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ACOMS+ 및 학술지 리포지터리 설명회

  • 한국과학기술정보연구원(KISTI) 서울분원 대회의실(별관 3층)
  • 2024년 07월 03일(수) 13:30
 

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저서성 유공충 군집 및 퇴적물 지화학 조성에서 나타나는 전복양식 활동 영향 및 퇴적환경과의 상관성

Relativity of sedimentary environment and effect on benthic foraminiferal assemblage and geochemistry of sediment in abalone farming

Abstract

Geochemical and benthic foraminiferal analyses of sediments (core and surface) were conducted in an abalone farm located at Pyeongil-do, Wando-gun, to understand the degree to which the abalone farming affect the benthic environment and ecology, and relativity to sedimentary environment. The C/S ratio of surface sediment was 8.24 in average (6.77-13.01), and abundance and species diversity of benthic foraminifera were 10,470 individual in 20 ml of sediments and average 3.4, respectively, in the surface sediment, although OM deposited by farming was about 7-19 cm in thickness. The effect of abalone farming on benthic ecology and geochemistry was not distinct. In the northwestern sea of Pyeongil-do and Cheok-do (Zone A), the sedimentation rate was very low (average, 0.23 cm/year), the C/N ratio was high (St. No. 9: 18.50) and Elphidium advenum known to inhabit in the entrance sea area of bay was dominantly distributed. In the adjacent sea area of Pyeongil-do and Cheok-do (Zone A), however, the sedimentation rate was very high (average, 1.73 cm/year), Epistominella naraensis known to inhabit in the open sea area was dominantly distributed. It is consequently thought that abalone farms of northwestern sea of Pyeongil-do and Cheok-do are influenced by the fast flow of Deugryang Bay, and abalone farms of adjacent sea area of them are influenced by the open sea. As mentioned above, these coexistence of various sedimentary environment in farm is thought to be caused by topographical characteristics with irregular coastline of Rias type.

keywords
Benthic foraminifera, abalone farming, sedimentary environment

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