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Characterization of Clastic and Organic Sediments Near Dokdo, Korea

독도 인근 해저퇴적물과 유기 퇴적물 분포 특성

  • Received : 2013.05.29
  • Accepted : 2013.06.19
  • Published : 2013.06.30

Abstract

Sediment transport mechanism and distribution of organic sediments are elucidated by the study of particle size, mineralogy, organic matters and microfossils of the surface samples collected from seafloor adjacent Dokdo island. Shallow marine sediments are dominated by coarse- grained sediments including gravel and sand, and their sedimentation has mainly been controlled by traction. While the samples collected from oceanic zone are characterized by high contents of fine- grained sediments such as silt and mud in bulk sediments, and the changes of mineral compositions including clay minerals and feldspar, and the fine sediments have been deposited mainly by suspension. The change of organic sedimentary communities is detected between neritic and oceanic zone. Although marine organic matter is predominant in neritic zone, terrestrial organic matter is monopolized according to increasing water depth. This trend is associated with grain size of sediments. The results also suggest that high pollen concentrations in whole organic matters may played an important role in excessive organic carbon in sediment.

Keywords

Dokdo;sediment transport mechanism;organic carbon;palynomorph;pollen

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Acknowledgement

Supported by : 한국해양과학기술원, 해양수산부