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ORIGINAL RESEARCH article

Front. Mar. Sci.
Sec. Global Change and the Future Ocean
Volume 12 - 2025 | doi: 10.3389/fmars.2025.1505586
This article is part of the Research Topic Understanding the Response of Ecosystems to Increasing Human Pressures and Climate Change – Management Options View all 21 articles

Exploration and implication of green macroalgal proliferation in the Nanhui-east-tidal-flat: An investigation of post-reclamation mudflat wetlands

Provisionally accepted
  • 1 State Key Laboratory of Marine Geology, Tongji University, Shanghai, China
  • 2 College of Ocean and Earth Science, Xiamen University, Xiamen, Fujian Province, China
  • 3 College of Oceanography and Ecological Science, Shanghai Ocean University, Shanghai, Shanghai Municipality, China
  • 4 School of Oceanography, Shanghai Jiao Tong University, Shanghai, Shanghai Municipality, China

The final, formatted version of the article will be published soon.

    The Nanhui-east-tidal-flat (NETF) is significantly impacted by human activities.Prior research has not detected the presence of green macroalgae in the NETF,nor has it explored the effects of reclamation on the distribution of macroalgae.However,in 2021,a small-scale aggregated attached algal mats emerged in the NETF,potentially signaling the onset of a green tide and necessitating vigilant monitoring.Morphological and molecular biological identification analysis revealed that all collected green macroalgae were attributed to a single dominant species,Ulva prolifera,characterized by broad blades and prominent air bladders,colonizing various substrates.The attached U.prolifera exhibited continuous growth from March to May 2021,peaking at a wet weight of 373.6229g/m² and a dry weight of 72.7904g/m² on May 1,2021,within the accessible sampling period.The rapid proliferation of the"opportunistic" Ulva was facilitated by high-level eutrophication and favorable environmental conditions.Furthermore,six potential germplasm sources of U.prolifera are summarized.The dominance of Ulva in the intertidal zone often indicates high eutrophication and deteriorating ecological conditions.With long-term reclamation and repeated ecological restoration projects,the intertidal vegetation is subjected to a vicious cycle of growth and destruction.Therefore,it is important to recognize that U.prolifera germplasm (macroalgae and micropropagules) will persist over the long term,and mudflats with monotonous and eutrophic habitats are highly likely to experience future large-scale algal blooms.Notably,a small-scale floating green tide was observed in the sea area near NETF in July 2023,and such concerns are not unfounded.This study conducts foundational scientific research on the attached green tide algae,a type of research that is relatively scarce in other marine areas.Most studies tend to initiate foundational research only after the outbreak of green tides,lacking early background data from the marine environment,thus rendering this study of significant reference value.Concurrently,this study emphasizes that field surveys remain an essential approach for conducting foundational scientific research on green tide algae in the NETF region,with the need to select appropriate research methods based on the occurrence and development of algal mats,as required by the situation.Importantly,this study reflects the stability of marine ecosystems as a prerequisite for modern ocean management and services,provides new perspectives on the occurrence and development of green tides,and highlights potential ecological risk factors that should be considered in the implementation of intertidal construction projects.

    Keywords: Ecological risk, Harmful Algal Bloom, Indicator species, Ecosystem stability, reclamation, Eutrophication, Anthropogenic stressors, Modern ocean management

    Received: 03 Oct 2024; Accepted: 09 Jan 2025.

    Copyright: © 2025 Liu, Xia, Zeng, Xia and He. 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:
    Jinlin Liu, State Key Laboratory of Marine Geology, Tongji University, Shanghai, China
    Jing Xia, School of Oceanography, Shanghai Jiao Tong University, Shanghai, 200240, Shanghai Municipality, China

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