Tabel 1 in Pseudocyclammina Sarvakensis Sp. Nov. And Pseudotextulariella Brevicamerata Sp. Nov.: Further Evidence For The Cenomanian Megadiversity Of Larger Benthic Foraminifera From The Sarvak Formation Of Sw Iran

Tabel 1 Comparison of dimensions of Pseudotextulariella cretosa (Cushman) (late Albian–Cenomanian), P. brevicamerata sp. nov., and P. courtionensis Brönnimann (late Berriasian–Valanginian). Test height and diameter in mm.
Pseudotextulariella cretosa (Cushman 1932)Test heightTest diameterNumber of chambersThickness septa (µm)Height chamber lumen (µm)Order of raftersCushman 19321.751.75----Barnard & Banner, 1953up to 1.2up to 1.0---up to 5Grönhagen & Luterbacher 19660.5-1.30.35-1.015-30--up to 2Charollais & Brönnimann 1965-----up to 3Bucur & Baltres 2002up to 0.95up to 1.15-up to 35up to 110up to 2Pseudotextulariella brevicamerata sp. nov.up to 0.8up to 0.8520-34up to 2525-401Pseudotextulariella courtionensis Brönnimann, 1966up to 0.8up to 0.82up to 22up to 35up to 551