초록

AI-Helper

1985년 $6\~8$월 1986년 $6\~9$월에 동해남부해역 냉수조사의 일환으로서 실시된 수온관측자료 및 개폐형채집망을 사용하여 층별로 채집된 멸치난과 자${\cdot}$치어를 분석하였다. 수온약층은 1985년의 경우 연안측에서는 표층가까이에서, 외해측에서는 $20\~50m$층에서 형성되었으나 1986년에는 외해측까지 계절수온약층의 경사가 완만하게 형성되었다. 또한 멸치날${\cdot}$치어의 분포역은 1985연에는 울산 부근의 외해측에서, 1986년에는 감포부근의 연안측에서 주로 분포하였다. 특히 멸치 난은 일출시에는 대부분 발생초기에 해당되며 $10\~30m$층에 주로 분포하였으나 자정무렵에는 발생후기로 이행되고 $50\~100m$층에서의 분포비율이 높아지므로서 멸치 난은 발생이 진행됨에 따라 침하하는 경향을 보였다. 또한 자${\cdot}$치어의 경우에는 야간에는$0\~30m$층에서 주간에는 30m이심에서의 분포비율이 높았다.

Abstract ▼ AI-Helper

The vertical distribution of eggs and larvae of anchovy. Engraulis japonica were studied based on ichthyoplankton and the temperature distribution in the southwestern part of the Sea of Japan off Korea during the summer of 1985 and 1986. Thermoclines occurred at the surface layer in the coastal area...

The vertical distribution of eggs and larvae of anchovy. Engraulis japonica were studied based on ichthyoplankton and the temperature distribution in the southwestern part of the Sea of Japan off Korea during the summer of 1985 and 1986. Thermoclines occurred at the surface layer in the coastal area and at the sub-surface layer in the offshore area in the early summer of 1985. However, they occurred at the surface layer throughout the summer of 1986. Anchovy eggs and larvae were abundant in the offshore in 1985 and in the coastal area in 1986. It seems that the spawning ground of anchovy in 1985 shifted to the offshore owing to the sloping of thermoclines. According to the distribution layer of anchovy eggs by developmental stage, the eggs in the early developmental stage were abundant at $0\~30m$ layer about 06:00. But the eggs in the late developmental stage were abundant at $30\~100m$ loom layer about 24 : 00. These results suggest that anchovy spawn at the $0\~30m$ layer at night and eggs tend to sink to the $30\~100m$ layer in the course of development.