Increased blooms of a dinoflagellate in the NW Atlantic
Sampling by the Continuous Plankton Recorder (CPR) over the NW Atlantic from 1960 to 2000 has enabled long-term studies of the larger components of the phytoplankton community, highlighting various changes, particularly during the 1990s. Analysis of an index of phytoplankton biomass, the Phytoplankt...
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Language: | English |
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ftunivqespace:oai:espace.library.uq.edu.au:UQ:111275 2023-05-15T17:22:22+02:00 Increased blooms of a dinoflagellate in the NW Atlantic Johns, D. G. Edwards, M. Richardson, A. Spicer, J. I. 2003-01-01 https://espace.library.uq.edu.au/view/UQ:111275 eng eng Inter-Research doi:10.3354/meps265283 issn:0171-8630 issn:1616-1599 orcid:0000-0002-9289-7366 Ecology Marine & Freshwater Biology Oceanography phytoplankton long-term changes blooms NW Atlantic Ceratium arcticum Continuous Plankton Recorder Plankton Recorder Survey Newfoundland Ocean Journal Article 2003 ftunivqespace https://doi.org/10.3354/meps265283 2020-08-04T06:37:34Z Sampling by the Continuous Plankton Recorder (CPR) over the NW Atlantic from 1960 to 2000 has enabled long-term studies of the larger components of the phytoplankton community, highlighting various changes, particularly during the 1990s. Analysis of an index of phytoplankton biomass, the Phytoplankton Colour Index (PCI) has revealed an increase over the past decade, most marked during the winter (December to February) months. Examination of the structure of the community using multiple linear-regression models indicates that the winter phytoplankton community composition has changed markedly in the 1990s compared to the 1960s. One phytoplankter, the dinoflagellate Ceratium arcticum (Cleve), has undergone dramatic changes in abundance during this period, with pronounced large winter blooms and decreased autumnal levels, and its contribution to the Phytoplankton Colour index values has increased significantly. Other dominant species in the phytoplankton community, both diatoms and dinoflagellates, did not show the same variations over the examined time period. It is suggested that the response of C. arcticum is probably a result of previously reported changes in stratification in the NW Atlantic, due to dynamic hydro-climatic (freshening and cooling) events. Article in Journal/Newspaper Newfoundland The University of Queensland: UQ eSpace Marine Ecology Progress Series 265 283 287 |
institution |
Open Polar |
collection |
The University of Queensland: UQ eSpace |
op_collection_id |
ftunivqespace |
language |
English |
topic |
Ecology Marine & Freshwater Biology Oceanography phytoplankton long-term changes blooms NW Atlantic Ceratium arcticum Continuous Plankton Recorder Plankton Recorder Survey Newfoundland Ocean |
spellingShingle |
Ecology Marine & Freshwater Biology Oceanography phytoplankton long-term changes blooms NW Atlantic Ceratium arcticum Continuous Plankton Recorder Plankton Recorder Survey Newfoundland Ocean Johns, D. G. Edwards, M. Richardson, A. Spicer, J. I. Increased blooms of a dinoflagellate in the NW Atlantic |
topic_facet |
Ecology Marine & Freshwater Biology Oceanography phytoplankton long-term changes blooms NW Atlantic Ceratium arcticum Continuous Plankton Recorder Plankton Recorder Survey Newfoundland Ocean |
description |
Sampling by the Continuous Plankton Recorder (CPR) over the NW Atlantic from 1960 to 2000 has enabled long-term studies of the larger components of the phytoplankton community, highlighting various changes, particularly during the 1990s. Analysis of an index of phytoplankton biomass, the Phytoplankton Colour Index (PCI) has revealed an increase over the past decade, most marked during the winter (December to February) months. Examination of the structure of the community using multiple linear-regression models indicates that the winter phytoplankton community composition has changed markedly in the 1990s compared to the 1960s. One phytoplankter, the dinoflagellate Ceratium arcticum (Cleve), has undergone dramatic changes in abundance during this period, with pronounced large winter blooms and decreased autumnal levels, and its contribution to the Phytoplankton Colour index values has increased significantly. Other dominant species in the phytoplankton community, both diatoms and dinoflagellates, did not show the same variations over the examined time period. It is suggested that the response of C. arcticum is probably a result of previously reported changes in stratification in the NW Atlantic, due to dynamic hydro-climatic (freshening and cooling) events. |
format |
Article in Journal/Newspaper |
author |
Johns, D. G. Edwards, M. Richardson, A. Spicer, J. I. |
author_facet |
Johns, D. G. Edwards, M. Richardson, A. Spicer, J. I. |
author_sort |
Johns, D. G. |
title |
Increased blooms of a dinoflagellate in the NW Atlantic |
title_short |
Increased blooms of a dinoflagellate in the NW Atlantic |
title_full |
Increased blooms of a dinoflagellate in the NW Atlantic |
title_fullStr |
Increased blooms of a dinoflagellate in the NW Atlantic |
title_full_unstemmed |
Increased blooms of a dinoflagellate in the NW Atlantic |
title_sort |
increased blooms of a dinoflagellate in the nw atlantic |
publisher |
Inter-Research |
publishDate |
2003 |
url |
https://espace.library.uq.edu.au/view/UQ:111275 |
genre |
Newfoundland |
genre_facet |
Newfoundland |
op_relation |
doi:10.3354/meps265283 issn:0171-8630 issn:1616-1599 orcid:0000-0002-9289-7366 |
op_doi |
https://doi.org/10.3354/meps265283 |
container_title |
Marine Ecology Progress Series |
container_volume |
265 |
container_start_page |
283 |
op_container_end_page |
287 |
_version_ |
1766108977241784320 |