Cytheropteron testudo Sars, 1869

Sciuto, F & Rosso, M, 2015, Bathyal ostracods from the Santa Maria di Leuca deep-water coral province (northern Ionian Sea), Palaeontologia Electronica 8 (9), pp. 1-17 : 9

publication ID

https://doi.org/ 10.26879/497

DOI

https://doi.org/10.5281/zenodo.13314830

persistent identifier

https://treatment.plazi.org/id/177787EF-2A60-6F3F-FC78-B2E2FBFEF8D2

treatment provided by

Felipe

scientific name

Cytheropteron testudo Sars, 1869
status

 

Cytheropteron testudo Sars, 1869 View in CoL

Figure 6.11 View FIGURE 6. 1

1869 Cytheropteron testudo Sars , p.173, pl. 173, fig. 1.

1889 Cytheropteron testudo Sars ; Brady and Norman, p. 219, pl. 21, figs. 1, 2.

1985 Cytheropteron testudo Sars ; Montcharmont-Zei et al., p. 30, pl. 1, fig. 6.

1999 Cytheropteron testudo Sars ; Swanson and Ayress, p. 157, pl. 4, figs. 1-12, pl. 5, figs.1-13, pl. 6, figs. 10-12.

2003 Cytheropteron testudo Sars ; Stepanova et al., p. 31, pl. 11, figs. 5, 6.

2011 Cytheropteron testudo Sars ; Faranda and Gliozzi, p. 82, fig. 12.

2012 Cytheropteron testudo Sars ; Sciuto, p. 122, fig. 3a.

Remarks. C. testudo Sars, 1869 is presently restricted to the area between the Norwegian coasts and the Arctic bioprovince. Consequently, it is considered as one of the northern guests widespread in the Mediterranean during the Quaternary ( Faranda and Gliozzi, 2011). This species has been found in western Laptev Sea, at 68 m water depth by Stepanova et al. (2003); along the Norwegian coast, at depths of 80 to 240 m, and in the Recent Atlantic, between 1380 and 3526 m water depth by Dingle and Lord (1990); in the Queensland Plateau (SW Pacific) in Holocene to Recent sediments deeper than 500 m by Swanson and Ayress (1999). As fossils, the species has been reported from the Early Pliocene to the Quaternary from bathyal sediments of the Atlantic Ocean ( Whatley and Coles, 1987) and from to Early Pleistocene in bathyal sediments of the Mount S. Nicola section ( Aiello et al., 2000). In the Mediterranean Sea its last occurrence corresponds to the Last Glacial (Montcharmont-Zei et al., 1985). Therefore C. testudo could be considered as a stenothermic species restricted to very cold waters independently of depth.

This species was found only in the Framework Corals facies (CF).

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