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Trends in GlobAl MArine Fisheries - Sea Around Us Project

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The North <strong>Sea</strong> LME is relatively shallow, and<br />

is situated on the cont<strong>in</strong>ental shelf of north-western<br />

Europe. The LME <strong>in</strong>cludes one of the most<br />

diverse coastal regions <strong>in</strong> the world, with a great<br />

variety of habitats (fjords, estuaries, deltas, banks,<br />

beaches, sandbanks and mudflats, marshes, rocks<br />

and islands). Among its many river systems and<br />

estuaries are the Thames, Rh<strong>in</strong>e, Elbe and Ems.<br />

A temperate climate and four seasons characterize<br />

this LME, with climate be<strong>in</strong>g an important<br />

driv<strong>in</strong>g force (after fish<strong>in</strong>g) of biomass change<br />

<strong>in</strong> the LME. Great Brita<strong>in</strong>, Norway, Sweden,<br />

Denmark, Germany, the Netherlands, Belgium<br />

and France are the countries border<strong>in</strong>g the North<br />

<strong>Sea</strong> (Sherman and Hempel 2008). Fish<strong>in</strong>g is a<br />

long-established activity <strong>in</strong> the North <strong>Sea</strong> LME<br />

and there is a wealth of fisheries data (Froese and<br />

Pauly 2003). The most important species for human<br />

consumption represented <strong>in</strong> the catch are<br />

Atlantic cod, saithe (Pollachius virens), Atlantic<br />

herr<strong>in</strong>g (Clupea harengus), European sprat<br />

(Sprattus sprattus) and flatfishes. Land<strong>in</strong>gs from<br />

the <strong>in</strong>dustrial fishmeal reduction fishery consist<br />

ma<strong>in</strong>ly of sandlances (sandeels Ammodytes spp.)<br />

Norway pout (Trisopterus esmarkii) and sprat.<br />

There are several commercially important shellfish<br />

species of molluscs and crustaceans. The<br />

BA-DAP for the North <strong>Sea</strong> LME <strong>in</strong>dicates a<br />

steady decl<strong>in</strong>e <strong>in</strong> <strong>in</strong>dicator <strong>in</strong> the early years, followed<br />

by a sudden, steep decl<strong>in</strong>e <strong>in</strong> 1970 towards<br />

strongly abundance dom<strong>in</strong>ated fisheries (Figure<br />

4). The <strong>in</strong>dex has rema<strong>in</strong>ed steady ever s<strong>in</strong>ce. It<br />

is worth not<strong>in</strong>g that throughout the time period<br />

considered here (1950–2004), the <strong>in</strong>dex was negative,<br />

suggest<strong>in</strong>g that the fisheries <strong>in</strong> this LME<br />

<strong>Trends</strong> <strong>in</strong> global mar<strong>in</strong>e fisheries – a critical view<br />

have been abundance dom<strong>in</strong>ated for the entire<br />

time period, as illustrated by the predom<strong>in</strong>ance<br />

of relatively small, yet abundant species such as,<br />

e.g., herr<strong>in</strong>g (Clupea harengus) and sandlances<br />

(Ammodytes).<br />

The Baltic <strong>Sea</strong> LME is the world’s largest<br />

brackish water body, and its catchment area is four<br />

times larger than its surface area (Sherman and<br />

Hempel 2008), nearly 93 percent of which belongs<br />

to n<strong>in</strong>e riparian countries: Denmark, Estonia,<br />

F<strong>in</strong>land, Germany, Latvia, Lithuania, Poland,<br />

Russia and Sweden. The non-coastal countries <strong>in</strong><br />

the catchment area <strong>in</strong>clude Belarus, the Czech<br />

Republic, Slovakia and Ukra<strong>in</strong>e. Atlantic cod,<br />

herr<strong>in</strong>g and European sprat dom<strong>in</strong>ate the fish<br />

community as well as catches <strong>in</strong> terms of numbers<br />

and biomass. The Baltic <strong>Sea</strong> LME shows an <strong>in</strong>terest<strong>in</strong>g<br />

BA-DAP pattern (Figure 4). It <strong>in</strong>itially<br />

was marg<strong>in</strong>ally positive, suggest<strong>in</strong>g a slight biomass<br />

dom<strong>in</strong>ance <strong>in</strong> catches, before decl<strong>in</strong><strong>in</strong>g to<br />

an abundance dom<strong>in</strong>ated catch pattern until the<br />

early 1970s (negative BA-DAP, Figure 4). This<br />

was followed by a return to a positive, biomass<br />

dom<strong>in</strong>ance <strong>in</strong> the early 1980s, and a subsequent<br />

steady decl<strong>in</strong>e to an abundance dom<strong>in</strong>ance pattern<br />

which is ma<strong>in</strong>ta<strong>in</strong>ed today (Figure 4). The<br />

decl<strong>in</strong>e <strong>in</strong> <strong>in</strong>dex <strong>in</strong> the 1960s and early 1970s was<br />

driven by the <strong>in</strong>crease <strong>in</strong> catches of herr<strong>in</strong>g and<br />

sprat, while the 1980 biomass dom<strong>in</strong>ance was the<br />

result of a brief resurgence of cod catches, with a<br />

concomitant substantial decl<strong>in</strong>e <strong>in</strong> sprat catches.<br />

The subsequent collapse of the cod stocks and<br />

resurgence of sprat catches resulted <strong>in</strong> the most<br />

recent decl<strong>in</strong>e <strong>in</strong> the <strong>in</strong>dex (Figure 4). The predom<strong>in</strong>ance<br />

of three taxa <strong>in</strong> the Baltic <strong>Sea</strong> catches,<br />

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