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Analysis of stable isotope ratios in blood of tracked wandering albatrosses fails to distinguish a δ(13) C gradient within their winter foraging areas in the southwest Atlantic Ocean.
Ceia, Filipe R; Ramos, Jaime A; Phillips, Richard A; Cherel, Yves; Jones, Daniel C; Vieira, Rui P; Xavier, José C.
Afiliação
  • Ceia FR; MARE - Marine and Environmental Sciences Centre, Department of Life Sciences, Universidade de Coimbra, 3004-517, Coimbra, Portugal.
  • Ramos JA; MARE - Marine and Environmental Sciences Centre, Department of Life Sciences, Universidade de Coimbra, 3004-517, Coimbra, Portugal.
  • Phillips RA; British Antarctic Survey, Natural Environment Research Council, High Cross, Madingley Road, Cambridge, CB3 0ET, UK.
  • Cherel Y; Centre d'Etudes Biologiques de Chizé, UPR 7372 du CNRS-Université de La Rochelle, 79360, Villiers-en-Bois, France.
  • Jones DC; British Antarctic Survey, Natural Environment Research Council, High Cross, Madingley Road, Cambridge, CB3 0ET, UK.
  • Vieira RP; MARE - Marine and Environmental Sciences Centre, Department of Life Sciences, Universidade de Coimbra, 3004-517, Coimbra, Portugal.
  • Xavier JC; Departamento de Biologia & CESAM, Universidade de Aveiro, Campus Universitário de Santiago, 3810-193, Aveiro, Portugal.
Rapid Commun Mass Spectrom ; 29(24): 2328-36, 2015 Dec 30.
Article em En | MEDLINE | ID: mdl-26563703
ABSTRACT
RATIONALE The main limitation of isotopic tracking for inferring distribution is the lack of detailed reference maps of the isotopic landscape (i.e. isoscapes) in the marine environment. Here, we attempt to map the marine δ(13) C isoscape for the southwestern sector of the Atlantic Ocean, and assess any temporal variation using the wandering albatross as a model species.

METHODS:

Tracking data and blood and diet samples were collected monthly from wandering albatrosses rearing chicks at Bird Island, South Georgia, during the austral winter between May and October 2009. The δ(13) C and δ(15) N values were measured by mass spectrometry in plasma and blood cells, and related to highly accurate data on individual movements and feeding activity obtained using three types of device GPS, activity (immersion) loggers and stomach temperature probes.

RESULTS:

The tracked birds foraged in waters to the north or northwest of South Georgia, including the Patagonian shelf-break, as far as 2000 km from the colony. The foraging region encompassed the two main fronts in the Southern Ocean (Polar and Subantarctic fronts). The δ(13) C values varied by only 2.1 ‰ in plasma and 2.5 ‰ in blood cells, and no relationships were found between the δ(13) C values in plasma and the mean latitude or longitude of landings or feeding events of each individual.

CONCLUSIONS:

The failure to distinguish a major biogeographic gradient in δ(13) C values suggest that these values in the south Atlantic Ocean are fairly homogeneous. There was no substantial variation among months in either the δ(13) C or the δ(15) N values of plasma or blood cells of tracked birds. As birds did not show a significant change in diet composition or foraging areas during the study period, these results provide no evidence for major temporal variation in stable isotope ratios in consumer tissues, or in the regional marine isoscape in the austral winter of 2009.
Assuntos

Texto completo: 1 Coleções: 01-internacional Base de dados: MEDLINE Assunto principal: Aves / Isótopos de Carbono / Migração Animal Limite: Animals Idioma: En Ano de publicação: 2015 Tipo de documento: Article

Texto completo: 1 Coleções: 01-internacional Base de dados: MEDLINE Assunto principal: Aves / Isótopos de Carbono / Migração Animal Limite: Animals Idioma: En Ano de publicação: 2015 Tipo de documento: Article