High-resolution isotope analysis of young alewife Alosa pseudoharengus otoliths: assessment of temporal resolution and reconstruction of habitat occupancy and thermal history
Otoliths of age 0 year alewife Alosa pseudoharengus collected in different Lake Michigan habitats were microsampled, and carbon and oxygen isotope ratios (δ18Ootolith and δ13Cotolith) of resulting microsamples were quantified. To assess the temporal resolution of the method, age and otolith growth r...
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| Published in | Journal of fish biology Vol. 73; no. 10; pp. 2434 - 2451 |
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| Main Authors | , , , |
| Format | Journal Article |
| Language | English |
| Published |
Oxford, UK
Blackwell Publishing Ltd
01.12.2008
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| Subjects | |
| Online Access | Get full text |
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| Abstract | Otoliths of age 0 year alewife Alosa pseudoharengus collected in different Lake Michigan habitats were microsampled, and carbon and oxygen isotope ratios (δ18Ootolith and δ13Cotolith) of resulting microsamples were quantified. To assess the temporal resolution of the method, age and otolith growth rates were also estimated by counting otolith daily growth increments. Core and outer intra‐otolith samples averaged 36 and 23 days, respectively. Because of the accretionary nature of otolith growth, a habitat switch by a larva occurring between 0 and 18 days post‐hatch may not be recognized by this approach. Taking this temporal resolution into account, A. pseudoharengus habitat occupancy and thermal history in nearshore Lake Michigan, and a connecting drowned river‐mouth lake were documented. Comparisons between δ18Ootolith and δ13Cotolith profiles, and isotope values of Lake Michigan habitats suggested that movements by individual fish between a nearshore area of Lake Michigan proper and drowned river‐mouth lake habitats were rare. Some individuals evidently moved between habitats, and such movements occurred during different periods of ontogeny. Thermal reconstructions, based on δ18Ootolith values suggested that during early life (e.g. first month of life) young A.pseudoharengus appeared to inhabit microhabitats with temperatures greater than mean epilimnetic temperatures. This study demonstrates not only the utility of intra‐otolith geochemical analysis to describe the complexity of fish behaviour in fresh water but also identifies limitations of the present approach. |
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| AbstractList | Otoliths of age 0 year alewife Alosa pseudoharengus collected in different Lake Michigan habitats were microsampled, and carbon and oxygen isotope ratios (δ18Ootolith and δ13Cotolith) of resulting microsamples were quantified. To assess the temporal resolution of the method, age and otolith growth rates were also estimated by counting otolith daily growth increments. Core and outer intra‐otolith samples averaged 36 and 23 days, respectively. Because of the accretionary nature of otolith growth, a habitat switch by a larva occurring between 0 and 18 days post‐hatch may not be recognized by this approach. Taking this temporal resolution into account, A. pseudoharengus habitat occupancy and thermal history in nearshore Lake Michigan, and a connecting drowned river‐mouth lake were documented. Comparisons between δ18Ootolith and δ13Cotolith profiles, and isotope values of Lake Michigan habitats suggested that movements by individual fish between a nearshore area of Lake Michigan proper and drowned river‐mouth lake habitats were rare. Some individuals evidently moved between habitats, and such movements occurred during different periods of ontogeny. Thermal reconstructions, based on δ18Ootolith values suggested that during early life (e.g. first month of life) young A.pseudoharengus appeared to inhabit microhabitats with temperatures greater than mean epilimnetic temperatures. This study demonstrates not only the utility of intra‐otolith geochemical analysis to describe the complexity of fish behaviour in fresh water but also identifies limitations of the present approach. Otoliths of age 0 year alewife Alosa pseudoharengus collected in different Lake Michigan habitats were microsampled, and carbon and oxygen isotope ratios ( δ 18 O otolith and δ 13 C otolith ) of resulting microsamples were quantified. To assess the temporal resolution of the method, age and otolith growth rates were also estimated by counting otolith daily growth increments. Core and outer intra‐otolith samples averaged 36 and 23 days, respectively. Because of the accretionary nature of otolith growth, a habitat switch by a larva occurring between 0 and 18 days post‐hatch may not be recognized by this approach. Taking this temporal resolution into account, A. pseudoharengus habitat occupancy and thermal history in nearshore Lake Michigan, and a connecting drowned river‐mouth lake were documented. Comparisons between δ 18 O otolith and δ 13 C otolith profiles, and isotope values of Lake Michigan habitats suggested that movements by individual fish between a nearshore area of Lake Michigan proper and drowned river‐mouth lake habitats were rare. Some individuals evidently moved between habitats, and such movements occurred during different periods of ontogeny. Thermal reconstructions, based on δ 18 O otolith values suggested that during early life ( e.g. first month of life) young A. pseudoharengus appeared to inhabit microhabitats with temperatures greater than mean epilimnetic temperatures. This study demonstrates not only the utility of intra‐otolith geochemical analysis to describe the complexity of fish behaviour in fresh water but also identifies limitations of the present approach. Otoliths of age 0 year alewife Alosa pseudoharengus collected in different Lake Michigan habitats were microsampled, and carbon and oxygen isotope ratios (d18Ootolith and d13Cotolith) of resulting microsamples were quantified. To assess the temporal resolution of the method, age and otolith growth rates were also estimated by counting otolith daily growth increments. Core and outer intra-otolith samples averaged 36 and 23 days, respectively. Because of the accretionary nature of otolith growth, a habitat switch by a larva occurring between 0 and 18 days post-hatch may not be recognized by this approach. Taking this temporal resolution into account, A. pseudoharengus habitat occupancy and thermal history in nearshore Lake Michigan, and a connecting drowned river-mouth lake were documented. Comparisons between d18Ootolith and d13Cotolith profiles, and isotope values of Lake Michigan habitats suggested that movements by individual fish between a nearshore area of Lake Michigan proper and drowned river-mouth lake habitats were rare. Some individuals evidently moved between habitats, and such movements occurred during different periods of ontogeny. Thermal reconstructions, based on d18Ootolith values suggested that during early life (e.g. first month of life) young A.pseudoharengus appeared to inhabit microhabitats with temperatures greater than mean epilimnetic temperatures. This study demonstrates not only the utility of intra-otolith geochemical analysis to describe the complexity of fish behaviour in fresh water but also identifies limitations of the present approach. |
| Author | Höök, T. O. Dufour, E. Patterson, W. P. Rutherford, E. S. |
| Author_xml | – sequence: 1 givenname: E. surname: Dufour fullname: Dufour, E. email: elise.dufour@mnhn.fr organization: Muséum National d'Histoire Naturelle, UMR 5197 Archéozoologie, Histoire des Sociétés Humaines et des Peuplements Animaux, 57 rue Cuvier, CP 56, 75231 Paris cedex 5, France , ‡ University of Michigan, School of Natural Resources and Environment, Cooperative Institute for Limnology and Ecosystems Research , § NOAA, Great Lakes Environmental Research Lab 2205 Commonwealth Blvd., Ann Arbor, MI 48105, U.S.A. and ¶ Saskatchewan Isotope Laboratory, Department of Geological Sciences, University of Saskatchewan, 114 Science Place, Saskatoon, SK S7N 5E2, Canada – sequence: 2 givenname: T. O. surname: Höök fullname: Höök, T. O. organization: Muséum National d'Histoire Naturelle, UMR 5197 Archéozoologie, Histoire des Sociétés Humaines et des Peuplements Animaux, 57 rue Cuvier, CP 56, 75231 Paris cedex 5, France , ‡ University of Michigan, School of Natural Resources and Environment, Cooperative Institute for Limnology and Ecosystems Research , § NOAA, Great Lakes Environmental Research Lab 2205 Commonwealth Blvd., Ann Arbor, MI 48105, U.S.A. and ¶ Saskatchewan Isotope Laboratory, Department of Geological Sciences, University of Saskatchewan, 114 Science Place, Saskatoon, SK S7N 5E2, Canada – sequence: 3 givenname: W. P. surname: Patterson fullname: Patterson, W. P. organization: Muséum National d'Histoire Naturelle, UMR 5197 Archéozoologie, Histoire des Sociétés Humaines et des Peuplements Animaux, 57 rue Cuvier, CP 56, 75231 Paris cedex 5, France , ‡ University of Michigan, School of Natural Resources and Environment, Cooperative Institute for Limnology and Ecosystems Research , § NOAA, Great Lakes Environmental Research Lab 2205 Commonwealth Blvd., Ann Arbor, MI 48105, U.S.A. and ¶ Saskatchewan Isotope Laboratory, Department of Geological Sciences, University of Saskatchewan, 114 Science Place, Saskatoon, SK S7N 5E2, Canada – sequence: 4 givenname: E. S. surname: Rutherford fullname: Rutherford, E. S. organization: Muséum National d'Histoire Naturelle, UMR 5197 Archéozoologie, Histoire des Sociétés Humaines et des Peuplements Animaux, 57 rue Cuvier, CP 56, 75231 Paris cedex 5, France , ‡ University of Michigan, School of Natural Resources and Environment, Cooperative Institute for Limnology and Ecosystems Research , § NOAA, Great Lakes Environmental Research Lab 2205 Commonwealth Blvd., Ann Arbor, MI 48105, U.S.A. and ¶ Saskatchewan Isotope Laboratory, Department of Geological Sciences, University of Saskatchewan, 114 Science Place, Saskatoon, SK S7N 5E2, Canada |
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| Snippet | Otoliths of age 0 year alewife Alosa pseudoharengus collected in different Lake Michigan habitats were microsampled, and carbon and oxygen isotope ratios... Otoliths of age 0 year alewife Alosa pseudoharengus collected in different Lake Michigan habitats were microsampled, and carbon and oxygen isotope ratios ( δ... |
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| Title | High-resolution isotope analysis of young alewife Alosa pseudoharengus otoliths: assessment of temporal resolution and reconstruction of habitat occupancy and thermal history |
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