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CORRECTION article

Front. Mar. Sci., 28 August 2025

Sec. Marine Biogeochemistry

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

This article is part of the Research TopicBiogeochemical Cycling and Depositional Processes of Critical Metals in the Deep Sea and Their Constraints on Global ChangesView all 10 articles

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

This article is a correction to:

  1. Giant Diatom Blooms Driven by Deep Water Upwelling Since Late MIS3? Evidence from the Rim of the Mariana Trench

    1. Read original article
Junyu Lin,Junyu Lin1,2Dong Xu,*Dong Xu1,2*Yue LiYue Li2Liming Ye,Liming Ye1,2Qian Ge,Qian Ge1,2Yeping Bian,Yeping Bian1,2Xibin Han,Xibin Han1,2Weiyan Zhang,Weiyan Zhang1,2Shenghui Cheng,Shenghui Cheng1,2
  • 1State Key Laboratory of Submarine Geoscience, Hangzhou, China
  • 2Second Institute of Oceanography, Ministry of Natural Resources, Hangzhou, China

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

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.

Figure 7. 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.

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.

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.

Edited and reviewed by:

Xiaodong Jiang, Guangdong University of Technology, China

Copyright © 2025 Lin, Xu, Li, Ye, Ge, Bian, Han, Zhang and Cheng. This is an open-access article distributed under the terms of the Creative Commons Attribution License (CC BY). The use, distribution or reproduction in other forums is permitted, provided the original author(s) and the copyright owner(s) are credited and that the original publication in this journal is cited, in accordance with accepted academic practice. No use, distribution or reproduction is permitted which does not comply with these terms.

*Correspondence: Dong Xu, eHVkb25nQHNpby5vcmcuY24=

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.