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

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Plate 5<br />

Scheibelberg –<br />

Type location <strong>of</strong> <strong>the</strong> Scheibelberg Formation, situated north <strong>of</strong> Steinplatte / Kammerköhr Alm.<br />

(A): Outcrop <strong>of</strong> Hornsteinknollenkalk and Kendlbach limestones along <strong>the</strong> tourist trail from<br />

Schwarzl<strong>of</strong>er Alm passing <strong>the</strong> western slope <strong>of</strong> Scheibelberg mountain.<br />

(B): Large boulder <strong>of</strong> corroded Hornsteinknollenkalk penetrated by several siliceous bulbs.<br />

Rettenbachalm / Jaglingbach –<br />

<strong>Liassic</strong> sedimentation from <strong>the</strong> sou<strong>the</strong>rn part <strong>of</strong> <strong>the</strong> Triassic carbonate platform (East <strong>of</strong> Bad<br />

Ischl, Höllengebirgs nappe).<br />

(C): View over <strong>the</strong> river bed <strong>of</strong> Jaglingbach that is formed by folded Adnet limestone. At <strong>the</strong><br />

upper right corner: Grey siliceous limestones <strong>of</strong> <strong>the</strong> Allgäu Formation.<br />

(D): Anticline <strong>of</strong> knobby Adnet limestones with ferromanganese crusts at <strong>the</strong> Jaglingbach river<br />

bed.<br />

(E): Breccia <strong>of</strong> Adnet limestone clasts with high amounts <strong>of</strong> isolated spicules (grey color).<br />

Contact seams between clasts are characterized by pressure solution and microstylolites.<br />

Scanned thin section.<br />

(F): Close-up <strong>of</strong> one <strong>of</strong> <strong>the</strong> clasts in (E), exhibiting spicules <strong>of</strong> collapsed sponge skeletons.<br />

(G): Adnet breccia. Cluster <strong>of</strong> spicules embedded in microbialite (lighter red). The mixture <strong>of</strong><br />

isolated monaxons, hexactins (white arrows) from Lyssacinosid species and dichotriaen<br />

spicules <strong>of</strong> demosponges (black arrow) illustrate <strong>the</strong> problem to characterize allochthonous<br />

and autochthonous components <strong>of</strong> <strong>the</strong> sediment.

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