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Sigmoilopsis

provided by wikipedia EN

Sigmoilinopsis is a genus of miliolid Foraminifera, with an ovate test, chambers one-half coil in length, arranged in rapidly changing planes in the early stage resulting in two spiralling series that appear sigmoid in section, gradually becoming planispiral in the adult. Walls are thick, porcelaneous but enclosing a large quantity of agglutinated quartz particles, sponge spicules, and shell fragments; the aperture terminal, rounded, with a small tooth.

Sigmoilinopsis is grossly similar to Sigmoilina but with less enveloping chambers allowing earlier ones to be externally visible, and in incorporating agglutinated material.

Sigmoilinopsis is included in the Hauerinidae (Loeblich & Tappan 1988). Previously it was assigned to the Miliolidae (Loeblich & Tappan 1964) and included in the subfamily Quinqueloculininae.

References

  • Alfred R. Loeblich Jr and Helen Tappan,1988. Forminiferal Genera and their Classification. e-book [1]
  • Alfred R. Loeblich Jr and Helen Tappan, 1964. Sarcodina Chiefly "Thecamoebians" and Foraminiferida; Treatise on Invertebrate Paleontology, Part C Protista 2. Geological Society of America and University of Kansas Press.
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Sigmoilopsis: Brief Summary

provided by wikipedia EN

Sigmoilinopsis is a genus of miliolid Foraminifera, with an ovate test, chambers one-half coil in length, arranged in rapidly changing planes in the early stage resulting in two spiralling series that appear sigmoid in section, gradually becoming planispiral in the adult. Walls are thick, porcelaneous but enclosing a large quantity of agglutinated quartz particles, sponge spicules, and shell fragments; the aperture terminal, rounded, with a small tooth.

Sigmoilinopsis is grossly similar to Sigmoilina but with less enveloping chambers allowing earlier ones to be externally visible, and in incorporating agglutinated material.

Sigmoilinopsis is included in the Hauerinidae (Loeblich & Tappan 1988). Previously it was assigned to the Miliolidae (Loeblich & Tappan 1964) and included in the subfamily Quinqueloculininae.

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Diagnosis

provided by World Register of Marine Species
Test ovate in outline, chambers one-half coil in length, with rapidly changing planes in the early stage resulting in two spiralling series that appear sigmoid in section, gradually becoming planispiral in the adult, chambers with floors, chamber lumen narrow; wall thick, porcelaneous but enclosing a large quantity of agglutinated quartz particles, sponge spicules, and shell fragments; aperture terminal, rounded, with a small tooth. Miocene to Holocene; Europe; Atlantic; Caribbean; Australia; New Zealand. (Loeblich & Tappan, 1987, Foraminiferal Genera and Their Classification)

Reference

Loeblich, A. R.; Tappan, H. (1987). Foraminiferal Genera and their Classification. Van Nostrand Reinhold Company, New York. 970pp.

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