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Vocabulary flashcards covering major geological eras, time scales, and fossilization concepts discussed in the lecture.
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Pre-Cambrian
Era before the Cambrian (~4.58–542 million years ago); Earth forms and early life develops.
Cambrian
Period starting ~542 million years ago; rapid diversification of life (Cambrian explosion).
Paleozoic
Era from ~542 to 251 million years ago; includes Cambrian to Permian; ends with a major mass extinction.
Permian
Period (~299–251 mya) marked by a large mass extinction at its end; diversification of reptiles.
Mesozoic
Era from ~251 to 65 million years ago; age of dinosaurs; includes Triassic, Jurassic, Cretaceous.
Triassic
Period ~251–201 mya; recovery after Permian; first dinosaurs and mammals appear.
Jurassic
Period ~201–145 mya; peak dinosaur diversity; early birds appear.
Cretaceous
Period ~145–65 mya; dinosaurs dominate; ends with KT boundary extinction.
KT boundary (Cretaceous-Paleogene boundary)
Marker at ~66 mya; mass extinction (dinosaurs) linked to asteroid impact and volcanic activity.
Paleogene
Subdivision of the Cenozoic (65–23 mya); includes Paleocene and Eocene; mammals diversify.
Neogene
Subdivision of the Cenozoic (23–2.6 mya); includes Miocene and Pliocene; primate evolution continues; origin of humans.
Paleocene
Early Paleogene (~65–56 mya); mammals diversify after dinosaur extinction.
Eocene
Mid Paleogene (~56–34 mya); primate radiation; resembles modern primates.
Oligocene
Late Paleogene (~34–23 mya); further primate evolution; origin of many anthropoids.
Miocene
Period (~23–5.3 mya); important for ape evolution and early hominins.
Pliocene
Period (~5.3–2.6 mya); Australopiths appear; early Homo evolves.
Australopiths
Early hominins in Africa; bipedal; ancestors of Homo.
Homo sapiens
Modern humans; appears in Africa about 300,000 years ago.
Agriculture
Domestication of plants and animals; leads to sedentism and the rise of cities.
Sedentism
Living in one place due to agriculture; sustained human settlement.
Sedimentary rocks
Rocks formed by deposition of particles; often contain fossils in strata.
Igneous rocks
Rocks formed by cooling of molten magma or lava; not suitable for fossils.
Metamorphic rocks
Rocks altered by heat/pressure; fossils usually not preserved.
Fossilization
Process of mineral replacement of organic material, turning remains into rock.
Fossil
Preserved remains or traces of ancient organisms.
Holocene
Current geological epoch (~11.7k years ago–present); rise of agriculture and civilizations.