Are the Consequences If Some Algal Species Are Lost? Saarinen, Anniina; Salovius-Lauren, Sonja; Mattila, Johanna

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Are the Consequences If Some Algal Species Are Lost? Saarinen, Anniina; Salovius-Lauren, Sonja; Mattila, Johanna This is an electronic reprint of the original article. This reprint may differ from the original in pagination and typographic detail. Epifaunal community composition in five macroalgal species - What are the consequences if some algal species are lost? Saarinen, Anniina; Salovius-Lauren, Sonja; Mattila, Johanna Published in: Estuarine, Coastal and Shelf Science DOI: 10.1016/j.ecss.2017.08.009 Publicerad: 01/01/2018 Document Version (Referentgranskad version om publikationen är vetenskaplig) Document License CC BY-NC-ND Link to publication Please cite the original version: Saarinen, A., Salovius-Lauren, S., & Mattila, J. (2018). Epifaunal community composition in five macroalgal species - What are the consequences if some algal species are lost? Estuarine, Coastal and Shelf Science, 207, 402–413. https://doi.org/10.1016/j.ecss.2017.08.009 General rights Copyright and moral rights for the publications made accessible in the public portal are retained by the authors and/or other copyright owners and it is a condition of accessing publications that users recognise and abide by the legal requirements associated with these rights. Take down policy If you believe that this document breaches copyright please contact us providing details, and we will remove access to the work immediately and investigate your claim. This document is downloaded from the Research Information Portal of ÅAU: 11. Oct. 2021 1 1 Epifaunal community composition in five macroalgal species – what 2 are the consequences if some algal species are lost? 3 1 4 Corresponding author: Anniina Saarinen a 5 Affiliation address: a Husö biological station, Environmental and Marine Biology, Faculty of 6 Science and Engineering, Åbo Akademi University, Tykistökatu 6, FI-20520 Turku, Finland 7 [email protected] 8 Present address: 1 County Administrative Board of Västerbotten, Storgatan 71 B, SE-903 30, Umeå, 9 Sweden 10 11 Second author: Sonja Salovius-Laurén a 12 Affiliation address: a Husö biological station, Environmental and Marine Biology, Faculty of 13 Science and Engineering, Åbo Akademi University, Tykistökatu 6, FI-20520 Turku, Finland 14 [email protected] 15 2 16 Third author: Johanna Mattila a 17 Affiliation address: a Husö biological station, Environmental and Marine Biology, Faculty of 18 Science and Engineering, Åbo Akademi University, Tykistökatu 6, FI-20520 Turku, Finland 19 Present address: 2 Department of Aquatic Resources, Division of Coastal Research, Swedish 20 University of Agricultural Sciences, Skolgatan 6, SE-742 42 Öregrund, Sweden 21 [email protected] 22 23 24 2 25 Abstract 26 Anthropogenic disturbances such as eutrophication and climate change are affecting the distribution 27 and coverage of macroalgae in coastal areas worldwide. How these changes will affect the littoral 28 food webs is challenging to predict as we still lack basic knowledge of epifaunal communities in 29 different macroalgal species. The aim of this study was therefore to compare the epifauna in five 30 common macroalgal species in the northern Baltic Sea. Samples of macroalgae and the associated 31 epifauna were collected in mesh bags at 2 m depth in July-August 2014. The epifaunal abundance 32 data were analyzed with univariate and multivariate methods. The results revealed significant 33 differences in the epifaunal composition among the studied macroalgal species. Ceramium 34 tenuicorne hosted the significantly highest and Fucus vesiculosus the lowest abundance of epifauna 35 per algal dry weight. When comparing the relative epifaunal abundances in percentage, we found 36 that different epifaunal taxa representing different functional groups dominated Pylaiella littoralis 37 (Chironomidae, deposit feeder), Cladophora rupestris (Gammarus spp., herbivorous/omnivorous) 38 and Furcellaria lumbricalis (Mytilus trossulus, suspension feeder). However, most of the epifaunal 39 taxa were found in all algal species studied. We conclude that the loss or decline of specific 40 macroalgal species will affect the ecosystem functions and energy flows to the higher trophic levels, 41 but that none of the studied algal species seems to be crucial for the existence of single taxa or 42 functional group of epifauna. 43 44 Key words: epifaunal taxa, abundance; functional groups, eutrophication, rocky shores, Baltic Sea, 45 N 60 ̊ E 19 ̊ 46 3 47 1. Introduction 48 Macroalgae are important primary producers along rocky shores worldwide (Ryther, 1963; Mann, 49 1973; Littler and Murray, 1974) and offer habitats for a variety of marine organisms (Seed and 50 O’Connor, 1981; Norderhaug et al., 2005; Christie et al., 2009). They also contribute to several 51 ecosystem services such as nutrient cycling, CO2 capture and storage as well as in maintaining the 52 fish stocks by providing nursery and foraging grounds (Costanza et al., 1997; Rönnbäck et al., 53 2007). The invertebrates living on the algae, epifauna, form an important linkage to higher trophic 54 levels, as they serve as food for fish (Norderhaug et al., 2005; Eriksson et al., 2009) and birds 55 (MacNeil et al. 1999), as well as affect the host algae by consuming it fresh (Himmelman and 56 Steele, 1971; Jormalainen et al., 2001) or as particulate organic matter (Norderhaug et al., 2003). 57 Grazing may even help to distribute algal spores (Buschmann and Bravo, 1990) and the 58 consumption of diatoms and epiphytic algae from the surface of the host algae enhances the host 59 algae’s photosynthesis and growth (Brönmark, 1985; Karez et at., 2000). 60 61 A variety of abiotic and biotic factors determine the composition of epifauna associated with 62 macroalgae. Of the macroalgal characteristics, morphological complexity and the available surface 63 area of an alga are often seen as primarily structuring the epifaunal community (Lippert et al., 2001; 64 Parker et al., 2001; Christie et al., 2009; Nordenhaug et al., 2014). Nevertheless, macroalgal species 65 also differ in longevity and chemical composition and the associated epifauna differ in their 66 functional characteristics (e.g. Jansson et al., 1982; Steneck and Watling, 1982) such as in size, life 67 cycle and feeding traits. Therefore, it is not surprising that for some epifauna, a specific macroalgal 68 species may offer a better shelter from predation (Hacker and Madin, 1991; Svensson et al., 2004; 69 Wernberg et al., 2013) and wave action (Fenwick, 1976; Prathep et al., 2003), better food sources 70 (Orav-Kotta and Kotta, 2003; Poore, 2004; Orav-Kotta et al., 2009), places for larval settlement 71 (Seed et al., 1981) or material for nest building (Brennan and Mclachan, 1979; Råberg and Kautsky, 4 72 2007). Indeed, studies worldwide have shown that epifaunal community composition varies 73 between different macroalgal species, but the epifauna are rarely dependent on any single algal 74 species (Taylor and Cole, 1994; Lippert et al 2001; Parker et al., 2001; Kraufvelin and Salovius, 75 2004; Bates and DeWreede 2007). 76 77 Information on the relationship between different algal species and associated epifaunal 78 assemblages is needed to predict future changes in the food webs as the macroalgal communities 79 change due to eutrophication (Kangas et al., 1982; Rönnberg et al., 1985; Schramm and Nienhuis, 80 1996), overfishing of predatory fish (Eriksson et al., 2009; Jackson et al., 2001), changing climate 81 (Harley et al., 2012; Jueterbock et al., 2013; Svensson, 2015) and several other human-induced 82 disturbances such as introduced species (Jormalainen et al., 2016), and trampling and harvesting 83 (Crowe et al., 2000). Furthermore, EU’s Marine Strategy Framework Directive requires the member 84 states to address the lack of knowledge of different components of the marine ecosystems such as 85 the macroalgae and benthic invertebrates to be able to develop indicators for measuring potential 86 changes and to protect, preserve and restore the marine environment (European commission, 2008). 87 88 In addition to climate change, eutrophication is considered as one of the biggest threats to the 89 macroalgal communities in the Baltic Sea, since it results in shifts in the macroalgal composition 90 from perennial species, such as bladder wrack Fucus vesiculosus (L., 1753), to ephemeral fast 91 growing filamentous species such as Pylaiella littoralis (L., Kjellman 1872) (Kangas et al., 1982; 92 Kautsky et al., 1986; Eriksson et al., 1998). Predicted elevated sea water temperatures (Jueterbock 93 et al., 2013) and decreasing salinity (Philippart et al., 2011) due to climate change, will likely 94 decrease the distribution of marine algal species such as fucoids (Jueterbock et al., 2013) and 95 increase the primary production and distribution of filamentous green algae such as Cladophora 96 glomerata (L., Kützing 1843) (Svensson, 2015). The decline of predatory fish in the Baltic Sea has 5 97 also been shown to promote bloom forming macroalgae as a result of decreased invertebrate grazer 98 control (Eriksson et al., 2009). These human-induced changes in the macroalgal communities are 99 likely to affect the associated epifauna as well as higher trophic levels (Pihl et al., 1995; Råberg and 100 Kautsky, 2007; Wikström and Kautsky, 2007). Consequently, we need to predict what happens to 101 epifaunal communities if some macroalgal species decline or are even lost from the ecosystem. The 102 decline of F. vesiculosus and changes in its epifaunal community are of high concern as F. 103 vesiculosus is considered as a key species in the ecosystem hosting a diverse assemblage of 104 epifauna and epiphytes and functioning as a spawning, breeding and foraging ground for fish 105 (Jansson et al., 1982; Kautsky et al., 1992). However, only few studies have compared F. 106 vesiculosus associated epifauna to epifauna associated with other macroalgal species (Kraufvelin 107 and Salovius, 2004; Zander et al., 2015). Furthermore, these studies have compared the epifauna of 108 belt forming algal species from different depths and consequently affected by varying exposure to 109 waves, that is known to affect the epifaunal diversity (Norderhaug et al., 2012) as well as secondary 110 production of mobile epifauna (Norderhaug and Christie, 2011).
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