Biological activity exceeds biogenic structure in influencing sediment nitrogen cycling in experimental oyster reefs

Oysters are estuarine ecosystem engineers, in that their physical structure and biological function affect ecosystem processes such as organic matter and nutrient cycling. Oysters deliver material to the sediments through biodeposition and sedimentation caused by modification of flow around the reef. We conducted an experiment to distinguish between biotic effects and physical structure of oyster reefs on sediment nitrogen cycling. Experimental reefs consisting of live oysters, oyster shells alone and mudflats (controls) were sampled for a period of 4 wk for sediment organic matter, C and N content and fluxes of nitrogen (NH4+, NOX and N2) and oxygen (O2). We hypothesized that the biological activity of the oyster would deposit more, higher quality organic matter compared to deposition from flow modification alone, thus facilitating denitrification and having a larger impact on sediment nitrogen cycling. Compared to the controls, the live oyster experimental reefs increased sediment denitrification by 61% and the shell experimental reefs showed a 24% increase. The live oyster experimental reef also had the largest O2 demand and NH4+ production. Reef structure likely increased organic matter deposition, but the higher quality and larger quantity of organic matter associated with live oysters increased denitrification and microbial respiration. This experiment shows that the ecosystem service of nitrogen removal provided by oysters is primarily driven by the biological function of the oysters and secondarily from the physical structure of the reef. Our increased understanding of how oysters engineer ecosystems and modify nutrient cycling can help guide future oyster restoration efforts

Role of carbonate burial in Blue Carbon budgets

Calcium carbonates (CaCO 3 ) often accumulate in mangrove and seagrass sediments. As CaCO 3 production emits CO 2 , there is concern that this may partially offset the role of Blue Carbon ecosystems as CO 2 sinks through the burial of organic carbon (C org ). A global collection of data on inorganic carbon burial rates (C inorg , 12% of CaCO 3 mass) revealed global rates of 0.8 TgC inorg yr −1 and 15–62 TgC inorg yr −1 in mangrove and seagrass ecosystems, respectively. In seagrass, CaCO 3 burial may correspond to an offset of 30% of the net CO 2 sequestration. However, a mass balance assessment highlights that the C inorg burial is mainly supported by inputs from adjacent ecosystems rather than by local calcification, and that Blue Carbon ecosystems are sites of net CaCO 3 dissolution. Hence, CaCO 3 burial in Blue Carbon ecosystems contribute to seabed elevation and therefore buffers sea-level rise, without undermining their role as CO 2 sinks. © 2019, The Author(s)

Leidenfrost transition temperature for stainless steel meshes

On surfaces well above 100 °C water does not simply boil away. When there is a sufficient heat transfer between the solid and the liquid a continuous vapour layer instantaneous forms under a droplet of water and the drop sits on a cushion of vapour, highly mobile and insulated from the solid surface. This is known as the Leidenfrost effect and the temperature at which this occurs if known as the Leidenfrost transition temperature. In this report, an investigation of discontinuous surfaces, stainless steel meshes, have been tested to determine the effect of the woven material on the Leidenfrost phenomenon. It was found that with increasing the open area of the mesh pushes up the Leidenfrost temperature from 265 °C for an open area of 0.004 mm2 to 315 °C for open area of 0.100 mm2. This allows suppression of the Leidenfrost effect as it can be increase to over 300 °C from 185 °C for a stainless steel surface

Role of carbonate burial in Blue Carbon budgets

Calcium carbonates (CaCO3) often accumulate in mangrove and seagrass sediments. As CaCO3 production emits CO2, there is concern that this may partially offset the role of Blue Carbon ecosystems as CO2 sinks through the burial of organic carbon (Corg). A global collection of data on inorganic carbon burial rates (Cinorg, 12% of CaCO3 mass) revealed global rates of 0.8 TgCinorg yr−1 and 15–62 TgCinorg yr−1 in mangrove and seagrass ecosystems, respectively. In seagrass, CaCO3 burial may correspond to an offset of 30% of the net CO2 sequestration. However, a mass balance assessment highlights that the Cinorg burial is mainly supported by inputs from adjacent ecosystems rather than by local calcification, and that Blue Carbon ecosystems are sites of net CaCO3 dissolution. Hence, CaCO3 burial in Blue Carbon ecosystems contribute to seabed elevation and therefore buffers sea-level rise, without undermining their role as CO2 sinks