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Fluxes of water, sediments, and biogeochemical compounds in salt marshes

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TLDR
In this article, a review of recent studies on these fluxes and their effects on both ecosystem functioning and morphological evolution of salt marshes is presented, with particular emphasis on the uptake by marsh macrophytes and diatoms.
Abstract
Tidal oscillations systematically flood salt marshes, transporting water, sediments, organic matter, and biogeochemical elements such as silica. Here we present a review of recent studies on these fluxes and their effects on both ecosystem functioning and morphological evolution of salt marshes. We reexamine a simplified model for the computation of water fluxes in salt marshes that captures the asymmetry in discharge between flood and ebb. We discuss the role of storm conditions on sediment fluxes both in tidal channels and on the marsh platform. We present recent methods and field instruments for the measurement of fluxes of organic matter. These methods will provide long-term data sets with fine temporal resolution that will help scientists to close the carbon budget in salt marshes. Finally, the main processes controlling fluxes of biogenic and dissolved silica in salt marshes are explained, with particular emphasis on the uptake by marsh macrophytes and diatoms.

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Microplastics affect sedimentary microbial communities and nitrogen cycling.

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Landscape evolution in tidal embayments: modeling the interplay of erosion, sedimentation, and vegetation dynamics

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Impact of climate change on UK estuaries: A review of past trends and potential projections

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Dual role of salt marsh retreat: Long-term loss and short-term resilience

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On the ecogeomorphological feedbacks that control tidal channel network evolution in a sandy mangrove setting

TL;DR: The modelling results presented here indicate the critical control exerted by ecogeomorphological interactions in driving landscape evolution.
References
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Journal ArticleDOI

Responses of coastal wetlands to rising sea level

TL;DR: In this paper, the authors show that the long-term stability of salt marsh ecosystems is explained by interactions among sea level, land elevation, primary production, and sediment accretion that regulate the elevation of the sediment surface toward an equilibrium with mean sea level.
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Global carbon sequestration in tidal, saline wetland soils

TL;DR: In this article, the average soil carbon density of mangrove swamps (0.055 ± 0.004 g cm−3) is significantly higher than the salt marsh average ( 0.039 − 0.003 g cm −3) due to increased decay rates at higher temperatures.
Journal ArticleDOI

Drag, turbulence, and diffusion in flow through emergent vegetation

TL;DR: In this article, a model is developed to describe the drag, turbulence and diffusion for flow through emergent vegetation, which for the first time captures the relevant underlying physics, and covers the natural range of vegetation density and stem Reynolds' numbers.
Journal ArticleDOI

Major role of marine vegetation on the oceanic carbon cycle

TL;DR: In this paper, a bottom-up approach derived from upscaling a compilation of published individual estimates of carbon burial in vegetated habitats (seagrass meadows, salt marshes, and mangrove forests) to the global level and a top-down approach derived derived from considerations of global sediment balance and the organic carbon content of vegeatated sediments was evaluated.
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