2022
DOI: 10.1016/j.scitotenv.2022.157988
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Linking eutrophication to carbon dioxide and methane emissions from exposed mangrove soils along an urban gradient

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Cited by 22 publications
(5 citation statements)
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References 111 publications
(149 reference statements)
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“…Lastly, several literature gaps are associated with the aforementioned index. First, an identified shortcoming is often the use of CO 2 to measure environmental degradation [42][43][44][45][46]. However, it has been discovered that this proxy does not reflect the whole of human activity and it is not comprehensive enough to represent the environment concerns.…”
Section: Introductionmentioning
confidence: 99%
“…Lastly, several literature gaps are associated with the aforementioned index. First, an identified shortcoming is often the use of CO 2 to measure environmental degradation [42][43][44][45][46]. However, it has been discovered that this proxy does not reflect the whole of human activity and it is not comprehensive enough to represent the environment concerns.…”
Section: Introductionmentioning
confidence: 99%
“…Higher urbanization and eutrophic settings surrounding the microtidal mangrove ) compared to the pristine, mesotidal creek (Chynel et al 2022) also contribute to organic enrichment and increase pCO2 in the microtidal creek. Previous studies found that sediment-atmosphere CO2 fluxes were 3 times lower in the mesotidal creek (~120 mmol m -2 d -1 ) when compared to a nearby eutrophic mangrove (Barroso et al 2022), confirming that pristine mangroves emit less CO2 into the atmosphere than impacted/eutrophic systems. The dry soil-air flux found by Barroso et al (2022) is much higher than the average water-air CO2 emission (38 ± 31 mmol m -2 d -1 ) found by our study but comparable to the CO2 porewaterexchange rates in that system (110 ± 40 mmol m -2 d -1 ) or to the global average for mesotidal mangroves (92 ± 84 mmol m -2 d -1 , Table 5).…”
Section: Porewater-derived Versus Water-atmosphere Co2 Fluxesmentioning
confidence: 65%
“…Sedimentary δ 15 N has also been used to reconstruct the impact and historical changes of human activities on N accumulation. 17 , 55 For example, human sewage input, fertilizers, feces, and other allochthonous OM sources are usually enriched in the heavier 15 N. 56 In addition to the effects of N source input, δ 15 N signatures are often determined by complex biogeochemistry processes (including N fixation, remineralization, nitrification, volatilization, and denitrification). 57 Therefore, the increase in δ 15 N in recent sediments may be related to increased denitrification and inputs from aquaculture wastewater and farm runoff.…”
Section: Discussionmentioning
confidence: 99%