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chapter 26

AB
half-lifethe number of years it takes for 50% of an isotope to decay
magnetic reversalsreversal of the polarity of Earth's magnetic field
genetic annealingproduction of a new genome through the transfer of part of the genome of one organism to another.
stromatolitesrocks made of branded domes of sediment where most forms of ancient prokaryotic life are found
snowball Earth hypothesishypothesis that glaciers covered the planet 750-570 million years ago, confining life to limited places
serial endosymbiosismodel of the origin of eukaryotes consisting of a sequence of endosymbiotic events in which cellular structures were derived form small prokaryotes that had been engulfed by larger cells
Pangeasupercontinent formed at the end of the Paleozoic era when plate movements brought all the land masses together
protobiontsaggregate of biologically produced molecules surrounded by a membrane or membrane-like structure
geologic recorddivision of Earth's history into time periods
three domain systemsystem of taxonomic classification based on three superkingdoms: Bacteria, Archaea, and Eukarya
radiometric datingmethod used to determine ages of rocks and fossils on a scale of absolute time, based on the half-life of radioactive isotopes
ribozymean enzyme-like RNA molecule that catalyzes reactions during RNA splicing



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