Coastal agricultural landscapes: Mapping and understanding grazing intensity on Welsh saltmarshes

Coastal wetlands such as saltmarshes support local communities and industries through ecosystem services and benefit the well-being of local communities in many regions of the world. Along sheltered temperate and sub-tropical coastlines, saltmarshes provide coastal protection, provision of recreational space and wildlife habitat. Those in northwest Europe provide a valuable resource for local agricultural communities through livestock grazing. Following the departure of the UK from the EU and the related potential changes to agricultural policies and markets, it is timely to evaluate the status of saltmarsh livestock grazing. In particular, knowledge of grazing patterns, policy futures and stakeholder perceptions are required to support traditional cultural practice and the ecological status of saltmarshes. This study focuses on the devolved UK nation of Wales, as it has a strong traditional agricultural and pastoral economy, and a landscape of significant conservation value. Yet there are substantial evidence and knowledge gaps regarding livestock grazing and its saltmarsh impact. We present the first map showing the spatial distribution of saltmarsh grazing practice in the UK. Drawing on insights gathered through an expert workshop and interviews with saltmarsh landowners and managers across Wales (N = 35), the paper discusses the challenges and benefits of coastal grazing on saltmarshes, highlighting the diverse values, personal connection and sense of identity associated with marshes. Interviews reveal deep rooted social and cultural values attributed to saltmarshes by the rural coastal community. The study illustrates the need for an integrated approach to management of saltmarshes, accounting for the social, cultural, economic, and environmental values within decision-making

Faunal mediated carbon export from mangroves in an arid area

The outwelling paradigm argues that mangrove and saltmarsh wetlands export much excess production to downstream marine systems. However, outwelling is difficult to quantify and currently 40–50% of fixed carbon is unaccounted for. Some carbon is thought outwelled through mobile fauna, including fish, which visit and feed on mangrove produce during tidal inundation or early life stages before moving offshore, yet this pathway for carbon outwelling has never been quantified. We studied faunal carbon outwelling in three arid mangroves, where sharp isotopic gradients across the boundary between mangroves and down-stream systems permitted spatial differentiation of source of carbon in animal tissue. Stable isotope analysis (C, N, S) revealed 22–56% of the tissue of tidally migrating fauna was mangrove derived. Estimated consumption rates showed that 1.4% (38 kg C ha−1 yr−1) of annual mangrove litter production was directly consumed by migratory fauna, with <1% potentially exported. We predict that the amount of faunally-outwelled carbon is likely to be highly correlated with biomass of migratory fauna. While this may vary globally, the measured migratory fauna biomass in these arid mangroves was within the range of observations for mangroves across diverse biogeographic ranges and environmental settings. Hence, this study provides a generalized prediction of the relatively weak contribution of faunal migration to carbon outwelling from mangroves and the current proposition, that the unaccounted-for 40–50% of mangrove C is exported as dissolved inorganic carbon, remains plausible.Qatar National Research Foundation, National Priorities Research Programme research grant: NPRP 7 - 1302 - 1 - 24

Rapid Losses of Surface Elevation following Tree Girdling and Cutting in Tropical Mangroves

The importance of mangrove forests in carbon sequestration and coastal protection has been widely acknowledged. Large-scale damage of these forests, caused by hurricanes or clear felling, can enhance vulnerability to erosion, subsidence and rapid carbon losses. However, it is unclear how small-scale logging might impact on mangrove functions and services. We experimentally investigated the impact of small-scale tree removal on surface elevation and carbon dynamics in a mangrove forest at Gazi bay, Kenya. The trees in five plots of a Rhizophora mucronata (Lam.) forest were first girdled and then cut. Another set of five plots at the same site served as controls. Treatment induced significant, rapid subsidence (−32.1±8.4 mm yr−1 compared with surface elevation changes of +4.2±1.4 mm yr−1 in controls). Subsidence in treated plots was likely due to collapse and decomposition of dying roots and sediment compaction as evidenced from increased sediment bulk density. Sediment effluxes of CO2 and CH4 increased significantly, especially their heterotrophic component, suggesting enhanced organic matter decomposition. Estimates of total excess fluxes from treated compared with control plots were 25.3±7.4 tCO2 ha−1 yr−1 (using surface carbon efflux) and 35.6±76.9 tCO2 ha−1 yr−1 (using surface elevation losses and sediment properties). Whilst such losses might not be permanent (provided cut areas recover), observed rapid subsidence and enhanced decomposition of soil sediment organic matter caused by small-scale harvesting offers important lessons for mangrove management. In particular mangrove managers need to carefully consider the trade-offs between extracting mangrove wood and losing other mangrove services, particularly shoreline stabilization, coastal protection and carbon storage

Outwelling from arid mangrove systems is sustained by inwelling of seagrass productivity

Mangrove forest productivity is normally sustained by nutrients from terrestrial runoff, with freshwater inputs driving the resulting outwelling of production, but arid mangroves lack this input. The movement of material between seagrass beds and mangroves was examined using the stable C and N isotopic composition of organisms, sediments and suspended matter in 3 seagrass-mangrove transects in the Arabian Gulf. The isotopic signal of suspended particulate material indicated a mixed origin that did not differ over a spring tide. Filter feeders showed significant 13C enrichment along transects from mangrove forests into seagrass beds, indicating that location within a habitat had a significant effect on isotopic composition. Similarly, 13C of both sediments and grazers increased sharply outside the mangrove forest, suggesting retention of mangrove carbon, although some outwelling was detected, the strength of which was site specific. The lack of freshwater-mediated nutrient inputs suggests any outwelling of mangrove ecosystem productivity must be balanced by inwelling, and isotopic signatures of both sediment grazers and filter feeders found within the mangrove forest confirmed the inwelling of seagrass production. Significant mangrove isotope signals in the tissue of juveniles of fishes commercially harvested offshore indicate ontogenetic movement of carbon. Additional biological movement of mangrove carbon through ontogenetic migration and 'trophic relay' is evidenced by the isotopic signature of juvenile and mature fish captured in waters exiting the mangrove forest, which indicated they fed on mangrove-sustained food webs. This study demonstrates tight coupling between arid mangroves and subtidal seagrass areas and implies that arid mangroves cannot be managed or replanted without consideration of connectivity to downstream systems such as seagrasses.Scopu

Organic Carbon Stocks of Great British Saltmarshes

Funding: This research was finically supported by the Natural Environment Research Council funded Carbon Storage in Intertidal Environments (C-SIDE) project (grant NE/R010846/1) with additional support from the Scottish Blue Forum.Coastal wetlands, such as saltmarshes, are globally widespread and highly effective at capturing and storing 'blue carbon' and have the potential to regulate climate over varying timescales. Yet only Australia and the United States of America have national inventories of organic carbon held within saltmarsh habitats, hindering the development of policies and management strategies to protect and preserve these organic carbon stores. Here we couple a new observational dataset with 4,797 samples from 26 saltmarshes across Great Britain to spatially model organic carbon stored in the soil and the above and belowground biomass of Great British saltmarshes. Using average values derived from the 26 marshes, we deliver first-order estimates of organic carbon stocks across Great Britain's 448 saltmarshes (451.66 km 2 ). The saltmarshes of Great Britain contain 5.20 ± 0.65 Mt of organic carbon, 93% of which is in the soil. On average, the saltmarshes store 11.55 ± 1.56 kg C m -2 with values ranging between 2.24 kg C m -2 and 40.51 kg C m -2 depending on interlinked factors such as geomorphology, organic carbon source, sediment type (mud vs sand), sediment supply, and relative sea level history. These findings affirm that saltmarshes represent the largest intertidal blue carbon store in Great Britian, yet remain an unaccounted for component of the United Kingdom's natural carbon stores.Publisher PDFPeer reviewe