CORRECTION article
Front. Mar. Sci.
Sec. Marine Biogeochemistry
Volume 12 - 2025 | doi: 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
Provisionally accepted
- Second Institute of Oceanography, Ministry of Natural Resources, Hangzhou, China
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Error in figure/table 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 CIA-A-CN-K diagram illustrating the degree of chemical weathering.] and its caption **[ 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).] appear below. The authors apologize for this error and state that this does not change the scientific conclusions of the article in any way. The original article has been updated.
Keywords: Last glacial period, Western Pacific, Mariana trench, Laminated diatom mats, Ethmodiscus rex
Received: 07 Jul 2025; Accepted: 14 Aug 2025.
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) or licensor 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:
Junyu Lin, Second Institute of Oceanography, Ministry of Natural Resources, Hangzhou, China
Dong Xu, Second Institute of Oceanography, Ministry of Natural Resources, Hangzhou, China
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