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Biostratigraphy. TypeUnitsDefined?True time units? LithoMember Formation Group Rock lithologyNo – time transgressive BioZone Stage FossilsSort of ChronoEon,

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Presentation on theme: "Biostratigraphy. TypeUnitsDefined?True time units? LithoMember Formation Group Rock lithologyNo – time transgressive BioZone Stage FossilsSort of ChronoEon,"— Presentation transcript:

1 Biostratigraphy

2 TypeUnitsDefined?True time units? LithoMember Formation Group Rock lithologyNo – time transgressive BioZone Stage FossilsSort of ChronoEon, Era, Period, Epoch, Age TimeYes, but how do you measure? SequenceSystem Tract Sequence Transgression/RegressionNo – occur at different places at different times CyclocyclesAstronomical cyclesYes, but how do you recognize? MagnetoPolarity zonePatterns of magnetic polarity Sort of – if correlated to isotopic dates

3 Comparing Rock and Time units ChronostratRock-Time (Biostrat)Example EonEonothemPhanerozoic EraErathemMesozoic PeriodSystemCretaceous Epoch Early Middle Late Series Lower Middle Upper Late Cretaceous Upper Cretaceous AgeStageMaestrichtian 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 aren’t 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 weren’t 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 zoneDefinition Taxon range zone (total)First to last of one species Concurrent range zoneOverlap of taxa, 1 st to last of different species Interval range zoneInterval between two species: 1 st to 1 st, last to last Lineage (consecutive- range) zone 1 st appearance within a lineage (commonly used in forams) Assemblage zoneDefined on 1 st and last of one taxa, characterized by other taxa Acme (abundance) zoneAbundance 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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