Acarinina primitiva


Classification: pf_cenozoic -> muricate non-spinose -> Truncorotaloididae -> Acarinina -> Acarinina primitiva
Sister taxa: << < A. boudreauxi, A. bullbrooki, A. coalingensis, A. collactea, A. cuneicamerata, A. echinata, A. esnaensis, A. esnehensis, A. interposita, A. mcgowrani, A. mckannai, A. medizzai, A. nitida, A. pentacamerata, A. praetopilensis, A. primitiva, A. pseudosubsphaerica, A. pseudotopilensis, A. punctocarinata, A. quetra, A. rohri, A. sibaiyaensis, A. soldadoensis, A. strabocella, A. subsphaerica, A. topilensis, A. wilcoxensis,

Taxonomy

Citation: Acarinina primitiva (Finlay 1947)
Rank: Species
Basionym: Globoquadrina primitiva
Synonyms:
Taxonomic discussion: The outward, superficial morphologic similarity of the type species primitiva to that of the Neogene globoquadrinid form Globoquadrina dehiscens led Jenkins (1965b) to create the generic name Pseudogloboquadrina for Eocene morphotypes, but the morphology is similar to other Paleogene acarininids and this name is unnecessary (see also Blow, 1979, p. 950).
Acarinina primitiva is the dominant acarininid in middle Eocene austral assemblages and its disappearance/extinction in the late middle Eocene (?Chron C18n) is a useful datum level for regional correlation. See discussion in Berggren and Norris (1997, p. 69), Olsson and others (1999, p. 437) and above for A. coalingensis for further relevant data. [Berggren et al. 2006]

Catalog entries: Globoquadrina primitiva;

Type images:

Short diagnosis: Distinguished by triangular (broadly wedge-shaped) chambers; asymmetrically situated aperture resulting in distinct projection of umbilical face of last chamber over the umbilicus. Acarinina coalingensis has more rounded, inflated chambers than A. primitiva and lacks the straight, incised intercameral sutures on the umbilical side.

NB The short diagnoses are used in the tables of daughter-taxa to act as quick summaries of the differences between e.g. species of one genus. They have initially been copied from the diagnostic characters/distinguishing features sections of the Eocene and Paleocene Atlases, they will be edited as the site is developed.

Description


Diagnostic characters: Distinguished by triangular (broadly wedge-shaped) chambers; asymmetrically situated aperture resulting in distinct projection of umbilical face of last chamber over the umbilicus. Acarinina coalingensis has more rounded, inflated chambers than A. primitiva and lacks the straight, incised intercameral sutures on the umbilical side. [Berggren et al. 2006]

Wall type: Coarsely muricate, often with relatively smooth umbilical face to final chamber, normal perforate, nonspinose. [Berggren et al. 2006]

Test morphology: Robust, compact, subquadrate, strongly and bluntly muricate test; 3-4 triangular-shaped chambers in last whorl); chambers arranged at distinct right angles to each other and usually separated by distinct and incised sutures (particularly between preantepenultimate and antepenultimate chambers) on the umbilical side; umbilicus narrow, deep; aperture asymmetrically placed at base of last chamber, interiomarginal, umbilical-extraumbilical; high, smooth or beaded (but not muricate) face to final chamber above aperture, chambers on spiral side tangentially longer than broad; sutures curved, generally obscured by muricate ornament; peripheral margin subangular in edge view; [Berggren et al. 2006]

Size: Maximum diameter of holotype 0.29mm, thickness 0.26 mm. [Berggren et al. 2006]

Character matrix

test outline:Subquadratecoiling axis:Lowchamber arrangement:Trochospiralumbilicus:Narrow
edge view:Inequally biconvexumbilical or test sutures:Strongly depressedspiral sutures:Strongly depressedshell porosity:Finely Perforate: 1-2.5
wall texture:Coarsely muricateaperture:Umb.-extraumbilicalaperture border:N/Aaccessory apertures:None
periphery:Muricocarinateumb chamber shape:Inflatedsp chbr shape:Inflatedperiph margin shape:Subangular
umb depth:Deepdiameter mm:0.29width mm:breadth mm:0.26
final-whorl chambers:3.0-4.0

Biogeography and Palaeobiology


Geographic distribution: Essentially temperate-high latitude (austral; South Indian Ocean and Subantarctic Ocean distribution; less commonly reported in low latitudes (Caribbean, Atlantic, Indo-Pacific). [Berggren et al. 2006]
Aze et al. 2011 summary: Middle to high latitudes, less commonly in low latitudes; based on Berggren et al. (2006b)

Isotope paleobiology: No data available. [Berggren et al. 2006]
Aze et al. 2011 ecogroup 1 - Open ocean mixed-layer tropical/subtropical, with symbionts. Based on very heavy δ13C and relatively light δ18O. Sources cited by Aze et al. 2011 (appendix S3): this study

Phylogenetic relations: This form descended from Acarinina coalingensis in the early Eocene by means of developing a more subquadrate test and concomitant sutural incision and chamber separation in the final whorl. [Berggren et al. 2006]

Biostratigraphic distribution

Geological Range:
Notes: Zone E6 to Zone E13. Berggren and others (2000) recorded the lowest/earliest occurrence of A. primitiva in association with the lowest/ earliest A. coalingensis in Zone P4c and Chron C25r and C25n at DSDP Site 384 in the northwest Atlantic Ocean (see also compilation in Berggren and others, 1995, p. 155); we now regard these records as referable to A. coalingensis. The last occurrence datum has been fixed by Huber (1991) to lower Zone AP11 at Sites 738 Kerguelen Plateau, by Stott and Kennett (1990) to a level in mid-Chron C18n at ODP Site 689 on Maud Rise and by Berggren (1992) to a level within/slightly above questionable Chron 18n at Site 748, Kerguelen Plateau, which is approximately equivalent to Zone E13 in the (sub)tropics. [Berggren et al. 2006]
Last occurrence (top): within E13 zone (37.99-39.97Ma, top in Bartonian stage). Data source: Eocene Atlas
First occurrence (base): within E6 zone (50.20-50.67Ma, base in Ypresian stage). Data source: Eocene Atlas

Plot of occurrence data:

Primary source for this page: Berggren et al. 2006 - Atlas of Eocene Planktonic Foraminifera, chapter 9, p. 302

References:

Basov, I.A., (1995). Paleogene planktonic foraminifer biostratigraphy of Sites 883 and 884, Detroit Seamount (Subarctic Pacific). Proceedings of the Ocean Drilling Program, Scientific Results, 145: 157- 170.

Berggren, W.A. & Norris, R.D., (1997). Biostratigraphy, phylogeny and systematics of Paleocene trochospiral planktonic foraminifera. Micropaleontology, Supplement 1, 43: 1-116.

Berggren 1992 [sorry, not in our bibliography yet]

Berggren, W.A.; Kent, D.V.; Swisher, I., C.C. & Aubry, M.-P., (1995). A revised Cenozoic geochronology and chronostratigraphy. In: Berggren, W.A. et al. (Editors), Geochronology, Time Scales and Global Stratigraphic Correlations. SEPM (Society for Sedimentary Geology) Special Publication No. 54.

Berggren, W.A.; Pearson, P.N.; Huber, B.T. & Wade, B.S., (2006). Taxonomy, biostratigraphy, and phylogeny of Eocene Acarinina. In: Pearson, P.N. et al. (Editors), Atlas of Eocene Planktonic Foraminifera, Cushman Foundation Special Publication 41. Allen Press, Lawrence, Kansas, pp. 257-326.

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, 1413 pp.

Bolli, H.M., (1957). The genera Globigerina and Globorotalia in the Paleocene-Lower Eocene Lizard Springs Formation of Trinidad. In: Loeblich, A.R., Jr. et al. (Editors), Studies in Foraminifera, U.S. National Museum Bulletin 215. U.S. Government Printing Office, Washington, D.C., pp. 97-124.

Bolli, H.M.; Loeblich, A.R., Jr. & Tappan, H., (1957). Planktonic foraminiferal families Hantkeninidae, Orbulinidae, Globorotaliidae and Globotruncanidae. In: Loeblich, A.R., Jr. et al. (Editors), Studies in Foraminifera, U.S. National Museum Bulletin 215. U.S. Government Printing Office, Washington, DC, pp. 3-50.

Brönnimann, P., (1952). Globigerinoita and Globigerinatheka, new genera from the Tertiary of Trinidad, B.W.I. Cushman Foundation for Foraminiferal Research, Special Publication, 3(1): 25-28.

Brönnimann, P., (1952). Note on planktonic foraminifera from Danian localities of Jutland, Denmark. Eclogae Geologicae Helvetiae, 45(2): 339-341.

Brönnimann, P., (1952). Trinidad Paleocene and lower Eocene Globigerinidae. Bulletin of American Paleontology, 34(143): 1-34.

Brönnimann, P., (1952). Globigerinidae from the Upper Cretaceous (Cenomanian-Maestrichtian) of Trinidad, B. W. I. Bulletin of American Paleontology, 34(140): 1-70.

Finlay, H.J., (1947). New Zealand foraminifera: Key species in stratigraphy - no. 5. New Zealand Journal of Science and Technology, 28(5): 259-292.

Hillebrandt, A., (1962). Das paleozan und seine Foraminiferenfauna im Becken von Reichehall und Salzburg. Abhandlungen Bayerische Akademie der Wissenschaften Mathematisch Naturwissenschaftliche Klasse, 108: 1-182.

Hornibrook, N.d.B., (1953). Faunal migrations to New Zealand, I: Immigration of foraminifera to New Zealand during the Upper Cretaceous and Tertiary. New Zealand Journal of Science and Technology, 34: 436-444.

Hornibrook, N.d.B., (1961). Tertiary Foraminifera from Oamaru District (N.Z.). New Zealand Geological Survey, Paleontological Bulletin, 34(1).

Huber, B.T., (1991). Paleogene and early Neogene planktonic foraminifer biostratigraphy of ODP Leg 119 Sites 738 and 744, Kerguelen Plateau (southern Indian Ocean). Proceedings of the Ocean Drilling Program, Scientific Results, 119: 427-449.

Jenkins, D.G., (1965). A re-examinition of Globorotalia collactea Finlay, 1939. New Zealand Journal of Geology and Geophysics, 8: 843-848.

Jenkins, D.G., (1965). Planktonic Foraminiferal zones and new taxa from the Danian to lower Miocene of New Zealand. New Zealand Journal of Geology and Geophysics, 8(6): 1088-1126.

Jenkins, D.G., (1971). New Zealand Cenozoic Planktonic Foraminifera. New Zealand Geological Survey, Paleontological Bulletin, 42: 1-278.

Lu, G. & Keller, G., (1993). The Paleocene-Eocene transition in the Antarctic Indian Ocean: Inference from planktic foraminifera. Marine Micropaleontology, 21: 101-142.

Pearson, P.N.; Shackleton, N.J. & Hall, M.A., (1993). Stable isotope paleoecology of middle Eocene planktonic foraminifera and multi-species isotope stratigraphy, DSDP Site 523, South Atlantic. Journal of Foraminiferal Research, 23: 123-140.

Stainforth, R.M.; Lamb, J.L.; Luterbacher, H.; Beard, J.H. & Jeffords, R.M., (1975). Cenozoic planktonic foraminiferal zonation and characteristics of index forms. The University of Kansas Paleontological Contributions, 62: 1-425.

Stott, L.D. & Kennett, J.P., (1990). The Paleoceanographic and Paleoclimatic signature of the Cretaceous/Paleogene boundary in the Antarctic: Stable isotopic results from ODP Leg 113. Proceedings of the Ocean Drilling Program, Scientific Results, 113: 829-848.


Acarinina primitiva compiled by the pforams@mikrotax project team viewed: 30-5-2017

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