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Phylum Arthropoda
Subphylum Crustacea
Class Ostracoda
Order Halocyprida
Family Thaumatocyprididae
Danielopolina bahamensis Kornicker & Iliffe, 1989
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Danielopolina bahamensis: after Kornicker & Iliffe, 1989 |
Taxonomic Characterization: Carapace without surface spines. Each
lamella of furca with 3 short fused claws. Each valve without a single
posterodorsal process. Walls of surface reticulations formed by ridges. Second
joint of first antenna without bristles (Kornicker and Iliffe, 1989).
Disposition of Specimens: National Museum of Natural History, Smithsonian
Institution, catalog numbers USNM 193285-8.
Ecological Classification: Stygobitic
Size: Adult female carapace is 0.41 mm; adult male is 0.43 mm.
Number of Species in Genus: Eleven (ten anchialine stygobitic, one deep
sea)
Genus Range:
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Species Range: Known only from Hatchet Bay Cave, Hatchet Bay, Eleuthera
Island, Bahamas.
Closest Related Species: D. bahamensis closely resembles D.
wilkensi from the Canary Islands.
Habitat: Anchialine limestone cave
Ecology: Collected at depths of 0-3 m in waters with a salinity of 32 ppt.
Additional fauna included an ostracod species Deeveya jillae, a calanoid
copepod and a macellicephalan polynoid polychaete (perhaps a young
Pelagomecellicephala iliffei). Brown unidentified particles were found
within the gut.
Life History: Of the 13 specimens collected, they included 1 adult male (holotype),
2 adult females (paratypes) and 10 juveniles (sex unknown). Sexual dimorphism is
found within the species. Males with a single copulatory organ having long
curved anterior part with slender tip, and shorter styliform part with 3 hairs
at tip. The genital pore is obscured on female. In addition, differences are
present on the first and second antennae (Kornicker & Iliffe, 1989). There are 5
growth stages.
Evolutionary Origins: The family Thaumatocyprididae is composed of five
genera. Two genera are known only from fossils, two inhabit the deep sea, and
Danielopolina primarily inhabits anchialine environments. The evolutionary
origins of stygobitic ostracodes remain undetermined. They may have originated
from the deep sea (Iliffe 1990:95; 1991:227-228) or from shallow water crevices
(Danielopol, 1990:141; Danielopol et al., 1996:82). These ostracodes may have
been in shallow anchialine pools and then migrated to the more stable cave
environment (Kornicker & Iliffe, 1998:2).
Conservation Status: Restricted to a single cave on Eleuthera.
References:
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Contributor: Louis S. Kornicker, National Museum of Natural History, Washington, DC
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