Palaeobiology Flashcards
(258 cards)
Definition: The branch of palaeontology that deals with the processes of fossilization
Taphonomy
Definition: The physical and chemical processes that affect sedimentary materials after deposition
Diagenesis
To be a fossil, an organism must:
1. Die and avoid destruction
2. Be in an environment where they can be buried
3. Be fossilized
4. Avoid d—— or m——- processes
5. Avoid e—–
6. Become e—— and discovered
diagenetic, metamorphic,
erosion, exposed
Fossils can have a n—— cast (rarer) or an i—– cast
natural, internal
Why is the fossil record incomplete?
1. S—— only accumulates on small area of Earth
2. Only small amount of organisms fossilized
3. Most d——— with the rock they are in
4. Only a t— fraction found & studied
sediment, destroyed, tiny
Why is the fossil record biased?
1. Certain o——- parts preserve better
2. Certain e——— preserve better
3. O—- rock more likely to be destoryed
4. C——— bias ie. First-world countried
Organism(s), environments, older, collector
Which kingdom leaves these parts fossilized?
Stromatolites and certain bacterial sheathes
Bacteria
Which kingdom leaves these parts fossilized? Those with an exo or endoskeleton.
Protists (single-celled living things)
Which kingdom leaves these parts fossilized? Woody tissues made of lignin. Cuticles made of Cutan. Spores known as sporopollenin.
Plants
Which kingdom leaves these parts fossilized? Chitnous spores and hyphae. Unfortunately these are often similar across species and the ‘useful’ part is lost.
Fungi
Which kingdom leaves these parts fossilized? Those with recalcitrant exo and endoskeletons
Animals
In which environments do sediments accumulate?
- C——– S—-.
- Rarely in deep sea r– c— from the atmosphere
- OCCASIONALLY in inland f—– in the mountains
continental shelves, red clay, faults
Large-scale biases of fossil distribution:
1. S–Level changes
2. Continental c——-. More s—- when continents SPLIT
3. Atmospheric composition. More o—— = more composition
sea, configuration, shelf, oxygen
Definition: It is probable that patterns in the fossil record reflect both biological and geological signals. We must therefore understand the geological signals
The common cause hypothesis
How to interpret the fossil record;
- Plot s—– and t——- distribution of fossils
- Consider g— ranges where fossilization didn’t occur
- Consider probabilities of r— extensions
- Analyze volume of r— depositied per time slice and the e——- area of rock per time slice
spatial, temporal, ghost, range, rock, exposed
The fossil record is GOOD to:
- Give us a t—f—- for evolution
- Tells us what organisms e——- from and what wetn e—– / why it did
time-frame, evolved, extinct
Dinosaurs are GOOD to study due to having b—- and t—- but BAD as a lot were t——–
bones, teeth, terrestrial
Dinosaurs first evolved in the T—— and lived through the Jurassic and the C———
Triassic, Cretaceous
What is a Fossil-Lagerstatten?
a sedimentary deposit that exhibits extraordinary fossils with exceptional preservation—sometimes including preserved soft tissues.
What are the two types of fossil-lagerstatten?
1. ———- deposits such as bone beds, mass kills and strand deposits
2. ——- deposits where preservation is of unusual quality
Concentration (where fossils occur in unusual concentrations), Conservation
What can create a bone bed?
A landslide
What can create a mass kill?
A pond drying out or something
What creates a strand line deposit?
The tide
What are the 3 basic types of conservation deposits?
1. Preservation of o—— which aren’t usuually preserved.
2. Preservation of p—- of organisms which aren’t usually preserved (skin)
3. Organisms preserved in unusually a———- or unusual configurations (ichthysaur giving birth)
organisms, parts, articulation