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waders and their estuarine food supplies - Vlaams Instituut voor de ...

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Tahle 1 Weight loss ('•- ± SE) m Macoma (12to21 mm, n = 960<br />

specimens! sUsted III sea waler at 4 "C for I). I. 2 or .' daw after<br />

inlkviion. Average wejghl ol each mm-class on da) u is set to um<br />

Subsequent changes are expressed as relative <strong>de</strong>viation on day I to<br />

3. The differences are weakly significant according to a one was<br />

analysis of variance (R J *»0.23 p*»0 03, n = 26). The percentage<br />

ash (± SE) differs significantly es<br />

Macoma<br />

AFDW. % nsli. ",<br />

Scrobicularia<br />

\ll>w. c y ash.'<br />

100 21 2 ±0.9 HK) 30.0 ± 1.2<br />

101.8 ±3.3 I2.8±l.() 94.1 ±2.6 17.6 ±0.7<br />

29<br />

of stomach emptying, since about a quarter of the ash<br />

disappeared. Therefore no correction was ma<strong>de</strong> for the<br />

duration ol the storage.<br />

i l) Immersion in boiling water mav have dissolved<br />

flesh. This effect also appeared to be negligibly small,<br />

even when the immersion lime was 13 s (Table 2),<br />

Immersion halved the percentage ash. partly because<br />

salt dissolved but mainly because of the loss of s<strong>and</strong><br />

particles. The immersion time was kepi as short as<br />

possible <strong>and</strong> ihe flesh removed as soon as the shells<br />

Stalled to gape. No correction was ma<strong>de</strong> for this,<br />

possibly very small, loss of AFDW.<br />

(3) The AFDW of bivalves < 11 mm long could not<br />

be compared directly with that of the larger bivalves<br />

When the shells o( small bivalves are ignited, organic<br />

material in the hard parts (viz. eonchine) disappears<br />

along with water tightly bound in the shell. To<br />

<strong>de</strong>termine how huge an error this introduced, samples<br />

of shells were cleaned by placing them in a solution of<br />

coOagenase at 37 °C for 24 h. so that all the flesh could<br />

be easily removed. The AFDW of the shells, bound<br />

water inclusive, was low (Fig. 2): 2.6% of the DW oi<br />

the shell in Macoma. 1.99 in Scrobicularia (no spat).<br />

2,9% in Mya <strong>and</strong> 2.2'.. in ("< rastodt rma. These values<br />

are in agreement with data of llibberi (1976),<br />

Beukema (19X0. 1982a), K-leef et al. (1982), <strong>and</strong><br />

Goulletquer & Wolowicz (1989). Nonetheless, the<br />

contribution of the shell itself to the total AFDW ol the<br />

shell <strong>and</strong> flesh together varied between 15% <strong>and</strong> 40%.<br />

li was greatest in Cerasto<strong>de</strong>rma in winter, when the<br />

DW of the shell was 14 to 15 times that of the flesh, li<br />

was least in Mamma in summer when the DW ol tin.*<br />

shell was still 5 limes that of ihe llesh. In view of this<br />

large contribution ma<strong>de</strong> by the AFDW of ihe shell.<br />

Rg. 2 was used lo estimate how much should be subtracted<br />

from the total AFDW on those occasions when<br />

soli <strong>and</strong> hard parts of bivalves had not been separated.<br />

this being usually the bivalves < 11 mm long.<br />

(4) The DW was <strong>de</strong>termined for all si/e classes, bin<br />

sometimes the ash content was not measured. The<br />

percentage ash appeared in<strong>de</strong>pen<strong>de</strong>nt of size but<br />

varied seasonal!) digs. 3 <strong>and</strong> 4), The average percentage<br />

ash contenl per month was used to convert<br />

DW into AFDW on those occasions when samples had<br />

not been ignited. A similar seasonal variation in ash<br />

content was found in Macoma by Beukema & <strong>de</strong><br />

Bruin (1977). but it occurred at a lower level, probably

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