Fossil Record Flashcards
uniformitarianism
a principle that states the geologic process that occurred in the past can be explained by current geologic process
catastrophism
a principle that states that geologic change occurs suddenly
paleontology
the scientific study of fossils
relative dating
any method of determining whether an event or object is older or younger than the events or objects
absolute dating
any method of measuring the age of an event or object in years
superposition
a principle that states that younger rocks lie above older rocks if the layers have not been disturbed
isotope
an atom the has the same number of protons (or the same atomic number) as other atoms of the same element do but that has a different number of neutrons ( and thus a different atomic number)
radioactive decay
the process in which a radioactive isotope tends to break down into a stable isotope of the same element or a different element
half-life
the time needed for half of a sample of radioactive substance to undergo radioactive decay
fossil
the remains or physical evidence of an organism preserved by geological process
trace fossil
a fossilized mark that is formed in soft sediment by the movement of an animal
mold
a mark or cavity made in a sedimentary surface by a shell or other body
cast
a type of fossil that forms when sediments fill in the cavity left by a decomposed organism
unconformity
a break in the geologic record created when rock layers are eroded or when sediment is no deposited for a long period of time
mass extinction
when a big group of organisms go extinct at the same time
Jurassic period (for 16-20 list when the time period was and what was the dominant animal group on Earth)
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The Jurassic period (199.6 million to 145.5 million years ago) was characterized by a warm, wet climate that gave rise to lush vegetation and abundant life. Many new dinosaurs emerged—in great numbers. Among them were stegosaurs, brachiosaurs, allosaurs, and many others
Cretaceous period
The Cretaceous is defined as the period between 145.5 and 65.5 million years ago,* the last period of the Mesozoic Era, following the Jurassic and ending with the extinction of the dinosaurs (except birds).
Devonian period
The Devonian is a geologic period and system of the Paleozoic, spanning 60.3 million years from the end of the Silurian, 419.2 million years ago, to the beginning of the Carboniferous, 358.9 Mya. It is named after Devon, England, where rocks from this period were first studied
Quaternary period
The Quaternary Period is the third and last of the three periods of the Cenozoic Era. You and I are living in this period, which began only 2.58 million years ago. This is less than 0.1% of all of geologic time! A thin layer of sediments deposited during the Quaternary covers much of the Earth’s land surface.
Permian period
The Permian is a geologic period and stratigraphic system which spans 47 million years from the end of the Carboniferous Period 298.9 million years ago, to the beginning of the Triassic Period 251.9 Mya. It is the last period of the Paleozoic Era; the following Triassic Period belongs to the Mesozoic Era.