| Literature DB >> 22022513 |
Paulo Catry1, Maria P Dias, Richard A Phillips, José P Granadeiro.
Abstract
Although seabirds that are trans-equatorial migrants show apparently broad overlap among populations in the non-breeding season, such large-scale pattern may conceal subtle but nevertheless key differences in migratory behaviour. These specializations could reflect adaptation to different environments during the breeding season, carry-over effects from the breeding to the nonbreeding period, or asymmetries in competitive ability of birds of different origin. We compared the migratory and wintering behaviour of Cory's shearwaters Calonectris diomedea nesting in Berlengas and in the Selvagens, two colonies in contrasting oceanographic environments, separated by ca. 1200 km. Although no differences were found in winter distribution, there was a marked divergence in timing, route and the use of staging areas during the postbreeding (autumn) migration. Birds from Berlengas typically travelled to oceanic waters in the North Atlantic for an extended stopover, whereas those from Selvagens rarely did so. In the South Atlantic, birds from Selvagens spent more time in flight, perhaps because they had higher energy and nutrient requirements for feather replacement compared to birds from Berlengas, which moult more flight feathers during breeding. Stable isotope analyses of feathers suggested that this variation in activity patterns was unrelated to trophic ecology. Differences in migration routes and stopovers may expose populations to distinct threats, and should be taken into consideration when defining units for conservation purposes and developing appropriate management strategies.Entities:
Mesh:
Year: 2011 PMID: 22022513 PMCID: PMC3191162 DOI: 10.1371/journal.pone.0026079
Source DB: PubMed Journal: PLoS One ISSN: 1932-6203 Impact factor: 3.240
Figure 1Non-breeding distribution of Cory's shearwaters from Berlengas (n = 10, red shading) and from Selvagens (n = 25, blue shading) and activity levels on two main wintering grounds.
Shadings represent the 95% kernel density contours for each group of study birds tracked with geolocators in 2006/07. Triangles indicate colony locations. Note that birds from Berlengas spent more time resting on the sea surface in each of the two main wintering areas.
Timing of migration of birds from Berlengas and Selvagens in winter 2006/07.
| Berlengas | Selvagens | Statistical comparison | |
| Departure date from colony | 22 Oct±11 d | 7 Nov±12 d | Mann-Whitney Test, U = 38.5; P = 0.003 |
| (n = 10) | (n = 23) | ||
| Date of transit south across 10° N | 19 Nov±7 d | 18 Nov±13 d | Mann-Whitney Test, U = 80.0; P = 0.335 |
| (n = 9) | (n = 23) | ||
| Arrival at the wintering area: | Col.: F = 0.03; p = 0.871, Wint. area: F = 0.277; p = 0.604 | ||
| Benguela | 6 Dec±11 d | 5 Dec±11 d | |
| (n = 6) | (n = 10) | ||
| South Atlantic | 10 Dec±9 d | 7 Dec±9 d | |
| (n = 3) | (n = 8) | ||
| Departure from wintering area: | Col: F = 3.52; p = 0.072, Wint area: F = 0.08; p = 0.780 | ||
| Benguela | 20 Feb±5 d | 19 Feb±9 d | |
| (n = 6) | (n = 10) | ||
| South Atlantic | 27 Feb±8 d | 15 Feb±7 d | |
| (n = 3) | (n = 8) | ||
| Return to the colony: | 19 Mar±10 d | 12 Mar±10 d | Col: F = 3.09; p = 0.091, Wint area: F = 0.028; p = 0.888 |
| (n = 9) | (n = 18) | ||
| Benguela | 16 Mar±10 d | 15 Mar±10 d | |
| (n = 6) | (n = 10) | ||
| South Atlantic | 27 Mar±8 d | 09 Mar±9 d | |
| (n = 3) | (n = 8) |
Figure 2Post-breeding (autumn 2006) migration tracks of Cory's shearwaters.
Tracks from (A) Berlengas and from (B) Selvagens that wintered in the South Atlantic. Note that while most individuals from Berlengas made extensive excursions into North Atlantic pelagic waters, those from Selvagens mostly traveled directly from the colony area to the South Atlantic.
Activity patterns and stable isotope levels in primary 8 of Cory's shearwaters from two colonies wintering either in Benguelas or in the central South Atlantic.
| Berlengas | Selvagens | Comparison | |||
| Benguela (n = 6) | Cental South Atlantic (n = 3) | Benguela (n = 10) | Central South Atlantic (n = 8) | ||
| % of time on sea surface | 77.1±5.9 | 78.8±5.2 | 66.9±13.7 | 73.1±3.5 | Col: F = 4.56; p = 0.04, Wint area: F = 1.75; p = 0.20 |
| Landing rate (landings per hour) | 4.5±1.0 | 5.8±1.0 | 4.3±0.8 | 7.1±2.1 | Col: F = 1.19; p = 0.29, Wint area: F = 18.76; p = 0.0002 |
| Night flight index | 0.4±0.1 | 0.9±0.1 | 0.5±0.2 | 0.8±0.2 | Col: F = 0.66; p = 0.42 Wint area: F = 24.16; p<0.0001 |
| δ13N in P8 | 15.09±0.92 | 15.28±0.95 | 15.45±0.36 | 14.56±1.36 | Col: F = 0.09; p = 0.76, Wint area: F = 1.97; p = 0.17 |
| δ13Cin P8 | −15.22±1.21 | −16.16±0.32 | −14.96±0.59 | −16.12±0.31 | Col: F = 0.07; p = 0.93, Wint area: F = 15.49; p = 0.0007 |