate 101 3.3.1 M ultiple modes of locomotion: the 6.1.3 Oxygenation 104 empiricist approach 46 6.1.4 Salinity 107 3.3.2 B urrowing pre-adaptations: the 6.1.5 Sedimentation rate 109 morpho-structural approach 55 6.1.6 Food supply 110 3.3.3 I n search of a universal mechanism: the 6.1.7 Bathymetry 111 rationalist approach 56 6.1.8 Water turbidity 113 3.4 Movement ecology 57 6.1.9 Climate 113 4 The ichnofacies model 58 6.1.10 Water table 115 4.1 The ichnofacies concept 58 6.2 Role of taphonomy 116 4.2 Softground marine ichnofacies 59 6.3 Ichnodiversity and ichnodisparity 117 4.2.1 Psilonichnus ichnofacies 59 6.4 Population strategies 119 4.2.2 Skolithos ichnofacies 60 6.5 Resident and colonization ichnofaunas 119 4.2.3 Cruziana ichnofacies 62 6.6 Ecosystem engineering 120 4.2.4 Zoophycos ichnofacies 64 6.7 Organism–organism interactions 121 4.2.5 Nereites ichnofacies 65 6.8 Spatial heterogeneity 123 4.3 Substrate-controlled ichnofacies 67 7 Ichnology of shallow-marine clastic environments 126 4.3.1 Glossifungites ichnofacies 67 7.1 Wave-dominated shallow marine 126 4.3.2 Trypanites ichnofacies 69 7.1.1 Backshore 128 4.3.3 Gnathichnus ichnofacies 71 7.1.2 Foreshore 131 4.3.4 Teredolites ichnofacies 71 7.1.3 Upper shoreface 131 4.4 Invertebrate continental ichnofacies 73 7.1.4 Middle shoreface 131 4.4.1 Scoyenia ichnofacies 73 7.1.5 Lower shoreface 132 4.4.2 Mermia ichnofacies 75 7.1.6 Offshore transition 136 4.4.3 Coprinisphaera ichnofacies 76 7.1.7 Upper offshore 136 4.4.4 Termitichnus ichnofacies 77 7.1.8 Lower offshore 139 4.4.5 Celliforma ichnofacies 77 7.1.9 Shelf 139 4.4.6 Octopodichnus–Entradichnus ichnofacies 78 7.2 Tide-dominated shallow marine 139 4.5 Vertebrate ichnofacies 79 7.2.1 Supratidal marsh and mangroves 141 4.5.1 Chelichnus ichnofacies 80 7.2.2 Mud flat 143 4.5.2 Grallator ichnofacies 80 7.2.3 Mixed flat 145 4.5.3 Brontopodus ichnofacies 80 7.2.4 Sand flat 145 4.5.4 Batrachichnus ichnofacies 80 7.2.5 Tidal channels and creeks 146 4.5.5 Characichichnos ichnofacies 80 7.2.6 Subtidal sandbars and tidal dunes 146 4.6 Pitfalls and confusions in ichnofacies analysis 80 7.3 Mixed tide- and wave-influenced shorelines 147 5 The ichnofabric approach 83 7.3.1 Wave-dominated tidal flats 148 5.1 Tiering 83 7.3.2 Tidal beaches 150 5.2 Ichnofabrics: concepts and methods 84 7.4 Muddy shorelines 150 5.2.1 Q uantifying bioturbat ion and 8 Ichnology of marginal-marine environments 152 illustrating ichnofabrics 84 8.1 Estuaries 152 5.2.2 Taphonomy of ichnofabrics 85 8.1.1 Wave-dominated estuaries 152 5.3 Types of ichnofabrics 86 8.1.2 Tide-dominated estuaries 156 5.4 The ichnoguild concept 87 8.2 Bays 160 5.5 Paleosol ichnofabrics 90 8.2.1 Restricted bays 160 5.6 The role of bioturbation, bioerosion, and 8.2.2 Open bays 162 biodeposition 91 8.3 Deltas 163 5.7 Bioturbation-enhanced permeability and 8.3.1 River-dominated deltas 165 reservoir characterization 91 8.3.2 Wave-dominated deltas 169 5.8 Critical evaluation: ichnofabrics versus 8.3.3 Tide-dominated deltas 174 ichnofacies or ichnofabrics and ichnofacies? 96 8.4 Fjords 175 9 Ichnology of deep-marine clastic environments 181 Part II Spatial trends 9.1 Slopes 181 6 Trace fossils and paleoecology 99 9.1.1 Topographically simple slopes 181 6.1 Response to environmental parameters 99 9.1.2 Topographically complex slopes 184

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