Geology topics

David A. Methven

Publications and source records attributed to David A. Methven.

3 recordsLinked to original sources

USGS1992

Threshold foraging behavior of baleen whales

We conducted hydroacoustic surveys for capelin Mallotus villosus in Witless Bay, Newfoundland, Canada, on 61 days during the summers of 1983 to 1985. On 32 of those days in whlch capelin surveys were conducted, we observed a total of 129 baleen whales - Including 93 humpback Megaptera novaeangliae , 31 minke Balaenoptera acutorostrata and 5 fin whales B. phvsalus . Although a few whales were observed when capelin schools were scarce, the majority (96%) of whales were observed when mean daily capelin densities exceeded 5 schools per linear km surveyed (range of means over 3 yr: 0.0 to 14.0 schools km -1 ). Plots of daily whale abundance (no. h -1 surveyed) vs daily capelin school density (mean no. schools km -1 surveyed) in each summer revealed that baleen whales have a threshold foraging response to capelin density. Thresholds were estimated using a simple itterative step-function model. Foraging thresholds of baleen whales (7.3, 5.0, and 5.8 schools km -1 ) varied between years in relation to the overall abundance of capelin schools in the study area during summer (means of 7.2, 3.3, and 5.3 schools km -1 , respectively).

Newfoundland↗

USGS1991

Seasonal abundance and vertical distribution of capelin ( Mallotus villosus ) in relation to water temperature at a coastal site off eastern Newfoundland

The seasonal abundance and vertical distribution of capelin in relation to water temperature have been investigated by conducting repeated hydroacoustic surveys at a coastal site off eastern Newfoundland. Water temperatures were warmer in 1983 than in 1984 as indicated by the earlier appearance and greater depth of the seasonal thermocline. Correspondingly, schools of capelin appeared earlier, were more abundant, and extended deeper in the water column in 1983 than in 1984. Most capelin were found between the surface and the 5°C isotherm. In both years, initial peaks of capelin abundance occurred when nearshore water temperatures increased from about 0-1 ° C to above 6 ° C and, at or near, periods of maximum tidal oscillation. Short-term variations in the depth of the 5 ° C isotherm were related to nearshore wind-induced upwelling events. Annual variations corresponded to the volume of cold (>0 ° C) water and sea-ice transported south by the Labrador Current.

Newfoundland↗

USGS1989

Seasonal and annual variation in the diet of Atlantic cod ( Gadus morhua ) in relation to the abundance of capelin ( Mallotus villosus ) off eastern Newfoundland, Canada

The importance of capelin as prey for cod has long been known (Thompson, 1943; and see Lilly (1987) for a review); however, no studies have been conducted on how the highly dynamic seasonal and yearly variations in capelin abundance affect cod diet. We studied the occurrence of capelin in cod stomachs in relation to the relative abundance of capelin at Witless Bay, Newfoundland (47°15’N 52°46’W), during June, July and August, 1982-1984. The mean number of capelin per stomach and the per cent occurrence of stomachs containing capelin were determined for each collection of stomachs. A total of 680 stomachs were examined. Cod were sampled from those caught in gillnets by fishermen and averaged 66 cm ± 8 (s.d.) in 1983 and 62 cm ± 8 (s.d.) in 1984. Relative abundance of capelin in the local habitat was determined by conducting hydroacoustic surveys around Gull Island in Witless Bay, the same area where cod were collected for stomach content analysis. Only hydroacoustic surveys conducted within three days of cod stomach collections were analyzed. Further details of hydroacoustic surveys including quantifications of acoustic echograms are described in Piatt (1989).

Newfoundland↗