Early to middle Holocene development of the Tsushima Warm Current based on benthic and planktonic foraminifera in the Nakdong River delta (southeast Korea)

Author:

Takata Hiroyuki,Khim Boo-Keun,Shin Seungwon,Lee Jin-YoungORCID,Kim Jin-Cheul,Katsuki Kota,Cheong DaekyoORCID

Funder

Atmospheric See-At Technology Development Program

Publisher

Elsevier BV

Subject

Earth-Surface Processes

Reference57 articles.

1. Bathymetric distribution of the Recent benthic foraminifers around Japan – as a contribution to the new paleobathymetric scale;Akimoto;Geol. Soc. Japan, Memoirs,1989

2. Diatom distribution in surface sediments from Chinese inshore waters and the relationship to modern environmental variables;Chen;Chin. J. Oceanol. Limnol.,2014

3. Delta formation in the Nakdong River, Korea, during the Holocene as inferred from the diatom assemblage;Cho;J. Coast Res.,2017

4. Statistics and Data Analysis in Geology;Davis,1973

5. Holocene influx of the Tsushima Current into the Japan Sea signaled by spatial and temporal changes in Neogloboquadrina incompta distribution;Domitsu;Holocene,2008

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