Geographic variations in dorsal and anal ray counts of juvenile Japanese flounder, Paralichthys olivaceus, in the Japan Sea

Citation
I. Kinoshita et al., Geographic variations in dorsal and anal ray counts of juvenile Japanese flounder, Paralichthys olivaceus, in the Japan Sea, ENV BIOL F, 57(3), 2000, pp. 305-313
Citations number
30
Categorie Soggetti
Aquatic Sciences
Journal title
ENVIRONMENTAL BIOLOGY OF FISHES
ISSN journal
03781909 → ACNP
Volume
57
Issue
3
Year of publication
2000
Pages
305 - 313
Database
ISI
SICI code
0378-1909(200003)57:3<305:GVIDAA>2.0.ZU;2-D
Abstract
Meristic counts of early and late wild settled juveniles of Japanese flound er, Paralichthys olivaceus (Paralichthyidae), in Wakasa Bay, Japan, were co mpared, with specimens collected from 26 sites spread along ca. 1700 km of coastline facing the Japan Sea. Mean dorsal and anal ray counts of the earl y settled group at Kyoto were significantly larger than those of the late s ettled group. A discontinuous geographic boundary in mean dorsal and anal r ay counts was found around Wakasa Bay and the Noto Peninsula with both mean s significantly larger in the southern group than in the northern group. Me an ray counts of the early and late settlers at Kyoto were similar to those of the southern and northern groups, respectively. The effect of water tem perature on meristic characters was tested on two groups of laboratory-rear ed juveniles. Mean dorsal and anal ray counts were larger in juveniles rear ed at higher water temperatures. The early and late settler groups were est imated to hatch in late February and late April, respectively, representing negative response of meristic characters to water temperatures if these tw o groups hatched out in Wakasa Bay. Differences in the dorsal and anal ray counts between the early and late settled groups at Kyoto can, therefore be attributed to genotypic, not phenotypic variation. This suggests the possi bility of transport of larvae of the early group from areas further south t o Wakasa Bay by the warm Tsushima Current, a branch of the Kuroshio, which flows northeastward along the coast of the Japan Sea, particularly when the temperature gradation between the south and north areas during these seaso ns is considered.