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(11) Fig. 4. Diatom zonation and relative abundance of dominent diatom..

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(13) 556. 박영숙․김명진․이종덕․구자진. 다른 구간에 비해서 상대적으로 빠른 약 5 cm/100년 의 퇴적속도를 보이고, 140 cm∼100 cm 구간에서는 퇴 적속도가 급격히 줄어들어 약 0.8 cm/100년, 100 cm ∼50 cm 구간에서는 약 1.1 cm/100년, 50 cm∼30 cm 구간에서는 약 1.2 cm/100년으로 평균 약 1.0 cm/ 100년의 속도로 퇴적층이 형성되었음을 알 수 있다 (Fig. 5). 5.2 고환경 해석. 규조 분대 별로 다음과 같이 해석하였다(Fig. 6). 규조 분대 I: 전체적인 규조의 산출 개체수가 매우 적 고 보존 상태가 아주 불량하며 극히 소량의 담수종이 산출되는 것으로 보아 이 시기의 퇴적층은 물이 흐르 지 않는 약간 건조된 육성 퇴적층으로서 규조 화석의. 보존이 좋지 못한 환경으로 생각된다. 규조 분대 II: Aulacoseira spp.와 cyst가 우세하게 산 출되며 Eunotia spp., Gomphonema spp., Pinnularia spp. 가 같이 다량 산출한다. 이러한 군집은 파랑이 심하고 퇴적물의 유입이 많은 호수 연안 소택지 환경 (freshwater lake littoral swamp environment) 을 지시한다(Caballero et al., 1999, Owen et al., 2004). 이 시기에 퇴적속도가 빠른 것도 이러한 사실을 뒷받 침 해준다. 해수종과 기수종으로서 Actinocyclus sp., Actinoptychus senarius, Paralia sulcata, Cyclotella striata등이 적은 양이지만 같이 산출된다(Sancetta, 1983; Hendey, 1964; Wang and Jiang, 1987). 규조 분대 III: 전체적인 규조의 산출이 대폭 감소하. Fig. 6. The occurrence of the fresh water, brackish water and marine diatoms..

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