Miliolacea is one of five superfamilies belonging to the Miliolida, (suborder Miliolina in Loeblich & Tappan 1988). Miliolaceans produce a coiled test, commonly with two, less frequently three or more, chambers per whorl arranged in varying planes about the longitudinal axis, which later may become involute or uncoil. Advanced forms may have secondary partitions within the chambers. Species within the Milioacea are found in Upper Triassic (Norian) to recent marine sediments.
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| - Milioloidea (es)
- Miliolacea (en)
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| - Miliolacea is one of five superfamilies belonging to the Miliolida, (suborder Miliolina in Loeblich & Tappan 1988). Miliolaceans produce a coiled test, commonly with two, less frequently three or more, chambers per whorl arranged in varying planes about the longitudinal axis, which later may become involute or uncoil. Advanced forms may have secondary partitions within the chambers. Species within the Milioacea are found in Upper Triassic (Norian) to recent marine sediments. (en)
- Milioloidea, tradicionalmente denominada Miliolacea, es una superfamilia de foraminíferos del suborden Miliolina y del orden Miliolida. Su rango cronoestratigráfico abarca desde el Noriense (Triásico superior) hasta la Actualidad. (es)
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| - Late Triassic - Holocene (en)
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| - "Quinqueloculina seminula" (en)
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| - Quinqueloculina seminula (en)
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| - *Austrotrillinidae
*Hauerinidae
*Miliolechinidae
*Miliolidae
*Riveronidae
*Spiroloculinidae (en)
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| - Miliolacea is one of five superfamilies belonging to the Miliolida, (suborder Miliolina in Loeblich & Tappan 1988). Miliolaceans produce a coiled test, commonly with two, less frequently three or more, chambers per whorl arranged in varying planes about the longitudinal axis, which later may become involute or uncoil. Advanced forms may have secondary partitions within the chambers. Species within the Milioacea are found in Upper Triassic (Norian) to recent marine sediments. (en)
- Milioloidea, tradicionalmente denominada Miliolacea, es una superfamilia de foraminíferos del suborden Miliolina y del orden Miliolida. Su rango cronoestratigráfico abarca desde el Noriense (Triásico superior) hasta la Actualidad. (es)
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