Related Experiment Video
Updated: Dec 3, 2025

10:11
The Benthic Exchange of O2, N2 and Dissolved Nutrients Using Small Core Incubations
Published on: August 3, 2016
10.2K
Tidal driven nutrient exchange between mangroves and estuary reveals a dynamic source-sink pattern.
Fenfang Wang1, Peng Cheng2, Nengwang Chen3
1Key Laboratory of the Coastal and Wetland Ecosystems, College of the Environment and Ecology, Xiamen University, Xiamen, 361102, China.
Chemosphere
|October 30, 2020
Summary
Mangroves act as a nutrient source and sink, influencing coastal ecosystems. However, upstream pollution can negate their role in mitigating coastal eutrophication.
Area of Science:
- Coastal Ecology
- Nutrient Biogeochemistry
- Estuarine Science
Background:
- Nitrogen (N) and phosphorus (P) are critical for mangrove productivity and coastal health.
- Limited understanding exists regarding nutrient cycling and mangrove-estuary interactions.
Purpose of the Study:
- To investigate tidal-driven nutrient exchange across the mangrove-estuary interface.
- To determine the source-sink dynamics of nutrients in this critical zone.
Main Methods:
- Quantified lateral nutrient fluxes using hourly concentration data (2016-2018).
- Estimated water mass dynamics with the FVCOM hydrodynamic model.
Main Results:
- Mangroves consistently export ammonium (NH4-N) and dissolved reactive phosphorus (DRP) while acting as a nitrate (NO3-N) sink.
- Dissolved organic nitrogen (DON) and phosphorus (DOP) showed seasonal shifts from source to sink.
- Mangroves reduced overall dissolved inorganic nitrogen (DIN), dissolved total nitrogen (DTN), and total phosphorus (TP) loading to the estuary.
Conclusions:
- Mangroves play a dual role in nutrient cycling, acting as both a source and sink.
- Upstream pollution from aquaculture and sewage can overwhelm the mitigating effects of mangroves, increasing nutrient export.
Related Concept Videos
Primary Production
24.8K
The total amount of energy acquired by primary producers in an ecosystem is called gross primary production (GPP). However, of this energy, producers use some for metabolic processes, and some is lost as heat, decreasing the amount of energy available to the next trophic level. The remaining usable amount of energy is called the net primary productivity (NPP). In terrestrial ecosystems, NPP is driven by climate, while light penetration and nutrient availability drive NPP in aquatic ecosystems.
24.8K
Xylem and Transpiration-driven Transport of Resources
25.7K
The xylem of vascular plants distributes water and dissolved minerals that are taken up by the roots to the rest of the plant. The cells that transport xylem sap are dead upon maturity, and the movement of xylem sap is a passive process.
25.7K
Water and Mineral Acquisition
34.8K
Specialized tissues in plant roots have evolved to capture water, minerals, and some ions from the soil. Roots exhibit a variety of branching patterns that facilitate this process. The outermost root cells have specialized structures called root hairs that increase the root surface, thus increasing soil contact. Water can passively cross into roots, as the concentration of water in the soil is higher than that of the root tissue. Minerals, in contrast, are actively transported into root cells.
34.8K
Osmoregulation in Fishes
52.2K
When cells are placed in a hypotonic (low-salt) fluid, they can swell and burst. Meanwhile, cells in a hypertonic solution—with a higher salt concentration—can shrivel and die. How do fish cells avoid these gruesome fates in hypotonic freshwater or hypertonic seawater environments?
52.2K
Trophic Efficiency
24.0K
Trophic level transfer efficiency (TLTE) is a measure of the total energy transfer from one trophic level to the next. Due to extensive energy loss as metabolic heat, an average of only 10% of the original energy obtained is passed on to the next level. This pattern of energy loss severely limits the possible number of trophic levels in a food chain.
24.0K

