Marquiss, Mick; Newton, Ian
ORCID: https://orcid.org/0000-0002-7757-4008; Hobson, Keith A.; Kolbeinsson, Yann.
2012
Origins of irruptive migrations by common crossbills Loxia curvirostra into northwestern Europe revealed by stable isotope analysis.
Ibis, 154 (2).
400-409.
10.1111/j.1474-919X.2012.01221.x
Abstract
We used analyses of stable hydrogen isotope (d2H) measurements in Common Crossbill
feathers (d2Hf) to infer the region of origin of Crossbills collected from different irruptions
into Britain, Iceland and the Faeroes, comparing these values with those from birds
sampled in breeding areas in Britain and elsewhere in the western Palaearctic. No differences
in d2Hf values were found between different species or sexes of Crossbills that
could be presumed to have grown their feathers in the same region, but juveniles had
lower d2Hf values than adults that had grown their feathers in the same region. On the
basis mainly of museum skins, immigrant birds were sampled from 30 different irruption
years, spanning the period 1866–2009, with annual samples varying from one to 29 individuals.
The variation in d2Hf values within irruptions was substantially less than the variation
between irruptions, indicating that irruptions in different years originated in
different parts of the western Palaearctic boreal zone. Birds with lower d2Hf values
tended to arrive later in the migration season, which was consistent with the idea that
they had travelled further. In 17 of the irruption years, the birds had mean d2Hf values
more than )120&, suggesting that they had originated somewhere in the region extending
from northern Scandinavia to northwestern Russia. In these years the birds arrived
early, in June and July. In 10 of the irruption years, the mean d2Hf values were between
)120 and )130&, suggesting origins further east, in northern Russia, east of Archangel
(about 40�E). In only three of the 30 years (1898, 2002, 2009) the mean d2Hf values
were even lower (< 130&), and these birds arrived in late July, August and September.
Birds in these three irruptions had probably come from Siberia, east of the Ural Mountains.
In at least three irruption years (1898, 1927, 1985) the observed range of d2Hf
values suggested that birds had come from more than one of these regions, including east of the Urals in 1898 and 1927.
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