Lack of Stable-Isotope Differences Between Canada Goose Populations Nesting in the Subarctic and Temperate Zones

Ratios of stable isotopes in feathers have great potential for identifying the connectivity of bird migrations and the origin of harvested individuals of game species. In particular, the relationship between the hydrogen ratio due to latitudinal variation in precipitation (δDp) and that in feathers...

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Published in:The Condor
Main Authors: Kristin Mylecraine Munafo, Lisle Gibbs
Format: Text
Language:English
Published: American Ornithological Society 2012
Subjects:
Online Access:https://doi.org/10.1525/cond.2012.100091
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spelling ftbioone:10.1525/cond.2012.100091 2023-07-30T04:02:44+02:00 Lack of Stable-Isotope Differences Between Canada Goose Populations Nesting in the Subarctic and Temperate Zones Kristin Mylecraine Munafo Lisle Gibbs Kristin Mylecraine Munafo Lisle Gibbs world 2012-08-31 text/HTML https://doi.org/10.1525/cond.2012.100091 en eng American Ornithological Society doi:10.1525/cond.2012.100091 All rights reserved. https://doi.org/10.1525/cond.2012.100091 Text 2012 ftbioone https://doi.org/10.1525/cond.2012.100091 2023-07-09T09:23:43Z Ratios of stable isotopes in feathers have great potential for identifying the connectivity of bird migrations and the origin of harvested individuals of game species. In particular, the relationship between the hydrogen ratio due to latitudinal variation in precipitation (δDp) and that in feathers (δDf) is often used to determine unknown individuals' latitude of origin. We assessed this relationship between Canada Geese nesting in the temperate zone (Branta canadensis maxima) and the subarctic (B. c. interior). For this game species, the origin of harvested birds is important for developing management that maintains a desirable level of harvest while ensuring continued viability of all subspecies and breeding populations. We collected freshly grown primaries from three populations of interior and five of maxima and analyzed them for δD, δ13C, and δ15N. Multivariate analysis suggested no overall differences in isotopic composition between subspecies. A univariate assessment indicated a significant difference in δ15Nf, despite substantial overlap between subspecies, and no difference in δDf or δ13Cf. Of particular interest is the lack of difference in δDf, despite the large latitudinal differences in δDp and between the subspecies' breeding ranges. Values of δDf averaged -131.85‰ ± 1.36 for interior, -131.63‰ ± 0.71 for maxima, and we found no overall relationship between δDf and δDp. Overall, our results suggest that δD, δ13C, and δ15N alone have limited ability to discriminate between subspecies interior and maxima and hence have limited applicability for estimating the origin of harvested birds and/or identifying molt migrants of maxima. Text Branta canadensis Canada Goose Subarctic BioOne Online Journals Canada The Condor 114 3 491 499
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description Ratios of stable isotopes in feathers have great potential for identifying the connectivity of bird migrations and the origin of harvested individuals of game species. In particular, the relationship between the hydrogen ratio due to latitudinal variation in precipitation (δDp) and that in feathers (δDf) is often used to determine unknown individuals' latitude of origin. We assessed this relationship between Canada Geese nesting in the temperate zone (Branta canadensis maxima) and the subarctic (B. c. interior). For this game species, the origin of harvested birds is important for developing management that maintains a desirable level of harvest while ensuring continued viability of all subspecies and breeding populations. We collected freshly grown primaries from three populations of interior and five of maxima and analyzed them for δD, δ13C, and δ15N. Multivariate analysis suggested no overall differences in isotopic composition between subspecies. A univariate assessment indicated a significant difference in δ15Nf, despite substantial overlap between subspecies, and no difference in δDf or δ13Cf. Of particular interest is the lack of difference in δDf, despite the large latitudinal differences in δDp and between the subspecies' breeding ranges. Values of δDf averaged -131.85‰ ± 1.36 for interior, -131.63‰ ± 0.71 for maxima, and we found no overall relationship between δDf and δDp. Overall, our results suggest that δD, δ13C, and δ15N alone have limited ability to discriminate between subspecies interior and maxima and hence have limited applicability for estimating the origin of harvested birds and/or identifying molt migrants of maxima.
author2 Kristin Mylecraine Munafo
Lisle Gibbs
format Text
author Kristin Mylecraine Munafo
Lisle Gibbs
spellingShingle Kristin Mylecraine Munafo
Lisle Gibbs
Lack of Stable-Isotope Differences Between Canada Goose Populations Nesting in the Subarctic and Temperate Zones
author_facet Kristin Mylecraine Munafo
Lisle Gibbs
author_sort Kristin Mylecraine Munafo
title Lack of Stable-Isotope Differences Between Canada Goose Populations Nesting in the Subarctic and Temperate Zones
title_short Lack of Stable-Isotope Differences Between Canada Goose Populations Nesting in the Subarctic and Temperate Zones
title_full Lack of Stable-Isotope Differences Between Canada Goose Populations Nesting in the Subarctic and Temperate Zones
title_fullStr Lack of Stable-Isotope Differences Between Canada Goose Populations Nesting in the Subarctic and Temperate Zones
title_full_unstemmed Lack of Stable-Isotope Differences Between Canada Goose Populations Nesting in the Subarctic and Temperate Zones
title_sort lack of stable-isotope differences between canada goose populations nesting in the subarctic and temperate zones
publisher American Ornithological Society
publishDate 2012
url https://doi.org/10.1525/cond.2012.100091
op_coverage world
geographic Canada
geographic_facet Canada
genre Branta canadensis
Canada Goose
Subarctic
genre_facet Branta canadensis
Canada Goose
Subarctic
op_source https://doi.org/10.1525/cond.2012.100091
op_relation doi:10.1525/cond.2012.100091
op_rights All rights reserved.
op_doi https://doi.org/10.1525/cond.2012.100091
container_title The Condor
container_volume 114
container_issue 3
container_start_page 491
op_container_end_page 499
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