Correlation of TL layers for the synchronous paleoceanographic events in the East Sea (Sea of Japan) during the Late Quaternary
TL layers (i.e., dark mud layers), either thin or thick, as determined by the L* values with lithologic observation, are distinct paleoceanographic signatures in the East Sea (Sea of Japan), which were formed in response to the global eustatic sealevel fluctuations between interglacials and glacials...
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| Published in | Geosciences journal (Seoul, Korea) Vol. 13; no. 2; pp. 113 - 120 |
|---|---|
| Main Authors | , , , , , , |
| Format | Journal Article |
| Language | English |
| Published |
Berlin/Heidelberg
Springer-Verlag
01.06.2009
Springer Nature B.V 한국지질과학협의회 |
| Subjects | |
| Online Access | Get full text |
| ISSN | 1226-4806 1598-7477 |
| DOI | 10.1007/s12303-009-0010-8 |
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| Abstract | TL layers (i.e., dark mud layers), either thin or thick, as determined by the L* values with lithologic observation, are distinct paleoceanographic signatures in the East Sea (Sea of Japan), which were formed in response to the global eustatic sealevel fluctuations between interglacials and glacials during the Late Quaternary. These lithologic markers were consistently correlated among the three sediment cores (MD01-2407, 05GCRP21, and KR05-09PC1) collected from the Oki Ridge of the southern Yamato Basin, the South Korea Plateau of the northern Ulleung Basin, and the Matsumae Plateau of the northeastern Japan Basin, respectively. Reconstruction of age models for cores 05GCRP and KR05-09PC1 was aided in a good way by the AMS
14
C ages of planktonic foraminifera and identification of the tephra layers, and mainly by lithostratigraphic correlation with TL layers of well-dated core MD01-2407, based on the L* values. The correlation of TL layers among the three sediment cores was remarkable, indicating that the East Sea (Sea of Japan) experienced the synchronous and basin-wide scale paleoceanographic events during the Late Quaternary. Our study exemplifies the significant usefulness of these lithologic markers for further Late Quaternary paleoceanographic investigation. |
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| AbstractList | TL layers (i.e., dark mud layers), either thin or thick, as determined by the L* values with lithologic observation, are distinct paleoceanographic signatures in the East Sea (Sea of Japan), which were formed in response to the global eustatic sea-level fluctuations between interglacials and glacials during the Late Quaternary. These lithologic markers were consistently correlated among the three sediment cores (MD01-2407, 05GCRP21, and KR05-09PC1) collected from the Oki Ridge of the southern Yamato Basin, the South Korea Plateau of the northern Ulleung Basin, and the Matsumae Plateau of the northeastern Japan Basin, respectively. Reconstruction of age models for cores 05GCRP and KR05-09PC1 was aided in a good way by the AMS 14C ages of planktonic foraminifera and identification of the tephra layers, and mainly by lithostratigraphic correlation with TL layers of well-dated core MD01-2407, based on the L* values. The correlation of TL layers among the three sediment cores was remarkable, indicating that the East Sea (Sea of Japan) experienced the synchronous and basin-wide scale paleoceanographic events during the Late Quaternary. Our study exemplifies the significant usefulness of these lithologic markers for further Late Quaternary paleoceanographic investigation. (PUBLICATION ABSTRACT) TL layers (i.e., dark mud layers), either thin or thick, as determined by the L* values with lithologic observation, are distinct paleoceanographic signatures in the East Sea (Sea of Japan), which were formed in response to the global eustatic sealevel fluctuations between interglacials and glacials during the Late Quaternary. These lithologic markers were consistently correlated among the three sediment cores (MD01-2407, 05GCRP21, and KR05-09PC1) collected from the Oki Ridge of the southern Yamato Basin, the South Korea Plateau of the northern Ulleung Basin, and the Matsumae Plateau of the northeastern Japan Basin, respectively. Reconstruction of age models for cores 05GCRP and KR05-09PC1 was aided in a good way by the AMS 14 C ages of planktonic foraminifera and identification of the tephra layers, and mainly by lithostratigraphic correlation with TL layers of well-dated core MD01-2407, based on the L* values. The correlation of TL layers among the three sediment cores was remarkable, indicating that the East Sea (Sea of Japan) experienced the synchronous and basin-wide scale paleoceanographic events during the Late Quaternary. Our study exemplifies the significant usefulness of these lithologic markers for further Late Quaternary paleoceanographic investigation. TL layers (i.e., dark mud layers), either thin or thick, as determined by the L* values with lithologic observation, are distinct paleoceanographic signatures in the East Sea (Sea of Japan), which were formed in response to the global eustatic sea-level fluctuations between interglacials and glacials during the Late Quaternary. These lithologic markers were consistently correlated among the three sediment cores (MD01-2407, 05GCRP21, and KR05-09PC1) collected from the Oki Ridge of the southern Yamato Basin, the South Korea Plateau of the northern Ulleung Basin, and the Matsumae Plateau of the northeastern Japan Basin, respectively. Reconstruction of age models for cores 05GCRP and KR05-09PC1 was aided in a good way by the AMS 14C ages of planktonic foraminifera and identification of the tephra layers, and mainly by lithostratigraphic correlation with TL layers of well-dated core MD01-2407, based on the L* values. The correlation of TL layers among the three sediment cores was remarkable, indicating that the East Sea (Sea of Japan) experienced the synchronous and basin-wide scale paleoceanographic events during the Late Quaternary. Our study exemplifies the significant usefulness of these lithologic markers for further Late Quaternary paleoceanographic investigation. KCI Citation Count: 11 |
| Author | Khim, Boo-Keun Itaki, Takuya Tada, Ryuji Ikehara, Ken Park, Yu Hyeon Bahk, Jang Jun Kido, Yoshiki |
| Author_xml | – sequence: 1 givenname: Boo-Keun surname: Khim fullname: Khim, Boo-Keun email: bkkhim@pusan.ac.kr organization: Division of Earth Environmental System, Pusan National University – sequence: 2 givenname: Ryuji surname: Tada fullname: Tada, Ryuji organization: Department of Earth and Planetary Science, University of Tokyo – sequence: 3 givenname: Yu Hyeon surname: Park fullname: Park, Yu Hyeon organization: Division of Marine Geology, South Sea Institute, KORDI – sequence: 4 givenname: Jang Jun surname: Bahk fullname: Bahk, Jang Jun organization: Petroleum and Marine Resources Division, Korea Institute of Geoscience and Mineral Resources – sequence: 5 givenname: Yoshiki surname: Kido fullname: Kido, Yoshiki organization: OD Science Technical Support Section #1, Marine Works Japan Ltd – sequence: 6 givenname: Takuya surname: Itaki fullname: Itaki, Takuya organization: Institute of Geology and Geoinformation, Geological Survey of Japan, AIST – sequence: 7 givenname: Ken surname: Ikehara fullname: Ikehara, Ken organization: Institute of Geology and Geoinformation, Geological Survey of Japan, AIST |
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| CitedBy_id | crossref_primary_10_1016_j_jseaes_2015_04_040 crossref_primary_10_1111_bor_12484 crossref_primary_10_1002_jqs_1554 crossref_primary_10_1029_2018PA003343 crossref_primary_10_2343_geochemj_2_0606 crossref_primary_10_1016_j_jseaes_2012_12_036 crossref_primary_10_2343_geochemj_2_0305 crossref_primary_10_1007_s12601_022_00076_w crossref_primary_10_1177_09596836211003238 crossref_primary_10_1016_j_pocean_2010_12_016 crossref_primary_10_1016_j_quaint_2014_07_024 crossref_primary_10_1016_j_jseaes_2013_12_020 crossref_primary_10_1016_j_nimb_2009_10_145 crossref_primary_10_1016_j_palaeo_2025_112892 crossref_primary_10_1017_pab_2018_37 crossref_primary_10_3389_feart_2021_647495 |
| Cites_doi | 10.1016/S0031-0182(99)00137-6 10.1016/0033-5894(92)90072-Q 10.1016/j.palaeo.2006.11.020 10.1007/BF02239520 10.1016/S0921-8181(99)00008-9 10.4116/jaqua.34.4_289 10.1029/1998PA900016 10.1029/91PA00560 10.4116/jaqua.29.417 10.1029/98GL00359 10.1016/0025-3227(92)90222-4 10.1016/0033-5894(87)90046-9 10.1016/S0025-3227(01)00217-1 10.1007/BF02910318 10.1029/1998PA900023 10.1029/95PA03553 10.1016/0304-4203(91)90016-P 10.1006/qres.2001.2289 10.1016/0025-3227(92)90032-D 10.1016/j.palaeo.2006.11.029 10.1016/j.palaeo.2006.11.019 10.1016/j.pocean.2004.06.005 10.1016/0009-2541(94)90059-0 10.1175/1520-0485(1999)029<1701:FACPOI>2.0.CO;2 10.1029/98JC01948 10.1029/2001GL013078 10.1016/j.palaeo.2006.11.026 10.1016/j.palaeo.2006.11.021 10.1016/S0025-3227(99)00079-1 10.1038/342637a0 10.1029/1999PA000393 10.1016/j.quaint.2007.04.004 10.1016/0025-3227(93)90150-T 10.1029/1999GL002341 10.2973/odp.proc.sr.127128-1.159.1992 10.5575/geosoc.102.125 10.2973/odp.proc.sr.127128.160.1992 |
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| Title | Correlation of TL layers for the synchronous paleoceanographic events in the East Sea (Sea of Japan) during the Late Quaternary |
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