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12.1 The Fossil Record KEY CONCEPT Specific environmental conditions are necessary in order for fossils to form. 12.1 The Fossil Record Fossils can form in several ways. • Permineralization occurs when minerals carried by water are deposited around a hard structure. 12.1 The Fossil Record • A natural cast forms when flowing water removes all of the original tissue, leaving an impression. 12.1 The Fossil Record • Trace fossils record the activity of an organism. 12.1 The Fossil Record • Amber-preserved fossils are organisms that become trapped in tree resin that hardens after the tree is buried. 12.1 The Fossil Record • Preserved remains form when an entire organism becomes encased in material such as ice. 12.1 The Fossil Record • Specific conditions are needed for fossilization. • Only a tiny percentage of living things became fossils. 12.1 The Fossil Record Radiometric dating provides an accurate way to estimate the age of fossils. • Relative dating estimates the time during which an organism lived. – It compares the placement of fossils in layers of rock. – Scientists infer the order in which species existed. 12.1 The Fossil Record • Radiometric dating uses decay of unstable isotopes. – Isotopes are atoms of an element that differ in their number of neutrons. neutrons protrons 12.1 The Fossil Record • Radiometric dating uses decay of unstable isotopes. – Isotopes are atoms of an element that differ in their number of neutrons. – A half-life is the amount of time it takes for half of the isotope to decay. 12.3 of Life Record 12.1- Origin The Fossil KEY CONCEPT The origin of life on Earth remains a puzzle. 12.3 of Life Record 12.1- Origin The Fossil 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. • The cloud and dust condensed forming our solar system. (4.6 bya) 12.3 of Life Record 12.1- Origin The Fossil Several sets of hypotheses propose how life began on Earth. • There are two organic molecule hypotheses. – Miller-Urey experiment (in put of energy from lightening) electrodes “atmosphere” water “ocean” heat source amino acids – meteorite hypothesis (brought organic compounds) 12.3 of Life Record 12.1- Origin The Fossil • There are different hypotheses of early cell structure. – iron-sulfide bubbles hypothesis 12.3 of Life Record 12.1- Origin The Fossil • There are different hypotheses of early cell structure. – lipid membrane hypothesis, lipids spontaneously made a cell membrane 12.3 of Life Record 12.1- Origin The Fossil • 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. 12.4 Organisms 12.1- Early The Single-Celled Fossil Record KEY CONCEPT Single-celled organisms existed 3.8 billion years ago. 12.4 Organisms 12.1- Early The Single-Celled Fossil Record Microbes have changed the physical and chemical composition of Earth. • The oldest known fossils are a group of marine cyanobacteria. – prokaryotic cells – added oxygen to atmosphere – deposited minerals 12.4 Organisms 12.1- Early The Single-Celled Fossil Record • Fossil stromatolites provide evidence of early colonies of life. (contain cyanobacteria) 12.4 Organisms 12.1- Early The Single-Celled Fossil Record 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. 12.6 Evolution 12.1- Primate The Fossil Record KEY CONCEPT Humans appeared late in Earth’s history. 12.6 Evolution 12.1- Primate The Fossil Record Humans share a common ancestor with other primates. • Primates are mammals with flexible hands and feet, forward-looking eyes and enlarged brains. 12.6 Evolution 12.1- Primate The Fossil Record • Primates evolved into prosimians and anthropoids. – Prosimians are the oldest living primates. – They are mostly small and nocturnal. 12.6 Evolution 12.1- Primate The Fossil Record – 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. 12.6 Evolution 12.1- Primate The Fossil Record Hominids Characteristics: • Bipedal means walking on two legs. – foraging – carrying infants and food – using tools • Walking upright has important adaptive advantages. 12.6 Evolution 12.1- Primate The Fossil Record 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. 12.6 Evolution 12.1- Primate The Fossil Record 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. Australopithecus afarensis Homo habilis Homo neanderthalensis Homo sapiens