Ichnology : organism-substrate interactions in space and time /
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| Formato: | Desconocido |
| Lenguaje: | Español |
| Publicado: |
Cambridge :
Cambridge University Press,
2011
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| Edición: | 1st ed. |
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| Aporte de: | Registro referencial: Solicitar el recurso aquí |
Tabla de Contenidos:
- Introduction
- Part I Conceptual tools and methods-- 1 The basics of ichnology
- 1.1 Basic concepts
- 1.2 Characteristics of trace fossils
- 1.2.1 Trace fossils represent evidence of behavior
- 1.2.2 The same organism may produce more than one ichnotaxon
- 1.2.3 The same ichnotaxon may be produced by more than one organism
- 1.2.4 Multiple architects may produce a single structure
- 1.2.5 Producers are commonly soft-bodied animals that are rarely preserved
- 1.2.6 Trace fossils are commonly preserved in rock units that are otherwise unfossiliferous
- 1.2.7 The same biogenic structure may be differentially preserved in various substrates
- 1.2.8 Trace fossils commonly have long stratigraphic ranges
- 1.2.9 Trace fossils commonly have narrow environmental ranges
- 1.2.10 Trace fossils are rarely transported
- 1.3 Preservation of trace fossils
- 1.3.1 Stratinomic classifi cations
- 1.3.2 Physiochemical processes of preservation and alteration
- 1.4 Ethology of trace fossils
- 1.4.1 Resting traces or cubichnia
- 1.4.2 Locomotion traces or repichnia
- 1.4.3 Death traces or mortichnia
- 1.4.4 Grazing traces or pascichnia
- 1.4.5 Feeding traces or fodinichnia
- 1.4.6 Dwelling traces or domichnia
- 1.4.7 Traps and farming traces or agrichnia
- 1.4.8 Escape traces or fugichnia
- 1.4.9 Equilibrium traces or equilibrichnia
- 1.4.10 Predation traces or praedichnia
- 1.4.11 Nesting traces or calichnia
- 1.4.12 Pupation chambers or pupichnia
- 1.4.13 Fixation/anchoring traces or fi xichnia
- 1.4.14 Bioclaustration structures or impedichnia
- 1.4.15 Discussion: complex traces and extended organisms
- 2 Taxonomy of trace fossils
- 2.1 Approach and philosophy
- 2.2 Some problems and practical guidelines
- 2.3 Ichnotaxobases
- 2.3.1 General form
- 2.3.2 Wall and lining
- 2.3.3 Branching
- 2.3.4 Fill
- 2.3.5 Spreite
- 2.4 Compound and composite trace fossils
- 2.4.1 Compound trace fossils
- 2.4.2 Composite trace fossils
- 2.5 Hierarchies in ichnotaxonomy
- 2.6 Vertebrate ichnotaxonomy
- 2.7 The uncertainty principle in ichnotaxonomy
- 2.8 Classifi cation of trace fossils in outcrops and cores
- 3 Paleobiology of trace fossils
- 3.1 Modes of life
- 3.1.1 Feeding strategy
- 3.1.2 Position with respect to the substrate–water interface
- 3.1.3 Level of motility
- 3.2 Modes of interaction with the substrate
- 3.3 Locomotion and burrowing mechanisms
- 3.3.1 Multiple modes of locomotion: the empiricist approach
- 3.3.2 Burrowing pre-adaptations: the morpho-structural approach
- 3.3.3 In search of a universal mechanism: the rationalist approach
- 3.4 Movement ecology
- 4 The ichnofacies model
- 4.1 The ichnofacies concept
- 4.2 Softground marine ichnofacies
- 4.2.1 Psilonichnus ichnofacies
- 4.2.2 Skolithos ichnofacies
- 4.2.3 Cruziana ichnofacies
- 4.2.4 Zoophycos ichnofacies
- 4.2.5 Nereites ichnofacies
- 4.3 Substrate-controlled ichnofacies
- 4.3.1 Glossifungites ichnofacies
- 4.3.2 Trypanites ichnofacies
- 4.3.3 Gnathichnus ichnofacies
- 4.3.4 Teredolites ichnofacies
- 4.4 Invertebrate continental ichnofacies
- 4.4.1 Scoyenia ichnofacies
- 4.4.2 Mermia ichnofacies
- 4.4.3 Coprinisphaera ichnofacies
- 4.4.4 Termitichnus ichnofacies
- 4.4.5 Celliforma ichnofacies
- 4.4.6 Octopodichnus–Entradichnus ichnofacies
- 4.5 Vertebrate ichnofacies
- 4.5.1 Chelichnus ichnofacies
- 4.5.2 Grallator ichnofacies
- 4.5.3 Brontopodus ichnofacies
- 4.5.4 Batrachichnus ichnofacies
- 4.5.5 Characichichnos ichnofacies
- 4.6 Pitfalls and confusions in ichnofacies analysis
- 5 The ichnofabric approach
- 5.1 Tiering
- 5.2 Ichnofabrics: concepts and methods
- 5.2.1 Quantifying bioturbation and illustrating ichnofabrics
- 5.2.2 Taphonomy of ichnofabrics
- 5.3 Types of ichnofabrics
- 5.4 The ichnoguild concept
- 5.5 Paleosol ichnofabrics
- 5.6 The role of bioturbation, bioerosion, and biodeposition
- 5.7 Bioturbation-enhanced permeability and reservoir characterization
- 5.8 Critical evaluation: ichnofabrics versus ichnofacies or ichnofabrics and ichnofacies?
- Part II Spatial trends
- 6 Trace fossils and paleoecology
- 6.1 Response to environmental parameters
- 6.1.1 Hydrodynamic Energy
- 6.1.2 Substrate
- 6.1.3 Oxygenation
- 6.1.4 Salinity
- 6.1.5 Sedimentation rate
- 6.1.6 Food supply
- 6.1.7 Bathymetry
- 6.1.8 Water turbidity
- 6.1.9 Climate
- 6.1.10 Water table
- 6.2 Role of taphonomy
- 6.3 Ichnodiversity and ichnodisparity
- 6.4 Population strategies
- 6.5 Resident and colonization ichnofaunas
- 6.6 Ecosystem engineering
- 6.7 Organism–organism interactions
- 6.8 Spatial heterogeneity
- 7 Ichnology of shallow-marine clastic environments
- 7.1 Wave-dominated shallow marine
- 7.1.1 Backshore
- 7.1.2 Foreshore
- 7.1.3 Upper shoreface
- 7.1.4 Middle shoreface
- 7.1.5 Lower shoreface
- 7.1.6 Offshore transition
- 7.1.7 Upper offshore
- 7.1.8 Lower offshore
- 7.1.9 Shelf
- 7.2 Tide-dominated shallow marine
- 7.2.1 Supratidal marsh and mangroves
- 7.2.2 Mud fl at
- 7.2.3 Mixed fl at
- 7.2.4 Sand fl at
- 7.2.5 Tidal channels and creeks
- 7.2.6 Subtidal sandbars and tidal dunes
- 7.3 Mixed tide- and wave-infl uenced shorelines
- 7.3.1 Wave-dominated tidal fl ats
- 7.3.2 Tidal beaches
- 7.4 Muddy shorelines
- 8 Ichnology of marginal-marine environments
- 8.1 Estuaries
- 8.1.1 Wave-dominated estuaries
- 8.1.2 Tide-dominated estuaries
- 8.2 Bays
- 8.2.1 Restricted bays
- 8.2.2 Open bays
- 8.3 Deltas
- 8.3.1 River-dominated deltas
- 8.3.2 Wave-dominated deltas
- 8.3.3 Tide-dominated deltas
- 8.4 Fjords
- 9 Ichnology of deep-marine clastic environments
- 9.1 Slopes
- 9.1.1 Topographically simple slopes
- 9.1.2 Topographically complex slopes
- 9.2 Deep-marine turbidite systems
- 9.2.1 Fine-grained turbidite systems
- 9.2.2 Coarse-grained turbidite systems
- 9.3 Hyperpycnal systems
- 9.4 Basin plains
- 10 Ichnology of continental environments
- 10.1 Alluvial fans
- 10.2 Rivers
- 10.2.1 Channels
- 10.2.2 Overbank
- 10.3 Lakes
- 10.3.1 Closed lakes
- 10.3.2 Open lakes
- 10.4 Deserts
- 10.5 Paleosols
- 11 Ichnology of carbonate environments, rocky shorelines, and volcanic terrains
- 11.1 Carbonate systems
- 11.1.1 Shallow-marine tropical carbonates
- 11.1.2 Reefs
- 11.1.3 Shelf and deep-sea chalk
- 11.1.4 Carbonate turbidites
- 11.2 Rocky shorelines
- 11.3 Volcanic terranes
- Part III A matter of time
- 12 Trace fossils in sequence stratigraphy
- 12.1 Recognition of discontinuity surfaces
- 12.2 Erosional discontinuities
- 12.2.1 Regressive surfaces of marine erosion
- 12.2.2 Lowstand surfaces of erosion
- 12.2.3 Transgressive surfaces of erosion
- 12.2.4 Co-planar surfaces of lowstand erosion and transgressive erosion
- 12.3 Non-erosional discontinuities
- 12.4 Characterization of parasequences
- 12.4.1 Wave-dominated parasequences
- 12.4.2 Tide-dominated parasequences
- 12.4.3 Deltaic parasequences
- 12.5 Delineation of parasequence sets and systems tracts
- 12.5.1 Progradational patterns
- 12.5.2 Retrogradational patterns
- 12.6 Carbonate sequence stratigraphy
- 12.7 Continental sequence stratigraphy
- 12.7.1 Lake basins
- 12.7.2 Alluvial plains
- 12.8 Evaluation of the models
- 13 Trace fossils in biostratigraphy
- 13.1 The Proterozoic–Cambrian boundary
- 13.2 Cruziana stratigraphy
- 13.3 Arthrophycid stratigraphy
- 13.4 Other invertebrate ichnotaxa
- 13.5 Tetrapod trackways
- 14 Trace fossils in evolutionary paleoecology
- 14.1 Evolutionary events
- 14.1.1 The early record of complex life
- 14.1.2 Ediacaran ecosystems
- 14.1.3 The Cambrian explosion
- 14.1.4 The Ordovician radiation
- 14.1.5 The origin of dinosaurs
- 14.1.6 Mass extinctions
- 14.2 Animal–substrate interactions and ecosystems through time
- 14.2.1 Colonization of shallow-marine environments
- 14.2.2 Colonization of the deep sea
- 14.2.3 Colonization of hard substrates
- 14.2.4 Colonization of tidal fl ats
- 14.2.5 Colonization of brackish-water environments
- 14.2.6 Colonization of freshwater and terrestrial environments
- 14.2.7 Arthropod–plant interactions through the Phanerozoic
- 15 Ichnology in paleoanthropology and archaeology
- 15.1 Applications in paleoanthropology
- 15.1.1 The Pliocene record
- 15.1.2 The Early Pleistocene record
- 15.1.3 The Middle Pleistocene record
- 15.1.4 The Late Pleistocene record
- 15.1.5 The Holocene record
- 15.2 Applications in archaeology
- 15.2.1 Biogenic structures in natural and artifi cial substrates
- 15.2.2 Ichnological hierophanies.