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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).

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