G. Muttoni et al., MAGNETOSTRATIGRAPHY AND BIOSTRATIGRAPHY OF AN ANISIAN-LADINIAN (MIDDLE TRIASSIC) BOUNDARY SECTION FROM HYDRA (GREECE), Palaeogeography, palaeoclimatology, palaeoecology, 111(3-4), 1994, pp. 249-262
On the island of Hydra, the Anisian/Ladinian boundary is exposed in a
24 m thick section of nodular reddish Han-Bulog Limestone. This paper
is focused on the magnetostratigraphy and conodont biostratigraphy of
this section. The Anisian/Ladinian boundary is defined by the First Ap
pearance Datum (FAD) of the conodont species Gondolella trammeri Kozur
(base of the Nevadites ammonoid zone), and occurs in a normal polarit
y zone. Microfacies analysis has distinguished a lower and upper litho
facies recording gradual shallowing from pelagic conditions to a platf
orm margin paleoenvironment.