Anth Notes 5

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Foothill College *

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1H

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Anthropology

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Oct 30, 2023

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pdf

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2

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I. Introduction Dating in anthropology refers to the methods and techniques used to determine the age of artifacts, fossils, and archaeological sites. Accurate dating is essential for understanding the chronology of human evolution, culture, and history. II. Relative Dating Methods A. Stratigraphy Stratigraphy is based on the principle that older layers of sediment or rock are found at the bottom, and younger layers are found at the top. Archaeologists analyze the order and depth of layers to establish a relative chronology. B. Seriation Seriation is a technique that arranges artifacts based on their stylistic and temporal changes. It is often used for dating objects with no absolute dates. C. Typology Typology involves classifying artifacts into types based on shared characteristics. Changes in artifact types over time can help establish relative dates. III. Absolute Dating Methods A. Radiocarbon Dating (C-14) Radiocarbon dating is a widely used method for dating organic materials up to around 50,000 years ago. It relies on the decay of the radioactive isotope C-14 in once-living organisms. B. Luminescence Dating Luminescence dating, including thermoluminescence and optically stimulated luminescence, is used to date minerals in archaeological sediments. It determines the last exposure to light or heat. C. Potassium-Argon (K-Ar) Dating K-Ar dating is used for dating volcanic rock and minerals. It relies on the decay of radioactive potassium isotopes into argon gas. D. Tree-Ring Dating (Dendrochronology) Tree-ring dating measures the width of annual growth rings in trees. It provides precise dates for wooden artifacts and can extend back thousands of years. IV. Genetic Dating
Genetic dating, including mitochondrial DNA and Y-chromosomal DNA analysis, is used to trace human evolution and migration patterns. It provides insights into the timing of key events in human prehistory. V. Challenges in Dating Challenges in dating include contamination of samples, calibration of radiocarbon dates, and understanding local environmental factors. Different dating methods may provide slightly different results, and it's crucial to use multiple techniques for cross-validation.
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