Methane Emissions from Surface of Mangrove River on Hainan Island, China

The surfaces of rivers are considered important sources of atmospheric methane (CH4), however research on this topic is still constrained, especially in freshwater rivers and with the consideration of spatial heterogeneity. Three regions (upper reaches, midstream and downstream) were selected to examine the CH4 fluxes from a freshwater river surface in a mangrove forest wetland from 2012 to 2013, using floating chambers. Results showed that the CH4 fluxes varied significantly among the three regions, with the lowest fluxes at downstream (0.50 ± 0.20 mg m−2 h−1), and highest at upper reaches (1.19 ± 0.36 mg m−2 h−1). The average emission rate at midstream was 0.95 ± 0.37 mg m−2 h−1. The methane flux also varied with seasons, with higher flux in rain-abundant seasons. On average, the CH4 flux in our research river was 0.88 ± 0.31 mg m−2 h−1, which was less than other tropical rivers. In addition, we found that the CH4 flux was significantly correlated with the water characteristics of temperature and atmospheric pressure. Thereby, this study quantified the methane emission from a freshwater river surface in a tropical mangrove forest, enriching the existing knowledge of river surface CH4 flux.

Particulate Organic Carbon in the Tropical Usumacinta River, Southeast Mexico: Concentration, Flux, and Sources

Particulate organic carbon (POC) derived from inland water plays an important role in the global carbon (C) cycle; however, the POC dynamic in tropical rivers is poorly known. We assessed the POC concentration, flux, and sources in the Usumacinta, the largest tropical river in North America, to determine the controls on POC export to the Gulf of Mexico. We examined the Mexican middle and lower Usumacinta Basin during the 2017 dry (DS) and rainy (RS) seasons. The POC concentration ranged from 0.48 to 4.7 mg L−1 and was higher in the RS, though only in the middle basin, while remaining similar in both seasons in the lower basin. The POC was predominantly allochthonous (54.7 to 99.6%). However, autochthonous POC (phytoplankton) increased in the DS (from 5.1 to 17.7%) in both basins. The POC mass inflow–outflow balance suggested that floodplains supply (C source) autochthonous POC during the DS while retaining (C sink) allochthonous POC in the RS. Ranging between 109.1 (DS) and 926.1 t POC d−1 (RS), the Usumacinta River POC export to the Gulf of Mexico was similar to that of other tropical rivers with a comparable water discharge. The extensive floodplains and the “Pantanos de Centla” wetlands in the lowlands largely influenced the POC dynamics and export to the southern Gulf of Mexico.

Phytodiversity and Phytosociology of Riparian Trees Along the Elevation Gradient In The Pamba River, Southern Western Ghats, India

BackgroundThe riparian vegetation along the tropical rivers become threatened due to anthropogenic interference. The tree species diversity and distribution along longitudinal and transversal dimensions is variable and has a pivotal role in the river ecology. The data on the riparian tree species diversity and distribution is inevitable for the nature-based restoration efforts. To test the variability along with the river profile, we investigated the tree species diversity and phytosociology in the tropical river Pamba, Southern Western Ghats. Variation of elevation (701–1923m asl Highrange; 71–700m asl Highland; 8–70m asl Midland and <7.0m asl Lowland) as an indicator of topographic species diversity, we laid a total of 54 × 3 quadrats and data were analyzed with Excel and PC-Ord. ResultsShannon-Wiener's diversity is uniform (1.43689–1.84841) and showed homogeneity (Multiple site similarity index = 0.825396825). Humboldtia vahliana, Neolamarckia cadamba, Vateria indica and Syzygium hemisphericum were showed the highest Importance Value Index. DBH size class (15–>331cm) demonstrated a reverse ‘J’ shaped curve. The tree density and total basal area demonstrated an increasing trend from Lowland to Highrange. Validation of Quadrat data with TWINSPAN and Braun-Blanquet table analysis indicated Ochreinauclea missionis-Ficus hispida-Neolamarckia cadamba in Lowland, Mallotus philippensis-Macaranga peltata-Ficus hispida in Midland, Madhuca neriifolia-Hydnocarpus alpina-Humboldtia vahliana in Highland and Symplocos cochinchinensis var. laurina-Syzygium hemisphericum-Cullenia exarillata in Highrange as dominant stand types. Reciprocal Averaging and Hierarchical Clustering revealed unequivocal classification of quadrats following species composition and elevation. Clumped dispersion was noticed in the Midland and Highland. High regeneration of Madhuca neriifolia, Hopea ponga and Humboldtia vahliana were observed along the elevation gradient.ConclusionsThe present research illustrated that the species diversity of riparian forest in the Pamba river is high and comparable with similar tropical rivers. The phytodiversity, phytosociology and regeneration data are significant for developing a conservation strategy of the anthropogenically fragmented Pamba river. Based on the stand type and regeneration data, Madhuca neriifolia, Hopea ponga, Humboldtia vahliana and Ochreinauclea missionis were suitable for buffer design and restoration along with the Pamba river profile.

Assessment of the dissolved inorganic and organic carbon flux in Cauvery, a tropical river of Southern India.

&lt;p&gt;The carbon fluxes in rivers plays a critical role in the global carbon cycle but its role is always understated. The tropical rivers alone accounts for about 70% of global riverine carbon fluxes due to their large areal extent, varying climatic conditions and land use. Studies on the dissolved carbon fluxes in non-perennial tropical rivers are limited, but it holds much importance as that of perennial rivers. Hence, the present study was carried out with an objective to understand about the inorganic and organic carbon fluxes in a large non-perennial tropical river of Southern India. The samples were collected from 28 locations along the river thrice in a year from 2013-2020 and were analysed for major ions, DIC and DOC. The concentration of DIC in the river water in most of the locations is greater than that of DOC. The DOC concentration is greater at pristine locations thereby decreasing along the flow direction of the river, whereas the DIC concentration increases along the flow direction. The spatial and temporal variability in DOC and DIC concentrations is attributed due to the changes in the rainfall, river flow, climate, lithology, land use patterns, in the catchment. The DIC concentration was found to be majorly governed by silicate and carbonate weathering along with biogenic process, mineralisation and other river process, whereas the primary production, microbial process along with soil organic carbon influences the DOC concentration in the rivers. Thus, this study identifies the sources of DIC and DOC in rivers and the processes which influences the carbon export to the sea.&lt;/p&gt;