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At present, these habitats, according to the resolution from the International Congress of Marine Cave Biology held in Bermuda during 1984, are definitively defined as flooded inland marine caves and groundwaters that
lack any direct surface connection
with the open sea, with a wide range of different salinities, and showing the following subterranean features:
Anchialine habitats are rich of remarkable and unusual fauna, including primitive crustacean relicts such as Remipedia. Anchialine taxa, as a rule, show highly disjunct distributions: they inhabit cave and coastal anchialine habittas from isolated locations in both Atlantic and Pacific oceans, and are onsidered true Thetyan relicts. In last decade noteworthy representatives of this groups, of great phylogenetic value, have been discovered such as subterranean platycopioids, calanoids, speleoithonids, novocriniids, etc. It is interesting to note that crustaceans (remipedes, ostracods, copepods, amphipods, isopods, mysids, thermosbaenaceans, decapods) dominate among animals living exclusively in anchialine environments, some of them being much better represented tan others (Kornicher & Ilffe, 2000).
In recent years approximately more than 300 new species, 50 new genera, at least 10 new families, two new orders and even a new class of crustaceans (the Remipedia) have been described from anchialine caves, particularly on islands.
The recent discovery od misophrioid copepods in anchialine caves on Bermuda revealed that this habitat has been also exploited by this group of crustaceans previously considered a most deep-sea taxon (Boxshall, 1984).
As regard the origin of the anchihaline stygobiontes, two main hypotheses are at present known: the "deep sea hypothesis" (Iliffe a. o., 1984) and the "shallow water hypothesis" (Stock, 1986; Danielopol, 1990).According to the former most anchialine immigrants evolved from deep sea water ancestors; on the contrary, the latter support a shallow, coastal waters origin for most anchialine colonizers.
The most remarkable italian anchialine systems can be found along the Tuscanian tirrenian coast (Punta degli Stretti cave), along the Sardinian and Sicilian coasts, and along the adriatic and ionian coasts (caves between S. Cesarea Terme and Castro Marina: Zinzuluza, Buco dei Diavoli, L'Abisso and phreatic habitats in wells)
Anchialine waters of Italy are very densely populated, for the most part by crustaceans, water mites and oligochaetes: the mesohaline habitats are almost exclusively characterized by the genera Pseudoniphargus, Microcharon, Monodella, Spelaomysis, Typhlocaris, Halicyclops, Neocyclops, Schizopera ; oligohaline and limnic habitats are dominated by the genera Hadzia, Stygiomysis, Orniphargus, Salentinella and Diacyclops. The numerous ostracod species can live both in mesohaline and oligohaline waters, being for the most part stygophilic (Eucandona fabaeformis, Pseudocandona pratensis, Cypria ophtalmica, Herpetocypris brevicaudata, Notodromas persica, Cypridopsis vidua, Plesiocypridopsis newtoni, Sarscypridopsis aculeata ), only two species, viz. Pseudolimnocythere hypogea and Trapezicandona italica (Karanovic & Pesce, in press) are stygobitic.
Similar faunistic conditions are characteristic to the anchialine areas of the adriatic balkanic coasts.
Particularly the anchialine fauna of the Salentine Peninsula includes a gret number of palaeomediterranean taxa, which show close affinities with the Gondwana fauna, and could be considered relict elements of a tropical and/or subtropical miocenic fauna.
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Paramisophria (Copepod, Calanoida, Arietellidae) from anchialine caves on
the Canary and Galápagos Islands. Sarsia, 78(1):57-68.
Pansini A. & G. L. Pesce. 1998. Higginsia ciccaresei sp. nov. (Porifera: Demospongiae) from a marine cave on the Apulian coast (Mediterranean Sea). J. Mar. Biol. Ass. U.K., 78: 1083-1091.
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anchialine caves in Bermuda. Sarsia, 78(1):43-56.
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