The isotopic composition of zirconium in silicon carbide grains from t
he Murchison meteorite was measured by resonant ionization mass spectr
ometry of laser-ablated neutral atoms. These grains are condensates fr
om the atmospheres of red giant stars that existed before the formatio
n of our sun and solar system, and they contain records of nucleosynth
esis in these stars. The r-process-dominated isotope zirconium-96 was
depleted by more than a factor of 2 compared with the s-process-domina
ted isotopes zirconium-90, zirconium-91, zirconium-92, and zirconium-9
4, in agreement with expectations for neutron capture nucleosynthesis
in asymptotic giant branch stars.