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Tomasello, Di Maida, Calvo, Pirrotta, Borra & Procaccini Seagrass meadows at the extreme of environmental tolerance
the surface down to a depth of 45 m and covers 2–4% of then those structures are expected to be vulnerable to
the whole benthic substratum in the basin (approximately even small changes of the extreme environmental condi-
38,000 km2; den Hartog 1977; Procaccini et al. 2003). tions to which the single genotypes are exposed, and
Sexual reproduction is irregular and is sporadic in some could thus explain the observed regression. Moreover, we
localities (Diaz-Almela et al. 2006, 2007), whereas clonal aimed to define the level of genetic isolation among
growth by means of stolons seems to be the predominant stands growing inside, at the entrance and outside the
way of meadow expansion (Migliaccio et al. 2005; lagoon. We used all 13 microsatellite loci available for the
Arnaud-Haond et al. 2007b; Rozenfeld et al. 2007). Large species (Procaccini & Waycott 1998; Alberto et al. 2003).
clones can extend over more than 100 m (Ruggiero et al. We interpreted the results in respect to growth perfor-
2002; Migliaccio et al. 2005; Zupo et al. 2006). Neverthe- mances and occurrence of flowering in the last few years,
less, populations generally show high genetic variability as obtained through reconstructive techniques, in an attempt
a result of sexual reproduction or immigration of foreign to better understand the regression in atoll size and distri-
genotypes (Arnaud-Haond et al. 2005, 2007b). Posidonia bution observed in the last few years and provide support
oceanica can occur in salinities between 33& and 39& for the management of P. oceanica meadows within this
(Gobert et al. 2006; Sa`nchez-Lizaso et al. 2008) and toler- important coastal lagoon.
ate temperatures between 9 °C and 29 °C (Boudouresque
& Meinesz 1982). Coastal lagoons are stressful environ- Material and methods
ments for P. oceanica because environmental conditions
can reach the survival limits of this species (La Loggia Study area and sampling design
et al. 2004). The Stagnone di Marsala, a semi-enclosed
lagoon situated at the western coast of Sicily, is a singular Six Posidonia oceanica meadows were selected for this
environment where P. oceanica forms peculiar reef-like study along the western coast of Sicily. Samples were col-
structures (Calvo & Frada` Orestano 1984). In some areas lected in two sites inside the Stagnone di Marsala lagoon
of the lagoon, these reefs are atoll-shaped, which is a very (Atolls and Re´cif) and four sites outside the lagoon (Pla-
rare feature of Posidonia meadows. This phenomenon is teau, Nubia, Marsala and Favignana), where continuous
also observed in small areas along the Tunisian, Turkish and extensive meadows are present (Calvo et al. 1995)
and Corsican coasts (Blanpied et al. 1979; Boudouresque (Fig. 1). The Stagnone di Marsala lagoon is sub-divided
et al. 1990; Pasqualini et al. 1995). Pergent & Pergent- into a northern and a southern basin by an emerging
Martini (1995) and Boudouresque et al. (2006) hypothe- P. oceanica reef barrier (Re´cif-barri`ere) (Calvo & Frada`
sized that atolls derive from nearly circular patches where Orestano 1984). The southern basin has an average depth
plagiotropic (horizontal) shoots only grow outwards, of 2 m and is connected to the open sea through an
whereas the shoots on the central portion of the atolls opening 3000 m wide, in which it is possible to observe a
die. According to this hypothesis, one or a few genotypes vast P. oceanica reef platform (Plateau recifale). The
should be the founders of such structures without subse- northern basin, where P. oceanica grows in atoll-shaped
quent recruitment within the patch itself. In the Stagnone structures, is characterized by an average depth of 1 m
di Marsala, clear regression of P. oceanica stands has been and connected with the open sea northwards through an
recorded over the last decades, both in the overall distri- opening 400 m wide and 20–30 cm deep. This basin
bution of the meadows and in the number and diameter shows more distinct lagoon features than the southern
of atolls (personal observation by the authors). one, resulting from the limited water exchange and slow
turnover (about 65 days; Calvo et al. 2005). Geomorpho-
Our initial observations suggest that P. oceanica atolls logical conformation, shallow water, presence of isles and
in the Stagnone di Marsala occur at the limits of the spe- emerging vegetation also hinder water circulation (Maz-
cies’ tolerance, with temperature and salinity values zola & Sara` 1995; La Loggia et al. 2004). Indeed, higher
reaching 30 °C and 48&, respectively (Mazzola & Vizzini annual variation in temperature and salinity values were
2005). We focused our research on this peculiar habitat recorded within the lagoon (10–30 °C and 33–48&,
because global change is expected to affect most strongly respectively) with respect to the nearby open coastline
the populations occurring near the species’ environmental (temperature: 14.1–26.4 °C; salinity close to 37&) (Vizz-
tolerance limits (Reusch & Wood 2007). Moreover, com- ini et al. 2002; Mazzola & Vizzini 2005).
bined information on ecology and genetic diversity can
add to our understanding of the effects of genetic isola- In February 2006, about 40 individual orthotropic
tion in a fragmented landscape (Manel et al. 2003; Pro- P. oceanica shoots (ramets growing vertically) were ran-
caccini et al. 2007). domly sampled for each site. Shoots were collected at
depths ranging between 1 and 6 m and at a minimum
The aim of this work was to test whether each atoll of reciprocal distance of 8–10 m, to reduce the risk of sam-
P. oceanica is composed of a single genotype. If correct,
Marine Ecology 30 (2009) 288–300 ª 2009 Blackwell Verlag GmbH 289