Impact of oceanic warming on the distribution of seaweeds in polar and cold-temperate waters

Abstract Temperature is one of the most important factors controlling the biogeographic distribution of seaweeds and is expected to increase due to the rise in anthropogenic greenhouse gas concentrations, especially in polar and cold-temperate regions. To estimate prospective distributional shifts i...

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Published in:botm
Main Authors: Müller, Ruth, Laepple, Thomas, Bartsch, Inka, Wiencke, Christian
Format: Article in Journal/Newspaper
Language:English
Published: Walter de Gruyter GmbH 2009
Subjects:
Online Access:http://dx.doi.org/10.1515/bot.2009.080
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spelling crdegruyter:10.1515/bot.2009.080 2024-09-30T14:26:57+00:00 Impact of oceanic warming on the distribution of seaweeds in polar and cold-temperate waters Müller, Ruth Laepple, Thomas Bartsch, Inka Wiencke, Christian 2009 http://dx.doi.org/10.1515/bot.2009.080 https://www.degruyter.com/document/doi/10.1515/BOT.2009.080/xml https://www.degruyter.com/document/doi/10.1515/BOT.2009.080/pdf en eng Walter de Gruyter GmbH botm volume 52, issue 6, page 617-638 ISSN 1437-4323 0006-8055 journal-article 2009 crdegruyter https://doi.org/10.1515/bot.2009.080 2024-09-02T04:07:51Z Abstract Temperature is one of the most important factors controlling the biogeographic distribution of seaweeds and is expected to increase due to the rise in anthropogenic greenhouse gas concentrations, especially in polar and cold-temperate regions. To estimate prospective distributional shifts in cold-water key structural seaweeds from both hemispheres, we related temperature requirements and recent distributions of seaweeds to observed mean sea surface temperature (SST) isotherms for the periods 1980–1999 (Meteorological Office Hadley Centre's SST data set; HadISST) and to modelled temperatures for 2080–2099 [Coupled Model Intercomparison Project 3 (CMIP3) database prepared for the Intergovernmental Panel on Climate Change Fourth Assessment Report (IPCC AR4) report] based on moderate greenhouse gas emissions Special Report on Emission Scenarios – Scenario B1 (SRESA1B). Under this scenario, North Atlantic polar to cold-temperate seaweeds investigated will extend their distribution into the High Arctic until the end of the 21st century, but retreat along the northeastern Atlantic coastline. In contrast, selected Antarctic seaweeds will probably not significantly alter their latitudinal distributions, as deduced from our presently incomplete knowledge of their temperature requirements. We identified several cold-temperate regions where seaweed composition and abundance will certainly change with elevated temperatures. The results are discussed in the context of local temperature conditions, effects of multifactorial abiotic and biotic interactions and expected ecological consequences for seaweed-dominated ecosystems. Article in Journal/Newspaper Antarc* Antarctic Arctic Climate change North Atlantic De Gruyter Arctic Antarctic botm 52 6 617 638
institution Open Polar
collection De Gruyter
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language English
description Abstract Temperature is one of the most important factors controlling the biogeographic distribution of seaweeds and is expected to increase due to the rise in anthropogenic greenhouse gas concentrations, especially in polar and cold-temperate regions. To estimate prospective distributional shifts in cold-water key structural seaweeds from both hemispheres, we related temperature requirements and recent distributions of seaweeds to observed mean sea surface temperature (SST) isotherms for the periods 1980–1999 (Meteorological Office Hadley Centre's SST data set; HadISST) and to modelled temperatures for 2080–2099 [Coupled Model Intercomparison Project 3 (CMIP3) database prepared for the Intergovernmental Panel on Climate Change Fourth Assessment Report (IPCC AR4) report] based on moderate greenhouse gas emissions Special Report on Emission Scenarios – Scenario B1 (SRESA1B). Under this scenario, North Atlantic polar to cold-temperate seaweeds investigated will extend their distribution into the High Arctic until the end of the 21st century, but retreat along the northeastern Atlantic coastline. In contrast, selected Antarctic seaweeds will probably not significantly alter their latitudinal distributions, as deduced from our presently incomplete knowledge of their temperature requirements. We identified several cold-temperate regions where seaweed composition and abundance will certainly change with elevated temperatures. The results are discussed in the context of local temperature conditions, effects of multifactorial abiotic and biotic interactions and expected ecological consequences for seaweed-dominated ecosystems.
format Article in Journal/Newspaper
author Müller, Ruth
Laepple, Thomas
Bartsch, Inka
Wiencke, Christian
spellingShingle Müller, Ruth
Laepple, Thomas
Bartsch, Inka
Wiencke, Christian
Impact of oceanic warming on the distribution of seaweeds in polar and cold-temperate waters
author_facet Müller, Ruth
Laepple, Thomas
Bartsch, Inka
Wiencke, Christian
author_sort Müller, Ruth
title Impact of oceanic warming on the distribution of seaweeds in polar and cold-temperate waters
title_short Impact of oceanic warming on the distribution of seaweeds in polar and cold-temperate waters
title_full Impact of oceanic warming on the distribution of seaweeds in polar and cold-temperate waters
title_fullStr Impact of oceanic warming on the distribution of seaweeds in polar and cold-temperate waters
title_full_unstemmed Impact of oceanic warming on the distribution of seaweeds in polar and cold-temperate waters
title_sort impact of oceanic warming on the distribution of seaweeds in polar and cold-temperate waters
publisher Walter de Gruyter GmbH
publishDate 2009
url http://dx.doi.org/10.1515/bot.2009.080
https://www.degruyter.com/document/doi/10.1515/BOT.2009.080/xml
https://www.degruyter.com/document/doi/10.1515/BOT.2009.080/pdf
geographic Arctic
Antarctic
geographic_facet Arctic
Antarctic
genre Antarc*
Antarctic
Arctic
Climate change
North Atlantic
genre_facet Antarc*
Antarctic
Arctic
Climate change
North Atlantic
op_source botm
volume 52, issue 6, page 617-638
ISSN 1437-4323 0006-8055
op_doi https://doi.org/10.1515/bot.2009.080
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