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    dc:creator "Schröder, Stefan; Soto, Francisco" ;
    dc:title "Cantabriastraea cantabrica Schröder & Soto, 2003, gen. et" ;
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<http://dx.doi.org/10.5281/zenodo.13390843>
    bibo:endPage "558" ;
    bibo:issue "4" ;
    bibo:journal "Acta Palaeontologica Polonica" ;
    bibo:pubDate "2003-09-30" ;
    bibo:startPage "547" ;
    bibo:volume "48" ;
    dc:creator "Schröder, Stefan; Soto, Francisco" ;
    dc:date "2003" ;
    dc:title "Lower Devonian (Emsian) rugose corals from the Cantabrian Mountains, northern Spain" ;
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    dc:description "Fig. 6. Cantabriastraea cantabrica gen. et sp. nov. A. Cross section of holotype DPO 14780. B. Longitudinal section of the same. Both × 2. Specimen from the Upper Emsian of Colle." ;
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<http://dx.doi.org/10.5281/zenodo.13390893>
    dc:description "Fig. 7. Cantabriastraea cantabrica gen. et sp. nov. A. Colony DPO 14811 consisting of a large protocorallite disrupted by nonparricidal, marginal increase in distal view (A1); septa appear as broad and flat ridges which are stronglyretiformtowardstheperiphery.Undersideofthesamecolony(A2), partly encrusted by Aulopora sp.; × 2. B. Colony DPO 14813. B1. Colony underside showing a single protocorallite turned to the left. B2. Upper surface of the same colony; × 1. All specimens from the Upper Emsian of Colle." ;
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<http://dx.doi.org/10.5281/zenodo.13390897>
    dc:description "Fig. 9. A. Cantabriastraea cantabrica gen. et sp. nov., specimen DPO 14789. A1. Cross sec− tion of tabularium and inner dissepimentarium. Trabeculae are oriented perpendicular to the rows of dissepiments; × 15. A2. Detail of A1; trabeculae intercalate between existing ones or bifurcate; × 20. A3. Septa in cross section with strong dilations in inner dissepimentarium caused by thickening of trabeculae. Towards the periphery (left side) septa become irregular carinate and may split into discrete trabeculae; × 24. B, C. Tabulophyllum bonarense sp. nov. B. Wall of corallite DPO 14673 in cross sec− tion. Thickenings of wall and lonsdaleoid dis− sepiments show a fibrous structure caused by thickened septal bases; × 24. C. Thin septa of corallite DPO 14686 (compare with Fig. 4G) inserting on lonsdaleoid dissepiments (dark lines in lower part of picture). Central part to− wards the axis (top of picture) is strongly af− fected by cement; × 24. All specimens from the Upper Emsian of Colle." ;
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