4.1 Environmental factors and their influence on wetland conditions
The temperature and precipitation during the study period were consistent with Korea’s typical monsoon climate, with no significant differences among the three wetland conditions, indicating that climatic variability was unlikely to have directly impacted the wetland ecosystems (Kim et al. 2014b). Water level fluctuations in the L wetland during the drought period may be closely associated with the proliferation of terrestrial plants and their subsequent influence on soil characteristics (Xu et al. 2015).
As drought conditions persisted, terrestrial plants likely adapted by extending their root systems deeper and wider in search of water, absorbing more moisture from the soil and releasing it into the atmosphere through transpiration (Zambrano et al. 2019; Mohammadi Alagoz et al. 2023). For example, Echinochloa crus-galli, which showed high coverage in the L wetland, may have contributed to the reduction in water levels during the prolonged drought through its well-developed root structure and effective water absorption (Hu et al. 2023). Additionally, changes in soil structure due to root growth may have created a more porous environment, facilitating water infiltration into the ground and further reducing surface water (Liu et al. 2020; Wang et al. 2022). In contrast, in the C and S wetlands, aquatic plants such as Iris ensata, Veronica anagallis-aquatica, Nymphoides peltata, and Equisetum hyemale, which were identified as dominant species, likely contributed more effectively to maintaining water levels by reducing evaporation through their water retention capabilities (Ahmad et al. 2016; Gaballah et al. 2020; Choung et al. 2021). In conclusion, despite consistent climatic conditions across the sites, differences in water levels between the wetlands were likely influenced by the spread of terrestrial plants, resulting changes in soil structure, and the role of aquatic plants. However, as environmental variables such as soil moisture and transpiration were not directly measured, further detailed analysis is necessary.
4.2 Differences in species richness and community composition among the three wetland treatments
This study analyzed the differences in community structure and recovery processes of BMIs in among three wetlands, to assess the impact of drought intensity and duration on wetland ecosystems. The results indicate that BMI communities remained stable in the C wetland, while certain changes in community structure were observed in the S and L wetlands.
The BMI community structure in the C wetland remained stable throughout the study period. During the transition from Phase 1 to Phase 2, new species were introduced, leading to an increase in species diversity despite the loss of some species. In the transition to Phase 3, there was a slight loss of species, but both the Bray-Curtis similarity and Jaccard index indicated high similarity, suggesting minimal community variation within the C wetland. These results suggest that aquatic ecosystems, in the absence of external disturbances, can maintain long-term stability (Bogan et al. 2015). This finding aligns with previous studies that have demonstrated community structure in stable habitats remains relatively unchanged over time (Hillebrand et al. 2008).
The NMS analysis revealed that the C wetland exhibited relatively higher functional evenness compared to the S and L wetlands. This finding aligns with previous research indicating that functional diversity tends to be maintained in stable environments (Loreau et al. 2001). Studies emphasizing the importance of functional evenness in stable ecosystems further support these results. Adler et al. (2007) highlighted that functional diversity contributes to ecosystem stability and resilience, playing a key role in regulating species populations through interspecific interactions. For example, indicator species analysis identified Anax nigrofasciatus as a key indicator species in Phase 2. As a top predator, this species is sensitive to specific habitat conditions, and its presence as an indicator suggests that the C wetland provided suitable conditions with abundant prey resources for sustaining higher trophic levels. While species such as chironomids, Radix auricularia, Cloeon dipterum, and Ischnura asiatica were abundant in the C wetland, their population levels were relatively lower compared to those in the S and L wetlands. his suggests that the presence of top predators, such as A. nigrofasciatus, facilitated stronger interspecific interactions, preventing excessive population growth of certain species and contributing to the overall stability of the community (Adler et al. 2007).
The S wetland experienced changes in BMIs communities due to drought, with a decline in species richness after the drought. However, the similarity between pre- and post-drought communities was higher compared to the L wetland. This can be attributed to the survival and rapid recolonization of drought-tolerant species, such as Physa acuta, which remained resilient after the drought (Gulanicz et al. 2018). As P. acuta lacks flight capabilities, it does not migrate to other habitats during drought but instead survives by burrowing into the mud or reducing its metabolic activity (Aspin et al. 2018). This response aligns with the pulse disturbance theory, which explains how certain species rapidly recolonize habitats following disturbances (Bender et al. 1984; Lake 2003). Additionally, species that have previously experienced drought are generally regarded as relatively resistant or resilient to predictable drying disturbances, a pattern similar to post-drought recovery observed in intermittent streams (Bogan et al. 2015). This similarity suggests that the mechanisms of resilience in wetland ecosystems may be comparable to those observed in stream ecosystems.
As the community progressed into Phase 3, the BMIs of abundance increased more than fourfold compared to Phase 1, indicating rapid recovery following the short-term drought. During this recovery, Dixidae sp. was identified as an indicator species, suggesting that the introduction of new species played a significant role in community recovery. Dixidae sp. likely functioned as an early colonizer and decomposer, rapidly establishing itself after the disturbance, in line with the pulse disturbance theory (Bender et al. 1984). By decomposing organic material, Dixidae sp. likely contributed to nutrient cycling and supported the recovery of ecosystem functions (Gullan and Cranston 2014). This process had a significant impact on lower trophic levels, leading to increased reproduction of aquatic insects and creating favorable conditions for higher-level predators, such as dragonflies, to recolonize the habitat (Boulton and Lake 1992). As a result, a total of 10 species of Odonata were identified. This suggests that decomposers like Dixidae sp. played a key role in restructuring ecosystem functions during early habitat recovery, providing the foundation for top predators to reoccupy the ecosystem (Gullan and Cranston 2014). Furthermore, Adámek et al. (2022) demonstrated that Diptera larvae maintained high species richness and abundance in semi-aquatic habitats due to their ability to breathe air directly through spiracles, independent of dissolved oxygen levels. This adaptability aligns with our findings, where Dixidae sp. played a pivotal role in early habitat recovery, indicating a similar pattern between the two studies. Additionally, MRPP analysis revealed significant differences in community structure between Phase 2 and Phase 3 in the S wetland, indicating ongoing changes as the community continued to recover from the drought.
The L wetland experienced the most severe community changes and recovery processes. Although species loss was lower than in the S wetland, the L wetland exhibited the greatest dissimilarity in community structure compared to its pre-drought state. This reflects the extreme environmental conditions that long-term drought imposed on sensitive species. Many aquatic macroinvertebrates struggled to survive under prolonged drought, leading to a sharp decline in community similarity. These findings align with studies by Dallas and Rivers-Moore (2014) and Stuart et al. (2020), both of which emphasize the significant impact of long-term drought on aquatic species survival and the resulting changes in community structure. In Phase 2, Chironomidae emerged as the dominant taxon. Chironomidae are well-adapted to low-oxygen and stagnant water environments, and their rapid reproductive capacity allows them to quickly colonize new habitats (Kim et al. 2014b; Martel-Cea et al. 2021; Saffarinia et al. 2022). These traits likely contributed to the high dominance of Chironomidae in the L wetland following the drought. As the system progressed into Phase 3, some species diversity was restored; however, the effects of the prolonged drought remained evident. Lepidostoma sinuatum was identified as a key indicator species in Phase 3, suggesting that it is a drought-tolerant species capable of adapting to the altered environmental conditions. Similarly, Whiles et al. (1993) study found that Lepidostoma rapidly recolonized disturbed habitats as an early colonizer, playing a pivotal role in the reassembly of communities following disturbance. This observation supports the conclusion that L. sinuatum was able to adapt to the post-drought habitat changes, contributing significantly to the recovery of the community structure (Ehlers et al. 2020).
Overall, the varying drought conditions demonstrated that species with different levels of resilience and adaptability within the BMI community were selected, ultimately shaping the community structure (Boulton and Lake 1992; Bogan and Lytle 2011). These findings highlight the importance of understanding the impacts of drought on ecosystems and underscore the need to consider species-specific adaptive strategies in ecosystem management (Lytle and Poff 2004).
4.3 Functional Responses of BMIs to Drought Disturbance
Drought serves as an environmental filter, selecting for biological traits suited to specific conditions while excluding others (Southwood 1977; Poff 1997; Vineetha and Nandan 2021). This study compared the functional traits of BMIs among the three wetlands, revealing notable changes in functional traits in response to drought, particularly in ‘feeding habits’, ‘living types’, ‘food types’, and ‘voltinism’. These results are consistent with previous studies, emphasizing that drought creates favorable conditions for species with specific biological traits, thereby altering both functional diversity and community composition in ecosystems (Bogan et al. 2015; Apsin et al. 2018; Vineetha and Nandan, 2021)
The ‘feeding habits’ of BMIs showed some differences in specific traits across the three wetlands. In the C wetland, functional traits remained relatively stable, with an increase in predator (FH4) frequency as food resources became more abundant. In environments with abundant food resources, predators tend to dominate within the community (Ledger et al. 2008). In contrast, the S and L wetlands, both affected by drought, exhibited an increase in the frequency of piercers (FH2) and a decline in predators (FH4). The rise in piercers (FH2) suggests their ability to efficiently utilize resources in the resource-limited conditions caused by drought (Chase 2007; Chester and Robson, 2011). This demonstrates that in habitats with intensified resource limitations, certain functional groups, such as piercers, are able to occupy more favorable conditions for survival.
The ‘living types’ of BMIs responded differently to changes in habitat conditions caused by drought. In the C wetland, living types remained generally stable, while in the S and L wetlands, drought-induced changes in the habitat led to distinct responses based on species traits. Species highly dependent on the physical structure of the habitat, such as climbers (LT2), experienced a decline in frequency during the drought but showed a tendency to increase as the habitat recovered. The clingers (LT4), which depend on stable substrates, exhibited higher frequencies in the S and L wetlands. This increase could be attributed to the presence of terrestrial plants in these wetlands, which likely enhanced the structural complexity of the habitat, creating more surfaces for clingers to attach to. The additional physical habitat structure provided by terrestrial plants likely facilitated improved habitat conditions for these species, promoting their recolonization after the drought. This added complexity in the habitat may have created more favorable environments for clingers, enabling them to re-establish more effectively in the post-drought period. The swimmers (LT5), primarily represented by Coleoptera, were less sensitive to physical habitat changes due to their strong mobility and aerial dispersal abilities (Vineetha and Nandan 2021). These observations highlight how species’ responses varied based on their living types, with ecological traits and habitat dependency playing key roles in determining their resilience or vulnerability to drought-induced environmental changes.
The changes in resource availability among three wetlands were reflected in the ‘food type’ of BMIs. In the C wetland, where resource availability remained stable, no significant changes in feeding habits were observed. The herbivorous species (FT1), which rely on specific plant resources, are more sensitive to environmental stress compared to carnivorous and omnivorous species. In environments experiencing stressors such as drought, plant resources can rapidly decline, leaving herbivores with limited or no alternative food sources, making them more vulnerable to these stress factors (Cummins 1973). In contrast, carnivores and omnivores can exploit a broader range of food resources, enabling them to survive more consistently in resource-limited environments factors (Cummins 1973).
In the C wetland, multivoltine (V3) were relatively dominant, while semivoltine (V1) maintained a stable presence. However, in the S and L wetlands, multivoltine (V3) rapidly occupied the habitat following the drought, indicating their ability to reproduce quickly under stress conditions due to their shorter life cycles (Williams 2006; Herbst et al. 2019). In the S wetland, semivoltine (V1) also managed to recolonize as the habitat recovered. In contrast, in the L wetland, semivoltine (V1) nearly disappeared even during the recovery phase, with multivoltine (V3) dominating the community. This pattern aligns with the findings of Kim et al. (2014b) and Vineetha and Nandan (2021) which suggest that long-term drought creates conditions favorable for species with shorter life cycles, allowing them to reproduce more rapidly. As a result, these conditions can reduce ecological diversity by favoring species that are able to exploit such environments, ultimately leading to a decline in the overall biodiversity of the habitat.
4.4 Impact of drought on BMI community and functional diversity indices
Species richness showed a declining trend in all wetlands throughout the study period, whereas species evenness exhibited different patterns among three wetlands (Table 8). In the C wetland, evenness gradually increased as the BMIs community stabilized. The increase in species evenness observed in stabilized habitats can be attributed to the decline or disappearance of dominant species, as confirmed in our study within the C wetland (Brown et al. 2018).
In contrast, the S wetland exhibited a temporary decline in species evenness following the drought, followed by an increase during the community recovery phases. This pattern aligns with the findings of Ledger et al. (2013), which suggest that, in the early stages of post-drought recovery, certain functional groups may dominate the community. However, as time passes and the community continues to recover, species evenness gradually increases as more species reestablish and diversify within the habitat. Meanwhile, in the L wetland, species evenness continued to decline even after the drought. This may be the result of prolonged drought conditions, which allowed certain species to maintain dominance, limiting the recolonization of other species and leading to a gradual simplification of the community structure.
In terms of trait-based indices (Table 8), both the C and S wetlands showed a gradual decline in FRic as the community stabilized. This reflects a reduction in competition within stable habitats, allowing certain functional groups to become dominant and leading to a decrease in functional richness. In the L wetland, community instability may have led to the emergence of new ecological niches, potentially facilitating species turnover. As a result of the drought, functional diversity declined, with certain species becoming dominant and creating opportunities for new species to occupy available space. However, this turnover process is more likely to contribute to a simplification of the community rather than a recovery of functional diversity. Herbst et al. (2019) also noted that such conditions can lead to the rapid colonization of short-generation species, further destabilizing the community structure.
FEve in the L wetland initially declined following the drought but showed an increasing trend during the community recovery phase. This may be due to species from specific functional groups (e.g., semivoltine) dominating the community by exploiting available resources. Over time, however, other functional groups (e.g., predators) gradually returned, regulating excessive population growth and promoting more balanced species interactions within the community. This pattern is consistent with the findings of Ledger et al. (2011).
Roscher et al. (2014) demonstrated that in disturbed functional spaces, species that benefit from niche availability rapidly occupy those spaces, leading to an initial increase in functional evenness (FEve). However, as dominance by certain functional groups resumes, functional evenness can subsequently decrease. Similarly, in this study, the S wetland exhibited a temporary increase in FEve following the drought, likely due to the rapid colonization of species with diverse functional traits. Over time, however, specific species, such as Radix auricularia, became dominant, leading to a decline in evenness.
Environmental disturbances such as prolonged droughts can significantly limit functional diversity within ecosystems by allowing specific functional groups to dominate. According to the theory of FDiv explained by Villéger et al. (2008), FDiv measures how species are distributed in functional trait space, with higher values indicating a more even distribution of species across diverse functional roles. In the L wetland, the prolonged drought (8 months) created conditions that favored a few species, which monopolized resources and dominated the community. As a result, other species were unable to thrive or perform their functional roles, leading to a reduction in overall functional diversity. Consequently, species became more concentrated around the functional center, decreasing FDiv.
In both the C and L wetlands, FDis showed a gradual increase, whereas in the S wetland, FDis increased during the early post-drought recovery phase but declined in Phase 3. This trend suggests that in the S wetland, species with varying functional traits initially colonized the habitat during recovery, but over time, a few dominant species stabilized the community, reducing functional trait diversity and FDis. According to Laliberté and Legendre (2010), FDis measures species' relative abundances and functional distances. As certain species dominate, functional trait diversity decreases, resulting in lower FDis. In contrast, while L wetland exhibited a rising trend in FDis, this does not necessarily imply greater community resilience or stability. The increase may reflect the dispersion of specific functional traits rather than community recovery. Long-term ecosystem recovery involves complex factors, including species interactions, survival rates, and functional role diversity. Therefore, the increasing FDis in L wetland alone cannot conclude that the community has achieved stability or resilience. Instead, it emphasizes the need to interpret functional diversity indices in the context of broader ecological factors. Moreover, despite the L wetland showing higher FRic, FEve, and FDis than the S wetland, it is difficult to conclude that L wetland is more stable or biodiverse. The Jaccard similarity index revealed that L wetland had the lowest similarity to its pre-drought community, despite showing species composition similarities with S wetland. Differences in functional trait groups further suggest distinct recovery trajectories between the wetlands.
The findings of this study have important implications for wetland management and conservation in the context of climate change. The observed changes in functional diversity and community structure, particularly after long-term drought, suggest that increasing drought frequency could lead to significant long-term alterations in wetland ecosystems. Conservation strategies should focus on protecting drought-vulnerable functional groups and enhancing ecosystem resilience. However, it's crucial to note that while our mesocosm experiment provides valuable insights, it may not capture all the complexities of natural wetland systems. Field studies are necessary to validate these findings and to understand how factors not represented in our mesocosms, such as larger spatial scales and more diverse species interactions, might influence drought responses. Future research should focus on long-term field studies of wetland responses to drought, incorporating a wider range of environmental variables and species interactions. Additionally, investigating the genetic and physiological mechanisms underlying species' drought tolerance could provide further insights into ecosystem resilience.
In conclusion, this study underscores the complex dynamics of wetland ecosystem recovery following drought disturbances. Our findings highlight the need for adaptive management strategies that consider both short-term resilience and long-term shifts in community structure and function. As climate change continues to alter hydrological patterns, understanding these ecological responses will be crucial for effective wetland conservation and the preservation of their vital ecosystem services.