, Volume 151, Issue 4, pp 605–615 | Cite as

Stable carbon and nitrogen isotope ratio profiling of sperm whale teeth reveals ontogenetic movements and trophic ecology

  • Sónia MendesEmail author
  • Jason Newton
  • Robert J. Reid
  • Alain F. Zuur
  • Graham J. Pierce
Population Ecology


Teeth from male sperm whales (Physeter macrocephalus) stranded in the North-eastern Atlantic were used to determine whether chronological profiles of stable isotope ratios of C (δ13C) and N (δ15N) across dentine growth layers could be used to detect known ontogenetic benchmarks in movements and trophic ecology. Profiles showed a general decrease in δ13C (median = 1.91‰) and an increase in δ15N (median = 2.42‰) with age. A marked decline in δ13C occurred for all 11 teeth around 9–10 years and again for six individuals around 20 years. After the early twenties the δ13C continued to decline with age for all teeth. These results are consistent with males segregating from natal groups in low latitudes with the onset of puberty between 4 and 15 years and gradually dispersing pole-ward into 13C-depleted temperate waters. Penetration into further depleted, productive high latitudes after the age of 20 might facilitate the spurt of accelerated growth rate observed around this age. Breeding migrations back to lower latitudes were not reflected in the δ13C profiles possibly due to being short compared to the time spent feeding in high latitudes. The timings of marked isotopic change in the δ15N profiles reflect those of the δ13C profiles, suggesting a link between dietary changes and movements. The observed increase in δ15N with age is likely to be caused by a trophic level increase as males grow in size, probably feeding on larger prey. An additional explanation could be that, in the higher latitudes of the North Atlantic, the main prey source is the high trophic level squid Gonatus fabricii. Also, the lower latitudes from where males disperse are depleted in basal 15N. Profiles of δ13C and δ15N in sperm whale teeth gathered from different regions, sexes, and periods in time, could provide a unique way to understand the ecology of this species across different oceans.


Dentine Dietary history Migration Physeter macrocephalus Stable isotopes 



We thank Colin MacLeod, Jennifer Learmonth, Patricia Lastra, Gabriele Stowasser and David Mackenzie, at the University of Aberdeen, for help with sample preparation and Dave McNamara (Donegal County Council) for the provision of the Irish tooth. We thank Colin MacLeod and two anonymous reviewers for useful comments on the manuscript. S. M. was supported through a PhD studentship by the Portuguese Foundation for Science and Technology (grant SFRH/BD/5466/2001), and the stable isotope analyses were carried out at the NERC Life Sciences Mass Spectrometry Facility (application no. EK74-11/04).


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Copyright information

© Springer-Verlag 2006

Authors and Affiliations

  • Sónia Mendes
    • 1
    Email author
  • Jason Newton
    • 2
  • Robert J. Reid
    • 3
  • Alain F. Zuur
    • 4
  • Graham J. Pierce
    • 1
  1. 1.School of Biological Sciences (Zoology)University of AberdeenAberdeenUK
  2. 2.NERC Life Sciences Mass Spectrometry FacilitySUERCEast KilbrideUK
  3. 3.Wildlife UnitSAC Veterinary ServicesInvernessUK
  4. 4.Highland Statistics LimitedNewburghUK

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