The first appearance of this species marks the base of the lower Miocene G. woodi Zone in Australia and New Zealand, although Spezzaferri (1994) documented a few specimens of G. connecta in DSDP Holes 588C and 593 (Tasman Sea) from the upper Zone P22 (= Zone O7). Spezzaferri (1994) also recorded some specimens of G. connecta from Zone P22 at high latitudes in the North Atlantic Ocean. Jenkins (1964) identified Globoturborotalita woodi as the ancestor of G. connecta and the evolution to be synchronous in New Zealand and southeast Australia. [Spezzaferri et al. 2018]
Catalog entries: Globigerina woodi connecta
Type images:Distinguishing features:
Parent taxon (Globoturborotalita): Trochospiral test with a single, large, open umbilical aperture. Cancellate wall. 4-4½ chambers in final whorl
This taxon: Like G. woodi but compact test and more highly arched aperture
Morphology:
Wall type:
Character matrix
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: | Broadly rounded | accessory apertures: | None |
spiral sutures: | Weakly depressed | umb depth: | Deep | wall texture: | Cancellate | shell porosity: | Macroperforate: >2.5µm |
umbilical or test sutures: | Moderately depressed | final-whorl chambers: | 3-3.5 | N.B. These characters are used for advanced search. N/A - not applicable |
Geographic distribution
Isotope paleobiology
Phylogenetic relations
G. connecta differs from G. woodi in having a compact test and a more highly arched aperture. Morphologically transitional forms connecting these two species occur within the range of G. connecta. G. connecta evolved from G. woodi in the Gg. dehiscens Zone (Early Miocene) and is the immediate ancestor of Globigerinoides triloba. [Kennett & Srinivasan 1983]
Most likely ancestor: Globoturborotalita woodi - at confidence level 4 (out of 5). Data source: Kennett & Srinivasan 1983, fig.8; Aze et al. 2011; Spezzaferri et al. 2018.
Geological Range:
Notes: Zone O7 (Spezzaferri, 1994) to Zone M4, i.e., lower Miocene Globigerinoides trilobus Zone of Jenkins (1985). [Spezzaferri et al. 2018]
Last occurrence (top): within M4 zone (16.38-17.54Ma, top in Burdigalian stage). Data source: Spezzaferri et al. 2018
First occurrence (base): within O7 zone (22.96-25.21Ma, base in Chattian stage). Data source: Spezzaferri et al. 2018
Plot of occurrence data:
Primary source for this page: Spezzaferri et al. 2018 - Olig Atlas chap.8 p.240; Kennett & Srinivasan 1983, p.44
Aze, T. et al. (2011). A phylogeny of Cenozoic macroperforate planktonic foraminifera from fossil data. Biological Reviews. 86: 900-927. gs Basov, I. A., Ciesielski, P. F., Krasheninnikov, V. A., Weaver, F. M. & Wise, S. W. (1983). Biostratigraphic and paleontologic synthesis: Deep Sea Drilling Project Leg 71, Falkland Plateau and Argentine Basin. Initial Reports of the Deep Sea Drilling Project. 71: 445-460. gs Chaisson, W. P. & Leckie, R. M. (1993). High-resolution Neogene planktonic foraminifer biostratigraphy of Site 806, Ontong Java Plateau (Western Equatorial Pacific). Proceedings of the Ocean Drilling Program, Scientific Results. 130: 137-178. gs Chaproniere, G. C. H. (1988). Globigerina woodi from the late Oligocene and early Miocene of southeastern Australia. Journal of Foraminiferal Research. 18: 105-115. gs Jenkins, D. G. (1960). Planktonic foraminifera from the Lakes Entrance oil shaft, Victoria, Australia. Micropaleontology. 6: 345-371. gs Jenkins, D. G. (1964). A new planktonic foraminiferal subspecies from the Australasian Lower Miocene. Micropaleontology. 10(1): 72-. gs Jenkins, D. G. (1971). New Zealand Cenozoic Planktonic Foraminifera. New Zealand Geological Survey, Paleontological Bulletin. 42: 1-278. gs Jenkins, D. G. (1978). Guembelitria samwelli Jenkins, a new species from the Oligocene of the Southern Hemishere. Journal of Foraminiferal Research. 8(2): 132-137. gs Jenkins, D. G. (1985). Southern mid-latitude Paleocene to Holocene planktic foraminifera. In, Bolli, H. M., Saunders, J. B. & Perch-Nielsen, K. (eds) Plankton Stratigraphy. Cambridge University Press, Cambridge 263-282. gs Kennett, J. P. & Srinivasan, M. S. (1983). Neogene Planktonic Foraminifera. Hutchinson Ross Publishing Co., Stroudsburg, Pennsylvania. 1-265. gs Li, Q. & McGowran, B. (2000). Miocene foraminifera from Lakes Entrance Oil Shaft, Gippsland, southeastern Australia. Association of Australasian Palaeontologists, Memoirs. 22: 1-142. gs Pearson, P. N., Premec-Fucek, V. & Premoli Silva, I. (2006b). Taxonomy, biostratigraphy, and phylogeny of Eocene Turborotalia. 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 15): 433-460. gs O Spezzaferri, S. (1994). Planktonic foraminiferal biostratigraphy and taxonomy of the Oligocene and lower Miocene in the oceanic record. An overview. Palaeontographia Italica. 81: 1-187. gs Spezzaferri, S., Olsson, R. K., Hemleben, C., Wade, B. S. & Coxall, H. K. (2018d). Taxonomy, biostratigraphy, and phylogeny of Oligocene and Lower Miocene Globoturborotalita. In, Wade, B. S., Olsson, R. K., Pearson, P. N., Huber, B. T. & Berggren, W. A. (eds) Atlas of Oligocene Planktonic Foraminifera. Cushman Foundation for Foraminiferal Research, Special Publication . 46(Chap 8): 231-268. gs References:
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Globoturborotalita connecta compiled by the pforams@mikrotax project team viewed: 8-12-2023
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