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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.

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