Nitrogen Processes Within Tropical Mangroves in Australia

Abstract Coastal wetlands have long been identified as ecosystems that can ameliorate N inputs into the ocean. The processes associated with N uptake, transformation, and losses are relatively well understood for temperate wetlands; however, information on tropical wetlands is scarce. In this study, we conducted a whole ecosystem approach to measure N processes within tropical mangroves in the Moresby estuary in northeast Australia. We measured N stocks (trees and soils), inputs from sedimentation, fixation, and accumulation as woody biomass, and outputs through denitrification, anammox, and soil respiration (N 2 O emissions). Potential denitrification was detected along anammox (average, min‐max) at 883 (485–1,450) gN ha −1 day −1 , followed by sediment accumulation with 108 (0–375) gN ha −1 day −1 , and tree uptake with 93 (13–153) gN ha −1 day −1 . Lower rates were found for N fixation with 45 (0–260) gN ha −1 day −1 and soil respiration as N 2 O with uptakes of −0.36 (−2.7 – 0.40) gN ha −1 day −1 . Overall, mangroves in the Moresby estuary are fixing some N in their standing litter while removing NO 3 and NH 4 + from the water column through denitrification and anammox, temporarily storing N as woody biomass, and accumulating particulate N in their sediments. These mangroves are also functioning as sinks of N 2 O. Thus, the protection and restoration of these mangroves provide water quality and climate benefits.