Photosynthetic Variables Estimation in a Mangrove Forest

Paramanik, Somnath; Varghese, Roma; Barnwal, Surbhi; Behera, Soumit K.; Bhattyacharya, Bimal K.

doi:10.1002/9781119788157.ch6

Cited by 3 publications

(1 citation statement)

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“…Ra represents the intensity of light energy, which is converted into chemical energy for organic carbon production in photosynthetic reactions [12]. LAI was closely linked to the carbon uptake, as it indicates the amount of foliage that intercepts light and gas exchange through the stomata [42]. Increasing Ra and LAI promoted GPP (Figure 5a,b), since both factors determine how much plants intercept and convert solar radiation into biomass [43,44].…”

Section: Biophysical Controls Of Carbon Fluxesmentioning

confidence: 99%

Variations in CO2 and CH4 Exchange in Response to Multiple Biophysical Factors from a Mangrove Wetland Park in Southeastern China

et al. 2023

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Mangrove ecosystems can be both significant sources and sinks of greenhouse gases. The restoration of mangrove forests is increasingly used as a natural climate solution tool to mitigate climate change. However, the estimates of carbon exchanges remain unclear, especially from restored mangroves. In this study, we observed the temporal variations in carbon dioxide (CO2) and methane (CH4) fluxes and their biophysical controls for 4 years, based on a closed-path eddy covariance (EC) system. The measurements were conducted in a mangrove wetland park with 14-year-old restored mangroves surrounded by open waters in Guangdong Province, China. The EC measurements showed that the mangrove ecosystem acted as a CO2 source with a net CO2 ecosystem exchange (NEE) of 305 g C m−2 from January 2019 to May 2020 by the 5-m tower measurement. After the tower was adjusted to 10 m, the mangrove showed a CO2 sink with an NEE of −345 g C m−2 from June 2020 to December 2022. The change in tower height influenced the interpretation of interannual trends on NEE. There were no significant interannual trends in the gross primary productivity (GPP) and the ecosystem respiration (Re) values. The change from CO2 source to sink may be attributed to the decrease in land surface proportion by the tower replacement, which reduces the proportion of the mangrove canopy respiration and, therefore, captures lower CO2 fluxes from open waters. The restored mangroves indicated strong CH4 sources of 23.2–26.3 g C m−2 a−1. According to the random forest analysis, the land surface proportion, radiation, and relative humidity were the three most important predictors of NEE, while the CH4 flux was most sensitive to air temperature. Compared to the natural and long-term restored mangroves, this 14-year-old restored mangrove had not yet achieved a maximum carbon sequestration capability. Our study highlights the need for the careful design of long-term observations from restored mangroves and proposes future needs in the context of carbon neutrality.

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