1. Introduction
Aquatic ecosystems are often described as highly interconnected systems, yet that description only partially captures their actual complexity. Beneath the visible interactions among fish, plankton, and aquatic vegetation lies a constantly shifting network of microbial activity, nutrient exchange, trophic regulation, and environmental feedback mechanisms that together determine ecosystem stability and productivity. For decades, ecologists attempted to simplify these interactions into relatively linear pathways of energy transfer. Early ecological theories, particularly those developed through classical food-chain concepts, established the foundation for understanding predator–prey relationships and ecological succession within aquatic environments (Elton, 1927). Later, trophic-dynamic perspectives expanded this understanding by emphasizing energy movement across trophic levels and ecological efficiency within food webs. Even so, many early frameworks assumed that trophic boundaries were relatively rigid, an assumption that increasingly appears inadequate when considering the remarkable feeding flexibility observed across aquatic organisms.
Modern aquatic ecology instead recognizes trophic systems as fluid and highly responsive to environmental conditions. Organisms rarely occupy a single ecological role throughout their life history. Seasonal nutrient variability, habitat alteration, prey availability, and environmental stress can all reshape trophic interactions in ways that are difficult to predict using traditional food-chain models alone. Continuous trophic position approaches therefore emerged as a more realistic framework for interpreting feeding dynamics, especially in ecosystems where omnivory, microbial recycling, and detrital pathways significantly influence nutrient transfer and energy flow (Post, 2002). Such ecological flexibility appears especially important in marine and freshwater ecosystems where planktonic organisms frequently alternate between multiple ecological functions depending on environmental context.
Among these organisms, zooplankton occupy a particularly influential position within aquatic food webs. They form the essential biological bridge connecting primary producers with higher trophic consumers such as fish, seabirds, and marine mammals (Lomartire et al., 2021). Yet, their ecological significance extends well beyond simple grazing activity. Copepods and other planktonic taxa increasingly are recognized as biological microhabitats supporting complex bacterial and fungal assemblages that contribute directly to nutrient recycling and dissolved organic matter transformation (Feng et al., 2023). In many respects, these microbial associations reshape the classical understanding of pelagic food webs by revealing how microorganisms contribute not only to decomposition processes but also to ecosystem productivity itself.
This understanding aligns closely with the concept of the microbial loop, now widely considered one of the defining paradigms in aquatic ecology. The microbial loop explains how dissolved organic carbon, rather than remaining unavailable within aquatic systems, can be recycled by bacteria and subsequently transferred back into higher trophic pathways through protozoa and microzooplankton grazing (Azam et al., 1983). This process effectively reconnects microbial metabolism with broader ecosystem productivity. Particularly under oligotrophic or nutrient-limited conditions, microbial recycling may become a major determinant of ecosystem resilience and carbon retention (Calbet & Landry, 2014). Moreover, zooplankton-mediated carbon transport contributes significantly to biological carbon sequestration, linking trophic ecology with global biogeochemical cycles and climate regulation (Steinberg & Landry, 2017).
At the same time, aquatic ecosystems are increasingly exposed to environmental pressures capable of destabilizing these delicate trophic relationships. Climate change remains perhaps the most pervasive driver of ecological transformation across freshwater and marine systems. Rising temperatures alter stratification patterns, oxygen availability, nutrient circulation, and hydrological dynamics, often producing cascading ecological consequences. Long-term warming trends in marine systems have already been associated with substantial shifts in copepod abundance and diversity, particularly within the North Atlantic region (Beaugrand, 2003). Similar processes occur in stratified lakes and fjords, where reduced vertical mixing can suppress nutrient redistribution and ultimately limit primary productivity.
These climate-driven alterations may also weaken ecological resilience by disrupting microbial and planktonic community structure. Ecological network analyses increasingly suggest that disturbed ecosystems often exhibit reduced connectivity and lower resistance to species loss (Forster et al., 2021). Such vulnerability becomes even more concerning when combined with additional stressors including invasive species, eutrophication, and chemical pollution.
Biological invasions now represent one of the major threats to aquatic biodiversity worldwide. Invasive organisms frequently alter trophic interactions through competition, predation, and habitat restructuring, often producing ecosystem-level consequences that extend far beyond direct species displacement (Molnar et al., 2008). Arctic marine ecosystems, for example, have experienced notable trophic restructuring following the expansion of the invasive snow crab, Chionoecetes opilio, which has modified benthic feeding relationships and altered energy pathways within fjord ecosystems (Zalota et al., 2024). Such ecological changes can gradually destabilize native food webs, particularly when ecosystems are already under pressure from climate-driven environmental shifts. More broadly, invasive species have become increasingly recognized not merely as isolated ecological disturbances but as long-term drivers of ecosystem transformation requiring active management and monitoring (Simberloff, 2013).
Chemical pollutants further complicate trophic interactions within aquatic systems. Pharmaceuticals, pesticides, and industrial contaminants now enter aquatic habitats at unprecedented rates through wastewater discharge, agricultural runoff, and urban development. Even when present at relatively low concentrations, these compounds may induce subtle but ecologically meaningful changes in microbial metabolism, reproductive biology, and predator–prey interactions. Antidepressants such as paroxetine, for instance, have been shown to influence benthic microbial food webs and nitrogen cycling processes through indirect trophic effects (Li et al., 2022). Such findings highlight a broader ecological concern: environmental contaminants often produce cascading ecosystem responses that extend well beyond direct toxicity alone.
Another increasingly important environmental challenge involves harmful algal blooms (HABs), particularly cyanobacterial blooms intensified by nutrient enrichment and climate warming. Cyanobacteria employ a range of defensive strategies, including toxin production and colony formation, that reduce zooplankton grazing efficiency and alter trophic transfer within aquatic food webs (Moustaka-Gouni & Sommer, 2020). Experimental studies further suggest that toxic cyanobacteria can substantially modify zooplankton feeding behavior, reproductive performance, and survival patterns (Nandini & Sarma, 2023). Earlier laboratory investigations similarly demonstrated that cyanobacteria often impair zooplankton growth and grazing efficiency through both physical and biochemical mechanisms (Lampert, 1987).
Cyanotoxins such as microcystins and cylindrospermopsin have also become a growing concern because of their ability to move through aquatic food webs. Some toxins may undergo biodilution, whereas others appear capable of bioaccumulating within mollusks, crustaceans, and fish, potentially creating ecological and public health risks (Ferrão-Filho & Kozlowsky-Suzuki, 2011). Freshwater organisms consumed by humans may therefore act as vectors for toxin exposure, emphasizing the importance of toxin monitoring and ecological risk assessment (Ibelings & Chorus, 2007). Cylindrospermopsin accumulation has even been documented in crayfish and other aquatic consumers, illustrating the potential for long-term trophic transfer (Saker & Eaglesham, 1999; Kinnear, 2010). In parallel, marine cyanobacterial symbioses continue to reveal additional ecological complexity associated with toxin production, nutrient cycling, and microbial interactions (Mutalipassi et al., 2021).
Advances in analytical technologies have substantially improved our ability to investigate these complex ecological processes. Molecular approaches such as DNA metabarcoding and environmental DNA sequencing now enable researchers to identify cryptic biodiversity and characterize planktonic communities with far greater precision than traditional microscopy alone (Bucklin et al., 2021). High-throughput sequencing technologies increasingly provide insight into microbial composition, trophic interactions, and ecosystem responses to environmental stress.
Stable isotope analysis has similarly become indispensable in aquatic trophic research. Carbon isotope signatures help distinguish primary production sources, while nitrogen isotopes provide valuable information regarding trophic positioning because nitrogen enrichment generally increases with successive trophic transfers (DeNiro & Epstein, 1978; Peterson & Fry, 1987). These isotopic approaches are now widely used to reconstruct food-web architecture and evaluate shifts associated with environmental disturbance and ecosystem change.
Beyond laboratory-based analyses, computational ecology has emerged as a powerful framework for integrating biological, chemical, and environmental data. Ecological network analysis, Bayesian trophic models, and ecosystem-scale statistical approaches increasingly allow researchers to evaluate ecosystem robustness, trophic connectivity, and resilience under environmental stress (Forster et al., 2021; Bogue et al., 1957 and Eaglesham et al., 1999). These methods are particularly valuable because they capture indirect ecological interactions that may otherwise remain difficult to detect.
Importantly, trophic ecology also has practical applications in ecosystem management and sustainable production systems. Integrated Multitrophic Aquaculture (IMTA), for example, attempts to replicate natural nutrient recycling processes by combining fed aquaculture species with extractive organisms such as bivalves and holothurians capable of assimilating excess nutrients (Chatzivasileiou et al., 2022; Chopin et al., 2004). Similarly, biomanipulation strategies involving selective control of fish populations have demonstrated that trophic regulation can significantly influence phytoplankton abundance and zooplankton structure within lakes (Brooks & Dodson, 1965; Hrbáček, 1962). Physiological variation among filter-feeding organisms may also influence nutrient uptake efficiency and ecological performance within these systems (Bayne, 2002).
Collectively, these findings suggest that aquatic trophic dynamics emerge from the interaction of microbial processes, environmental stressors, biological adaptation, and ecosystem-level feedback mechanisms rather than from isolated ecological pathways alone. Understanding these interactions has become increasingly important as aquatic ecosystems face accelerating anthropogenic pressures. This narrative review therefore synthesizes current knowledge regarding trophic organization, microbial interactions, environmental stressors, and emerging analytical approaches within aquatic ecosystems, with particular emphasis on how environmental disturbances reshape ecological stability, trophic connectivity, and ecosystem resilience.



