We have measured excess Ir and depletion of C-14, two independent indicator
s of cosmic material, in peat cores from the central Tunguska impact site.
Both Ir and 14C show pronounced anomalies in the same stratigraphical depth
interval. We have estimated an integral deposition of nonradioactive cosmo
genic C of 6.8 +/- 1.0 mg C cm(-2), and an integrated Ir deposition of 5.9
+/- 1.2 pg Ir cm(-2). The very high C/Ir ratio and a deduced delta(13)C val
ue of +55 +/- 10 parts per thousand relative to V Pee Dee Belemnite (VPDB)
of the impactor material found in this study points towards a cometary type
impactor, rather than a chondritic or achondritic asteroidal type impactor
.