Phenology of marine species

Indicator Assessment
Prod-ID: IND-101-en
Also known as: CLIM 014
expired Created 09 Nov 2012 Published 20 Nov 2012 Last modified 03 Feb 2017
7 min read
This page was archived on 03 Feb 2017 with reason: No more updates will be done
Temperature increases in the ocean have caused many marine organisms in European seas to appear earlier in their seasonal cycles than in the past. Some plankton species have advanced their seasonal cycle by 4–6 weeks in recent decades. Projections of the phenological responses of individual species are not available, but phenological changes are expected to continue with projected further climate change. Changes in the plankton phenology have important consequences for other organisms within an ecosystem and ultimately for the structure of marine food webs at all trophic levels. Potential consequences include increased vulnerability of North Sea cod stocks to over-fishing and changes in seabird populations.
This indicator is discontinued. No more assessments will be produced.

Key messages

  • Temperature increases in the ocean have caused many marine organisms in European seas to appear earlier in their seasonal cycles than in the past. Some plankton species have advanced their seasonal cycle by 4–6 weeks in recent decades.
  • Projections of the phenological responses of individual species are not available, but phenological changes are expected to continue with projected further climate change.
  • Changes in the plankton phenology have important consequences for other organisms within an ecosystem and ultimately for the structure of marine food webs at all trophic levels. Potential consequences include increased vulnerability of North Sea cod stocks to over-fishing and changes in seabird populations.

How is climate change affecting the seasonal cycle of marine organisms in European seas?

Decapoda larvae abundance and phenology in the central North Sea

Decapoda larvae abundance and phenology in the central North Sea

Note: Left: Decapoda larvae abundance (number of individuals) in the central North Sea (1958–2009). Right: Phenology shown as average month of peak decapoda abundancein the central North Sea (1958–2009).

Data source:

Data provenance info is missing.

Downloads and more info

Past trends

The zooplankton growing season indicator shows the annual timing of peak seasonal abundance of decapoda larvae from 1958–2009 in the central North Sea (Figure 1, left). A shift towards an earlier seasonal peak is clearly visible, in particular since 1988. Since the 1990s the seasonal development of decapoda larvae has occurred 4–6 weeks earlier than the long-term average (baseline mean 1958–2009). This trend towards an earlier seasonal appearance of decapoda larvae during the 1990s is highly correlated with SSTs (Figure 1, right). Even though decapoda larvae are not routinely identified to species level, a recent study has shown that these phenological shifts are a response at the species level, and not simply different seasonal timings by different species [i].

Projections

Projections of the phenological responses of individual species under climate change have not yet been made, but the empirical evidence suggests that phenological changes will continue as climate warming continues. It is currently uncertain as to whether genetic adaptations within species populations can cope with these changes, at least partly, or whether the pace of climate change is too fast for genetic adaptations to take place. This uncertainty is further compounded by the difference in phenological responses between species and functional groups. If current patterns and rates of phenological change are indicative of future trends, future climate warming may exacerbate trophic mismatching. This could further disrupt the functioning, persistence and resilience of many ecosystems, potentially having a major impact on ecosystem services.

[i] John A. Lindley and Richard R. Kirby, „Climate-induced changes in the North Sea Decapoda over the last 60 years“, Climate Research 42, Nr. 3 (September 16, 2010): 257–264.

Indicator specification and metadata

Indicator definition

  • Decapoda larvae abundance and phenology in the central North Sea

Units

  • Mean number of decapods per sample
  • Month of peak abundance

Rationale

Justification for indicator selection

Phenology is the study of annually recurring life-cycle events of species, such as the timing of migrations and flowering of plants. In the marine environment, phenology indicators include the timing of the spring phytoplankton bloom and the peak in abundance of other marine organisms. Change in phenology is one of the key indicators of the impacts of climate change on biological populations. Because marine species have different sensitivities to changes in temperature, these changes may lead to large shifts in the marine food web that can ultimately affect the food available to fish, birds or marine mammals. Differing responses have been seen across various levels of the food web.

Changes in the phenology of different plankton species are seen as a factor contributing to the decline in North Sea cod stocks, which was caused initially by over-fishing, and they have probably affected other fish populations (such as sand eels) that are an essential food source for seabirds.

In the North Sea, work on pelagic phenology has shown that plankton communities, including fish larvae, are very sensitive to regional climate warming. Responses to warming vary between trophic levels and functional groups, which may create a so-called ‘trophic mismatch’ between one species and their food source. The sexual maturation of decapoda larvae has been found to be particularly sensitive to water temperature and is therefore regarded as representative of phenological changes in the shelf-sea environments. Other taxa that also have their seasonal development closely triggered by temperature changes are also highly sensitive (e.g. echinoderm larvae, dinoflagellates, copepods).

Scientific references

  • No rationale references available

Policy context and targets

Context description

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.

Targets

No targets have been specified.

Related policy documents

  • Climate-ADAPT: Adaptation in EU policy sectors
    Overview of EU sector policies in which mainstreaming of adaptation to climate change is ongoing or explored
  • Climate-ADAPT: Country profiles
    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 in the future. This web portal 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 enhances the preparedness and capacity of all governance levels to respond to the impacts of climate change.

Methodology

Methodology for indicator calculation

Data from the Sir Alister Hardy Foundation for Ocean Science (SAHFOS) on Decapoda larvae 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

Not applicable

Methodology references

No methodology references available.

Uncertainties

Methodology uncertainty

Not applicable

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/)

Rationale uncertainty

No uncertainty has been specified

Data sources

Metadata

Topics:

information.png Tags:
DPSIR: Impact
Typology: Descriptive indicator (Type A - What is happening to the environment and to humans?)
Indicator codes
  • CLIM 014
Temporal coverage:
information.png Geographic coverage:

Countries

, , , , , , , , , , , , , , , , , , , , , , , , , ,

Geographical areas

Dates

First draft created:
09 Nov 2012, 03:58 PM
Publish date:
20 Nov 2012, 04:00 PM
Last modified:
03 Feb 2017, 03:00 PM

Frequency of updates

This indicator is discontinued. No more assessments will be produced.

EEA Contact Info

Trine Christiansen

Permalinks

Older versions

Document Actions

For references, please go to https://www.eea.europa.eu/data-and-maps/indicators/marine-phenology-1/assessment or scan the QR code.

PDF generated on 24 Oct 2019, 04:28 AM

EEA Page URL QR
The EEA is an agency of the European Union

Engineered by: EEA Web Team

Software updated on 02 October 2019 07:51 from version 19.9.28

Software version: EEA Plone KGS 19.10.2

Code for developers

Systems Status

Legal notice

Creative commons license

CMS login