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      기원전 2000년경 해수면 상승에 대한 고고학적 검토 - 남해안지역을 중심으로 -

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      https://www.riss.kr/link?id=A75200092

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      다국어 초록 (Multilingual Abstract) kakao i 다국어 번역

      On examination of the Shell Mounds of Southern Korea in the Neolithic Age, we've often found out some evidence about the sea level's rising from the past. That is, in the case of the Shell Mounds at the shore, there were not only the union but the layer of abrasion shell between the treasure of the highest and the lowest, also we can discover the layer's disturbance phenomena such as submarine deposits. This is a research that have reviewed some examples on the remains of the sea level's rising focused on the Dongsamdong Site, and then through it I analogize when the sea level's rising happened and how big it progressed. As a result, I can make sure that the sea level's rising was happened by the Bonggyeri type Pottery recorded as the later of the Neolithic Age and Yijung Guyeon Pottery recorded as the last of it chronologically in the southern coast over those two periods. That period came under 4,300 B.P. and 4,000 B.P. according to absolute epoch, the seashore gravel layer was built up to the maximum 8.63m above sea level in the case of the latter. Also it's judged that the maximum sea osmosis gave an effect on the greatest surviving height, 13m above sea level, of the Dongsamdong Site. In view of the results so far achieved, I confirmed that there was the same situation during the similar times after comparing with one of Japan and Balhae's historic sites. It coincided with the cold current from the movement of the Alps glacial period, too. Therefore, it's the greatest sea level's rising followed by global warming since the postglacial period, it's expected not the local happening but the global warming in the southern Korea. At the same time, the Shell Mounds of Nongsori in Kimhae-3,440 B.P.-considered as the last step of pottery with double mouth rim was formed in the sub-zero sea level, reversely as coming to this time, global cooling was coming along and then it made sea level much lower than now. Finally this Environmental change brought about the erosion of Neolithic Age's culture, which was self-supporting economy, as changing into cultivation culture in order to adapt this new environment effectively it moved into the era of patternless earthenware.
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      On examination of the Shell Mounds of Southern Korea in the Neolithic Age, we've often found out some evidence about the sea level's rising from the past. That is, in the case of the Shell Mounds at the shore, there were not only the union but the lay...

      On examination of the Shell Mounds of Southern Korea in the Neolithic Age, we've often found out some evidence about the sea level's rising from the past. That is, in the case of the Shell Mounds at the shore, there were not only the union but the layer of abrasion shell between the treasure of the highest and the lowest, also we can discover the layer's disturbance phenomena such as submarine deposits. This is a research that have reviewed some examples on the remains of the sea level's rising focused on the Dongsamdong Site, and then through it I analogize when the sea level's rising happened and how big it progressed. As a result, I can make sure that the sea level's rising was happened by the Bonggyeri type Pottery recorded as the later of the Neolithic Age and Yijung Guyeon Pottery recorded as the last of it chronologically in the southern coast over those two periods. That period came under 4,300 B.P. and 4,000 B.P. according to absolute epoch, the seashore gravel layer was built up to the maximum 8.63m above sea level in the case of the latter. Also it's judged that the maximum sea osmosis gave an effect on the greatest surviving height, 13m above sea level, of the Dongsamdong Site. In view of the results so far achieved, I confirmed that there was the same situation during the similar times after comparing with one of Japan and Balhae's historic sites. It coincided with the cold current from the movement of the Alps glacial period, too. Therefore, it's the greatest sea level's rising followed by global warming since the postglacial period, it's expected not the local happening but the global warming in the southern Korea. At the same time, the Shell Mounds of Nongsori in Kimhae-3,440 B.P.-considered as the last step of pottery with double mouth rim was formed in the sub-zero sea level, reversely as coming to this time, global cooling was coming along and then it made sea level much lower than now. Finally this Environmental change brought about the erosion of Neolithic Age's culture, which was self-supporting economy, as changing into cultivation culture in order to adapt this new environment effectively it moved into the era of patternless earthenware.

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      목차 (Table of Contents)

      • I. 머리말
      • II. 문제의 제기
      • III 동삼동유적에서 나타나는 해수면 상승의 흔적
      • 1. 동삼동유적의 성격과 조사내용
      • 2. 층위의 구성과 해수면 상승흔적
      • I. 머리말
      • II. 문제의 제기
      • III 동삼동유적에서 나타나는 해수면 상승의 흔적
      • 1. 동삼동유적의 성격과 조사내용
      • 2. 층위의 구성과 해수면 상승흔적
      • 3. 유구와 출토유물의 성격
      • IV. 해수면 상승의 양상과 전개
      • 1. 해수면 상승에 대한 타 사례의 검토
      • 2. 해수면 상승으로 나타나는 유적의 양상
      • V. 해수면 상승의 시기 검토
      • VI. 맺음말
      • 참고문헌
      • Abstract
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      참고문헌 (Reference)

      1 임상택, "한국 중서부 빗살무늬토기문화 연구" 서울대학교 2006

      2 도유호, "지탑리원시유적 발굴보고" 과학원출판사 1961

      3 신숙정, "우리나라 남해안지역의 신석기문화 연구" 학연문화사 1994

      4 한창균, "옥천 대천리 신석기유적"

      5 손보기, "상노대도의 선사시대 살림" 수서원 1982

      6 하인수, "범방패총Ⅰ"

      7 이동주, "동삼동 진입도로지역 유적의 조사내용과 성격; 남부지방 신석기문화의 제문제" 2006

      8 김용기, "농소리패총 발굴조사 개보" 대학박물관협회 4 : 1971

      9 정징원, "김해수가리패총Ⅰ"

      10 이영주, "김해 화목동유적"

      1 임상택, "한국 중서부 빗살무늬토기문화 연구" 서울대학교 2006

      2 도유호, "지탑리원시유적 발굴보고" 과학원출판사 1961

      3 신숙정, "우리나라 남해안지역의 신석기문화 연구" 학연문화사 1994

      4 한창균, "옥천 대천리 신석기유적"

      5 손보기, "상노대도의 선사시대 살림" 수서원 1982

      6 하인수, "범방패총Ⅰ"

      7 이동주, "동삼동 진입도로지역 유적의 조사내용과 성격; 남부지방 신석기문화의 제문제" 2006

      8 김용기, "농소리패총 발굴조사 개보" 대학박물관협회 4 : 1971

      9 정징원, "김해수가리패총Ⅰ"

      10 이영주, "김해 화목동유적"

      11 심봉근, "금관가야권유적 정밀지표조사보고서" 동아대학교 박물관 1993

      12 안춘배, "거창임불리 선사주거지 조사개보(1)" 영남고고학회 6 : 1989

      13 東亜大学校博物館, "釜山港 国際旅客 및 海警埠頭 築造工事에 따른 文化財 水中地表調査 結果 報告書" 2003

      14 慶星大学校博物館, "釜山東三洞遺蹟" 2006

      15 横山将三郎, "釜山府絶影島東三洞貝塚調査報告" 5 (5): 1933

      16 衫原荘介, "神奈川県夏島における縄文文化初頭の貝塚" 明治大学 1957

      17 桑山龍進, "相模夏島貝塚の遺物" 58 (58): 1941

      18 国立晉州博物館, "煙台島Ⅰ" 1993

      19 安田喜憲, "気候と文明の盛衰" 朝倉書店 1992

      20 国立中央博物館, "東三洞貝塚Ⅲ; 제3차 발굴조사 보고서" 2004

      21 国立中央博物館, "東三洞貝塚Ⅱ; 제2차 발굴조사 보고서" 2004

      22 国立中央博物館, "東三洞貝塚Ⅰ; 제1차 발굴조사 보고서" 2005

      23 国立中央博物館, "東三洞貝塚-動物遺体"

      24 釜山博物館, "東三洞貝塚 浄化地域 発掘調査報告書" 2007

      25 慶南文化財研究院, "東三洞 進入道路 拡張区間 試掘調査報告" 2004

      26 東亜大学校博物館, "東三1地区 公有水面 埋立事業地域内 水中文化財 試掘調査 概要" 現場説明会 資料 2005

      27 国立中央博物館, "朝島貝塚"

      28 西岡秀雄, "寒暖の歴史-気候700年週期説" 好学社 1949

      29 東亜大学校博物館, "太宗台 遊園地 進入道路 拡張区間内 文化財 発掘調査 概要" 現場説明会資料 2005

      30 최몽룡, "多元論的 입장에서 본 한국문화의 기원과 시베리아; 한국 청동기․철기시대와 고대사회의 복원" 주류성출판사 2008

      31 及川民次郎, "南朝鮮牧ノ島東三洞貝塚" 考古学 4-5, 1933

      32 下山正一, "北部九州에 있어서 縄文海進과 古環境" 부산여자대학 가야문화연구소 2 : 1991

      33 Zhao Songling, "Transgression and coastal changes in Bohai Sea and its vicinities since the late Pleistocene" Late Quaternarysea- level Changes 1987

      34 L.L. Sample, "Tongsamdong : A Contribution to Korea Neolitic Culture History" 11 (11): 1974

      35 Huntington. E., "The climatic factor as illustrated in arid America" The Carnegie Institution of Washington 1914

      36 Bortenschlager. S, "Choronostraitigraphic subdivisions of the Holocene in the Alps" 16 : 75-79, 1982

      37 Tooley, Michael J., "China sea-level changes" Late Quoternary sea-lavel Changes 1987

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      학술지 이력
      연월일 이력구분 이력상세 등재구분
      2026 평가예정 재인증평가 신청대상 (재인증)
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      2017-01-01 평가 등재학술지 유지 (계속평가) KCI등재
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      2013-01-01 평가 등재학술지 유지 (등재유지) KCI등재
      2010-01-01 평가 등재학술지 유지 (등재유지) KCI등재
      2007-01-01 평가 등재학술지 선정 (등재후보2차) KCI등재
      2006-01-01 평가 등재후보학술지 유지 (계속평가) KCI등재후보
      2004-07-01 평가 등재후보학술지 선정 (신규평가) KCI등재후보
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      기준연도 WOS-KCI 통합IF(2년) KCIF(2년) KCIF(3년)
      2016 0.46 0.46 0.43
      KCIF(4년) KCIF(5년) 중심성지수(3년) 즉시성지수
      0.41 0.37 0.629 0.09
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