After midterm Flashcards
(124 cards)
French developments
George Cuvier and Alexander brongniart developed ideas of faunal succession
Who was the first person to go beyond faunal succession and develop a modern concept of biostrigraphy?
Alcide dorbigny
What did dorbigny study?
Studied the Jurassic fossils and strata in southern France
Albert Oppel
Completed the modernization of bio stratigraphy
What makes a good biostratigraphic indicator fossil?
Distinctive Abundant Widespread geological distribution Not facies specific Rapid evolution Short temporal range
Reasons why local first and last appearance data isn’t globl
Biogeopgraphic: all species are geographic in origin, may immigrate to other places, suffer local extinction
Preservation
Facies specificity
Uncomformites: no rocks of that age in local sections
Classification of grace fossils
Ethnologic or taxonomic
Ethologic
Trace fossils are primarily evidence of animal behaviour
Seilacher established a small number of ethologic categories
Categories of ethologics
Resting trace: cubichnia Locomotion trace: Repichnia Grazing trace: pascichnia Feeding traces: Fodinichnia Dwelling traces: domichnia Traps/farming traces: agrichnia Escape traces: Fugichnia Equilibrium traces: equilibrichnia Predation traces: praedichnia Nesting traces: calichnia Fixation/ anchoring traces: fixichnia Death traces: mortichnia
Bio stratigraphy
The art and science of telling time from rocks
Based on faunal succession which was first discovered by William smith
Ichnofacies
Trace fossil association that recurs throughout geologic time in response to a set of paleoenvironmental conditions
Food resource paradigm
Limiting factor of distribution of trace making organisms in shallow marine water
Brackish water trace fossil model
- Reduced diversity of trace fossils in many cases mono specific
- Reduced size of trace fossils compared to their fully marine counterparts
- Predominance of simple trace fossils
- Sparse bioturbation
Ediacaran kimberella
In Russia probably a mollusk
Graphic correlation
Quantitative method of biostratigraphy developed by Alan shaw. Works by correlating multiple stratigraphic sections
If correlation is 45 degrees then sections had identical fossil distribution and rock accumulation
If different then one section had sediment accumulating faster then the other section
Biostratigraphic resolution
Ideally when using biostrigraphy for correlation we would like to do so with the greatest detail. Subdivide rocks into shorter zones this allows us to discriminate between events that happen closer together in time
Precision
+ or - error of an age
Dual biostratigraphy
Attempts to take in the spatial distribution of fossils as well as the temporal distribution
Bio facies
Biotic stratigraphic unit of environmental significance. How these are identified is you look at the different genera in your fossil collection
Paleoecology
Study of the interactions of fossils with each other and with the environment they lived in the geological past
Paleoautecology
Relationships of individual organisms to their environment
Palesynecology
Relationships of groups of organisms to each other and to their environment
Information potential
Life habits of extinct organisms
Nature of ancient communities and ecosystems
Paleoenvironmental reconstruction
Sea level changes
Pelagic
Live in the water column
Can be subdivided into plankton (floaters) and nekton (swimmers)