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Porifera-microbialites of the Lower Liassic (Northern Calcareous ...

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Plate 9<br />

Adnet / Rot-Grau-Schnöll Quarry –<br />

Outcrops <strong>of</strong> <strong>the</strong> <strong>Lower</strong> <strong>Liassic</strong> Schnöll Formation and locations <strong>of</strong> <strong>the</strong> two studied pr<strong>of</strong>iles.<br />

(A): Location <strong>of</strong> <strong>the</strong> pr<strong>of</strong>ile in <strong>the</strong> nor<strong>the</strong>astern part <strong>of</strong> <strong>the</strong> quarry. Outcropping walls, about 5-<br />

6 m in height, were cut by rope saws. The T/J boundary lies below <strong>the</strong> quarry floor.<br />

(B): Quarry wall in <strong>the</strong> southwestern part, about 2.5 m in height. Red and grey limestones <strong>of</strong> <strong>the</strong><br />

Schnöll Formation overlay grey packstones <strong>of</strong> <strong>the</strong> Kendlbach Formation.<br />

(C): Part <strong>of</strong> <strong>the</strong> SW pr<strong>of</strong>ile, showing highly condensed Hettangian limestones. The basal<br />

“sponge layer” <strong>of</strong> reworked material is overlain by a heterogenous sequence <strong>of</strong><br />

echinoderm-foraminifer-biomicrites, intercalated by sponge-rich horizons and several<br />

erosional events. sp = sponge remnants on top <strong>of</strong> an eroded layer, nd = neptunian dike.<br />

(D): Main part <strong>of</strong> <strong>the</strong> NE pr<strong>of</strong>ile showing several sponge-rich layers (Langmoos Mb. and <strong>Lower</strong><br />

Guggen Mb.). Lighter circles and blotches refer to cross sections <strong>of</strong> <strong>the</strong> numerous tube- and<br />

cup-shaped sponges. In <strong>the</strong> center, a layer with low content <strong>of</strong> sponges reveals <strong>the</strong> mottled<br />

feature that reflects closely interwoven parts <strong>of</strong> well and less oxidized sediments. es =<br />

erosional surfaces, ps = pressure solution.

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