The problem that confronted Helen Coxall of Stockholm University and her international team was deceptively simple but had festered for five decades. Two distinct spinose morphotypes occur in central Arctic cores at different stratigraphic levels. The younger, shallower horizons, potentially including the Last Interglacial around 120,000 years ago, contain a small form generally assigned to Turborotalita quinqueloba, a well-known subpolar species that today thrives along the sea-ice edge of the Nordic Seas. The deeper, older horizons contain a larger, more loosely coiled form that has been variously called Globigerina exumbilicata or Turborotalita egelida. Without a reliable taxonomic framework, researchers could not confidently correlate these bioevents between cores, let alone interpret what they meant for past climate. Compounding the confusion, the name egelida was virtually unknown to most foraminifera specialists and had never appeared in the last great taxonomic synthesis of Neogene and Quaternary planktonic foraminifera.

To resolve the mess, the team combined classical micropalaeontology with modern quantitative rigor. They imaged hundreds of specimens using both light microscopy and high-resolution scanning electron microscopy, drawing on sediment cores spanning the Eurasian and Amerasian basins as well as living plankton collected south of Iceland during a 2002 research cruise. Crucially, they also tracked down and imaged, many for the first time, the original type specimens housed in the Smithsonian’s Cushman Collection, including the holotypes of exumbilicata, egelida and quinqueloba itself. Around 300 individuals from each of three key populations were measured for traits including maximum test diameter, proloculus size, final chamber dimensions and apertural lip thickness, then subjected to multivariate analysis of variance and linear discriminant analysis.

The statistics delivered a verdict with unusual clarity for microfossil work. The three populations occupy significantly different regions of morphospace, with a Pillai’s Trace statistic of 1.18 and a p-value below 0.001. Leave-one-out cross-validation of the discriminant model achieved an overall classification accuracy of nearly 89 percent, and the younger Arctic morphotype was correctly assigned in 98.3 percent of cases. The first discriminant axis, explaining just over 70 percent of between-group variance, was driven mainly by final chamber geometry and overall shell size, while the second axis was dominated by proloculus diameter, the size of the tiny initial chamber around which the whole shell is built.

On this evidence, the team confirmed that the younger Arctic invader is indeed Turborotalita quinqueloba, but with a twist. The central Arctic specimens are true dwarfs, averaging just 114 micrometres across compared with 190 micrometres for their Nordic Sea cousins, and they lack the thick gametogenic calcite crust that characterises sedimented shells from the subpolar North Atlantic. Yet their proloculus sizes are almost identical to those of classic quinqueloba, and they retain the species’ diagnostic tear-drop-shaped final chamber that overhangs the umbilicus. The researchers interpret the size difference as an environmental response, a dwarfing effect seen before in polar populations near the species’ modern northern limit, rather than evidence of a separate species. In other words, when conditions briefly warmed enough, quinqueloba pushed into the central Arctic and shrank under the stress.

The older morphotype is a different story altogether. It builds larger shells, averages fewer chambers, coils more loosely to leave a wide open umbilicus, and sports a globular final chamber that never overhangs the aperture. Its proloculus is strikingly larger, averaging nearly 22 micrometres against roughly 14 in both quinqueloba populations, and its wall texture is unique: broad, flat spine bases and, in spiral view, rows of pustules aligned into costellae-like radiating ridges, a feature never observed in Turborotalita. The team concludes that this form deserves recognition as a distinct morphospecies, and likely a distinct biological taxon, rather than a growth stage or ecophenotypic variant of quinqueloba.

Then comes the taxonomic detective work that gives the study its bite. The name egelida, coined by Richard Cifelli and R. K. Smith in 1970 from living plankton netted in the North Atlantic, turns out to rest on immature specimens. The team’s own genetically confirmed, living quinqueloba pumped from Icelandic waters lack the elongate final chamber that develops only at full maturity, and they look almost exactly like Cifelli and Smith’s egelida type material. Since the Arctic fossils are mature, sedimented shells, egelida cannot be the right name. Instead, the authors reinstate Globigerina exumbilicata, established by the pioneering Arctic oceanographer Yvonne Herman in 1974 from Alpha Ridge cores, whose holotype they imaged for the first time. Lacking the defining ampullate final chamber of Turborotalita, the species is provisionally placed in the genus Globigerina, with the generic name held in quotation marks to signal uncertainty.

The study also exposes a long-running case of mistaken identity with implications for anyone counting foraminifera under a light microscope. A smooth-walled, shiny, five-chambered morphotype of the polar species N. pachyderma, known as Nps-5, can look remarkably like small quinqueloba or even exumbilicata. Herman herself conflated this form with egelida in Baffin Bay plankton samples in the 1980s, an error the new SEM imagery decisively corrects: Nps-5’s walls bear solid, irregularly distributed pustules with no spine holes, whereas true spinose taxa show distinctive spine bases with central cavities. The authors argue that scanning electron microscopy should be treated as primary data in foraminiferal taxonomy, because the characters that define species often emerge only in the final stages of life.

Perhaps the most tantalising implication concerns timing. The latest biostratigraphic constraints, anchored by the last occurrence of the nannofossil Pseudoemiliania lacunosa around 440,000 years ago and dinoflagellate cyst events older than 1.8 million years, place the exumbilicata acme somewhere in the early to middle Pleistocene, not in the MIS 11 interglacial to which it had long been assigned. If the Globigerina affiliation holds, this would mean a member of the Globigerina lineage attempted to colonise the polar Arctic before N. pachyderma achieved its ecological dominance, an experiment in polar occupation that modern Globigerina bulloides, confined today to the southern Arctic gateways, has never repeated. The exumbilicata zone also appears to mark a pivotal transition from agglutinated to calcareous-dominated assemblages across the entire central Arctic.

Why does this matter beyond the world of shell taxonomy? Because these tiny fossils are among the few direct archives of past Arctic Ocean conditions, and their abundance peaks are used as markers of warm, seasonally ice-free intervals that may be analogues for where today’s rapidly warming Arctic is heading. A consistent taxonomic framework means cores from the Amerasian and Eurasian basins can finally be correlated on common ground, and paleoenvironmental reconstructions can be built on solid species definitions rather than a tangle of synonyms and misidentifications. After half a century of confusion, the ghost invaders of the Arctic now have names, and with names comes the ability to tell their story properly, one chamber at a time.

Subject of Research: Taxonomic revision of Quaternary subpolar spinose planktonic foraminifera from the central Arctic Ocean

Article Title: Quaternary Arctic planktonic foraminifera: morphological differentiation and taxonomic reassessment of subpolar spinose taxa

Article References: Coxall, H. K., Cronin, T. M., Darling, K., Husum, K., Handl, T., Huber, B. T., Kanvinde, M. M., Razmjooei, M., Vermassen, F., Voelker, A. H. L., Weitkamp, T. M., & O'Regan, M. (2026). Quaternary Arctic planktonic foraminifera: morphological differentiation and taxonomic reassessment of subpolar spinose taxa. Journal of Micropalaeontology, 45(2), 581-622. https://doi.org/10.5194/jm-45-581-2026

Image Credits: AI Generated

DOI: 10.5194/jm-45-581-2026

Keywords: planktonic foraminifera, Arctic Ocean, Quaternary, paleoceanography, taxonomy, Turborotalita quinqueloba, Globigerina exumbilicata, sea ice, morphometrics, scanning electron microscopy, Pleistocene, micropalaeontology