최소 단어 이상 선택하여야 합니다.
최대 10 단어까지만 선택 가능합니다.
다음과 같은 기능을 한번의 로그인으로 사용 할 수 있습니다.
NTIS 바로가기韓國鑛物學會誌 = Journal of the Mineralogical Society of Korea, v.27 no.3, 2014년, pp.159 - 168
전창표 (경북대학교 지질학과) , 김창환 (한국해양과학기술원 동해연구소 독도전문연구센터) , 김영규 (경북대학교 지질학과) , 이성주 (경북대학교 지질학과)
Holocene plaeoenvironmental changes were interpreted by grain size and mineral analyses of a piston core (HB 13-2), obtained along the western slope of the Hupo Basin, Korea. The core sediments are characterized by two discrete, sedimentary facies: upper unit (0-0.4 mbsf) dominated by bioturbation s...
* AI 자동 식별 결과로 적합하지 않은 문장이 있을 수 있으니, 이용에 유의하시기 바랍니다.
핵심어 | 질문 | 논문에서 추출한 답변 |
---|---|---|
동해 중부 연안이 환경변화에 대한 연구가 매우 제한적인 이유는? | 동해 중부 연안은 서해와 남해 연안에 비해 경사가 심하고 쇄설성 퇴적물의 낮은 공급으로 인해 홀로세 해침 이후의 환경변화에 대한 연구가 매우 제한적이다. 반면 후포분지는 수심 200 m 이하의 넓고 평탄한 지형을 갖고 있고 동쪽으로 남북 방향의 후포뱅크가 가로막아 다른 지역에 비해 퇴적률이 높다(Kim et al. | |
후포분지에 유입되는 퇴적물의 기원지 및 고해양환경을 규명하기 위해 무엇을 채취하였는가? | 후포분지에 유입되는 퇴적물의 기원지 및 고해양환경을 규명하기 위해 한국해양과학기술원의 이어도호를 이용하여 HB 13-2 피스톤 코어를 채취하였다(Fig. 1). | |
동해 중부 연안에서 후포분지가 환경변화를 연구할 수 있는 이상적인 지역인 이유는? | 동해 중부 연안은 서해와 남해 연안에 비해 경사가 심하고 쇄설성 퇴적물의 낮은 공급으로 인해 홀로세 해침 이후의 환경변화에 대한 연구가 매우 제한적이다. 반면 후포분지는 수심 200 m 이하의 넓고 평탄한 지형을 갖고 있고 동쪽으로 남북 방향의 후포뱅크가 가로막아 다른 지역에 비해 퇴적률이 높다(Kim et al., 2010). |
Adams, W.J., Kimerle, R.A., and Barnett Jr., J.W. (1992) Sediment quality and aquatic life assessment. Environmental Science and Technology, 26, 1863-1876.
Alizai, A., Hillier, S., Clift, P.D., Giosan, L., Hurst, A., VanLaningham, S., and Macklin, M. (2012) Clay mineral variations in Holocene terrestrial sediments from the Indus Basin. Quaternary Research, 77, 368-381.
Biscaye, P.E. (1965) Mineralogy and sedimentation of recent deep-sea clay on the Atlantic Ocean and adjacent seas and oceans. Geological Society of America Bulletin, 76, 803-832.
Blott, S.J., and Pye, K. (2001) GRADISTAT: a grain size distribution and statistics package for the analysis of unconsolidated sediments. Earth Surface Processes and Landforms, 26, 1237-1248.
Boulay, S., Colin, C., Trentesaux, A., Pluquet, F., Bertaux, J., Blamart, D., Buehring, C., and Wang, P. (2003) Mineralogy and sedimentology of Pleistocene sediment in the South China Sea (ODP Site 1144). In: Prell, W.L., Wang, P., Blum, P., Rea, D.K. and Clemens, S.C. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, 184, 1-21.
Cahoon, L.B., Nearhoof, J.E., and Tilton, C.L. (1999) Sediment grain size effect on benthic microalgal biomass in shallow aquatic ecosystems. Estuaries, 22, 735-741.
Chapman, P.M. (1989) Current approaches to developing sediment quality criteria. Environmental Toxicology and Chemistry, 8, 589-599.
Choi, J.-Y., Lim, D.-I., Park, C.-H., Kim, S.-Y., Kang, S., and Jung, H.-S. (2010) Characteristics of clay mineral compositions in river sediments around the Yellow Sea and its application to the provenance of the continental shelf mud deposits. Journal of the Geological Society of Korea, 46, 497-509 (in Korean with English abstract).
Domitsu, H., and Oda, M. (2008) Holocene influx of the Tsushima Current into the Japan Sea signalled by spatial and temporal changes in Neogloboquadrina incompata distribution. The Holocene, 18, 345-352.
Dou, Y., Yang, S., Li, Z., Clift, P.D., Yu, Hua, Berne, S., and Shi, X. (2010) Clay mineral evolution in the central Okinawa Trough since 28 ka: implications for sediment provenance and paleoenvironmental change. Palaeogeography, Plaeoclimatology, Palaeoecology, 288, 108-117.
Ehrmann, W. (1998) Implications of late Eocene to early Miocene clay mineral assemblages in McMurdo Sound (Ross Sea, Antarctica) on paleoclimate and ice dynamics. Palaeogeography, Palaeoclimatology, Palaeoecolgy, 139, 213-231.
Ehrmann, W., Setti, M., and Marinoni, L. (2005) Clay minerals in Cenozoic sediments off Cape Roberts (McMurdo Sound, Antarctica) reveal palaeoclimatic history. Palaeogeography, Palaeoclimatology, Palaeoecolgy, 229, 187-211.
Gao, S., Collins, M.B., Lanckneus, J., DeMoor, G., and Van Lancker, V. (1994) Grain size trends associated with net sediment transport patterns: An example from the Belgian continental shelf. Marine Geology, 121, 171-185.
Gimenez, L., Venturini, N., Kandratavicius, N., Hutton, M., Landfranconi, A., Rodriguez, M., Brugnoli, E., and Muniz, P. (2014) Macrofaunal patterns and animal-sediment relationships in Uriguayan estuaries and coastal lagoons (Atlantic coast of South America). Journal of Sea Research, 87, 46-55.
Horiuchi, K., Minoura, K., Hoshino, K., Oda, T., Nakamura, T., and Kawai, T. (2000) Palaeoenvironmental history of Lake Baikal during the last 23000 years. Palaeogeography, Palaeoclimatology, Palaeoecolgy, 157, 95-108.
KIGAM (2009) Coastal geohazard factor analysis (Uljin area). Korea Institute of Geoscience and Mineral Resources, KiGAM, Daejeon, 279p.
Kim, J.-H., Park, M.-H., Kong, G.-S., Han, H.-C., Cheong, T.-J., Choi, J., Kim, J.H., Kang, M.-H., Lee, C.-W., and Oh, J.-H. (2010) Geochemical results and implications of the organic matter in the Holocene sediments from the Hupo Basin. Economic and Environmental Geology, 43, 1-12 (in Korean with English abstract).
Kim, J.-M., Kennett, J.P., Park, B.-K., Kim, D.C., Kim, G.Y., and Roark, E.B. (2000) Paleoceanographic change during the last deglaciation, East Sea of Korea. Paleoceanography, 15, 254-266.
Koizumi, I. (2008) Diatom-derived SSTs (Td' ratio) indicate warm seas off Japan during the middle Holocene (8.2-3.3 kyr BP). Marine Micropaleontology, 69, 263-281.
Kylander, M.E., Ample, L., Wohlfarth B., and Veres, D. (2011) High-resolution X-ray fluorescence core scanning analysis of Les Echets (France) sedimentary sequence: new insights from chemical proxies. Journal of Quaternary Science, 26, 109-117.
Lamy, F., Klump, J., Hebbeln, D., and Wefer, G. (2000) Late Quaternary rapid climate change in northern Chile. Terra Nova, 12, 8-13.
Lee, K.E., 2007, Surface water changes recorded in Late Quaternary marine sediments of the Ulleung Basin, East Sea (Japan Sea). Palaeogeography, Palaeoclimatology, Palaeoecology, 247, 18-31.
Lee, Y.D., You, H.S., and Kim, S.Y. (1996) Silicoflagellate biostaratigraphy and sediment facies in Ulleung Basin, the East Sea. Journal of the Geological Society of Korea, 32, 73-90 (in Korean with English abstract).
Lim, D.I., Kang, S., Yoo, H.S., Choi, J.Y., Kim, H,N., and Shin, I.H. (2006) Late Quaternary sediments on the outer shelf of the Korea Strait and their paleoceanographic implications. Geo-Marine Letters, 26, 287-296.
Liu, J.P., Milliman, J.D., Gao, S., and Cheng, P. (2004) Holocene development of the Yellow River's subaqueous delta, North Yellow Sea. Marine Geology, 209, 45-67.
McCave, I.N., Crowhurst, S.J., Kuhn, G., Hillenbrand, C.-D., and Meredith, M.P. (2014) Minimal change in Antarctic Circumpolar Current flow speed between the last glacial and Holocene. Nature Geoscience, 7, 113-116.
McCave, I.N., Manighetti, B., and Robinson, S.G. (1995) Sortable silt and fine sediment size/composition slicing : Parameters for palaeocurrent speed and palaeoceanography. Paleoceanography, 10, 593-610.
McLachlan, A. (1996) Physical factors in benthic ecology: effects of changing sand particle size on beach fauna. Marine Ecology Progress Series, 131, 205-217.
Moon, D.K., Yi, H.-I., Shin, K.-H., Do, J.Y., and Cho, H.G. (2009) Mineral distribution of the southeastern Yellow Sea and South Sea of Korea using quantitative XRD analysis. Journal of the Mineralogical Society of Korea, 22, 49-61 (in Korean with English abstract).
Nahm, W.-H., Kim, J.-Y., Lim, J., and Yu, K.-M. (2011) Responses of the upriver valley sediment to Holocene environmental changes in the Paju area of Korea. Geomorphology, 133, 80-89.
Nishida, N., and Ikehara, K. (2013) Holocene evolution of depositional processes off southwest Japan: Response to the Tsushima Warm Current and sea-level rise. Sedimentary Geology, 290, 138-148.
Park, J., Yu, K.B., Lim, H.S., and Shin, Y.H. (2012) Holocene environmental changes on the east coast of Korea. Journal of Paleolimnology, 48, 535-544.
Petschick, R. (2000) MacDiff 4.2.5 Manual. Available from World Wide Web: http://www.geologie.uni-frankfurt.de/Staff/Homepages/Petschick/RainerE.html.
Poizot, E., Mear, Y., and Biscara, L. (2008) Sediment Trend Analysis through the variation of granulo metric parameters: A review of theories and applications. Earth-Science Reviews, 86, 15-41.
Ryu, E., Yi, S., and Lee, S.-J. (2005) Late Pleistocene-Holocene paleoenvironmental changes inferred from the diatom record of the Ulleung Basin, East Sea (Sea of Japan). Marine Micropaleontolgoy, 55, 157-182.
Thornalley, D.J.R., Barker, S., Becker, J., Hall, I.R., and Knorr, G. (2013) Abrupt changes in deep Atlantic circulation during the transition to full glacial conditions. Paleoceanography, 28, 253-262.
Wei, G., Liu, Y., Li, X., Shao, L., and Liang, X. (2003) Climatic impact on Al, K, Sc and Ti in marine sediments: Evidence from ODP Site 1144, South China Sea. Geochemical Journal, 37, 593-602.
Xu, Z., Li, T., Chang, F., Wan, S., Choi, J., and Lim D. (2014) Clay-sized sediment provenance in the northern Okinawa Trough since 22 kyr BP and its paleoenviromental implication. Palaeogeography, Plaeoclimatology, Palaeoecology, 399, 236-246.
Yao, Z., Liu, Y., Shi, X., and Suk, B.-C. (2012) Paleoenvironmental changes in the East/Japan Sea during the last 48 ka: indications from high-resolution X-ray fluorescence core scanning. Journal of Quaternary Science, 27, 932-940.
Yi, S. (2011) Holocene vegetation responses to East Asian Monsoonal changes in South Korea. In: Blanco, J. and Kheradmand, H. (eds.), Climate Change, 157-178.
*원문 PDF 파일 및 링크정보가 존재하지 않을 경우 KISTI DDS 시스템에서 제공하는 원문복사서비스를 사용할 수 있습니다.
출판사/학술단체 등이 한시적으로 특별한 프로모션 또는 일정기간 경과 후 접근을 허용하여, 출판사/학술단체 등의 사이트에서 이용 가능한 논문
※ AI-Helper는 부적절한 답변을 할 수 있습니다.