Pb. Best et Dm. Schell, STABLE ISOTOPES IN SOUTHERN RIGHT WHALE (EUBALAENA-AUSTRALIS) BALEEN AS INDICATORS OF SEASONAL MOVEMENTS, FEEDING AND GROWTH, Marine Biology, 124(4), 1996, pp. 483-494
Ratios of stable carbon and nitrogen isotopes were examined in the bal
een of 11 southern right whales originating from South Africa, includi
ng one neonate, six juveniles and four adults. Oscillations in carbon
isotope ratios were marked, and indicated feeding north of or at the S
ubtropical Convergence (STC) alternating with feeding south of the STC
. There was an inverse relationship in juveniles between the periodici
ty of the oscillations and the length of the baleen plate, indicating
a reduction in baleen growth with age. The size of the periodicity pre
dicted for the smallest juvenile plate was equivalent to the length of
the baleen at 1 yr of age as estimated from the rate of baleen growth
in calves, suggesting that the oscillations in carbon isotope ratios
were annual events. On this assumption: the timing of the formation of
the most recent carbon enrichment peak could be calculated for each i
ndividual, given the date of death and the rate of baleen growth in th
e preceding year; formation occurred over a period of 100 d from Janua
ry to April (mean in February). A similar analysis indicated that vall
eys in the nitrogen isotope ratios were formed between January and Jun
e (mean in April), and enrichment peaks between August and May (mean i
n December). These patterns were not inconsistent with previous scenar
ios of southern right whale migration, if the enrichment peaks in carb
on isotopes were taken to represent feeding just north of the STC, the
subsequent decline in enrichment levels to represent feeding south of
the STC in autumn, and the persistence of an isotopic signature chara
cteristic of high latitude plankton throughout the winter and early sp
ring to indicate that feeding essentially ceased when the northern mig
ration began, and did not resume until the southern migration was unde
r way. The oscillations in nitrogen isotope ratios would support this
interpretation, if they were assumed to represent cycles of starvation
and recovery. A comparison with baleen growth rates for bowhead whale
s allowed the ages of the six juveniles to be assessed. Their size at
age, when compared to the lengths and growth rates of calves measured
photogrammetrically, suggested that growth in body length of southern
right whales slows markedly between weaning and 1 yr, and may be almos
t negligible from 1 to 4 yr of age.