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Species Globrotalia miotumida Jenkins 1960


Discussion / Comments:
Jenkins (1985):
G. miotumida has 4 1/2 -5 chambers in the final whorl and is thin walled with a keeled periphery. In New Zealand the species appears to be restricted to the Middle and Late Miocene as in southeastern Australia, but at DSDP Leg 29 Site 284 in 'the Tasman Sea it ranges into the Early Pliocene. On Leg 40 Site 360, G. miotumida has the same range as in New Zealand but at the more northern Site 362 ranges again into the Early Pliocene (Jenkins, 1975, 1978c).
Synonym list:
Jenkins (1985):
1960 Globorotalia menardii miotumida Jenkins. - Jenkins : p.362 pl. 4, figs. 9a-c
1985 Globrotalia miotumida Jenkins. - Jenkins : p.277 figs. 7.12-13; 5
References:

Jenkins,D.G. (1960):
Planktonic foraminifers from the Lakes Entrance oil shaft, Victoria, Australia . Micropaleontology Vol. 6(4) p. 345-371

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
Anonymous: Unedited TaxonConcept data
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