pforams@mikrotax - Trilobatus sacculifer

Citation: Trilobatus sacculifer (Brady, 1877)

Basionym: Globigerina sacculifera

Variants:

Globigerinoides quadrilobatus (d'Orbigny 1846); [according to SCOR-WG138, André et al. 2013]
Globigerinoides immaturus LeRoy 1939 [according to SCOR-WG138, André et al. 2013]
Globigernoides trilobus (Reuss 1850) [according to SCOR-WG138, André et al. 2013]
Globigerinoides suleki Bermudez (1961)

Molecular genetic data indicates that these morphotypes are conspecific (André et al. 2013)

Taxonomic discussion:

In Kennett & Srinivasan (1983) Gs. trilobus, Gs. immaturus and Gs. quadrilobatus were primarily distinguished from Gs. sacculifer by absence of the elongate sack-like final chamber. Gs. quadrilobatus was distinguished from Gs. immaturus by having a high aperture and a lower rate of chamber expansion. Gs. trilobus has only 3 chambers in the final whorl. These four morphotypes all occur from the Early Miocene to the present day (e.g. Kennett & Srinivasan 1983) and they have been shown to be conspecific in the modern plankton (André et al. 2013). They are, however, used by palaeontologists including Spezzaferri et al. (2018) since they have different straigraphic ranges. [editor's comment - JRY 2018]

Poole & Wade (2019) provide extensive documentation of morphological vararion within this group.

Distinguishing features:
Parent taxon (Trilobatus): Supplementary apertures and cancellate wall.
This taxon: Low trochospiral, chambers spherical except final one which is sack-like

Description

Wall type: Spinose; Cancellate [Aze 2011]

Morphology: Test low trochospiral, chambers spherical except the final one, which is [often] elongate, sack like; three and a half to four in the final whorl, increasing slowly in size as added. The last chamber may be rather small, or it may be elongate and lobulate. Sutures on both sides slightly curved and depressed; surface with regular subhexagonal pore pits; umbilicus narrow, primary aperture interio-marginal, umbilical, a distinct arch bordered by a rim; prominent supplementary apertures on spiral side.

Biogeography and Palaeobiology

Geographic distribution: Low latitudes [Aze et al. 2011, based on Kennett & Srinivasan (1983)]

In modern oceans an abundant, warm water, species [SCOR WG138]

Isotope paleobiology: Aze et al. 2011 ecogroup 1 - Open ocean mixed-layer tropical/subtropical, with symbionts. Based on very heavy ∂¹³C and relatively light ∂¹⁸O Cited sources (Aze et al. 2011 appendix S3): Keller (1985); D. R. M. Stewart unpublished data

Phylogenetic relations: Molecular Genotypes recognised (data from PFR² database, June 2017. References: André et al. 2013 ; Darling et al. 1997; Ujiié & Lipps 2009; Seears et al. 2012).

Globigerinoides sacculifer (83 sequences)
Globigerinoides sacculifer I (98 sequences)

The species shows remarkably low genetic differentiation in comparison to most other common planktonic foraminifera and what differentiation there is shows no relation to test morphology (André et al. 2013).

Biostratigraphic distribution

Geological Range:
Last occurrence (top): Extant Data source: present in the plankton (SCOR WG138)
First occurrence (base): within N6 zone (17.54-17.59Ma, base in Burdigalian stage). Data source: Kennett & Srinivasan 1983 - this is range excluding triloba as a synonym

References:

André, A., Weiner, A., Quillévéré, F., Aurhas, R., Morard, R. & Douady, C. (2013). The cryptic and the apparent reversed: lack of genetic differentiation within the morphologically diverse plexus of the planktonic fora-minifer Globigerinoides sacculifer. Paleobiology. 39: 21-39. gs

Aze, T. et al. (2011). A phylogeny of Cenozoic macroperforate planktonic foraminifera from fossil data. Biological Reviews. 86: 900-927. gs

Bermudez, P. J. (1961). Contribucion al estudio de las Globigerinidea de la region Caribe-Antillana (Paleoceno-Reciente). Editorial Sucre, Caracas. 1119-1393. gs

Brady, H. B. (1877). Supplementary note on the foraminifera of the Chalk (?) of the New Britain group. Geological Magazine. 4(12): 534-536. gs

d'Orbigny, A. (1846). Foraminiferes fossiles du bassin tertiaire de Vienne (Austriche). Gide et Companie, Paris. 1-312. gs

Darling, K. F., Wade, C. M., Kroon, D. & Brown, A. J. L. (1997). Planktic foraminiferal molecular evolution and their polyphyletic origins from benthic taxa. Marine Micropaleontology. 30: 251-266. gs

Keller, G. (1985). Depth stratification of planktonic foraminifers in the Miocene Ocean. In, Kennett, J. P. (ed.) The Miocene Ocean: Paleoceanography and Biogeography. GSA Memoir. 163: 1-337. gs

Kennett, J. P. & Srinivasan, M. S. (1983). Neogene Planktonic Foraminifera. Hutchinson Ross Publishing Co., Stroudsburg, Pennsylvania. 1-265. gs

Lam, A. & Leckie, R. M. (2020a). Late Neogene and Quaternary diversity and taxonomy of subtropical to temperate planktic foraminifera across the Kuroshio Current Extension, northwest Pacific Ocean. Micropaleontology. 66(3): 177-268. gs

LeRoy, L. W. (1939). Some small foraminifera ostracoda and otoliths from the Neogene (Miocene) of the Rokan-Tapanoeli area, central Sumatra,. Natuurk. Tijdschr. Nederl.-Indie. 99(6): 215-296. gs

Loeblich, A. & Tappan, H. (1994). Foraminifera of the Sahul shelf and Timor Sea. Cushman Foundation for Foraminiferal Research, Special Publication. 31: 1-661. gs V O

Norris, R. D. (1998). Planktonic foraminifer biostratigraphy: Eastern Equatorial Atlantic. Proceedings of the Ocean Drilling Program, Scientific Results. 159: 445-479. gs V O

Poole, C. R. & Wade, B. S. (2019). Systematic taxonomy of the Trilobatus sacculifer plexus and descendant Globigerinoidesella fistulosa (planktonic foraminifera). Journal of Systematic Palaeontology. 1-42. gs

Postuma, J. A. (1971). Manual of planktonic foraminifera. Elsevier for Shell Group, The Hague. 1-406. gs

Seears, H. A., Darling, K. F. & Wade, C. M. (2012). Ecological partitioning and diversity in tropical planktonic foraminifera. BMC Evolutionary Biology. 12(54): 1-15. gs V O

Siccha, M. & Kucera, M. (2017). ForCenS, a curated database of planktonic foraminifera census counts in marine surface sediment samples. Scientific Data. 4(1): 1-12. gs

Spezzaferri, S. et al. (2015). Fossil and genetic evidence for the polyphyletic nature of the planktonic foraminifera "Globigerinoides", and description of the new genus Trilobatus. PLoS One. 1-20. gs V O

Ujiié, Y. & Lipps, J. H. (2009). Cryptic diversity in planktonic foraminifera in the northwest Pacific ocean. Journal of Foraminiferal Research. 39: 145-154. gs

test outline:	Lobate	chamber arrangement:	Trochospiral	edge view:	Equally biconvex	aperture:	Umbilical
sp chamber shape:	Globular	coiling axis:	Low-moderate	periphery:	N/A	aperture border:	Thin lip
umb chbr shape:	Globular	umbilicus:	Wide	periph margin shape:	Narrowly rounded	accessory apertures:	Sutural
spiral sutures:	Moderately depressed	umb depth:	Deep	wall texture:	Cancellate	shell porosity:	Macroperforate: >2.5µm
umbilical or test sutures:	Strongly depressed	final-whorl chambers:	3.5-4.0	N.B. These characters are used for advanced search. N/A - not applicable

Trilobatus sacculifer

Taxonomy

Description

Biogeography and Palaeobiology

Biostratigraphic distribution

References:

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