Spawning migration patterns were compared between sympatric populations of the anadromous Japan Sea (JS) form and Pacific Ocean (PO) form of the threespine stickleback Gasterosteus aculeatus in the Lake Akkeshi-Bekanbeushi River system, eastern Hokkaido, Japan. In Akkeshi Bay and Lake Akkeshi, the JS form had longer collecting peak periods and more collection peaks than the PO form. Furthermore, although the PO form migrated upstream in freshwater habitats, the greater part of the JS form stayed in brackish waters before breeding. These findings suggest that the 2 forms have distinctly different spawning migration patterns and breeding grounds.
of the correlation coefficients and regression slopes were tested by t-tests. Differences in the average Sr:Ca ratios between the low and high phases were examined through a Mann Whitney-U test.
Juvenile three-spined stickleback Gasterosteus aculeatus in their nursery pond had a bimodal length distribution after October in their first year of life. A sea-run migration of all individuals belonging to the lower modal group was observed, with a peak in early November. These data suggest that partial migration based on the early status of individual juveniles occurs in the Pacific Ocean form of three-spined stickleback.
The migratory history of anadromous white-spotted charr Salvelinus leucomaenis collected from Japanese coastal waters, was examined in terms of strontium (Sr) and calcium (Ca) uptake in the otolith, by means of wavelength dispersive X-ray spectrometry using an electron microprobe. Otolith Sr concentration or Sr : Ca ratios of anadromous S. leucomaenis , fluctuated strongly along the life history transect in accordance with the migration (habitat) pattern from sea to fresh water. The anadrmous S. leucomaenis showed phase L (low Sr : Ca ratio) from the core to the point 1000-2500 m m distant, averaging 1.3 ¥ 10 -3 to 2.7 ¥ 10 -3 and thereafter, the ratios increased sharply, being higher than 5.0 ¥ 10 -3 to 10.0 ¥ 10 -3 . These findings indicated that otolith Sr : Ca ratios reflected individual life histories, enabling a sea habitat to be identified from a freshwater habitat in this species.
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