Biological responses to environmental heterogeneity under future ocean conditions

Organisms are projected to face unprecedented rates of change in future ocean conditions due to anthropogenic climate‐change. At present, marine life encounters a wide range of environmental heterogeneity from natural fluctuations to mean climate change. Manipulation studies suggest that biota from more variable marine environments have more phenotypic plasticity to tolerate environmental heterogeneity. Here, we consider current strategies employed by a range of representative organisms across various habitats – from short‐lived phytoplankton to long‐lived corals – in response to environmental heterogeneity. We then discuss how, if and when organismal responses (acclimate/migrate/adapt) may be altered by shifts in the magnitude of the mean climate‐change signal relative to that for natural fluctuations projected for coming decades. The findings from both novel climate‐change modelling simulations and prior biological manipulation studies, in which natural fluctuations are superimposed on those of mean change, provide valuable insights into organismal responses to environmental heterogeneity. Manipulations reveal that different experimental outcomes are evident between climate‐change treatments which include natural fluctuations vs. those which do not. Modelling simulations project that the magnitude of climate variability, along with mean climate change, will increase in coming decades, and hence environmental heterogeneity will increase, illustrating the need for more realistic biological manipulation experiments that include natural fluctuations. However, simulations also strongly suggest that the timescales over which the mean climate‐change signature will become dominant, relative to natural fluctuations, will vary for individual properties, being most rapid for CO 2 (~10 years from present day) to 4 decades for nutrients. We conclude that the strategies used by biota to respond to shifts in environmental heterogeneity may be complex, as they will have to physiologically straddle wide‐ranging timescales in the alteration of ocean conditions, including the need to adapt to rapidly rising CO 2 and also acclimate to environmental heterogeneity in more slowly changing properties such as warming. Ausführliche Beschreibung

Gespeichert in:

Autor*in:	Boyd, Philip W [verfasserIn] Cornwall, Christopher E Davison, Andrew Doney, Scott C Fourquez, Marion Hurd, Catriona L Lima, Ivan D McMinn, Andrew

Format:	Artikel
Sprache:	Englisch

Erschienen:	2016

Rechteinformationen:	Nutzungsrecht: © 2016 John Wiley & Sons Ltd © 2016 John Wiley & Sons Ltd.

Schlagwörter:	climate variability ocean climate change marine life emergence phenotypic plasticity Global warming Marine biology Oceans Climate change

Übergeordnetes Werk:	Enthalten in: Global change biology - Oxford [u.a.] : Blackwell Science, 1995, 22(2016), 8, Seite 2633-2650
Übergeordnetes Werk:	volume:22 ; year:2016 ; number:8 ; pages:2633-2650

Links:	Volltext Link aufrufen Link aufrufen Link aufrufen

DOI / URN:	10.1111/gcb.13287

Katalog-ID:	OLC1980654913

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540			\|a Nutzungsrecht: © 2016 John Wiley & Sons Ltd
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650		4	\|a climate variability
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650		4	\|a Global warming
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700	1		\|a Cornwall, Christopher E \|4 oth
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700	1		\|a Fourquez, Marion \|4 oth
700	1		\|a Hurd, Catriona L \|4 oth
700	1		\|a Lima, Ivan D \|4 oth
700	1		\|a McMinn, Andrew \|4 oth
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allfields	10.1111/gcb.13287 doi PQ20160815 (DE-627)OLC1980654913 (DE-599)GBVOLC1980654913 (PRQ)c2027-f965dd23af2f17f1874d3f41ea8ec2936849f0d83bfb3f1eebdf2fa48deb38770 (KEY)0265675220160000022000802633biologicalresponsestoenvironmentalheterogeneityund DE-627 ger DE-627 rakwb eng 570 DNB BIODIV fid Boyd, Philip W verfasserin aut Biological responses to environmental heterogeneity under future ocean conditions 2016 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier Organisms are projected to face unprecedented rates of change in future ocean conditions due to anthropogenic climate‐change. At present, marine life encounters a wide range of environmental heterogeneity from natural fluctuations to mean climate change. Manipulation studies suggest that biota from more variable marine environments have more phenotypic plasticity to tolerate environmental heterogeneity. Here, we consider current strategies employed by a range of representative organisms across various habitats – from short‐lived phytoplankton to long‐lived corals – in response to environmental heterogeneity. We then discuss how, if and when organismal responses (acclimate/migrate/adapt) may be altered by shifts in the magnitude of the mean climate‐change signal relative to that for natural fluctuations projected for coming decades. The findings from both novel climate‐change modelling simulations and prior biological manipulation studies, in which natural fluctuations are superimposed on those of mean change, provide valuable insights into organismal responses to environmental heterogeneity. Manipulations reveal that different experimental outcomes are evident between climate‐change treatments which include natural fluctuations vs. those which do not. Modelling simulations project that the magnitude of climate variability, along with mean climate change, will increase in coming decades, and hence environmental heterogeneity will increase, illustrating the need for more realistic biological manipulation experiments that include natural fluctuations. However, simulations also strongly suggest that the timescales over which the mean climate‐change signature will become dominant, relative to natural fluctuations, will vary for individual properties, being most rapid for CO 2 (~10 years from present day) to 4 decades for nutrients. We conclude that the strategies used by biota to respond to shifts in environmental heterogeneity may be complex, as they will have to physiologically straddle wide‐ranging timescales in the alteration of ocean conditions, including the need to adapt to rapidly rising CO 2 and also acclimate to environmental heterogeneity in more slowly changing properties such as warming. Nutzungsrecht: © 2016 John Wiley & Sons Ltd © 2016 John Wiley & Sons Ltd. climate variability ocean climate change marine life emergence phenotypic plasticity Global warming Marine biology Oceans Climate change Cornwall, Christopher E oth Davison, Andrew oth Doney, Scott C oth Fourquez, Marion oth Hurd, Catriona L oth Lima, Ivan D oth McMinn, Andrew oth Enthalten in Global change biology Oxford [u.a.] : Blackwell Science, 1995 22(2016), 8, Seite 2633-2650 (DE-627)18815499X (DE-600)1281439-8 (DE-576)048525634 1354-1013 nnns volume:22 year:2016 number:8 pages:2633-2650 http://dx.doi.org/10.1111/gcb.13287 Volltext http://onlinelibrary.wiley.com/doi/10.1111/gcb.13287/abstract http://www.ncbi.nlm.nih.gov/pubmed/27111095 http://search.proquest.com/docview/1801397224 GBV_USEFLAG_A SYSFLAG_A GBV_OLC FID-BIODIV SSG-OLC-GEO SSG-OLC-FOR SSG-OLC-PHA SSG-OLC-DE-84 SSG-OPC-GGO GBV_ILN_601 GBV_ILN_4219 AR 22 2016 8 2633-2650
spelling	10.1111/gcb.13287 doi PQ20160815 (DE-627)OLC1980654913 (DE-599)GBVOLC1980654913 (PRQ)c2027-f965dd23af2f17f1874d3f41ea8ec2936849f0d83bfb3f1eebdf2fa48deb38770 (KEY)0265675220160000022000802633biologicalresponsestoenvironmentalheterogeneityund DE-627 ger DE-627 rakwb eng 570 DNB BIODIV fid Boyd, Philip W verfasserin aut Biological responses to environmental heterogeneity under future ocean conditions 2016 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier Organisms are projected to face unprecedented rates of change in future ocean conditions due to anthropogenic climate‐change. At present, marine life encounters a wide range of environmental heterogeneity from natural fluctuations to mean climate change. Manipulation studies suggest that biota from more variable marine environments have more phenotypic plasticity to tolerate environmental heterogeneity. Here, we consider current strategies employed by a range of representative organisms across various habitats – from short‐lived phytoplankton to long‐lived corals – in response to environmental heterogeneity. We then discuss how, if and when organismal responses (acclimate/migrate/adapt) may be altered by shifts in the magnitude of the mean climate‐change signal relative to that for natural fluctuations projected for coming decades. The findings from both novel climate‐change modelling simulations and prior biological manipulation studies, in which natural fluctuations are superimposed on those of mean change, provide valuable insights into organismal responses to environmental heterogeneity. Manipulations reveal that different experimental outcomes are evident between climate‐change treatments which include natural fluctuations vs. those which do not. Modelling simulations project that the magnitude of climate variability, along with mean climate change, will increase in coming decades, and hence environmental heterogeneity will increase, illustrating the need for more realistic biological manipulation experiments that include natural fluctuations. However, simulations also strongly suggest that the timescales over which the mean climate‐change signature will become dominant, relative to natural fluctuations, will vary for individual properties, being most rapid for CO 2 (~10 years from present day) to 4 decades for nutrients. We conclude that the strategies used by biota to respond to shifts in environmental heterogeneity may be complex, as they will have to physiologically straddle wide‐ranging timescales in the alteration of ocean conditions, including the need to adapt to rapidly rising CO 2 and also acclimate to environmental heterogeneity in more slowly changing properties such as warming. Nutzungsrecht: © 2016 John Wiley & Sons Ltd © 2016 John Wiley & Sons Ltd. climate variability ocean climate change marine life emergence phenotypic plasticity Global warming Marine biology Oceans Climate change Cornwall, Christopher E oth Davison, Andrew oth Doney, Scott C oth Fourquez, Marion oth Hurd, Catriona L oth Lima, Ivan D oth McMinn, Andrew oth Enthalten in Global change biology Oxford [u.a.] : Blackwell Science, 1995 22(2016), 8, Seite 2633-2650 (DE-627)18815499X (DE-600)1281439-8 (DE-576)048525634 1354-1013 nnns volume:22 year:2016 number:8 pages:2633-2650 http://dx.doi.org/10.1111/gcb.13287 Volltext http://onlinelibrary.wiley.com/doi/10.1111/gcb.13287/abstract http://www.ncbi.nlm.nih.gov/pubmed/27111095 http://search.proquest.com/docview/1801397224 GBV_USEFLAG_A SYSFLAG_A GBV_OLC FID-BIODIV SSG-OLC-GEO SSG-OLC-FOR SSG-OLC-PHA SSG-OLC-DE-84 SSG-OPC-GGO GBV_ILN_601 GBV_ILN_4219 AR 22 2016 8 2633-2650
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allfieldsGer	10.1111/gcb.13287 doi PQ20160815 (DE-627)OLC1980654913 (DE-599)GBVOLC1980654913 (PRQ)c2027-f965dd23af2f17f1874d3f41ea8ec2936849f0d83bfb3f1eebdf2fa48deb38770 (KEY)0265675220160000022000802633biologicalresponsestoenvironmentalheterogeneityund DE-627 ger DE-627 rakwb eng 570 DNB BIODIV fid Boyd, Philip W verfasserin aut Biological responses to environmental heterogeneity under future ocean conditions 2016 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier Organisms are projected to face unprecedented rates of change in future ocean conditions due to anthropogenic climate‐change. At present, marine life encounters a wide range of environmental heterogeneity from natural fluctuations to mean climate change. Manipulation studies suggest that biota from more variable marine environments have more phenotypic plasticity to tolerate environmental heterogeneity. Here, we consider current strategies employed by a range of representative organisms across various habitats – from short‐lived phytoplankton to long‐lived corals – in response to environmental heterogeneity. We then discuss how, if and when organismal responses (acclimate/migrate/adapt) may be altered by shifts in the magnitude of the mean climate‐change signal relative to that for natural fluctuations projected for coming decades. The findings from both novel climate‐change modelling simulations and prior biological manipulation studies, in which natural fluctuations are superimposed on those of mean change, provide valuable insights into organismal responses to environmental heterogeneity. Manipulations reveal that different experimental outcomes are evident between climate‐change treatments which include natural fluctuations vs. those which do not. Modelling simulations project that the magnitude of climate variability, along with mean climate change, will increase in coming decades, and hence environmental heterogeneity will increase, illustrating the need for more realistic biological manipulation experiments that include natural fluctuations. However, simulations also strongly suggest that the timescales over which the mean climate‐change signature will become dominant, relative to natural fluctuations, will vary for individual properties, being most rapid for CO 2 (~10 years from present day) to 4 decades for nutrients. We conclude that the strategies used by biota to respond to shifts in environmental heterogeneity may be complex, as they will have to physiologically straddle wide‐ranging timescales in the alteration of ocean conditions, including the need to adapt to rapidly rising CO 2 and also acclimate to environmental heterogeneity in more slowly changing properties such as warming. Nutzungsrecht: © 2016 John Wiley & Sons Ltd © 2016 John Wiley & Sons Ltd. climate variability ocean climate change marine life emergence phenotypic plasticity Global warming Marine biology Oceans Climate change Cornwall, Christopher E oth Davison, Andrew oth Doney, Scott C oth Fourquez, Marion oth Hurd, Catriona L oth Lima, Ivan D oth McMinn, Andrew oth Enthalten in Global change biology Oxford [u.a.] : Blackwell Science, 1995 22(2016), 8, Seite 2633-2650 (DE-627)18815499X (DE-600)1281439-8 (DE-576)048525634 1354-1013 nnns volume:22 year:2016 number:8 pages:2633-2650 http://dx.doi.org/10.1111/gcb.13287 Volltext http://onlinelibrary.wiley.com/doi/10.1111/gcb.13287/abstract http://www.ncbi.nlm.nih.gov/pubmed/27111095 http://search.proquest.com/docview/1801397224 GBV_USEFLAG_A SYSFLAG_A GBV_OLC FID-BIODIV SSG-OLC-GEO SSG-OLC-FOR SSG-OLC-PHA SSG-OLC-DE-84 SSG-OPC-GGO GBV_ILN_601 GBV_ILN_4219 AR 22 2016 8 2633-2650
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source	Enthalten in Global change biology 22(2016), 8, Seite 2633-2650 volume:22 year:2016 number:8 pages:2633-2650
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topic_facet	climate variability ocean climate change marine life emergence phenotypic plasticity Global warming Marine biology Oceans Climate change
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authorswithroles_txt_mv	Boyd, Philip W @@aut@@ Cornwall, Christopher E @@oth@@ Davison, Andrew @@oth@@ Doney, Scott C @@oth@@ Fourquez, Marion @@oth@@ Hurd, Catriona L @@oth@@ Lima, Ivan D @@oth@@ McMinn, Andrew @@oth@@
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author	Boyd, Philip W
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title	Biological responses to environmental heterogeneity under future ocean conditions
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title_sort	biological responses to environmental heterogeneity under future ocean conditions
title_auth	Biological responses to environmental heterogeneity under future ocean conditions
abstract	Organisms are projected to face unprecedented rates of change in future ocean conditions due to anthropogenic climate‐change. At present, marine life encounters a wide range of environmental heterogeneity from natural fluctuations to mean climate change. Manipulation studies suggest that biota from more variable marine environments have more phenotypic plasticity to tolerate environmental heterogeneity. Here, we consider current strategies employed by a range of representative organisms across various habitats – from short‐lived phytoplankton to long‐lived corals – in response to environmental heterogeneity. We then discuss how, if and when organismal responses (acclimate/migrate/adapt) may be altered by shifts in the magnitude of the mean climate‐change signal relative to that for natural fluctuations projected for coming decades. The findings from both novel climate‐change modelling simulations and prior biological manipulation studies, in which natural fluctuations are superimposed on those of mean change, provide valuable insights into organismal responses to environmental heterogeneity. Manipulations reveal that different experimental outcomes are evident between climate‐change treatments which include natural fluctuations vs. those which do not. Modelling simulations project that the magnitude of climate variability, along with mean climate change, will increase in coming decades, and hence environmental heterogeneity will increase, illustrating the need for more realistic biological manipulation experiments that include natural fluctuations. However, simulations also strongly suggest that the timescales over which the mean climate‐change signature will become dominant, relative to natural fluctuations, will vary for individual properties, being most rapid for CO 2 (~10 years from present day) to 4 decades for nutrients. We conclude that the strategies used by biota to respond to shifts in environmental heterogeneity may be complex, as they will have to physiologically straddle wide‐ranging timescales in the alteration of ocean conditions, including the need to adapt to rapidly rising CO 2 and also acclimate to environmental heterogeneity in more slowly changing properties such as warming.
abstractGer	Organisms are projected to face unprecedented rates of change in future ocean conditions due to anthropogenic climate‐change. At present, marine life encounters a wide range of environmental heterogeneity from natural fluctuations to mean climate change. Manipulation studies suggest that biota from more variable marine environments have more phenotypic plasticity to tolerate environmental heterogeneity. Here, we consider current strategies employed by a range of representative organisms across various habitats – from short‐lived phytoplankton to long‐lived corals – in response to environmental heterogeneity. We then discuss how, if and when organismal responses (acclimate/migrate/adapt) may be altered by shifts in the magnitude of the mean climate‐change signal relative to that for natural fluctuations projected for coming decades. The findings from both novel climate‐change modelling simulations and prior biological manipulation studies, in which natural fluctuations are superimposed on those of mean change, provide valuable insights into organismal responses to environmental heterogeneity. Manipulations reveal that different experimental outcomes are evident between climate‐change treatments which include natural fluctuations vs. those which do not. Modelling simulations project that the magnitude of climate variability, along with mean climate change, will increase in coming decades, and hence environmental heterogeneity will increase, illustrating the need for more realistic biological manipulation experiments that include natural fluctuations. However, simulations also strongly suggest that the timescales over which the mean climate‐change signature will become dominant, relative to natural fluctuations, will vary for individual properties, being most rapid for CO 2 (~10 years from present day) to 4 decades for nutrients. We conclude that the strategies used by biota to respond to shifts in environmental heterogeneity may be complex, as they will have to physiologically straddle wide‐ranging timescales in the alteration of ocean conditions, including the need to adapt to rapidly rising CO 2 and also acclimate to environmental heterogeneity in more slowly changing properties such as warming.
abstract_unstemmed	Organisms are projected to face unprecedented rates of change in future ocean conditions due to anthropogenic climate‐change. At present, marine life encounters a wide range of environmental heterogeneity from natural fluctuations to mean climate change. Manipulation studies suggest that biota from more variable marine environments have more phenotypic plasticity to tolerate environmental heterogeneity. Here, we consider current strategies employed by a range of representative organisms across various habitats – from short‐lived phytoplankton to long‐lived corals – in response to environmental heterogeneity. We then discuss how, if and when organismal responses (acclimate/migrate/adapt) may be altered by shifts in the magnitude of the mean climate‐change signal relative to that for natural fluctuations projected for coming decades. The findings from both novel climate‐change modelling simulations and prior biological manipulation studies, in which natural fluctuations are superimposed on those of mean change, provide valuable insights into organismal responses to environmental heterogeneity. Manipulations reveal that different experimental outcomes are evident between climate‐change treatments which include natural fluctuations vs. those which do not. Modelling simulations project that the magnitude of climate variability, along with mean climate change, will increase in coming decades, and hence environmental heterogeneity will increase, illustrating the need for more realistic biological manipulation experiments that include natural fluctuations. However, simulations also strongly suggest that the timescales over which the mean climate‐change signature will become dominant, relative to natural fluctuations, will vary for individual properties, being most rapid for CO 2 (~10 years from present day) to 4 decades for nutrients. We conclude that the strategies used by biota to respond to shifts in environmental heterogeneity may be complex, as they will have to physiologically straddle wide‐ranging timescales in the alteration of ocean conditions, including the need to adapt to rapidly rising CO 2 and also acclimate to environmental heterogeneity in more slowly changing properties such as warming.
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title_short	Biological responses to environmental heterogeneity under future ocean conditions
url	http://dx.doi.org/10.1111/gcb.13287 http://onlinelibrary.wiley.com/doi/10.1111/gcb.13287/abstract http://www.ncbi.nlm.nih.gov/pubmed/27111095 http://search.proquest.com/docview/1801397224
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author2	Cornwall, Christopher E Davison, Andrew Doney, Scott C Fourquez, Marion Hurd, Catriona L Lima, Ivan D McMinn, Andrew
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At present, marine life encounters a wide range of environmental heterogeneity from natural fluctuations to mean climate change. Manipulation studies suggest that biota from more variable marine environments have more phenotypic plasticity to tolerate environmental heterogeneity. Here, we consider current strategies employed by a range of representative organisms across various habitats – from short‐lived phytoplankton to long‐lived corals – in response to environmental heterogeneity. We then discuss how, if and when organismal responses (acclimate/migrate/adapt) may be altered by shifts in the magnitude of the mean climate‐change signal relative to that for natural fluctuations projected for coming decades. The findings from both novel climate‐change modelling simulations and prior biological manipulation studies, in which natural fluctuations are superimposed on those of mean change, provide valuable insights into organismal responses to environmental heterogeneity. Manipulations reveal that different experimental outcomes are evident between climate‐change treatments which include natural fluctuations vs. those which do not. Modelling simulations project that the magnitude of climate variability, along with mean climate change, will increase in coming decades, and hence environmental heterogeneity will increase, illustrating the need for more realistic biological manipulation experiments that include natural fluctuations. However, simulations also strongly suggest that the timescales over which the mean climate‐change signature will become dominant, relative to natural fluctuations, will vary for individual properties, being most rapid for CO 2 (~10 years from present day) to 4 decades for nutrients. We conclude that the strategies used by biota to respond to shifts in environmental heterogeneity may be complex, as they will have to physiologically straddle wide‐ranging timescales in the alteration of ocean conditions, including the need to adapt to rapidly rising CO 2 and also acclimate to environmental heterogeneity in more slowly changing properties such as warming.</subfield></datafield><datafield tag="540" ind1=" " ind2=" "><subfield code="a">Nutzungsrecht: © 2016 John Wiley & Sons Ltd</subfield></datafield><datafield tag="540" ind1=" " ind2=" "><subfield code="a">© 2016 John Wiley & Sons Ltd.</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">climate variability</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">ocean climate change</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">marine life</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">emergence</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">phenotypic plasticity</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Global warming</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Marine biology</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Oceans</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Climate change</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Cornwall, Christopher E</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Davison, Andrew</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Doney, Scott C</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Fourquez, Marion</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Hurd, Catriona L</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Lima, Ivan D</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">McMinn, Andrew</subfield><subfield code="4">oth</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">Enthalten in</subfield><subfield code="t">Global change biology</subfield><subfield code="d">Oxford [u.a.] : Blackwell Science, 1995</subfield><subfield code="g">22(2016), 8, Seite 2633-2650</subfield><subfield code="w">(DE-627)18815499X</subfield><subfield code="w">(DE-600)1281439-8</subfield><subfield code="w">(DE-576)048525634</subfield><subfield code="x">1354-1013</subfield><subfield code="7">nnns</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:22</subfield><subfield code="g">year:2016</subfield><subfield code="g">number:8</subfield><subfield code="g">pages:2633-2650</subfield></datafield><datafield tag="856" ind1="4" ind2="1"><subfield code="u">http://dx.doi.org/10.1111/gcb.13287</subfield><subfield code="3">Volltext</subfield></datafield><datafield tag="856" ind1="4" ind2="2"><subfield code="u">http://onlinelibrary.wiley.com/doi/10.1111/gcb.13287/abstract</subfield></datafield><datafield tag="856" ind1="4" ind2="2"><subfield code="u">http://www.ncbi.nlm.nih.gov/pubmed/27111095</subfield></datafield><datafield tag="856" ind1="4" ind2="2"><subfield code="u">http://search.proquest.com/docview/1801397224</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_USEFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SYSFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_OLC</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">FID-BIODIV</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OLC-GEO</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OLC-FOR</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OLC-PHA</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OLC-DE-84</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OPC-GGO</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_601</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4219</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">22</subfield><subfield code="j">2016</subfield><subfield code="e">8</subfield><subfield code="h">2633-2650</subfield></datafield></record></collection>
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Biological responses to environmental heterogeneity under future ocean conditions

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