Caron (1985):
M. schneegansi differs from M. sigali in having more inflated and petaloid-shaped chambers, increasing more rapidly in size, and umbilical sutures which are not raised- It diners from Dicarinella primitiva in its typical keel formed by two closely spaced parallel rows of pustules (Caron, 1974, pl. 1, figs. 4-5).
Some specimens show intermediate characters between the
genera Dicarinella and Marginotruncana. |
Sigal,J. (1952): Apercu stratigraphique sur la Micropaléontologie du Crétacé . XIXe Congrès Géologique International (Série 1), Alger Vol. 26 p. 3-47
Caron,M. (1974): Sur la validité de quelques espèces de Globotruncana du Turonien et du Coniacien . Actes du VIe Colloque Africain de Micropaleontologie, Tunis Vol. 28 p. 329-345
Caron,M. (1985): Cretaceous planktic foraminifera. In: Plankton stratigraphy Eds: Bolli, H.M.Saunders, J.B.Perch-Nielsen, K. p. 17–86
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