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Morozovella crater Finlay 1939 from: Jenkins, D.G. (1985): Southern mid-latitude Paleocene to Holocene planktic foraminifera. In: Plankton stratigraphy Eds: Bolli, H.M.Saunders, J.B.Perch-Nielsen, K. p. 263-282
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Species Morozovella crater Finlay 1939



Discussion / Comments:
Jenkins (1985):
M. crater differs from M. caucasica in having 5 chambers in the final whorl as opposed to 61, in the holotype. The latter form i's rare in New Zealand. M. crater has a short range in the Early Eocene of New Zealand (Jenkins, 1971) and at DSDP Leg 29 Site 277 (Jenkins, 1975). Toumarkine (1978) recorded Globorotalia aragonensis caucasica from the Early Eocene of Leg 40 Sites 361 and 363 in the Southeast Atlantic, but did not record M. crater.
Synonym list:
Jenkins (1985):
1939 Globorotalia crater Finlay. - Finlay : p.125
1985 Morozovella crater Finlay. - Jenkins : p.273 figs. 6.9; 5
Was used in synonym list of:
References:

Finlay,H.J. (1939):
New Zealand foraminifera; key species in stratigraphy, No. 3 . Transactions of the Royal Society of New Zealand Vol. 69 p. 309-29

Jenkins,D.G. (1985):
Southern mid-latitude Paleocene to Holocene planktic foraminifera.
In: Plankton stratigraphy Eds: Bolli, H.M.Saunders, J.B.Perch-Nielsen, K. p. 263-282

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