Biostratigraphy - PowerPoint PPT Presentation

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Biostratigraphy

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... forams, rads, ammonites, graptolites, pollen, nannofossils But zones are defined for less-than-ideal organisms, e.g., dinosaurs, clams, conodonts, ... – PowerPoint PPT presentation

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Title: Biostratigraphy


1
Biostratigraphy
2
Type Units Defined? True time units?
Litho Member Formation Group Rock lithology No time transgressive
Bio Zone Stage Fossils Sort of
Chrono Eon, Era, Period, Epoch, Age Time Yes, but how do you measure?
Sequence System Tract Sequence Transgression/Regression No occur at different places at different times
Cyclo cycles Astronomical cycles Yes, but how do you recognize?
Magneto Polarity zone Patterns of magnetic polarity Sort of if correlated to isotopic dates
3
Comparing Rock and Time units
Chronostrat Rock-Time (Biostrat) Example
Eon Eonothem Phanerozoic
Era Erathem Mesozoic
Period System Cretaceous
Epoch Early Middle Late Series Lower Middle Upper Late Cretaceous Upper Cretaceous
Age Stage Maestrichtian
Zone (regional) Baculites rex
4
  • Larger units are built from smaller ones
  • Eg, stages are defined by the zones in them.
  • We define bottoms only
  • If you define bottoms AND tops, one boundary has
    two definitions that may not coincide.

5
Why arent biostrat correlations true time
correlations?
  • Are you looking at last appearance or
    unconformity?
  • Facies dependence facies are time-transgressive
  • Regional speciation extinction
  • Shifting climate zones/biogeographic provinces

6
Other challenges
  • Preservation problems
  • Poorly preserved organisms and less abundant
    organisms are unlikely to be found
  • Signor-Lipps effect poorly preserved and less
    abundant species appear to go extinct earlier
    than they actually do.
  • Lazarus species apparently come back from the
    dead because they werent preserved in between
    two occurrences
  • Zombie species - appear above their extinction
    because they were exposed by erosion and
    reworked, then deposited in younger sediment

7
What makes a good index fossil?
  • Abundant
  • Facies independent (planktonic, nektonic)
  • Easily preserved and collected
  • Widely distributed (global if possible)
  • Short species life (rapidly evolving)
  • Easily identified
  • Best organisms forams, rads, ammonites,
    graptolites, pollen, nannofossils
  • But zones are defined for less-than-ideal
    organisms, e.g., dinosaurs, clams, conodonts,
    trilobies

8
Kind of zone Definition
Taxon range zone (total) First to last of one species
Concurrent range zone Overlap of taxa, 1st to last of different species
Interval range zone Interval between two species 1st to 1st, last to last
Lineage (consecutive-range) zone 1st appearance within a lineage (commonly used in forams)
Assemblage zone Defined on 1st and last of one taxa, characterized by other taxa
Acme (abundance) zone Abundance peak of one taxa
9
Quantitative Biostratigraphy
  • Uses a wider range of data than
    appearance/disappearance
  • Abundance peaks
  • Ratios of species
  • Based in sophisticated statistics
  • Correlation analysis (matches patterns of peaks)
  • Cluster analysis makes groups for assemblage
    zones
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