Unit 3 Flashcards
The study of fossilization; how are they formed and how are they preserved in geologic record
Taphonomy
Begining with the most recent and going back list the Eras we are responsibile for knowing
- Cenozoic
- Mesozoic
- Palaeozoic
- Precambrian
List the periods that took place during the Palaeozoic Era
(Starting with the most recent)
- Permian
- Carboniferous
- Devonian
- Silurian
- Ordovician
- Cambrian
List the periods that took place during the Mesozoic Era
(Starting with the most recent)
- Cretaceous
- Jurassic
- Triassic
List the periods that took place during the Cenozoic Era
(Starting with the most recent)
- Quaternary
- Tertiary
How long ago was the extinction event that marked the end of the Precambrian Era and the beggining of the Palaeozoic Era
590 million years ago
How long ago was the extinction event that marked the end of the Palaeozoic Era and the beggining of the Mesozoic Era
250 million years ago
How long ago was the extinction event that marked the end of the Mesozoic Era and the beggining of the Cenozoic Era
65 million years ago
The extinction event that is happening now marks the end of what Era
Cenozoic Era
List some examples of Catastrophism
- Vulcanism
- Earthquakes
- Tsunamis
- Floods
- Climate Change (rapid)
- Extraterrestrial Impacts
List some examples of Uniformitarianism
- Sedimentation
- Erosion / Weathering
- Subsidence
- Uplift
Any evidence of past life
fossil
A piece of the organism or whole organism
Direct fossil
Some indication of the organism but no organism present
Indirect fossil
can be seen with the naked eye; large/showy
Macrofossil
Can only be seen with a microscope; very small
microfossil
This mode of preservation occurs when a specimen is compressed or flattened by the weight of sediments in water and there is organic material present
Compaction
This mode of preservation occurs when a specimen is compressed or flattened by the weight of sediments in water and there is no organic material present
Impression
This mode of preservation happens when compounds from water seep into tissue and form precipitates that become rock that fills in spaces to support tissue
Permineralization/Petrification
This mode of preservation occurs when electrically charged sediments are drawn to the surface and lithify. Internal mater is completely replaced.
Mold: the outline of the specimen
Cast: like a “copy” of the specimen that can be made from a mold
Durible hard parts are preserved more or less unchanged
Duripartic
Organisms that get caught in plant resin and becomes hard (Amber)
Encasement
Drying out of organisms in high or low temperatures with no moisture
Dessication
In most cases formation of a fossil requires
- Decay must be inhibited (by low temperature, low humidity, low oxygen, or acid pH)
- Plant and animal parts must remain undisturbed (once formed fossils can also be destroyed through erosion/weathering, chemical dissolution and fragmentation/disarticulation as well as a combination of heat and pressure)
- A source of sediments (Most fossils are produced in sediments that become rock; lithification)












