Horizontal and vertical movement of yellowtails Seriola quinqueradiata during summer to early winter recorded by archival tags in the northeastern Japan Sea

2020 ◽  
Vol 636 ◽  
pp. 139-156
Author(s):  
S Furukawa ◽  
A Kozuka ◽  
T Tsuji ◽  
H Kubota

Yellowtails Seriola quinqueradiata are an important fishery resource around Japan. Here we investigated the movement ecology and habitat utilization of this migratory fish. Archival tags were implanted in 26 adult yellowtails (61-90 cm in fork length) to examine their seasonal movement patterns and vertical distribution. Yellowtails were captured and released around Noto Peninsula in the Japan Sea on 27 May 2004. Eight individuals were recaptured more than 2 mo later, and we analyzed their daily position and vertical movement with ambient water temperature recorded in 60 or 120 s intervals. Most yellowtail individuals moved from the central coast of Japan to the north (from the west of Tsugaru Strait to the west of Hokkaido) in June. Individuals resided in the northern part of the Japan Sea from summer to mid-fall (late July to late October). Seasonal thermoclines developed during this northward movement and subsequent period of residency, with individuals primarily occupying the surface mixed layer during the daytime and at night; however, individuals made frequent short dives through the thermocline, especially during the daytime. These phenomena may be related to foraging based on the distribution of their prey. In late October, yellowtails started a rapid southward movement, primarily remaining in vertical thermal mixing coastal areas, and not entering the coldwater masses that formed offshore. This southward movement pattern might indicate that yellowtails avoid cold offshore water temperatures.

Ocean Science ◽  
2018 ◽  
Vol 14 (3) ◽  
pp. 355-369 ◽  
Author(s):  
Taketoshi Kodama ◽  
Taku Wagawa ◽  
Naoki Iguchi ◽  
Yoshitake Takada ◽  
Takashi Takahashi ◽  
...  

Abstract. This study evaluates spatial variations in zooplankton community structure and potential controlling factors along the Japanese coast under the influence of the coastal branch of the Tsushima Warm Current (CBTWC). Variations in the density of morphologically identified zooplankton in the surface layer in May were investigated for a 15-year period. The density of zooplankton (individuals per cubic meter) varied between sampling stations, but there was no consistent west–east trend. Instead, there were different zooplankton community structures in the west and east, with that in Toyama Bay particularly distinct: Corycaeus affinis and Calanus sinicus were dominant in the west and Oithona atlantica was dominant in Toyama Bay. Distance-based redundancy analysis (db-RDA) was used to characterize the variation in zooplankton community structure, and four axes (RD1–4) provided significant explanation. RD2–4 only explained < 4.8 % of variation in the zooplankton community and did not show significant spatial difference; however, RD1, which explained 89.9 % of variation, did vary spatially. Positive and negative species scores on RD1 represent warm- and cold-water species, respectively, and their variation was mainly explained by water column mean temperature, and it is considered to vary spatially with the CBTWC. The CBTWC intrusion to the cold Toyama Bay is weak and occasional due to the submarine canyon structure of the bay. Therefore, the varying bathymetric characteristics along the Japanese coast of the Japan Sea generate the spatial variation in zooplankton community structure, and dominance of warm-water species can be considered an indicator of the CBTWC.


2017 ◽  
Author(s):  
Taketoshi Kodama ◽  
Taku Wagawa ◽  
Naoki Iguchi ◽  
Yoshitake Takada ◽  
Takashi Takahashi ◽  
...  

Abstract. This study evaluates spatial variations in zooplankton community structure and potential controlling factors along the Japanese coast under the influence of the coastal branch of the Tsushima Warm Current (CBTWC). Variations in the density of morphologically-identified zooplankton in the surface layer in May were investigated for a 15-year period. The density of zooplankton (individuals per cubic meter) varied between sampling stations, but there was no consistent west–east trend. Instead, there were different zooplankton community structures in the west and east, with that in Toyama Bay particularly distinct: Corycaeus affinis and Calanus sinicus were dominant in the west and Oithona atlantica was dominant in Toyama Bay. Distance-based redundancy analysis (db-RDA) was used to characterize the variation in zooplankton community structure, and four axes (RD1–4) provided significant explanation. RD2–4 only explained


Author(s):  
Tomoharu Senjyu

AbstractThe flow field in the Toyama Deep-Sea Channel (TDSC) in the Japan Sea was investigated based on mooring observations. An asymmetric current system accompanying offshore and onshore currents over the east- and west-side slopes in the channel, respectively, is suggested. A bottom intensified flow characteristic was observed at the offshore stations in the Yamato Basin. The asymmetric current system in the channel is also suggested by the asymmetric distribution of water characteristics across the TDSC in Toyama Bay; a cold dense water mass with higher dissolved oxygen (DO) and higher transmittance (Tr) was found over the west-side slope of the channel, whereas a water mass with lower DO and lower Tr was distributed over the east-side slope, suggesting a turbidity current from the head of Toyama Bay. The currents facing the shallower depth on their right-hand-side, along with the density distribution in the TDSC, suggest a density current system under the influence of the earth’s rotation. The dissolved oxygen concentration in the TDSC was significantly lower than that in the offshore region of the same temperature range. This suggests that the water mass over the west-side slope in the TDSC is a modified offshore water mass which experienced significant mixing with the low DO water mass over the east-side slope in the TDSC, probably due to strong shear between the offshore and onshore currents in the narrow channel.


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