Field investigations and bed-by-bed sampling of ammonoids provide the
basis for a more detailed and better constrained biostratigraphic sche
me of Triassic deposits in the northern Caucasus. For the first time,
these deposits are subdivided into ten ammonoid beds comprising the Tr
iassic interval from the middle Scythian to the upper Rhaetian. The be
ds are correlated with the standard ammonoid zones. The Anisian deposi
ts, which are especially rich in ammonoids, are correlated with synchr
onous sedimentary sections in Turkey, Iran, China, and the USA. New da
ta elucidate that in the studied, region there is a considerable strat
igraphic hiatus spanning the upper Anisian and the lower Ladinian.