CORRECTION article

Front. Mar. Sci., 28 August 2025

Sec. Marine Biogeochemistry

Volume 12 - 2025 | https://doi.org/10.3389/fmars.2025.1661159

Correction: Giant diatom blooms driven by deep water upwelling since late MIS3? Evidence from the rim of the Mariana Trench

  • 1. State Key Laboratory of Submarine Geoscience, Hangzhou, China

  • 2. Second Institute of Oceanography, Ministry of Natural Resources, Hangzhou, China

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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.

Figure 7

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.

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 ).

The original version of this article has been updated.

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Publisher’s note

All claims expressed in this article are solely those of the authors and do not necessarily represent those of their affiliated organizations, or those of the publisher, the editors and the reviewers. Any product that may be evaluated in this article, or claim that may be made by its manufacturer, is not guaranteed or endorsed by the publisher.

Summary

Keywords

last glacial period, Western Pacific, Mariana Trench, laminated diatom mats, Ethmodiscus rex

Citation

Lin J, Xu D, Li Y, Ye L, Ge Q, Bian Y, Han X, Zhang W and Cheng S (2025) Correction: Giant diatom blooms driven by deep water upwelling since late MIS3? Evidence from the rim of the Mariana Trench. Front. Mar. Sci. 12:1661159. doi: 10.3389/fmars.2025.1661159

Received

07 July 2025

Accepted

14 August 2025

Published

28 August 2025

Volume

12 - 2025

Edited and reviewed by

Xiaodong Jiang, Guangdong University of Technology, China

Updates

Copyright

*Correspondence: Dong Xu,

Disclaimer

All claims expressed in this article are solely those of the authors and do not necessarily represent those of their affiliated organizations, or those of the publisher, the editors and the reviewers. Any product that may be evaluated in this article or claim that may be made by its manufacturer is not guaranteed or endorsed by the publisher.

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