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Biodiversity Journal, 2014, 5 (1): 105–114

The long journey of Fusinus rostratus (Olivi,1792) (Gastropoda
Fasciolariidae) from Portugal coasts toVenice Lagoon

Paolo Russo

Santa Croce 421 - 30135 Venezia, Italy; e-mail: russorusso@virgilio.it

ABSTRACT   In the present paper the following morpha of Fusinus rostratus (Olivi, 1792) (Gastropoda Fa-
           sciolariidae) were investigated: Atlantic, Central and Southern Tyrrhenian Sea, Egadi Islands
           and the Sicilian Channel, Coasts of North Africa, the Central Adriatic Sea, Upper Adriatic Sea
           and the Venice Lagoon. Each of these morpha shows such morphological characteristics to be
           easily separated from the others. It is interesting to observe that the morphotype from the coast
           of Portugal is by far morphologically the closest to that from Northern Adriatic. A feature com-
           mon to all the described morphotypes, is the presence of secondary cords, regularly spaced
           between the primary ones. The aim of this study is to split this species by geographical areas
           in order to facilitate further studies.

KEY WORDS  Fusinus rostratus; Fasciolariidae; Mediterranean Sea; morphotipi.

Received 28.01.2014; accepted 21.03.2014; printed 30.06.2014
Proceedings of the Seventh Malacological Pontine Meeting, September 9th-10th, 2013 - San Felice Circeo, Italy

INTRODUCTION                                         cies is endemic to the Mediterranean. It is an eury-
                                                     bates species, found in a few centimeters of water
    The Fusinus rostratus (Olivi, 1792) (Gastro-     in the Lagoon of Venice (Buzzurro & Russo, 2001;
poda Fasciolariidae) is a species distributed all    Russo, 2012) to a maximum of detected depth of
over the Mediterranean Sea. It is more common        823 m (D'Amico, 1912). It is related to soft sedi-
in the northern and central Adriatic and in Tyrrhe-  ments (Vio & De Min, 1994, 1996), muddy (Mon-
nian Sea. It is also reported for the Atlantic Co-   terosato, 1877), debris and muddy (Coen & Vatova,
asts, Portugal (Hidalgo, 1917; Barash & Danin,       1932), debris and muddy-sandy (Vatova, 1943),
1992), the Canary Islands (Aradas & Benoit, 1870     muddy-sandy (Vatova, 1940; Taviani, 1978). It also
Poppe & Goto, 1991; Barasch & Danin, 1992).          occurs in Peyssonnelia polymorpha facies and
There are also records from Morocco (Pasteur-        mäerl (Jacquotte, 1962; Ledoyer, 1969). It feeds on
Humbert, 1962; Barasch & Danin, 1988, 1992;          polychetes.
Ardovini & Cossignani, 2004) and Mauritania
(Lozet & Dejean-Arrecgros, 1977) but these lat-          Here, we consider the following morpha: Atlan-
ters should be investigated; rare in the Aegean Sea  tic, Central and Southern Tyrrhenian Sea, Egadi Is-
with records that require a careful study (personal  lands and the Strait of Sicily, Coasts of North
observation).                                        Africa, Central Adriatic Sea, Northern Adriatic Sea
                                                     and the Venice Lagoon.
    According to Mallard & Robin (2005) this spe-
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