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Young-Suk Bak

Dados Biográficos

ID7518210
NOMEYoung-Suk Bak
PRENOMESYoung-Suk
SOBRENOMEBak
ASSINATURABAK Y
AFILIAÇÕESChonbuk National University, Korea
VERIFICADONão
TOTAL DE OBRAS3
TOTAL DE CITAÇÕES0
TOTAL COMO AUTOR3
TOTAL COMO EDITOR0
PRIMEIRO ANO DE PUBLICAÇÃO2010
ANO MAIS RECENTE DE PUBLICAÇÃO2015
ÍNDICE H0
  • Mid-Holocene sea-level fluctuation inferred from diatom analysis from sediments on the west coast of Korea

    Open Access•Young-Suk Bak•ARTICLE•Quaternary International•2015

  • Late Quaternary glacial–interglacial variations in sediment supply in the southern Drake Passage

    Open Access•Jae Il Lee, Ho Il Yoon et al.•ARTICLE•Quaternary Research•2012

    Geochemical characteristics of marine sediment from the southern Drake Passage were analyzed to reconstruct variations in sediment provenance and transport paths during the late Quaternary. The 5.95 m gravity core used in this study records paleoenvironmental changes during the last approximately 600 ka. Down-core variations in trace element, rare earth element, and Nd and Sr isotopic compositions reveal that sediment provenance varied according …

  • Climate changes in the South Orkney Plateau during the last 8600 years

    Open Access•Jae Il Lee, Young‐Suk Bak et al.•ARTICLE•The Holocene•2010

    Climatic and oceanographic changes in the South Orkney Plateau, western Antarctica, during the last 8600 years are reconstructed from a 525 cm long gravity core based on sedimentological, geochemical and diatom analyses. The core sediments are composed mostly of light greyish olive diatomaceous silt and mud with a few diatom ooze laminae in the basal part. The core can be divided at 350 cm into two units (4800 cal. yr BP): the lower unit is chara…

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  • Climate changes in the South Orkney Plateau during the last 8600 years

    Open Access•Jae Il Lee, Young‐Suk Bak et al.•ARTICLE•The Holocene•2010

    Climatic and oceanographic changes in the South Orkney Plateau, western Antarctica, during the last 8600 years are reconstructed from a 525 cm long gravity core based on sedimentological, geochemical and diatom analyses. The core sediments are composed mostly of light greyish olive diatomaceous silt and mud with a few diatom ooze laminae in the basal part. The core can be divided at 350 cm into two units (4800 cal. yr BP): the lower unit is chara…

  • Late Quaternary glacial–interglacial variations in sediment supply in the southern Drake Passage

    Open Access•Jae Il Lee, Ho Il Yoon et al.•ARTICLE•Quaternary Research•2012

    Geochemical characteristics of marine sediment from the southern Drake Passage were analyzed to reconstruct variations in sediment provenance and transport paths during the late Quaternary. The 5.95 m gravity core used in this study records paleoenvironmental changes during the last approximately 600 ka. Down-core variations in trace element, rare earth element, and Nd and Sr isotopic compositions reveal that sediment provenance varied according …

  • Mid-Holocene sea-level fluctuation inferred from diatom analysis from sediments on the west coast of Korea

    Open Access•Young-Suk Bak•ARTICLE•Quaternary International•2015

Geology and Paleoclimatology Research (3 obras) · Methane Hydrates and Related Phenomena (3 obras) · Sediment (3 obras) · Geology (2 obras) · Holocene (2 obras) · Isotope Analysis in Ecology (2 obras) · Oceanography (2 obras) · Paleontology (2 obras) · Biogenic silica (1 obras) · Carbonate (1 obras)

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