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Origin of Life. Chapter 12. KEY CONCEPT The origin of life on Earth remains a puzzle. . Earth was very different billions of years ago. . There have been many hypotheses of Earth’s origins. The most widely accepted hypothesis of Earth’s origins is the nebula hypothesis. electrodes.
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Origin of Life Chapter 12
Earth was very different billions of years ago. • There have been many hypotheses of Earth’s origins. • The most widely accepted hypothesis of Earth’s origins is the nebula hypothesis.
electrodes “atmosphere” water “ocean” heat source amino acids Several sets of hypotheses propose how life began on Earth. • There are two organic molecule hypotheses. • Miller-Urey experiment • meteorite hypothesis
iron-sulfide bubbles hypothesis • There are different hypotheses of early cell structure.
lipid membrane hypothesis • There are different hypotheses of early cell structure.
A hypothesis proposes that RNA was the first genetic material. • Ribozymes are RNA molecules that catalyze their own replication. • DNA needs enzymes to replicate itself.
Microbes have changed the physical and chemical composition of Earth. • The oldest known fossils are a group of marine cyanobacteria. • prokaryotic cells • added oxygen toatmosphere • deposited minerals
Fossil stromatolites provide evidence of early colonies of life.
Eukaryotic cells may have evolved through endosymbiosis. • Endosymbiosis is a relationship in which one organism lives within the body of another. • Mitochondria and chloroplasts may have developed through endosymbiosis.
The evolution of sexual reproduction led to increased diversity. • Genetic variation is an advantage of sexual reproduction. • Sexual reproduction may have led to the evolution of multicellular life.
Life moved onto land during the Paleozoic Era. • Multicellular organisms first appeared during the Paleozoic era. • The era began 544 million years ago and ended 248 million years ago. • The Cambrian explosion led to a huge diversity of animal species.
Reptiles radiated during the Mesozoic era. • The Mesozoic era is known as the Age of Reptiles. • It began 248 million years ago and ended 65 million years ago. • Dinosaurs, birds, flowering plants, and first mammals appeared.
Mammals radiated during the Cenozoic era. • The Cenozoic era began 65 million years ago and continues today. • Placental mammals and monotremes evolved and diversified. • Anatomically modern humans appeared late in the era.
Humans share a common ancestor with other primates. • Primates are mammals with flexible hands and feet, forward-looking eyes and enlarged brains.
Prosimians are the oldest living primates. • They are mostly small and nocturnal. • Primates evolved into prosimians and anthropoids.
Anthropoids are humanlike primates. • They are subdivided into the New World monkeys, Old World monkeys, and hominoids. • Homonoids are divided into hominids, great apes, and lesser apes. • Hominids include living and extinct humans.
foraging • carrying infants and food • using tools • Walking upright hasimportant adaptiveadvantages. • Bipedal means walking on two legs.
There are many fossils of extinct hominids. • Most hominids are either the genus Australopithecus or Homo. • Australopithecines were a successful genus. • The Homo genus first evolved 2.4 million years ago.
Australopithecus afarensis Homo habilis Homo neanderthalensis Homo sapiens Modern humans arose about 200,000 years ago. • Homo sapiens fossils date to 200,000 years ago. • Human evolution is influenced by a tool-based culture. • There is a trend toward increased brain size in hominids.