Acetabularia moldavica, Barattolo & Ionesi & Ţibuleac, 2019
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publication ID |
https://doi.org/ 10.4202/app.00537.2018 |
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DOI |
https://doi.org/10.5281/zenodo.10626624 |
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persistent identifier |
https://treatment.plazi.org/id/03D62622-D148-FFB2-FC97-DE70FC7FF90E |
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treatment provided by |
Felipe |
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scientific name |
Acetabularia moldavica |
| status |
sp. nov. |
Acetabularia moldavica sp. nov.
Figs. 4–8 View Fig View Fig View Fig View Fig View Fig .
Etymology: From the Moldova Region.
Type material: Holotype: fertile cap ( Fig. 4F View Fig ), MP-UAIC 8228/ PD.1 . Paratypes: specimens contained on the surfaces of five thin marl layers, MP-UAIC 8228/ PD .1–5.
Type locality: The outcrop is located 2.5 km WSW from Pătrăuţi village (Suceava County) along the Bradul stream incision, at 411 m asl, coordinates 47°43’12” N, 26°09’53” E ( Fig. 2B View Fig ) GoogleMaps .
Type horizon: A clay seam, about 40 cm thick, within a sequence of sand and sandstone beds, twenty metres above the horizon Pătrăuţi I ( Fig. 2 View Fig ); Sarmatian (middle Miocene) .
Diagnosis.— Discs made of 10–24 mucronate fertile rays with evidence of both corona superior and inferior. Each ray, quite flat in transverse section, contains 14–35 mineralized gametangia (cysts). The mineralized cyst layer, 20–25 μm thick, is made of fibrous aragonite crystals set perpendicular to the wall surface. A delicate extracellular calcareous layer sometimes envelopes the fertile rays ( Table 1 View Table 1 ).
Description. —General features of the calcareous skeleton: The alga is known only by its fertile caps ( Figs. 4–7 View Fig View Fig View Fig View Fig ). No trace possibly related to the stem has been found on the rock surface. The fertile disks are slightly concave, the central upper part being sunken ( Fig. 4A, D, G View Fig ) while the lower part is protruding ( Fig. 4E, F View Fig ). Some thin extracellular mineralized layers envelope the basal part (primary lateral), superior and inferior coronae, and the space between the fertile rays ( Fig. 5D, E View Fig ). Occasionally a delicate extracellular sheet covers the upper and lower sides of the disk, and a thin radial rib marks the boundary between gametophores ( Figs. 5B View Fig , 6B View Fig ).
Primary laterals, upper and lower corona: According to level at which the structure is broken and the side exposed, it is possible to observe the mineralized walls and cavities belonging to corona superior and inferior ( Fig. 5C, D View Fig ). The coronal structure of Fig. 7B View Fig 1 View Fig (fragment of a cap in upper view), is probably broken at the basal part (primary lateral) level, and therefore prominences (arrows) correspond to mineralized walls among the basal parts (furrows). The pore in each furrow connects the basal part with the corona inferior below.
Fertile rays (gametophores): The gametophore develops beyond the basal part, and is about 1.2–3.2 mm long and 0.5–1.0 mm wide distally. The outer end is pointed (mucronate; Fig. 4A–G View Fig ), but this character decreases as size increases ( Fig. 5A View Fig 1 View Fig ) and is not evident in Figs. 5B View Fig , 6B View Fig . The transverse distal sections are elliptical in small sized specimens and rectangular in large ones, both are arranged horizontally. A cap contains 10–24 gametophores.
Gametangia (cysts): Fertile rays are estimated to contain 14–35 mineralized gametangia (cysts), closely packed so that their outlines are roughly polygonal to quadrangular. Cysts are usually bound together at the cyst-cyst contact ( Fig. 7C– E View Fig ). The spaces between cysts appear to be uncalcified ( Fig. 7A View Fig ), but very occasionally micro-spherulitic crystal aggregates have been observed under SEM ( Fig. 8 View Fig ). Mineralized cysts are 0.26–0.38 mm in diameter. The wall is 20–25 μm thick, fibrous, made by acicular crystals arranged orthogonal to the wall surface (seemingly original aragonite). Each gametangium has a circular opening, 50 μm wide, closed by a mineralized lid, that is commonly lost.
Reconstruction of the thallus: Figure 9 View Fig depicts the possible appearance of the alga in axial ( Fig. 9A, B View Fig ) and apical view ( Fig. 9C View Fig ). Extracellular mineralization is drawn in black, and the intracellular mineralized cyst wall is dark gray ( Fig. 9A, B View Fig ). Cyst structure is shown in Fig. 10A View Fig .
Comparisons.— Acetabularia moldavica sp. nov. differs from all other fossil Acetabularia species by the presence of mineralized gametangia. Moreover, the number of fertile rays in a cap is very low (10–24), whereas it is much higher in A. miocenica (90–100), A. chiavonica (78), and A. transylvana (90–100).
Remarks.— The sediments of Moldavian Platform represent lacustrine environments evolving into peat bog facies (observed to alternate cyclically), while being connected to the Carpathian Orogen by temporary land bridges ( Ionesi et al. 1993; Ţibuleac 1999; Ionesi 2006).
On the contrary, there is no consensus regarding reverse brackish-marine evolution, despite its being reported within the Moldavian Platform (Ţibuleac 1999; Ionesi 2006).
Dasycladaceans are euryhaline organisms and prefer shallow water conditions ranging from mangrove swamps to coral reefs environments ( Valet 1979). The pelitic facies containing A. moldavica sp. nov. suggests a soft substrate and in-situ fossilisation. The alga probably populated environments equivalent to a mangrove swamp. Acetabulariaceans quoted by Génot et al. (2002) probably required marine conditions.
Stratigraphic and geographic range.— Type locality and horizon only.
| PD |
Dutch Plant Protection Service, Culture Collection of Plant Pathogenic Bacteria |
| A |
Harvard University - Arnold Arboretum |
| I |
"Alexandru Ioan Cuza" University |
No known copyright restrictions apply. See Agosti, D., Egloff, W., 2009. Taxonomic information exchange and copyright: the Plazi approach. BMC Research Notes 2009, 2:53 for further explanation.
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