UTRECHT MICROPALEONTOLOGICAL BUllETINS
UTRECHT MICROPALEONTOLOGICAL BUllETINS
UTRECHT MICROPALEONTOLOGICAL BUllETINS
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sediment, corresponding in colour to that of the underlying bed. The basal<br />
marly limestone (sample 80) passes upwards into brownish and indurated<br />
limestone (sample 81). The total thickness of this unit amounts to 50 cm.<br />
The lower boundary of the second finely laminated unit is marked by<br />
a rapid change in colour to rose-brown. The sediment seems to be clayey;<br />
burrowing is present but rare. Some less distinctly laminated interbeds have<br />
a thickness of up to 4 cm. Samples 82 and 83 were collected in this 60 cm<br />
part of the succession. At the top of the previous unit the sediment changes<br />
into a light brown, less distinctly bedded limestone, which contains burrows<br />
filled with white limestone of pelletoidal texture. This sediment passes in<br />
turn into homogeneous limestone which is overlain by a laminated bed with<br />
a thickness of 6 cm and a compact, indurated limestone of 15 cm (sample<br />
84). The unit ends with a marly, partly laminated limestone of 20 cm thickness<br />
(sample 85).<br />
The undulating lower contact of the third laminated unit of rose-coloured<br />
sediment (thickness 45 cm) is rather sharp and well traceable in the horizontal<br />
sense. The sediment is of remarkably low weight and shows delicate<br />
lamination with small scale undulations, draping over larger specimens of<br />
Fig. 10 Horizontal burrows on a bedding plane in a laminated interval of the Trubi at Capo Rossello<br />
(exposure 3).