Ichnology : organism-substrate interactions in space and time /

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Detalles Bibliográficos
Autor principal: Buatois, Luis A.
Otros Autores: Mángano, María Gabriela
Formato: Desconocido
Lenguaje:Español
Publicado: Cambridge : Cambridge University Press, 2011
Edición:1st ed.
Materias:
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.