Foraminifera taxon details
Stomatostoecha Applin, Loeblich & Tappan, 1950 †
738405 (urn:lsid:marinespecies.org:taxname:738405)
accepted
Genus
Stomatostoecha plummerae Applin, Loeblich & Tappan, 1950 † (type by original designation)
marine, brackish, fresh, terrestrial
fossil only
feminine
Applin, E. R.; Loeblich, A. R.; Tappan, H. (1950). Two new Lower Cretaceous lituolid foraminifera. <em>Journal of the Washington Academy of Sciences, Washington, D.C.</em> 40: 75-79., available online at https://www.biodiversitylibrary.org/part/50569#/summary
page(s): p. 76 [details]
page(s): p. 76 [details]
Diagnosis Test discoidal to lenticular, numerous broad and low chambers increasing rapidly in breadth so that the spire increases...
Diagnosis Test discoidal to lenticular, numerous broad and low chambers increasing rapidly in breadth so that the spire increases rapidly in height, coiling planispiral and incompletely involute, leaving a depressed umbilicus; wall finely agglutinated, imperforate, simple in structure; apertural face high and truncate and may be slightly depressed centrally, aperture a small areal slit in the early stage as seen in thin section, becoming terminal in the expanded and nearly uncoiled later portion. L. Cretaceous (Albian); USA: Texas. (Loeblich & Tappan, 1987, Foraminiferal Genera and Their Classification) [details]
Hayward, B.W.; Le Coze, F.; Vachard, D.; Gross, O. (2025). World Foraminifera Database. Stomatostoecha Applin, Loeblich & Tappan, 1950 †. Accessed at: https://www.marinespecies.org/foraminifera/aphia.php?p=taxdetails&id=738405 on 2026-09-13
Date
action
by
original description
Applin, E. R.; Loeblich, A. R.; Tappan, H. (1950). Two new Lower Cretaceous lituolid foraminifera. <em>Journal of the Washington Academy of Sciences, Washington, D.C.</em> 40: 75-79., available online at https://www.biodiversitylibrary.org/part/50569#/summary
page(s): p. 76 [details]
page(s): p. 76 [details]
From editor or global species database
Diagnosis Test discoidal to lenticular, numerous broad and low chambers increasing rapidly in breadth so that the spire increases rapidly in height, coiling planispiral and incompletely involute, leaving a depressed umbilicus; wall finely agglutinated, imperforate, simple in structure; apertural face high and truncate and may be slightly depressed centrally, aperture a small areal slit in the early stage as seen in thin section, becoming terminal in the expanded and nearly uncoiled later portion. L. Cretaceous (Albian); USA: Texas. (Loeblich & Tappan, 1987, Foraminiferal Genera and Their Classification) [details]