A. Gremare et al., ON THE DRAMATIC INCREASE OF DITRUPA-ARIETINA MULLER,O.F. (ANNELIDA, POLYCHAETA) ALONG BOTH THE FRENCH AND THE SPANISH CATALAN COASTS, Estuarine, coastal and shelf science (Print), 47(4), 1998, pp. 447-457
The distribution and population structure of the serpulid polychaete D
itrupa arietina were assessed along the section of the Mediterranean c
oast between Barcelona and Montpellier. The study combined: (1) the an
alysis of the existing historical data referring to the period before
the 1970s; (2) the results of impact assessment surveys carried out in
the late 1980s and the 1990s; and (3) the results of two surveys carr
ied out in the Bay of Blanes and along the coast between Cape Cerbere
and Port-la-Nouvelle during 1996. The results of the surveys carried o
ut in the 1990s show the occurrence of high densities (i.e. >1000 ind
m(-2)) of Ditrupa arietina at all the sites sampled. These results can
be compared with the few reports of this species before 1970, leading
to the conclusion that D. arietina has recently increased all along t
he Catalan coast. Ditrupa arietina is preferentially found between 20
and 30 m depth, which mostly corresponds to well-sorted fine sands and
muddy sands. Both the results of population monitoring and the hetero
geneity of population structure at small spatial scale show that the d
ynamics of this species is unstable. The observed distribution pattern
is therefore interpreted as resulting from a response to both wide-sc
ale environmental parameters (accounting for the dramatic increase of
the species at a wide geographical scale), and to local environmental
factors (accounting for small-scale heterogeneity in population struct
ure). Analysis of the relationship between sedimentary data and densit
ies of D. arietina suggests that this species is highly sensitive to t
he presence of fine sediments. However, because of the regional import
ance of the phenomenon, it is concluded that the dramatic increase of
D. arietina along both the Spanish and the French Catalan coast does n
ot result from sediment instability. (C) 1998 Academic Press.