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The Schwagerinidae comprise a family of large, generally fusiform, foraminiferans included in the Fusulinacea, a superfamily of fusulinids, locally abundant during the later Carboniferous (Pennsylvanian) and most of the Permian. As with all fusulinaceans, the Schagerinidae are a shallow water form which in places make up a significant portion of the sediment, now limestone. More familiar genera include Schwagerina, Triticites, and Parafusulina.

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  • Schwagerinidae (es)
  • Schwagerinidae (en)
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  • Schwagerinidae es una familia de foraminíferos bentónicos de la superfamilia Fusulinoidea, del suborden Fusulinina​ y del orden Fusulinida.​ Su rango cronoestratigráfico abarca desde el Moscoviense (Carbonífero superior) hasta el Pérmico superior. (es)
  • The Schwagerinidae comprise a family of large, generally fusiform, foraminiferans included in the Fusulinacea, a superfamily of fusulinids, locally abundant during the later Carboniferous (Pennsylvanian) and most of the Permian. As with all fusulinaceans, the Schagerinidae are a shallow water form which in places make up a significant portion of the sediment, now limestone. More familiar genera include Schwagerina, Triticites, and Parafusulina. (en)
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  • Dunbar and Henbest, 1930 (en)
fossil range
  • Late Carb - Late Permian (en)
taxon
  • Schwagerinidae (en)
has abstract
  • Schwagerinidae es una familia de foraminíferos bentónicos de la superfamilia Fusulinoidea, del suborden Fusulinina​ y del orden Fusulinida.​ Su rango cronoestratigráfico abarca desde el Moscoviense (Carbonífero superior) hasta el Pérmico superior. (es)
  • The Schwagerinidae comprise a family of large, generally fusiform, foraminiferans included in the Fusulinacea, a superfamily of fusulinids, locally abundant during the later Carboniferous (Pennsylvanian) and most of the Permian. M.L. Thompson (1964) gives the following diagnosis: Shell large, fusiform to irregularly cylindrical, planispiral, involute in most, irregularly uncoiled in some; spirotheca thick, composed of tectum and alveolar kariotheca; septa fluted in end zones of primitive genera, fluted completely across shell and to tops of chambers of more advanced genera; tummel singular in most forms, multiple in one genus; axial fillings absent to massive; chomata massive to slight. As with all fusulinaceans, the Schagerinidae are a shallow water form which in places make up a significant portion of the sediment, now limestone. More familiar genera include Schwagerina, Triticites, and Parafusulina. (en)
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