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32 Cards in this Set

  • Front
  • Back

Three constraints for reconstructions

biological, physiological and chemical possibility

paleontology

general study of fossils

Paleobiology

study of extinct organism lifestyle

Functional morphology

shape of a biological structure is directly relation to its functionality

Three methods of reconstruction

analogy, modelling, context

Analogous reconstruction

based on form/function relationships


esp. useful for homologous structures

Modelling reconstruction

use of physical or mathematical modes

Context

based off associated fossils and sediment

Relationship between sediment and current

Finer sediments indicate faster water currents

Cost of transport

energy need to move the body based of muscle composition

Cost of transport gives information about

metabolic requirements and maneuverability

Three levels of reliability

Probable, plausible and possible

Body fossils

record of physical body

Trace fossils

evidence of organismal behavior

Ichnotaxa

species implicated by trace fossil

Environmental bias of fossilization

Favors depositional environments over erosional environments

Lagerstatten

ideal conditions for fossilization

Requirements of Lagerstatten

rapid burial, fine grain sediment, biologically and physiologically benign environment

Taphonomy

study of changes to organic material during fossilization

Biotic stage

birth--> death (gathers information about life)

Internment stage

death --> burial

Destructive processes of internment stage

decomp, dissassociation, abrasion, breakage and winnowing

Diagenetic stage

burial --> discovery

Destructive processes of diagenetic stage

dissolution, compaction and crystal intrusion

Investigative stage

discovery --> eventual loss

Biases in fossil records

adults, hard-boned, depositional, common, large

Types of fossilization

freezing, desiccation, petrifaction, carbonization and trace fossils

Desiccation

produces a mummy, rapid drying in arid environments

Petrifaction

addition of a new chemical (permineralization, replacement and recrystallization)

Permineralization

empty spaces in organic material replaced by new chemical

Recrystallization

modified organic material --> related crystalline form

Carbonization

degradation into carbon film (retains overall form but not internal structure)