• 제목/요약/키워드: Soro-ri

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청원 소로리 토탄층에서 고대 볍씨와 함께 출토된 뿌리잎벌레류의 화석 (Insect Fossils (Coleoptera: Chrysomelidae: Donaciinae) Found Together with Ancient Rice in Soro-ri Peat Layer)

  • 남상찬;이성균;안승락;이융조;조수원
    • 한국응용곤충학회지
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    • 제47권4호
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    • pp.333-336
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    • 2008
  • 청주 근교 청원군 소로리의 토탄층에서 고대 볍씨에 관한 조사를 실시하던 중 다른 여러가지 유기물들과 함께 곤충의 파편으로 보이는 조각들이 함께 출토되었다. 비록 완전한 개체의 형태는 아니지만 딱정벌레의 외골격은 두껍고 단단해 지금까지 보존되어온 것으로 보인다. 그 중 일부는 종 수준까지의 동정도 가능하였는데, 앞날개의 형태 등을 기준으로 현세종과 비교 분석한 결과, Plateumaris sericea 및 Donacia flemola와 동일 또는 매우 근연한 종으로 동정되었다. 이들은 딱정벌레목(Coleoptera), 잎벌레과(Chrysomelidae), 뿌리잎벌레아과(Donaciinae)에 속하는 종류로, 습지식물인 사초과나 벼과 식물을 주로 가해하며, 유충기에는 물 속 뿌리부분을 가해하면서 수서생활을 한다. 그들의 상세한 생태적 정보를 바탕으로 할 때, 이러한 증거는 당시의 소로리 환경이 습지였음을 분명하게 증거하고 있음을 알 수 있다. 따라서, 고대 볍씨의 연구에 있어서 이들 곤충화석의 증거는 소로리의 당시 환경이 벼등 습지식물이 자라기 좋은 환경이었음을 말해주고 있다.

Post LGM Fluvial Environment and Palynological Changes of South Korea

  • Kim, Ju-Yong;Yang, Dong-Yoon;Bong, Pil-Yoon;Nahm, Wook-Hyun;Lee, Heon-Jong;Lee, Yung-Jo;Hong, Sei-Sun;Lee, Jin-Young;Kim, Jin-Wkan;Oh, Keun-Chang
    • 한국제4기학회지
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    • 제17권2호
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    • pp.17-23
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    • 2003
  • In Korea terrestrial fluvial sequences can be used as pedological and sedimentological markers indicating a millenium-scale environmental and climatic changes imprinted in fluvial sub-environments, which in turn are represented by the cyclicity of fluvial sands, backswamp organic muds, and flooding muds intercalations of frostcracked or dessicated brown paleosols. Post LGM and Holocene fluvial and alluvial sedimentary sequences of Korea are formed in such landscapes of coastal, floodplain, backswamp and hillslope areas. Among them, the most outstanding depositional sequences are fluvial gravels, sands and organic mud deposits in coastal, fluvial, or alluvial wetlands. The aim of this study is to explain the sedimentary sequences and palynofloral zones since the last 15,000years, on the basis of organic muds layers intercalated in fluvial sand deposits. Jangheung-ri site of Nam river, Soro-ri site of Miho river, Youngsan rivermouth site in Muan, Oksan-ri site of Hampyeong and Sanggap-ri site of Gochang are illustrated to interpret their sedimentary facies, radiocarbon datings, and palynofloral zonation. Up to the Middle to Late Last Glacial(up to 30-35Ka), old river-bed, flooding, and backswamp sequences contain such arboreal pollens as Pinus, Abies, and Picea, and rich in non-arboreal pollens like Cyperaceae, Gramineae, Ranunculaceae, and Compositae. During the LGM and post-LGM periods until Younger Dryas, vegetation has changes from the sub-alpine conifer forest(up to about 17-11Ka), through the conifer and broad-leaved deciduous forest, or mixed forest (formed during 16,680-13,010yrB.P), to the deciduous and broad-leaved forest (older than 9,500yrB.P). In the Earliest Holocene flooding deposits, fragments of plant roots are abundant and subjected to intensive pedogenic processes. During Holocene, three arboreal pollen zones are identified in the ascending order of strata; Pinus-Colyus zone(mixed conifer and deciduous broad-leaved forest, about up to 10Ka), Alnus-Quercus forest (the cool temperate deciduous broad-leaved forest, about 10Ka-2Ka), and Pinus forest (the conifer forest, about after 2Ka), as examplified in Soro-ri site of Cheonwon county. The palynological zonations of Soro-ri, Oksan-ri, Sanggap-ri, Youngsan estuary, and Gimhae fluvial plain have been recognized as a provisional correlation tool, and zonations based on fluvial backswamp and flooding deposits shows a similar result with those of previous researchers.

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관개기 대구획 광역논에서의 영양물질 거동 (Nutrient Behavior at Paddy Field Area with Large-Scaled Plots during Irrigation Periods)

  • 오승영;김진수;정구영
    • 한국수자원학회:학술대회논문집
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    • 한국수자원학회 2005년도 학술발표회 논문집
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    • pp.1254-1258
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    • 2005
  • Net outflow flux and unit load of pollutants were investigated at a paddy fields area(Soro-ri) with large-scaled plots on loam soil during irrigation seasons of $2001\~2003$. Water samples were collected, and inflow and outflow were .measured at $5\~10$ day intervals during non-storm periods and at $2\~6$ hours intervals during storm events. The average concentration of TP in percolated water was much smaller than that in irrigation and surface outflow water likely due to phosphorus absorption capacity of paddy soils. Net outflow flux in study area was significantly correlated with rainfall and surface outflow discharge. Nutrient flux from Paddy fields can be abated by reduction in outflow surface discharge.

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광역논에서의 영양 물질(N, P)의 거동 특성 (Characteristics of Behavior of the Nutrients at Paddy Field Area with Large-Scaled Plots)

  • 오승영;김진수;정구영
    • 한국농공학회:학술대회논문집
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    • 한국농공학회 2003년도 학술발표논문집
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    • pp.567-570
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    • 2003
  • Nutrients behavior were investigated at a paddy fields area(Soro-ri) with large-scaled plots on loam soil during irrigation seasons of $2001{\sim}2002$. The average concentration of TN, TDN and TDP in drainage water was higher than that in irrigation water. On the other hand, TP in irrigation water was higher than that in drainage water. The ratio of a TDN to TN accounts for over 90% and the ratio of TDP to TP accounts for $50{\sim}70%$. Especially, the ratio of TDP to TP in drainage water was bigger than that in irrigation water, suggesting that much of particulate component was reduced due to sedimentation and adsorption in paddy fields plots.

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광역논에서의 용존성과 입자성 영양물질의 거동 특성 (Behavior of the Dissolved and Particulate Nutrient at Paddy Field Area)

  • 오승영;김진수;정구영
    • 한국수자원학회:학술대회논문집
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    • 한국수자원학회 2004년도 학술발표회
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    • pp.543-546
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    • 2004
  • Nutrients behavior were investigated at a paddy fields area(Soro-ri) with large-scaled plots on loam soil during irrigation seasons of $2001\~2003$. The average concentration of TN, TDN and TDP in drainage water was higher than that in irrigation water. On the other hand, the average concentration TP in irrigation water was higher than in drainage water. The ratio of TDN to TN accounted (or over $90\%$ and the ratio of TDP to TP accounted for $50\~70\%$. Especially the ratio of TDP to TP in drainage water was higher than that in irrigation water, suggesting that much of particulate component was reduced due to sedimentation and adsorption in paddy fields plots. Overall, particulate phosphorus usually account for 44 to $77\%$ of tile total phosphorus during storm events.

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관개기 대구획 광역논에서의 오염부하 원단위 (Unit Loads of Pollutants in a Paddy Fields Area with Large-Scaled Plots during Irrigation Seasons)

  • 오승영;김진수;김규성;김선종;윤춘경
    • 한국농공학회지
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    • 제44권2호
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    • pp.136-147
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    • 2002
  • Characteristics of unit loads of pollutants were investigated at a paddy fields area(Soro-ri) with large-scaled plots on loam soil during irrigation seasons of 1999 ∼2000. The average irrigation requirement of experimental paddy area are estimated at over 3,000 mm. The unit loads of pollutants in paddy fields area are determined by subtracting irrigation water load from outflow load (percolated and surface outflow loads). Surface outflow load in rainy days was calculated using the relationships of discharge and load, which are grouped into fertilizing and non-fertilizing periods. The ratios of the surface outflow load in rainy days to the total surface outflow load are 16.4% for T-N, 26.8% for T-P, and 23.3% far CODc,. The unit loads of pollutants show month-to-month and year-to-year variations, and monthly unit load of pollutants can show negative values, indicating that the paddy area acts as the pollutants sink. The average unit loads of the pollutants during irrigation seasons were estimated at 18.2 kg/ha fur T-N, 0.31 kg/ha for T-P, and 43.3 kg/ha for CODc,, which are smaller than the reported values for Kosei area in Japan.

청원 옥산 소로리 유적지 일대 유기질 니층의 화분분석에 의한 식생변천사에 관한 연구 (A Study on Vegetation History of Organic Muds of Sorori Archaeological Site, Oksan-myeon, Cheongwon-gun, Korea)

  • 김주용;양동윤;봉필윤;이융조;박지훈
    • 한국제4기학회지
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    • 제15권2호
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    • pp.75-81
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    • 2001
  • 한반도 내륙지역의 제4기 후기의 식생변천 과정을 밝히기 위하여, 충북 청원군 옥산면 소로리 유적지($36^{\circ}41'3"N$, $127^{\circ}24'49"E$)의 퇴적물을 대상으로 화분분석을 실시하였다. 그 결과, 이 지역 일대는 \circled1OS-1의 아고산성 침엽수림(만빙기;약 15,000yr.B.P.~10,000yr.B.P.)$\longrightarrow$\circled2OS-2의 침엽ㆍ낙엽 활엽수혼합림(후빙기 초기;약 10,000yr. B.P.경)$\longrightarrow$\circled3OS-3의 냉온대성 낙엽활엽수림(후정기 중기;약 10.000yr.B.P.~2,000yr.B.P.)$\longrightarrow$\circled4OS-4의 침엽수림(후빙기 후기;약 2,000yr.B.P.) 이후)로 변천하였음을 알 수 있었다.을 알 수 있었다.

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