“…Middle Triassic sphinctozoan-and inozoan-dominated reefs or reefal carbonates are known from numerous localities in the western Tethys (Alps: ott, 1967;Dullo & Lein, 1980;BraDner & reSch, 1981;foiS & gaetani, 1981henrich, 1982;SenowBari-Daryan & others, 1993;rüffer & Zamparelli, 1997;emmerich & others, 2005 ZanKl, 1969;SenowBariDaryan, 1978SenowBariDaryan, , 1980aSenowBariDaryan, , 1990SenowBariDaryan & Schäfer, 1979;Schäfer, 1979;Dullo & lein, 1980; for more informa-tion, see flügel, 1981flügel & SenowBari-Daryan, 2001); from northern Italy (münSter, 1841; ruSSo, 1981;BiZZarini & ruSSo, 1986); from southern Italy (maStanDrea & rettori, 1989;SenowBariDaryan & Zamparelli, 1999; from the Carpathians (JaBlonSKy, 1971(JaBlonSKy, , 1972(JaBlonSKy, , 1975Balogh & KovácS, 1976;KovácS, 1978aKovácS, , 1978bflügel & others, 1992; from the former Yugoslavia (SenowBari-Daryan, 1981ramoS & turnSeK, 1984;turnSeK, BuSer, & ogorelec, 1987); and from Greece SenowBariDaryan, 1982;SenowBari-Daryan & Schäfer, 1983;SenowBari-Daryan, matarangaS, & vartiS-matarangaS, 1996).…”