Abstract
Age validation of bluenose Hyperoglyphe antarctica was sought using the independent bomb chronometer procedure. Radiocarbon ( 14 C) levels were measured in core micro‐samples from 12 otoliths that had been aged using a zone count method. The core 14 C measurement for each fish was compared with the value on a surface water reference curve for the calculated birth year of the fish. There was good agreement, indicating that the line‐count ageing method described here is not substantially biased. A second micro‐sample was also taken near the edge of nine of the otolith cross‐sections to help define a bomb‐carbon curve for waters deeper than 200–300 m. There appears to be a 10 to 15 year lag in the time it takes the 14 C to reach the waters where adult H. antarctica are concentrated. The maximum estimated age of this species was 76 years, and females grow significantly larger than males. Von Bertalanffy growth curves were estimated, and although they fit the available data reasonably well, the lack of aged juvenile fish results in the K and t 0 parameters being biologically meaningless. Consequently, curves that are likely to better represent population growth were estimated by forcing t 0 to be −0·5.