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4 results for “Valospongia”
Fig. 6 in First post-Cambrian records of the reticulosan sponges Valospongia and Hintzespongia from the late Tremadocian of North Wales
Fig. 6. The hexactine-bearing sponge Hintzespongia? sp., NIGP154638, Dol-cyn-Afon Formation, upper Tremadocian, Lower Ordovician, Ceunant-ygarreg-ddu stream section, Arenig Fawr, North Wales, UK. A. Overall view of specimen showing several regions with exposed spicules, each revealing skeletal layers interpreted as having originally been dominantly diagonal (d), sub-orthogonal (o) or both (d, o), and with example of possible inner layer parietal gap (pg). B. Detail of central part of specimen, showing both diagonal and sub-orthogonal spicule arrays. C. Camera lucida drawing of region shown in B, with sub-orthogonal series stippled. Scale bars 5 mm. All photographs taken under water.
Fig. 3 in First post-Cambrian records of the reticulosan sponges Valospongia and Hintzespongia from the late Tremadocian of North Wales
Fig. 3. Examples of undescribed sponges from the Dol-cyn-Afon Formation (early Migneintian, upper Tremadocian, Lower Ordovician), Arenig Fawr. A. NIGP 154639, indeterminate choiid, disarticulating, from Ceunant-ygarreg-ddu. B. NIGP 154640, three specimens of a Hazelia-like sponge, from Amnodd Wen. C. NIGP154641, undescribed reticulosan from Amnodd Wen. Scale bars 5 mm. All photographs taken under water.
Fig. 2 in First post-Cambrian records of the reticulosan sponges Valospongia and Hintzespongia from the late Tremadocian of North Wales
Fig. 2. Locality map showing the positions of the study sites within the local area, west of Arenig Fawr. Ceunant-y-garreg-ddu location marks the base of an extensive section through the upper part of the formation. Inset map shows the position of the localities within the UK.
Fig. 5 in First post-Cambrian records of the reticulosan sponges Valospongia and Hintzespongia from the late Tremadocian of North Wales
Fig. 5. The hexactine-bearing sponge Valospongia bufo sp. nov. Cut-away reconstruction, showing (left to right) outer surface including reticulate covering of mounds; outer layer with apices of mounds cut off, as seen in the majority of specimens due to partial compression of the skeletons; inner layer (or perhaps two layers superimposed) with combination of approximately diagonal and orthogonal elements of the skeletal mesh.
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