Bathycythere vanstraateni Sissingh, 1971
publication ID |
https://doi.org/ 10.26879/497 |
DOI |
https://doi.org/10.5281/zenodo.13314840 |
persistent identifier |
https://treatment.plazi.org/id/177787EF-2A61-6F3E-FF23-B66DFBE9FB92 |
treatment provided by |
Felipe |
scientific name |
Bathycythere vanstraateni Sissingh, 1971 |
status |
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Bathycythere vanstraateni Sissingh, 1971 View in CoL
Figure 6.9 View FIGURE 6. 1
1971 Bathycythere vanstraateni Sissingh , p. 410, pl. 1, 2, figs. 2-4.
1971 Xandarosina n. nudum, Benson and Sylvester-Bradley, p. 68, figs. 3 a, b.
1975 Bathycythere vanstraateni Sissingh ; Breman, p. 213, pl. 4, fig. 20.
1980 Bathycythere vanstraateni Sissingh ; Colalongo and Pasini, p. 52, plate 4, figs. 7, 8.
1983 Bathycythere vanstraateni Sissingh ; Bonaduce et al., p. 463.
1985 Bathycythere vanstraateni Sissingh ; Montcharmont-Zei et al., pl. 1, fig. 7.
1988 Bathycythere vanstraateni Sissingh ; Colalongo and Pasini, p. 283.
1988 Bathycythere vanstraateni Sissing ; van Harten and Droste, p. 732, pl. 1, fig. 1.
1990 Bathycythere vanstraateni Sissingh ; Colalongo et al., p. 483.
1997 Bathycythere vanstraateni Sissingh ; Pasini and Colalongo, p. 18.
2004 Bathycythere vanstraateni Sissingh ; Mazzini, p. 48, figs. 25 K-N.
Remarks. This species is poorly represented in the SML area and is restricted to the Framework Coral facies (FC) and the Hardground fragments colonized by the Solitary Coral facies (SC).
B. vanstraateni is listed among the abyssal ostracods living in the Atlantic Ocean, and Pasini and Colalongo (1997) considered it as a psychrospheric species. It seems to be extinct in the Recent Mediterranean, from where it has been recorded from depths shallower than the SML ones ( van Harten, 1990).
Breman (1975) found this species in sediments from the Adriatic Sea dated to the basal Holocene including the AllerØd and the Younger Dryas climatic stages. van Harten and Droste (1988) stated that this species disappeared from the eastern Mediterranean about 9 Ka ago together with K. monosteracensis and M. adriatica , following an anoxic event related to sapropel deposition. A comparable distribution can be desumed from Colalongo et al. (1990, figure 3) for cores from the Tyrrhenian Sea.
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