Journal Article10.1023/A:1021166010892
Nitrogen vs. phosphorus limitation across an ecotonal gradient in a mangrove forest
TL;DR: In this paper, a factorial experiment with three nutrient treatment levels (control, N,P) and three zones along a tree-height gradient (fringe, transition, dwarf) on offshore islands in Belize was conducted.
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Abstract: Mangrove forests are characterized by distinctive tree-height gradientsthat reflect complex spatial, within-stand differences in environmentalfactors,including nutrient dynamics, salinity, and tidal inundation, across narrowgradients. To determine patterns of nutrient limitation and the effects ofnutrient availability on plant growth and within-stand nutrient dynamics, weused a factorial experiment with three nutrient treatment levels (control, N,P)and three zones along a tree-height gradient (fringe, transition, dwarf) onoffshore islands in Belize. Transects were laid out perpendicular to theshoreline across a mangrove forest from a fringe stand along the seaward edge,through a stand of intermediate height, into a dwarf stand in the interior ofthe island. At three sites, three trees were fertilized per zone for 2yr. Although there was spatial variability in response, growth byR. mangle was generally nitrogen (N) -limited in thefringe zone;phosphorus (P) -limited in the dwarf zone; and, N- and/or P-limited in thetransition zone. Phosphorus-resorption efficiency decreased in all three zones,and N-resorption efficiency increased in the dwarf zone in response to Penrichment. The addition of N had no effect on either P or N resorptionefficiencies. Belowground decomposition was increased by P enrichment in allzones, whereas N enrichment had no effect. This study demonstrated thatessential nutrients are not uniformly distributed within mangrove ecosystems;that soil fertility can switch from conditions of N to P limitation acrossnarrow ecotonal gradients; and, that not all ecological processes respondsimilarly to, or are limited by, the same nutrient.
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Citations
Iron and sulfur geochemistry in semi-arid mangrove soils (Ceará, Brazil) in relation to seasonal changes and shrimp farming effluents.
Gabriel Nuto Nóbrega,Tiago Osório Ferreira,Ricardo Espíndola Romero,A. G. B. Marques,Xosé Luis Otero +4 more
TL;DR: The data show that both factors (seasonal weather variations and shrimp effluents) play important roles in the geochemical processes that occur in these soils and, thus, may affect their functioning and maintenance.
Nutrient and Physicochemical Properties As Potential Causes of Stress in Mangroves of the Central Red Sea
Abdullahi Bala Alhassan,Mohammed Othman Aljahdali +1 more
TL;DR: This study investigates stress causes in Central Red Sea mangroves, finding significant differences in water salinity, temperature, nutrient content, and antioxidant enzyme activities among six study sites, with nutrient limitation and salinity contributing to stress in all sites.
Shrub Mangroves Facilitate Self‐Sustaining Conditions for Colonization: Insights From the Nanliu Delta, China
Xiaoyan Zhou,Zhijun Dai,Davide Tognin,Jiejun Luo,Riming WANG,Bingbin Feng,Luca Carniello,Xiaoyan Zhou,Zhijun Dai,Davide Tognin,Jiejun Luo,Riming WANG,Bingbin Feng,Luca Carniello +13 more
Abstract: Abstract Shrub mangrove (SM) tidal flats are vital ecosystems in tropical and subtropical regions, yet they are threatened by rising sea levels and anthropogenic activities. With their lower canopy height, SMs influence hydro‐sedimentary processes differently from the well‐studied tree mangroves, highlighting the need for a deeper understanding of the stability of the tidal flats they colonize. Here, we analyze hydrodynamic and sediment transport processes over a full spring‐neap tidal cycle on an Aegiceras corniculatum tidal flat in the Nanliu delta China, to explore the bio‐morphodynamic feedback shaping SM tidal flats. Our findings reveal distinct differences in hydrodynamics and sediment transport between the flood and ebb phases, with the flood phase playing a significantly stronger influence. During the flood phase, the interaction between tidal flow and increasing vegetation density landward results in a significant reduction in flow velocity (up to 36%), particularly concentrated at the vegetation fringe. This reduction diminishes sediment transport capacity (up to 80%), leading to a decline in suspended sediment concentration as it moves landward, resulting in localized deposition in front of the densely vegetated area. This process is further supported by the substantial vertical accretion observed over an annual timescale. Our observations reveal that sediment deposition at the front edge of the dense SM zone is associated with a coarsening of surface sediments, which creates favorable conditions for seedling establishment and drives seaward vegetation expansion. These findings highlight the critical role of SMs in coastal ecosystem resilience and the evolution of tidal flats.
Nutrient Addition Differentially Affects Ecological Processes of Avicennia germinans in Nitrogen versus Phosphorus Limited Mangrove Ecosystems
TL;DR: Fertilization experiments in nitrogen and phosphorus-limited mangrove forests suggested that N- versus P- limited mangroves do have different thresholds and eutrophication is more likely to cause a shift in nutrient limitation at P-limited Twin Cays than N-limited IRL.
Nutrient variability in mangrove soil: anthropogenic, seasonal and depth variation factors
TL;DR: Carbon, nitrogen, phosphorus and potassium analysis showed that they were significantly different in all locations but not between seasons, and the protected mangroves habitat in Johor has siltier and clayey component and can retain more nutrients for the plant growth.
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