Anthropology Chapter 8 – Flashcards

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The study of extinct organisms, based on their fossilized remains
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Paleontology
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Preserved remnants of once living things, often buried in the ground
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Fossils
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The study of the deposition of plant or animal remains and the environmental conditions affecting their preservation
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Taphonomy
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The study of the Earth strata- layers of rock, representing various periods of deposition
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Geology
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The study of the order of rock layers and the sequence of events they reflect
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Stratigraphy
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Categories of time into which Earth's history is divided by geologists and paleontologists
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The geologic time scale
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GTS consists of
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Eons, eras, periods, epochs
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Earth is approximately _ billion years old.
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4.6
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Primates and human evolution occur in the _____ (the last _ million years
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Cenozoic Era, 65
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Geologic time scale is divided into two eons
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Precambrian and Phanerozoic
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_____ dates 4.6 billion- 543mya (divided into three eras) and it comprises almost 90% of Earth's history
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Precambrian Eon
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_____ dates 543mya- present
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Phanerozoic Eon
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Phanerozoic Eon is divided into three eras
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Paleozoic- Cambrian explosion Mesozoic- age of dinosaurs Cenozoic- age of mammals
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Paleontologists order the _____, as geologists order Earth history- in a series of three eras Paleozoic Mesozoic Cenozoic
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Evolution of major life forms
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The first step in determining the antiquity of fossil remains is learning its
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Provenience
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The origin or original source of a fossil (the precise location from which a fossil comes)
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Provenience
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Establishing the age of a fossil in comparison to other materials found above and below it
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Relative dating techniques
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Relative dating techniques use principles of
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Stratigraphy
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Chemical techniques within sites, such as similar chemical signatures, fluorine and other elements from the soil
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Relative dating techniques
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Absolute dating techniques Estimate the age of an object in absolute terms through the use of a natural clock such as radioactive decay or tree ring growth
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Chronometric dating techniques
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Dating method that uses tree ring count to determine numerical age
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Dendrochronology
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Absolute dating techniques Chronometric techniques that use radioactive decay of isotopes to estimate age
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Radio metric dating
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Two or more forms of a chemical element that have the same number of protons but vary in the number of neutrons
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Isotopes
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The time it takes for half of the radioisotopes in a substance to decay
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Half-life
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Absolute dating techniques Radiometric dating method in which the ratio of 14C to 12C is measured to provide an absolute date for material younger than 50,000 years
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Radiocarbon dating
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Absolute dating techniques Measures the number of tracks left behind by isotope decay (fragments produced from isotope decay leave tracks on rock crystal)
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Fission track dating
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_____ dating can date materials several million years old and is used to date volcanic ash and obsidian (volcanic glass)
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Fission track dating
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Paleomagnetic dating and amino acid dating are
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Non-radiometric absolute dating method
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Based on changes in Earth's magnetic field, which changes the planet's polarity
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Paleomagnetic dating
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Base on the decay of protein molecules following an organism's death
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Amino acid dating
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Electron spin resonance dating and thermo luminescence dating are
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Non-radiometric absolute dating methods
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Uses microwave spectroscopy to measure electrons' spins in various materials
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Electron spin resonance dating
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The energy trapped in a material is measured when the object is heated (base on the amount of the sun's energy trapped in the material)
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Thermoluminescence dating
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DNA from living organisms can be compared to estimate the amount of time since two species diverged from a common ancestor- closely related species accumulate genetic differences over time at a regular rate
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Genetic dating: the molecular clock
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A thin layer of clay that seperates rock layers from the end of the Cretaceous period to those from the beginning of the Teritary period
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K-T boundary
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