In recent decades, mounting evidence suggests that biological invasions by invasive (also called alien or non-native) species are a growing threat to global biodiversity, and is exacerbated by climate warming
[1][2]. Globalization, the transformation of technological regimes and expansions of transportation networks which modify the marine habitats are other recognized drivers behind the rapid shifting of invasive species across a broad geographical range
[3][4][5]. In a narrower sense, species invasions can adversely influence the dynamics of specific communities, particularly concerning the extirpation of native species
[6][7] and the reduction of species richness
[8]. Climate, recipient communities, and invaders are considered the prime determinants of invasion impacts, with the characteristics of recipient communities being the most critical determinant
[9]. The mechanisms of invasion impact on the diversity of native species, however, are still not well understood and in fact, previous findings on invasion consequences for species richness have been contradictory; viz., either positive, negative, neutral, or multifarious impacts
[9]. This invasion paradox has led to many controversial debates over the past two decades
[10]. The diversity and impact of invasive species on marine ecosystems are extensively covered in a recent review by Salimi et al. (2021)
[11].
Studies on aquatic ecosystems showed that the interactions between marine herbivores and various plants and/or algae (hereinafter referred to as the “autotrophs”) could reduce or even prevent the detrimental impacts of species invasions
[12][13]. Lyons and Scheibling
[14] reported that the establishment of the invasive green algae
Codium fragile was enhanced by sea urchin food preference for kelps under increased water temperature and wave action, leading to increased herbivore pressure on local kelp stands. By and large, generalist marine herbivores such as most fishes and sea urchins that feed on autotrophs are common biological control agents that suppress the establishment and abundance of invasive species in the recipient communities
[15][16]. It has been reported that the feeding (or grazing) preferences of the herbivores can determine the relationship between native or invasive autotrophs
[17][18]. Recent findings also suggested that mechanisms underlying autotroph palatability could help resolve the inconsistent results of novelty
[19][20].
Since the 1980s, efforts have been undertaken to understand the foraging behaviour of generalist marine herbivores
[21][22][23][24]. Their selective foraging behaviour, which aims chiefly to regulate their nutritional needs for growth, fecundity, and performance
[25][26], has been found to exert a profound impact on the biological structure of many marine ecosystems
[27]. As such, theoretic insights on the nutritional relationships between herbivores and autotrophs will assist in the control and management of invasive species
[28][29][30]. Generalist herbivores have also been found to make their food selection based on autotroph palatability, which depends primarily on their other unique attributes including, among others, secondary metabolites, morphology and physical stress
[31][32][33][34][35]. Significant research has been devoted to examining the role and importance of some secondary metabolites in the survival and adaptation of autotrophs
[36][37][38], but less attention has been paid to dissecting the value of their other attributes that may also influence the preferences of herbivores, i.e., whether to feed on native or invasive plants, or both
[12]. It is worth noting that autotrophic characteristics may have the opposite effect on autotroph-herbivore interactions in controlled experimental studies where herbivores are restricted to a single autotroph species than in effects seen in field studies where herbivores are free to move around and cause natural autotroph damage. Future research examining the significance of autotroph features in interactions between autotrophs and herbivores must therefore carefully take into account the context in which the relationships have been observed
[19].
2. Marine Algae and Their Unique Attributes
Algae are the ultimate source of nutrients and energy for other organisms living in aquatic ecosystems. Although not considered plants, algae are photosynthetic in nature and produce over 70% of the global oxygen content
[39][40][41]. Algae are also effective at sequestering carbon by converting almost 50% of the atmospheric carbon dioxide into organic molecules that build essential cellular constituents and intensify their energy production
[42][43][44][45][46]. Macroalgae, being the most important primary producers in the oceans, house a wide range of nutritional quality within and among groups which often influences their palatability to herbivores
[25][47]. For the most part, the proteins in macroalgae contain important amino acids, particularly the ones that cannot be synthesized by the animal body
[48][49]. Animal hosts can thus obtain all these essential amino acids through symbiosis with the algae
[50]. A variety of macroalgae reproduce either exclusively sexually or asexually, whilst some species demonstrate an alternation of generations involving both reproductive strategies in succession
[51][52][53]. The following subsections discuss the unique characteristics and ecological relationships of each major group of macroalgae, including red algae (Rhodophytes), brown algae (Phaeophytes), and green algae (Chlorophytes)
[45][46].
Figure 1 depicts the three major groups of macroalgae and examples of their common species.
Figure 1. Major groups of macroalgae and examples of their common species.
2.1. Red Algae (Division Rhodophyta)
The first group is the eukaryotic red algae, or the Rhodophytes, comprising more than 6000 species of primarily marine algae ranging from microscopic to macroscopic in size
[54][55]. These algae store their energy as a specialized polysaccharide, known as floridean starch, and their cell walls are made of unique cellulose and polysaccharides, such as agars and carrageenan galactans
[56][57][58]. However, some other red algae may adopt sulfated mannans or neutral xylans as the main cell wall components rather than carrageenans
[57]. Their photosynthetic pigments include chlorophylls
a and
d, while their accessory pigments are carotenoids, phycobilins, and xanthophyll
[54][59][60] (
Table 1). Some notable examples of red algae are, among others, filamentous species like
Pleonosporum spp. and coralline algae like
Porolithon spp., which contribute significantly to the building of tropical reefs and thalloid species. It is worth noting that the red algae have no flagellated cells or cells with any vestigial structure of flagellation
[20]. Irish moss (
Chondrus crispus Stackhouse), also known as the carrageen moss, is an example of an economically important red alga which has been used to bind proteins together to stabilize and add texture to various foods and beverages like ice cream, yogurt, and deli meats
[61][62]. Another economically and nutritionally important species of red algae is nori (
Porphyra umbilicalis Kützing); a high-protein and high-fibre algae which is commonly used in Japanese cuisine as an ingredient to wrap sushi
[63].
Porphyra was proved to have the greatest protein content (ca. 35%) among the marine macroalgae, while some members of the brown algae in the order Laminariales have the lowest content (ca. 7%)
[64][65].
Table 1. Major groups of macroalgae and their attributes.
2.2. Brown Algae (Division Chromophyta)
In contrast to other algal groups, brown algae or the Phaeophytes are mostly developed from a secondary endosymbiosis event which involved a non-photosynthetic eukaryote and a unicellular red alga. Resultantly, brown algae exhibit several morphological and metabolic features that make them the most complex macroalgae
[66]. Phaeophytes are mostly macroscopic in size, inclusive of the giant kelp (
Macrocystis pyrifera (Linnaeus) C.Agardh), which can grow up to 10 m in length
[67]. Most of the approximately 1800 species of brown algae live in the marine environment, especially in cool temperate waters located in both the Northern and Southern Hemispheres
[68][69]. Fucans and alginates are the specific polysaccharides compounds, which can be found in the cell wall of brown algae
[66]. Generally, brown algae consist of three distinctly recognizable parts–the holdfast, stipe, and leaf-like blades
[70]. The holdfast is a root-like structure at the bottom, which is often joined by a stipe to one or more leaf-like blades depending on the species. The blades serve as the primary surface for important processes including photosynthesis and nutrient exchange in the algae
[71][72]. Although photosynthesis takes place predominantly in the blades, it is crucial that the stipe has the adequate length to place the blades sufficiently close to the light source. Alternatively, algae can absorb sufficient light by swelling the body (thallus) or increasing their growth rate
[73]. The photosynthetic pigments in brown algae are chlorophylls
a and
c, and their accessory pigments include carotenoids and xanthophylls
[74] (
Table 1). Fucoxanthin contains brown-coloured pigment and the unique xanthophyll in brown algae which gives them their characteristic dark colour
[75]. Unlike red algae, most of the brown algae have two flagella which help them achieve locomotion
[76]. Some examples of brown algae include the rockweeds (
Ascophyllum spp. and
Fucus spp.) and the giant kelps (
Macrocystis sp.). These algae usually contain laminarin and mannitol, storage sugars which can be fermented to make alcohol
[77]. Some brown algae possess the ability to take up certain important substances from seawater. For instance, the iodine concentration in an edible kelp, kombu, can be thousands of times as great in the cells of the species as in its surrounding water
[78].
2.3. Green Algae (Division Chlorophyta)
On the other hand, green algae or the Chlorophytes are generally more closely related to the higher plants in comparison to brown and red algae, in particular their chloroplast structure
[79][80]. The cell walls of most species of green algae are built mainly by cellulose, with some incorporation of glycans (hemicelluloses)
[81]. Their photosynthetic pigments in the chloroplast are chlorophylls
a and
b, while their accessory pigments are carotenoids and xanthophylls, found in embryophytes
[81] (
Table 1). Green algae comprise of 9000 to 12,000 species, with the majority of them occurring in freshwater rather than the marine environments
[80][81]. Most green algae are microscopic, except for a small number of species in some specific genera such as those in
Cladophora which are multicellular and macroscopic
[81][82][83]. The unicellular genera
Chlamydomonas and
Chlorella are some common examples of green algae in both marine and freshwater ecosystems worldwide, which consist of species that disperse in a wide range of habitats
[84]. An example of more complex green algae includes
Volvox, which forms large hollow-spherical colonies that consist of thousands of cells
[85]. The green algae
Ulva spp.,
Caulerpa spp.,
Enteromorpha spp., and
Codium spp. are commonly used as a food source for humans. The
Ulva spp., known generally as sea lettuce, are extensively consumed in many Asian countries especially in Japan, China, and the Republic of Korea
[80][86]. Access to nitrogen is one of the major limiting factors in the growth of green algae on the grounds that most of them thrive in shallow water
[87]. Nevertheless, the increased runoff of fertilizer-related nitrogen into the oceans, mainly from agriculture has created favourable conditions for the growth of green algae and also other groups of algae in the past few decades
[88]. According to Lee (2018), the majority of green algae form zoogametes, which are motile flagellated gametes
[20]. The review by Moreira et al. (2021) details how macroalgae from various divisions differ in their flagellal construction, orientation, and life cycle in general
[83].