BSEP116B Biodiversity in the Baltic Sea - Helcom
BSEP116B Biodiversity in the Baltic Sea - Helcom
BSEP116B Biodiversity in the Baltic Sea - Helcom
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From an ecological po<strong>in</strong>t of view, available light at<br />
<strong>the</strong> seabed is one of <strong>the</strong> primary physical parameters<br />
<strong>in</strong>fluenc<strong>in</strong>g and structur<strong>in</strong>g <strong>the</strong> biological<br />
communities <strong>in</strong> <strong>the</strong> mar<strong>in</strong>e environment as it is <strong>the</strong><br />
driv<strong>in</strong>g force beh<strong>in</strong>d primary production. Available<br />
light was <strong>in</strong>cluded as it dist<strong>in</strong>guishes between <strong>the</strong><br />
photic zone where primary production occurs and<br />
<strong>the</strong> non-photic zone.<br />
Sal<strong>in</strong>ity was divided <strong>in</strong>to six categories reflect<strong>in</strong>g<br />
species distribution boundaries or ecological<br />
requirements throughout <strong>the</strong> <strong>Baltic</strong> <strong>Sea</strong>. Unfortunately,<br />
no coherent data for benthic species<br />
cover<strong>in</strong>g <strong>the</strong> entire <strong>Baltic</strong> <strong>Sea</strong> region are available<br />
that can l<strong>in</strong>k species distribution and sal<strong>in</strong>ity.<br />
Focus was <strong>the</strong>refore placed on <strong>the</strong> known<br />
requirements of certa<strong>in</strong> key species, e.g., <strong>the</strong><br />
sal<strong>in</strong>ity at which bladder wrack (Fucus vesiculosus)<br />
becomes <strong>the</strong> dom<strong>in</strong>at<strong>in</strong>g submerged brown alga.<br />
Table 2.1.1 summarizes <strong>the</strong> reason<strong>in</strong>g for <strong>the</strong> specific<br />
categories.<br />
O<strong>the</strong>r environmental parameters were considered,<br />
but <strong>the</strong>y were ei<strong>the</strong>r more relevant for<br />
detailed habitat mapp<strong>in</strong>g purposes, e.g., wave<br />
exposure; not relevant for <strong>the</strong> entire region, e.g.,<br />
ice cover; not significantly <strong>in</strong>fluenc<strong>in</strong>g <strong>the</strong> species<br />
distribution <strong>in</strong> <strong>the</strong> <strong>Baltic</strong> <strong>Sea</strong>, e.g., temperature;<br />
or of only m<strong>in</strong>or importance compared to o<strong>the</strong>r<br />
geographical areas, such as tidal currents. Lastly,<br />
<strong>the</strong> aim was to limit <strong>the</strong> number of mar<strong>in</strong>e landscapes<br />
to a manageable number (see Al-Hamdani<br />
& Reker 2007 for details). Us<strong>in</strong>g this approach,<br />
60 mar<strong>in</strong>e landscapes were identified <strong>in</strong> <strong>the</strong> <strong>Baltic</strong><br />
<strong>Sea</strong> (Figure 2.1.1d, Box 2.1.2).<br />
How well can we trust <strong>the</strong> maps?<br />
An essential factor <strong>in</strong> <strong>the</strong> durability of benthic<br />
mar<strong>in</strong>e landscape maps is that <strong>the</strong>y provide a true<br />
reflection of <strong>the</strong> broad-scale species assemblages<br />
<strong>in</strong> <strong>the</strong> <strong>Baltic</strong> <strong>Sea</strong>. If <strong>the</strong>y do not meet this criterion,<br />
<strong>the</strong>y are of limited use for support<strong>in</strong>g a susta<strong>in</strong>able<br />
Figure 2.1.1a. Map of mar<strong>in</strong>e seabed sediments,<br />
as divided <strong>in</strong>to five categories, <strong>in</strong> <strong>the</strong> Kattegat and<br />
<strong>Baltic</strong> <strong>Sea</strong>; compiled from sediment <strong>in</strong> formation<br />
from GEUS, GTK and SGU.<br />
20<br />
Figure 2.1.1b. Model results show<strong>in</strong>g <strong>the</strong> distribution<br />
of areas where at least 1% of available light<br />
reaches <strong>the</strong> seabed (<strong>the</strong> photic zone) and <strong>the</strong> nonphotic<br />
zone. Data source: DHI and ICES.