Climate Change and the European Water Dimension - Agri ...
Climate Change and the European Water Dimension - Agri ...
Climate Change and the European Water Dimension - Agri ...
You also want an ePaper? Increase the reach of your titles
YUMPU automatically turns print PDFs into web optimized ePapers that Google loves.
Figure IV.C.13. Long-term monthly changes (1958-1999) in <strong>the</strong> plankton index. A<br />
negative anomaly in <strong>the</strong> index indicates a low value for Calanus finmarchicus, euphausiids,<br />
mean size of calanoid copepods with <strong>the</strong> exception of C. helgol<strong>and</strong>icus (opposite pattern) <strong>and</strong><br />
Pseudo-calanus spp. (no relationship). A positive anomaly indicates a high abundance of<br />
preys (<strong>and</strong> preys of suitable size). Cod recruitment (in decimal logarithm) in <strong>the</strong> North Sea<br />
(curve in white) is superimposed. The period of <strong>the</strong> Gadoid Outburst (Cushing 1984) is also<br />
indicated. Modified from Beaugr<strong>and</strong> et al. (2003).<br />
Temperature increases metabolic rate <strong>and</strong> <strong>the</strong>refore increases <strong>the</strong> energy dem<strong>and</strong>.<br />
Temperature rises decreases <strong>the</strong> quality <strong>and</strong> <strong>the</strong> quantity of prey available for larvae<br />
(so <strong>the</strong> energetic supply). Temperature rise may have <strong>the</strong>refore augmented <strong>the</strong><br />
energetic unbalance of larval cod that may have resulted in increasing larval mortality<br />
(<strong>the</strong> hypo<strong>the</strong>ses of size specific survival or growth dependent mortality). These<br />
results provide evidence that changes in <strong>the</strong> plankton ecosystem are <strong>the</strong> probable<br />
cause of <strong>the</strong> increased recruitment during <strong>the</strong> period 1963-1983, which was called<br />
<strong>the</strong> “Gadoid Outburst”.<br />
IV.C.8. Habitats<br />
The coastal marine system is organized as a succession of spatial units, each of <strong>the</strong>m<br />
having its own characteristics <strong>and</strong> where <strong>the</strong> organisms are adapted to a specific range<br />
of environmental conditions. Estuaries, salt-marshes, lagoons, rocky shores, seagrass<br />
meadows, s<strong>and</strong>y beaches, all <strong>the</strong>se units or habitats are often very productive, <strong>and</strong> in<br />
<strong>the</strong> same time, very vulnerable to changes in <strong>the</strong> external forcing which are issued from<br />
l<strong>and</strong>, atmosphere <strong>and</strong> ocean <strong>and</strong> interact in <strong>the</strong> coastal zone at overlapping scales.<br />
Coastal lagoons around Europe are already experiencing drastic <strong>and</strong> irreversible<br />
changes (see part B <strong>and</strong> part E of <strong>the</strong> Report) in <strong>the</strong>ir ecosystems reacting to both<br />
climatic trends <strong>and</strong> increasing human pressure. Seagrass beds are ano<strong>the</strong>r example of<br />
marine habitats under climate change threats, particularly vulnerable to increase in<br />
storminess.<br />
Seagrass meadows<br />
Seagrasses are vascular plants, typically configured like <strong>the</strong>ir terrestrial counterparts with<br />
a system of leaves, flowers <strong>and</strong> roots. Originally deriving from l<strong>and</strong> <strong>and</strong>/or freshwater<br />
102