Globigerinacollactea (Finlay).—Bolli, 1957a:72, pl. 15: figs. 21-23 [G. rex Zone, Guayaguayare well 159, Trinidad].— Bolli, 1957b:162, pl. 35: fig. 18a, b [G. palmerae Zone, Navet Fm., Trinidad]. [Not Finlay, 1939.]
Acarininamattseensisalticonica Fleisher, 1974: pl. 2: figs. 1-5 [lower Eocene Zone P8, DSDP Site 229, Arabian Sea].
Globorotalia (Acarinina) appressocamerata Blow, 1979:907-908, pl. 144: figs. 2, 4-9 (7=holotype) [Zone P8b, DSDP Hole 20C, South Atlantic Ocean].
Globorotalia (Acarinina) cf. appressocamerata Blow, 1979:907-908, pl. 144: figs. 1, 3 [Zone P8b, DSDP Hole 20C, South Atlantic Ocean].
Acarininaappressocamerata Blow.—Lu and Keller, 1995: pl. 3: figs. 9, 10 [Zone P7, DSDP Site 577, Shatsky Rise, north-west Pacific Ocean].
Taxonomic discussion: This is a distinct early Eocene acarininid with superficial resemblance to the (predominantly) Paleocene morphotype Acarininasubsphaerica (Shutskaya). Blow (1979, p. 907) drew attention to these similarities in describing his new species Acarininaappressocamerata but observed that appressocamerata differed from subsphaerica in having more angulate chambers on the umbilical side and a more sharply delimited, more open, quadrate-shaped umbilicus (compared to the more rounded chambers and more restricted umbilicus in subsphaerica). Blow (1979, p. 908) also observed the lack of stratigraphic overlap between these two forms. Acarininasubsphaerica is abundant in Zone P4, and its last common occurrence in tropical sites has been used to subdivide Zone P4 (Berggren and others, 1995), although it may range higher in higher latitudes (Olsson and others, 1999, Berggren and others, 2000). Our detailed studies in Egypt have shown A. alticonica to appear in mid-Zone E4, a little lower than recorded by Blow (1979, p. 908). It forms a distinct component of early Eocene faunas (together with A. interposita, A. pentacamerata, A. soldadoensis, Morozovellaformosa, M. lensiformis, M. subbotinae, among others). Fleisher’s (1974) species Acarininamattseensisalticonica, which he described as having a restricted range in Zone P8 (=E6) in the Arabian Sea, appears to be a prior synonym exhibiting the same morphologic characters recorded by Blow (1979) in describing appressocamerata. While Fleisher drew attention to superficial resemblance of his taxon with Subbotina senni, he firmly rejected any affinity between the two forms. [Berggren et al. 2006]
Distinguishing features: Parent taxon (Acarinina): Moderate to low trochospire; chambers ovoid, usually 4-6 in final whorl. Wall muricate with pustules on umbilical shoulders; This taxon: High trochospiral test with closely appressed, angular chambers; strongly muricate
NB These concise distinguishing features statements are used in the tables of daughter-taxa to act as quick summaries of the differences between e.g. species of one genus. They are being edited as the site is developed and comments on them are especially welcome.
Description
Diagnostic characters: This form is distinguished by its strongly muricate test with a high trochospire and closely appressed, angular chambers. It is distinguished from A. subsphaerica and A. pseudosubsphaerica n. sp. by having more compressed, angular chambers and a less high-spired test. [Berggren et al. 2006] Morphology: Medium to high trochospiral, biconvex to subspherical, weakly lobulate test; circular outline, rounded periphery in edge view; in umbilical view equatorial profile slightly lobate, 5 moderately inflated, embracing, appressed, angulate chambers in last whorl, gradually increasing in size, tightly coiled around relatively narrow, deep umbilicus which is bordered by circumumbilical coalescence of prominent muricae; intercameral sutures radial, weakly incised; aperture a low arched, umbilical-extraumbilical slit bordered by distinct lip; on spiral side 11-12 chambers, tangentially longer than radially broad, coiled in 2½ whorls; intercameral sutures weakly curved and incised; chambers rounded in edge view. [Berggren et al. 2006] Wall type: Densely muricate, particularly around umbilicus. [Berggren et al. 2006] Size: Maximum diameter of holotype of A. alticonica: 0.31 mm; axial elevation: 0.30 mm (Fleisher, 1974, p. 1013); Maximum diameter of holotype of A. appressocamerata: 0.37 mm (Blow, 1979, p. 907) [Berggren et al. 2006]
Character matrix
test outline:
Subcircular
chamber arrangement:
Trochospiral
edge view:
Equally biconvex
aperture:
Umbilical-extraumbilical
sp chamber shape:
Inflated
coiling axis:
Moderate-high
periphery:
N/A
aperture border:
Thin lip
umb chbr shape:
Inflated
umbilicus:
Narrow
periph margin shape:
Broadly rounded
accessory apertures:
None
spiral sutures:
Strongly depressed
umb depth:
Deep
wall texture:
Coarsely muricate
shell porosity:
Finely Perforate: 1-2.5µm
umbilical or test sutures:
Strongly depressed
final-whorl chambers:
4.5-5.5
N.B. These characters are used for advanced search. N/A - not applicable
Biogeography and Palaeobiology
Geographic distributionCaribbean, South Atlantic, Tethys (Egypt). [Berggren et al. 2006]
Aze et al. 2011 summary: Low to middle latitudes; based on Berggren et al. (2006b) Isotope paleobiologyNo data available. [Berggren et al. 2006] Aze et al. 2011 ecogroup 1 - Open ocean mixed-layer tropical/subtropical, with symbionts; based on comparison with other species of the genus. Phylogenetic relationsProbably descended from A. soldadoensis and ancestral to A. pseudosubsphaerica n. sp. [Berggren et al. 2006]
Geological Range: Notes: Zone E4-E7. [Berggren et al. 2006] Last occurrence (top): within E7 zone (45.72-50.20Ma, top in Lutetian stage). Data source: Eocene Atlas First occurrence (base): in mid part of E4 zone (50% up, 53.6Ma, in Ypresian stage). Data source: Eocene Atlas
Plot of occurrence data:
Range-bar - range as quoted above, pink interval top occurs in, green interval base occurs in.
Triangles indicate an event for which a precise placement has been suggested
(NB There is no histogram as there are no occurrence records for the taxon in the Neptune database) Parent: Acarinina
Primary source for this page: Berggren et al. 2006 - Eocene Atlas, chap. 9, p. 262
References:
Berggren, W. A., Kent, D. V., Swisher, I. , C. C. & Aubry, M. -P. (1995b). A revised Cenozoic geochronology and chronostratigraphy. In, Berggren, W. A., Kent, D. V., Aubry, M. -P. & Hardenbol, J. (eds) Geochronology, Time Scales and Global Stratigraphic Correlations. SEPM (Society for Sedimentary Geology) Special Publication No. 54, 129-212. gs
Berggren, W. A., Van Fossen, M., V. , K. D., Norris, R. D. & Quillévéré, F. (2000). Integrated Paleocene calcareous plankton magnetobiochronology and stable isotope stratigraphy: DSDP Site 384 (NW Atlantic Ocean): , v. 159, p. 1-51. Palaeogeography Palaeoclimatology Palaeoecology. 159(1): 1-51. gs
Berggren, W. A., Pearson, P. N., Huber, B. T. & Wade, B. S. (2006b). Taxonomy, biostratigraphy, and phylogeny of Eocene Acarinina. In, Pearson, P. N., Olsson, R. K., Hemleben, C., Huber, B. T. & Berggren, W. A. (eds) Atlas of Eocene Planktonic Foraminifera. Cushman Foundation for Foraminiferal Research, Special Publication . 41(Chap 9): 257-326. gsO
Blow, W. H. (1979). The Cainozoic Globigerinida: A study of the morphology, taxonomy, evolutionary relationships and stratigraphical distribution of some Globigerinida (mainly Globigerinacea). E. J. Brill, Leiden. 2: 1-1413. gs
Bolli, H. M. (1957b). Planktonic foraminifera from the Oligocene-Miocene Cipero and Lengua formations of Trinidad, B.W.I. In, Loeblich, A. R. , Jr., Tappan, H., Beckmann, J. P., Bolli, H. M., Montanaro Gallitelli & E. Troelsen, J. C. (eds) Studies in Foraminifera. U.S. National Museum Bulletin . 215: 97-123. gs
Bolli, H. M. (1957a). Planktonic foraminifera from the Eocene Navet and San Fernando formations of Trinidad. In, Loeblich, A. R. , Jr., Tappan, H., Beckmann, J. P., Bolli, H. M., Montanaro Gallitelli, E. & Troelsen, J. C. (eds) Studies in Foraminifera. U.S. National Museum Bulletin . 215: 155-172. gs
Finlay, H. J. (1939b). New Zealand foraminifera: Key species in stratigraphy - no. 2. Transactions of the Royal Society of New Zealand. 69(1): 89-128. gs
Fleisher, R. L. (1974a). Cenozoic planktonic foraminifera and biostratigraphy, Arabian Sea, Deep Sea Drilling Project, Leg 23A. Initial Reports of the Deep Sea Drilling Project. 23: 1001-1072. gsO
Lu, G. & Keller, G. (1995). Planktic foraminiferal faunal turnovers in the subtropical Pacific during the Late Paleocene to Early Eocene. Journal of Foraminiferal Research. 25: 97-116. gs
Olsson, R. K., Hemleben, C., Berggren, W. A. & Huber, B. T. (1999). Atlas of Paleocene Planktonic Foraminifera. Smithsonian Institution Press, Washington, DC. (85): 1-252. gs
Acarinina alticonica compiled by the pforams@mikrotax project teamviewed: 9-2-2026