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<front>
<journal-meta>
<journal-id journal-id-type="publisher-id">Front. Mar. Sci.</journal-id>
<journal-title>Frontiers in Marine Science</journal-title>
<abbrev-journal-title abbrev-type="pubmed">Front. Mar. Sci.</abbrev-journal-title>
<issn pub-type="epub">2296-7745</issn>
<publisher>
<publisher-name>Frontiers Media S.A.</publisher-name>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="doi">10.3389/fmars.2025.1493581</article-id>
<article-categories>
<subj-group subj-group-type="heading">
<subject>Marine Science</subject>
<subj-group>
<subject>Original Research</subject>
</subj-group>
</subj-group>
</article-categories>
<title-group>
<article-title>Development amongst the seagrass <italic>Cymodocea nodosa</italic> influences the morphology of the brown algae <italic>Gongolaria barbata</italic> in a coastal lagoon of the northern Adriatic Sea</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author" corresp="yes">
<name>
<surname>Smith</surname>
<given-names>Shannen M.</given-names>
</name>
<xref ref-type="author-notes" rid="fn001">
<sup>*</sup>
</xref>
<xref ref-type="author-notes" rid="fn003">
<sup>&#x2020;</sup>
</xref>
<uri xlink:href="https://loop.frontiersin.org/people/2828326/overview"/>
<role content-type="https://credit.niso.org/contributor-roles/conceptualization/"/>
<role content-type="https://credit.niso.org/contributor-roles/data-curation/"/>
<role content-type="https://credit.niso.org/contributor-roles/formal-analysis/"/>
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<contrib contrib-type="author">
<name>
<surname>Bilajac</surname>
<given-names>Andrea</given-names>
</name>
<role content-type="https://credit.niso.org/contributor-roles/conceptualization/"/>
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<contrib contrib-type="author">
<name>
<surname>Glju&#x161;&#x107;i&#x107;</surname>
<given-names>Edi</given-names>
</name>
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<contrib contrib-type="author">
<name>
<surname>Najdek</surname>
<given-names>Mirjana</given-names>
</name>
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<contrib contrib-type="author">
<name>
<surname>Ive&#x161;a</surname>
<given-names>Ljiljana</given-names>
</name>
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<aff id="aff1">
<institution>Center for Marine Research, Ru&#x111;er Bo&#x161;kovi&#x107; Institute</institution>, <addr-line>Zagreb</addr-line>, <country>Croatia</country>
</aff>
<author-notes>
<fn fn-type="edited-by">
<p>Edited by: Susana Carvalho, King Abdullah University of Science and Technology, Saudi Arabia</p>
</fn>
<fn fn-type="edited-by">
<p>Reviewed by: Edson A. Vieira, Federal University of Rio Grande do Norte, Brazil</p>
<p>Felipe Ribeiro, Universidade Federal Fluminense, Brazil</p>
</fn>
<fn fn-type="corresp" id="fn001">
<p>*Correspondence: Shannen M. Smith, <email xlink:href="mailto:shannen.m.smith@outlook.com">shannen.m.smith@outlook.com</email>
</p>
</fn>
<fn fn-type="present-address" id="fn003">
<p>&#x2020;Present address: Shannen M. Smith, Aquatic Sciences, South Australian Research and Development Institute, Adelaide, SA, Australia</p>
</fn>
</author-notes>
<pub-date pub-type="epub">
<day>18</day>
<month>06</month>
<year>2025</year>
</pub-date>
<pub-date pub-type="collection">
<year>2025</year>
</pub-date>
<volume>12</volume>
<elocation-id>1493581</elocation-id>
<history>
<date date-type="received">
<day>09</day>
<month>09</month>
<year>2024</year>
</date>
<date date-type="accepted">
<day>12</day>
<month>05</month>
<year>2025</year>
</date>
</history>
<permissions>
<copyright-statement>Copyright &#xa9; 2025 Smith, Bilajac, Glju&#x161;&#x107;i&#x107;, Najdek and Ive&#x161;a</copyright-statement>
<copyright-year>2025</copyright-year>
<copyright-holder>Smith, Bilajac, Glju&#x161;&#x107;i&#x107;, Najdek and Ive&#x161;a</copyright-holder>
<license xlink:href="http://creativecommons.org/licenses/by/4.0/">
<p>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.</p>
</license>
</permissions>
<abstract>
<p>Marine forests are declining worldwide and understanding the ecology of extant forests is crucial for developing practices that best conserve and restore them for the future. In  the Mediterranean region, there has been an increasing effort to restore forest forming fucalean seaweeds and to understand the ecological context that supports their persistence. Here, we describe population metrics for a significant extant fucalean forest located in a coastal lagoon on the southern Istrian peninsula (Croatia). In &#x160;&#x107;uza Lagoon, <italic>Gongolaria barbata</italic> settles within two main substrate types, on small stones and pebbles amongst seagrass <italic>Cymodocea nodosa</italic> and on rocky substrate provided by larger, more exposed boulders within the meadow but where seagrass does not grow. Amongst seagrass, <italic>G. barbata</italic> grew to a greater maximum height, observed during both its growth and dormant phases. On boulders, any disadvantage in height appeared to be offset by higher recruitment where the overall density was similar between the two areas. Opportunistic recruitment of <italic>G. barbata</italic> during the senescent period for <italic>C. nodosa</italic> appeared to contribute to their coexistence in this unique location and seagrasses appeared to reduce the prevalence of cauloid damage for <italic>G. barbata.</italic> These findings highlight the importance of understanding fine-scale ecological interactions that support the persistence of isolated patches of vulnerable marine forests.</p>
</abstract>
<kwd-group>
<kwd>Adriatic sea</kwd>
<kwd>coastal lagoon</kwd>
<kwd>coexistence</kwd>
<kwd>
<italic>Cymodocea nodosa</italic>
</kwd>
<kwd>
<italic>Gongolaria barbata</italic>
</kwd>
<kwd>marine forests</kwd>
</kwd-group>
<counts>
<fig-count count="6"/>
<table-count count="0"/>
<equation-count count="0"/>
<ref-count count="69"/>
<page-count count="10"/>
<word-count count="4869"/>
</counts>
<custom-meta-wrap>
<custom-meta>
<meta-name>section-in-acceptance</meta-name>
<meta-value>Marine Ecosystem Ecology</meta-value>
</custom-meta>
</custom-meta-wrap>
</article-meta>
</front>
<body>
<sec id="s1" sec-type="intro">
<title>Introduction</title>
<p>The structure and composition of benthic marine habitats are being altered all around the world as groups of foundation species are lost and replaced by groups of lesser ecological complexity. Foundation species create complex physical habitat structure and positively interact with and enhance the resilience of local biological communities (<xref ref-type="bibr" rid="B20">Dayton, 1972</xref>; <xref ref-type="bibr" rid="B60">Stachowicz, 2001</xref>; <xref ref-type="bibr" rid="B3">Angelini et&#xa0;al., 2011</xref>). Marine macrophytes are historically the foundation species found in shallow subtidal temperate environments, large brown seaweeds (i.e. kelps of the orders Laminariales and Fucales) forming forest-like structures on rocky substrates (<xref ref-type="bibr" rid="B62">Teagle et&#xa0;al., 2017</xref>) and seagrasses forming vast meadows where sandy substrates dominate. Seaweed and seagrass communities can coexist where rocky and sandy substrates meet and create a unique set of interactions, however, there are relatively few studies that formally test these interactions in temperate regions. Of those that do, the majority present evidence for negative outcomes for either group citing some level of resource competition, with little evidence for facilitation usually (but not exclusively) in favor of the seagrass (reviewed in <xref ref-type="bibr" rid="B57">Richard and Quij&#xf3;n, 2023</xref>).</p>
<p>In the Mediterranean Sea, macroalgal species of genera <italic>Cystoseira, Ericaria</italic> and <italic>Gongolaria</italic> (order Fucales; hereafter collectively referred to as <italic>Cystoseira sensu lato</italic>), are considered the dominant canopy forming species for temperate rocky reefs, but in recent decades have dramatically declined (<xref ref-type="bibr" rid="B2">Airoldi and Beck, 2007</xref>; <xref ref-type="bibr" rid="B36">Ive&#x161;a et&#xa0;al., 2016</xref>; <xref ref-type="bibr" rid="B41">Mangialajo et&#xa0;al., 2008</xref>; <xref ref-type="bibr" rid="B49">Orlando-Bonaca et&#xa0;al., 2021a</xref>; <xref ref-type="bibr" rid="B64">Thibaut et&#xa0;al., 2005</xref>). The presence of any extant marine forest habitat is considered a positive indicator for ecosystem health (<xref ref-type="bibr" rid="B4">Ballesteros et&#xa0;al., 2007</xref>). The importance of conserving these areas is highlighted by research describing the ecological value (<xref ref-type="bibr" rid="B16">Chemin&#xe9;e et&#xa0;al., 2013</xref>; <xref ref-type="bibr" rid="B54">Piazzi et&#xa0;al., 2018</xref>; <xref ref-type="bibr" rid="B55">Pinna et&#xa0;al., 2020</xref>) and by habitat level protection under the Barcelona Convention (<xref ref-type="bibr" rid="B65">United Nations Environment Programme/Mediterranean Action Plan (UNEP/MAP), 2013</xref>). Similarly, ecologically valuable seagrass habitats are declining globally (<xref ref-type="bibr" rid="B23">Duarte et&#xa0;al., 2008</xref>; <xref ref-type="bibr" rid="B52">Orth et&#xa0;al., 2006</xref>; <xref ref-type="bibr" rid="B68">Waycott et&#xa0;al., 2009</xref>), including in the Mediterranean Sea (<xref ref-type="bibr" rid="B24">Dunic et&#xa0;al., 2021</xref>; <xref ref-type="bibr" rid="B15">Chefaoui et&#xa0;al., 2018</xref>). <italic>Cymodocea nodosa</italic> (Ucria) Ascherson is one of few seagrass species native to the Mediterranean, and forms highly valuable meadows across its distribution along the Mediterranean and Atlantic coasts (<xref ref-type="bibr" rid="B14">Chefaoui et&#xa0;al., 2016</xref>) and in the Mediterranean, meadows are considered a protected habitat under the Bern Convention (<xref ref-type="bibr" rid="B17">Council of Europe, 2000</xref>). It is projected that a dramatic loss of <italic>C. nodosa</italic> cover will occur over the coming decades (<xref ref-type="bibr" rid="B15">Chefaoui et&#xa0;al., 2018</xref>), despite some potential refuge areas in cooler regions, including the Adriatic Sea, where an increase in cover could occur (<xref ref-type="bibr" rid="B15">Chefaoui et&#xa0;al., 2018</xref>), particularly as the species may replace more vulnerable <italic>Posidonia oceanica</italic> (Linnaeus) Delile meadows under threat (<xref ref-type="bibr" rid="B13">Burgos et&#xa0;al., 2017</xref>).</p>
<p>In the northern Adriatic Sea, a unique cold-temperate bioregion of the Mediterranean (<xref ref-type="bibr" rid="B9">Bianchi and Morri, 2000</xref>), fucalean forests have declined over the past decade, where only a scattering of remnant populations is documented along the Italian (e.g. <xref ref-type="bibr" rid="B39">Mancuso et&#xa0;al., 2018</xref>), Slovenian (e.g. <xref ref-type="bibr" rid="B49">Orlando-Bonaca et&#xa0;al., 2021a</xref>) and Croatian (e.g. <xref ref-type="bibr" rid="B36">Ive&#x161;a et&#xa0;al., 2016</xref>) coastlines that make up this region. Among these isolated forests, the species <italic>Gongolaria barbata</italic> (Stackhouse) Kuntze in particular is commonly observed as a surviving species, an anomaly given a strong regional history of mixed species forests (<xref ref-type="bibr" rid="B35">Ive&#x161;a and Devescovi, 2014</xref>; <xref ref-type="bibr" rid="B36">Ive&#x161;a et&#xa0;al., 2016</xref>). Along the west Istrian Croatian coast, <xref ref-type="bibr" rid="B34">Ive&#x161;a et&#xa0;al. (2022)</xref> have identified a significant remanent population of <italic>G. barbata</italic> in a costal lagoon where it coexists with the seagrass <italic>C. nodosa</italic>. Interestingly, the functionally similar fucoid, <italic>Cystoseira foeniculacea</italic> (Linnaeus) Greville, is also found to persist in a nearby coastal lagoon (Stju&#x17e;a) in Strunjan Bay, Slovenia where it also coexists amongst a high biomass of seagrasses (<italic>C. nodosa</italic> and <italic>Zostera noltei</italic> Hornemann, <xref ref-type="bibr" rid="B6">Battelli and Catra, 2021</xref>, <xref ref-type="bibr" rid="B7">2023</xref>). It is therefore perhaps the case that coastal lagoons can represent local refuges for supporting a high biomass of marine macrophytes and/or interactions between seaweed and seagrasses contribute to their simultaneous persistence in these environments.</p>
<p>&#x160;&#x107;uza Lagoon is 68.6&#xa0;ha in area, has a maximum depth of approximately 1.5m and <italic>C. nodosa</italic> is the dominant habitat forming macrophyte across most of the lagoon as it is dominated by sandy substrate, save for approximately 2&#xa0;ha along the western edge where a shift to rocky/rubble substrate supports a significant settlement of <italic>G. barbata</italic> (<xref ref-type="bibr" rid="B34">Ive&#x161;a et&#xa0;al., 2022</xref>). Historically, &#x160;cuza Lagoon was used as an aquaculture basin and thus was heavily fished but the activity was abandoned, and the lagoon is now protected from such activities under the European Union Natura 2000 guidelines. The lagoon is isolated from the sea due to the construction of a pedestrian footbridge and thus there are a range of biotic and abiotic factors that contribute to its unique environment. Importantly, the thermal range of the lagoon is extreme, where the temperature can dip below zero and reach up to 34&#xb0;C (<xref ref-type="bibr" rid="B34">Ive&#x161;a et&#xa0;al., 2022</xref>). It is therefore quite remarkable that <italic>G. barbata</italic>, with a previously recorded thermal maxima of 23&#xb0;C (throughout the Adriatic Sea, <xref ref-type="bibr" rid="B26">Ercegovi&#x107;, 1952</xref>), thrives here when it is currently rare elsewhere along the coastline (<xref ref-type="bibr" rid="B36">Ive&#x161;a et&#xa0;al., 2016</xref>). In contrast, <italic>C. nodosa</italic> is less sensitive to higher temperatures, which was shown experimentally (<xref ref-type="bibr" rid="B47">Olsen et&#xa0;al., 2012</xref>) and by its widespread distribution (<xref ref-type="bibr" rid="B14">Chefaoui et&#xa0;al., 2016</xref>). The response of both species to extreme cold temperatures is not yet well understood.</p>
<p>It is possible that temporal alternation in the growth cycle of the dominant macrophytes in the lagoon contributes to the coexistence of the two species. <italic>G. barbata</italic> has a diplontic monophasic lifecycle that is typical of fucalean species (<xref ref-type="bibr" rid="B26">Ercegovi&#x107;, 1952</xref>; <xref ref-type="bibr" rid="B58">Rindi et&#xa0;al., 2023</xref> and references therein). Locally, the growth of vegetative branches occurs in the autumn months (<xref ref-type="bibr" rid="B34">Ive&#x161;a et&#xa0;al., 2022</xref>), hypothesized to be triggered by a temperature threshold of ~18&#xb0;C (<xref ref-type="bibr" rid="B10">Bilajac et&#xa0;al., 2024</xref>). During this time, receptacles develop, and fertility is induced in the late winter/early spring when biomass peaks (<xref ref-type="bibr" rid="B34">Ive&#x161;a et&#xa0;al., 2022</xref>; author observations). Annual (branch) material is then lost during the summer months, and the alga enters a &#x201c;dormant phase&#x201d; where perennial material remains and prominent, smooth cauloid apexes are evident. During this time, cauloids can become covered in epiphytes (<xref ref-type="bibr" rid="B34">Ive&#x161;a et&#xa0;al., 2022</xref>) and growth is significantly reduced, particularly at high temperatures (<xref ref-type="bibr" rid="B26">Ercegovi&#x107;, 1952</xref>; <xref ref-type="bibr" rid="B34">Ive&#x161;a et&#xa0;al., 2022</xref>; <xref ref-type="bibr" rid="B10">Bilajac et&#xa0;al., 2024</xref>). <italic>C. nodosa</italic> however, is a flowering marine angiosperm, capable of both sexual and clonal reproduction (<xref ref-type="bibr" rid="B33">Hemminga and Duarte, 2000</xref>), but the strength of either strategy is highly variable and regionally specific (<xref ref-type="bibr" rid="B40">M&#xe1;&#xf1;ez-Crespo et&#xa0;al., 2020</xref>). <italic>C. nodosa</italic> meadows show a high turnover of biomass (<xref ref-type="bibr" rid="B18">Cunha and Duarte, 2007</xref>), can show variations in growth pattern based on depth (<xref ref-type="bibr" rid="B46">Olesen et&#xa0;al., 2002</xref>) but generally peak leaf growth is observed in the summer months (<xref ref-type="bibr" rid="B18">Cunha and Duarte, 2007</xref>; <xref ref-type="bibr" rid="B46">Olesen et&#xa0;al., 2002</xref>; <xref ref-type="bibr" rid="B53">P&#xe9;rez and Romero, 1994</xref>), patterns which have been confirmed for meadows in the northern Adriatic (<xref ref-type="bibr" rid="B12">Bra&#x10d;un et&#xa0;al., 2020</xref>; <xref ref-type="bibr" rid="B48">Orlando-Bonaca et&#xa0;al., 2016</xref>). Epiphytes recruit heavily on older <italic>C. nodosa</italic> leaves throughout the year, which are then shed in the months prior to summer (<xref ref-type="bibr" rid="B11">Bra&#x10d;un et&#xa0;al., 2021</xref>).</p>
<p>Understanding mechanisms that facilitate the survival of any extant <italic>Cystoseira s.l.</italic> forest patches across the Mediterranean provides valuable information for formulating effective conservation practices. The identification of this population is important given its documented decline and current rarity along west Istrian coastline (<xref ref-type="bibr" rid="B36">Ive&#x161;a et&#xa0;al., 2016</xref>) and similarly is under threat in wider Mediterranean (e.g. <xref ref-type="bibr" rid="B63">Thibaut et&#xa0;al., 2015</xref>; <xref ref-type="bibr" rid="B49">Orlando-Bonaca et&#xa0;al., 2021a</xref>; <xref ref-type="bibr" rid="B61">Tamburello et&#xa0;al., 2022</xref>). We hypothesize that the population&#x2019;s unique morphology could provide insight into its persistence here. <xref ref-type="bibr" rid="B27">Falace and Bressan (2006)</xref> demonstrated that the morphology of <italic>G. barbata</italic> can be plastic based on environmental cues. Observationally, &#x160;&#x107;uza&#x2019;s <italic>G. barbata</italic> population shows obvious morphological distinction from other isolated patches found at other sites outside of the lagoon along the west Istrian coastline, possibly suggesting an evolutionary adaptation to the lagoonal environment (<xref ref-type="bibr" rid="B34">Ive&#x161;a et&#xa0;al., 2022</xref>). This could be partially in response to competitive interactions and/or coexistence with <italic>C. nodosa</italic>, as we have not observed this interaction amongst remnant patches elsewhere. Within the lagoon itself there are two growth forms, one where a holdfast attaches to the rocky substrate, as is typical for this species and another &#x201c;detached&#x201d; form that is free floating where the holdfast is absent or non-functional (<xref ref-type="bibr" rid="B34">Ive&#x161;a et&#xa0;al., 2022</xref>). Despite this free-living lifestyle however, the detached form is spatially restricted to the south-western part of the lagoon where it is primarily found trapped amongst seagrass fronds (<xref ref-type="bibr" rid="B34">Ive&#x161;a et&#xa0;al., 2022</xref>). This observation suggests that there may be an interaction between the two dominant macrophytes, however here we focus on the attached form that is present both amongst seagrass and on exposed boulders for comparison.</p>
<p>In this study, the density and maximum thallus height of <italic>G. barbata</italic> was measured <italic>in-situ</italic> using quadrates placed within two distinct settlement habitats (raised submerged rocks outside <italic>C. nodosa</italic> and pebbles embedded within the <italic>C. nodosa</italic> seagrass meadow). Based on observation, we expect that <italic>G. barbata</italic> will grow to a larger maximum height when amongst seagrass compared to when exposed on larger rocky substrates. We aim (1) to test whether the presence of seagrass influences localized settlement and morphology of <italic>G. barbata</italic> and, (2) to document the presence of a unique marking (characterized by a damaged cauloid apex) that is observed among the <italic>G. barbata</italic> population largely within &#x160;&#x107;uza but occasionally outside of the lagoon as well (author observations). Specifically, this study aims to understand the strength of a seaweed-seagrass interaction in influencing population dynamics of a threatened canopy-forming macroalga.</p>
</sec>
<sec id="s2" sec-type="materials|methods">
<title>Materials and methods</title>
<sec id="s2_1">
<title>Benthic cover</title>
<p>&#x160;&#x107;uza Lagoon (44.820377&#xb0;E, 13.889650&#xb0;N), is a sandy coastal lagoon located in the south of the Istrian peninsula (Croatia; <xref ref-type="fig" rid="f1">
<bold>Figure&#xa0;1</bold>
</xref>). To characterize the benthic cover representative of the two settlement substrates, three 20 x 20cm quadrats were placed within areas consisting of either boulder substrate or pebble/unconsolidated substrate within <italic>C. nodosa</italic> meadows (hereafter these groups are referred to as &#x2018;boulder&#x2019; and &#x2018;seagrass&#x2019; respectively). At seven time points throughout the autumn 2022 &#x2013; autumn 2023 (02/11/2022, 15/11/2022, 23/05/2023, 11/08/2023, 15/09/2023, 02/10/2023, 17/10/2023) quadrats were photographed. Benthic cover was quantified using a random point count method (n = 20 points) via coral net (coralnet.ucsd.edu), where organisms that fell under each point were assigned one of the following labels: Algae (including Turf, <italic>G. barbata</italic>, <italic>Valonia</italic> spp., calcified benthic- and macro-algae, <italic>Dictyota</italic> spp., Filamentous green algae and <italic>Rytiphlaea tinctoria</italic> (Clemente) C. Agardh, Ascidian, Seagrass (<italic>C. nodosa</italic>), Hard substrate (bare rock), Loose substrate (pebble and shell grit), Sand, Silt and Other (including tube worms, hydroids/bryozoans, benthic invertebrates and bivalves, anemones and instances where the point fell on the boarder of the quadrat). Benthic composition within boulder compared to seagrasses was tested via permutational multivariate analysis of variance using the <italic>adonis</italic> function in vegan R package (<xref ref-type="bibr" rid="B45">Oksanen et&#xa0;al., 2022</xref>). The analysis was run specifying 9999 permutations and substrate type (boulder or unconsolidated amongst seagrass) and date (n = 7) were fixed factors. The similarity matrix was generated using the Bray-Curtis method and homogeneity of dispersion was checked via the <italic>betadisper</italic> function in vegan. Data were visualized as a biplot generated using the <italic>princomp</italic> function in the R stats package (<xref ref-type="bibr" rid="B56">R Core Team, 2021</xref>).</p>
<fig id="f1" position="float">
<label>Figure&#xa0;1</label>
<caption>
<p>Map showing the northern Adriatic Sea (right plot), highlighting the location of the study site, &#x160;&#x107;uza Lagoon (green dot) on the southern Istrian peninsula, Croatia. Within the Lagoon (left plot), the five sub-areas used for sampling are labelled (A1-5) and the location of the pedestrian footbridge that separates the lagoon from the sea is shown as a dashed line.</p>
</caption>
<graphic mimetype="image" mime-subtype="tiff" xlink:href="fmars-12-1493581-g001.tif"/>
</fig>
</sec>
<sec id="s2_2">
<title>
<italic>G. barbata</italic> population dynamics</title>
<p>The density and growth of <italic>G. barbata</italic> was monitored over the period encompassing autumn 2022 &#x2013; autumn 2023. During the maximum growth period, the population was sampled four times on 04/10/2022, 18/10/2022, 02/11/2022 and 15/11/2022, before anomalously low autumn temperatures and consistently low winter temperatures prevented sampling. We sampled again in the spring of 2023 on 23/05/2023 before unsafe swimming conditions (poor water quality) in the lagoon prevented sampling in early summer. During the later summer during <italic>G. barbata</italic>&#x2019;s minimum growth (dormancy) phase, we sampled the population twice on 11/08/2023 and 15/09/2023, with a final early autumn 2023 sampling period on 02/10/2023. During these sampling efforts, 50 x 50cm quadrats were randomly placed either amongst seagrass or on a boulder (n = 3 per group) and the number of <italic>G. barbata</italic> individuals was counted and the maximum height (base of the holdfast to the tallest point on the algae which could be a vegetative branch or cauloid dependent on season) was recorded following <xref ref-type="bibr" rid="B34">Ive&#x161;a et&#xa0;al. (2022)</xref>. To ensure good spatial representation of the <italic>G. barbata</italic> population and to avoid recounting individuals at each sampling point the lagoon was divided up into five areas that were &gt; 10m apart (<xref ref-type="fig" rid="f1">
<bold>Figure&#xa0;1</bold>
</xref>). At each sampling effort, at least one area was selected, and a full set of quadrats (n = 6) was completed per area.</p>
<p>Analysis of cohorts over the sampling period was conducted as above with height as the response variable. Similarly, when investigating evidence of recruitment, data was filtered to include only individuals that were &lt;3cm and the abundance of individuals that fit this criterion was the model response variable. We consider 3cm as an appropriate cut off to estimate recruitment based on <italic>in situ</italic> observation and published growth trajectories (<xref ref-type="bibr" rid="B59">Savonitto et&#xa0;al., 2021</xref>; <xref ref-type="bibr" rid="B8">Bianchelli et&#xa0;al., 2023</xref>; <xref ref-type="bibr" rid="B38">Lokov&#x161;ek et&#xa0;al., 2023</xref>).</p>
<p>The overall density of <italic>G. barbata</italic> within the two substrate types (boulder; examples <xref ref-type="fig" rid="f2">
<bold>Figures&#xa0;2B, D</bold>
</xref> or seagrass; examples <xref ref-type="fig" rid="f2">
<bold>Figures&#xa0;2A, C</bold>
</xref>) was statistically compared using an ANOVA via the <italic>aov</italic> function in R stats package (<xref ref-type="bibr" rid="B56">R Core Team, 2021</xref>) where the number of individuals was the response variable and substrate type (boulder or unconsolidated amongst seagrass) was a fixed factor. Population density throughout the study period was analyzed using a linear mixed effects model via the <italic>lmer</italic> function in the R package lme4 (<xref ref-type="bibr" rid="B5">Bates et&#xa0;al., 2020</xref>). Number of individuals was the response variable, substrate type (exposed boulder or unconsolidated amongst seagrass) and time (n = 8) were fixed factors and area (1-5) was a random factor. For these analyses and those following, a p value of &lt;0.05 was used to infer statistical significance which was calculated using the <italic>Anova</italic> function in the R package car (<xref ref-type="bibr" rid="B29">Fox et&#xa0;al., 2020</xref>). Where applicable and significant, interactions were observed between model factors, pairwise comparisons were calculated via the <italic>emmeans</italic> function in the emmeans package for R (<xref ref-type="bibr" rid="B37">Lenth et&#xa0;al., 2019</xref>). Model assumptions were visually checked via residuals scatter plots.</p>
<fig id="f2" position="float">
<label>Figure&#xa0;2</label>
<caption>
<p>
<italic>G</italic>. <italic>barbata</italic> growing within the two substrate types: amongst <italic>C</italic>. <italic>nodosa</italic> (seagrass) and on boulders within &#x160;&#x107;uza Lagoon (per horizontal orientation) and during its minimum vs maximum growth periods in summer/autumn and winter/spring respectively (per vertical orientation). <bold>(A)</bold> <italic>G</italic>. <italic>barbata</italic> amongst seagrass during the minimum growth phase, <bold>(B)</bold> <italic>G</italic>. <italic>barbata</italic> growing amongst seagrass during the maximum growth period, <bold>(C)</bold> <italic>G</italic>. <italic>barbata</italic> on a boulder during the minimum growth phase and, <bold>(D)</bold> <italic>G</italic>. <italic>barbata</italic> on a boulder during the maximum growth phase.</p>
</caption>
<graphic mimetype="image" mime-subtype="tiff" xlink:href="fmars-12-1493581-g002.tif"/>
</fig>
<p>During quadrat surveys it was noted where cauloid apices were absent/damaged for individual alga (<xref ref-type="supplementary-material" rid="SM1">
<bold>Supplementary Figure S1</bold>
</xref>). The total number of alga where apices were damaged on boulders or within seagrass at each sampling time was statistically tested via a linear mixed effects model with the frequency of observation (i.e. proportion of individuals where at least one apex was absent) being the response value, substrate type (exposed boulder or unconsolidated amongst seagrass) and time (n = 8) were fixed factors and area (1-5) was a random factor. All other parameters and procedures were run as described above.</p>
</sec>
</sec>
<sec id="s3" sec-type="results">
<title>Results</title>
<sec id="s3_1">
<title>Benthic cover</title>
<p>Boulder substrates were consistently characterized by algae (usually low-lying turfs) and areas of unconsolidated substrate by a high cover of <italic>C. nodosa</italic> (close to 100% at times) with bare loose substrate and sand being more represented during lower growth periods as expected (<xref ref-type="supplementary-material" rid="SM1">
<bold>Supplementary Figure S2</bold>
</xref>). There was a clear distinction in the benthic cover between the substrate types (exposed boulder and unconsolidated substrate amongst seagrass; Pseudo-F<sub>1,75</sub> = 5.005, p = 0.009). Benthic cover also varied based on sampling time (Pseudo-F<sub>1, 75</sub> = 9.739, p &lt; 0.001) as expected given the seasonality in growth of <italic>C. nodosa</italic>, but there was no interaction between substrate type and sampling time (Pseudo-F<sub>1, 75</sub> = -0.512, p = 0.971).</p>
</sec>
<sec id="s3_2">
<title>
<italic>G. barbata</italic> population dynamics</title>
<p>Overall, the density of <italic>G. barbata</italic> individuals per 50 x 50cm quadrat was similar for both boulder and unconsolidated substrates, showing a mean density per 0.25m<sup>2</sup> of 7(&#xb1;1) and 6(&#xb1;1) individuals respectively (<xref ref-type="fig" rid="f3">
<bold>Figure&#xa0;3</bold>
</xref>; F<sub>1,118</sub> = 1.55, p = 0.216). When testing for the effect of sampling time however, density was influenced by the interaction between recruitment substrate and sampling time (<xref ref-type="fig" rid="f4">
<bold>Figure&#xa0;4</bold>
</xref>; Substrate type by time interaction: &#x3c7;<sup>2</sup>=32.93, p&lt;0.001). During September (summer) sampling there were more <italic>G. barbata</italic> individuals counted on boulders compared to among seagrass (<italic>post hoc</italic> pairwise test: p=0.005). The density of <italic>G. barbata</italic> on boulders during the September sampling period was also higher than the density on boulders in early October 2022 (p=0.031) and higher than that amongst seagrass in May (p&lt;0.001) and August (p=0.035).</p>
<fig id="f3" position="float">
<label>Figure&#xa0;3</label>
<caption>
<p>Mean (&#xb1; se) number of <italic>G. barbata</italic> individuals per 50 x 50cm quadrat counted across all lagoon areas (n = 5) and across sampling times (n = 8) from autumn 2022 &#x2013; autumn 2023. Total number of observations = 60 per substrate type; boulder (brown) and unconsolidated amongst seagrass (green).</p>
</caption>
<graphic mimetype="image" mime-subtype="tiff" xlink:href="fmars-12-1493581-g003.tif"/>
</fig>
<fig id="f4" position="float">
<label>Figure&#xa0;4</label>
<caption>
<p>The number of <italic>G. barbata</italic> individuals per 50 x 50cm quadrat counted for each sampling time (n = 8) on boulders (brown) and amongst seagrass (green). At each sampling time there was a minimum of one area sampled and a maximum of four. Within each area there were three boulder, and three seagrass quadrats sampled. The number of areas sampled for each time point was as follows: 4/10/22&#xa0;=&#xa0;2, 18/10/22&#xa0;=&#xa0;4, 2/11/22&#xa0;=&#xa0;4, 15/11/22&#xa0;=&#xa0;3, 23/05/23&#xa0;=&#xa0;2, 11/08/23&#xa0;=&#xa0;2, 15/09/23&#xa0;=&#xa0;2, 2/10/23&#xa0;=&#xa0;1.&#xa0;A total of 120 quadrats was sampled over the whole period, 60 on boulders and 60 amongst seagrass.</p>
</caption>
<graphic mimetype="image" mime-subtype="tiff" xlink:href="fmars-12-1493581-g004.tif"/>
</fig>
<p>
<italic>G. barbata</italic> measured <italic>in situ</italic> ranged in height from a minimum of 0.8cm measured on boulders to 51.5cm measured among seagrass (<xref ref-type="fig" rid="f5">
<bold>Figure&#xa0;5</bold>
</xref>) with a median height of 14.0cm measured across both substrate types. On average, <italic>G. barbata</italic> measured amongst seagrass grew to almost double the maximum height of those measured on boulders (&#x3c7;<sup>2</sup> = 203.94, p &lt; 0.001), with an observed mean of 21.8 (&#xb1;0.6) cm and 12.0 (&#xb1;0.4) cm respectively. As expected by the known lifecycle of <italic>G. barbata</italic>, height was influenced by sampling time (&#x3c7;<sup>2</sup> = 178.60, p &lt; 0.001) where maximum growth was observed during the autumn/winter months and declined towards spring and summer (<xref ref-type="fig" rid="f5">
<bold>Figure&#xa0;5</bold>
</xref>), independent of substrate type (Substrate type x Sampling date interaction: &#x3c7;<sup>2</sup>=13.53, p=0.061).</p>
<fig id="f5" position="float">
<label>Figure&#xa0;5</label>
<caption>
<p>Maximum height measured for <italic>G. barbata</italic> individuals counted <italic>in situ</italic> by sampling time (n = 8) on boulders (brown) and amongst seagrass (green). A total of 808 individuals were measured. At each sampling time there was a minimum of one area sampled and a maximum of four. Within each area there were three boulder, and three seagrass quadrats sampled. The number of areas sampled for each time point were as follows: 4/10/22&#xa0;=&#xa0;2, 18/10/22&#xa0;=&#xa0;4, 2/11/22&#xa0;=&#xa0;4, 15/11/22&#xa0;=&#xa0;3, 23/05/23&#xa0;=&#xa0;2, 11/08/23&#xa0;=&#xa0;2, 15/09/23&#xa0;=&#xa0;2, 2/10/23&#xa0;=&#xa0;1.</p>
</caption>
<graphic mimetype="image" mime-subtype="tiff" xlink:href="fmars-12-1493581-g005.tif"/>
</fig>
<p>During the peak cumulative growth period (early November) there was a clear distinction in the size class distribution of <italic>G. barbata</italic> measured on boulders versus amongst seagrass (<xref ref-type="supplementary-material" rid="SM1">
<bold>Supplementary Figure S3</bold>
</xref>, p &lt; 0.001). 25% of individuals measured amongst seagrass were &gt; 32cm, compared to 8% for those measured on boulders being within this size class and this coincided with the period of low seagrass cover (<xref ref-type="supplementary-material" rid="SM1">
<bold>Supplementary Figure S2</bold>
</xref>). During the lowest cumulative growth period (September 2023), there was a clear shift in the size class distribution, where 24% of individuals on boulders and 5% of individuals measured amongst seagrass were &lt;4cm, coinciding with high seagrass cover (<xref ref-type="supplementary-material" rid="SM1">
<bold>Supplementary Figure S3</bold>
</xref>).</p>
<p>On boulders there was a higher number of smaller individuals (&lt;3cm) compared to amongst seagrass (&#x3c7;<sup>2</sup> = 51.58, p &lt; 0.001) and the spring/summer time points showed a higher number of smaller individuals compared to the autumn/winter time points (<xref ref-type="supplementary-material" rid="SM1">
<bold>Supplementary Figure S3</bold>
</xref>: &#x3c7;<sup>2</sup> = 10.25, p = 0.001). This difference was particularly evident during September sampling (<xref ref-type="supplementary-material" rid="SM1">
<bold>Supplementary Figure S3</bold>
</xref>; <xref ref-type="supplementary-material" rid="SM1">
<bold>Supplementary Table S6</bold>
</xref>).</p>
<p>Independent of sampling time, a higher percentage of <italic>G. barbata</italic> observed on boulders (overall mean of 49.9 &#xb1;4.4%) consistently showed a damaged cauloid apex compared to those amongst seagrass (13.7 &#xb1;2.4%; <xref ref-type="fig" rid="f6">
<bold>Figure&#xa0;6</bold>
</xref>; Substrate type &#x3c7;<sup>2</sup> = 52.87, p &lt; 0.001; substrate type by sampling time interaction &#x3c7;<sup>2</sup> = 2.20, p = 0.139).</p>
<fig id="f6" position="float">
<label>Figure&#xa0;6</label>
<caption>
<p>The percentage of <italic>G. barbata</italic> individuals observed on boulders (brown, n = 433 observations) and amongst seagrass (green, n = 375 observations) showing a damaged cauloid apex. At each sampling time there was a minimum of one area sampled and a maximum of four. Within each area there were three boulder, and three seagrass quadrats sampled. The number of areas sampled for each time point were as follows: 4/10/22&#xa0;=&#xa0;2, 18/10/22&#xa0;=&#xa0;4, 2/11/22&#xa0;=&#xa0;4, 15/11/22&#xa0;=&#xa0;3, 23/05/23&#xa0;=&#xa0;2, 11/08/23&#xa0;=&#xa0;2, 15/09/23&#xa0;=&#xa0;2, 2/10/23&#xa0;=&#xa0;1.</p>
</caption>
<graphic mimetype="image" mime-subtype="tiff" xlink:href="fmars-12-1493581-g006.tif"/>
</fig>
</sec>
</sec>
<sec id="s4" sec-type="discussion">
<title>Discussion</title>
<p>The population dynamics of the ecologically important macroalgal species <italic>G. barbata</italic> are influenced by the presence or absence of the seagrass <italic>C. nodosa</italic> in a coastal lagoon of the northern Adriatic Sea. &#x160;&#x107;uza Lagoon hosts what is potentially one of the last significant populations of <italic>G. barbata</italic> along the western Istrian coastline (Croatia). Understanding the ecological context in which it persists here is valuable for informing targeted conservation and restoration efforts in other locations where it is declining or has been lost. <italic>G. barbata</italic> reached a greater maximum height during its peak growth phase in the autumn/winter months of 2022/23 when living amongst <italic>C. nodosa</italic> compared to when it had settled on exposed boulders. This height advantage was maintained over the spring/summer months in 2023 when only perennial parts of the algae were present, suggesting an adaptation of the entire growth form that is not limited to the seasonal generation of adventitious branch material. We found evidence that recruitment of <italic>G. barbata</italic> was influenced by settlement amongst seagrass compared to on boulders, observing more recruitment to the latter. However, further experimental work would be required to understand the overall similarity in density observed between the two settlement strategies beyond the recruitment stage. Our results support previous work describing the high plasticity in growth forms of <italic>G. barbata</italic> in reponse to localized environmental conditions. In &#x160;&#x107;uza Lagoon, an alternation of peak growth periods likely contributes to the persistence and coexistence of significant populations of ecologically valuable marine macrophytes <italic>G. barbata</italic> and <italic>C. nodosa.</italic>
</p>
<p>Recruitment of <italic>G. barbata</italic> is highly influenced by benthic topography (<xref ref-type="bibr" rid="B21">Devescovi, 2015</xref>), and within &#x160;&#x107;uza Lagoon, it is also possible that boulder substrate provides greater recruitment opportunity comparted to areas dominated by unconsolidated substrate interspersed beneath the seagrass canopy. Amongst seagrass, <italic>G. barbata</italic> settles on small stones and pebbles and other unconsolidated hard substrate that form a secondary benthic substrate layer. A reduced surface area of appropriate recruitment substrate may explain a reduction in the number of small individuals or recruits observed here for the 2022/23 season. Alternatively, low recruitment amongst seagrass could indicate competitive exclusion during the period of peak cover for <italic>C. nodosa</italic> where boulder substrates may provide refuge from such competition. However, the difference in recruitment was not maintained when comparing the overall density, implying that opportunistic recruitment amongst seagrass, while less common, is not a barrier to survival. Amongst <italic>G. barbata</italic> that develop amongst seagrass, it is possible that taller cauloids and heightened branch material observed here is driven by light limitation at the recruit stage enforced by the <italic>C. nodosa</italic> canopy, but this would require further investigation. Nevertheless, such a fine-scale difference in form is consistent with research conducted elsewhere that shows a high degree of morphological variation for <italic>G. barbata</italic> across relatively small geographic ranges (<xref ref-type="bibr" rid="B27">Falace and Bressan, 2006</xref>; <xref ref-type="bibr" rid="B51">Orlando-Bonaca et&#xa0;al., 2022</xref>). Additionally, in &#x160;&#x107;uza Lagoon, amongst the seagrass there are &#x201c;detached&#x201d; individuals that are not fixed to any substrate (author observations). This ecotype was described by <xref ref-type="bibr" rid="B34">Ive&#x161;a et&#xa0;al. (2022)</xref> and is spatially restricted to the south-west of the lagoon but is often found trapped amongst the seagrass meadow or amongst <italic>R. tinctoria</italic> complexes that are also commonly observed amongst seagrasses. This high adaptability in form, coupled with the demonstrated physiological adaptation to extreme thermal conditions for this population (<xref ref-type="bibr" rid="B34">Ive&#x161;a et&#xa0;al., 2022</xref>; <xref ref-type="bibr" rid="B10">Bilajac et&#xa0;al., 2024</xref>), suggests a resilience worth investigating in the context of its long-term survival and its potential as a donor population for fucalean restoration along the broader coastline.</p>
<p>Damage to perennial cauloid apices is an observed feature among <italic>Cystoseira s.l.</italic> species along the western Istrian coast which was also observed for <italic>G. barbata</italic> within &#x160;&#x107;uza Lagoon (author observations). This feature was consistently recorded more frequently amongst individuals that had settled on boulders compared to those settled amongst seagrass, even in the summer months when cauloids host a high epiphyte biomass that conceal some such markings. It is possible that this feature is a sign of herbivory, however outside of the lagoon, where urchins are present, cauloid damage of this nature is also frequently observed. The herbivorous fish <italic>Sarpa salpa</italic> is present within and outside of the lagoon and is a voracious grazer of <italic>Cystoseira s.l</italic> (<xref ref-type="bibr" rid="B67">Verg&#xe9;s et&#xa0;al., 2009</xref>; <xref ref-type="bibr" rid="B31">Gianni et&#xa0;al., 2017</xref>; <xref ref-type="bibr" rid="B51">Orlando-Bonaca et&#xa0;al., 2022</xref>, <xref ref-type="bibr" rid="B50">2021</xref>). However, <italic>S. salpa</italic> is not strictly herbivorous throughout its lifecycle (<xref ref-type="bibr" rid="B22">Dobroslavi&#x107; et&#xa0;al., 2012</xref>; <xref ref-type="bibr" rid="B32">Havelange et&#xa0;al., 2008</xref>) and can also target <italic>C. nodosa</italic> and its epiphyte load for feeding (<xref ref-type="bibr" rid="B42">Marco-M&#xe9;ndez et&#xa0;al., 2017</xref>) and further investigation would be needed to better understand this interaction. It is also possible that herbivorous invertebrates could also graze on <italic>G. barbata</italic> in &#x160;&#x107;uza Lagoon, and this is an important consideration given that early life stage <italic>Cystoseira s.l.</italic> species are susceptible to invertebrate grazing (<xref ref-type="bibr" rid="B43">Monserrat et&#xa0;al., 2023</xref>). However, this would not necessarily explain damaged cauloid apices observed for adult individuals. The ecological significance of damaged cauloid apices, the ecological relevance of seagrasses providing protection from it here and its prevalence amongst <italic>Cystoseira s.l</italic> populations elsewhere warrants further investigation.</p>
<p>Understanding the mechanisms that allow the survival of remnant marine forests is of increasing conservation importance because harnessing any observable positive interactions within extant forests may benefit conservation efforts. In &#x160;&#x107;uza Lagoon it is likely crucial that there are very few sea urchins observed (<xref ref-type="bibr" rid="B34">Ive&#x161;a et&#xa0;al., 2022</xref>), contributing to the observed abundance of both <italic>G. barbata</italic> and <italic>C. nodosa</italic> as both species are susceptible to urchin overgrazing (<xref ref-type="bibr" rid="B1">Agnetta et&#xa0;al., 2015</xref>; <xref ref-type="bibr" rid="B19">Cvitkovi&#x107; et&#xa0;al., 2024</xref>; <xref ref-type="bibr" rid="B28">Fernandez et&#xa0;al., 2012</xref>; <xref ref-type="bibr" rid="B30">Giakoumi et&#xa0;al., 2012</xref>; <xref ref-type="bibr" rid="B36">Ive&#x161;a et&#xa0;al., 2016</xref>; <xref ref-type="bibr" rid="B44">Nikolaou et&#xa0;al., 2023</xref>; <xref ref-type="bibr" rid="B64">Thibaut et&#xa0;al., 2005</xref>). In the context of at risk marine algal forests, there is increasing evidence for the role of habitat refugia (such as coastal lagoons, rockpools and microstructures) in providing refuge from herbivory and thus supporting the survival of isolated patches of canopy forming seaweeds (<xref ref-type="bibr" rid="B6">Battelli and Catra, 2021</xref>; <xref ref-type="bibr" rid="B69">Zarco-Perello et&#xa0;al., 2021</xref>; <xref ref-type="bibr" rid="B43">Monserrat et&#xa0;al., 2023</xref>) and long-term exclusion of over-abundant grazers is currently a major roadblock to the success of marine forest restoration in the Mediterranean (<xref ref-type="bibr" rid="B66">Verdura et&#xa0;al., 2023</xref>) and worldwide (<xref ref-type="bibr" rid="B25">Eger et&#xa0;al., 2022</xref>). Furthermore, water quality and excessive nutrient input has been shown to cause large-scale negative impacts on <italic>Cystoseira s.l.</italic> populations in the past (<xref ref-type="bibr" rid="B36">Ive&#x161;a et&#xa0;al., 2016</xref>), and for &#x160;&#x107;uza Lagoon the impact of nutrient input and fluctuations in water chemistry caused by nearby terrestrial activity is unknown yet makes the survival of the forest here more notable. It is important to study the ecology of persistent populations of at-risk species to understand any adaptive mechanisms that may be important considerations for conservation efforts. In the case of &#x160;&#x107;uza Lagoon, here we show that the adaptability of <italic>G. barbata</italic>, even at the micro-environment level may contribute to its survival in a unique lagoonal environment.</p>
</sec>
</body>
<back>
<sec id="s5" sec-type="data-availability">
<title>Data availability statement</title>
<p>The raw data supporting the conclusions of this article will be made available by the authors, without undue reservation.</p>
</sec>
<sec id="s6" sec-type="author-contributions">
<title>Author contributions</title>
<p>SS: Conceptualization, Data curation, Formal analysis, Methodology, Writing &#x2013; original draft, Writing &#x2013; review &amp; editing. AB: Conceptualization, Data curation, Methodology, Writing &#x2013; review &amp; editing. EG: Conceptualization, Data curation, Methodology, Writing &#x2013; review &amp; editing. MN: Methodology, Supervision, Writing &#x2013; review &amp; editing. LI: Conceptualization, Data curation, Funding acquisition, Methodology, Supervision, Writing &#x2013; review &amp; editing, Project administration.</p>
</sec>
<sec id="s7" sec-type="funding-information">
<title>Funding</title>
<p>The author(s) declare that financial support was received for the research and/or publication of this article. This project was funded by Croatian Science Foundation project: The response of habitat forming brown macroalgae of the genus Cystoseira on local and global stressors (grant no. IP-2019-04-6984) and by the European Union through the project BRIGANTINE: Chemico-physical and multispectral data fusion for Adriatic Sea monitoring by autonomous vessel (INTERREG Italy-Croatia Program 2021-2027, grant no. ITHR0200237).</p>
</sec>
<ack>
<title>Acknowledgments</title>
<p>The authors thank three reviewers for their valuable feedback on an earlier version of the manuscript.</p>
</ack>
<sec id="s8" sec-type="COI-statement">
<title>Conflict of interest</title>
<p>The authors declare that the research was conducted in the absence of any commercial or financial relationships that could be constructed as a potential conflict of interest.</p>
</sec>
<sec id="s9" sec-type="disclaimer">
<title>Publisher&#x2019;s note</title>
<p>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.</p>
</sec>
<sec id="s10" sec-type="supplementary-material">
<title>Supplementary material</title>
<p>The Supplementary Material for this article can be found online at: <ext-link ext-link-type="uri" xlink:href="https://www.frontiersin.org/articles/10.3389/fmars.2025.1493581/full#supplementary-material">https://www.frontiersin.org/articles/10.3389/fmars.2025.1493581/full#supplementary-material</ext-link>
</p><supplementary-material xlink:href="DataSheet1.docx" id="SM1" mimetype="application/vnd.openxmlformats-officedocument.wordprocessingml.document"/>
</sec>
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