Cl. Baduini et al., Determining the body condition of short-tailed shearwaters: implications for migratory flight ranges and starvation events, MAR ECOL-PR, 222, 2001, pp. 265-277
Short-tailed shearwaters Puffinus tenuirostris migrate annually from breedi
ng areas in southeast Australia and Tasmania to the Bering Sea to feed on a
bundant prey aggregations, mainly euphausiids, Occasionally thousands of sh
earwaters die of starvation en route, within, or on return from the Bering
Sea, Collection of live and dead shearwaters in the southeastern Bering Sea
in 1997, 1998, and 1999 allowed us to measure seasonal changes in energy r
eserves during a major mortality event, As birds lost body mass, lipid mass
initially decreased faster than that of pectoralis muscle, but loss of pec
toralis mass increased markedly at a body mass around 500 g when lipids wer
e almost depleted (similar to 33 g remaining). Death occurred as body mass
approached 426 g. Individuals near this body mass had lipid values permitti
ng estimated flight ranges of 140 to 400 km, a range less than that potenti
ally covered in 1 d by shearwaters searching for prey (440 to 1124 km d(-1)
). Seasonal differences in body composition were most striking among body a
nd bone marrow lipid contents, with the lowest values occurring during the
die-off in fall 1997 and in fall 1998. The lack of shearwater mortality in
fall 1998 may have resulted from more consistent winds that decreased fligh
t costs and from greater availability of alternative fish prey. Our data al
low estimates of usable energy stores and flight ranges based on lipid rese
rves in short-tailed shearwaters. Estimated flight ranges suggest that if f
eeding conditions are poor near Japan or near other termination points of t
he transequatorial migration routes shearwaters may have few reserves avail
able to support foraging for food and starvation events may occur, Our find
ings suggest how their energetic strategies and migration are shaped by sea
sonal and annual variability of prey during transglobal movements of short-
tailed shearwaters between oceanic regions.