Porsildia acerviphora, Thomsen & Østergaard, 2015

Thomsen, Helge A. & Østergaard, Jette B., 2015, Coccolithophorids in Polar Waters: Quaternariella and Porsildia gen. nov. Mercedesia gen. nov., Ericiolus,, Acta Protozoologica 54 (3), pp. 155-169 : 166

publication ID

https://doi.org/ 10.4467/16890027AP.15.013.3210

persistent identifier

https://treatment.plazi.org/id/2462E075-FFA7-A666-6521-FF77FA4615EE

treatment provided by

Felipe

scientific name

Porsildia acerviphora
status

sp. nov.

P. acerviphora sp. nov. ( Figs 36–41 View Figs 36–39 View Figs 40–41 )

Diagnosis: With all characteristics of the genus. Up to 10 circumflagellar pole coccoliths. The central process measures 1.7–1.9 µm in length and 0.2–0.3 µm in width. The length of the distal twin pair of elongate elements is 0.5–0.7 µm. Body coccoliths oval (1.0–1.2 × 0.6–0.7 µm) with an irregular outline and a central heap of calcified elements. The rim has an irregular up- per margin and it is asymmetrical; one end bears a distinctly larger, widening and pointed, element of variable shape. The height of the rim is variable within the range 0.2–0.4 µm.

Holotype: Figs 37, 39 View Figs 36–39 (same cell) from Arctic Station , Disko Bay, West Greenland, occurring in a sample from 50 metres depth (34 PSU, 2°C) processed 1 Sep. 1990.

Etymology: from ‘acervus’ (L) pile and ‘phora’ (Gr.) carrying.

The material from West Greenland, comprising only two specimens, is supplemented with material from Svalbard (courtesy of M. Heldal, Univ. of Bergen) collected from the Adventsfjord (June 2012) and the Isfjord (Aug. 2013). The SEM images ( Figs 40–41 View Figs 40–41 ) document the general appearance of the robust central process. The solid and somewhat irregular rim is also evident from both micrographs, as is also the pile of rectangular elements found in the central area of a body coccolith. Numerical data comparing material from West Greenland and Svalbard is provided in Table 4. It is evident that the cells examined, irrespective of geographical origin or times of collection, are basically identical. It is evident from Fig. 41 View Figs 40–41 that the central area heap of calcified elements in body coccoliths shows much diversity with regard to shape and dimensions of the individual elements. Some are square while others are rectangular. Typical dimensions are within the range 0.12–0.23 µm and the thickness of a plate ca. 0.05 µm. The material examined so far does not allow for conclusions with regard to the structure of the central area in the circumflagellar coccoliths .

Porsildia acerviphora is included in this paper because of its Arctic origin and also because its body coccoliths have a structure similar to those found on the heterococcolithophorid species that forms part of the Quaternariella obscura life cycle ( Figs 30–35 View Figs 28–35 ). Shared characteristics are 1) the coccolith wall formed by an irregular mix of square ( Figs 30, 32, 35 View Figs 28–35 , 39 View Figs 36–39 ; arrows), rectangular and pentagonal ( Figs 30, 32, 35 View Figs 28–35 , 39 View Figs 36–39 ; arrowheads) elements, and 2) the occurrence of a central structure of differently sized and shaped elements in the central area of the body coccoliths ( Figs 33, 35 View Figs 28–35 , 39 View Figs 36–39 , 41 View Figs 40–41 ).

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