BIOEE 1780: PRELIM 1 Flashcards
\FOSSILS
are the remains or traces of once living organisms and they can take many forms: skeleton, impression cast trace or even poop
Why aren’t there more fossils
predators and scavengers
bacterial decay
dissolution in water
physical disturbance (wave action, wind etc)
Special conditions to promote fossilization
rapid burial
protection from physical disturbance
anaerobic environments
Where are most fossils found in
Sedimentary Rocks
Sedimentary Rocks
are formed from deposition of sediments falling to the bottom of a body of water
What gets preserved from fossils
- the hard parts in ANIMALS
- seeds, pollen leaves, wood, and rarely flowers in PLANTS
- bacteria, microbial mats in MICROBES
Stromatolites
formed from biofilms of cyanobacteria that trap sediment which eventually hardens and forms layer
Types of preservation
- original remains
-permineralization retains structures
-trace fossils
-impression fossils
Impression fossil
are fossils made from a carbonaceous film imprint of the organism
Permineralization
is a process where minerals are deposited in tiny holes within bones, or wood and over time completely replace organisms and all that remains is a stone structure
original remains
have the most information
Lagerstatten
storage place and is used to refer to exceptional perservation
Cambrian Explosion
period of time at the beginning of the Phanerzotic is when nearly all of the major animal phyla appeared
Burgess Shale
famous lagerstatten from the cambrian and has yielded many of the organisms that contribute to our understanding of the Cambrian explosion
Relative Dating 4 principles
-superposition
-original horizontality
-lateral continuity
-cross-cutting
superposition
youngest layer on top
original horizontality
layers are first deposited horizontally and due to the movement of continental plates are repositioned