- species arranged by lineage and FAD (time control age-window is: 0-800Ma) | ||||
exilis sublineage | ||||
Globorotalia pertenuis Like G. exilis but larger and with a distinctly more lobate and compressed test. | ||||
Globorotalia exilis Like G. limbata but with a more compressed, thinner, and delicate test. | ||||
miocenica sublineage | ||||
Globorotalia multicamerata Like G. limbata but with more chambers in final whorl (usually 8-10 vs 6-8), a circular-outline to the test, and a wide, circular and deep umbilicus | ||||
Globorotalia miocenica Distinguished from other species of the menardii lineage by its distinctly planoconvex test and circular outline. | ||||
Globorotalia pseudomiocenica strongly-biconvex test with a sub-circular equatorial periphery and pronounced keel. | ||||
Globorotalia limbata Like G. menardii but uniformly increasing chambers in the final whorl; spiral sutures, initially straight then become sharply curved near the periphery, giving a hockey-stick shape | ||||
menardi sublineage | ||||
Globorotalia menardii Like G. praemenardii but larger, with raised spiral sutures, and a more massive keel. | ||||
Globorotalia praemenardii Like G. archeomenardii but larger, more lobulate, and with less convex spiral side. | ||||
Globorotalia archeomenardii Lenticular, low trochospiral, prominent keel and densely perforate surface; aperture low-arched slit, with a distinct lip |
Although Globorotalia (G.) praescitula, originally evolved in the temperate areas, it subsequently migrated to the tropics and thence gave rise to Menardella during the late Early Miocene (Text Fig. 14). Although the earliest representative of Menardella (Gr. (M.) archeomenardii) first appeared within Early Miocene Zone N8, the lineage did not become dominant among the tropical globorotaliids until the extinction of Fohsella at 12.4 Ma.
Members of Menardella during the Pliocene and Quaternary exhibit a wide range of variation, especially with respect to the strength of the keel, the number of chambers in the final whorl coiling mode, and bending of the final chamber. [Kennett & Srinivasan 1983]
Catalog entries: Globorotalia (Menardella)
Distinguishing features:
Parent taxon (Globorotalia): Smooth wall; compressed chambers:
This taxon: G. archeomenardii - menardii, limbata - miocenica & exilis - pertenius lineages
Geographic distribution
Most likely ancestor: hirsuta lineage - at confidence level 4 (out of 5). Data source: Kennett & Srinvasan 1983; Stewart 2003; Aze et al. 2011.
Likely descendants: tumida lineage;
plot with descendants
Geological Range:
Last occurrence (top): Extant. Data source: Total of ranges of the species in this database
First occurrence (base): within M5b subzone (15.10-16.27Ma, 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. 120
Bandy, O. L. (1972). Origin and development of Globorotalia (Turborotalia) pachyderma (Ehrenberg). Micropaleontology. 18(3): 294-318. gsReferences:
menardii lineage compiled by the pforams@mikrotax project team viewed: 7-12-2024
Short stable page link: https://mikrotax.org/pforams/index.php?id=104168 Go to Archive.is to create a permanent copy of this page - citation notes |