radiolaria - rads_cenozoic - Drymyomma elegans radiolaria - rads_cenozoic - Drymyomma elegans

Drymyomma elegans


Classification: rads_cenozoic -> Actinommidae -> Actinommidae inc sed -> Drymyomma -> Drymyomma elegans
Sister taxa: D. elegans, D. sp.

Taxonomy

Citation: Drymyomma elegans Jørgensen 1900
Taxonomic rank: species
Basionym: Drymyomma elegans
Synonyms:
1900 Drymyomma elegans - Jørgensen p. 58-59 (not figured)
1905 Drymyomma elegans - Jørgensen pl. 8, figs. 34a-b
1976 Drymyomma elegans - Bjørklund pl. 3, figs. 1-4
1998 Drymyomma elegans - Cortese and Bjørklund pl. 3, figs. 17-19

From Suzuki Paleotax db:

1899 Drymyomma elegans n. sp. Jörgensen p. 58-59
1905 Drymyomma elegans Jorgensen Jörgensen p. 117, pl. 8, fig. 34
1976 Drymyomma elegans Jorgensen Bjørklund pl. 3, figs. 1-4
1998 Drymyomma elegans Jörgensen Cortese & Bjørklund p. 154, pl. 3, figs. 17-19
Taxonomic discussion: Jorgensen 1900 Open nomenclature

Catalog entries: Drymyomma elegans

Original description: Aeussere Kugel dichtwandig, mit ziemlich grossen, breitwandigen Poren, Durchmesser 0,096 mm.
Mittlere Kugel mit viel kleineren, breitwandigen Poren. Durchmesser 0,036 mm. Innerste Kugel ungefähr wie die zweite, nur kleiner Durchmesser 0.015 mm. Ungefähr 20 kräftige, dreischneidige, lang zugespitzte, im Basaltheile breite Hauptstacheln, die etwas ungleich lang sind, bis 0,084 mm. hervorragend. Diese Hauptstacheln sind zwischen den zwei äusseren Kugeln schmäler, erreichen ihre grösste Breite erst an der Aussenseite der dritten Kugel. Die kleinsten Radialstacheln sind häufig mit einem einfachen Ast versehen. Ausserdem finden sich an der äusseren Kugel zahlreiche cylindrische Nebenstacheln, etwas mehr als halb so lang wie die Hauptstacheln, an der Mitte oder höher in 2 bis 4 divergirende Aeste getheilt.

Description


Published descriptions


Jørgensen 1905 - Drymyomma elegans

This species, when fully developed, is very easily recognized by its branched byspines on the outside shell. The outside shell is strongly developed, thick walled, diameter ± 85µ. The pores are roundish with broad intermediate walls, unevenly developed, though not so much so as in Chromyechinus borealis, on an average about the same size or perhaps most of them little smaller. The two inner shells seem in all important respects to answer to those of the following species, Chromyechinus borealis. Still, I must call attention to the fact that I have had very little chance of examining them more thoroughly, as the species occurs so sparsely. The number of the main spines seems to vary (?) from about 15 up to about 20. The largest are beautifully developed, long, slender and always branchless, a few of the smaller ones seem, on the contrary, occasionally to have a single needle shaped side branch, like the corresponding one in Chromyechinus borealis. Of byspines there are some resembling the main spines, only smaller and especially narrower. From these 3-edged spines there seems to be every transition to numerous narrow needle shaped ones without distinct edges. Most of the byspines, especially the narrow ones, carry in their upper halves from 1-4 obliquely diverging narrow branches, some of these again carrying a similar, but shorter, side branch. There seems to be a regular transition from the more delicate radial spines to the more strongly developed, 3-edged and branchless, byspines. It is, however, as above mentioned, probably not quite certain that the previously mentioned Echinomma-forms with long, slender main spines and byspines, should all be included in this species. These forms occur, with us, much more frequently than the fully developed Drymyomma elegans. Rare and scarce, only found at a few places in 1899: Sea off Gaukværö, 19/1, 0-700 m., Senja, 21/1, 0-130 m., the Vest Fiord, 1/2, 0-200 m., Skorven, 4/2, 350-300 m., the Tys Fiord I, 28/3, 0-700 m.

Distribution: Very rare also on the west coast of Norway, only in deep water. Also known from the Norwegian Ocean off Sundmøre and from the Vest Fiord, Feb. 1901 (Cfr. Gran L. 70, p. 150-151).


Biogeography and Palaeobiology

Biostratigraphic distribution

Geological Range:
Last occurrence (top): Extant. Data source: Lazarus et al. 2015 - "R age group"
First occurrence (base): within Quaternary Period (0.00-2.59Ma, base in Gelasian stage). Data source: Lazarus et al. 2015 - "R age group"

Plot of occurrence data:

References:

Bjørklund, K. R. (1976). Radiolaria from the Norwegian Sea, Leg 38 of the Deep Sea Drilling Project. Initial Reports of the Deep Sea Drilling Project. 38: 1101-1168. gs

Cortese, G. & Bjørklund, K. R. (1998b). The taxonomy of boreal Atlantic Ocean Actinommida (Radiolaria). Micropaleontology. 44(2): 149-160. gs

Jørgensen, E (1900). Protophyten und Protozoen im Plankton aus der norwegischen Westkuste. Bergens Museums Aarbog. 1899(6): 51-95. gs O

Jørgensen, E (1905). The protist plankton and diatoms in bottom samples: Radiolaria. In, Nordgaard (ed.) Hydrographical and biological investigation in Norwegian Fjord. 49-151. gs O


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Drymyomma elegans compiled by the radiolaria@mikrotax project team viewed: 21-6-2025

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