Radiocarbon and uranium-series ages of the calcareous deposits of the
Plitvice Lakes show that travertines were deposited during three warm,
humid, interglacial oxygen isotope stages. According to our measureme
nts, only calcite crystals or crystal aggregates represent reliable ma
terial for both Th-230/U-234 and U-234/U-238 dating. Compact old trave
rtine in the form of sandstone is less reliable; it can be dated by bo
th methods provided that its detrital contamination is not significant
, demonstrated by very low C-14 activity (< 1.5-2.0 pMC) and a high Th
-230/Th-232 ratio. Old porous travertine contaminated with recent carb
onates and Th-bearing clay (pMC > 5, Th-230/Th-232 < 5) gives erroneou
s results by both methods. Stage 1 (Holocene) deposition is shown prim
arily by C-14 dating corroborated by sedimentological and palynologic
studies as well as by both Th-230/U-234 and U-234/U-238 disequilibrium
methods. The intensive growth of travertine barriers coincided with s
ignificant climate warming in the Holocene. Stage 5 deposition is conf
irmed by the Th-230/U-234 dating of crystalline calcite aggregates emb
edded in the travertine matrix and by concordant Th-230/U-234 and U-23
4/U-238 ages, assuming that the U-234/U-238 activity ratio of 1.88 obs
erved in modern streams and in Holocene deposits can be extended to pa
st epochs. The travertine deposition period was very short, peaking ca
. 120 +/- 10 ka BP. Stage 11 deposition is indicated by U-234/U-238 da
ting only, the period being within the U-234 decay range, but not that
of Th-230. Stage 11 travertine was deposited ca. 420 +/- 50 ka BP. We
did not find travertine samples with U-series ages indicating a growt
h period during relatively warm Stages 7 and 9; due to the scarcity of
old travertine outcrops, these and possibly other stages cannot be ex
cluded on the basis of presented data. All of these isotopic dating re
sults concur with the field relation of the travertine complex of the
Plitvice Lakes.