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pacts on benthic communities by facilitating competitive exclusion, predation, and extinc-
tion(Agius,
2007
).Planktonisaparticularly goodindicator ofclimate change,inparticular
members of the genus
Ceratium
, important primary producers in tropical and temperate
waters, have expanded their range into warmer water. For example, before 1970,
C. tricho-
ceros
was only found south of the UK, but is now found off the west coast of Scotland and
in the northern North Sea. Dramatic biogeographical shifts have also been documented for
warm-water assemblages of calanoid copepod, which have moved 1000 km further north
in the north-east Atlantic over the past 40 years, with a concomitant retraction in the range
so-called Lessepsian migration of various Red Sea species through the Suez Canal to the
Mediterranean, the outbreak of the green algae
Caulerpa taxifolia
and
Caulerpa racemosa
in the Mediterranean, the introduction of Ponto-Caspian species in the Baltic, and the ex-
pansionoftheJapanese oyster
Crassostrea gigas
intheWaddenSeaandalongthesouthern
species on existing communities are diverse, and often not well known. The role of alien
species should therefore be assessed in a more integrated and dynamic context of shifting
species' ranges and changing compositions and structures of communities (Walther
et al.,
Asynthesis ofthe various types ofimpacts onmarine biodiversity andthuspotentially
on related ecosystem services is reported in
Figure 4.1
.
Figure 4.1
The effects of different drivers (including climate change as temperature rise, acidification and hypoxia)
on function of biodiversity and goods and services in different oceanic regions