GEOLOGICAL TIME Flashcards
o Absolute age dating
(radiometric dating)
Decay products of radioactive elements in minerals to get absolute ages
* Igneous rocks, metamorphic rocks
o Relative age dating
(this is older than that)
Steno’s principles
principle behind half-life
– isotopes are variants of the same parent atom, differing in #of neutrons,
o Formula- measured by ratio of parent to daughter
N(t) = N0(1/2) ^t/t1/2
half-life
the time required for half of the radioactive nuclei in a sample to decay
o Nonconformity
A boundary between non-sedimentary rocks (below) and sedimentary rocks (above)
* Occurs when time passes before deposition og the next layer
* Layer is eroded.
disconformity
A boundary between two sequences of sedimentary rocks where the underlying nest have been eroded (no tilted) prior to the deposition of the younger ones
o Angular unconformity
A boundary between two sequences of sedimentary rocks where the underlying ones have been tilted or folded and eroded prior to the deposition of the younger ones
o Para conformity
A time gap in a sequence of sedimentary rocks that does not show up as an angular unconformity or a disconformity
different types of unconformities
nonconformity
disconformity
angular unconformity
para conformity
o What determines a time boundary (4)
Appearance of new species
Extinction events
Shifts in ciliate
Natural catastrophes
o Hadean eon (4.54-4.0 Ga)
No evidence of life
Differentiation of earths layers
Development of atmosphere and oceans
o Archean eon (4.0-2.5 Ga)
Oldest known fossils
Free oxygen not available
First continents form
o Proterozoic eon (2.5Ga- 451 Ma)
Great oxygenation event
Protocontinents accrete and form supercontinents
Snowball earth ~700Ma
First microscopic and macroscopic multicellular life ~550 Ma
First eukaryotes
Cambrain explosion
o Phanerozoic eon (541 Ma- present)
Marked by the Cambrain explosion and the diversity of life forms
Paleozoic, Mesozoic, and Cenozoic mean old, middle and new life