Cribrionella ohridana Jovanovska, Cvetkoska, Tofilovska, Ognjanova-Rumenova & Levkov, 2016

Jovanovska, Elena, Cvetkoska, Aleksandra, Tofilovska, Slavica, Ognjanova-Rumenova, Nadja & Levkov, Zlatko, 2016, Description of a new fossil diatom genus, Cribrionella gen. nov. (Bacillariophyta) from Quaternary sediments of Lake Ohrid, Phytotaxa 252 (1), pp. 31-42 : 34

publication ID

https://doi.org/ 10.11646/phytotaxa.252.1.3

DOI

https://doi.org/10.5281/zenodo.13674827

persistent identifier

https://treatment.plazi.org/id/E33BD466-DD7D-FFF1-29DA-0723FF6CED68

treatment provided by

Felipe

scientific name

Cribrionella ohridana Jovanovska, Cvetkoska, Tofilovska, Ognjanova-Rumenova & Levkov
status

sp. nov.

Cribrionella ohridana Jovanovska, Cvetkoska, Tofilovska, Ognjanova-Rumenova & Levkov , sp. nov. ( Figs 2–61 View FIGURES 2–48 View FIGURES 49–54 View FIGURES 55–61 )

Valves circular in shape, 2.0–7.5 μm in diameter ( Figs 2–61 View FIGURES 2–48 View FIGURES 49–54 View FIGURES 55–61 ). Central area flat, variable in size and shape: large circular to small circular-elongate, or absent. From valve exterior, some specimens with ornamented central area, bearing irregularly shaped depressions that do not penetrate valve wall interior ( Figs 50, 54 View FIGURES 49–54 ). Internally, valve central part covered with central lamina, variable in size and shape ( Figs 55, 56 View FIGURES 55–61 ). Valve marginal lamina with submarginal alveoli interrupted with thick and inwardly raised circumferential silica trabeculae (black arrow in Fig. 56 View FIGURES 55–61 ). The submarginal alveoli followed by 2–4 regularly or irregularly arranged areolae. Striae coarse composed of large and round areolae ( Figs 7, 23, 31 View FIGURES 2–48 , 49, 50, 52 View FIGURES 49–54 ). From outside, submarginal alveoli and areolae occluded by cribra ( Figs 49, 51, 52 View FIGURES 49–54 ), surrounded by small cribrate openings slightly depressed into valve surface (white arrow in Fig. 53 View FIGURES 49–54 ). From inside, areolae separated with thick silicified bars (black arrow in Fig. 57 View FIGURES 55–61 ). Internally, each areola crossed by 1 – 2 thick and inwardly raised circumferential silica trabeculae (black arrow in Fig. 58 View FIGURES 55–61 ). Single marginal rimoportula present; externally situated on costa, with relatively wide and round opening (arrow in Fig. 49 View FIGURES 49–54 ). Internally, rimoportula with sessile labium positioned on costa, very close to alveolar opening, in oblique direction (black arrow in Fig. 60 View FIGURES 55–61 ). Marginal fultuportulae on every 4 – 5 costa, with round and simple external opening, positioned on valve-mantle junction ( Figs 50 – 52 View FIGURES 49–54 , black arrow in Fig. 53 View FIGURES 49–54 ). Internally, each marginal fultoportula with short central tube, laterally surrounded by two satellite pores ( Figs 60, 61 View FIGURES 55–61 ). Valve face fultoportulae absent. From outside, ring of small granules present at valve-mantle junction ( Figs 49, 50, 53 View FIGURES 49–54 ). Valvocopula closed, bearing 1 – 3 rows of pores (black arrows in Figs 51 View FIGURES 49–54 , 59 View FIGURES 55–61 ).

Type:— MACEDONIA. Lake Ohrid: site DEEP, core 5045-1, 41° 02’ 57” N, 20° 42’ 54” E, sediment samples from a 185.39 m depth composite core, March–June 2013 (holotype: MKDNC!, circled specimen on slide 009499, specimen illustrated on Fig. 13 View FIGURES 2–48 . Isotype: BRM! ZU10/65).

Etymology:— The specific epithet “ ohridana ” resembles the type locality Lake Ohrid where the species is described from.

Distribution:— Freshwater fossil species observed only from its type locality, the core samples from Lake Ohrid.

BRM

Alfred-Wegener-Institut für Polar- und Meeresforschung

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