Witch Flounder: Age Determination Methods for Northwest Atlantic Species

Witch Flounder, Glyptocephalus cynoglossus

J.M. Burnett

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Witch flounder, or grey sole, is a small-mouthed, right-sided pleuronectid distributed in deep, cold waters from Labrador to North Carolina. Witch flounder are sedentary and do not undertake seasonal migrations (Bigelow and Schroeder 1953). Most commercial catches occur at depths of 90-270 m over mud bottom at temperatures ranging from 2C in winter to 9C during summer (Burnett and Clark 1983). Although numerous stocks of witch flounder have been delineated in Canadian waters (Fairbairn 1981, Bowering and Misra 1982), no stock identification studies have been conducted for our region. Witch flounder in the Gulf of Maine-Georges Bank region are considered to be a unit stock for assessment purposes.

Relative to other flatfish in the region, the witch flounder can be characterized as slow-growing, late-maturing, and long-lived. The maximum observed length and age for the Gulf of Maine-Georges Bank region are 72 cm total length and 30 years, respectively. Median age at sexual maturity for male witch flounder is 4 years and 6.5 years for females. Spawning occurs over a protracted period with a peak occurring during May and June. The pelagic larval stage is lengthy compared with other flounders, lasting from 4-6 months (Bigelow and Schroeder 1953) to a year (Evseenko and Nevinsky 1973).

The first study of witch flounder age was conducted by Huntsman (1918), who used scales as the ageing structure. Molander (1925) and Bowers (1960) both employed whole otoliths for witch flounder from the eastern Atlantic, but did not validate their methodology. Powles and Kennedy (1967) polished whole otoliths from Scotian Shelf samples, validating their interpretation of hyaline zones as annuli by using modal analysis of backcalculated mean lengths at age of younger fish. Burnett (1987) examined thin-sectioned otoliths from the Gulf of Maine-Georges Bank collections. The method was validated by an examination of the seasonal progression of otolith edge type.

At the NEFSC Woods Hole Laboratory, thin-sectioned otoliths are examined with the following exceptions: 1) whole otoliths are used when possible for younger fish to save preparation time, and 2) scales are used for commercial samples when dealers do not allow otolith extraction. However, scales cannot be aged accurately beyond 10 years of age due to compression of annuli on the scale edge. Upon removal from the fish, samples are stored dry.

Although either otolith is a suitable structure, the ventral otolith (easily distinguished in larger fish by its greater length and lesser height) generally provides better interpretations in older fish due to minimal dorsolateral compression within the sacculus. A low speed macrotome saw is used for thin-sectioning otoliths to thicknesses of 0.178 ± 0.051 mm (0.007 ± 0.002 inches); the most successful orientation of the section is transversely through the nucleus along the dorsolateral axis. The resulting section allows tracing of hyaline zones from the sulcus area into the otolith body.

Sections are immersed in ethyl alcohol and viewed against a dark background at magnifications of 25-50x with reflected light. Age determinations are based on the number of hyaline zones present. Figure 1 shows a section from an otolith taken from a 54 cm female assigned an age of 17 years. Features of interest include: a) poorly defined first annulus; b) broad, well defined opaque and hyaline zones present through ages 2-9; c) a check between annuli 6 and 7, possibly associated with initial reproductive efforts; d) narrowing of both zones subsequent to age 5; and e) splitting of opaque zones which can be mistaken for annuli in the outer fields. The section from an 11 cm male (Figure 2) illustrates both a settling check within the nucleus associated with metamorphosis and settling to a benthic habitat and me lack of a well-defined first annulus; this fish, captured in July, was assigned an age of 1+. Figure 3 represents a typical intermediate aged fish, in this instance, a 34 cm female captured in April. Again, the first annulus is poorly defined; however, the settling check and annuli 2-4 are prominent in this age-5 interpretation. For older fish, both lateral fields must be utilized: earlier annuli, more distinct and less subject to zone-splitting in the ventral field, can be traced around to the dorsal field. This generally affords better interpretation of later annuli. Later annuli may also be more accurately evaluated within the sulcus, providing a point of reference has been established in the otolith body. Care must be taken in evaluating the outer annuli of older fish and in categorizing the type and width of edge material; often increasing magnifications and the examination of the otolith halves are necessary in both instances.

An important clue in the age-determination process is also provided by the spacing of opaque and hyaline zones. Annual incremental growth of witch flounder diminishes sharply after age 12 and remains fairly uniform thereafter; often decisions between true annuli and splits within opaque zones can be made by examining the spacing of otolith events.

To summarize, thin sectioning of otoliths is a reliable method for witch flounder. Sectioning increases the preparation time, but the resulting improvement in accuracy of the age determinations justifies the approach. Reliable age determinations beyond age 10 will be an important prerequisite for analytical assessment of this species.

References

Bigelow, H.B., and W.C. Schroeder. 1953. Fishes of the Gulf of Maine. U.S. Fish Wildl. Serv., Fish. Bull. 53(74), 577 p.

Bowering, W.R., and R.K. Misra. 1982. Comparisons of witch flounder (Glyptocephalus cynoglossus) stocks of the Newfoundland-Labrador area, based upon a new multivariate analysis method for meristic characters. Can. J. Fish. Aquat. Sci 39:564-570.

Bowers, A.B. 1960. Growth of the witch (Glyptocephalus cynoglossus) in the Irish Sea. Int. Counc. Explor. Sea, J. Cons. 25:168-176.

Burnett, J. 1987. The population biology of the witch flounder (Glyptocephalus cynoglossus L.) in the Gulf of Maine-Georges Bank region. M.S. thesis, Univ. Mass., Amherst, MA 01003, 116 p.

Burnett, J., and S.H. Clark. 1983. Status of witch flounder in the Gulf of Maine - 1983. Ref. Doc. 83-36, Woods Hole Lab., Northeast Fish. Cent., Natl. Mar. Fish. Serv., NOAA, Woods Hole, MA 02543, 31 p.

Evseenko, S.A., and N.M. Nevinsky. 1973. Breeding and development of witch flounder (Glyptocephalus cynoglossus) in the Northwest Atlantic Ocean. Res. Doc. 73/49, Ser. 2990, Int. Comm. Northw. Atl. Fish., Dartmouth, Nova Scotia, Canada B2Y 3Y9, 23 p. mimeo.

Fairbairn, D.J. 1981. Which witch is which? A study of the stock structure of witch flounder (Glyptocephalus cynoglossus) in the Newfoundland region. Can. J. Fish. Aquat. Sci. 38:782-794.

Huntsman, A.G. 1918. The growth of scales in fishes. Trans. R. Can. Inst. 12:61-101.

Molander, A.R. 1925. Observations of the witch (Glyptocephalus cynoglossus L.) and its growth. Publications de Circonstance, Cons. Perm. Int. Explor. Mer 85.

Powles, P.M., and V.S. Kennedy. 1967. Age determination of Nova Scotian grey sole, Glyptocephalus cynoglossus L., from otoliths. Int. Comm. Northw. Atl. Fish., Res. Bull. 4:91-100.