Patterns of jellyfish abundance in the North Atlantic

A number of explanations have been advanced to account for the increased frequency and intensity at which jellyfish (pelagic cnidarians and ctenophores) blooms are being observed, most of which have been locally directed. Here, we investigate seasonal and inter-annual patterns in abundance and distr...

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Main Authors: Gibbons, MJ, Richardson, AJ
Format: Article in Journal/Newspaper
Language:unknown
Published: 2009
Subjects:
Online Access:http://plymsea.ac.uk/id/eprint/5741/
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spelling ftplymouthml:oai:plymsea.ac.uk:5741 2023-05-15T17:30:11+02:00 Patterns of jellyfish abundance in the North Atlantic Gibbons, MJ Richardson, AJ 2009 http://plymsea.ac.uk/id/eprint/5741/ unknown Gibbons, MJ; Richardson, AJ. 2009 Patterns of jellyfish abundance in the North Atlantic. Hydrobiologia, 616 (1). 51–65. Publication - Article NonPeerReviewed 2009 ftplymouthml 2022-09-13T05:48:23Z A number of explanations have been advanced to account for the increased frequency and intensity at which jellyfish (pelagic cnidarians and ctenophores) blooms are being observed, most of which have been locally directed. Here, we investigate seasonal and inter-annual patterns in abundance and distribution of jellyfish in the North Atlantic Ocean to determine if there have been any system-wide changes over the period 1946–2005, by analysing records of the presence of coelenterates from the Continuous Plankton Recorder (CPR) survey. Peaks in jellyfish abundance are strongly seasonal in both oceanic and shelf areas: oceanic populations have a mid-year peak that is more closely related to peaks in phyto- and zooplankton, whilst the later peak of shelf populations mirrors changes in SST and reflects processes of advection and aggregation. There have been large amplitude cycles in the abundance of oceanic and shelf jellyfish (although not synchronous) over the last 60 years, with a pronounced synchronous increase in abundance in both areas over the last 10 years. Inter-annual variations in jellyfish abundance in oceanic areas are related to zooplankton abundance and temperature changes, but not to the North Atlantic Oscillation or to a chlorophyll index. The long-term inter-annual abundance of jellyfish on the shelf could not be explained by any environmental variables investigated. As multi-decadal cycles and more recent increase in jellyfish were obvious in both oceanic and shelf areas, we conclude that these are likely to reflect an underlying climatic signal (and bottom-up control) rather than any change in fishing pressure (top-down control). Our results also highlight the role of the CPR data in investigating long-term changes in jellyfish, and suggest that the cnidarians sampled by the CPR are more likely to be holoplanktic hydrozoans and not the much larger meroplanktic scyphozoans as has been suggested previously. Article in Journal/Newspaper North Atlantic North Atlantic oscillation Plymouth Marine Science Electronic Archive (PlyMSEA - Plymouth Marine Laboratory, PML)
institution Open Polar
collection Plymouth Marine Science Electronic Archive (PlyMSEA - Plymouth Marine Laboratory, PML)
op_collection_id ftplymouthml
language unknown
description A number of explanations have been advanced to account for the increased frequency and intensity at which jellyfish (pelagic cnidarians and ctenophores) blooms are being observed, most of which have been locally directed. Here, we investigate seasonal and inter-annual patterns in abundance and distribution of jellyfish in the North Atlantic Ocean to determine if there have been any system-wide changes over the period 1946–2005, by analysing records of the presence of coelenterates from the Continuous Plankton Recorder (CPR) survey. Peaks in jellyfish abundance are strongly seasonal in both oceanic and shelf areas: oceanic populations have a mid-year peak that is more closely related to peaks in phyto- and zooplankton, whilst the later peak of shelf populations mirrors changes in SST and reflects processes of advection and aggregation. There have been large amplitude cycles in the abundance of oceanic and shelf jellyfish (although not synchronous) over the last 60 years, with a pronounced synchronous increase in abundance in both areas over the last 10 years. Inter-annual variations in jellyfish abundance in oceanic areas are related to zooplankton abundance and temperature changes, but not to the North Atlantic Oscillation or to a chlorophyll index. The long-term inter-annual abundance of jellyfish on the shelf could not be explained by any environmental variables investigated. As multi-decadal cycles and more recent increase in jellyfish were obvious in both oceanic and shelf areas, we conclude that these are likely to reflect an underlying climatic signal (and bottom-up control) rather than any change in fishing pressure (top-down control). Our results also highlight the role of the CPR data in investigating long-term changes in jellyfish, and suggest that the cnidarians sampled by the CPR are more likely to be holoplanktic hydrozoans and not the much larger meroplanktic scyphozoans as has been suggested previously.
format Article in Journal/Newspaper
author Gibbons, MJ
Richardson, AJ
spellingShingle Gibbons, MJ
Richardson, AJ
Patterns of jellyfish abundance in the North Atlantic
author_facet Gibbons, MJ
Richardson, AJ
author_sort Gibbons, MJ
title Patterns of jellyfish abundance in the North Atlantic
title_short Patterns of jellyfish abundance in the North Atlantic
title_full Patterns of jellyfish abundance in the North Atlantic
title_fullStr Patterns of jellyfish abundance in the North Atlantic
title_full_unstemmed Patterns of jellyfish abundance in the North Atlantic
title_sort patterns of jellyfish abundance in the north atlantic
publishDate 2009
url http://plymsea.ac.uk/id/eprint/5741/
genre North Atlantic
North Atlantic oscillation
genre_facet North Atlantic
North Atlantic oscillation
op_relation Gibbons, MJ; Richardson, AJ. 2009 Patterns of jellyfish abundance in the North Atlantic. Hydrobiologia, 616 (1). 51–65.
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