waders and their estuarine food supplies - Vlaams Instituut voor de ...
waders and their estuarine food supplies - Vlaams Instituut voor de ...
waders and their estuarine food supplies - Vlaams Instituut voor de ...
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PREDICTING SEASONAL AND ANNUAL FLUCTUATIONS IN THE LOCAL EXPLOITION OF DIFFERENT PREY<br />
50<br />
40 -<br />
A 77«.<br />
85*<br />
30 -<br />
20<br />
84<br />
/Co<br />
/83<br />
10<br />
50<br />
40<br />
n i<br />
30|-<br />
20-<br />
10-<br />
62<br />
•<br />
i •'.' : ,<br />
/ y=-42*0 88x<br />
r.0.74<br />
81 p=0.02<br />
79 •<br />
•<br />
( ) 20 40 60 80 100<br />
total biomass (gm-2)<br />
C<br />
20 40 60 80<br />
harvestable biomass (gm z )<br />
0<br />
0.0 0.4 0.8 1.2 1.6<br />
intake rate (trigs-' feeding)<br />
y = -3.0.81K<br />
r=0.95<br />
p=0.0001<br />
_L-<br />
100<br />
Fig. 20. \verage feeding <strong>de</strong>nsity in Deotanber (Oystercatcherha"')<br />
;is ii function ol A. total bkxnass, B. harvestable biomass <strong>and</strong> C predicted<br />
intake rale (mg s' feeding); same data us Fig, 16. Since no<br />
bird counts were available lor December 1985. we compared lor<br />
lhat year Food supply ami hinl clensiiy at the end ol October, Bird<br />
<strong>de</strong>nsit) in December was, on average, 1.5 times as high as in Octo-<br />
v I'll: hence Ibis [imliiplymy factor WHS used to estimate the<br />
<strong>de</strong>nsity in l°85.<br />
ol the Wad<strong>de</strong>n Sea. where the Oystercatchers <strong>de</strong>creased<br />
from October onwards. /\s an example, lio.<br />
19B shows the monthly averages for nearby Schiermonnikoog.<br />
given separately for the eastern <strong>and</strong> western<br />
pan of the isl<strong>and</strong>.<br />
260<br />
How can we explain why our Stud) area attracted<br />
so many Oystercalchers in mid-winter? 'Flic* simples!<br />
explanation is that birds leave a feeding site if the) can<br />
achieve a higher intake rale elsewhere. II so. buds<br />
feeding in summer on mudflats with buried bivalves<br />
<strong>and</strong> Ragworms as the only prev would leave these areas<br />
in late summer to move to mussel <strong>and</strong> cockle beds<br />
(Fig. 15A). Since cockle <strong>and</strong> mussel beds are usually<br />
found on the lower part of the shore, <strong>and</strong> Macoma <strong>and</strong><br />
Ragworms occur on mudflats often situated above<br />
mean sea level, the high shore is in summer a relatively<br />
more important feeding area than in winter. However,<br />
it is unlikely lhat this explains why our study area attracted<br />
so many Oystercatchers in winter. The tidal<br />
Hats in our study area consisted of mud <strong>and</strong> the greater<br />
pan were situated above mean sea level, so fewer buds<br />
would be expected to remain to feed in winter. In fact,<br />
the reverse was found I lie. 19). Possibly, the ten<strong>de</strong>ncy<br />
of Oystercatchers lo concentrate from October onwards<br />
on tidal Hals adjacent to inl<strong>and</strong> feeding areas<br />
(Fig. 19) explains this unexpected finding. This would<br />
explain Ihe relatively low numbers remaining to vv unci<br />
on Ihe eastern part of Schiermonnikoog. where there is<br />
no grassl<strong>and</strong>, <strong>and</strong> the relatively high numbers wintering<br />
along the Frisian coast <strong>and</strong> on western Schiermonnikoog<br />
where grassl<strong>and</strong> is available. The bird census<br />
data of ihe Dutch Wad<strong>de</strong>n Sea (Zegers & Kwint 1992)<br />
also revealed that the number of Oystercatchers on<br />
Vliel<strong>and</strong>. an isl<strong>and</strong> without inl<strong>and</strong> feeding areas, is in<br />
vv inlet 47'r lower than in late summer, whereas ihe<br />
winter numbers along the mainl<strong>and</strong> coast of the<br />
provinces Noord-Holl<strong>and</strong>, Friesl<strong>and</strong> <strong>and</strong> Groningen.<br />
w ith extensive grassl<strong>and</strong>s next to die sea wall, arc 28* I<br />
higher, on average, than in late summer; ibis calculation<br />
is based upon a comparison between the January<br />
counls from the four mild winters 1981. 1983. 1989<br />
<strong>and</strong> 1991, <strong>and</strong> preceding counts from August OT<br />
September. As shown elsewhere (Zwarts et al. 1996d).<br />
the daily variation in exposure lime of the low water<br />
feeding areas in the Wad<strong>de</strong>n Sea is much larger in winler<br />
than in summer. Consequently, the ability to compensate<br />
at high ti<strong>de</strong> for short feeding periods is more<br />
important in the w inter half of the year lli-.ni in the summer<br />
half. This opportunity is apparently important<br />
enough for Oysiercatchers to move to parts of the<br />
Wad<strong>de</strong>n Sea where compensatory feeding on grassl<strong>and</strong><br />
is available.