Evolution Flashcards
Aristotle
Organisms are fixed and unchanging
Scala naturae: ladder of nature (simple organisms on bottom and complex organisms on top)
Georges Cuvier
Late 1700s to early 1800s
Catastrophism: catastrophe killed off organisms and new ones appeared
James Hutton
Mid to late 1700s
Gradualism: gradual processes can lead to big changes given enough time
Charles Lyell
Early to mid 1800s
Uniformitarianism: geological processes that operate now are the same as those that operated in the past and operate at the same rate now as they did then
Carolus Linnaeus
Father of modern taxonomy
Grouped similar organisms into categories
Jean-Baptiste de Lamarck
Late 1700s to early 1800s
Proposed that gradual change could explain fossil record
Organisms evolve through use/disuse and inheritance of acquired characteristics
Darwin’s Voyage to South America
Temperate SA species resembled SA tropical species more than they resembled temperate European species
Earthquake geology: after an earthquake, the land raised up
Studied animals: iguanas, tortoises, finches, etc.
Natural Selection
Heritable variation exists in populations
Organisms produce more offspring than can possibly survive
Those with favorable traits will leave more offspring
Differential survival and reproduction will result in accumulation of favorable traits within the population
Alfred Russel Wallace
Visited Rio Negro in Brazil
Studied birds of paradise and orangutans
Came to same conclusions as Darwin
Sent a manuscript to Darwin, which prompted him to publish his findings
On the Origin of Species
Darwin’s published work
Species presently inhabiting the earth are descendants of ancestral species that were different
Mechanism of species change: natural selection
Modern definition of evolution
Change in a population’s gene frequency over time
Rise of Life
Earth is roughly 4.6 billion years old
About 3.9 billion years ago, earth stopped being bombarded by space debris
Oparin-Haldane Hypothesis (1920)
Atmosphere+H20+lightning or UV= organic molecules
Modern hypothesis: volcanoes or deep sea vents were sites of organic synthesis
Meteorites contain amino acids
Synthesizing Polymers
Dripping amino acids onto hot rocks makes polymers
First cell theory
RNA monomers can form spontaneously
Protocells (abiotically produced) took up RNA and divided
Absolute Aging
Use radioactive isotopes to determine age of fossils (within a range)
Precambrian Era
1st era
Mostly prokaryotes
Phanerozoic Era
Paleozoic: marine and terrestrial (reptiles) animals, vascular plants
Mesozoic: dinosaurs, cone-bearing and flowering plants
Cenozoic: mammals, birds, insects
Permian Extinction
End of Paleozoic era
Causes: volcanic eruption in Siberia and formation of Pangaea
Cretaceous/Tertiary Extinction
End of Mesozoic era
Causes: meteorite strike in Yucatan, volcanism
Stromatolites
Oldest fossils
Groups of prokaryotes
Rise of Eukaryotes
Endosymbiosis: one prokaryote engulfed another
Rise of Multicellularity
Groups of prokaryotes (stromatolites) came together
Cambrian Era
Most major phyla appeared
Large, shelled or animals with exoskeletons
Tree of Life
3 domains evolved from universal common ancestor: archaea (prokaryotes, usually anaerobic), bacteria, eukarya
Homology
Similarity resulting from common ancestry
Vestigial Structures
Organs/structures with little or no current use; relics of common ancestor
Biogeography
Geographic distribution of organisms
Convergent Evolution
Independent evolution of similar features in different lineages
Fossil Record Patterns
Prokaryotes came first, then eukaryotes, then fish, then amphibians…