Foraminifera taxon details
Kolchidina Morozova, 1967 †
737708 (urn:lsid:marinespecies.org:taxname:737708)
accepted
Genus
Ammobaculites manyschensis Bykova, 1953 † accepted as Ammobaculites paleocenicus Cushman, 1947 † accepted as Kolchidina paleocenica (Cushman, 1947) † (type by original designation)
marine, brackish, fresh, terrestrial
fossil only
feminine
Morozova, V. G.; Kozhevnikova, G. E.; Kuryleva, A. M. (1967). Датско-палеоценовые разнофациальные отложения Копет-Дага и методы их корреляции по фораминиферам - Danian-Paleocene heterofacial deposits of Kopet-Dag and methods of their correlation according to foraminifers. <em>Труды ГИН - Transactions of the Geological Institute (Academy of Sciences USSR).</em> 157: 1-212., available online at http://ginras.ru/library/pdf/157_1967_morozova_etal_forams_paleogene.pdf
page(s): p. 176 [details] Available for editors
[request]
page(s): p. 176 [details] Available for editors
[request]
Hayward, B.W.; Le Coze, F.; Vachard, D.; Gross, O. (2024). World Foraminifera Database. Kolchidina Morozova, 1967 †. Accessed at: https://www.marinespecies.org/foraminifera/aphia.php?p=taxdetails&id=737708 on 2024-04-20
Date
action
by
original description
Morozova, V. G.; Kozhevnikova, G. E.; Kuryleva, A. M. (1967). Датско-палеоценовые разнофациальные отложения Копет-Дага и методы их корреляции по фораминиферам - Danian-Paleocene heterofacial deposits of Kopet-Dag and methods of their correlation according to foraminifers. <em>Труды ГИН - Transactions of the Geological Institute (Academy of Sciences USSR).</em> 157: 1-212., available online at http://ginras.ru/library/pdf/157_1967_morozova_etal_forams_paleogene.pdf
page(s): p. 176 [details] Available for editors [request]
page(s): p. 176 [details] Available for editors
[request] From editor or global species database
Diagnosis Test enrolled in early stage, later may be uncoiled and rectilinear, chambers inflated, sutures straight; wall finely to coarsely agglutinated, commonly including a variety of mineral grains, fish bone fragments, or smaller foraminifers; wall and septa simple in structure, but wall against the spiral suture may be considerably thickened, so that chamber lumen is reduced in size and restricted to the outer part of the coil or to the corresponding part of the later uniserial chambers; aperture areal and arcuate to semilunate in the early coil, paralleling the axis of coiling, becoming multiple and terminal in the uncoiled stage, consisting of a ring of openings in a depression covering most of the upper surface of the final chamber. L. Paleocene (Danian); USA: Alabama, USSR: Crimea, Caucasus, Turkmenia, Russian Platform. (Loeblich & Tappan, 1987, Foraminiferal Genera and Their Classification) [details]