• Globigerina angipora Stache.—Finlay, 1939:125 [not illustrated]. [Not Stache, 1865 = nomen dubium.]
• Globigerina angiporoides Hornibrook, 1965:835-838, text-figs. 1a-i, 2 [uppermost Eocene, Campbells Beach, South Island, New Zealand].Quilty, 1976:637, pl. 1, figs. 5, 6 [lower Oligocene Zone P19, DSDP Site 321, Nazca Plate, southeast Pacific Ocean].Loubere, 1985, pl. 4, fig. 4 [lower Oligocene Zone P20, DSDP Hole 549A, northeast Atlantic Ocean].Poore, 1984, pl. 2, figs. 5, 6 [lower Oligocene Zone OL2, DSDP Site 522, Angola Basin, South Atlantic Ocean].van Eijden and Smit, 1991:109-110, pl. 2, fig. 8 [lower Oligocene Zone P20, ODP Hole 756C, eastern Indian Ocean].
• Globigerina (Subbotina) angiporoides angiporoides Hornibrook.Jenkins, 1971:160-161, pl. 20, figs. 588-594 [upper Eocene-lower Oligocene, Earthquakes Marl, South Island, New Zealand].
• Globigerina angiporoides angiporoides Hornibrook.Poore and Brabb, 1977:255, pl. 1, figs. 1-4 [lower Oligocene, San Lorenzo Fm., Santa Cruz Mountains, California].
• Subbotina angiporoides angiporoides (Hornibrook).Blow, 1979:1250-1252, pl. 12, fig. 3 [metatype; uppermost Eocene, Campbells Beach, South Island, New Zealand], fig. 4 [lower Oligocene Zone P19, Lindi, Tanzania].
• Subbotina angiporoides (Hornibrook).—Huber, 1991:440, pl. 5, fig. 5 [lower Oligocene Zone AP13, ODP Hole 738B, Kerguelen Plateau, South Indian Ocean].—Spezzaferri and Premoli Silva, 1991:257, pl. XV, fig. 3 [Subzone P21a = Zone O3-O5, DSDP Hole 538A, Gulf of Mexico], fig. 4 [lower Oligocene Zone P20 = Zone O1, DSDP Hole 538A, Gulf of Mexico].—Gallagher and Holdgate, 2000, fig.14 [lower Oligocene Zone P18-P21a = Zone O1-O4, Otway Basin, Australia].—Li and others, 2003, pl. 2, fig. 15 [lower Oligocene, ODP Hole 1134A, Great Australian Bight].—Olsson and others, 2006:126-129, pl. 6.6 (partim), figs. 1-3 [SEMs of holotype of Globigerina angiporoides, upper Eocene, Campbells Beach, South Island, New Zealand], fig. 4 [upper Eocene, Atlantic City Borehole, ODP Hole 150X, New Jersey ], figs. 6, 7, 13 [upper Eocene, ODP Hole 690B, Maud Rise, Weddell Sea], figs. 8, 12, SEMs of paratype of Globigerina angiporoides minima Jenkins [middle Eocene Globigerinatheka (Globigerapsis) index index Zone (not upper Eocene as stated by Olsson and others, 2006), Hampden Beach, South Island, New Zealand].
• Subbotina angiporoides minima (Jenkins).—Nocchi and others, 1991:270, pl. 6, figs. 13-15 [lower Oligocene Zone P18-P20 = Zone O1-O2, ODP Hole 703A, Subantarctic South Atlantic Ocean]. [Not Jenkins, 1966.]
• Globigerina linaperta Finlay subsp. transdanubica Samuel, 1972:181-182, pl. 37, fig. 4a-c, pl. 38, figs. 1, 2 [upper Eocene, Nagyveleg-1 borehole, Bakony Mountains, Hungary].
• Globorotalia sp. 2. Loubere, 1985:559, pl. 4, fig. 1 [lower Oligocene Zone P18, DSDP Hole 549A, northeastern Atlantic Ocean], figs. 2, 3 [upper Eocene Zone P17, DSDP Hole 549A, northeastern Atlantic Ocean].
• Not Subbotina angiporoides (Hornibrook).—Leckie and others, 1993:125, pl. 1, fig. 18 [lower Oligocene Zone P18, ODP Hole 628A, western North Atlantic Ocean ], fig. 19 [lower Oligocene Zone P19, ODP Hole 803D, Ontong Java Plateau, western equatorial Pacific Ocean ], fig. 20 [lower Oligocene Zone P19, ODP Hole 628A, western North Atlantic Ocean] (= Subbotina utilisindex).—Olsson and others, 2006:126-129, pl. 6.6 (partim), fig. 5, SEM of paratype of Globigerina angiporoides [middle (not upper, as stated) Eocene, Campbells Beach, South Island, New Zealand], figs. 9-11, SEMs of holotype of Globigerina angiporoides minima Jenkins [middle (not upper, as stated) Eocene, Hampden Beach, South Island, New Zealand] (= Subbotina minima).

Globigerina angipora Stache was described from sediments collected from the lower Oligocene (according to Hornibrook, 1965) Whaingaroa siltstone of New Zealand (Stache, 1865:287, pl. 24, fig. 36a-b). Unfortunately the description and illustrations are poor by modern standards and according to Hornibrook (1965), subsequent New Zealand taxonomists (following Finlay, 1939) identified a different form under the same name. Hornibrook (1965) declared angipora a nomen dubium and erected angiporoides to incorporate those forms previously described as angipora. A full discussion of this species was provided by Olsson and others (2006). The species is a common component of early Oligocene high latitude assemblages. Olsson and others (2006) considered Subbotina angiporoides minima (Jenkins) to be a junior synonym of Subbotina angiporoides (Hornibrook), however here we recognize Subbotina minima as a distinct species. [Wade et al. 2018]

Hornibrook (1961) used the name Globigerina angipora Stache, 1865 for a taxon resembling Stache’s figures. Later, after it was confirmed that Stache’s specimens were lost he declared the species a nomen dubium and erected the name angiporoides for this taxon. The species is a common element of middle Eocene-early Oligocene austral assemblages and its extinction has been used to define the top of the Globigerina angiporoides Zone of Jenkins (1966) and the Subbotina angiporoides Zone (Zone AP13) of Stott and Kennett (1990). Jenkins (1966) distinguished Globigerina angiporoides minima as an ancestral form that is smaller and less tightly coiled with a more open umbilicus and more inflated chambers. However, these forms are very difficult to distinguish consistently and, they are here considered synonymous. Morphologic overlap of these forms is revealed by similarity of the more loosely coiled paratype of G. angiporoides (Pl.6.6, Fig. 5) with the holotype of G. angiporoides minima (Pl.6.6, Figs. 9-11) and similarity of the more tightly coiled paratype of G. angiporoides minima (Pl.6.6, Fig. 8) with the holotype of G. angiporoides (Pl.6.6, Figs. 1-3).
Blow (1979, p. 1253-1255) distinguished Subbotina angiporoides lindiensis from S. angiporoides s.str. by its less tightly coiled, less closely appressed, and less embracing chambers. Unlike S. angiporoides s.str., the final chambers of Blow’s illustrated paratypes of S. angiporoides lindiensis, though broken, are kummerform and positioned adjacent to, rather than over, the umbilicus. The holotype of S. angiporoides lindiensis, which was originally illustrated as Globigerina linaperta pseudoeocaena (Subbotina) by Blow and Banner (1962, pl. 11, fig. M) is very similar to Blow’s paratypes, except for the absence of a kummerform chamber. The chamber arrangement and presence of a broad apertural lip on all forms of Blow’s subspecies suggest that it is more closely related to Subbotina yeguaensis (Weinzierl and Applin) than to S. angiporoides. [Olsson et al. 2006]

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