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BSEP116B Biodiversity in the Baltic Sea - Helcom

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Box 1.2. Regime shifts <strong>in</strong> <strong>the</strong> <strong>Baltic</strong> <strong>Sea</strong> as detected by an Integrated Ecosystem Assessment<br />

The ICES/HELCOM Work<strong>in</strong>g Group on Integrated Assessments<br />

of <strong>the</strong> <strong>Baltic</strong> <strong>Sea</strong> (WGIAB) has conducted Integrated Ecosystem<br />

Assessments (IEAs) on a number of offshore and one coastal<br />

sub-region of <strong>the</strong> <strong>Baltic</strong> <strong>Sea</strong> (see table) (ICES 2008a). IEAs are<br />

multivariate analyses of time series of <strong>the</strong> physical, chemical<br />

and biological environment as well as socio-economic factors.<br />

The analyses were targeted to assess <strong>the</strong> impact of climate,<br />

fisheries, and eutrophication on <strong>the</strong> different sub-regions.<br />

All seven sub-regions <strong>in</strong>vestigated displayed pronounced<br />

structural changes, i.e., regime shifts, dur<strong>in</strong>g <strong>the</strong> past two<br />

to three decades. The major period of restructur<strong>in</strong>g <strong>in</strong> <strong>the</strong><br />

<strong>Baltic</strong> sub-regions was at <strong>the</strong> end of <strong>the</strong> 1980s. The Sound,<br />

central <strong>Baltic</strong> <strong>Sea</strong>, Gulf of Riga, Gulf of F<strong>in</strong>land, and Bothnian<br />

Bay also underwent structural change dur<strong>in</strong>g <strong>the</strong> mid-1990s,<br />

probably related to <strong>the</strong> major <strong>in</strong>flow <strong>in</strong> 1993.<br />

For <strong>the</strong> central <strong>Baltic</strong> <strong>Sea</strong>, two relatively stable periods were<br />

detected <strong>in</strong> 1974–1987 and 1994–2006. The first period<br />

was characterized by comparatively high cod and<br />

herr<strong>in</strong>g spawner biomass and recruitment, and high<br />

abundances of <strong>the</strong> copepod Pseudocalanus acuspes,<br />

whereas <strong>in</strong> <strong>the</strong> later period <strong>the</strong> system was spratdom<strong>in</strong>ated<br />

with high abundances of Acartia spp. and<br />

Temora longicornis. Between <strong>the</strong> two shifts, <strong>the</strong>re was<br />

a transition period of highly variable climatic and hydrographic<br />

conditions and no major <strong>in</strong>flow events, result<strong>in</strong>g<br />

<strong>in</strong> low sal<strong>in</strong>ity and high temperature values.<br />

The ma<strong>in</strong> drivers of <strong>the</strong> observed ecosystem changes<br />

vary between sub-regions, but <strong>the</strong>y all <strong>in</strong>clude <strong>the</strong><br />

<strong>in</strong>creas<strong>in</strong>g temperature and decreas<strong>in</strong>g sal<strong>in</strong>ity <strong>in</strong>fluenced<br />

by large-scale atmospheric processes. In addition<br />

to temperature and sal<strong>in</strong>ity, fish<strong>in</strong>g pressure was<br />

identified as an important driver for <strong>the</strong> central <strong>Baltic</strong><br />

<strong>Sea</strong> and Bothnian <strong>Sea</strong> as well as nutrients for <strong>the</strong><br />

highly eutrophied Gulf of F<strong>in</strong>land.<br />

Regime shifts (RS 1 to RS 4) <strong>in</strong> <strong>the</strong> different sub-bas<strong>in</strong>s of <strong>the</strong> <strong>Baltic</strong> <strong>Sea</strong> <strong>in</strong> several time periods.<br />

System Period covered RS 1 RS 2 RS 3 RS 4<br />

The Sound 1979–2005 1987/88 1995/96<br />

Central <strong>Baltic</strong> <strong>Sea</strong> 1974–2006 1987/88 1994/95<br />

Gulf of Riga 1974–2006 1988/89 1997/98<br />

Gulf of F<strong>in</strong>land 1979–2007 1988/89 1995/96 2002/03<br />

Bothnian <strong>Sea</strong> 1979–2006 1982/83 1988/89<br />

Bothnian Bay 1979–2006 1987/88 1993/94<br />

Kvädöfjärden, Nor<strong>the</strong>rn <strong>Baltic</strong> Proper 1971–2006 1976/77 1987/88 2004/05<br />

16<br />

There is ample evidence for a positive relationship<br />

between <strong>the</strong> number of species and ecosystem<br />

productivity and stability over time as well as for<br />

<strong>the</strong> capacity of an ecosystem to recover after<br />

disturbances (Naeem & Li 1997, Worm et al.<br />

2006). Changes <strong>in</strong> <strong>the</strong> environment that result <strong>in</strong><br />

decreased biodiversity are <strong>the</strong>refore considered<br />

to make systems less resilient and more prone to<br />

undergo regime shifts. In an ecosystem such as<br />

<strong>the</strong> <strong>Baltic</strong> <strong>Sea</strong> that is characterized by low species,<br />

genetic, and functional diversity, protection of<br />

biodiversity is thus central to ensur<strong>in</strong>g ecosystem<br />

resilience.<br />

1.5 Protection of<br />

biodiversity—Global and<br />

European targets<br />

Protection of biodiversity is an <strong>in</strong>tegral part of<br />

<strong>the</strong> ecosystem approach to <strong>the</strong> management<br />

of human activities. The 1992 United Nations<br />

Convention on Biological Diversity has provided<br />

<strong>the</strong> basis and concepts for much of <strong>the</strong> work on<br />

biodiversity protection. At <strong>the</strong> UN World Summit<br />

on Susta<strong>in</strong>able Development <strong>in</strong> 2002, <strong>the</strong> governments<br />

committed <strong>the</strong>mselves to significantly<br />

reduc<strong>in</strong>g <strong>the</strong> rate of biodiversity loss by 2010.<br />

Halt<strong>in</strong>g <strong>the</strong> loss of biodiversity by 2010 is also a

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