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134            S.  Ragonese, M.L.  Bianchini l  Fisheries Research 26 (1996) 125-137

                  between the  other alternati ves  Heincke' s autumn estimate  ( Z =  1.1 )  should  be  preferred
                  since the method is more suitable for cases of discrete recruitment.
                    Assuming a maximum life span of6 years  (Demestre and Lleonart, 1993), Alagaraya's
                  approximation produces an annua! natura! mortality coefficient M= O. 77, approximated to
                  M  h= 0.8  for  successive computations; the alternative M =  0.5  represents a more conser-
                                                                    1
                  vative choice. The parameters used to compute the yield-per-recruit values are summarized
                  in T ab le 3; the resulting four curves, for the two mean ages of first capture (te= l; tz =  1.5)
                  and the two M values, are presented in Fig. 5. As expected, the shape of the curves suggests
                  a rapi d  increase of Y l R for  small  increments of F,  and  thereafter the  curves ftatten  out,
                  without any evidence of a clear maximum.
                    For M h= 0.8, the yield-per-recruit could be substantially increased even by raising only
                  F  ( i.e.  the population is  actually underexploited); o n the contrary, for M =  0.5,  gains in
                                                                                    1
                  the Y l R could no t be obtained without changing the age of first capture too.


                  4. Discussion

                    Length-based methods are currently the only  techniques available for the estimation of
                  growth  and  mortality  parameters  for  deep-water  shrimps,  as  hard  parts  are  lost  during
                  moulting, tagging is not feasible, and rearing experiences ( Sardà, 1986) for Aristeus anten-
                  natus are  only in  an  embryonic phase.  Despite the  discontinuities in  the  growth process
                  (Dali et  al.,  1990), continuous asymptotic models, such as  the  VBGF,  are considered a
                  reasonable approximation for shrimps (Pauly et al.,  1984; Garcia, 1985).
                    T ab  le 4 summarizes the VBGF estimates for other Mediterranean populations of Aristeus
                  antennatus ( see the introduction for references), which indicate asymptotic carapace lengths
                  ranging from 63 to 76 mm an d a relatively long l ife span ( up to 6 years); the annua! Brody's
                  coefficients fall  in the range 0.3-0.9,  with the exception of the Ligurian stock  (K =  1.71;
                  Orsi-Re lini and Relini,  1985).
                    While ali  growth  values  (MIX,  'fast'  and  'slow'  ELEFAN)  for  the  population  of the
                  Strait of Sicily fall inside the above ranges, the present analysis shows the need to take into
                  consideration the variability of parameters (mainly a sampling problem)  on one side, and
                  the consistency of the MIX estimates on the other side.
                    The population of the Strait of Sicily shows  a discrete recruitment, whereas a more or
                  less prolonged presence of juveniles is generally reported for the other populations ( Sardà,
                  1988).
                  T ab le 4
                  Summary of the  VBGF estimates for the  Mediterranean  populations of Aristeus antennalus  ( CL.x  in  mm;  1 0  in
                  year)

                  Area                   C Lx       Kly        lo           Source
                  Catalan Sea            76         0.3        -0.07        Demestre and Lleonart ( 1993)
                  Algeria                63.5       0.33                    Y ahiaoui (1990)
                  Ligurian Sea           63         1.71         0.44       Orsi-Relini and Relini ( 1985)
                  Southern Tyrrhenian    69.4       0.34                    Arculeo et al.  (1992)
                  lonian Sea             66.2       0.93                    Matarrese et al.  ( 1992)
                  Strait of Sicily       69.1       0.53         o          Present paper
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