Ocean temperature, but not acidification, causes sea anemone bleaching under a near-future climate scenario

Abstract Climate change is causing ocean temperature and partial pressure of carbon dioxide (p$ CO_{2} $) to increase. For sea anemones that have Symbiodiniaceae, high temperatures induce bleaching, whereas rises in p$ CO_{2} $ can enhance photosynthesis and increase host growth and abundance. It is...
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Autor*in:	Pryor, Sophie H. [verfasserIn] Andrews, Luke [verfasserIn] Kelaher, Brendan P. [verfasserIn] Tagliafico, Alejandro [verfasserIn] Scott, Anna [verfasserIn]

Format:	E-Artikel
Sprache:	Englisch

Erschienen:	2021

Schlagwörter:	Anemonefish Climate change Coral reefs CO Symbiodiniaceae

Übergeordnetes Werk:	Enthalten in: Coral reefs - Berlin : Springer, 1982, 40(2021), 2 vom: 15. Feb., Seite 355-364
Übergeordnetes Werk:	volume:40 ; year:2021 ; number:2 ; day:15 ; month:02 ; pages:355-364

Links:	Volltext

DOI / URN:	10.1007/s00338-021-02050-9

Katalog-ID:	SPR043681395

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520			\|a Abstract Climate change is causing ocean temperature and partial pressure of carbon dioxide (p$ CO_{2} $) to increase. For sea anemones that have Symbiodiniaceae, high temperatures induce bleaching, whereas rises in p$ CO_{2} $ can enhance photosynthesis and increase host growth and abundance. It is, however, not clear how the interaction of these two stressors impacts sea anemones that provide habitat for anemonefishes. Here, we investigated the bleaching response of the sea anemone Entacmaea quadricolor, under four conditions: (i) current temperature and current p$ CO_{2} $ (control); (ii) future p$ CO_{2} $; (iii) future temperature; and (iv) future temperature and future p$ CO_{2} $. After 16 days of exposure, future temperature, but not p$ CO_{2} $ nor their interaction, significantly reduced the Symbiodiniaceae density and total chlorophyll Symbiodiniaceae $ cell^{−1} $. Colour score was lower in the sea anemones exposed to future temperature than current temperature from day 4 onwards. In contrast, total chlorophyll symbiont $ cell^{−1} $ increased in the future temperature treatments, and light-adapted effective quantum yield remained similar in all treatments. Although p$ CO_{2} $ had no impact within the time frame of our experiment, the predicted future temperature induced bleaching in E. quadricolor. As bleaching events increase in frequency and severity, this will likely impact the abundance of host sea anemones and their symbiotic anemonefishes.
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700	1		\|a Tagliafico, Alejandro \|e verfasserin \|4 aut
700	1		\|a Scott, Anna \|e verfasserin \|4 aut
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author_variant	s h p sh shp l a la b p k bp bpk a t at a s as
matchkey_str	article:14320975:2021----::catmeaueuntcdfctocuesanmnbecignea
hierarchy_sort_str	2021
bklnumber	38.48 42.94
publishDate	2021
allfields	10.1007/s00338-021-02050-9 doi (DE-627)SPR043681395 (DE-599)SPRs00338-021-02050-9-e (SPR)s00338-021-02050-9-e DE-627 ger DE-627 rakwb eng 550 ASE 38.48 bkl 42.94 bkl Pryor, Sophie H. verfasserin aut Ocean temperature, but not acidification, causes sea anemone bleaching under a near-future climate scenario 2021 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract Climate change is causing ocean temperature and partial pressure of carbon dioxide (p$ CO_{2} $) to increase. For sea anemones that have Symbiodiniaceae, high temperatures induce bleaching, whereas rises in p$ CO_{2} $ can enhance photosynthesis and increase host growth and abundance. It is, however, not clear how the interaction of these two stressors impacts sea anemones that provide habitat for anemonefishes. Here, we investigated the bleaching response of the sea anemone Entacmaea quadricolor, under four conditions: (i) current temperature and current p$ CO_{2} $ (control); (ii) future p$ CO_{2} $; (iii) future temperature; and (iv) future temperature and future p$ CO_{2} $. After 16 days of exposure, future temperature, but not p$ CO_{2} $ nor their interaction, significantly reduced the Symbiodiniaceae density and total chlorophyll Symbiodiniaceae $ cell^{−1} $. Colour score was lower in the sea anemones exposed to future temperature than current temperature from day 4 onwards. In contrast, total chlorophyll symbiont $ cell^{−1} $ increased in the future temperature treatments, and light-adapted effective quantum yield remained similar in all treatments. Although p$ CO_{2} $ had no impact within the time frame of our experiment, the predicted future temperature induced bleaching in E. quadricolor. As bleaching events increase in frequency and severity, this will likely impact the abundance of host sea anemones and their symbiotic anemonefishes. Anemonefish (dpeaa)DE-He213 Climate change (dpeaa)DE-He213 Coral reefs (dpeaa)DE-He213 CO (dpeaa)DE-He213 Symbiodiniaceae (dpeaa)DE-He213 Andrews, Luke verfasserin aut Kelaher, Brendan P. verfasserin aut Tagliafico, Alejandro verfasserin aut Scott, Anna verfasserin aut Enthalten in Coral reefs Berlin : Springer, 1982 40(2021), 2 vom: 15. Feb., Seite 355-364 (DE-627)268756112 (DE-600)1472576-9 1432-0975 nnns volume:40 year:2021 number:2 day:15 month:02 pages:355-364 https://dx.doi.org/10.1007/s00338-021-02050-9 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GGO SSG-OPC-ASE GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_267 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_381 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 38.48 ASE 42.94 ASE AR 40 2021 2 15 02 355-364
spelling	10.1007/s00338-021-02050-9 doi (DE-627)SPR043681395 (DE-599)SPRs00338-021-02050-9-e (SPR)s00338-021-02050-9-e DE-627 ger DE-627 rakwb eng 550 ASE 38.48 bkl 42.94 bkl Pryor, Sophie H. verfasserin aut Ocean temperature, but not acidification, causes sea anemone bleaching under a near-future climate scenario 2021 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract Climate change is causing ocean temperature and partial pressure of carbon dioxide (p$ CO_{2} $) to increase. For sea anemones that have Symbiodiniaceae, high temperatures induce bleaching, whereas rises in p$ CO_{2} $ can enhance photosynthesis and increase host growth and abundance. It is, however, not clear how the interaction of these two stressors impacts sea anemones that provide habitat for anemonefishes. Here, we investigated the bleaching response of the sea anemone Entacmaea quadricolor, under four conditions: (i) current temperature and current p$ CO_{2} $ (control); (ii) future p$ CO_{2} $; (iii) future temperature; and (iv) future temperature and future p$ CO_{2} $. After 16 days of exposure, future temperature, but not p$ CO_{2} $ nor their interaction, significantly reduced the Symbiodiniaceae density and total chlorophyll Symbiodiniaceae $ cell^{−1} $. Colour score was lower in the sea anemones exposed to future temperature than current temperature from day 4 onwards. In contrast, total chlorophyll symbiont $ cell^{−1} $ increased in the future temperature treatments, and light-adapted effective quantum yield remained similar in all treatments. Although p$ CO_{2} $ had no impact within the time frame of our experiment, the predicted future temperature induced bleaching in E. quadricolor. As bleaching events increase in frequency and severity, this will likely impact the abundance of host sea anemones and their symbiotic anemonefishes. Anemonefish (dpeaa)DE-He213 Climate change (dpeaa)DE-He213 Coral reefs (dpeaa)DE-He213 CO (dpeaa)DE-He213 Symbiodiniaceae (dpeaa)DE-He213 Andrews, Luke verfasserin aut Kelaher, Brendan P. verfasserin aut Tagliafico, Alejandro verfasserin aut Scott, Anna verfasserin aut Enthalten in Coral reefs Berlin : Springer, 1982 40(2021), 2 vom: 15. Feb., Seite 355-364 (DE-627)268756112 (DE-600)1472576-9 1432-0975 nnns volume:40 year:2021 number:2 day:15 month:02 pages:355-364 https://dx.doi.org/10.1007/s00338-021-02050-9 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GGO SSG-OPC-ASE GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_267 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_381 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 38.48 ASE 42.94 ASE AR 40 2021 2 15 02 355-364
allfields_unstemmed	10.1007/s00338-021-02050-9 doi (DE-627)SPR043681395 (DE-599)SPRs00338-021-02050-9-e (SPR)s00338-021-02050-9-e DE-627 ger DE-627 rakwb eng 550 ASE 38.48 bkl 42.94 bkl Pryor, Sophie H. verfasserin aut Ocean temperature, but not acidification, causes sea anemone bleaching under a near-future climate scenario 2021 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract Climate change is causing ocean temperature and partial pressure of carbon dioxide (p$ CO_{2} $) to increase. For sea anemones that have Symbiodiniaceae, high temperatures induce bleaching, whereas rises in p$ CO_{2} $ can enhance photosynthesis and increase host growth and abundance. It is, however, not clear how the interaction of these two stressors impacts sea anemones that provide habitat for anemonefishes. Here, we investigated the bleaching response of the sea anemone Entacmaea quadricolor, under four conditions: (i) current temperature and current p$ CO_{2} $ (control); (ii) future p$ CO_{2} $; (iii) future temperature; and (iv) future temperature and future p$ CO_{2} $. After 16 days of exposure, future temperature, but not p$ CO_{2} $ nor their interaction, significantly reduced the Symbiodiniaceae density and total chlorophyll Symbiodiniaceae $ cell^{−1} $. Colour score was lower in the sea anemones exposed to future temperature than current temperature from day 4 onwards. In contrast, total chlorophyll symbiont $ cell^{−1} $ increased in the future temperature treatments, and light-adapted effective quantum yield remained similar in all treatments. Although p$ CO_{2} $ had no impact within the time frame of our experiment, the predicted future temperature induced bleaching in E. quadricolor. As bleaching events increase in frequency and severity, this will likely impact the abundance of host sea anemones and their symbiotic anemonefishes. Anemonefish (dpeaa)DE-He213 Climate change (dpeaa)DE-He213 Coral reefs (dpeaa)DE-He213 CO (dpeaa)DE-He213 Symbiodiniaceae (dpeaa)DE-He213 Andrews, Luke verfasserin aut Kelaher, Brendan P. verfasserin aut Tagliafico, Alejandro verfasserin aut Scott, Anna verfasserin aut Enthalten in Coral reefs Berlin : Springer, 1982 40(2021), 2 vom: 15. Feb., Seite 355-364 (DE-627)268756112 (DE-600)1472576-9 1432-0975 nnns volume:40 year:2021 number:2 day:15 month:02 pages:355-364 https://dx.doi.org/10.1007/s00338-021-02050-9 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GGO SSG-OPC-ASE GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_267 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_381 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 38.48 ASE 42.94 ASE AR 40 2021 2 15 02 355-364
allfieldsGer	10.1007/s00338-021-02050-9 doi (DE-627)SPR043681395 (DE-599)SPRs00338-021-02050-9-e (SPR)s00338-021-02050-9-e DE-627 ger DE-627 rakwb eng 550 ASE 38.48 bkl 42.94 bkl Pryor, Sophie H. verfasserin aut Ocean temperature, but not acidification, causes sea anemone bleaching under a near-future climate scenario 2021 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract Climate change is causing ocean temperature and partial pressure of carbon dioxide (p$ CO_{2} $) to increase. For sea anemones that have Symbiodiniaceae, high temperatures induce bleaching, whereas rises in p$ CO_{2} $ can enhance photosynthesis and increase host growth and abundance. It is, however, not clear how the interaction of these two stressors impacts sea anemones that provide habitat for anemonefishes. Here, we investigated the bleaching response of the sea anemone Entacmaea quadricolor, under four conditions: (i) current temperature and current p$ CO_{2} $ (control); (ii) future p$ CO_{2} $; (iii) future temperature; and (iv) future temperature and future p$ CO_{2} $. After 16 days of exposure, future temperature, but not p$ CO_{2} $ nor their interaction, significantly reduced the Symbiodiniaceae density and total chlorophyll Symbiodiniaceae $ cell^{−1} $. Colour score was lower in the sea anemones exposed to future temperature than current temperature from day 4 onwards. In contrast, total chlorophyll symbiont $ cell^{−1} $ increased in the future temperature treatments, and light-adapted effective quantum yield remained similar in all treatments. Although p$ CO_{2} $ had no impact within the time frame of our experiment, the predicted future temperature induced bleaching in E. quadricolor. As bleaching events increase in frequency and severity, this will likely impact the abundance of host sea anemones and their symbiotic anemonefishes. Anemonefish (dpeaa)DE-He213 Climate change (dpeaa)DE-He213 Coral reefs (dpeaa)DE-He213 CO (dpeaa)DE-He213 Symbiodiniaceae (dpeaa)DE-He213 Andrews, Luke verfasserin aut Kelaher, Brendan P. verfasserin aut Tagliafico, Alejandro verfasserin aut Scott, Anna verfasserin aut Enthalten in Coral reefs Berlin : Springer, 1982 40(2021), 2 vom: 15. Feb., Seite 355-364 (DE-627)268756112 (DE-600)1472576-9 1432-0975 nnns volume:40 year:2021 number:2 day:15 month:02 pages:355-364 https://dx.doi.org/10.1007/s00338-021-02050-9 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GGO SSG-OPC-ASE GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_267 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_381 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 38.48 ASE 42.94 ASE AR 40 2021 2 15 02 355-364
allfieldsSound	10.1007/s00338-021-02050-9 doi (DE-627)SPR043681395 (DE-599)SPRs00338-021-02050-9-e (SPR)s00338-021-02050-9-e DE-627 ger DE-627 rakwb eng 550 ASE 38.48 bkl 42.94 bkl Pryor, Sophie H. verfasserin aut Ocean temperature, but not acidification, causes sea anemone bleaching under a near-future climate scenario 2021 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract Climate change is causing ocean temperature and partial pressure of carbon dioxide (p$ CO_{2} $) to increase. For sea anemones that have Symbiodiniaceae, high temperatures induce bleaching, whereas rises in p$ CO_{2} $ can enhance photosynthesis and increase host growth and abundance. It is, however, not clear how the interaction of these two stressors impacts sea anemones that provide habitat for anemonefishes. Here, we investigated the bleaching response of the sea anemone Entacmaea quadricolor, under four conditions: (i) current temperature and current p$ CO_{2} $ (control); (ii) future p$ CO_{2} $; (iii) future temperature; and (iv) future temperature and future p$ CO_{2} $. After 16 days of exposure, future temperature, but not p$ CO_{2} $ nor their interaction, significantly reduced the Symbiodiniaceae density and total chlorophyll Symbiodiniaceae $ cell^{−1} $. Colour score was lower in the sea anemones exposed to future temperature than current temperature from day 4 onwards. In contrast, total chlorophyll symbiont $ cell^{−1} $ increased in the future temperature treatments, and light-adapted effective quantum yield remained similar in all treatments. Although p$ CO_{2} $ had no impact within the time frame of our experiment, the predicted future temperature induced bleaching in E. quadricolor. As bleaching events increase in frequency and severity, this will likely impact the abundance of host sea anemones and their symbiotic anemonefishes. Anemonefish (dpeaa)DE-He213 Climate change (dpeaa)DE-He213 Coral reefs (dpeaa)DE-He213 CO (dpeaa)DE-He213 Symbiodiniaceae (dpeaa)DE-He213 Andrews, Luke verfasserin aut Kelaher, Brendan P. verfasserin aut Tagliafico, Alejandro verfasserin aut Scott, Anna verfasserin aut Enthalten in Coral reefs Berlin : Springer, 1982 40(2021), 2 vom: 15. Feb., Seite 355-364 (DE-627)268756112 (DE-600)1472576-9 1432-0975 nnns volume:40 year:2021 number:2 day:15 month:02 pages:355-364 https://dx.doi.org/10.1007/s00338-021-02050-9 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GGO SSG-OPC-ASE GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_267 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_381 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 38.48 ASE 42.94 ASE AR 40 2021 2 15 02 355-364
language	English
source	Enthalten in Coral reefs 40(2021), 2 vom: 15. Feb., Seite 355-364 volume:40 year:2021 number:2 day:15 month:02 pages:355-364
sourceStr	Enthalten in Coral reefs 40(2021), 2 vom: 15. Feb., Seite 355-364 volume:40 year:2021 number:2 day:15 month:02 pages:355-364
format_phy_str_mv	Article
institution	findex.gbv.de
topic_facet	Anemonefish Climate change Coral reefs CO Symbiodiniaceae
dewey-raw	550
isfreeaccess_bool	false
container_title	Coral reefs
authorswithroles_txt_mv	Pryor, Sophie H. @@aut@@ Andrews, Luke @@aut@@ Kelaher, Brendan P. @@aut@@ Tagliafico, Alejandro @@aut@@ Scott, Anna @@aut@@
publishDateDaySort_date	2021-02-15T00:00:00Z
hierarchy_top_id	268756112
dewey-sort	3550
id	SPR043681395
language_de	englisch
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author	Pryor, Sophie H.
spellingShingle	Pryor, Sophie H. ddc 550 bkl 38.48 bkl 42.94 misc Anemonefish misc Climate change misc Coral reefs misc CO misc Symbiodiniaceae Ocean temperature, but not acidification, causes sea anemone bleaching under a near-future climate scenario
authorStr	Pryor, Sophie H.
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topic_title	550 ASE 38.48 bkl 42.94 bkl Ocean temperature, but not acidification, causes sea anemone bleaching under a near-future climate scenario Anemonefish (dpeaa)DE-He213 Climate change (dpeaa)DE-He213 Coral reefs (dpeaa)DE-He213 CO (dpeaa)DE-He213 Symbiodiniaceae (dpeaa)DE-He213
topic	ddc 550 bkl 38.48 bkl 42.94 misc Anemonefish misc Climate change misc Coral reefs misc CO misc Symbiodiniaceae
topic_unstemmed	ddc 550 bkl 38.48 bkl 42.94 misc Anemonefish misc Climate change misc Coral reefs misc CO misc Symbiodiniaceae
topic_browse	ddc 550 bkl 38.48 bkl 42.94 misc Anemonefish misc Climate change misc Coral reefs misc CO misc Symbiodiniaceae
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title	Ocean temperature, but not acidification, causes sea anemone bleaching under a near-future climate scenario
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title_full	Ocean temperature, but not acidification, causes sea anemone bleaching under a near-future climate scenario
author_sort	Pryor, Sophie H.
journal	Coral reefs
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author_browse	Pryor, Sophie H. Andrews, Luke Kelaher, Brendan P. Tagliafico, Alejandro Scott, Anna
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author-letter	Pryor, Sophie H.
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title_sort	ocean temperature, but not acidification, causes sea anemone bleaching under a near-future climate scenario
title_auth	Ocean temperature, but not acidification, causes sea anemone bleaching under a near-future climate scenario
abstract	Abstract Climate change is causing ocean temperature and partial pressure of carbon dioxide (p$ CO_{2} $) to increase. For sea anemones that have Symbiodiniaceae, high temperatures induce bleaching, whereas rises in p$ CO_{2} $ can enhance photosynthesis and increase host growth and abundance. It is, however, not clear how the interaction of these two stressors impacts sea anemones that provide habitat for anemonefishes. Here, we investigated the bleaching response of the sea anemone Entacmaea quadricolor, under four conditions: (i) current temperature and current p$ CO_{2} $ (control); (ii) future p$ CO_{2} $; (iii) future temperature; and (iv) future temperature and future p$ CO_{2} $. After 16 days of exposure, future temperature, but not p$ CO_{2} $ nor their interaction, significantly reduced the Symbiodiniaceae density and total chlorophyll Symbiodiniaceae $ cell^{−1} $. Colour score was lower in the sea anemones exposed to future temperature than current temperature from day 4 onwards. In contrast, total chlorophyll symbiont $ cell^{−1} $ increased in the future temperature treatments, and light-adapted effective quantum yield remained similar in all treatments. Although p$ CO_{2} $ had no impact within the time frame of our experiment, the predicted future temperature induced bleaching in E. quadricolor. As bleaching events increase in frequency and severity, this will likely impact the abundance of host sea anemones and their symbiotic anemonefishes.
abstractGer	Abstract Climate change is causing ocean temperature and partial pressure of carbon dioxide (p$ CO_{2} $) to increase. For sea anemones that have Symbiodiniaceae, high temperatures induce bleaching, whereas rises in p$ CO_{2} $ can enhance photosynthesis and increase host growth and abundance. It is, however, not clear how the interaction of these two stressors impacts sea anemones that provide habitat for anemonefishes. Here, we investigated the bleaching response of the sea anemone Entacmaea quadricolor, under four conditions: (i) current temperature and current p$ CO_{2} $ (control); (ii) future p$ CO_{2} $; (iii) future temperature; and (iv) future temperature and future p$ CO_{2} $. After 16 days of exposure, future temperature, but not p$ CO_{2} $ nor their interaction, significantly reduced the Symbiodiniaceae density and total chlorophyll Symbiodiniaceae $ cell^{−1} $. Colour score was lower in the sea anemones exposed to future temperature than current temperature from day 4 onwards. In contrast, total chlorophyll symbiont $ cell^{−1} $ increased in the future temperature treatments, and light-adapted effective quantum yield remained similar in all treatments. Although p$ CO_{2} $ had no impact within the time frame of our experiment, the predicted future temperature induced bleaching in E. quadricolor. As bleaching events increase in frequency and severity, this will likely impact the abundance of host sea anemones and their symbiotic anemonefishes.
abstract_unstemmed	Abstract Climate change is causing ocean temperature and partial pressure of carbon dioxide (p$ CO_{2} $) to increase. For sea anemones that have Symbiodiniaceae, high temperatures induce bleaching, whereas rises in p$ CO_{2} $ can enhance photosynthesis and increase host growth and abundance. It is, however, not clear how the interaction of these two stressors impacts sea anemones that provide habitat for anemonefishes. Here, we investigated the bleaching response of the sea anemone Entacmaea quadricolor, under four conditions: (i) current temperature and current p$ CO_{2} $ (control); (ii) future p$ CO_{2} $; (iii) future temperature; and (iv) future temperature and future p$ CO_{2} $. After 16 days of exposure, future temperature, but not p$ CO_{2} $ nor their interaction, significantly reduced the Symbiodiniaceae density and total chlorophyll Symbiodiniaceae $ cell^{−1} $. Colour score was lower in the sea anemones exposed to future temperature than current temperature from day 4 onwards. In contrast, total chlorophyll symbiont $ cell^{−1} $ increased in the future temperature treatments, and light-adapted effective quantum yield remained similar in all treatments. Although p$ CO_{2} $ had no impact within the time frame of our experiment, the predicted future temperature induced bleaching in E. quadricolor. As bleaching events increase in frequency and severity, this will likely impact the abundance of host sea anemones and their symbiotic anemonefishes.
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container_issue	2
title_short	Ocean temperature, but not acidification, causes sea anemone bleaching under a near-future climate scenario
url	https://dx.doi.org/10.1007/s00338-021-02050-9
remote_bool	true
author2	Andrews, Luke Kelaher, Brendan P. Tagliafico, Alejandro Scott, Anna
author2Str	Andrews, Luke Kelaher, Brendan P. Tagliafico, Alejandro Scott, Anna
ppnlink	268756112
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doi_str	10.1007/s00338-021-02050-9
up_date	2024-07-03T20:12:25.434Z
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Ocean temperature, but not acidification, causes sea anemone bleaching under a near-future climate scenario

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