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      해양환경에 따른 부유성 유공충 용해 정도 지표의 적용 가능성 평가 = Evaluation of dissolution indices for planktic foraminifera in various environmental settings

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      https://www.riss.kr/link?id=A106586349

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      다국어 초록 (Multilingual Abstract)

      Fossil planktic foraminifera is a useful indicator of the paleoenvironment of the surface ocean. Because of its susceptibility to dissolution, various indices for preservation state of planktic foraminifera have been used to determine better the degre...

      Fossil planktic foraminifera is a useful indicator of the paleoenvironment of the surface ocean.
      Because of its susceptibility to dissolution, various indices for preservation state of planktic foraminifera have been used to determine better the degree of bias introduced by the species-dependent resistance to dissolution.
      This study aims to evaluate six dissolution indices of foraminifera from four Pacific sites, each representing different surface and deep ocean condition. Compared to the fragmentation rate (FLS), demanding and time-consuming but one of the most reliable dissolution indices regardless of the ambient environment, each index has different sensitivity on preservation state owing to the environmental factors. Carbonate fraction (CaCO3) and coarse sized fraction (CSF) are fairly well correlated with FLS in the foraminifera-dominated tropical ocean where the influx of other sedimentary components is insignificant. The assemblage dissolution index (FDX) and percentage of resistant species (Res) based on the relative enrichment of dissolution-resistant species are best applicable at the central equatorial Pacific site without any significant changes in the primary faunal assemblage. The benthic/planktic ratio (B) varies with FLS similarly at a productive Northwestern Pacific site, but should be carefully applied in many cases owing to the strong dependence of benthic foraminifera on food availability. The results of this study suggest the importance of rigorous application criteria of the foraminifera dissolution index in various depositional environments.

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      국문 초록 (Abstract)

      부유성 유공충의 미화석은 과거 표층해양환경의 지시자로서 유용하게 이용된다. 이들은 퇴적된 후 종에 따라 다른 용해 저항성을 가지므로, 이에 따른 환경 기록의 왜곡 정도를 파악하기 위...

      부유성 유공충의 미화석은 과거 표층해양환경의 지시자로서 유용하게 이용된다. 이들은 퇴적된 후 종에 따라 다른 용해 저항성을 가지므로, 이에 따른 환경 기록의 왜곡 정도를 파악하기 위해 다양한 용해도를 평가할수 있는 지표가 이용되어 왔다. 본 연구에서는 서로 다른 해양환경에서 획득된 네 점의 심해퇴적물 주상시료에서 분석한 여섯 가지의 용해도 평가 지표를 비교하여 평가하였다. 높은 정확도를 가지지만 많은 시간과 노력을요하는 파편도(FLS)와 비교할 때, 각각의 지표는 환경 요소에 따라 다른 적용가능성을 나타냈다. 탄산염 함량(CaCO3)과 조립도(CSF)는 유공충이 우점하며 이외의 퇴적물 유입이 미미한 열대 해양에서 FLS와 좋은 상관관계를 보인다. 종 용해지표(FDX)와 저항종 비율(Res)은 용해 저항성이 강한 종의 상대적 비율에 기반한 지표로일차적인 종 군집구조의 변화가 크지 않은 중앙 적도태평양 해역에서 적용하기에 적합하다. 저서성/부유성 비율(B)은 생산성이 높은 북서태평양 지역에서 FLS와 유사한 변화 양상을 나타내나, 먹이 의존도가 높은 저서성유공충의 특성을 고려해야 한다. 본 연구의 결과를 통해 다양한 원양 퇴적환경에 대한 유공충 용해 지표의 적용기준을 제시하였다.

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      참고문헌 (Reference)

      1 Reimer, P.J., "and Marine13 radiocarbon age calibration curves 0-50,000 years cal BP" 55 : 1869-1887,

      2 Locarnini, R. A., "World Ocean Atlas 2018, Volume 1: Temperature" 52-, 2018

      3 Pfuhl, H. A., "Two proximal, high-resolution records of foraminiferal fragmentation and their implications for changes in dissolution" 51 : 809-832, 2004

      4 Chiu, T. -C., "Toward better paleocarbonate ion reconstructions : New insights regarding the CaCO3 size index" 23 : PA2216-, 2008

      5 Hays, J. D., "The significance of calcium carbonate oscillations in Eastern Equatorial Atlantic deep-sea sediments for the end of the Holocene warm interval" 2 : 355-362, 1972

      6 McCarthy, F. M. G., "The micropaleontological character of anomalous calcareous sediments of late Pliocene through early Pleistocene age below the CCD in the northwestern North Pacific Ocean" 215 : 1-15, 2004

      7 Berger, W. H., "Sedimentation of planktic foraminifera" 11 : 325-358, 1971

      8 Honjo, S, "Seasonality and interaction of biogenic and lithogenic particulate flux at the Panama Basin" 218 : 883-884, 1982

      9 Arrhenius, G., "Reports of the Swedish Deep Sea Expedition 1947-48" 227-, 1952

      10 Malmgren, B. A., "Ranking of dissolution susceptibility of planktic foraminifera at high latitudes of the South Atlantic Ocean" 8 : 183-191, 1983

      1 Reimer, P.J., "and Marine13 radiocarbon age calibration curves 0-50,000 years cal BP" 55 : 1869-1887,

      2 Locarnini, R. A., "World Ocean Atlas 2018, Volume 1: Temperature" 52-, 2018

      3 Pfuhl, H. A., "Two proximal, high-resolution records of foraminiferal fragmentation and their implications for changes in dissolution" 51 : 809-832, 2004

      4 Chiu, T. -C., "Toward better paleocarbonate ion reconstructions : New insights regarding the CaCO3 size index" 23 : PA2216-, 2008

      5 Hays, J. D., "The significance of calcium carbonate oscillations in Eastern Equatorial Atlantic deep-sea sediments for the end of the Holocene warm interval" 2 : 355-362, 1972

      6 McCarthy, F. M. G., "The micropaleontological character of anomalous calcareous sediments of late Pliocene through early Pleistocene age below the CCD in the northwestern North Pacific Ocean" 215 : 1-15, 2004

      7 Berger, W. H., "Sedimentation of planktic foraminifera" 11 : 325-358, 1971

      8 Honjo, S, "Seasonality and interaction of biogenic and lithogenic particulate flux at the Panama Basin" 218 : 883-884, 1982

      9 Arrhenius, G., "Reports of the Swedish Deep Sea Expedition 1947-48" 227-, 1952

      10 Malmgren, B. A., "Ranking of dissolution susceptibility of planktic foraminifera at high latitudes of the South Atlantic Ocean" 8 : 183-191, 1983

      11 Conan, S. M. H., "Quantifying carbonate dissolution and calibration of foraminiferal dissolution indices in the Somali Basin" 182 : 325-349, 2002

      12 Mekik, A. F., "Progress toward a multi-basin calibration for quantifying deep sea calcite preservation in the tropical/subtropical world ocean" 299 : 104-117, 2010

      13 Kroon, D., "Planktonic and benthic foraminiferal abundances and their ratios (P/B) as expressions of mid-late Quaternary changes in water mass distribution and flow intensity" 133 : 181-188, 1993

      14 Chaisson, W., "Planktonic Foraminiferal Assemblages and Paleoceanographic Change in the Trans-tropical Pacific Ocean: A Comparison of West (Leg 130) an East (Leg 138), Latest Miocene to Pleistocene" 138 : 555-597, 1995

      15 Berger, W. H., "Planktic foraminifera:Differential settling, dissolution, and redeposition" 17 : 275-287, 1972

      16 Berger, W. H., "Planktic foraminifera: selective solution and the lysocline" 8 : 111-138, 1970

      17 Berger, W. H., "Planktic foraminifera: selective solution and paleoclimatic interpretation" 15 : 31-43, 1968

      18 Berger, W. H., "Paleoproductivity:the benthic/planktic ratio in foraminifera as a productivity index" 81 : 15-25, 1988

      19 Mekik, F. A., "Organic carbon flux and organic carbon to calcite flux ratio recorded in deep-ea carbonates: Demonstration and a new proxy" 16 : 1052-, 2002

      20 Khim, B. K., "Orbital variations of biogenic CaCO3 and opal abundance in the western and central equatorial Pacific Ocean during the Late Quaternary" 23 : 107-117, 2012

      21 Thunell, R. C., "Optimum indices of calcium carbonate dissolution in deep-sea sediments" 4 : 525-528, 1976

      22 Lisitsin, A. P., "Oceanic Sedimentation: Lithology and Geochemistry" American Geophysical Union 400-, 1996

      23 Iwasaki, S., "Observation of the dissolution process of Globigerina bulloides tests (planktic foraminifera)by X‐ray microcomputed tomography" 30 : 317-331, 2015

      24 Petchey, F., "New marine ΔR values for the South Pacific subtropical gyre region" 50 : 373-397, 2008

      25 Burr, G. S., "Modern and Pleistocene Reservoir Ages Inferred from South Pacific Corals" 51 : 319-335, 2009

      26 Seo, I., "Migration of the Kuroshio Extension in the Northwest Pacific since the Last Glacial Maximum" 496 : 323-331, 2018

      27 Yamane, M., "Late Quaternary variations in water mass in the Shatsky Rise area, northwest Pacific Ocean" 48 : 205-223, 2003

      28 Martinez, J. I., "Late Pleistocene Dissolution Cycles in the Vanuatu Region, Western Pacific Ocean" 134 : 293-308, 1994

      29 Broecker, W. S., "Lamont radiocarbon measurements VIII" 3 : 176-204, 1961

      30 Reimers, C. E., "Flocculation of siliceous detritus on the sea floor of a deep Pacific seamount. Deep Sea Research Part A" 36 : 1841-1861, 1989

      31 Parker, F. L., "Faunal and solution patterns of planktic foraminifera in surface sediments of the South Pacific" 18 : 73-107, 1971

      32 Kawahata, H., "Export fluxes in the western Pacific warm pool" 47 : 2061-2091, 2000

      33 Li, B., "Evolution of planktic foraminifera and thermocline in the southern South China Sea since 12 Ma (ODP-184, Site 1143)" 44 : 889-896, 2001

      34 Olausson, E., "Evidence of climatic changes in North Atlantic deep-sea cores, with remarks on isotopic paleotemperatures analysis" 3 : 221-252, 1965

      35 Naik, S. S., "Evaluation of the CaCO3dissolution proxies in sediment cores from above the lysocline" 213 : 69-73, 2010

      36 Archer, D., "Effect of deep-sea sedimentary calcite preservation on atmospheric CO2concentration" 367 : 260-263, 1994

      37 Calvo, E., "Eastern Equatorial Pacific productivity and related-CO2 changes since the last glacial period" 108 : 5537-5541, 2011

      38 Berger, W. H., "Distribution of carbonate in surface sediments of the Pacific Ocean" 81 : 2617-2627, 1976

      39 Biscaye, P. E., "Distribution of calcium carbonate in surface sediments of the Atlantic Ocean" 81 : 2595-2603, 1976

      40 Ding, X., "Distribution and ecology of planktic foraminifera from the seas around the Indonesian Archipelago" 58 : 114-134, 2006

      41 Rottman, M. L., "Dissolution of planktic foraminifera and pteropods in south China Sea sediments" 9 : 41-49, 1979

      42 Volat, J. L., "Dissolution and carbonate fluctuations in Pleistocene deep-sea cores: a review" 34 : 1-28, 1980

      43 Ruddiman, W. F., "Differential solution of planktic foraminifera" 47 : 2629-2651, 1967

      44 Schott, W., "Die Forminiferen in dem äquatorialen Teil des Atlantischen Ozeans" 6 : 411-616, 1935

      45 Kucera, M., "Developments in Marine Geology, 1" Elsevier 213-262, 2007

      46 Zaunbrecher, L. K., "Coral records of central tropical Pacific radiocarbon variability during the last millennium" 25 : PA4212-, 2010

      47 Bordiga, M., "Coccolithophore carbonate during the last 450ka in the NW Pacific Ocean (ODP site 1209B, Shatsky Rise)" 29 : 57-69, 2014

      48 Seo, I., "Climatic evolution of the central equatorial Pacific since the Last Glacial Maximum" 17 : 3454-3468, 2016

      49 Murray, R. W., "Chemical transport to the seafloor of the equatorial Pacific Ocean across a latitudinal transect at 135 W: tracking sedimentary major, trace, and rare earth element fluxes at the Equator and the Intertropical Convergence Zone" 57 : 4141-4163, 1993

      50 Peterson, L. C., "Carbonate dissolution in recent sediments of the eastern equatorial Indian Ocean: Preservation patterns and carbonate loss above the lysocline" 64 : 259-290, 1985

      51 Le, J., "Carbonate dissolution fluctuations in the western equatorial Pacific during the late Quaternary" 7 : 21-42, 1992

      52 Hancock, H. J., "Carbonate dissolution episodes in Paleocene and Eocene sediment, Shatsky Rise, west-central Pacific" 198 : 1-24, 2006

      53 Kimoto, K., "Carbonate dissolution and planktic foraminiferal assemblages observed in three piston cores collected above the lysocline in the western equatorial Pacific" 47 : 227-251, 2003

      54 Emerson, S., "Carbon fluxes at the sediment water interface of the deep-sea: calcium carbonate preservation" 39 : 139-162, 1981

      55 Broecker, W. S., "CaCO3 size distribution:a paleocarbonate ion proxy?" 14 : 596-604, 1999

      56 Stuiver, M., "CALIB 7.1 [WWW program]"

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      학술지 이력

      학술지 이력
      연월일 이력구분 이력상세 등재구분
      2023 평가예정 해외DB학술지평가 신청대상 (해외등재 학술지 평가)
      2020-01-01 평가 등재학술지 유지 (해외등재 학술지 평가) KCI등재
      2017-01-01 평가 등재학술지 유지 (계속평가) KCI등재
      2013-04-29 학술지명변경 외국어명 : 미등록 -> Journal of the Geological Society of Korea KCI등재
      2013-01-01 평가 등재 1차 FAIL (등재유지) KCI등재
      2010-01-01 평가 등재학술지 유지 (등재유지) KCI등재
      2008-01-01 평가 등재학술지 유지 (등재유지) KCI등재
      2006-01-01 평가 등재학술지 유지 (등재유지) KCI등재
      2004-01-01 평가 등재학술지 유지 (등재유지) KCI등재
      2001-07-01 평가 등재학술지 선정 (등재후보2차) KCI등재
      1999-01-01 평가 등재후보학술지 선정 (신규평가) KCI등재후보
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      기준연도 WOS-KCI 통합IF(2년) KCIF(2년) KCIF(3년)
      2016 0.94 0.94 0.91
      KCIF(4년) KCIF(5년) 중심성지수(3년) 즉시성지수
      0.87 0.84 1.386 0.19
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