Lecture 2 - the nature of the fossil record Flashcards
to become a useful fossil an organism must:
1 - die and avoid destruction by biological and physical processes
2 - be transported into an environment where it is incorporated into a sediment - then fossilised by taphonomy
3 - that sediment must then avoid destruction by diagenetic, metamorphic or erosive processes
4 - fossil must become exposed at the surface and discovered by someone who will study it
why is the fossil record incomplete?
1 - sediment only accumulates over a very small area of the earth at any given time
2 - only a tiny fraction of the organisms that ever live will be fossilised
3 - most fossils will be destroyed with the rock that contains them
4 - only a tiny fraction of fossils ever formed will be collected and studied
why is the fossil record biased?
1 - certain organisms/ parts of organisms are preferentially preserved
2 - certain environments preferentially preserve sediment and hence fossils
3 - older rocks are more likely to be destroyed
4 - collector bias e.g. from different parts of the world
organisms that leave a fossil record are:
bacteria - sheath and structures built by bacteria
protists - those that form exo- and endoskeletons
plants - woody tissues (lignin), cuticles and spores preserve well
fungi - chitinous spores and hyphae preserve well
animals - those with recalcitrant exo- and endoskeletons
oceanic crust covers what percentage of the planet?
70%
why does most sediment occur on continental crust?
oceanic crust is constantly created / destroyed therefore sediment doesn’t build up
what are large-scale bias’ related to the earth-system?
- sea level changes - due to long term climate trends and continental configuration
- continental configuration - more / less shelf
- atmospheric composition - e.g. oxygen level
how do we successfully interpret the fossil record?
- plot the spatial and temporal distribution of fossils therefore allowing us to work out the plate positions at that time
when interpreting the fossil record we can also consider:
- ghost ranges - sharing of common ancestors
- probabilities of range extensions
when interpreting the fossil record we can analyse
- volume of rock deposited per time slice
- exposed area of rock per time slice
Dinosaur time span?
- first appeared in the Triassic period
- late Jurassic more familiar, larger dinosaurs evolve
- early late Cretaceous period, birds appear
- late Cretaceous period mass extinction