Distribution of marine species (CLIM 015) - Assessment published Nov 2012
Climate change (Primary topic)
Coasts and seas
Typology: Descriptive indicator (Type A - What is happening to the environment and to humans?)
- CLIM 015
- Calanus ratio in the North Sea
- Annual mean number of Calanus per sample
- Ratio [dimensionless]
- Number of Calanus [dimensionless]
Key policy question: How is climate change affecting the regional distribution of marine organisms in European seas?
- Increases in regional sea temperatures have triggered a major northward expansion of warmer-water plankton in the North-east Atlantic and a northward retreat of colder-water plankton. This northerly movement is about 10 ° latitude (1 100 km) over the past 40 years, and it seems to have accelerated since 2000.
- Sub-tropical species are occurring with increasing frequency in European waters, and sub-Arctic species are receding northwards.
- Further changes in the distribution of marine species are expected, with projected further climate change, but quantitative projections are not available.
Calanus ratio in the North Sea
Note: Continuous Plankton Recorder data. Left: Temporal and seasonal distribution of the Calanus ratio (1958–2009). Right: Change in Calanus ratio in the North Sea between (1958 and 2009).
- CPR Dataset (SAHFOS) provided by Sir Alister Hardy Foundation for Ocean Science (SAHFOS)
Increases in regional sea temperatures have triggered a major northward movement of warmer-water plankton in the North-east Atlantic and a similar retreat of colder-water plankton to the north. This northerly movement is about 10 o latitude (1 100 km) over the past 40 years (a mean poleward movement of between 200 and 250 km per decade), and there appears to have been an acceleration since 2000 [i]. Recently, a Norwegian study showed even faster rates of northward movement between 1997 and 2010. Out of about 1 600 benthic marine species found in coastal waters of southern Norway, 565 species had expanded their distribution northwards along the coast, at rates of 500–800 km per decade [ii]. These rates are much faster than any other documented terrestrial study.
Further changes in the distribution of marine species are expected with projected further climate change, but quantitative projections are not available.
[i] Grégory Beaugrand, „Decadal changes in climate and ecosystems in the North Atlantic Ocean and adjacent seas“, Deep Sea Research Part II: Topical Studies in Oceanography 56, Nr. 8–10 (April 2009): 656–673, doi:10.1016/j.dsr2.2008.12.022.
[ii] T. Brattegard, Endringer i norsk marin bunnfauna 1997-2010 DN-utredning 8-2011 (Trondheim: Direktoratet for naturforvaltning, 2011), http://www.dirnat.no/content/500042260/Endringer-i-norsk-marin-bunnfauna-1997-2010.
Continuous Plankton Recorder (CPR) survey
provided by Sir Alister Hardy Foundation for Ocean Science (SAHFOS)
Policy context and targets
In April 2013 the European Commission presented the EU Adaptation Strategy Package (http://ec.europa.eu/clima/policies/adaptation/what/documentation_en.htm). This package consists of the EU Strategy on adaptation to climate change /* COM/2013/0216 final */ and a number of supporting documents. One of the objectives of the EU Adaptation Strategy is Better informed decision-making, which should occur through Bridging the knowledge gap and Further developing Climate-ADAPT as the ‘one-stop shop’ for adaptation information in Europe. Further objectives include Promoting action by Member States and Climate-proofing EU action: promoting adaptation in key vulnerable sectors. Many EU Member States have already taken action, such as by adopting national adaptation strategies, and several have also prepared action plans on climate change adaptation.
The European Commission and the European Environment Agency have developed the European Climate Adaptation Platform (Climate-ADAPT, http://climate-adapt.eea.europa.eu/) to share knowledge on observed and projected climate change and its impacts on environmental and social systems and on human health; on relevant research; on EU, national and subnational adaptation strategies and plans; and on adaptation case studies.
No targets have been specified.
Related policy documents
Climate-ADAPT: Mainstreaming adaptation in EU sector policies
Overview of EU sector policies in which mainstreaming of adaptation to climate change is ongoing or explored
Climate-ADAPT: National adaptation strategies
Overview of activities of EEA member countries in preparing, developing and implementing adaptation strategies
DG CLIMA: Adaptation to climate change
Adaptation means anticipating the adverse effects of climate change and taking appropriate action to prevent or minimise the damage they can cause, or taking advantage of opportunities that may arise. It has been shown that well planned, early adaptation action saves money and lives later. This webportal provides information on all adaptation activities of the European Commission.
EU Adaptation Strategy Package
In April 2013 the European Commission adopted an EU strategy on adaptation to climate change which has been welcomed by the EU Member States. The strategy aims to make Europe more climate-resilient. By taking a coherent approach and providing for improved coordination, it will enhance the preparedness and capacity of all governance levels to respond to the impacts of climate change.
Methodology for indicator calculation
Data from the Sir Alister Hardy Foundation for Ocean Science (SAHFOS) on Calanus abundance in the central North Sea 1958–2009 is used for the indicator. The Continuous Plankton Recorder (CPR) survey is the longest running, large-scale marine biological survey in the world. The CPR is a near-surface (10 m) plankton sampler voluntarily towed each month behind merchant ships on their normal routes of passage. Methods of analysis for, 400 phyto and zooplankton taxa have remained almost unchanged since 1958.
Methodology for gap filling
No methodology references available.
Data sets uncertainty
In general, changes related to the physical and chemical marine environment are better documented than biological changes because links between cause and effect are better understood and often time series of observations are longer. The longest available records of plankton are from the Continuous Plankton Recorder (CPR) are some 60 years long. It is a sampler that is towed behind many different merchant vessels, along fixed shipping routes. Sampling was started in the North Sea in the 1950s and today a network covering the entire north Atlantic has been established. No other plankton time series of equivalent length and geographical coverage exist for the European regional seas, although many new initiatives investigating species distributions and their changes in Europe’s seas are now emerging.
Further information on uncertainties is provided in Section 1.7 of the EEA report on Climate change, impacts, and vulnerability in Europe 2012 (http://www.eea.europa.eu/publications/climate-impacts-and-vulnerability-2012/)
No uncertainty has been specified
More information about this indicator
See this indicator specification for more details.
Contacts and ownership
EEA Contact InfoTrine Christiansen
EEA Management Plan2012 2.0.1 (note: EEA internal system)
Frequency of updates
For references, please go to www.eea.europa.eu/soer or scan the QR code.
PDF generated on 06 May 2015, 10:19 AM