1. Introduction
Wildfire regimes across the Mediterranean Basin have shifted markedly over recent decades, with a growing tendency toward large, high-impact events driven by warmer and drier conditions, longer fire seasons, and accumulated fuels in many landscapes. Drought- and heat-amplified fire weather increases the probability of large fires and extreme behavior, pushing many systems from predominantly fuel-limited toward increasingly drought-driven regimes. Contemporary fire statistics and annual assessments from the European Forest Fire Information System (EFFIS/Copernicus) document the scale and frequency of recent fire seasons and provide a consistent reference framework for comparing events among years and countries [
1].
In addition to the direct loss of vegetation, a serious fire can trigger cascading hy-drological and geomorphological consequences. Meanwhile, the burning of underbrush and canopy cover reduces interception and surface roughness. Changes in the structure and hydrophobicity of soil due to fire can also greatly depress infiltration while promoting shallow land flow. These processes increase the likelihood of post-fire first flushes, gullies, landslides and sediment redistribution, often concentrated in those initial rain periods after the fire. Because these hazards pose threats to downstream infrastructure and water supplies that can endanger human life, reducing rapid erosion in order to reduce flood risks is a major aspect of post-fire management [
2].
Post-fire rehabilitation commonly includes “emergency” or early-stage stabilization measures on hillslopes and in channels that aim to slow runoff, increase infiltration, and retain sediment. Among these, barrier type treatments such as contour-felled log erosion barriers on hillslopes, woody check dams/log dams in channels, and wattles/brush structures are widely implemented because they can be deployed relatively quickly using locally available burned wood or woody debris [
3,
4]. However, the performance of these measures is known to be context-dependent (e.g., burn severity, rainfall regime, slope, soil properties, installation quality) [
4,
5]. A systematic review and meta-analysis showed that barrier treatments and cover-based treatments generally reduce post-fire soil erosion, while runoff reductions are more consistently associated with cover and barrier approaches than with other intervention types; importantly, the same synthesis highlighted strong geographic bias in the evidence base and the need for broader evaluation outside a few well-studied regions [
4]. Field-scale evaluations of contour-felled log erosion barriers also indicate that effectiveness varies and that maintenance and installation details can strongly influence outcomes [
5].
A critical issue for Mediterranean post-fire decision-making is that “effectiveness” should not be defined solely by sediment retention or short-term hydrology. Vegetation recovery is central both to long-term slope stabilization and to biodiversity conservation. In fire-prone ecosystems, post-fire community assembly reflects the balance between resprouting and seeding strategies, pre-fire legacies, and environmental filtering, and it can be sensitive to post-fire interventions that modify microsites, resource availability, or disturbance regimes. Evaluating restoration success therefore benefits from combining structural attributes (e.g., cover/biomass), taxonomic diversity (richness and diversity indices), and compositional turnover, rather than relying on single indicators [
6,
7,
8,
9,
10].
From the standpoint of plant community ecology, post-fire community recovery transcends mere plant re-establishment. It constitutes a process of community assembly, influenced by the enduring impacts of the disturbance, the mechanisms of plant regeneration, and the environmental determinants governing plant survival [
11]. In Mediterranean ecosystems, early post-fire trajectories are often determined by the balance between resprouters and obligate seeders, the persistence of soil and canopy seed banks, and the extent to which recruitment is constrained by dispersal limitation, microsite availability, drought stress, and post-fire soil conditions [
12,
13,
14,
15]. Recovery therefore may follow different trajectories even within the same burned landscape, depending on how local conditions filter establishment and survival. In this sense, resilience is expressed not only as rapid increases in cover or biomass, but also as the capacity of plant communities to reassemble in ways that maintain or redirect biodiversity patterns and successional pathways [
14,
16]. Post-fire rehabilitation structures may interact with these processes by altering surface roughness, sediment retention, shade, litter accumulation, and near-ground moisture conditions, thereby influencing which taxa establish successfully during the first years after fire [
3,
4,
17,
18]. This ecological framework supports the use of multi-metric vegetation assessment, because structural recovery alone may mask important differences in diversity, composition, and early recovery trajectories [
6,
7,
8,
9,
10].
Recent syntheses on post-fire rehabilitation in Mediterranean forests underline substantial heterogeneity in the indicators used to judge outcomes, persistent shortages of long-term monitoring, and limited integration of ecological metrics alongside physical/engineering endpoints [
3,
4]. In parallel, restoration ecology frameworks emphasize that robust success assessment should be explicitly objective-led and multidimensional, combining structural attributes, diversity, and compositional change measured through time, rather than relying on single proxies [
6,
7,
8,
9,
10]. Despite these recommendations, much of the applied evidence base for post-fire treatments still centers on soil properties, runoff and erosion responses [
19,
20], while biodiversity-oriented vegetation recovery is less consistently evaluated, and the geographic distribution of field evidence remains uneven across Mediterranean regions [
3,
4].
This evidence gap is particularly relevant for Greece, where post-fire rehabilitation is frequently implemented at operational scales using locally available burned wood in nature-based barrier structures (e.g., wattles/brush structures, contour-oriented log barriers on hillslopes, and log dams in channels). However, there is limited comparative, repeated (multi-year) field evidence from Greek Mediterranean forests on how specific wooden structure types relate to early vascular plant recovery trajectories, including richness, cover/biomass, and community composition [
3,
4,
5,
6,
7,
8,
9,
10]. As a result, post-fire decision-making that aims to jointly address hazard mitigation and biodiversity recovery often proceeds with incomplete ecological performance information for the measures most commonly deployed.
In this study, we address this gap by evaluating early vascular plant recovery in fire-affected forest landscapes in Greece that burned during the 2021 wildfire season, using repeated field surveys conducted in summers 2022 and 2023. We focus on areas including Parnitha (Attica) and Mavrolimni (Corinthia/Peloponnese), representing contrasting climatic settings and land use mosaics within the Mediterranean Basin. Following operational post-fire rehabilitation implemented by the National Forest Service, a network of experimental plots was established and assigned to dominant wooden, nature-based structure types used locally wattles, contour-oriented log barriers on hillslopes, and log dams in channels intended to slow runoff, trap sediment, and reduce erosion [
3,
4,
5]. Within these plots, vascular plant composition and key recovery endpoints (species richness, density, cover, biomass) were quantified using quadrat sampling during the main growing season in both monitoring years.
Within this ecological framework, this study aimed to evaluate early post-fire responses of vascular vegetation across the dominant wooden rehabilitation structure types used operationally in Greek burned forests. Specifically, we aimed to (i) measure short-term variations in vascular plant diversity, vegetation cover, and biomass across different structure types over two post-fire years; (ii) assess shifts in plant community composition among structure types and years using dissimilarity analyses; and (iii) identify taxa linked to particular structure types that could serve as indicators of early post-fire recovery pathways. We hypothesized that (H1) vegetation cover and biomass would increase strongly from 2022 to 2023 across all structure types, reflecting rapid early recovery; (H2) diversity patterns and community composition would differ among structure types because the rehabilitation structures act as microsite filters influencing recruitment and early community assembly; and (H3) particular taxa would show non-random associations with specific structure types, reflecting contrasting regeneration strategies and early niche differentiation after fire. By combining structural, diversity, compositional, and indicator–species metrics, the study aims to strengthen the evidence base for post-fire management in Greek Mediterranean forests and to support decision-making that jointly considers hazard mitigation and biodiversity recovery.
3. Results
For readability, detailed species- and family-level composition data are summarized in the
Supplementary Materials, whereas the main text emphasizes the principal patterns in diversity, community composition, indicator taxa, and interannual recovery.
3.1. Vascular Plant Composition in Parnitha
Family-level composition (expressed as the percentage of species belonging to each family within each structure type × year) differed among structure types and between years in Parnitha (
Figure 6). Because proportional composition alone can obscure differences in total richness and abundance, the corresponding absolute values are also provided in the
Supplementary Materials (Tables S33 and S34), which report the pooled number of species per family and the total number of individuals per family for each structure type × year. These absolute summaries show that pooled species richness was lowest in log barriers in 2022 (8 species), increased in log barriers in 2023 (11 species), and remained higher in wattles and log dams (16–21 pooled species depending on year). They also indicate strong numerical dominance of Pinaceae in log barriers (426 individuals in 2022; 470 in 2023), despite its representation by a single species, whereas Poaceae contributed the greatest number of species in wattles and log dams. Finally, Poaceae and Asteraceae contributed substantially to species richness in wattles and log dams, whereas log barriers showed lower species richness in 2022 and a stronger representation of Cistaceae, followed by a broader family distribution in 2023.
3.2. Alpha Plant Diversity, Cover and Biomass of Vascular Plants in Parnitha
Species richness (S) ranged from 3.67 ± 0.33 to 11.00 ± 0.58 across structure types (
Table 2). Richness was significantly lower in log barriers-2022 (3.67 ± 0.33) compared with all other structure types, which did not differ among them (all a). Shannon–Wiener diversity (H′) showed the highest values in wattles (Wattles-2022: 1.90 ± 0.13; Wattles-2023: 2.24 ± 0.04), followed by Log dams-2023 (1.77 ± 0.15) and Log dams-2022 (1.554 ± 0.49), while Log barriers-2023 (1.39 ± 0.43) and especially Log barriers-2022 (0.67 ± 0.28) exhibited the lowest diversity, with significant pairwise differences indicated by distinct letters. A similar pattern was observed for Simpson diversity (1 − D) and Pielou evenness (J′): both indices were highest in wattles (0.82–0.87 for 1 − D; 0.90–0.93 for J′), intermediate in log dams (Log dams-2023; Log dams-2022), and lowest in log barriers (Log barriers-2023; Log barriers-2022), with all groups differing significantly as denoted by different letters (
Table 2).
3.3. Changes in Plant Community Composition Across Structure Types and Years in Parnitha
The Bray–Curtis heatmap provided a descriptive summary of aggregated compositional differences among the structure type × year samples (BC range: 0.21–0.93) (
Figure 7). However, plot-level PERMANOVA on Bray–Curtis dissimilarities derived from log(x + 1)-transformed abundances did not detect a significant structure effect in 2022 (pseudo-F = 1.56, R
2 = 0.34,
p = 0.12; permutations = 1680) or 2023 (pseudo-F = 2.40, R
2 = 0.44,
p = 0.07; permutations = 1680). PERMDISP did not indicate heterogeneity of multivariate dispersion (2022: F = 0.64,
p = 0.79; 2023: F = 2.28,
p = 0.35). Accordingly, the heatmap patterns should be interpreted as descriptive compositional contrasts rather than as statistically supported structure type differences within years.
The log barriers produced the least dissimilarity between years (log barriers-2022 and log barriers-2023: BC = 0.21), followed by the log dams (log dams-2022 and log dams-2023: BC = 0.28). Also, Wattles had the greatest annual turn (wattles-2022 and wattles-2023: BC = 0.39). Wattles exhibited significant differences in structure to log barriers (BC = 0.86–0.93), with greatest dissimilarity between wattles in 2022 and log barriers in 2023 (BC = 0.93). Log dam comparisons were typically intermediate as well (e.g., log dams-2023 vs. log barriers-2023: BC = 0.63; log dams-2022 vs. wattles-2022: BC = 0.76), which indicates that communities associated with log dams could be found compositionally, in between those characterized for log barriers and wattles.
3.4. Temporal Changes in Vegetation Cover and Biomass in Parnitha
Mean vegetation cover increased strongly between 2022 and 2023 across all structure types (overall mean ± SE: 31.1 ± 6.7% in 2022 vs. 67.9 ± 3.1% in 2023) (
Figure 8). The year × structure type interaction was not significant (Wald χ
2(2) = 4.04,
p = 0.133); thus, an additive model was fitted. In this model, year had a significant effect (Wald χ
2(1) = 17.45,
p = 2.95 × 10
−5), whereas structure type showed no statistically significant main effect at α = 0.05 (Wald χ
2(2) = 5.54,
p = 0.06). At the year × structure level, mean cover (±SE) ranged from 16.7 ± 4.6% (log barriers, 2022) to 71.5 ± 6.5% (log dams, 2023).
Mean vegetation biomass also increased from 2022 to 2023 (overall mean ± SE: 71.6 ± 19.4 g m
−2 in 2022 vs. 102.1 ± 18.7 g m
−2 in 2023) (
Figure 9). The year × structure type interaction was not significant (Wald χ
2(2) = 3.04,
p = 0.21), and the additive model indicated a significant year effect (Wald χ
2(1) = 11.41,
p = 7.31 × 10
−4). The main effect of structure type was not significant at α = 0.05 (Wald χ
2(2) = 5.29,
p = 0.07). Across year × structure combinations, mean biomass (±SE) ranged from 25.2 ± 14.8 g m
−2 (log barriers, 2022) to 162.5 ± 46.3 g m
−2 (wattles, 2023).
3.5. Vascular Plant Composition in Mavrolimni
The family-level composition in Mavrolimni, expressed as the percentage of species per family within each structure type × year, varied across structure types (
Figure 10). To complement these percentages, absolute values are presented in the
Supplementary Materials (Tables S35 and S36) as pooled number of species per family and total individuals per family for each structure type × year. These data indicate an increase in pooled species richness from 4 to 9 in log dams and from 8 to 11 in log barriers between 2022 and 2023.
In 2022, log barriers were predominantly composed of Cistaceae (3 species; 148 individuals). In 2023, Cistaceae continued to be the most numerous, with 178 individuals, and other families also increased. Log dams in 2023 exhibited a wider variety of families, notably Fabaceae (2 species; 28 individuals), Poaceae (23 individuals), and Pinaceae (21 individuals), all of which made significant contributions. Overall, the main trend at Mavrolimni was a temporal increase in floristic diversity across both structure types during the early stages of recovery.
3.6. Alpha Plant Diversity, Cover and Biomass of Vascular Plants in Mavrolimni
Alpha diversity differed among the structure type × year groups (
Table 3). Species richness (S) was significantly higher in 2023 than in 2022 for both structure types: log dams-2023 (7.33 ± 0.67) and log barriers-2023 (7.75 ± 0.85) exceeded log dams-2022 (2.00 ± 0.58) and log barriers-2022 (4.25 ± 0.48). The Shannon–Wiener diversity (H′) exhibited a consistent pattern, with elevated values recorded in 2023 (log dams-2023: 1.92 ± 0.10; log barriers-2023: 1.78 ± 0.16) compared to 2022 (log dams-2022: 0.57 ± 0.30; log barriers-2022: 1.09 ± 0.14). Similarly, Simpson diversity (1 − D) increased in 2023, with log dams-2023 (0.84 ± 0.01) and log barriers-2023 (0.77 ± 0.05) significantly surpassing the values observed in 2022 (log dams-2022: 0.37 ± 0.19; log barriers-2022: 0.59 ± 0.09). Pielou evenness (J′) varied among the groups, registering as lowest in log barriers-2022 (0.79 ± 0.13), whereas the groups log dams-2022, log dams-2023, and log barriers-2023 demonstrated similarly higher evenness indices (ranging from 0.88 to 0.96).
3.7. Changes in Plant Community Composition Across Structure Types and Years in Mavrolimni
The Bray–Curtis heatmap provided a descriptive summary of aggregated compositional differences among the structure type × year samples (BC range: 0.38–0.90) (
Figure 11). However, plot-level PERMANOVA on Bray–Curtis dissimilarities calculated from log(x + 1)-transformed abundances did not detect a significant difference between structures in 2022 (pseudo-F = 0.17, R
2 = 0.03,
p = 0.91; permutations = 35) or 2023 (pseudo-F = 1.11, R
2 = 0.18,
p = 0.361; permutations = 35). PERMDISP tests did not yield statistically significant results (2022: F = 1.09,
p = 0.38; 2023: F = 0.43,
p = 0.77). Accordingly, the heatmap patterns observed in Mavrolimni should be regarded as descriptive rather than inferential.
The smallest difference was found between log barriers-2022 and log barriers-2023 (BC = 0.38), showing very little change from one year to the next within log barriers. Conversely, log dams showed greater dissimilarity over the years (log dams-2022 vs. log dams-2023: BC = 0.70). In 2022, the most notable differences among structural types were observed with log dams, especially when compared to log barriers (BC = 0.88–0.90). In 2023, log dams appeared more similar to log barriers in that year (BC = 0.53) than to those in 2022 (BC = 0.62).
3.8. Temporal Changes in Vegetation Cover and Biomass in Mavrolimni
Mean vegetation cover increased markedly from 2022 to 2023 for both structure types (log barriers: 11.5 ± 2.9% to 60.4 ± 6.6%; log dams: 15.8 ± 12.9% to 71.2 ± 7.6%) (
Figure 12). The year × structure type interaction was not significant (Wald χ
2(1) = 1.06,
p = 0.30), therefore an additive model was used. In this model, year had a strong effect (Wald χ
2(1) = 61.05,
p = 5.56 × 10
−15), while the main effect of structure type was not significant (Wald χ
2(1) = 0.75,
p = 0.38).
Mean vegetation biomass increased from 2022 to 2023, but the magnitude of change differed between structure types (log barriers: 19.6 ± 9.6 to 109.9 ± 29.7 g m
−2; log dams: 103.7 ± 29.5 to 142.2 ± 42.7 g m
−2) (
Figure 13). The year × structure type interaction was significant (Wald χ
2(1) = 3.86,
p = 0.04). Simple-effects tests indicated a significant year-to-year increase within log barriers (Wald χ
2(1) = 46.74,
p = 8.12 × 10
−12), but not within log dams (Wald χ
2(1) = 2.68,
p = 0.10). In 2022, biomass was higher in log dams than in log barriers (Wald χ
2(1) = 4.08,
p = 0.04), whereas the structure difference was not significant in 2023 (Wald χ
2(1) = 1.91,
p = 0.16).
3.9. Indicator Species Analysis Across Structure Types in Parnitha
The Indicator Species Analysis shows that only a few plant species are significantly associated with each structure type in Parnitha (
Table 4,
Figure 14). This was corroborated by the IndVal results (IndVal permutation test, stratified by year; 4999 permutations;
p < 0.05). Four indicator species of wattle were
Aegilops geniculata (IndVal = 66.67; A = 1.00; B = 0.67;
p = 0.02),
Melica ciliata (66.67; 1.00; 0.67;
p = 0.02),
Quercus coccifera (66.67; 1.00; 0.67;
p = 0.02), and
Cistus salviifolius (56.67; 0.68; 0.83;
p = 0.03). Log dams were denoted by
Anagallis arvensis (IndVal = 51.93; A = 0.62; B = 0.83;
p = 0.040), whereas log barriers were strongly indicated by
Pinus halepensis (IndVal = 83.90; A = 0.84; B = 1.00;
p = 0.03), reflecting high fidelity and specificity to this structure type within the pooled two-year dataset. When the analysis was repeated separately within each year (2022 and 2023; plots per structure type), no species reached significance (
p < 0.05), again suggesting a lack of within-year replicability.
Moreover, indicator species analysis revealed two taxa that are significantly linked to log barriers in Mavrolimni (
Table 5,
Figure 15). The strongest indicator was
Cistus salviifolius (IndVal = 93.73; A = 0.94; B = 1.00;
p = 0.00), indicating both high specificity and total faithfulness to the specific plots that enforced logs as barriers. The second indicator of log barriers was
Pinus halepensis (IndVal = 59.97; A = 0.69; B = 0.88;
p = 0.02). No species were significant indicators of log dams at
p < 0.05. When the analysis was repeated within each year (2022 and 2023) separately, no indicator species reached significance, consistent with limited within-year replication. Accordingly, the significant associations identified here are best regarded as provisional structure-linked signals within the present sampling design, rather than as definitive bioindicators.
These indicator taxa should be interpreted cautiously. Their significance in the pooled two-year dataset reflects statistical specificity and fidelity to particular structure types within the present sampling design, rather than synchronous recovery timing or equivalent successional roles. This is especially relevant for Cistus salviifolius and Pinus halepensis, which represent different post-fire regeneration strategies in Mediterranean ecosystems. Cistus salviifolius is a typical early fire-follower, whereas P. halepensis is an obligate seeder whose recruitment may begin soon after fire but whose establishment and persistence follow a longer, microsite-dependent trajectory. Their simultaneous emergence as indicator taxa therefore suggests asynchronous but co-occurring structure-associated early assembly patterns, rather than a contradiction in ecological interpretation.
3.10. Interannual Recovery (Δ2023–2022) and Composite Recovery Index
3.10.1. Parnitha
Interannual recovery magnitude (Δ2023–2022) differed among structure types primarily for vegetation cover in Parnitha (
Figure 16). The increase in cover was greatest in log barriers (mean Δcover = 52.17%, 95% CI: 39.66–64.67) and log dams (38.17%, 95% CI: −3.15–79.48), while wattles exhibited a smaller increase (20.17%, 95% CI: −3.48–43.81). A one-way ANOVA indicated a significant structure type effect on Δcover (F(2,6) = 5.90,
p = 0.03), with borderline support from the permutation test (
p_perm = 0.05). Post hoc Tukey HSD separated wattles from the two log-based structures (α = 0.05).
In contrast, Δ vegetation density did not differ among structure types (F(2,6) = 0.02, p = 0.97; p_perm = 0.95), and neither Δ species richness (F(2,6) = 2.58, p = 0.15; p_perm = 0.20) nor Δlog(1 + biomass) (F(2,6) = 1.40, p = 0.31; p_perm = 0.21) showed statistically supported differences, indicating higher among-plot variability for these endpoints over the 2022–2023 interval.
A composite Recovery Index was calculated per plot as the mean of z-scored interannual changes (Δ2023–2022) in vegetation cover, vegetation density, species richness, and log-transformed biomass [Δlog(1 + biomass)] in Parnitha. The Recovery Index differed numerically among structure types, with log barriers showing the highest mean recovery score (0.63; 95% CI: −1.81 to 3.07), whereas log dams (−0.28; 95% CI: −1.56 to 1.00) and wattles (−0.35; 95% CI: −0.81 to 0.10) exhibited lower mean scores (
Figure 17). However, differences among structure types were not statistically significant (one-way ANOVA: F(2,6) = 2.14,
p = 0.19; permutation test:
p_perm = 0.13), although the effect size was moderate (η
2 = 0.41).
3.10.2. Mavrolimni
Interannual recovery magnitude (Δ2023–2022) was quantified at plot level for vegetation cover, vegetation density, species richness, and log-transformed biomass [Δlog(1 + biomass)] and compared between structure types (log barriers; log dams) (
Figure 18). Both structure types showed large increases in vegetation cover (log barriers: mean Δcover = 56.9%, 95% CI: 33.8–80.0; log dams: 46.0%, 95% CI: −4.1–96.1), but Δcover did not differ significantly between structure types (one-way ANOVA: F(1,5) = 0.70,
p = 0.44; permutation test:
p = 0.51). Likewise, Δ vegetation density (log barriers: 7.00, 95% CI: −3.31–17.31; log dams: −2.17, 95% CI: −46.35–42.02) was not significantly different between structure types (F(1,5) = 0.95,
p = 0.375;
p_perm = 0.51). Changes in species richness were comparable (log barriers: 3.13, 95% CI: 0.50–5.75; log dams: 3.17, 95% CI: 0.30–6.04) with no structure type effect (F(1,5) = 0.00,
p = 0.97;
p_perm = 1.00). Similarly, biomass change expressed as Δlog(1 + biomass) did not differ between structures (log barriers: 1.07, 95% CI: −0.26–2.41; log dams: 1.02, 95% CI: −0.61–2.66; F(1,5) = 0.00,
p = 0.93;
p_perm = 0.94). Finally, recovery magnitude was substantial across metrics but did not show statistically supported differences between log barriers and log dams (2022–2023).
The composite Recovery Index was calculated per plot as the mean of z-scored interannual changes (Δ2023–2022) in vegetation cover, vegetation density, species richness, and log-transformed biomass [Δlog(1 + biomass)] (
Figure 19). The Recovery Index did not differ between structure types (one-way ANOVA: F(1,5) = 0.94,
p = 0.37; permutation test:
p_perm = 0.40; η
2 = 0.15). The mean Recovery Index was slightly higher for log barriers (0.15; 95% CI: −0.55 to 0.86) than for log dams (−0.20; 95% CI: −1.55 to 1.13), indicating only a weak, non-significant tendency towards higher composite recovery in log barriers.
4. Discussion
4.1. Rapid Early Recovery, with Structure Type Shaping the “Biodiversity Signal”
Across both Greek fire-affected landscapes, vegetation cover and biomass increased strongly from the first to the second monitoring year, indicating rapid early reassembly typical of many Mediterranean systems when post-fire climatic conditions permit [
46,
47,
48]. This pattern is consistent with the broader shift toward drought-amplified fire regimes and the increasing importance of post-fire climatic constraints (especially drought duration) in controlling short-term recovery rates in Mediterranean forests [
60,
61,
62]. Against that strong interannual signal, our results show that the different wooden, nature-based rehabilitation structures did not simply act as “neutral” engineering additions. Instead, structure type was associated with pronounced descriptive compositional contrasts (Bray–Curtis heatmaps), with limited plot-level PERMANOVA support within years, particularly in the first post-fire years when microsite limitation, propagule availability, and environmental filtering are strongest [
63,
64].
The family-level patterns observed in the first two monitoring years are also ecologically consistent with typical Mediterranean post-fire colonization processes. The prominence of Poaceae and Asteraceae, especially in wattles and log dams in Parnitha, suggests a strong contribution of herbaceous early colonizers able to exploit the open, high-light and low-competition conditions that follow fire. In Mediterranean post-fire environments, taxa from these families frequently contribute to the early regenerating flora, and seed-bank studies have likewise shown a strong representation of Poaceae and Asteraceae among the readily emerging post-fire species. This pattern is ecologically plausible because many grasses and forbs can establish rapidly after disturbance, while many Asteraceae are also effective colonizers of open ground due to efficient dispersal and ruderal behavior. By contrast, the stronger representation of Cistaceae, particularly in log barriers, is consistent with the role of Cistus sp. as characteristic fire-following seeders in Mediterranean ecosystems, often promoted by persistent soil seed banks and high establishment during the first post-fire stages. Taken together, these family-level patterns indicate that the early recovery observed here was driven not only by overall increases in vegetation cover and richness, but also by the rapid assembly of herbaceous colonizers and fire-following shrubs favored by post-fire microsites and structure-related environmental filtering [
65,
66,
67]. Viewed through the lens of post-disturbance succession, the vegetation dynamics observed here correspond to an early secondary successional stage, characterized by rapid re-establishment of herbaceous cover, increasing species richness, and incomplete compositional stabilization during the first two post-fire years. In this phase, vegetation assembly is expected to be driven primarily by regeneration traits, propagule availability, microsite conditions, and post-fire climatic constraints, rather than by immediate convergence toward a single mature-community endpoint. Our results are consistent with that interpretation: the strong year effect indicates a dominant regional recovery signal, whereas the differences among rehabilitation structures suggest locally modified successional trajectories created by structure-related environmental filtering. In this sense, the structures appear not to replace the broader post-fire recovery template, but to modulate it by favoring different combinations of colonizers, fire-followers, resprouters, and obligate seeders. Ecological resilience in the present study should therefore be interpreted cautiously, not as a rapid return to pre-fire composition, which could not be tested here, but as short-term structural resilience expressed through rapid recovery of vegetation cover and biomass alongside multiple plausible compositional pathways during early assembly [
67,
68,
69]. A key ecological interpretation is that these barrier type interventions may be better viewed as spatially explicit “microsite modifiers” rather than purely hydrological devices. By trapping fine sediments and organic matter, altering surface roughness, and locally moderating soil moisture and temperature, wooden barriers can create small-scale heterogeneity in establishment conditions [
70]. Similar facilitation pathways are widely described for coarse woody debris and deadwood legacies, which can provide safe sites and microclimatic buffering for regeneration after disturbance [
71]. Importantly, the same physical mechanisms that reduce runoff connectivity and sediment transport after severe fire (e.g., increased roughness and obstruction of overland flow) can also restructure recruitment opportunities for herbs, shrubs, and tree seedlings [
72,
73].
4.2. Why Did Structure Type Matter Most for Diversity/Composition?
In Parnitha, wattles consistently supported higher diversity indices relative to log-based hillslope barriers, while log barriers showed a markedly “compressed” diversity signal in the first monitoring year and a partial rebound in the second year. One plausible mechanism is that wattles (branch/brush piles, typically placed on gentler hillslopes) may preferentially retain fine material and seeds while maintaining a patchier disturbance footprint, promoting a richer assemblage of short-lived herbs and graminoids. In contrast, contour-oriented log barriers can create more continuous bands of deposition and shading and may also be preferentially installed on steeper or more erosion-prone positions where burn severity and soil limitation can be higher; such sites can select for fewer taxa early on, even when overall cover is increasing [
70,
72,
73]. Field work elsewhere similarly emphasizes that log erosion barriers can be effective for sediment retention yet highly variable in ecological outcomes, depending on placement, slope, rainfall regime, and installation quality. Mediterranean evidence from Spain also indicates that log erosion barriers can enhance vegetation recovery early, but benefits may weaken with time and can be spatially heterogeneous [
73].
The compositional (beta-diversity) results warrant cautious interpretation. The Bray–Curtis heatmaps were intended as descriptive visualizations of aggregated structure × year community profiles, whereas the formal plot-level PERMANOVA tests did not detect statistically significant structure type effects within years. Because replicate numbers were small and uneven among some groups, the compositional contrasts observed in the heatmaps are best regarded as descriptive patterns and hypothesis-generating signals rather than as statistically confirmed structure type differences. This distinction is important because aggregation can obscure within-group variability, and distance-based multivariate analyses require careful interpretation alongside dispersion tests [
74,
75,
76].
Where interannual Bray–Curtis dissimilarity was relatively low within a structure type, this suggests persistence of a few dominant taxa and/or stable microsite constraints; higher turnover suggests a more dynamic assembly trajectory driven by colonization, competitive sorting, and year-to-year climatic variation [
74]. Such differences matter for post-fire management because they imply that equivalent increases in cover may mask different biodiversity and successional pathways, precisely the issue raised by restoration-evaluation frameworks that argue for multidimensional success metrics (structure, diversity, composition) rather than single indicators [
77,
78].
4.3. Indicator Taxa Suggest Structure-Linked Microsite Filtering and Regeneration Niches
The indicator–species results should be interpreted cautiously. Although a small number of taxa showed significant associations with particular structure types, these associations emerged mainly in the pooled two-year dataset, whereas no species reached significance when the analyses were repeated separately within each monitoring year. Given the limited and uneven replication of the present sampling design, these taxa are best viewed as provisional structure-linked signals rather than as definitive bioindicators of rehabilitation structures. Within that cautious framework, the ecological identities of the significant taxa remain informative. In Parnitha, wattles were associated with grass and shrub elements, whereas log barriers were associated mainly with
Pinus halepensis. In Mavrolimni, log barriers were linked to
Cistus salviifolius and again
P. halepensis. These associations are ecologically coherent with known Mediterranean post-fire regeneration strategies, but they should not be interpreted as strong evidence of fixed or synchronous structure-specific recovery trajectories. Rather, they indicate that some rehabilitation structures may create microsites that are repeatedly used by taxa with contrasting early post-fire strategies. This caution is especially relevant for
Cistus salviifolius and
Pinus halepensis, which represent different regeneration modes in Mediterranean ecosystems.
Cistus salviifolius is a typical early fire-follower, whereas
P. halepensis is an obligate seeder whose successful establishment depends on longer-term microsite suitability after recruitment begins. Their simultaneous appearance among the significant taxa therefore does not demonstrate a single uniform recovery pathway. Instead, it suggests that the same structure type may favor establishment opportunities for taxa with different regeneration tempos. At this stage, these associations are more appropriately interpreted as hypothesis-generating patterns that warrant validation with stronger replication across years, sites, and burn severity conditions [
79,
80,
81,
82]. Viewed through a functional lens, the indicator taxa also point to clear differences in life form and regeneration mode among structure types. In Parnitha, wattles were associated with annual and perennial graminoids (e.g.,
Aegilops geniculata and
Melica ciliata), together with woody shrub elements such as
Quercus coccifera and
Cistus salviifolius, suggesting that these branch pile structures create heterogeneous microsites that can support both short-lived herbaceous colonizers and woody Mediterranean shrubs. By contrast, log barriers were associated mainly with
Pinus halepensis in Parnitha and with
P. halepensis and
C. salviifolius in Mavrolimni, indicating microsites favorable to early fire-followers and obligate seeders. From a post-fire regeneration perspective,
Quercus coccifera represents a typical resprouting woody species, whereas
Pinus halepensis is an obligate seeder whose recruitment depends on canopy seed release and microsite suitability after fire.
Cistus salviifolius is likewise a characteristic early post-fire seeder/fire-follower, typically promoted by persistent soil seed banks. Therefore, similar increases in vegetation cover may conceal ecologically different recovery pathways, ranging from rapid therophytic and graminoid colonization to shrub resprouting and pine recruitment. This functional interpretation further supports the view that rehabilitation structures act as microsite filters, shaping not only taxonomic diversity but also the balance among life forms and regeneration strategies during early post-fire assembly [
63].
4.4. Linking Hazard Mitigation Interventions to Biodiversity Outcomes: The Study’s Contribution
Most operational post-fire programs still prioritize near-term hydrological risk reduction because the post-fire window of elevated runoff and erosion hazard is often concentrated in the first storm seasons [
70]. Our results add a complementary, biodiversity-oriented evidence layer for Greece by showing that commonly deployed wooden structures are associated with measurable differences in plant diversity and descriptive compositional patterns; composition-level differences were weaker (PERMANOVA
p > 0.05) over two consecutive years, i.e., within the same time horizon that agencies care most about rapid stabilization.
Our findings are also consistent with recent evidence from other Mediterranean megafire-affected landscapes. In Sardinia, Rossetti et al. [
83] documented notable natural vegetation regrowth already within the first post-fire year, while also showing that recovery was heterogeneous among vegetation types, with more resilient responses in semi-natural grasslands than in shrublands and woodlands. At a broader regional scale, Blanco-Rodríguez et al. [
69] showed across western Mediterranean forest ecosystems that short-term post-fire recovery is primarily constrained by drought duration, with fire severity acting as an additional driver and semi-arid areas showing lower average recovery rates. The present study agrees with this broader Mediterranean pattern in two respects: first, vegetation cover and biomass increased strongly from 2022 to 2023 in both Greek study areas, indicating rapid early reassembly; second, recovery was clearly not uniform, because diversity patterns, indicator taxa, and descriptive compositional contrasts differed among rehabilitation structure types and between sites. In this sense, our results complement existing Mediterranean studies by adding a plot-based, management-oriented perspective showing that wooden post-fire rehabilitation structures may shape the early biodiversity signal through microsite modification, even when overall structural recovery is rapid. This directly addresses a recognized geographic and thematic gap: Mediterranean syntheses note that treatment effect evidence is unevenly distributed among regions and that ecological endpoints are less consistently monitored than erosion/runoff metrics [
72]. By pairing multi-metric vegetation monitoring with the operational structure types used by Greek Forest Services, the work advances “integrated evaluation” in a way that is actionable for management and compatible with restoration science recommendations for objective-led, multidimensional monitoring [
77,
78,
84].
A further point of significance is that these biodiversity results can be interpreted alongside hydrological performance within the same project context. Evidence from Greece indicates that the same structure classes (log dams, log barriers, wattles) can influence infiltration patterns two years post fire, underscoring why coupled ecohydrological assessment is more informative than treating “hazard mitigation” and “ecosystem recovery” as separate objectives [
84]. In practice, decision-makers need to know not only whether a measure slows runoff, but also whether it accelerates, delays, or redirects recovery trajectories for native plant communities in a global biodiversity hotspot region [
85,
86].
From a management perspective, these results suggest that the clearest structure-linked signal in the first two years concerns alpha diversity, whereas indicator–species associations remained limited and provisional and composition-level differences appear weaker and may require larger sample sizes to be detected consistently.
4.5. Limitations and Future Research Directions
This study captures an early (two-year) post-fire window, and causal attribution may be influenced by landscape placement and site selection effects (e.g., burn severity, slope position, and substrate) associated with where structures were installed. A further limitation concerns the experimental design itself. The total number of permanent plots was relatively small and unevenly distributed among sites and rehabilitation structure types, reflecting the operational placement of structures in the field rather than a fully balanced experimental design. As a result, statistical power was limited for some analyses, particularly for detecting subtle compositional differences and within-year indicator–species patterns, and some ecological signals may therefore have remained undetected. In addition, the absence of a burned untreated control means that the study cannot disentangle the effects of rehabilitation structures from background natural post-fire regeneration with the same strength as a treated–untreated design. Consequently, the present results should be interpreted primarily as comparisons among structure types within operationally restored burned areas, rather than as direct estimates of rehabilitation effects relative to no intervention. Because burn severity was not explicitly quantified as a covariate in the present analysis, part of the observed variation in vegetation recovery may reflect residual severity differences among plots, in addition to the effects associated with rehabilitation structure type.
In addition, the short monitoring horizon limits inference on whether initial diversity and compositional differences persist, converge, or amplify as shrubs and trees restructure canopy and fuel mosaics [
71]. A further limitation concerns the lack of plot-level pre-fire vegetation data. Although the broader pre-fire vegetation context of the two landscapes is known from site-level land cover information, the study cannot quantify the exact departure of each plot from its pre-fire floristic composition. Consequently, the results should be interpreted as comparisons of early post-fire vegetation among rehabilitation structure types and between monitoring years, rather than as complete pre-fire to post-fire vegetation trajectories.
Although the present revision strengthens the functional interpretation of the observed taxa, a full quantitative trait-based analysis across all recorded species was beyond the scope of the present sampling design and remains an important priority for future post-fire monitoring.
An additional limitation concerns survey timing. Although the May–July field window allowed for standardized sampling and biomass assessment, it may have underrepresented early-season annuals and other short-lived taxa whose aboveground presence in Mediterranean ecosystems is concentrated in the winter–spring period and may decline rapidly before or during summer drought. As a result, the reported richness, density, and cover values should be interpreted as conservative estimates for the full seasonal flora. An additional limitation concerns sampling grain: the 1 m2 quadrats used here are appropriate for standardized microsite-scale assessment of early post-fire vascular vegetation, cover, and biomass, but they may underrepresent rare, sparse, or patchily distributed taxa and do not capture the full stand-scale heterogeneity of burned Mediterranean forests. Therefore, the present results should be interpreted as localized vegetation responses around the rehabilitation structures rather than as complete forest–community inventories. Accordingly, the most useful next steps are as follows: (i) extending monitoring to capture medium-term trajectories (≥5 years), when resprouted dominance, pine recruitment success/failure, and competitive exclusion become clearer; (ii) explicitly stratifying sampling by burn severity, slope position, and substrate to better separate treatment effects from site selection effects; and (iii) combining plot vegetation data with objective measures of microsite conditions (soil moisture and temperature, litter depth, fine-sediment accumulation) together with hydrological indicators (e.g., infiltration, runoff connectivity) to test the facilitation and filtering mechanisms implied by the results. With these additions, Greek post-fire programs could move toward evidence-based selection and placement guidelines that better align risk reduction objectives with biodiversity recovery.
Accordingly, any structure-linked biodiversity patterns identified in the present study should be regarded as provisional and in need of validation through longer-term and more balanced monitoring. Taken together, the results indicate that early post-fire vegetation recovery was rapid in both burned landscapes, but the evidence for consistent structure-specific biodiversity effects remains preliminary. Wooden rehabilitation structures were associated more clearly with differences in alpha-diversity and with a limited set of provisional indicator–taxon associations than with simple cover responses or consistently supported compositional separation. Accordingly, the present findings are best interpreted as early structure-linked biodiversity signals within a short post-fire window, rather than as definitive evidence that rehabilitation structures impose fixed biodiversity “fingerprints”. Given the two-year monitoring period, the limited and uneven replication, the absence of a burned untreated control, and the potential contribution of residual site and burn severity differences, longer-term and more highly replicated monitoring will be necessary to determine whether these early patterns persist, converge, or disappear over time. Within these constraints, this study supports the inclusion of biodiversity and species-level metrics in operational post-fire monitoring, so that structure selection and placement can be evaluated more realistically alongside hazard mitigation objectives.