2021
DOI: 10.1029/2020ef001901
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Accelerated Sea‐Level Rise Limits Vegetation Capacity to Sequester Soil Carbon in Coastal Wetlands: A Study Case in Southeastern Australia

Abstract: Mangroves and saltmarshes are recognized to be some of the most carbon-rich environments found throughout the world (Donato et al., 2011;Ouyang & Lee, 2014). In these coastal environments, carbon stocks (also known as blue carbon) are stored in the form of underlying sediments, the living plant biomass, and the non-living plant biomass (J. Howard et al., 2014). Different processes including carbon gas emissions, litter

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Cited by 15 publications
(4 citation statements)
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“…As discussed for Venice Lagoon, it is caused by a much larger increase of the root:shoot quotient along the elevation gradient parameterized in KM12. The discontinuity of the simulated OM accretion at the mangrove-saltmarsh boundary by the DA07 is because the root:shoot quotient of saltmarsh species in the DA07 is set to be higher than that of mangrove species (Kakeh et al, 2016), but these quotient ratios may also vary depending on the hydrodynamic conditions and salinity gradient (Sandi et al, 2021). In Hunter Estuary, the simulated mineral accretion on the platform shows two spatial patterns: the nearly constant rate by the algorithms of F06, T03 and KM12 and the decline rate by the other algorithms (Figure 12c).…”
Section: Simulated Mineral and Om Accretion At The Three Coastal Wetl...mentioning
confidence: 99%
“…As discussed for Venice Lagoon, it is caused by a much larger increase of the root:shoot quotient along the elevation gradient parameterized in KM12. The discontinuity of the simulated OM accretion at the mangrove-saltmarsh boundary by the DA07 is because the root:shoot quotient of saltmarsh species in the DA07 is set to be higher than that of mangrove species (Kakeh et al, 2016), but these quotient ratios may also vary depending on the hydrodynamic conditions and salinity gradient (Sandi et al, 2021). In Hunter Estuary, the simulated mineral accretion on the platform shows two spatial patterns: the nearly constant rate by the algorithms of F06, T03 and KM12 and the decline rate by the other algorithms (Figure 12c).…”
Section: Simulated Mineral and Om Accretion At The Three Coastal Wetl...mentioning
confidence: 99%
“…These models are all useful for planning, however, there is an increasing desire for high precision maps of projected distribution changes to inform planning and decision making at the local scale. There are a range of models that have been developed to project coastal wetland responses to sea-level rise, largely arising from research undertaken in the USA and Europe (Fagherazzi et al, 2012;Fagherazzi et al, 2020;Wiberg et al, 2020), and rarely from locations in the southern hemisphere (Oliver et al, 2012;Rodríguez et al, 2017;Sandi et al, 2021). This is problematic as the sea-level history of coastal wetlands in the southern hemisphere, which has been relatively stable for the past few millennia, contrasts that of the northern hemisphere where shorelines have been highly influenced by glacio-isostatic adjustment (Clark and Lingle, 1979;Khan et al, 2015).…”
Section: Introductionmentioning
confidence: 99%
“…However, climate change and anthropogenic disturbances dramatically alter salt-marsh biomorphodynamic equilibrium, jeopardizing their survival (4,6,21,22), affecting carbon sequestration (23), and even shifting marshes from net sinks to sources of carbon (4,18). Global warming, increased carbon dioxide concentration, and sea-level rise have the potential to alter biomass production, organic soil decomposition and surface accretion (19,21,24,25).…”
Section: Introductionmentioning
confidence: 99%