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Species Acarinina aspensis Colom 1954 | ||||||
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Diagnosis / Definition: | ||||||
Pearson et al. (2006): DESCRIPTION. Type of wall: Normal perforate, non-spinose with coarse muricae. Test morphology: Low trochospiral, variable number of subglobular chambers (ranging from 6-8, rarely to 10) in last whorl; intercameral sutures radial, moderately depressed between weakly embracing chambers; umbilicus deep, wide as a result of relatively lax/evolute coiling, no circum-umbilical concentration of muricae; 2-2 1/2 whorls on spiral side; intercameral sutures weakly recurved between early chambers, straight, radial between later chambers; rounded periphery in edge view with no evidence of circumperipheral concentration of muricae; aperture interiomarginal, umbilical-extraumbilical, extending to peripheral margin in last chamber. Size: Dimensions of holotype unknown; this is, however, a relatively large form that can exceed 0.5 mm in maximum diameter. |
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Discussion / Comments: | ||||||
Pearson et al. (2006): DISTINGUISHING FEATURES.- This taxon is distinguished by its large and widely open umbilicus and high but variable number (6-8; rarely to 10) of chambers in the last whorl. DISCUSSION.- In comparison to Acarinina pentacamerata, A. aspensis is characterized by an increase in the number of chambers in the final whorl, a more evolute spire and concomitant increase in the width of the umbilicus. This form was originally described from the lower Eocene of Spain, at which time a large number of specimens were illustrated but no holotype designated. Blow (1979, p. 909) designated the specimen illustrated by Colom (1954, pl. 3: fig. 16, reillustrated on P1. 9.4, Fig. I) as a lectotype, perpetuating the taxonomic concept of this form established by Bolli (1957a, p. 167-168, pl. 37, figs. 18a-c). PHYLOGENETIC RELATIONSHIPS.- Bolli (1957b, p. 167) suggested derivation of aspensis from angulosa. Berggren (1964) and Blow (1979) suggested instead that it evolved from pentacamerata, a view which we uphold here. STRATIGRAPHIC RANGE.- Confirmed occurrences only in the lower part of Zone E7. Our studies suggest that aspensis may prove to be a very useful biostratigraphic marker. Some previous authors, since Bolli (1 957b, p. 167) have probably confused aspensis with cuneicamerata and hence suggested a much longer stratigraphic range, into the middle Eocene (see also Berggren 1977, p. 259 and Blow, 1979, p. 91 1). GEOGRAPHIC DISTRIBUTION.- Widespread in (sub)tropical regions of the world; not reliably reported (to our knowledge) from austral or boreal regions. STABLE ISOTOPE PALEOBIOLOGY.- No data available. REPOSITORY.- Lectotype (Blow, 1979, p. 909) reported to be in the personal collection of G. Colom. |
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Systematics: | ||||||
35 Ordo Foraminiferida Superfamilia Globigerinaceae Familia Truncorotaloididae Genus Acarinina Species Acarinina aspensis |
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Synonym list: | ||||||
Pearson et al. (2006): 1954 Globigerina aspensis Colom. - Colom : p.151 pl. 3, fig. 1-35 (flattened forms);
pl. 4, fig. 1-31 (trochoid forms) (No
holotype designated; lectotype, pl. 3: fig. 16 selected by
Blow, 1979:908); [Upper Ypresian - Lower Lutetian, Aspe,
Alicante, Spain.]
1956 Acarinina pentacamerata acceleratoria Khalilov. - Khalilov : p.253 pl. 5; fig. 7a-c [lower Eocene, north-eastern Azerbaidjan]
1957 Globorotalia aspensis Colom. - Bolli : p. 167-168 pl. 37; fig. 18a-c [Lower Eocene Globorotalia palmerae
Zone, Navet Fm., Trinidad]
1961 Globigerina aspensis Colom. - Bermudez : p. 1157-1157 pl. 1; fig. 2a-c [Lower Eocene, Universidad Fm., Havana Province,
Cuba]
1961 Globigerina colomi Bermudez. - Bermudez : p.1167 pl. 2; fig. 6a-c [lower Eocene, Universidad Fm., Cuba]
1965 Acarinina aspensis Colom. - Hillebrandt : p.340 pl. 5; fig. 8, 12, 13 [Lower Eocene G. palmerae Zone, Alicante,
Spain]
1968 Turborotalia? (Acarinina) aspensis Colom. - Samuel & Salaj : p.162 pl. 18; fig. 4 [Eocene, Carpathian Mountains, Slovakia]
1979 Turborotalia (Acarinina) aspensis Colom. - Blow : p. 908-911 pl. 148, fig. 7-9;
pl. 153, fig. 5-6;
pl. 157, fig. 1-6;
pl. 165, fig. 5-6;
pl. 203, fig. 6 [Zones P9-P1 0, Kane 9-C piston core, Endeavour
seamount, North Atlantic Ocean]
1995 Acarinina aspensis Colom. - Lu & Keller : pl. 3; fig. 16-18 [lower Eocene, DSDP Site 577, Shatsky Rise,
northwest Pacific Ocean]
1995 Acarinina aspensis Colom. - Poag & Commeau : pl. 2; fig. 28-29 [lower Eocene, Hammond Core, Maryland]
2006 Acarinina aspensis Colom. - Pearson et al. : p.270 pl. 9.4; fig. 1-16 (Pl. 9.4, Fig. 1 : reillustration of lectotype of
Globigerina aspensis Colom)
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References: | ||||||
Colom,G. (1954): Khalilov,D.M. (1956): Bolli,H.M. (1957): Bermudez,P.J. (1961): Hillebrandt,v.A.. (1965): Samuel,O.. and Salaj,J. (1968): Blow,W.H. (1979): Lu,G. and Keller,G. (1995): Poag,C.W.. and Commeau,J.A.. (1995): Pearson,P.N.; Olsson,R.K.; Hemleben,C.; Huber,B.T. and Berggren,W.A. (2006): |
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Anonymous: Unedited TaxonConcept data | ||||||
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