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
lateral continuity
each layer is deposited at the same time and so seven if erosion has removed has removed some of the layer- that layer is still the same after the gap caused by erosion
cross-cutting
geological layers or intrusions that cut across other layers are always younger
Index Fossils
are fossils that are distinct to a particular rock layer and are also geographically widespread to help identify layers in different locations
How do we know the age of a fossil
- relative dates
- absolute dates
geological chronology
is the science of dating geological layers and fossils
absolute dating
based on the radioactive decay of unstable isotopes
- decay of parent isotope gives rise to stable daughter isotope and the rate is referred to as half-life
-ONLY USES IGNEOUS ROCK because of 100% parent isotope
3 types of isotopes
- uranium- lead (older fossils)
- potassium- argon (older fossils)
- carbon (recent fossils)