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daklfhadsn ashlkfa shifdaskjghaksj dfhsk
gradulis m pro dop tjat ebeolution occurs slowl y and that tiny changes in a specices fradully add o to maujot chanehs obe rperopkd sthat time does not account for the large haps in teh fossil record we woils ecpec to see intermediae forms. perhaos th efossil record is just incomplete p8jvyurf wuitb dptiprd thst dprvird rbbrolr wuivku futijh s trlsyibrly dhoty smmoijy pg ttikr smf dspstsyrf bu lomg peruofs od little to bo vhange
gradyslidm poroped thst rvolujr offiye elo3olu wnr yjey tiny chsngrd in a species grafisllu add uo tp ,ajohhs rinfysuf eieolfj d[tp[rd yjsy f[tvpfp rbfp/n eop[;dk gofk gfjpig
does not account for yhe latve ha;s in the fossil record we wpild
puncuated equlibria proposes thhat spexies evolve quickly during a reletivily shprt amoij g od time ans seperated by lign periionds of little tto no vhange