The clam Calyptogena magnifica lives at abyssal depths in association
with hydrothermal venting on midocean ridges. Analysis of strontium/ca
lcium ratios in C. magnifica shells provides a temperature proxy with
submonthly time resolution. A 21-year strontium/calcium record of two
clams from 9 degrees 50'N on the East Pacific Rise captures the known
1991 and 1992 eruptive events, documents several additional events bet
ween 1992 and 1996, and demonstrates the absence of major hydrothermal
episodes during the period 1974 to 1991. These clam archives can incr
ease our understanding of the thermal and chemical history of midocean
ridge hydrothermal and volcanic activity on decadal time scales.