Cyclostratigraphy of the Late Miocene to Pliocene sediments at IODP sites U1425 and U1430 in the Japan Sea and paleoceanographic implications

Autor: Shunsuke Kurokawa, Ryuji Tada, Kenji M. Matsuzaki, Tomohisa Irino, Lofi Johanna

Publikováno v: Progress in Earth and Planetary Science, Vol 6, Iss 1, Pp 1-20 (2019)

Abstract High-resolution studies of sedimentary sequences have reconstructed paleoceanographic changes in the Atlantic and southern and equatorial Pacific Oceans during the Late Miocene and Pliocene, but comparable analyses are lacking for the North

Externí odkaz: https://doaj.org/article/be7f55e0cbdf41d5923f70c80e260a87

High-resolution and high-precision correlation of dark and light layers in the Quaternary hemipelagic sediments of the Japan Sea recovered during IODP Expedition 346

Autor: Tada, Ryuji, Irino, Tomohisa, Ikehara, Ken, Karasuda, Akinori, Sugisaki, Saiko, Xuan, Chuang, Sagawa, Takuya, Itaki, Takuya, Kubota, Yoshimi, Lu, Song, Seki, Arisa, Murray, Richard W., Alvarez-Zarikian, Carlos, Anderson, William T., Bassetti, Maria Angela, Brace, Bobbi J., Clemens, Steven C., da Costa Gurgel, Marcio H., Dickens, Gerald R., Dunlea, Ann G., Gallagher, Stephen J., Giosan, Liviu, Henderson, Andrew C.G., Holbourn, Ann E., Kinsley, Christopher W., Lee, Gwang Soo, Lee, Kyung Eun, Lofi, Johanna, Lopes, Christina I.C.D., Saavedra-Pellitero, Mariem, Peterson, Larry C., Singh, Raj K., Toucanne, Samuel, Wan, Shiming, Zheng, Hongbo, Ziegler, Martin, Stratigraphy and paleontology, Stratigraphy & paleontology

Publikováno v: Progress In Earth And Planetary Science (2197-4284) (Springer), 2018-03, Vol. 5, N. 19, P. 10p.
Progress in Earth and Planetary Science
Progress in Earth and Planetary Science, Springer/Japan Geoscience Union, 2018, 5 (1), ⟨10.1186/s40645-018-0167-8⟩
Progress in Earth and Planetary Science, Vol 5, Iss 1, Pp 1-10 (2018)
Springer Berlin Heidelberg
Progress in Earth and Planetary Science, 5. Springer

The Quaternary hemipelagic sediments of the Japan Sea are characterized by centimeter- to decimeter-scale alternation of dark and light clay to silty clay, which are bio-siliceous and/or bio-calcareous to a various degree. Each of the dark and light

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::773c01f45fbbbad40f0bb87ebd6e77ce
https://doi.org/10.1186/s40645-018-0167-8