The sedimentary record in Muir Inlet, a macrotidal fjord in Alaska, is
dominated by cyclic silt-mud rhythmites. Couplet thicknesses vary sys
tematically in a vertical sequence and reflect a semidiurnal tidal reg
ime. Semimonthly, monthly, bimonthly, and annual cycles can be identif
ied both visually in cores and by spectral frequency analysis. An aver
age annual sedimentation of 22.5 cm yr(-1) occurs over a four-month me
ltwater season and is confirmed by Pb-210 dating. These modern deepwat
er tidal rhythmites can be used to verify interpretations made on anci
ent rhythmites in the stratigraphic record, and they also provide a da
ting tool to interpret high latitude successions for high-resolution c
limate change.