R. Witbaard et al., Geographical differences in growth rates of Arctica islandica (Mollusca : Bivalvia) from the North Sea and adjacent waters, J MARINE BI, 79(5), 1999, pp. 907-915
Citations number
55
Categorie Soggetti
Aquatic Sciences
Journal title
JOURNAL OF THE MARINE BIOLOGICAL ASSOCIATION OF THE UNITED KINGDOM
Geographical differences in the shell growth rate of several populations of
the bivalve Arctica islandica (Mollusca: Bivalvia) were estimated by using
the growth lines laid down during their first ten years of life. Attention
was focused on populations from the North Sea, but for comparison small sa
mples from adjacent waters were also analysed. A four-fold difference in th
e average growth rate was found between the slowest and fastest growing she
lls.
Principal component analysis was used to summarize the inter-relationships
between environmental variables and growth rates. Shell growth correlated p
ositively with primary production and temperature and inversely with depth
and the silt content of the sediment. The North Sea specimens were found to
have a strong positive correlation with grain size. Since sediment charact
eristics also depend on bottom currents, it is suggested that these increas
ed rates reflect lateral seston flux as additional food supply.
In a multiple regression model, applied to all available data, average annu
al temperature, primary production and the interaction between production a
nd water depth explained 50% of the variance. The derived standard coeffici
ents for temperature, primary production and the interaction between depth
and primary production were 0.90, 0.47 and -0.92 respectively. The results
of this study suggest that the temperature effects on in situ shell growth
are easily overruled by other environmental factors.
If a similar model was calculated with North Sea data only 75% of the varia
nce was explained by temperature, primary production and depth x primary pr
oduction. The standard coefficient for primary production was 1.26. The rol
e of temperature in explaining the observed growth differences is negligibl
e since the standard coefficient is -0.098. The interaction term, depth x p
rimary production had a standard coefficient of -0.95.