Climate-driven regime shift of a temperate marine ecosystem
Ecosystems over time have endured much disturbance, yet they tend to remain intact, a characteristic we call resilience. Though many systems have been lost and destroyed, for systems that remain physically intact, there is debate as to whether changing temperatures will result in shifts or collapses...
Ausführliche Beschreibung
Autor*in: |
Thomas Wernberg [verfasserIn] |
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Format: |
Artikel |
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Sprache: |
Englisch |
Erschienen: |
2016 |
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Rechteinformationen: |
Nutzungsrecht: Copyright © 2016, American Association for the Advancement of Science. |
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Übergeordnetes Werk: |
Enthalten in: Science - Washington, DC : AAAS, American Assoc. for the Advancement of Science, 1883, 353(2016), 6295, Seite 169-172 |
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Übergeordnetes Werk: |
volume:353 ; year:2016 ; number:6295 ; pages:169-172 |
Links: |
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DOI / URN: |
10.1126/science.aad8745 |
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OLC197902250X |
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520 | |a Ecosystems over time have endured much disturbance, yet they tend to remain intact, a characteristic we call resilience. Though many systems have been lost and destroyed, for systems that remain physically intact, there is debate as to whether changing temperatures will result in shifts or collapses. Wernburg et al. show that extreme warming of a temperate kelp forest off Australia resulted not only in its collapse, but also in a shift in community composition that brought about an increase in herbivorous tropical fishes that prevent the reestablishment of kelp. Thus, many systems may not be resilient to the rapid climate change that we face. Science, this issue p. 169 Ecosystem reconfigurations arising from climate-driven changes in species distributions are expected to have profound ecological, social, and economic implications. Here we reveal a rapid climate-driven regime shift of Australian temperate reef communities, which lost their defining kelp forests and became dominated by persistent seaweed turfs. After decades of ocean warming, extreme marine heat waves forced a 100-kilometer range contraction of extensive kelp forests and saw temperate species replaced by seaweeds, invertebrates, corals, and fishes characteristic of subtropical and tropical waters. This community-wide tropicalization fundamentally altered key ecological processes, suppressing the recovery of kelp forests. | ||
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10.1126/science.aad8745 doi PQ20160720 (DE-627)OLC197902250X (DE-599)GBVOLC197902250X (PRQ)c1201-d3a9dffdaeaf52642626501549554048fc422968f9a49e939bf81a2e4f4ce02c0 (KEY)0063888920160000353629500169climatedrivenregimeshiftofatemperatemarineecosyste DE-627 ger DE-627 rakwb eng 500 DNB LING fid Thomas Wernberg verfasserin aut Climate-driven regime shift of a temperate marine ecosystem 2016 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier Ecosystems over time have endured much disturbance, yet they tend to remain intact, a characteristic we call resilience. Though many systems have been lost and destroyed, for systems that remain physically intact, there is debate as to whether changing temperatures will result in shifts or collapses. Wernburg et al. show that extreme warming of a temperate kelp forest off Australia resulted not only in its collapse, but also in a shift in community composition that brought about an increase in herbivorous tropical fishes that prevent the reestablishment of kelp. Thus, many systems may not be resilient to the rapid climate change that we face. Science, this issue p. 169 Ecosystem reconfigurations arising from climate-driven changes in species distributions are expected to have profound ecological, social, and economic implications. Here we reveal a rapid climate-driven regime shift of Australian temperate reef communities, which lost their defining kelp forests and became dominated by persistent seaweed turfs. After decades of ocean warming, extreme marine heat waves forced a 100-kilometer range contraction of extensive kelp forests and saw temperate species replaced by seaweeds, invertebrates, corals, and fishes characteristic of subtropical and tropical waters. This community-wide tropicalization fundamentally altered key ecological processes, suppressing the recovery of kelp forests. Nutzungsrecht: Copyright © 2016, American Association for the Advancement of Science. Scott Bennett oth Russell C Babcock oth Thibaut de Bettignies oth Katherine Cure oth Martial Depczynski oth Francois Dufois oth Jane Fromont oth Christopher J Fulton oth Renae K Hovey oth Euan S Harvey oth Thomas H Holmes oth Gary A Kendrick oth Ben Radford oth Julia Santana-Garcon oth Benjamin J Saunders oth Dan A Smale oth Mads S Thomsen oth Chenae A Tuckett oth Fernando Tuya oth Mathew A Vanderklift oth Shaun Wilson oth Enthalten in Science Washington, DC : AAAS, American Assoc. for the Advancement of Science, 1883 353(2016), 6295, Seite 169-172 (DE-627)12931482X (DE-600)128410-1 (DE-576)014533189 0036-8075 nnns volume:353 year:2016 number:6295 pages:169-172 http://dx.doi.org/10.1126/science.aad8745 Volltext http://www.ncbi.nlm.nih.gov/pubmed/27387951 http://search.proquest.com/docview/1802501251 GBV_USEFLAG_A SYSFLAG_A GBV_OLC FID-LING SSG-OLC-PHY SSG-OLC-CHE SSG-OLC-MAT SSG-OLC-FOR SSG-OLC-SPO SSG-OLC-IBL SSG-OLC-PHA SSG-OLC-DE-84 SSG-OPC-FOR GBV_ILN_11 GBV_ILN_20 GBV_ILN_21 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_30 GBV_ILN_31 GBV_ILN_39 GBV_ILN_40 GBV_ILN_47 GBV_ILN_55 GBV_ILN_59 GBV_ILN_60 GBV_ILN_62 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_92 GBV_ILN_101 GBV_ILN_110 GBV_ILN_120 GBV_ILN_131 GBV_ILN_170 GBV_ILN_171 GBV_ILN_179 GBV_ILN_181 GBV_ILN_211 GBV_ILN_252 GBV_ILN_259 GBV_ILN_290 GBV_ILN_600 GBV_ILN_601 GBV_ILN_647 GBV_ILN_754 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2012 GBV_ILN_2015 GBV_ILN_2018 GBV_ILN_2020 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2116 GBV_ILN_2120 GBV_ILN_2121 GBV_ILN_2173 GBV_ILN_2219 GBV_ILN_2221 GBV_ILN_2279 GBV_ILN_2286 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4036 GBV_ILN_4125 GBV_ILN_4219 GBV_ILN_4251 GBV_ILN_4277 GBV_ILN_4302 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4310 GBV_ILN_4314 GBV_ILN_4317 GBV_ILN_4318 GBV_ILN_4320 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4700 AR 353 2016 6295 169-172 |
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10.1126/science.aad8745 doi PQ20160720 (DE-627)OLC197902250X (DE-599)GBVOLC197902250X (PRQ)c1201-d3a9dffdaeaf52642626501549554048fc422968f9a49e939bf81a2e4f4ce02c0 (KEY)0063888920160000353629500169climatedrivenregimeshiftofatemperatemarineecosyste DE-627 ger DE-627 rakwb eng 500 DNB LING fid Thomas Wernberg verfasserin aut Climate-driven regime shift of a temperate marine ecosystem 2016 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier Ecosystems over time have endured much disturbance, yet they tend to remain intact, a characteristic we call resilience. Though many systems have been lost and destroyed, for systems that remain physically intact, there is debate as to whether changing temperatures will result in shifts or collapses. Wernburg et al. show that extreme warming of a temperate kelp forest off Australia resulted not only in its collapse, but also in a shift in community composition that brought about an increase in herbivorous tropical fishes that prevent the reestablishment of kelp. Thus, many systems may not be resilient to the rapid climate change that we face. Science, this issue p. 169 Ecosystem reconfigurations arising from climate-driven changes in species distributions are expected to have profound ecological, social, and economic implications. Here we reveal a rapid climate-driven regime shift of Australian temperate reef communities, which lost their defining kelp forests and became dominated by persistent seaweed turfs. After decades of ocean warming, extreme marine heat waves forced a 100-kilometer range contraction of extensive kelp forests and saw temperate species replaced by seaweeds, invertebrates, corals, and fishes characteristic of subtropical and tropical waters. This community-wide tropicalization fundamentally altered key ecological processes, suppressing the recovery of kelp forests. Nutzungsrecht: Copyright © 2016, American Association for the Advancement of Science. Scott Bennett oth Russell C Babcock oth Thibaut de Bettignies oth Katherine Cure oth Martial Depczynski oth Francois Dufois oth Jane Fromont oth Christopher J Fulton oth Renae K Hovey oth Euan S Harvey oth Thomas H Holmes oth Gary A Kendrick oth Ben Radford oth Julia Santana-Garcon oth Benjamin J Saunders oth Dan A Smale oth Mads S Thomsen oth Chenae A Tuckett oth Fernando Tuya oth Mathew A Vanderklift oth Shaun Wilson oth Enthalten in Science Washington, DC : AAAS, American Assoc. for the Advancement of Science, 1883 353(2016), 6295, Seite 169-172 (DE-627)12931482X (DE-600)128410-1 (DE-576)014533189 0036-8075 nnns volume:353 year:2016 number:6295 pages:169-172 http://dx.doi.org/10.1126/science.aad8745 Volltext http://www.ncbi.nlm.nih.gov/pubmed/27387951 http://search.proquest.com/docview/1802501251 GBV_USEFLAG_A SYSFLAG_A GBV_OLC FID-LING SSG-OLC-PHY SSG-OLC-CHE SSG-OLC-MAT SSG-OLC-FOR SSG-OLC-SPO SSG-OLC-IBL SSG-OLC-PHA SSG-OLC-DE-84 SSG-OPC-FOR GBV_ILN_11 GBV_ILN_20 GBV_ILN_21 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_30 GBV_ILN_31 GBV_ILN_39 GBV_ILN_40 GBV_ILN_47 GBV_ILN_55 GBV_ILN_59 GBV_ILN_60 GBV_ILN_62 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_92 GBV_ILN_101 GBV_ILN_110 GBV_ILN_120 GBV_ILN_131 GBV_ILN_170 GBV_ILN_171 GBV_ILN_179 GBV_ILN_181 GBV_ILN_211 GBV_ILN_252 GBV_ILN_259 GBV_ILN_290 GBV_ILN_600 GBV_ILN_601 GBV_ILN_647 GBV_ILN_754 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2012 GBV_ILN_2015 GBV_ILN_2018 GBV_ILN_2020 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2116 GBV_ILN_2120 GBV_ILN_2121 GBV_ILN_2173 GBV_ILN_2219 GBV_ILN_2221 GBV_ILN_2279 GBV_ILN_2286 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4036 GBV_ILN_4125 GBV_ILN_4219 GBV_ILN_4251 GBV_ILN_4277 GBV_ILN_4302 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4310 GBV_ILN_4314 GBV_ILN_4317 GBV_ILN_4318 GBV_ILN_4320 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4700 AR 353 2016 6295 169-172 |
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10.1126/science.aad8745 doi PQ20160720 (DE-627)OLC197902250X (DE-599)GBVOLC197902250X (PRQ)c1201-d3a9dffdaeaf52642626501549554048fc422968f9a49e939bf81a2e4f4ce02c0 (KEY)0063888920160000353629500169climatedrivenregimeshiftofatemperatemarineecosyste DE-627 ger DE-627 rakwb eng 500 DNB LING fid Thomas Wernberg verfasserin aut Climate-driven regime shift of a temperate marine ecosystem 2016 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier Ecosystems over time have endured much disturbance, yet they tend to remain intact, a characteristic we call resilience. Though many systems have been lost and destroyed, for systems that remain physically intact, there is debate as to whether changing temperatures will result in shifts or collapses. Wernburg et al. show that extreme warming of a temperate kelp forest off Australia resulted not only in its collapse, but also in a shift in community composition that brought about an increase in herbivorous tropical fishes that prevent the reestablishment of kelp. Thus, many systems may not be resilient to the rapid climate change that we face. Science, this issue p. 169 Ecosystem reconfigurations arising from climate-driven changes in species distributions are expected to have profound ecological, social, and economic implications. Here we reveal a rapid climate-driven regime shift of Australian temperate reef communities, which lost their defining kelp forests and became dominated by persistent seaweed turfs. After decades of ocean warming, extreme marine heat waves forced a 100-kilometer range contraction of extensive kelp forests and saw temperate species replaced by seaweeds, invertebrates, corals, and fishes characteristic of subtropical and tropical waters. This community-wide tropicalization fundamentally altered key ecological processes, suppressing the recovery of kelp forests. Nutzungsrecht: Copyright © 2016, American Association for the Advancement of Science. Scott Bennett oth Russell C Babcock oth Thibaut de Bettignies oth Katherine Cure oth Martial Depczynski oth Francois Dufois oth Jane Fromont oth Christopher J Fulton oth Renae K Hovey oth Euan S Harvey oth Thomas H Holmes oth Gary A Kendrick oth Ben Radford oth Julia Santana-Garcon oth Benjamin J Saunders oth Dan A Smale oth Mads S Thomsen oth Chenae A Tuckett oth Fernando Tuya oth Mathew A Vanderklift oth Shaun Wilson oth Enthalten in Science Washington, DC : AAAS, American Assoc. for the Advancement of Science, 1883 353(2016), 6295, Seite 169-172 (DE-627)12931482X (DE-600)128410-1 (DE-576)014533189 0036-8075 nnns volume:353 year:2016 number:6295 pages:169-172 http://dx.doi.org/10.1126/science.aad8745 Volltext http://www.ncbi.nlm.nih.gov/pubmed/27387951 http://search.proquest.com/docview/1802501251 GBV_USEFLAG_A SYSFLAG_A GBV_OLC FID-LING SSG-OLC-PHY SSG-OLC-CHE SSG-OLC-MAT SSG-OLC-FOR SSG-OLC-SPO SSG-OLC-IBL SSG-OLC-PHA SSG-OLC-DE-84 SSG-OPC-FOR GBV_ILN_11 GBV_ILN_20 GBV_ILN_21 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_30 GBV_ILN_31 GBV_ILN_39 GBV_ILN_40 GBV_ILN_47 GBV_ILN_55 GBV_ILN_59 GBV_ILN_60 GBV_ILN_62 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_92 GBV_ILN_101 GBV_ILN_110 GBV_ILN_120 GBV_ILN_131 GBV_ILN_170 GBV_ILN_171 GBV_ILN_179 GBV_ILN_181 GBV_ILN_211 GBV_ILN_252 GBV_ILN_259 GBV_ILN_290 GBV_ILN_600 GBV_ILN_601 GBV_ILN_647 GBV_ILN_754 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2012 GBV_ILN_2015 GBV_ILN_2018 GBV_ILN_2020 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2116 GBV_ILN_2120 GBV_ILN_2121 GBV_ILN_2173 GBV_ILN_2219 GBV_ILN_2221 GBV_ILN_2279 GBV_ILN_2286 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4036 GBV_ILN_4125 GBV_ILN_4219 GBV_ILN_4251 GBV_ILN_4277 GBV_ILN_4302 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4310 GBV_ILN_4314 GBV_ILN_4317 GBV_ILN_4318 GBV_ILN_4320 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4700 AR 353 2016 6295 169-172 |
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10.1126/science.aad8745 doi PQ20160720 (DE-627)OLC197902250X (DE-599)GBVOLC197902250X (PRQ)c1201-d3a9dffdaeaf52642626501549554048fc422968f9a49e939bf81a2e4f4ce02c0 (KEY)0063888920160000353629500169climatedrivenregimeshiftofatemperatemarineecosyste DE-627 ger DE-627 rakwb eng 500 DNB LING fid Thomas Wernberg verfasserin aut Climate-driven regime shift of a temperate marine ecosystem 2016 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier Ecosystems over time have endured much disturbance, yet they tend to remain intact, a characteristic we call resilience. Though many systems have been lost and destroyed, for systems that remain physically intact, there is debate as to whether changing temperatures will result in shifts or collapses. Wernburg et al. show that extreme warming of a temperate kelp forest off Australia resulted not only in its collapse, but also in a shift in community composition that brought about an increase in herbivorous tropical fishes that prevent the reestablishment of kelp. Thus, many systems may not be resilient to the rapid climate change that we face. Science, this issue p. 169 Ecosystem reconfigurations arising from climate-driven changes in species distributions are expected to have profound ecological, social, and economic implications. Here we reveal a rapid climate-driven regime shift of Australian temperate reef communities, which lost their defining kelp forests and became dominated by persistent seaweed turfs. After decades of ocean warming, extreme marine heat waves forced a 100-kilometer range contraction of extensive kelp forests and saw temperate species replaced by seaweeds, invertebrates, corals, and fishes characteristic of subtropical and tropical waters. This community-wide tropicalization fundamentally altered key ecological processes, suppressing the recovery of kelp forests. Nutzungsrecht: Copyright © 2016, American Association for the Advancement of Science. Scott Bennett oth Russell C Babcock oth Thibaut de Bettignies oth Katherine Cure oth Martial Depczynski oth Francois Dufois oth Jane Fromont oth Christopher J Fulton oth Renae K Hovey oth Euan S Harvey oth Thomas H Holmes oth Gary A Kendrick oth Ben Radford oth Julia Santana-Garcon oth Benjamin J Saunders oth Dan A Smale oth Mads S Thomsen oth Chenae A Tuckett oth Fernando Tuya oth Mathew A Vanderklift oth Shaun Wilson oth Enthalten in Science Washington, DC : AAAS, American Assoc. for the Advancement of Science, 1883 353(2016), 6295, Seite 169-172 (DE-627)12931482X (DE-600)128410-1 (DE-576)014533189 0036-8075 nnns volume:353 year:2016 number:6295 pages:169-172 http://dx.doi.org/10.1126/science.aad8745 Volltext http://www.ncbi.nlm.nih.gov/pubmed/27387951 http://search.proquest.com/docview/1802501251 GBV_USEFLAG_A SYSFLAG_A GBV_OLC FID-LING SSG-OLC-PHY SSG-OLC-CHE SSG-OLC-MAT SSG-OLC-FOR SSG-OLC-SPO SSG-OLC-IBL SSG-OLC-PHA SSG-OLC-DE-84 SSG-OPC-FOR GBV_ILN_11 GBV_ILN_20 GBV_ILN_21 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_30 GBV_ILN_31 GBV_ILN_39 GBV_ILN_40 GBV_ILN_47 GBV_ILN_55 GBV_ILN_59 GBV_ILN_60 GBV_ILN_62 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_92 GBV_ILN_101 GBV_ILN_110 GBV_ILN_120 GBV_ILN_131 GBV_ILN_170 GBV_ILN_171 GBV_ILN_179 GBV_ILN_181 GBV_ILN_211 GBV_ILN_252 GBV_ILN_259 GBV_ILN_290 GBV_ILN_600 GBV_ILN_601 GBV_ILN_647 GBV_ILN_754 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2012 GBV_ILN_2015 GBV_ILN_2018 GBV_ILN_2020 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2116 GBV_ILN_2120 GBV_ILN_2121 GBV_ILN_2173 GBV_ILN_2219 GBV_ILN_2221 GBV_ILN_2279 GBV_ILN_2286 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4036 GBV_ILN_4125 GBV_ILN_4219 GBV_ILN_4251 GBV_ILN_4277 GBV_ILN_4302 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4310 GBV_ILN_4314 GBV_ILN_4317 GBV_ILN_4318 GBV_ILN_4320 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4700 AR 353 2016 6295 169-172 |
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10.1126/science.aad8745 doi PQ20160720 (DE-627)OLC197902250X (DE-599)GBVOLC197902250X (PRQ)c1201-d3a9dffdaeaf52642626501549554048fc422968f9a49e939bf81a2e4f4ce02c0 (KEY)0063888920160000353629500169climatedrivenregimeshiftofatemperatemarineecosyste DE-627 ger DE-627 rakwb eng 500 DNB LING fid Thomas Wernberg verfasserin aut Climate-driven regime shift of a temperate marine ecosystem 2016 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier Ecosystems over time have endured much disturbance, yet they tend to remain intact, a characteristic we call resilience. Though many systems have been lost and destroyed, for systems that remain physically intact, there is debate as to whether changing temperatures will result in shifts or collapses. Wernburg et al. show that extreme warming of a temperate kelp forest off Australia resulted not only in its collapse, but also in a shift in community composition that brought about an increase in herbivorous tropical fishes that prevent the reestablishment of kelp. Thus, many systems may not be resilient to the rapid climate change that we face. Science, this issue p. 169 Ecosystem reconfigurations arising from climate-driven changes in species distributions are expected to have profound ecological, social, and economic implications. Here we reveal a rapid climate-driven regime shift of Australian temperate reef communities, which lost their defining kelp forests and became dominated by persistent seaweed turfs. After decades of ocean warming, extreme marine heat waves forced a 100-kilometer range contraction of extensive kelp forests and saw temperate species replaced by seaweeds, invertebrates, corals, and fishes characteristic of subtropical and tropical waters. This community-wide tropicalization fundamentally altered key ecological processes, suppressing the recovery of kelp forests. Nutzungsrecht: Copyright © 2016, American Association for the Advancement of Science. Scott Bennett oth Russell C Babcock oth Thibaut de Bettignies oth Katherine Cure oth Martial Depczynski oth Francois Dufois oth Jane Fromont oth Christopher J Fulton oth Renae K Hovey oth Euan S Harvey oth Thomas H Holmes oth Gary A Kendrick oth Ben Radford oth Julia Santana-Garcon oth Benjamin J Saunders oth Dan A Smale oth Mads S Thomsen oth Chenae A Tuckett oth Fernando Tuya oth Mathew A Vanderklift oth Shaun Wilson oth Enthalten in Science Washington, DC : AAAS, American Assoc. for the Advancement of Science, 1883 353(2016), 6295, Seite 169-172 (DE-627)12931482X (DE-600)128410-1 (DE-576)014533189 0036-8075 nnns volume:353 year:2016 number:6295 pages:169-172 http://dx.doi.org/10.1126/science.aad8745 Volltext http://www.ncbi.nlm.nih.gov/pubmed/27387951 http://search.proquest.com/docview/1802501251 GBV_USEFLAG_A SYSFLAG_A GBV_OLC FID-LING SSG-OLC-PHY SSG-OLC-CHE SSG-OLC-MAT SSG-OLC-FOR SSG-OLC-SPO SSG-OLC-IBL SSG-OLC-PHA SSG-OLC-DE-84 SSG-OPC-FOR GBV_ILN_11 GBV_ILN_20 GBV_ILN_21 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_30 GBV_ILN_31 GBV_ILN_39 GBV_ILN_40 GBV_ILN_47 GBV_ILN_55 GBV_ILN_59 GBV_ILN_60 GBV_ILN_62 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_92 GBV_ILN_101 GBV_ILN_110 GBV_ILN_120 GBV_ILN_131 GBV_ILN_170 GBV_ILN_171 GBV_ILN_179 GBV_ILN_181 GBV_ILN_211 GBV_ILN_252 GBV_ILN_259 GBV_ILN_290 GBV_ILN_600 GBV_ILN_601 GBV_ILN_647 GBV_ILN_754 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2012 GBV_ILN_2015 GBV_ILN_2018 GBV_ILN_2020 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2116 GBV_ILN_2120 GBV_ILN_2121 GBV_ILN_2173 GBV_ILN_2219 GBV_ILN_2221 GBV_ILN_2279 GBV_ILN_2286 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4036 GBV_ILN_4125 GBV_ILN_4219 GBV_ILN_4251 GBV_ILN_4277 GBV_ILN_4302 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4310 GBV_ILN_4314 GBV_ILN_4317 GBV_ILN_4318 GBV_ILN_4320 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4700 AR 353 2016 6295 169-172 |
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Thomas Wernberg @@aut@@ Scott Bennett @@oth@@ Russell C Babcock @@oth@@ Thibaut de Bettignies @@oth@@ Katherine Cure @@oth@@ Martial Depczynski @@oth@@ Francois Dufois @@oth@@ Jane Fromont @@oth@@ Christopher J Fulton @@oth@@ Renae K Hovey @@oth@@ Euan S Harvey @@oth@@ Thomas H Holmes @@oth@@ Gary A Kendrick @@oth@@ Ben Radford @@oth@@ Julia Santana-Garcon @@oth@@ Benjamin J Saunders @@oth@@ Dan A Smale @@oth@@ Mads S Thomsen @@oth@@ Chenae A Tuckett @@oth@@ Fernando Tuya @@oth@@ Mathew A Vanderklift @@oth@@ Shaun Wilson @@oth@@ |
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Climate-driven regime shift of a temperate marine ecosystem |
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Ecosystems over time have endured much disturbance, yet they tend to remain intact, a characteristic we call resilience. Though many systems have been lost and destroyed, for systems that remain physically intact, there is debate as to whether changing temperatures will result in shifts or collapses. Wernburg et al. show that extreme warming of a temperate kelp forest off Australia resulted not only in its collapse, but also in a shift in community composition that brought about an increase in herbivorous tropical fishes that prevent the reestablishment of kelp. Thus, many systems may not be resilient to the rapid climate change that we face. Science, this issue p. 169 Ecosystem reconfigurations arising from climate-driven changes in species distributions are expected to have profound ecological, social, and economic implications. Here we reveal a rapid climate-driven regime shift of Australian temperate reef communities, which lost their defining kelp forests and became dominated by persistent seaweed turfs. After decades of ocean warming, extreme marine heat waves forced a 100-kilometer range contraction of extensive kelp forests and saw temperate species replaced by seaweeds, invertebrates, corals, and fishes characteristic of subtropical and tropical waters. This community-wide tropicalization fundamentally altered key ecological processes, suppressing the recovery of kelp forests. |
abstractGer |
Ecosystems over time have endured much disturbance, yet they tend to remain intact, a characteristic we call resilience. Though many systems have been lost and destroyed, for systems that remain physically intact, there is debate as to whether changing temperatures will result in shifts or collapses. Wernburg et al. show that extreme warming of a temperate kelp forest off Australia resulted not only in its collapse, but also in a shift in community composition that brought about an increase in herbivorous tropical fishes that prevent the reestablishment of kelp. Thus, many systems may not be resilient to the rapid climate change that we face. Science, this issue p. 169 Ecosystem reconfigurations arising from climate-driven changes in species distributions are expected to have profound ecological, social, and economic implications. Here we reveal a rapid climate-driven regime shift of Australian temperate reef communities, which lost their defining kelp forests and became dominated by persistent seaweed turfs. After decades of ocean warming, extreme marine heat waves forced a 100-kilometer range contraction of extensive kelp forests and saw temperate species replaced by seaweeds, invertebrates, corals, and fishes characteristic of subtropical and tropical waters. This community-wide tropicalization fundamentally altered key ecological processes, suppressing the recovery of kelp forests. |
abstract_unstemmed |
Ecosystems over time have endured much disturbance, yet they tend to remain intact, a characteristic we call resilience. Though many systems have been lost and destroyed, for systems that remain physically intact, there is debate as to whether changing temperatures will result in shifts or collapses. Wernburg et al. show that extreme warming of a temperate kelp forest off Australia resulted not only in its collapse, but also in a shift in community composition that brought about an increase in herbivorous tropical fishes that prevent the reestablishment of kelp. Thus, many systems may not be resilient to the rapid climate change that we face. Science, this issue p. 169 Ecosystem reconfigurations arising from climate-driven changes in species distributions are expected to have profound ecological, social, and economic implications. Here we reveal a rapid climate-driven regime shift of Australian temperate reef communities, which lost their defining kelp forests and became dominated by persistent seaweed turfs. After decades of ocean warming, extreme marine heat waves forced a 100-kilometer range contraction of extensive kelp forests and saw temperate species replaced by seaweeds, invertebrates, corals, and fishes characteristic of subtropical and tropical waters. This community-wide tropicalization fundamentally altered key ecological processes, suppressing the recovery of kelp forests. |
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Climate-driven regime shift of a temperate marine ecosystem |
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