Abstract

<h2>Summary</h2> We document a substantial increase in global N<sub>2</sub>O emissions from mangroves. Based on our analysis of two decades of mangrove N<sub>2</sub>O emission studies, we estimate N<sub>2</sub>O emission of 0.023 Tg N year<sup>−1</sup> from global mangrove ecosystems. N<sub>2</sub>O fluxes from mangrove ecosystems are strongly increased by sediment dissolved inorganic nitrogen (DIN) concentration transported from river catchments to coastal waters. Continuing growth of nutrient inputs from anthropogenic sources, i.e., agricultural intensification, excessive fertilizer use and waste water discharge, will appreciably increase DIN loading and consequently global N<sub>2</sub>O emission from mangroves. Based on the Millennium Ecosystem Assessment scenarios of riverine DIN inputs into mangrove ecosystems coupled with our estimates of DIN-controlled emissions rates, we expect N<sub>2</sub>O emission to increase by 20%–51% by 2030 and 27%–74% by 2050 compared with estimated emissions in the year 2000. These forecasts underline the urgency of improvements in catchment-scale nitrogen management strategies.

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