Introduction and history Flashcards
William Smith
Made the 1st true geological map
Noticed layers of sedimentary rocks in any given location have the same fossil sequence
Fossil
Any nonliving biologically generated trace or material that paleontologists study as part of the record of life
Robert Hooke
Microscopic examination of fossil and modern wood and shells showed that they were the same
Nicolaus Steno
Decided “tongue stones” were really fossilized shark teeth
Argued that if fossils grew in place we should find half fossils
Said that a solid object will cause solids around it to form to its shape so fossils must have been there before rocks
1720 Beringer Hoax
Competitors gave him fake fossils, which he published a book about.
In the 16th century how did people believe fossils were made
From the solidification of a fluid
What does a paleontologist do?
Collects fossils from the field
Compare with previously described fossils and living organisms
Describe them if not previously known
Document their occurrence in a particular time/place/environment
Neo-Platonist
One of the schools of thinking about fossils. Thought fossils grew under celestial influence and emphasized the unity of nature.
Aristotelian
Believed fossils formed from “seeds” that washed into the ground.
Soft parts are made of which elements
CHNOPS
Redford ratio of N:P
16:1
Diagenesis
Processes that take place after burial
Taphonomy
Study of the process of fossilization
Represents the passage of biological info from the biosphere to the lithosphere
George’s Cuvier
An anatomist.
Noticed the oldest fossils were below younger ones
Established that fossils record a history of life.
Established the reality of extinction.
Lagerstatten
Unusual preservation. A fossil mother lode.
Time Averaging
How much time does a fossil collection represent.
Organisms found together may not have lived together.
Sedimentary processes may mix together fossils of different ages
Taphofacies
Bodied of sedimentary rock characterized by particular combinations of preserved features of the contained fossils.
Help us to reconstructing environments.
Stagnation deposits
A type of conservation lagerstatten caused by low oxygen which stops scavenging.
Obrution deposits
Lagerstatten conservation deposits. Caused by rapid burial maybe a worm or a huge sediment deposit.
Paleobiology
Looks at fossils as the remains of living organisms. A documentation of life of the past.
How organisms preserve Ina marine environment depends on…
Water energy (waves/currents), rates of sedimentation, oxygen.
The “external metaphors” of paleontology
Does the history of life have an arrow, what is the motor of organic change, is the history of life gradual or episodic, what is the tempo.
How do internal and external molds form?
Spaces are filled by sediment and then the minerals are dissolved leaving impressions on the sediment.
How do concretes form?
Precipitation of minerals around decaying organisms (soft tissue impressions are preserved)
Permineralization
Filling void spaces with minerals (petrified)
Biostratinomy
Begins with the death of an organism and ends with it’s burial. (Scavenging, bacterial decomposition, etc.)
Necrology
The study of death processes. How dead organisms or dead pieces of organisms are produced.