Daughter taxa (time control age-window is: 0-800Ma) | Granddaughter taxa | |||
margaritae->hirsuta sublineage | ||||
Globorotalia hirsuta Distinguished by its thick, relatively high-spired test, 4 chambers in the final whorl, and pustulose surface. | ||||
Globorotalia eastropacia Distinct but thin peripheral keel and strongly recurved spiral sutures, lobate outline | ||||
Globorotalia margaritae Like G. juanai & scitula, but more convexly rounded spiral side and concave to flat umbilical side; more delicate peripheral keel, and in the distinctly elongate, narrower, and more strongly curved chambers on spiral side. | ||||
Globorotalia juanai Like G. scitula but periphery rounded and early chambers umbonate | ||||
scitula sublineage | ||||
Globorotalia bermudezi Like G. scitula but much smaller, has inflated chambers on the umbilical side, and a more irregularly perforated test. | ||||
Globorotalia scitula Like G. praescitula but smooth surface and subcircular outline | ||||
Globorotalia praescitula Like G. zealandica but more chambers in final whorl (4½ vs 4), increased curvature of the sutures on the umbilical side, peripheral compression, and a return to a low-arched aperture | ||||
other species | ||||
Globorotalia cibaoensis Distinguished by its biconvex test with a rounded periphery (sometimes angular or narrowly keeled in the final chamber.) | ||||
Globorotalia gigantea Like G. scitula but much larger (>0.5mm vs ca 0.3mm) | ||||
Globorotalia challengeri Like G. praescitula, but 5-5½ chambers in final whorl (vs 4½), more inflated chambers, and a more rounded periphery |
Globorotalia (Globoconella) praescitula is the ancestral form for the Hirsutella lineage. During the early Middle Miocene, Gr. (G.) praescitula evolved into Globorotalia (Hirsutella) scitula in tropical to temperate areas and Globorotalia (Hirsutella) challengeri in temperate areas. Later in the Middle to Late Miocene, several taxa evolved in turn from Globorotalia (Hirsutella) scitula (Text Fig. 15). [Kennett & Srinivasan 1983]
There are significant inconsistencies in the literature regarding the hirsuta lineage. In particular:
Catalog entries: Globorotalia (Hirsutella), Obandyella
Distinguishing features:
Parent taxon (Globorotalia): Smooth wall; compressed chambers:
This taxon: G. scitula - juanai - margaritae - hirsuta lineage
Geographic distribution
Geological Range:
Last occurrence (top): Extant. Data source: Total of ranges of the species in this database
First occurrence (base): within M3 zone (17.54-19.30Ma, base in Burdigalian stage). Data source: Total of ranges of species in this database
Plot of occurrence data:
Primary source for this page: Kennett & Srinivasan 1983, p. 132
Bandy, O. L. (1972). Origin and development of Globorotalia (Turborotalia) pachyderma (Ehrenberg). Micropaleontology. 18(3): 294-318. gs Haman, D., Huddleston, R. W. & Donahue, J. P. (1981). Obandyella, a new name for Hirsutella Bandy, 1972 (Foraminiferida) non Cooper and Muir Wood,1951 (Brachiopoda). Proceedings of the Biological Society of Washington. 93(4): 1264-1265. gs Kennett, J. P. & Srinivasan, M. S. (1983). Neogene Planktonic Foraminifera. Hutchinson Ross Publishing Co., Stroudsburg, Pennsylvania. 1-265. gsReferences:
hirsuta lineage compiled by the pforams@mikrotax project team viewed: 14-1-2025
Short stable page link: https://mikrotax.org/pforams/index.php?id=104167 Go to Archive.is to create a permanent copy of this page - citation notes |