Front. Mar. Sci. Frontiers in Marine Science Front. Mar. Sci. 2296-7745 Frontiers Media S.A. 10.3389/fmars.2025.1661159 Marine Science Correction Correction: Giant diatom blooms driven by deep water upwelling since late MIS3? Evidence from the rim of the Mariana Trench Lin Junyu 1 2 Xu Dong 1 2 * Li Yue 2 Ye Liming 1 2 Ge Qian 1 2 Bian Yeping 1 2 Han Xibin 1 2 Zhang Weiyan 1 2 Cheng Shenghui 1 2 1 State Key Laboratory of Submarine Geoscience, Hangzhou, China 2 Second Institute of Oceanography, Ministry of Natural Resources, Hangzhou, China

Edited and reviewed by: Xiaodong Jiang, Guangdong University of Technology, China

*Correspondence: Dong Xu, xudong@sio.org.cn

28 08 2025 2025 12 1661159 07 07 2025 14 08 2025 Copyright © 2025 Lin, Xu, Li, Ye, Ge, Bian, Han, Zhang and Cheng. 2025 Lin, Xu, Li, Ye, Ge, Bian, Han, Zhang and Cheng

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 A Correction on Giant diatom blooms driven by deep water upwelling since late MIS3? Evidence from the rim of the Mariana Trench By Lin J, Xu D, Li Y, Ye L, Ge Q, Bian Y, Han X, Zhang W and Cheng S (2025) Front. Mar. Sci. 12:1556799. doi: 10.3389/fmars.2025.1556799 last glacial period Western Pacific Mariana Trench laminated diatom mats Ethmodiscus rex section-in-acceptance Marine Biogeochemistry

In the published article, there was an error in Figure 7 , “CIA-A-CN-K diagram illustrating the degree of chemical weathering”, as published. Figure 7 was inadvertently replaced with an earlier draft version during the production process. The corrected Figure 7 and its caption appear below.

CIA-A-CN-K diagram illustrating the degree of chemical weathering. Data sources: Chinese loess (Qiao et al., 2011 ); Mariana Arc and Mariana Trough (Ikeda et al., 2016 ); Mariana Trench (Luo et al., 2018b ); Kyushu–Palau Ridge (Lelikov et al., 2018 ; Ishizuka et al., 2011 ).

Ternary diagram illustrating chemical weathering using CIA(Chemical Index of Alteration), A, CN, and K axes with data points for various locations. Weathering intensity is labeled as strong, intermediate, and weak. Distinct markers represent E20 U1, E20 U3, China loess, and regions like Mariana Arc and Trench, and Kyushu-Palau Ridge, with fresh basalts and granitoids marked.

The original version of this article has been updated.

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