In search of the dead zone: Use of otoliths for tracking fish exposure to hypoxia
Otolith chemistry is often useful for tracking provenance of fishes, as well as examining migration histories. Whereas elements such as strontium and barium correlate well with salinity and temperature, experiments that examine manganese uptake as a function of these parameters have found no such co...
Ausführliche Beschreibung
Autor*in: |
Limburg, Karin E. [verfasserIn] |
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Format: |
E-Artikel |
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Sprache: |
Englisch |
Erschienen: |
2015transfer abstract |
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Umfang: |
12 |
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Übergeordnetes Werk: |
Enthalten in: Investigating the urban heat island effect of transit oriented development in Brisbane - Kamruzzaman, Md. ELSEVIER, 2017, New York, NY [u.a.] |
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Übergeordnetes Werk: |
volume:141 ; year:2015 ; pages:167-178 ; extent:12 |
Links: |
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DOI / URN: |
10.1016/j.jmarsys.2014.02.014 |
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ELV034628967 |
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245 | 1 | 0 | |a In search of the dead zone: Use of otoliths for tracking fish exposure to hypoxia |
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520 | |a Otolith chemistry is often useful for tracking provenance of fishes, as well as examining migration histories. Whereas elements such as strontium and barium correlate well with salinity and temperature, experiments that examine manganese uptake as a function of these parameters have found no such correlation. Instead, dissolved manganese is available as a redox product, and as such, is indicative of low-oxygen conditions. Here we present evidence for that mechanism in a range of habitats from marine to freshwater, across species, and also present ancillary proxies that support the mechanism as well. For example, iodine is redox-sensitive and varies inversely with Mn; and sulfur stable isotope ratios provide evidence of anoxic sulfate reduction in some circumstances. Further, S may be incorporated trophically whereas other elements appear to be taken up directly from water. This research suggests a potential means to identify individual fish exposure to hypoxia, over entire lifetimes. With further testing and understanding, in the future fish may be able to be used as “mobile monitors” of hypoxic conditions. | ||
520 | |a Otolith chemistry is often useful for tracking provenance of fishes, as well as examining migration histories. Whereas elements such as strontium and barium correlate well with salinity and temperature, experiments that examine manganese uptake as a function of these parameters have found no such correlation. Instead, dissolved manganese is available as a redox product, and as such, is indicative of low-oxygen conditions. Here we present evidence for that mechanism in a range of habitats from marine to freshwater, across species, and also present ancillary proxies that support the mechanism as well. For example, iodine is redox-sensitive and varies inversely with Mn; and sulfur stable isotope ratios provide evidence of anoxic sulfate reduction in some circumstances. Further, S may be incorporated trophically whereas other elements appear to be taken up directly from water. This research suggests a potential means to identify individual fish exposure to hypoxia, over entire lifetimes. With further testing and understanding, in the future fish may be able to be used as “mobile monitors” of hypoxic conditions. | ||
700 | 1 | |a Walther, Benjamin D. |4 oth | |
700 | 1 | |a Lu, Zunli |4 oth | |
700 | 1 | |a Jackman, George |4 oth | |
700 | 1 | |a Mohan, John |4 oth | |
700 | 1 | |a Walther, Yvonne |4 oth | |
700 | 1 | |a Nissling, Anders |4 oth | |
700 | 1 | |a Weber, Peter K. |4 oth | |
700 | 1 | |a Schmitt, Axel K. |4 oth | |
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10.1016/j.jmarsys.2014.02.014 doi GBVA2015014000021.pica (DE-627)ELV034628967 (ELSEVIER)S0924-7963(14)00043-8 DE-627 ger DE-627 rakwb eng 380 380 DE-600 380 910 VZ 55.80 bkl 74.08 bkl 74.75 bkl Limburg, Karin E. verfasserin aut In search of the dead zone: Use of otoliths for tracking fish exposure to hypoxia 2015transfer abstract 12 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Otolith chemistry is often useful for tracking provenance of fishes, as well as examining migration histories. Whereas elements such as strontium and barium correlate well with salinity and temperature, experiments that examine manganese uptake as a function of these parameters have found no such correlation. Instead, dissolved manganese is available as a redox product, and as such, is indicative of low-oxygen conditions. Here we present evidence for that mechanism in a range of habitats from marine to freshwater, across species, and also present ancillary proxies that support the mechanism as well. For example, iodine is redox-sensitive and varies inversely with Mn; and sulfur stable isotope ratios provide evidence of anoxic sulfate reduction in some circumstances. Further, S may be incorporated trophically whereas other elements appear to be taken up directly from water. This research suggests a potential means to identify individual fish exposure to hypoxia, over entire lifetimes. With further testing and understanding, in the future fish may be able to be used as “mobile monitors” of hypoxic conditions. Otolith chemistry is often useful for tracking provenance of fishes, as well as examining migration histories. Whereas elements such as strontium and barium correlate well with salinity and temperature, experiments that examine manganese uptake as a function of these parameters have found no such correlation. Instead, dissolved manganese is available as a redox product, and as such, is indicative of low-oxygen conditions. Here we present evidence for that mechanism in a range of habitats from marine to freshwater, across species, and also present ancillary proxies that support the mechanism as well. For example, iodine is redox-sensitive and varies inversely with Mn; and sulfur stable isotope ratios provide evidence of anoxic sulfate reduction in some circumstances. Further, S may be incorporated trophically whereas other elements appear to be taken up directly from water. This research suggests a potential means to identify individual fish exposure to hypoxia, over entire lifetimes. With further testing and understanding, in the future fish may be able to be used as “mobile monitors” of hypoxic conditions. Walther, Benjamin D. oth Lu, Zunli oth Jackman, George oth Mohan, John oth Walther, Yvonne oth Nissling, Anders oth Weber, Peter K. oth Schmitt, Axel K. oth Enthalten in Elsevier Kamruzzaman, Md. ELSEVIER Investigating the urban heat island effect of transit oriented development in Brisbane 2017 New York, NY [u.a.] (DE-627)ELV000581879 volume:141 year:2015 pages:167-178 extent:12 https://doi.org/10.1016/j.jmarsys.2014.02.014 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U SSG-OPC-GGO 55.80 Verkehrswesen Transportwesen: Allgemeines VZ 74.08 Wirtschaftsgeographie VZ 74.75 Verkehrsplanung Verkehrspolitik VZ AR 141 2015 167-178 12 045F 380 |
spelling |
10.1016/j.jmarsys.2014.02.014 doi GBVA2015014000021.pica (DE-627)ELV034628967 (ELSEVIER)S0924-7963(14)00043-8 DE-627 ger DE-627 rakwb eng 380 380 DE-600 380 910 VZ 55.80 bkl 74.08 bkl 74.75 bkl Limburg, Karin E. verfasserin aut In search of the dead zone: Use of otoliths for tracking fish exposure to hypoxia 2015transfer abstract 12 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Otolith chemistry is often useful for tracking provenance of fishes, as well as examining migration histories. Whereas elements such as strontium and barium correlate well with salinity and temperature, experiments that examine manganese uptake as a function of these parameters have found no such correlation. Instead, dissolved manganese is available as a redox product, and as such, is indicative of low-oxygen conditions. Here we present evidence for that mechanism in a range of habitats from marine to freshwater, across species, and also present ancillary proxies that support the mechanism as well. For example, iodine is redox-sensitive and varies inversely with Mn; and sulfur stable isotope ratios provide evidence of anoxic sulfate reduction in some circumstances. Further, S may be incorporated trophically whereas other elements appear to be taken up directly from water. This research suggests a potential means to identify individual fish exposure to hypoxia, over entire lifetimes. With further testing and understanding, in the future fish may be able to be used as “mobile monitors” of hypoxic conditions. Otolith chemistry is often useful for tracking provenance of fishes, as well as examining migration histories. Whereas elements such as strontium and barium correlate well with salinity and temperature, experiments that examine manganese uptake as a function of these parameters have found no such correlation. Instead, dissolved manganese is available as a redox product, and as such, is indicative of low-oxygen conditions. Here we present evidence for that mechanism in a range of habitats from marine to freshwater, across species, and also present ancillary proxies that support the mechanism as well. For example, iodine is redox-sensitive and varies inversely with Mn; and sulfur stable isotope ratios provide evidence of anoxic sulfate reduction in some circumstances. Further, S may be incorporated trophically whereas other elements appear to be taken up directly from water. This research suggests a potential means to identify individual fish exposure to hypoxia, over entire lifetimes. With further testing and understanding, in the future fish may be able to be used as “mobile monitors” of hypoxic conditions. Walther, Benjamin D. oth Lu, Zunli oth Jackman, George oth Mohan, John oth Walther, Yvonne oth Nissling, Anders oth Weber, Peter K. oth Schmitt, Axel K. oth Enthalten in Elsevier Kamruzzaman, Md. ELSEVIER Investigating the urban heat island effect of transit oriented development in Brisbane 2017 New York, NY [u.a.] (DE-627)ELV000581879 volume:141 year:2015 pages:167-178 extent:12 https://doi.org/10.1016/j.jmarsys.2014.02.014 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U SSG-OPC-GGO 55.80 Verkehrswesen Transportwesen: Allgemeines VZ 74.08 Wirtschaftsgeographie VZ 74.75 Verkehrsplanung Verkehrspolitik VZ AR 141 2015 167-178 12 045F 380 |
allfields_unstemmed |
10.1016/j.jmarsys.2014.02.014 doi GBVA2015014000021.pica (DE-627)ELV034628967 (ELSEVIER)S0924-7963(14)00043-8 DE-627 ger DE-627 rakwb eng 380 380 DE-600 380 910 VZ 55.80 bkl 74.08 bkl 74.75 bkl Limburg, Karin E. verfasserin aut In search of the dead zone: Use of otoliths for tracking fish exposure to hypoxia 2015transfer abstract 12 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Otolith chemistry is often useful for tracking provenance of fishes, as well as examining migration histories. Whereas elements such as strontium and barium correlate well with salinity and temperature, experiments that examine manganese uptake as a function of these parameters have found no such correlation. Instead, dissolved manganese is available as a redox product, and as such, is indicative of low-oxygen conditions. Here we present evidence for that mechanism in a range of habitats from marine to freshwater, across species, and also present ancillary proxies that support the mechanism as well. For example, iodine is redox-sensitive and varies inversely with Mn; and sulfur stable isotope ratios provide evidence of anoxic sulfate reduction in some circumstances. Further, S may be incorporated trophically whereas other elements appear to be taken up directly from water. This research suggests a potential means to identify individual fish exposure to hypoxia, over entire lifetimes. With further testing and understanding, in the future fish may be able to be used as “mobile monitors” of hypoxic conditions. Otolith chemistry is often useful for tracking provenance of fishes, as well as examining migration histories. Whereas elements such as strontium and barium correlate well with salinity and temperature, experiments that examine manganese uptake as a function of these parameters have found no such correlation. Instead, dissolved manganese is available as a redox product, and as such, is indicative of low-oxygen conditions. Here we present evidence for that mechanism in a range of habitats from marine to freshwater, across species, and also present ancillary proxies that support the mechanism as well. For example, iodine is redox-sensitive and varies inversely with Mn; and sulfur stable isotope ratios provide evidence of anoxic sulfate reduction in some circumstances. Further, S may be incorporated trophically whereas other elements appear to be taken up directly from water. This research suggests a potential means to identify individual fish exposure to hypoxia, over entire lifetimes. With further testing and understanding, in the future fish may be able to be used as “mobile monitors” of hypoxic conditions. Walther, Benjamin D. oth Lu, Zunli oth Jackman, George oth Mohan, John oth Walther, Yvonne oth Nissling, Anders oth Weber, Peter K. oth Schmitt, Axel K. oth Enthalten in Elsevier Kamruzzaman, Md. ELSEVIER Investigating the urban heat island effect of transit oriented development in Brisbane 2017 New York, NY [u.a.] (DE-627)ELV000581879 volume:141 year:2015 pages:167-178 extent:12 https://doi.org/10.1016/j.jmarsys.2014.02.014 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U SSG-OPC-GGO 55.80 Verkehrswesen Transportwesen: Allgemeines VZ 74.08 Wirtschaftsgeographie VZ 74.75 Verkehrsplanung Verkehrspolitik VZ AR 141 2015 167-178 12 045F 380 |
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10.1016/j.jmarsys.2014.02.014 doi GBVA2015014000021.pica (DE-627)ELV034628967 (ELSEVIER)S0924-7963(14)00043-8 DE-627 ger DE-627 rakwb eng 380 380 DE-600 380 910 VZ 55.80 bkl 74.08 bkl 74.75 bkl Limburg, Karin E. verfasserin aut In search of the dead zone: Use of otoliths for tracking fish exposure to hypoxia 2015transfer abstract 12 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Otolith chemistry is often useful for tracking provenance of fishes, as well as examining migration histories. Whereas elements such as strontium and barium correlate well with salinity and temperature, experiments that examine manganese uptake as a function of these parameters have found no such correlation. Instead, dissolved manganese is available as a redox product, and as such, is indicative of low-oxygen conditions. Here we present evidence for that mechanism in a range of habitats from marine to freshwater, across species, and also present ancillary proxies that support the mechanism as well. For example, iodine is redox-sensitive and varies inversely with Mn; and sulfur stable isotope ratios provide evidence of anoxic sulfate reduction in some circumstances. Further, S may be incorporated trophically whereas other elements appear to be taken up directly from water. This research suggests a potential means to identify individual fish exposure to hypoxia, over entire lifetimes. With further testing and understanding, in the future fish may be able to be used as “mobile monitors” of hypoxic conditions. Otolith chemistry is often useful for tracking provenance of fishes, as well as examining migration histories. Whereas elements such as strontium and barium correlate well with salinity and temperature, experiments that examine manganese uptake as a function of these parameters have found no such correlation. Instead, dissolved manganese is available as a redox product, and as such, is indicative of low-oxygen conditions. Here we present evidence for that mechanism in a range of habitats from marine to freshwater, across species, and also present ancillary proxies that support the mechanism as well. For example, iodine is redox-sensitive and varies inversely with Mn; and sulfur stable isotope ratios provide evidence of anoxic sulfate reduction in some circumstances. Further, S may be incorporated trophically whereas other elements appear to be taken up directly from water. This research suggests a potential means to identify individual fish exposure to hypoxia, over entire lifetimes. With further testing and understanding, in the future fish may be able to be used as “mobile monitors” of hypoxic conditions. Walther, Benjamin D. oth Lu, Zunli oth Jackman, George oth Mohan, John oth Walther, Yvonne oth Nissling, Anders oth Weber, Peter K. oth Schmitt, Axel K. oth Enthalten in Elsevier Kamruzzaman, Md. ELSEVIER Investigating the urban heat island effect of transit oriented development in Brisbane 2017 New York, NY [u.a.] (DE-627)ELV000581879 volume:141 year:2015 pages:167-178 extent:12 https://doi.org/10.1016/j.jmarsys.2014.02.014 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U SSG-OPC-GGO 55.80 Verkehrswesen Transportwesen: Allgemeines VZ 74.08 Wirtschaftsgeographie VZ 74.75 Verkehrsplanung Verkehrspolitik VZ AR 141 2015 167-178 12 045F 380 |
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10.1016/j.jmarsys.2014.02.014 doi GBVA2015014000021.pica (DE-627)ELV034628967 (ELSEVIER)S0924-7963(14)00043-8 DE-627 ger DE-627 rakwb eng 380 380 DE-600 380 910 VZ 55.80 bkl 74.08 bkl 74.75 bkl Limburg, Karin E. verfasserin aut In search of the dead zone: Use of otoliths for tracking fish exposure to hypoxia 2015transfer abstract 12 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Otolith chemistry is often useful for tracking provenance of fishes, as well as examining migration histories. Whereas elements such as strontium and barium correlate well with salinity and temperature, experiments that examine manganese uptake as a function of these parameters have found no such correlation. Instead, dissolved manganese is available as a redox product, and as such, is indicative of low-oxygen conditions. Here we present evidence for that mechanism in a range of habitats from marine to freshwater, across species, and also present ancillary proxies that support the mechanism as well. For example, iodine is redox-sensitive and varies inversely with Mn; and sulfur stable isotope ratios provide evidence of anoxic sulfate reduction in some circumstances. Further, S may be incorporated trophically whereas other elements appear to be taken up directly from water. This research suggests a potential means to identify individual fish exposure to hypoxia, over entire lifetimes. With further testing and understanding, in the future fish may be able to be used as “mobile monitors” of hypoxic conditions. Otolith chemistry is often useful for tracking provenance of fishes, as well as examining migration histories. Whereas elements such as strontium and barium correlate well with salinity and temperature, experiments that examine manganese uptake as a function of these parameters have found no such correlation. Instead, dissolved manganese is available as a redox product, and as such, is indicative of low-oxygen conditions. Here we present evidence for that mechanism in a range of habitats from marine to freshwater, across species, and also present ancillary proxies that support the mechanism as well. For example, iodine is redox-sensitive and varies inversely with Mn; and sulfur stable isotope ratios provide evidence of anoxic sulfate reduction in some circumstances. Further, S may be incorporated trophically whereas other elements appear to be taken up directly from water. This research suggests a potential means to identify individual fish exposure to hypoxia, over entire lifetimes. With further testing and understanding, in the future fish may be able to be used as “mobile monitors” of hypoxic conditions. Walther, Benjamin D. oth Lu, Zunli oth Jackman, George oth Mohan, John oth Walther, Yvonne oth Nissling, Anders oth Weber, Peter K. oth Schmitt, Axel K. oth Enthalten in Elsevier Kamruzzaman, Md. ELSEVIER Investigating the urban heat island effect of transit oriented development in Brisbane 2017 New York, NY [u.a.] (DE-627)ELV000581879 volume:141 year:2015 pages:167-178 extent:12 https://doi.org/10.1016/j.jmarsys.2014.02.014 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U SSG-OPC-GGO 55.80 Verkehrswesen Transportwesen: Allgemeines VZ 74.08 Wirtschaftsgeographie VZ 74.75 Verkehrsplanung Verkehrspolitik VZ AR 141 2015 167-178 12 045F 380 |
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in search of the dead zone: use of otoliths for tracking fish exposure to hypoxia |
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In search of the dead zone: Use of otoliths for tracking fish exposure to hypoxia |
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Otolith chemistry is often useful for tracking provenance of fishes, as well as examining migration histories. Whereas elements such as strontium and barium correlate well with salinity and temperature, experiments that examine manganese uptake as a function of these parameters have found no such correlation. Instead, dissolved manganese is available as a redox product, and as such, is indicative of low-oxygen conditions. Here we present evidence for that mechanism in a range of habitats from marine to freshwater, across species, and also present ancillary proxies that support the mechanism as well. For example, iodine is redox-sensitive and varies inversely with Mn; and sulfur stable isotope ratios provide evidence of anoxic sulfate reduction in some circumstances. Further, S may be incorporated trophically whereas other elements appear to be taken up directly from water. This research suggests a potential means to identify individual fish exposure to hypoxia, over entire lifetimes. With further testing and understanding, in the future fish may be able to be used as “mobile monitors” of hypoxic conditions. |
abstractGer |
Otolith chemistry is often useful for tracking provenance of fishes, as well as examining migration histories. Whereas elements such as strontium and barium correlate well with salinity and temperature, experiments that examine manganese uptake as a function of these parameters have found no such correlation. Instead, dissolved manganese is available as a redox product, and as such, is indicative of low-oxygen conditions. Here we present evidence for that mechanism in a range of habitats from marine to freshwater, across species, and also present ancillary proxies that support the mechanism as well. For example, iodine is redox-sensitive and varies inversely with Mn; and sulfur stable isotope ratios provide evidence of anoxic sulfate reduction in some circumstances. Further, S may be incorporated trophically whereas other elements appear to be taken up directly from water. This research suggests a potential means to identify individual fish exposure to hypoxia, over entire lifetimes. With further testing and understanding, in the future fish may be able to be used as “mobile monitors” of hypoxic conditions. |
abstract_unstemmed |
Otolith chemistry is often useful for tracking provenance of fishes, as well as examining migration histories. Whereas elements such as strontium and barium correlate well with salinity and temperature, experiments that examine manganese uptake as a function of these parameters have found no such correlation. Instead, dissolved manganese is available as a redox product, and as such, is indicative of low-oxygen conditions. Here we present evidence for that mechanism in a range of habitats from marine to freshwater, across species, and also present ancillary proxies that support the mechanism as well. For example, iodine is redox-sensitive and varies inversely with Mn; and sulfur stable isotope ratios provide evidence of anoxic sulfate reduction in some circumstances. Further, S may be incorporated trophically whereas other elements appear to be taken up directly from water. This research suggests a potential means to identify individual fish exposure to hypoxia, over entire lifetimes. With further testing and understanding, in the future fish may be able to be used as “mobile monitors” of hypoxic conditions. |
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In search of the dead zone: Use of otoliths for tracking fish exposure to hypoxia |
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