Fossil Record Flashcards
(20 cards)
Uniformitarianism
Principle that states that geologic processes that occured in the past can be explained by current geologic processes
Catastrophism
Principle that states that geologic change occurs suddenly
Paleontology
Scientific study of Fossils
Relative dating
Any method of determining whether an event or object is older or older than other events or objects
Superposition
Principle that states that younger rocks lie above older rocks if thelayers have not been disturbed
Absolute dating
Any method of measuring the age of an event or object in years
Isotope
Atom that has same amount of protons as other atoms of the same element
Radioactive Decay
The process in which a radioactive isotope tends to break down
Radiometric dating
a method of dating geological or archeological specimens by determining the relative proportions of particular radioactive isotopes present in a sample
Half-Life
he time taken for the radioactivity of a specified isotope to fall to half its original value.
Fossil
Remains of an organism
Trace Fossil
Fossilized mark that is formed in soft sediment
Mold
A fossil formed when an animal, plant, or other organism dies and is covered by sediment, its flesh decays and bones deteriorate due to chemical reactions, and a cavity remains below the ground surface.
Unconformity
a surface of contact between two groups of unconformable strata
Mass Extinction
a widespread and rapid decrease in the biodiversity on Earth. Such an event is identified by a sharp change in the diversity and abundance of multicellular organisms.
Jurassic period
The Jurassic was a geologic period and system that spanned 56 million years from the end of the Triassic Period 201.3 million years ago to the beginning of the Cretaceous Period 145 Mya. The Jurassic constitutes the middle period of the Mesozoic Era, also known as the Age of Reptiles.
Cretaceous Period
was the last and longest segment of the Mesozoic Era. It lasted approximately 79 million years, from the minor extinction event that closed the Jurassic Period about 145.5 million years ago to the Cretaceous-Paleogene (K-Pg) extinction event dated at 65.5 million years ago.
Devonian Period
a geologic period and system of the Paleozoic, spanning 60 million years from the end of the Silurian, 419.2 million years ago (Mya), 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 divided into two epochs: the Pleistocene (2.588 million years ago to 11.7 thousand years ago) and the Holocene (11.7 thousand years ago to today). The informal term “Late Quaternary” refers to the past 0.5–1.0 million years.
Permian Period
The Permian is a geologic period and 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 251.902 Mya. It is the last period of the Paleozoic era; the following Triassic period belongs to the Mesozoic era