http://chineseinput.net/에서 pinyin(병음)방식으로 중국어를 변환할 수 있습니다.
변환된 중국어를 복사하여 사용하시면 됩니다.
Khim, Boo-Keun The Korean Society of Oceanography 1997 Journal of the Korean Society of Oceanography Vol.32 No.1
Two marine bivalve shells were collected from the eastern and western coastal regions of Korea, respectively. Stable oxygen and carbon isotope profiles are constructed using the incremental sampling along the axis of maximum growth to provide the continuous ${\delta}^{18}$O and ${\delta}^{13}$C records, which register the physical, biological and chemical properties of seawater where the organisms live. Cycles in the ${\delta}^{18}$O profiles are interpreted as annual along with the identification of annual growth bands; the maximum ${\delta}^{18}$O values correspond with the coldest temperature of seawater whereas the minimum ${\delta}^{18}$O values with the warmest temperature. The primary control on the amplitude of the ${\delta}^{18}$O profiles is seasonal variation of seawater temperature. The offset of the baseline between ${\delta}^{18}$O values of the two specimens is attributed to differences in both temperature and seawater ${\delta}^{18}$O values between two localities. The ${\delta}^{13}$C profiles show the similar seasonality of carbon cycling associated with phytoplankton productivity. The offset in the ${\delta}^{13}$C profiles between two specimens may be, as in the case of oxygen isotope profile, attributed to the different ${\delta}^{13}$C value of the seawater DIC (dissolved inorganic carbon) between the western coast and the eastern coast. Relationships between the shell isotopic composition and the coastal water properties of shell growth are readily interpreted from the ${\delta}^{18}$O-${\delta}^{13}$C pair diagram of the shell isotope data, similar to the use of salinity-${\delta}^{18}$O diagram for identifying water masses. The preliminary stable isotope results of this study suggest that mollusk shell isotope geochemistry may be useful to monitor the properties of water masses in the coastal and inner shelf setting around Korea and improve the interpretation of paleoceanography, provided the fossil mollusks are well preserved.
Khim, Boo-Keun,Shin, Dong-Hyeok,Han, Sang-Joon The Korean Society of Oceanography 1997 Journal of the Korean Society of Oceanography Vol.32 No.3
This study presents results from a detailed sedimentological investigation of surface sediments obtained from the Korea Strait region, the southern part of the East Sea (Sea of Japan). The distribution of different types of bottom sediments is controlled by the recent fine-grained sediment transport and deposition combined with the lowerings of sea level during the last glacial period, forming a diverse mixture of organic-rich fine-grained and shelly coarse-grained sediments. In comparison to high organic concentration of fine-grained sediments in the inner continental shelf and slope areas, the shell-rich coarse-grained sediments on the outer shelf are discernible being further modified. These coarse-grained sediments are confirmed as relict resulting from the sediment dynamics during the lower sea levels of the last glacial period. Clay mineral distribution of the fine-grained sediments gives information about the transport mechanism. Presence of present-day current system (the Tsushima Warm Current) is most probable source for the fine-grained particles into the open East Sea from the East China Sea, indicating that Holocene sediment dynamics may be used to explain the observed distribution of surface coarse-grained shell-rich sediments.
Oxygen Isotope Data of Winter Water in the Western Weddell Sea: Preliminary Results
Khim, Boo-Keun,Park, Byong-Kwon,Kang, Sung-Ho The Korean Society of Oceanography 1998 Journal of the Korean Society of Oceanography Vol.33 No.1
In the western Weddell Sea, winter mixed layer is characterized by near-freezing temperature and higher salinity due to brine injection through sea-ice formation. This layer becomes Winter Water being capped by warmer and less saline Antarctic Surface Water during the sea-ice melt-ing season. In this study, Winter Water was preliminarily identified by the oxygen isotopic com-positions. The ${\delta}^{18}$O values of Winter Water show the progressively increasing trend from south to north in the study area. It presumably reflects the enhanced mixing with Antarctic Surface Water due to the extent of influence by low S'"0 value of sea-ice/glacier meltwater. Correlations between salinity and 6'"0 values of seawater can be used to more generally characterize Winter Water with a view to identification. However, the prediction on the degree of mixing from these relationships needs more detailed isotope data, although this study allows the oxygen isotopic composition of seawater as a tracer to identify the water mass.
Boo-Keun Khim 한국지질과학협의회 2002 Geosciences Journal Vol.6 No.4
Serripes groenlandicus shells were collected alivefrom the eastern regions of the Bering and Chukchi seas whereAlaskan Coastal Water occupies dominantly. High-resolution sta-ble isotope profiles of the shell carbonates exhibit distinct, appar-ently annual, cycles caused by seasonal variations of temperature,seawater isotopic composition and other factors. The shell d18Oprofiles show a moderately high-amplitude seasonal temperaturecycle with considerable interannual variability. Superimposed onthe temperature-controlled cycles are periodic excursions whichare associated with reduced salinity, and more negative seawaterd18O, related presumably to an increased freshwater flux to theAlaskan Coastal Current during the summer. Comparison betweentwo oxygen isotope profiles supports the occurrence of seasonaland interannual variability of Alaskan Coastal Water in the east-ern part of the Bering and Chukchi Shelf. The cycles in the d13Cprofiles are interpreted as being controlled primarily by phy-toplankton productivity and seasonal temperature. In addition, atrend of more negative d13C values towards the later stage ofgrowth may reflect physiological changes associated with sexualmaturity, gametogenesis, and slower growth rate. The oxygen andcarbon isotope profiles as a biorecorder of bivalve shells are sub-stantiated in the subarctic environments, probing the seasonal andinterannual variation of Alaskan Coastal Water.
Khim, Boo-Keun,Je, Jong-Geel,Han, Sang-Joon,Woo, Kyung-Sik,Park, Yong-Ahn 한국패류학회 1998 The Korean Journal of Malacology Vol.14 No.1
동해 연안에서 채취된 뷔나스백합(Mercenaria stimpsoni)의 연령과 성장률을 이매패의 표면에서 확인된 연륜과 이매패 각질에서 분석된 산소동위원소비의 성장에 따른 변화를 이용하여 비교하였다. 뷔나스백합의 산소동위원소상은 일련의 주기적인 변화를 뚜렷하게 보여주며 이러한 변화진폭은 이매패가 성장한 해수의 온도변화에 일차적으로 제어된다. 산소동위원소상의 주기화 연륜의 관계로부터 뷔나스백합의 연륜이 해마다 여름철에 형성됨을 보여준다. 해수 온도의 계절적 변화와 산소동위원소비에서 얻어진 예측 온도와의 비교로부터, 뷔나스백합은 겨울철에 성장이 멈추는 것으로 사료된다. 또한 산소도위원소비는 뷔나스백합의 성장에 따른 전형적인 노화현상을 보여준다. 따라서 이매패가 성장하는 해수의 물리화학적 조건에 의해 제어되는 산소동위원소비는 뷔나스백합의 경우 연령과 성장률을 측정하는 독립적인 시간 척도가 될 수 있다.