The study site is located at Haikou, Checheng Township, Pingtung County, southern Taiwan (22°5^′21.830^′′ N, 120°42^′42.408^′′ E; Fig. 1). Haikou has a tropical climate. According to observations from the Checheng Weather Station (120.7162° E, 22.0744° N; Fig. 1c), mean monthly air temperatures during 2022–2023 ranged from 21.0 to 29.2 °C, monthly total precipitation ranged from 0.5 to 318.8 mm, and mean monthly wind speeds ranged from 1.5 to 5.9 m s⁻¹ (Fig. 2). The study was conducted in a natural subtidal seagrass meadow covering approximately 4.38 ha and dominated by Thalassia hemprichii and Halophila pinifolia. According to the seagrass survey reported by Lin et al. (2023), the meadow had a mean seagrass cover of approximately 66 %, with seasonal estimates ranging from approximately 45 % to 90 %. Water depth at the seagrass and bare sand sites varied with the tidal cycle, ranging from approximately 0.5 m at low tide to 1.5 m at high tide. Figure 3 presents a conceptual diagram of the study area, in which the seagrass meadow is bordered seaward by a reef platform, beyond which the water depth increases sharply to approximately 10 m, forming the adjacent offshore coastal waters, hereafter referred to as the coastal water site.

Field investigations were conducted from 19 to 23 May (spring) and 26 September to 4 October (autumn) in 2022, and from 13 to 17 June (summer) in 2023. Winter fieldwork could not be conducted because of severe weather conditions. Surface water samples were collected at both the coastal water site and within the Haikou seagrass meadow during both daytime and nighttime across different seasons to examine the diurnal and seasonal variability of sea-to-air CH₄ fluxes. In situ benthic chamber incubations were conducted simultaneously in the Haikou seagrass meadow and adjacent unvegetated bare sand areas during both daytime and nighttime to investigate the diurnal and seasonal variability of sediment-to-water CH₄ fluxes under changing environmental conditions. Both incubation sites were located in the subtidal zone and experienced similar tidal depth variations. During each field campaign, porewater samples were also collected from the seagrass meadow and adjacent unvegetated bare sand sediments.

In situ benthic incubation experiments were conducted at four sites, including two seagrass meadow sites and two bare sand sites (Fig. 1b), to quantify changes in seawater chemical parameters influenced by sediments and benthic organisms in areas with and without seagrass. The closed chambers prevented interference from water exchange and water-air interactions. Designed to preserve the natural structure of aquatic plants and sediment surfaces, the chambers also ensured proper fluid dynamics without altering flow patterns when the lid was closed (Webb and Eyre, 2004). Each benthic chamber measured 40 cm in height and 32 cm in diameter (Fig. 4c). Its transparent structure allowed sunlight to penetrate, ensuring that the organisms and plants inside were not affected by shading. Before incubation, all chambers were left open for at least two hours to facilitate water exchange.

The in situ benthic incubation experiments were conducted during both day and night, with incubation durations adjusted according to seasonal weather and sea conditions. In spring, nighttime incubations were conducted for 5 h, whereas daytime incubations were limited to 3 h due to unfavorable conditions during the rainy season. In summer, both daytime and nighttime incubations were conducted for 5 h. In autumn, unstable storm conditions restricted the incubation period to 2 h. A magnetic agitator was placed inside each chamber to maintain continuous water circulation during incubation (Fig. 4d).

Incubation water was collected through a three-way valve installed on each chamber at the beginning and end of each incubation for benthic flux calculations. Ambient surface seawater surrounding the incubation setups in the seagrass bed was collected seven times a day at 06:00, 09:00, 12:00, 15:00, 18:00, 21:00, and 24:00. Surface seawater samples were also collected from the coastal water site outside the reef platform at the same times, except at 21:00 and 24:00 due to safety concerns.

Surface and chamber water samples for CH₄ analysis were collected in duplicate using 120 mL brown serum bottles. Bottles were rinsed twice with sample water, filled to slight overflow, and preserved with 200 µL of saturated mercuric chloride (HgCl₂) to inhibit microbial activity. After sealing with a butyl rubber stopper and aluminum cap, the bottles were shaken to mix, placed in an ice-filled cooler, transported to the laboratory, and stored at 4 °C in the dark.

Porewater samples were collected using porewater wells and a Luer-Lok syringe at sediment depths of 0, 2, 4, 6, 8, 12, 16, and 20 cm following the method of Falter and Sansone (2000). Samples were immediately transferred into 30 mL brown serum bottles, preserved with 50 µL HgCl₂, sealed with butyl rubber stoppers and aluminum caps, placed on ice in a dark cooler during transport, and stored at 4 °C in dark until analysis. Porewater samples were collected from both the seagrass meadow and bare sand sediments at locations separate from the chamber incubation sites to avoid disturbing the ongoing benthic chamber incubations. All seawater and porewater samples were analyzed within two months of collection.

At each water-sampling, water temperature, salinity, and dissolved oxygen (DO) were measured on-site using a portable multiparameter water quality meter (YSI ProDSS, USA), concurrently with the collection of discrete water samples for CH₄ analysis. Dissolved CH₄ concentrations were determined in the laboratory using the headspace technique (Weiss, 1981) and analyzed with a gas chromatograph (GC; Agilent 7890, USA) equipped with a flame ionization detector (FID). Detailed information on column configurations and calibration procedures can be found in Tseng et al. (2022).

CH₄ fluxes at the sea–air interface was calculated using the equation: 1Fsea-air=k×(Cobs-Ceq) where Cobs represents the observed concentration of dissolved CH₄ in seawater, Ceq denotes the expected equilibrium concentration and k is the gas exchange coefficient. The equilibrium CH₄ concentration was estimated using the solubility equation of Wiesenburg and Guinasso (1979), incorporating in-situ temperature, salinity, and atmospheric CH₄ molar fractions. Atmospheric CH₄ data for May, September, and October 2022, along with June 2023, were sourced from the NOAA Global Monitoring Laboratory (Lan et al., 2026).

The gas exchange coefficient was determined following Wanninkhof (2014): 2k=0.251×u2×Sc660-0.5 Here, Sc is the Schmidt number for CH₄, and u represents wind speed (m s⁻¹). Monthly wind speed data were obtained from the Checheng Weather Station (120.7162° E, 22.0744° N), operated by Taiwan's Central Weather Administration.

Benthic CH₄ production rates and sediment-to-water fluxes were measured with chambers inserted 10–15 cm into the sediment (Roth et al., 2019). Seawater samples from the chambers were taken at 2 to 5 h depending on seasonal weather and sea conditions, as described in Sect. 2.2. Benthic CH₄ production rates and sediment-to-water fluxes were calculated from the change in CH₄ concentration in the overlying chamber water during the incubation period using the following equations: 3Production rate=ΔCΔt4Fsediment-water=ΔCΔt×VchamberAchamber where Fsediment-water is sediment-to-water flux (µmol m⁻² h⁻¹ or µmol m⁻² d⁻¹); ΔC represent the differences in CH₄ concentration (nmol L⁻¹), during the incubation period Δt (h); Vchamber is the volume of overlying water in the chamber (m³); Achamber is the area of the chamber (m²). Here, benthic CH₄ production rate refers to the net accumulation rate of CH₄ concentration in the overlying chamber water during incubation and does not represent gross CH₄ production within the sediment.

Surface water temperatures ranged from 24.6 to 32.0 °C. Daytime and nighttime mean temperatures ranged from 28.3–30.0 °C and 26.1–28.5 °C, respectively, in the seagrass meadow, and from 28.7–29.6 °C and 26.3–29.2 °C, respectively, in the coastal water. Seasonal mean temperatures ranged from 27.2 to 29.1 °C in the seagrass meadow and from 27.5 to 29.4 °C in the coastal water (Table 1). Daytime surface water temperatures were higher than nighttime temperatures (Fig. 5a). Salinity ranged from 30.21 to 33.73, with seasonal mean values slightly lower in the seagrass meadow (31.94–32.88) than in the adjacent coastal waters (32.12–33.06; Fig. 5b). This difference may reflect the influence of rainfall, with average monthly precipitation ranging from 156 to 261 mm during the study period (Fig. 2). DO saturation in the seagrass meadow exhibited pronounced diurnal variation (Fig. 5c), increasing from nighttime averages of 87.0 %–94.5 % to daytime averages of 109.3 %–124.4 % (Table 1), likely driven by seagrass photosynthesis. In contrast, DO saturation in the coastal water was relatively stable, ranging from nighttime averages of 97.0 %–99.3 % to daytime averages of 100.5 %–107.5 % (Table 1). Seasonal mean DO saturation ranged from 98.9 % to 109.4 % in the seagrass meadow, slightly higher than that in the coastal water (99.9 %–102.8 %; Table 1).

Mean surface CH₄ concentrations were higher in the seagrass meadow than in the adjacent coastal water (Fig. 5d). Concentrations in the seagrass meadow ranged from 6.6 to 8.3 nM during the daytime and from 6.9 to 13.1 nM at night, whereas those in the coastal water ranged from 5.4 to 7.4 nM and from 4.2 to 5.4 nM, respectively. Seasonal mean CH₄ concentrations were also higher in the seagrass meadow (7.6–9.9 nM) than in the coastal water (4.9–6.0 nM; Table 1).

Sea-to-air CH₄ fluxes exhibited distinct spatial and seasonal patterns, influenced by both surface CH₄ concentrations and wind speed. Monthly mean wind speeds recorded at the Checheng Weather Station were 3.2 m s⁻¹ in spring 2022, 2.2 m s⁻¹ in summer 2023 and 2.6–5.4 m s⁻¹ in autumn 2022 (Table 1). Correspondingly, CH₄ sea-to-air fluxes were higher in the seagrass meadow than in the coastal water across all seasons and times of day (Figs. 6a and 7a). In both habitats, the highest sea-to-air CH₄ fluxes occurred in autumn 2022, averaging 6.8±3.1 µmol m⁻² d⁻¹ in the seagrass meadow and 4.9±5.2 µmol m⁻² d⁻¹ in the coastal water (Fig. 7a). In spring 2022, mean CH₄ fluxes decreased to 5.4±3.0 µmol m⁻² d⁻¹ in the seagrass meadow and 2.3±0.1 µmol m⁻² d⁻¹ in the coastal water (Fig. 7a). The lowest fluxes were observed in summer 2023, averaging 2.5±0.8 µmol m⁻² d⁻¹ in the seagrass meadow and 0.9±0.3 µmol m⁻² d⁻¹ in the coastal water (Fig. 7a). This seasonal pattern was consistent with the observed variation in wind speed (Table 1).

For the sediment-to-water CH₄ flux measurements, incubations were conducted at four sites, including two seagrass sites and two adjacent unvegetated bare sand sites. Incubation chambers were deployed at each site, and duplicate water samples were collected from each chamber at the beginning and end of each incubation for CH₄ analysis. Across the incubation experiments conducted in spring, summer, and autumn, a total of 284 water samples were collected and used to calculate sediment-to-water CH₄ fluxes.

CH₄ benthic fluxes were slightly higher at night than during the day in the seagrass meadow during spring and summer (Fig. 6b). Nighttime sediment incubations were not performed during autumn 2022 because storm event prevented field measurements. In the seagrass meadow, CH₄ production rates and sediment-to-water fluxes were 102.9±20.2 µmol m⁻³ d⁻¹ and 41.2±8.2 µmol m⁻² d⁻¹ in spring, 295.0±35.1 µmol m⁻³ d⁻¹ and 118.0±14.0 µmol m⁻² d⁻¹ in summer, and 263.3±710.4 µmol m⁻³ d⁻¹ and 105.3±284.2 µmol m⁻² d⁻¹ in autumn, respectively (Table 2). Overall, CH₄ production rates and sediment-to-water fluxes in the seagrass meadow remained relatively consistent seasonal patterns, although greater variability was observed in autumn (Fig. 7b). In contrast, bare sand sediments maintained relatively low CH₄ production rates and sediment-to-water fluxes during spring and summer but exhibited a marked increase in autumn (Fig. 7b). In spring, the CH₄ production rate was 42.1±11.1 µmol m⁻³ d⁻¹, with a sediment-to-water flux of 16.9±4.5 µmol m⁻² d⁻¹. In summer, the CH₄ production rate was 114.0±30.6 µmol m⁻³ d⁻¹, with a sediment-to-water flux of 45.6±12.2 µmol m⁻² d⁻¹. In autumn, the CH₄ production rate was substantially higher, reaching 972.2±957.1 µmol m⁻³ d⁻¹, accompanied by a sediment-to-water flux of 388.9±382.8 µmol m⁻² d⁻¹ (Table 2).

Porewater CH₄ concentrations ranged from 9.3–282.0 nM in spring 2022, 6.1–256.0 nM in summer 2023, and 9.1–190.3 nM in autumn 2022 in sandy sediments. In seagrass sediments, mean porewater CH₄ concentrations ranged from 8.1–92.0 nM in spring 2022, 11.8–364.8 nM in summer 2023 and 6.7–262.1 nM in autumn 2022 (Fig. 8). These patterns broadly corresponding to the observed benthic CH₄ production rates and sediment-to-water fluxes (Table 2). In seagrass sediments, porewater CH₄ concentrations varied with depth, with mean concentrations generally highest within the upper 0–12 cm across all sampling campaigns, before declining below 12 cm depth. Seasonal differences were also evident, with the highest porewater CH₄ concentration recorded during autumn 2022 (423.2 nM), followed by summer 2023 (364.8 nM), whereas spring 2022 exhibited comparatively lower concentrations throughout most of the sediment profile (Fig. 8). Seagrass sediments exhibited higher porewater CH₄ concentrations than bare sand sediments in summer 2023 and autumn 2022, particularly within the upper 12 cm of the sediment column (Fig. 8b and c). However, this pattern was reversed in spring 2022, when bare sand sediments exhibited higher porewater CH₄ concentrations than seagrass sediments below 10 cm depth (Fig. 8a). In bare sand sediments, porewater CH₄ concentrations also varied with depth, although vertical gradients were less consistent among seasons than those observed in seagrass sediments. Concentrations generally remained within a narrower range across the sediment profile (Fig. 8).

Dissolved CH₄ concentrations in the seagrass meadow exhibited diurnal variability, with surface waters peaking at night in spring 2022 and summer 2023 (Fig. 5d). This pattern likely reflects the influence of daytime photosynthesis, which increased DO saturation and may have suppressed CH₄ production or enhanced aerobic CH₄ oxidation, thereby limiting CH₄ accumulation in the water column. In contrast, lower nighttime DO saturation reduced oxidation potential and allowed sediment-derived CH₄ to accumulate in the shallow water column. However, the exception occurred during autumn 2022, when the typical diurnal pattern was disrupted by a nighttime storm event characterized by heavy rainfall and strong winds. Elevated wind speeds likely enhanced turbulence, vertical mixing, and air–water gas exchange, promoting rapid physical degassing of dissolved CH₄ and resulting in substantially lower nighttime concentrations than those observed during the other sampling periods. This finding highlights the importance of episodic weather events in regulating short-term CH₄ dynamics in shallow coastal ecosystems.

Compared with the seagrass meadow, the adjacent coastal waters exhibited lower and less variable dissolved CH₄ concentrations in the surface water. This contrast is likely attributable to the substantially greater water depth (approximately 10 m) at the adjacent coastal water site, which reduces the influence of sediment-derived CH₄ on surface waters. In contrast, the shallow water depth (0.5–1.5 m) within the seagrass meadow facilitates the transport of benthic CH₄ to the surface, resulting in higher dissolved CH₄ concentrations in the surface water. Although no significant seasonal differences in surface CH₄ concentrations were observed in either sampling sites, both the seagrass meadow and adjacent coastal waters acted as net sources of atmospheric CH₄ throughout the study period. Mean sea-to-air CH₄ fluxes were higher in the seagrass meadow (4.9±2.2 µmol m⁻² d⁻¹) than in the adjacent coastal waters (2.7±2.0 µmol m⁻² d⁻¹; Table 1), indicating that seagrass habitats function as localized CH₄ emission hotspots. These estimates, however, should be interpreted as seasonal baseline fluxes rather than annual budgets because winter sampling could not be conducted due to severe weather conditions, and the autumn observations were strongly influenced by an extreme storm event. The absence of significant seasonal changes in dissolved CH₄ concentrations further suggests that seasonal variability in sea-to-air CH₄ fluxes was primarily governed by changes in wind speed rather than by variations in dissolved CH₄ concentrations, highlighting the dominant role of physical gas transfer in regulating atmospheric CH₄ emissions. Although seagrass meadows are widely recognized for their capacity to sequester carbon over long timescales (Duarte et al., 2013; Fourqurean et al., 2012; Mcleod et al., 2011), our findings demonstrate that they also function as localized atmospheric CH₄ sources. These results emphasize that evaluations of the climate benefits of seagrass ecosystems should consider both their carbon sequestration capacity and their CH₄ emissions, particularly as changes in hydrodynamic conditions and extreme weather events may alter CH₄ exchange between sediment, water and the atmosphere.

CH₄ production and benthic fluxes in the seagrass meadow exhibited seasonal variability, with the lowest rates occurring in spring and substantially higher rates during summer and autumn (Fig. 7b). This seasonal pattern is likely driven by changes in hydrodynamic conditions that regulate organic matter accumulation within the meadow. At Haikou, strong winds and wave action prevail from October to April (Fig. 2), limiting the deposition and retention of organic particles within the seagrass bed. Consequently, the availability of organic substrates for methanogenesis is reduced, resulting in relatively low benthic CH₄ production and sediment-to-water fluxes during spring. In contrast, calmer conditions beginning in late spring and early summer favor the deposition and accumulation of organic matter, including seagrass detritus and epiphytic material, within the sediment. The enhanced availability of labile organic carbon likely stimulates microbial decomposition and methanogenesis, leading to the elevated benthic CH₄ production rates and sediment-to-water fluxes observed during summer and autumn.

The seasonal increase in benthic CH₄ production is supported by the porewater CH₄ profiles, which showed higher concentrations during summer and autumn (Fig. 8). According to Tang et al. (2025), sediments in the Haikou seagrass meadow contain an average total organic carbon content of approximately 0.40 %, with organic matter derived predominantly from marine sources, including aquatic plant material and microbial processing. The accumulation of this organic substrate provides the fuel required for microbial methanogenesis and likely explains the elevated porewater CH₄ concentrations observed during the warmer seasons.

Porewater CH₄ concentrations were consistently higher than those in the overlying water, indicating that sediment diffusion represented the primary pathway supplying CH₄ to the water column (Yu et al., 2024). However, only a fraction of the CH₄ produced in sediments is ultimately emitted to the atmosphere because substantial oxidation can occur before reaching the water surface. In addition, the decline in porewater CH₄ concentrations with sediment depth observed in this study is consistent with previous findings that sulfate-dependent anaerobic oxidation of CH₄ and competition for electron acceptors can limit CH₄ accumulation in deeper anoxic sediments (Rissanen et al., 2017). Although diffusion was the dominant transport pathway quantified in this study, ebullition may also contribute to CH₄ release when porewater CH₄ partial pressure exceeds hydrostatic pressure, allowing CH₄ bubbles to bypass oxidation within the sediment and water column (Sun et al., 2022). Therefore, the observed porewater CH₄ distributions likely reflect a dynamic balance among organic matter availability, microbial methanogenesis, aerobic and anaerobic CH₄ oxidation, and multiple transport pathways from sediment to the overlying water (Henriksson et al., 2024; Yau et al., 2023).

Overall, these findings indicate that seasonal hydrodynamic conditions indirectly regulate CH₄ emissions from the seagrass meadow by controlling the accumulation of organic matter available for methanogenesis. The combination of enhanced organic carbon deposition during calm periods, active microbial CH₄ production, and sediment-to-water transport explains the elevated sediment-to-water CH₄ fluxes observed during summer and autumn, while subsequent oxidation within the sediment and water column moderates the fraction of CH₄ ultimately released to the atmosphere.

In situ benthic chamber incubations demonstrated differences in CH₄ dynamics between seagrass and adjacent bare sand sediments. During both daytime and nighttime in spring 2022 and summer 2023, benthic CH₄ production rates and sediment-to-water fluxes were higher in seagrass sediments than in adjacent bare sand sediments (Figs. 6b and 7b). These differences reflect fundamental ecological and microbial contrasts between vegetated and unvegetated habitats. Seagrass meadows are highly productive ecosystems that contribute substantial quantities of organic matter to the sediments, providing abundant substrates for microbial decomposition and methanogenesis (Yau et al., 2023). In addition, seagrass roots modify sediment biogeochemistry by regulating oxygen availability and shaping microbial community composition, thereby influencing the balance between methanogenic archaea and methanotrophic bacteria (George et al., 2020). Liang et al. (2025) further demonstrated that seagrass sediments harbor a higher abundance of methanogenic archaea than adjacent unvegetated sediments, providing a microbial basis for the elevated CH₄ production observed in this study. Reduced oxygen penetration within the rhizosphere, together with active microbial communities, further promotes methanogenesis (Henriksson et al., 2024). Moreover, seagrass plants possess specialized gas-conducting tissues (aerenchyma) that facilitate internal gas transport. While these tissues primarily transport oxygen to belowground tissues, they can also provide pathways for sediment-derived CH₄ to diffuse or escape into the overlying water column, thereby enhancing CH₄ emissions from seagrass habitats (Yau et al., 2023; Li et al., 2021). Collectively, these biological and biogeochemical processes explain why seagrass sediments generally support higher CH₄ production and more sustained sediment-to-water fluxes than adjacent bare sand sediments (George et al., 2020; Schorn et al., 2022).

An exception to this general pattern occurred during the autumn 2022 sampling, when daytime benthic CH₄ production rates and sediment-to-water fluxes in bare sand sediments exceeded those in the seagrass meadow, while nighttime incubations could not be conducted because of the storm event (Fig. 6b). This anomaly was likely caused by heavy rainfall and strong winds that disturbed the unvegetated sandy sediments, promoting sediment resuspension and the rapid release of porewater CH₄. In contrast, the dense root and rhizome network of seagrasses stabilizes sediments and buffers against physical disturbance, making vegetated sediments less susceptible to storm-induced CH₄ pulses despite their generally higher background CH₄ production.

These contrasting responses were also reflected in the seasonal averages. Mean sediment-to-water CH₄ fluxes were 88.2±41.2 µmol m⁻² d⁻¹ in the seagrass meadow and 150.4±207.0 µmol m⁻² d⁻¹ in the adjacent bare sand sediments (Table 2). However, the higher seasonal mean for bare sand sediments was largely driven by the exceptionally high emissions recorded during the storm-affected autumn sampling. Excluding this episodic event, seagrass sediments exhibited higher baseline CH₄ production and sediment-to-water fluxes, whereas bare sand sediments generally maintained much lower emissions. These findings indicate that seagrass sediments function as persistent CH₄ sources sustained by continuous organic matter decomposition and microbial methanogenesis, whereas unvegetated bare sand sediments are characterized by relatively low background emissions punctuated by irregular, disturbance-driven CH₄ pulses. As climate change is projected to increase the intensity and frequency of typhoons and other extreme weather events (IPCC, 2021), episodic CH₄ release from unvegetated coastal sediments may become an increasingly important component of coastal GHG budgets, even though seagrass meadows remain the dominant long-term hotspots for benthic CH₄ production.

Despite acting as a net atmospheric CH₄ source, sediment-to-water CH₄ fluxes in the seagrass meadow were one to two orders of magnitude greater than the corresponding sea-to-air fluxes, indicating a substantial decoupling between benthic CH₄ production and atmospheric emissions. A simple mass-balance comparison further demonstrates that only a small fraction of sediment-derived CH₄ ultimately escaped to the atmosphere. Based on the estimated meadow area (4.38 ha) and an average water depth of 1 m, sediments released approximately 162, 465, and 415 mol CH₄ into the overlying water column during spring, summer, and autumn, respectively. In comparison, only 21, 10, and 27 mol CH₄ were emitted to the atmosphere during the corresponding sampling periods. Consequently, approximately 87 % of sediment-derived CH₄ in spring, 98 % in summer, and 94 % in autumn did not reach the atmosphere directly. Instead, much of this CH₄ was likely transported laterally by tidal exchange and coastal circulation, while a smaller fraction was consumed through microbial oxidation within the sediment and water column before atmospheric release. The relatively small standing stock of dissolved CH₄ in the water column (0.33–0.43 mol across seasons), despite substantial benthic inputs, further supports the rapid turnover and efficient redistribution of CH₄ within this shallow, hydrodynamically active seagrass ecosystem.

These findings demonstrate that benthic CH₄ production cannot be directly translated into atmospheric emissions. Rather, the fate of sediment-derived CH₄ is primarily governed by lateral transport driven by tidal exchange and coastal circulation, together with microbial oxidation and physical gas exchange, all of which regulate the fraction ultimately released to the atmosphere. However, this interpretation should be considered in light of several methodological limitations. Although in situ benthic chamber incubations are among the most representative approaches for quantifying sediment-to-water fluxes because they preserve the natural sediment-water interface while maintaining ambient light conditions, hydrodynamics, and biological interactions (Mallon et al., 2022), the chamber environment may still influence measured fluxes. Over the incubation period, changes in oxygen availability and microbial activity can alter CH₄ production and oxidation rates, particularly during longer deployments (Villnas et al., 2012). In addition, environmental conditions within the chamber may become more stable than in the surrounding environment, potentially enhancing photosynthetic activity and metabolic rates (Olivé et al., 2016). Conversely, shading by the chamber and suspended particles may reduce light penetration and photosynthetic efficiency, thereby affecting oxygen production and CH₄ oxidation (Mallon et al., 2022). Although these factors are unlikely to alter the observed habitat-specific and seasonal patterns, they may influence the absolute magnitude of the measured benthic fluxes.

Furthermore, the relative contributions of lateral transport and microbial oxidation could not be quantified directly in this study. Given the shallow water depth (0.5–1.5 m) and frequent tidal exchange within the Haikou seagrass meadow, lateral transport is likely to represent the dominant pathway for removing sediment-derived CH₄ from the meadow before atmospheric emission. Future studies integrating hydrodynamic observations, direct measurements of CH₄ oxidation rates, and continuous flux measurements across tidal cycles will help better constrain the fate of sediment-derived CH₄ and improve GHG budgets for blue carbon ecosystems.

In a broader geographic context, the sea-to-air CH₄ fluxes measured at Haikou were comparable to those reported for seagrass meadows at Koh Mook, Thailand (Halim et al., 2024), and Swan Lake, China (Tan et al., 2025), suggesting similar CH₄ emission characteristics among several Southeast Asian seagrass ecosystems (Table 3). However, the fluxes were substantially lower than those reported from the Chilika Lagoon, India (Banerjee et al., 2018), where tropical seagrass meadows exhibited considerably higher CH₄ emissions that were further enhanced under warming conditions through methylotrophic methanogenesis (Dai et al., 2025). Likewise, studies from the Caribbean have reported elevated CH₄ emissions from organic-rich, anoxic seagrass sediments, although seasonal variability and oxygen transport by seagrass plants can moderate net emissions (Saderne et al., 2023). Globally, seagrass ecosystems are generally recognized as net CH₄ sources, with a mean sea-to-air flux of 79.0 µmol m⁻² d⁻¹ (Eyre et al., 2023), substantially higher than the fluxes observed at Haikou. According to Eyre et al. (2023), the highest CH₄ emissions are typically associated with lagoons and salt marshes, where abundant plant-derived methylated compounds promote methylotrophic methanogenesis.

The sediment-to-water CH₄ fluxes measured in this study also fell within the range reported for other seagrass ecosystems (Table 3). The observed fluxes were comparable to those measured in Enhalus acoroides meadows in Awerange Bay, Indonesia (Alongi et al., 2008), exceeded those reported for Halophila ovalis and Zostera muelleri meadows in Wallis Lake, Australia (Camillini, 2020), but remained lower than fluxes measured in Posidonia australis meadows in Wallis Lake (Camillini, 2020) and seagrass habitats in South Bay, Virginia (Oreska et al., 2020). These differences underscore the importance of local environmental conditions, including sediment organic matter content, redox conditions, hydrodynamics, and nutrient availability, in regulating sediment methanogenesis and CH₄ transport. In addition, species-specific traits, such as belowground biomass, root oxygen release, and organic matter inputs, are likely to contribute to differences in sediment-to-water CH₄ fluxes among seagrass meadows (Garcias-Bonet and Duarte, 2017).

Taken together, these findings highlight the importance of region- and species-specific assessments when evaluating the contribution of seagrass ecosystems to GHG budgets. Tropical seagrass meadows differ fundamentally from temperate systems in their biogeochemical characteristics, microbial processes, and exposure to environmental disturbances, all of which influence CH₄ production and emissions (Pajares et al., 2017). Future studies should integrate microbial community analyses, porewater geochemistry, isotopic tracers, and trait-based approaches to better resolve the mechanisms controlling CH₄ cycling across different seagrass ecosystems. Such efforts are particularly important in tropical regions, where CH₄ emissions have the potential to offset a substantial proportion of the climate mitigation benefits associated with blue carbon storage. Although the sea-to-air CH₄ fluxes measured at Haikou were relatively low compared with the global average, the elevated benthic CH₄ production within the seagrass meadow and the potential for episodic, weather-driven CH₄ release underscore the need for habitat-specific assessments that consider both carbon sequestration and GHG emissions. These findings are consistent with the global synthesis of Eyre et al. (2023), which demonstrated that CH₄ emissions can partially offset the climate mitigation benefits of seagrass ecosystems and therefore should be incorporated into comprehensive blue carbon assessments.