Fossils Unit LO 1-11 Quiz Flashcards
Uniformitiasm vs Catastrophism
Newer idea that earth is old and everything now happened in the past.
Earth is young and created from catastrophes.
Outrcrop and Strata
Exposed bedrock on the surface of the Earth.
Layers that have been deposited over time.
Faults and intrusions
Something cuts through a rock layer, igneous rock being forced up into another rock layer
Stratigraphic Column
Layers that are in the same relative order in a sequence that must have been in line with each other.
5 lays of relative dating and what they mean
- Law of Superposition - oldest layers on bottom, younger as you go up
- Law of Original Horizontality - Layers are almost always originally horizontal
- Law of cross-cutting - faults and intrusions are younger than the layers that they cut across
- Law of inclusions - inclustions are older than the rock that they are in
- Law of Unconformities - Surface that represents a gap in the rock formation (either rock was not depositied or there was erosion)
Steps to an unconformity
- Deposition of a sediment
- Rocks are tilted (deformation)
- Erosion occurs, removing rocks and creating an uneven surface
- More rocks layers are deposited straight onto the slanted, eroded layer, causing an unconformity
Why are rock records incomplete?
various weathering things such as erosion cause rocks to move locations, leaving some areas without rocks that would have originally been there.
Body vs Trace fossils
Body fossils are fossils that preserve part of an organism’s actual body (bone, teeth, shell, feathers etc.) providing evidence on the organism’s actual structure. Preservation types include models, casts, carbon films, petrified, and preserved in something.
Trace fossils are fossils that provide indirect evidence of life (footprints, tracks, burrows, etc.) that reveal behavior or interactions of organisms. Preservation types include gastroliths, tracks, trails, and burrows.
Molds and casts
Molds - when a shell is buried then dissolves, it leaves a mold
Casts - when sediments and minerals fill the open space below a shell
Carbon film
organic matter in an organism is compressed and heated, leaving behind a thin residue of carbon
Preservation fossils
when an organism completely is inside of something (sap from tree, ice, tar)
Petrified fossils
when organic materials is replaced with minerals, turning it into a stone
What environmental conditions favor fossil preservation?
Areas that are below freezing are good areas for fossils to be preserved in ice. Tar and amber also preserve fossils. Some bog environments that are low-oxygen and acidic can naturally mummify animals into fossils. Also, really hot areas can dry out organisms, also causing them to mummify.
Four charactaristics of index fossils
Widespread around the Earth
Easily identifiable
From species that lived for a short time-span
Abundant
Index fossil example and how they help uncover the past
Trilobites are an example of an index fossil because they only live for around 2 geological time periods, where others live much longer. They are also easy to identify. This can be used to provide critical information about the past because you can see what organism lives when based on where they are around the trilobite and also how long they lived.