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256                        CALOGERO MUSCARELLA & ALESSANDRO BARAGONA




                 Coleoptera  Odocnemis  ruffoi  ruffoi (Canzoneri,  parently disassociated distribution of the Issid Ho-
                 1970). This last species belongs to a sub family of  moptera Conosimus malfanus Dlabola, 1987, until
                 Tenebrionidae, the Elopinae, which in the Mediter-  now known only for Marettimo and Salina. A future
                 ranean area enumerate several elements with a cir-  deeper look of the research might reveal the pres-
                 cumscribed  geonemy  and  numerous  endemic  ence of this species also alongside the northern Si-
                 species. Odocnemis ruffoi has an exclusively insular  cilian coastlines.
                 Tyrrhenian distribution: nominal form is found in
                 Marettimo, while another subspecies (ssp. osellai  Island of Ustica
                 Gardini,  1979)  was  described  for  the  Island  of
                 Montecristo, in the Tuscan Archipelago. This fact,  The Island of Ustica, as the Aeolian Island, is a
                 together with the peculiar, systematic position of  talassogenic island. It is the highest tip of a vast un-
                 the species, inspires the hypothesis of an area of  dersea volcanic apparatus, whose base is over 2000
                 relictual distribution, which might have shrunk in  meters below the sea level. The intense volcanic
                 comparison  to  the  original  one  for  unspecified  explosive  activity  that  took  place  starting  from
                 (maybe ecological) reasons. Both the islands were  Pliocene is accountable for the continuous accumu-
                 allegedly refuge-posts for O. ruffoi, while the isol-  lation of igneous and pyroclastic material on the sea
                 ation might have determined a successive differen-  bed which, in medium Pleistocene (approximately
                 tiation  in  the  two  sub-specific  forms  presently  350 million years ago) led to the emersion of the is-
                 known (AA.VV. 2009a; Aliquò & Soldati, 2010).  land  (AA.VV.,  2009a;  Bonomo  &  Ricci,  2010).
                 The  case  of  Allophylax  costatipennis  godenigoi  Ustica is separated from Sicily by a wide and deep
                 Canzoneri,  1970  is  different.  The  species  has  a  sea area and it has probably always remained isol-
                 northern-african type of distribution and it is present  ated,  even  during  pleistocenic  regressions.  The
                 on the island of Lampedusa (see Aliquò& Soldati,  young geological age of Ustica, together with its
                 2010) while it seems to be lacking in Sicily. The dif-  isolation, are the main conditions making its faun-
                 ferentiation of the population of Marettimo at an in-  istic populations (prevalently of a Sicilian or south-
                 fraspecific level seems to be due to its geographical  ern  Italian  type)  not  particularly  relevant.  (cf.
                 isolation in comparison to the ones of the rest of the  Francino Corti & Lanza, 1973). Only 5 endemic
                 area of distribution of the species (AA.VV., 2009a).  species, probably all of new formation, are pointed
                 Other important paleoendemic species of Maret-  out for the island. The most interesting element is
                 timo are the Isopod Crustaceans Bathytropa ruffoi  the  Cave  Isopod  Spelaeoniscus  vandeli Caruso,
                 Caruso, 1973 and Spelaeoniscus lagrecai Caruso,  1974, apparently well differentiated by the congen-
                 1973. The genus Bathytropa Budde-Lund, 1885 en-  eric species (Caruso & Lombardo, 1995). Inter-
                 compasses  8  species  diffused  in  different  point  esting is the presence of Oxychilus (Hyalocornea)
                 areas in the Mediterranean water basin: a distribu-  nortoni (Calcara, 1843), a specie belonging to the
                 tion which, according to Caruso (1973), suggests a  subgenus Hyalocornea Monterosato, 1892, in a par-
                 pre-Pliocenic origin. To the hypothetical fragment-  ticolar distribution with O. (H.) alicurensis typical
                 ation of the Tyrrhenid of the tertiary period is to be  of Alicudi, O. (H.) canini (Benoit, 1843) of north-
                 connected the origin of Spelaeoniscidae Racovitza,  western Sicily, O. (H.) egadiensis Riedel, 1973 of
                 1907 (Caruso, 1973), a family present, for Italy in  Favignana and Levanzo and probably also O. (H.?)
                 the sole Sicily with 5 endemic species, 3 of which  pomelianus Bourguignat, 1867 of NW-Algeria and
                 in the circum-sicilian islands (Argano et al., 1995;  the Galite Island in Tunisia (Riedel, 1980). The
                 Caruso & Lombardo, 1995). Other entities which  Blattaria Ectobius usticaensis Failla et Messina,
                 are exclusive of the archipelago belong to genera  1974, according to Failla et al. (1973) and Failla &
                 which  are  rich  in  point-schizo-endemic  species,  Messina (1974) who minutely studied the anatomy
                 such  as  the  Coleoptera  Otiorhynchus (Aram-  of the glandular dimples, allegedly belongs to a dif-
                 michnus) aegatensis Magnano, 1992 (present in all  ferent evolutionary line if compared to Ectobius
                 of the three islands), Entomoculia hieratica Poggi  Stephens,  1835  Sicilian  and  Aeolian.  Opatrum
                 et Baviera, 2013 (Marettimo), the Chrysomelidae  (Colpophorus) validum marcuzzii Canzoneri, 1972
                 Coleoptera Pachybrachis osellai Daccordi et Ruffo,  is part of a Northern African chorotype present,
                 1975 (present in Levanzo and Marettimo). The ap-  other than in insular Sicily with the nominal sub-
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