Otoliths of Arctic charr, Salvelinus alpinus, from north Labrador were
examined to gather life history information pertinent to anadromous m
igrations. Wavelength dispersive electron microprobe measurements conf
irm the presence of strontium in otolith tissue. Trace element analyse
s of charr otoliths imply that otolith strontium/calcium concentration
ratios are related to external environmental factors with salinity ha
ving a great influence. Otoliths clearly record habitat shifts consist
ent with migration across major salinity boundaries. Most charr first
migrate to sea following at least 2 years in freshwater. Generally, wh
en anadromy begins, it continues annually. Robust relationships in oto
lith chemistry, combined with macrostructure patterns in field-capture
d specimens, provide time-series data describing individual migrationa
l histories. Validation studies are still required in order to couple
information contained within daily increments with chemical analyses t
o infer additional temporal events in diadromous migrations.