CH 20. Flashcards
systematics
study of phylogenetic relationships
monophyletic taxa
each taxon includes ancestor and all descendants
paraphyletic taxon
leaves out a common descendant, No crazy uncle
polyphyletic taxon
includes species with different ancestors (blood family reunion + in law)
cladistics
method of determining phylogeny, identifies homologous characters in a group as ancestral or derived
plesiomorphy
homologous charactesr shared with ancestor, (trait that is inherited from a common ancestor and is shared by multiple species within a group)
snyaptomorphy
novel or evolved shared character different from ancestor
autapomorphy
derived and unique, unique to a given taxon. That is, it is found only in one taxon, but not found in any others or outgroup taxa
maximum parsimony
choose best tree with fewest evolutionary events
calde
all the species on a branch, share homologies
true of false, we can infer the sequence of evolutionary events from cladistic trees (but not absolute time)
ture
orthologous genes
inherited from common ancestor, encode very similar proteins with same function in both species (2+ species have same/similar gene with same function), a gene in different species that evolved from a common ancestor by speciation
more DNA differences =
more time elapsed since two groups diverged, less closely related (have had more time to accumulate mutations)
shared sequences are
homologous
molecular clocks estimate
divergence times, assumes constant rate of homologous DNA mutations, calibrated with known fossil ages
LUCA
last universal common ancestor
root of tree is complicated bc of
horizontal gene transfer (mitochondria and chloroplasts), gene transfer between first cells, domain eukarya all have mitochondria, transfer genetic material BETWEEN species
Hadeon Eon
molten rock surface no liquid water
archeon
crust cooled and solidified, formed global ocean from condensed water, volcanoes created first land, low O2 in atmosphere, first life (prokaryotic cells)
plate tectonics
crust breaks into moving plates
oxygen revolution
photosynthesis by prokaryotes made seas and atmosphere O2 rich, more successful bc more energy
proterozoic eon
continents form as islands merge, created areas of shadow seas, ice and glaciers, eukaryotic life began
mesozoic era
cretaceous mass extinction, dinosaurs bye