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Parvodinium elpatiewskyi Ostenfeld) Kretschmann et al 2019

Previous name used: Peridiniopsis elpatiewskyi (Ostenfeld) Bourrelly 1968

Phylum
Dinoflagellata
Class
Dinophyceae
Order
Peridiniales
Habitat
plankton, pelagial
Distinctive features
Co-occurs with P. cunningtonii
Organization
flagellated single cells
Color
yellow to golden-brown
Cell shape
prolate spheroid
Cell diameter (D)
21 - 30 µm, median: 26 µm (N=>2000)
Cell length (L)
28 – 37 µm, median: 32.5 µm (N=700)
Cell biovolume
6600 - 17500 µm³, median: 11500 µm³.
Biovolume equation
V, µm³ = 1.2514 D²·⁷⁹³ (regression eqn. based on >500 measurements of both D and L with V computed for a prolate sphaeroid).

Morphological features

Cells are pentangular (having 5 sides) or ovoid in shape and slightly flattened dorsi-ventrally. The epitheca is conical, with a “mouth” shaped apex (uppermost end) and is larger than the hypotheca, which is rounded but excavated on the antapex (base, opposite to the apex). The cingulum encircles the cell; the sulcus widens along the hypotheca. Several spines or teeth-like projections are present on the hypotheca, typically some of them are lined up as in a brush (Plate 1). The chloroplasts are numerous and discoid. A red body is occasionally seen (Plate 1). SEM shows that the plates are concave and ornamented by rows of fine punctae, and that the sulcus extends all the way to the concave base of the hypotheca. The resting cysts (not shown) are somewhat oval with a thick cell wall, 36 µm x 28 µm. Parvodinium elpatiewskyi is similar to P. cunningtonii in size and shape, and they tend to co-occur. See here our tips for distinguishing between these two species under the light microscope.
Parvodinium elpatiewskyi Ostenfeld) Kretschmann et al 2019 — plate 1 (from source)
Plate 1: Parvodinium elpatiewskyi from Lake Kinneret. The light microscope photos (a-c) show concave base, with a line of horns on one side, distinct cingulum, red bodies, rounded epitheca with a mouth-shaped apex. The SEM photos (d-f) show that the plates are concave, ornamented by rows of fine punctae, and that the sulcus extends all the way to the concave base of the hypotheca. Light microscope photos: Alla Alster; SEM photos: Barbara Hickel.

Ecology

Parvodinium elpatiewskyi is one of the common algal species in the Kinneret plankton, present in the water at all times of the year. In the absence of Peridinium gatunense in recent years, Parvodinium elpatiewskyi seems to be more abundant than in Peridinium bloom years, although 1999 was an exception (Fig. 1). It always occurs with a second species of the same genus - Parvodinium cunningtonii (Figs. 1, 2). Its abundance has a typical annual cycle with with a peak between April and June (Fig. 3). Cell size also fluctuates seasonally, being smaller in summer, larger in winter (Fig. 3). Peak cell size (February-March) precedes peak abundance by 2-3 months. These seasonal cycles are shared with Parvodinium cunningtonii and Peridiniopsis borgei. The multiannual average contribution of this dinoflagellate to total phytoplankton biomass is 3%. Its maximum biomass ever recorded was 53 g m⁻² - 41% of total biomass, in April 2006, a “no-Peridinium” year.

Environmental conditions

Parvodinium elpatiewskyi> 5 g m⁻² or > 25 cells mL⁻¹ occurred more frequently but not exclusively at calcium concentrations > 45 mg L⁻¹, pH > 8.5, dissolved oxygen > 10 mg L⁻¹, showing greater abundance at low NH₄ and TDP, wide range of DON (Fig. 4). Furthermore (not shown), the higher biomasses usually occur at chloride > 230 mg L⁻¹, conductivity > 1050 µS cm⁻¹, alkalinity > 115 mg CaCO₃ L⁻¹, at a relatively narrow range of long wave radiation (300-370 Watt m⁻²), but over the full range of short-wave radiation (100-350 Watt m⁻²) and water temperatures (14-30 °C), when the lake is stratified. Cell size declines with increasing temperature, especially at temperatures below 23C, and increases with calcium and alkalinity (Fig. 5).

Additional figures

Figure 1. Time series of the abundance (cells/mL) of three dinoflagellates: Parvodinium elpatiewskyi, Parvodinium cunningtonii, and Peridinium gatunense, showing that the two Parvodinium species tend to co-occur and that the abundance of both has greatly increased since the mid 1990s, when Peridinium gatunense no longer blooms each year.
Figure 2. Regression of Parvodinium cunningtoni abundance vs. Parvodinium elpatiewsky abundance.
Figure 3. The seasonal pattern of water column cell abundance (left) and volume per cell (right) of Parvodinium elpatiewskyi.
Figure 4. P. elpatiewskyi abundance (cells mL⁻¹) vs. selected environmental parameters recorded at the site and time of sampling, showing greater abundance at: low NH₄ and TDP; wide range of DON; and higher pH, DO and calcium levels.
Figure 5. P. elpatiewskyi cell size (mm³) vs. environmental parameters recorded at the site and time of sampling. Data for 2006-2020.

Cite this record as: Tamar Zohary, Alla Alster. 7 May 2026. Electronic publication. Israel Oceanographic & Limnological Research. https://kinneret-algae-atlas.org/ Searched on —.

Further reading

  1. Hansen G, Flaim G. 2007. Dinoflagellates of the Trentino Province, Italy. J Limnol. 66:107-141.

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