Macroalgal influence on particulate organic matter sources and early transformation in an Arctic fjord
Abstract. Accelerated Arctic warming is promoting the expansion of coastal macroalgal habitats, yet their influence on pelagic organic carbon cycling remains unresolved. This study investigate the influence of macroalgal beds on the biochemical composition of surface particulate organic matter (POM) in Kongsfjorden, Svalbard, during late summer 2023. Surface waters were sampled at four macroalgal-dominated sites (MDS) and from adjacent waters (Adj-W) located 500 m and 1500 m away. A multi-proxy approach integrating elemental composition, stable isotopes, biopolymeric fractions, monosaccharides, and amino acids was used to trace macroalgal contributions and their lateral redistribution. Concentrations of particulate organic carbon, particulate nitrogen, particulate carbohydrates, and proteins were consistently higher at MDS than in Adj-W, indicating localized enrichment of biochemically labile organic matter within macroalgal habitats. Molecular analyses revealed elevated concentrations of monosaccharides and amino acids at MDS, including macroalgal-associated sugars (glucose, galactose, fucose, mannuronic acid) and labile amino acids (Asp, Glu, Gly, Ser, Ala), demonstrating incorporation of macroalgal-bed derived matter into surface POM. Declining concentrations and composition shift in Adj-W, together with internal reorganization of biopolymeric and molecular composition, indicate efficient lateral export with selective early-stage transformation of POM. Bulk δ¹³C showed minimal spatial variation (−26.8 to −29.1 ‰), suggesting that macroalgal influence is expressed through biochemical restructuring rather than isotopic dominance. Principal component analysis identified a continuous macroalgal–pelagic gradient, with MDS occupying the macroalgal-influenced end. Overall, these findings indicate that Arctic macroalgal beds act as dynamic coastal biogeochemical hotspot, redistributing and transforming organic carbon beyond their immediate habitat.
This manuscript investigates the influence of macroalgal beds in the Arctic Kongsfjorden on the sources and early transformation processes of surface particulate organic matter. By comparing surface water samples from four macroalgae-dominated sites and their adjacent waters (500 m and 1500 m), and employing a combination of elemental analysis, stable isotopes, macromolecular composition, and molecular biomarkers, the authors found that macroalgal beds are a significant source of labile carbon and nitrogen compounds in surface POM, with their molecular fingerprints (e.g., monosaccharide and amino acid composition) showing distinct signatures. POM derived from macroalgae can be exported to the fjord scale and undergoes selective transformation during lateral transport. Principal component analysis revealed a continuous biogeochemical gradient from the macroalgal beds to the adjacent waters. Among the sites, Brandal stands out as a distinct biogeochemical hotspot influenced by macroalgae. This study provides important multi-proxy evidence for understanding how expanding macroalgal communities, under rapid Arctic warming, influence the sources, transport, and transformation of coastal organic carbon through benthic-pelagic coupling processes. It holds clear academic value for deepening the understanding of the Arctic coastal carbon cycle and is worthy of publication after revision.
Major Deficiencies and Revision Suggestions
1) The abstract and highlights sections are repetitive and could be further refined. (Lines 14-22, 24-45). It is suggested that the author revisits and integrates the content of these two sections. Consider refining the "Highlights" into the most concise and eye-catching core innovative findings, while the "Abstract" should maintain its independence, providing a complete yet succinct overview of the research background, methods, main results, and conclusions, avoiding simple repetition of the highlight statements.
2) Lines 511-536: The explanation for the mechanism behind the finding that "Brandal is a biogeochemical hotspot influenced by macroalgae" is primarily attributed to "high biomass," "favorable growth conditions," and "possible promotion of detritus retention by hydrological conditions," which is somewhat general. It is suggested to add a subsection or paragraph to explore more specifically the potential local driving factors that make the Brandal site a hotspot. For example, can known information about the site's geographical location, water depth, hydrodynamic characteristics (e.g., whether it is in a circulation or upwelling area), degree of freshwater input, etc., or citations of relevant literature, be incorporated to support the speculation that "hydrological conditions promote retention," making the conclusion more robust.
3) .Specific citation suggestions:
1) Lines 89-91: In the introduction, when discussing the complexity of organic matter sources in the Arctic coastal zone, after ".....(Singh et al., 2024b) and sediments (Roy et al., 2025) in Kongsfjorden", add: "Similarly, studies on the Qinghai-Tibetan Plateau saline lakes have shown that the molecular composition of dissolved organic matter is also strongly influenced by watershed inputs and internal biological processes (Jiang et al., 2022), and that terrestrially derived organic matter can be transformed driven by aquatic microbial communities (Yang et al., 2020)."
2)Line 457: After "observed decline in POC from MDS to Adj-W", insert: "This aligns with the classical understanding of preferential degradation of labile components in marine environments. In lake sediment systems, inputs of algal and terrestrial organic matter have been shown to stimulate significantly different microbial degradation processes (priming effects) (Yang et al., 2023), with methanogenesis potentially dominating the carbon flow under anoxic conditions (Yang et al., 2025), implying the key control of organic matter molecular composition on its transformation pathways."
3)Line 517: After "matter within this macroalgal-dominated habitat", insert: "Habitat heterogeneity is considered a primary factor driving microbial community assembly and functional differentiation in extreme environments (Huang et al., 2026). In Qinghai Lake, the assembly mechanisms of prokaryotic and microeukaryotic communities have been shown to be significantly different and regulated by different environmental factors (Han et al., 2023). Similarly, research in the Aral Sea region indicates that minor differences in salinity and mineralogy can lead to distinctly different responses in microbial and endophytic communities (Jiang et al., 2021). Therefore, the Brandal hotspot may result from the combined action of its unique substrate (macroalgal bed), local hydrodynamics (forming a 'retention zone'), and the resulting unique microbial community, reflecting the high specificity of biogeochemical processes at the microhabitat scale."
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Jiang et al, (2021) Onshore soil microbes and endophytes respond differently to salinity and mineralogy in the Aral Sea. Science of the Total Environment 765: 142675,https://doi.org/10.1016/j.scitotenv.2020.142675
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Jiang*, et al. (2022) Molecular composition of dissolved organic matter in saline lakes of the Qing-Tibetan Plateau. Organic Geochemistry 167: 104400. https://doi.org/10.1016/j.orggeochem.2022.104400
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Yang, et al., (2023) Predominance of positive priming effects induced by algal and terrestrial organic matter input in saline lake sediments. Geochimica et Cosmochimica Acta 349: 126–134, https://doi.org/10.1016/j.gca.2023.04.005
Yang, et al., (2025) Methanogenesis rather than carbon dioxide production frives positive priming effects in anoxic sediments of saline lakes. Chemical Geology 678: 122680, https://doi.org/10.1016/j.chemgeo.2025.122680
Huang et al. (2026) Habitat heterogeneity drives microbial community assembly and functional specialization in extreme arid ecosystems. Applied and Environmental Microbiology, https://doi.org/10.1128/aem.02588-25