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1.
Nitrogen limitation of growth and nutrient dynamics in a disturbed mangrove forest,Indian River Lagoon,Florida 总被引:1,自引:0,他引:1
The objectives of this study were to determine effects of nutrient enrichment on plant growth, nutrient dynamics, and photosynthesis in a disturbed mangrove forest in an abandoned mosquito impoundment in Florida. Impounding altered the hydrology and soil chemistry of the site. In 1997, we established a factorial experiment along a tree-height gradient with three zones, i.e., fringe, transition, dwarf, and three fertilizer treatment levels, i.e., nitrogen (N), phosphorus (P), control, in Mosquito Impoundment 23 on the eastern side of Indian River. Transects traversed the forest perpendicular to the shoreline, from a Rhizophora mangle-dominated fringe through an Avicennia germinans stand of intermediate height, and into a scrub or dwarf stand of A. germinans in the hinterland. Growth rates increased significantly in response to N fertilization. Our growth data indicated that this site is N-limited along the tree-height gradient. After 2 years of N addition, dwarf trees resembled vigorously growing saplings. Addition of N also affected internal dynamics of N and P and caused increases in rates of photosynthesis. These findings contrast with results for a R. mangle-dominated forest in Belize where the fringe is N-limited, but the dwarf zone is P-limited and the transition zone is co-limited by N and P. This study demonstrated that patterns of nutrient limitation in mangrove ecosystems are complex, that not all processes respond similarly to the same nutrient, and that similar habitats are not limited by the same nutrient when different mangrove forests are compared. 相似文献
2.
Complex gradients in forest structure across the landscape of offshore mangrove islands in Belize are associated with nutrient
deficiency and flooding. While nutrient availability can affect many ecological processes, here we investigate how N and P
enrichment interact with forest structure in three distinct zones (fringe, transition, dwarf) to alter patterns of herbivory
as a function of folivory, loss of yield, and tissue mining. The effects of nutrient addition and zone varied by functional
feeding group or specific herbivore. Folivory ranged from 0 to 0.4% leaf area damaged per month, but rates did not vary by
either nutrient enrichment or zone. Leaf lifetime damage ranged from 3 to 10% of the total leaf area and was caused primarily
by the omnivorous tree crab Aratus pisonii. We detected two distinct spatial scales of response by A. pisonii that were unrelated to nutrient treatment, i.e., most feeding damage occurred in the fringe zone and crabs fed primarily
on the oldest leaves in the canopy. Loss of yield caused by the bud moth Ecdytolopha sp. varied by zone but not by nutrient treatment. A periderm-mining Marmara sp. responded positively to nutrient enrichment and closely mirrored the growth response by Rhizophora mangle across the tree height gradient. In contrast, a leaf-mining Marmara sp. was controlled by parasitoids and predators that killed >89% of its larvae. Thus, nutrient availability altered patterns
of herbivory of some but not all mangrove herbivores. These findings support the hypothesis that landscape heterogeneity of
the biotic and abiotic environment has species-specific effects on community structure and trophic interactions. Predicting
how herbivores respond to nutrient over-enrichment in mangrove ecosystems also requires an assessment of habitat heterogeneity
coupled with feeding strategies and species-specific behavior measured on multiple scales of response. 相似文献
3.
Jacob E. Allgeier Amy D. Rosemond 《Journal of experimental marine biology and ecology》2011,407(2):330-336
The traditional model of nutrient availability in coastal estuarine ecosystems is based on predictable inputs of nitrogen (N) and phosphorus (P) via riverine and oceanic sources, respectively. But coastlines with low nutrient input from these sources may not fit into this simple framework. Here we use observational (seagrass nutrient content) and experimental (nutrient enrichment assays) data for assessing nutrient availability and limitation for primary producers along a spatial transect extending from the mouth (nearest to the ocean) to the terminal portion (boundary with the terrestrial ecosystem) of three coastal mangrove-lined tidal creeks in The Bahamas. Compiling seagrass nutrient content from all sites showed a negative relationship between seagrass nutrient limitation (either N or P) and distance from mouth, but this pattern differed across sites with respect to which nutrient was more limiting. Our experimental results demonstrated patterns of decreased response by microalgae to dual nutrient enrichment in one site with distance from the creek mouth, and increased response to single nutrient enrichment in another, with the third showing no trend along this gradient. Our findings show that Bahamian mangrove wetlands are extremely nutrient-limited ecosystems, and that the most limiting nutrient varied among sites. In general, these ecosystems deviate from the typical paradigm of spatial nutrient limitation patterns in estuaries. We suggest that various site-specific biological and physical factors may be more important than large-scale hydrologic factors in driving trends of nutrient availability in coastal ecosystems under strong nutrient constraints, such as in The Bahamas. Our findings suggest that even minor changes in nutrient loading rates can have significant implications for primary production in subtropical oligotrophic systems. 相似文献
4.
Mangrove growth in New Zealand estuaries: the role of nutrient enrichment at sites with contrasting rates of sedimentation 总被引:4,自引:0,他引:4
Lovelock CE Feller IC Ellis J Schwarz AM Hancock N Nichols P Sorrell B 《Oecologia》2007,153(3):633-641
Mangrove forest coverage is increasing in the estuaries of the North Island of New Zealand, causing changes in estuarine ecosystem
structure and function. Sedimentation and associated nutrient enrichment have been proposed to be factors leading to increases
in mangrove cover, but the relative importance of each of these factors is unknown. We conducted a fertilization study in
estuaries with different sedimentation histories in order to determine the role of nutrient enrichment in stimulating mangrove
growth and forest development. We expected that if mangroves were nutrient-limited, nutrient enrichment would lead to increases
in mangrove growth and forest structure and that nutrient enrichment of trees in our site with low sedimentation would give
rise to trees and sediments that converged in terms of functional characteristics on control sites in our high sedimentation
site. The effects of fertilizing with nitrogen (N) varied among sites and across the intertidal zone, with enhancements in
growth, photosynthetic carbon gain, N resorption prior to leaf senescence and the leaf area index of canopies being significantly
greater at the high sedimentation sites than at the low sedimentation sites, and in landward dwarf trees compared to seaward
fringing trees. Sediment respiration (CO2 efflux) was higher at the high sedimentation site than at the low one sedimentation site, but it was not significantly affected
by fertilization, suggesting that the high sedimentation site supported greater bacterial mineralization of sediment carbon.
Nutrient enrichment of the coastal zone has a role in facilitating the expansion of mangroves in estuaries of the North Island
of New Zealand, but this effect is secondary to that of sedimentation, which increases habitat area and stimulates growth.
In estuaries with high sediment loads, enrichment with N will cause greater mangrove growth and further changes in ecosystem
function. 相似文献
5.
Nutrient over-enrichment is a major threat to marine environments, but system-specific attributes of coastal ecosystems may
result in differences in their sensitivity and susceptibility to eutrophication. We used fertilization experiments in nitrogen
(N)- and phosphorus (P)-limited mangrove forests to test the hypothesis that alleviating different kinds of nutrient limitation
may have different effects on ecosystem structure and function in natural systems. We compared a broad range of ecological
processes to determine if these systems have different thresholds where shifts might occur in nutrient limitation. Growth
responses indicated N limitation in Avicennia germinans (black mangrove) forests in the Indian River Lagoon (IRL), Florida, and P limitation at Twin Cays, Belize. When nutrient
deficiency was relieved, A. germinans grew out of its stunted form by increasing wood relative to leaf biomass and shoot length relative to lateral growth. At
the P-limited site, P enrichment (+P) increased specific leaf area, N resorption, and P uptake, but had no effect on P resorption.
At the N-limited site, +N increased both N and P resorption, but did not alter biomass allocation. Herbivory was greater at
the P-limited site and was unaffected by +P, whereas +N led to increased herbivory at the N-limited site. The responses to
nutrient enrichment depended on the ecological process and limiting nutrient and suggested that N- versus P-limited mangroves
do have different thresholds. +P had a greater effect on more ecological processes at Twin Cays than did +N at the IRL, which
indicated that the P-limited site was more sensitive to nutrient loading. Because of this sensitivity, eutrophication is more
likely to cause a shift in nutrient limitation at P-limited Twin Cays than N-limited IRL. 相似文献
6.
Ilka C. Feller Anne H. Chamberlain Cyril Piou Samantha Chapman Catherine E. Lovelock 《Ecosystems》2013,16(7):1203-1215
Ecosystems in the tropics are predicted to have stronger responses to nutrient enrichment, greater diversity, and more intense biotic interactions than in temperate areas. Mangrove forests, which occur across a broad biogeographic range from warm temperate to tropical, provide a unique opportunity to test these hypotheses by investigating the responses of herbivores to nutrient enrichment in temperate versus tropical latitudes. Mangroves are complex intertidal ecosystems with spatial differences in structure and diversity along tidal gradients and are threatened globally by human activities including nutrient over-enrichment. In this study, we used long-term fertilization experiments at the Indian River Lagoon, FL; Twin Cays, Belize; and Bocas del Toro, Panamá to determine how increased nutrients impact herbivore abundance and herbivory of Rhizophora mangle at the tree, forest, and regional scales. At these locations, which span approximately 2185 km and 18.4º of latitude, we fertilized individual trees with one of three treatments (Control, +N, +P) in two zones (fringe, scrub) along transects perpendicular to the shoreline and measured their responses for 4 years. Herbivory was measured as folivory, loss of yield, and tissue mining. Although nutrient enrichment altered plant growth, leaf traits, and nutrient dynamics, these variables had little effect on folivory at any location. Our results did not support the prediction that herbivory and per capita consumption are greatest at the most tropical location. Instead, folivory was highest at the most temperate location and lowest at the intermediate location. Folivory was generally higher in the fringe than in the scrub zone, but the pattern varied by location, herbivore, and nutrient treatment. Folivory by a dominant herbivore, Aratus pisonii, decreased from the highest to the lowest latitude. Our data suggest that factors controlling population dynamics of A. pisonii cascade to the mangrove canopy, linking herbivory to crab densities. 相似文献
7.
P.J. Clarke 《Aquatic Botany》1985,23(3):275-290
The nitrogen status of the soil and plant components of an estuarine wetland near Sydney were investigated over 6 months to detect seasonal and spatial changes in nitrogen content. Organic carbon, organic nitrogen and inorganic nitrogen concentrations were measured in the soil at various depths in six vegetation zones across the wetland. Carbon and nitrogen content of the plant biomass were also determined in each of the zones. Soil redox potentials and pH were measured in situ and both were found to vary with depth and inundation frequency. Organic carbon, organic nitrogen and inorganic nitrogen in the soil decreased significantly from the fringe Casuarina forest (1391 g N m?2) through to the Avicennia mangrove zone (133 g N m?2). Exchangeable NH4+, NO3? and NO2? concentrations from less than 1% of the soil nitrogen pool and vary seasonally. The distinctive feature of the mangrove zone is that the plant component of the total nitrogen pool is large (55%). This contrasts with the saltmarsh and fringe communities, where the plant pools are small (15%) in comparison with the soil. These findings are consistent with the hypothesis that mangroves export organic nutrients whereas the saltmarsh and fringe communities act as nutrient sinks. 相似文献
8.
It is essential to know the nutrient limitation status of biofilms to understand how they may buffer uptake and export of
nutrients from polluted watersheds. We tested the effects of nutrient additions on biofilm biomass (chlorophyll a, ash free dry mass (AFDM), and autotrophic index (AI, AFDM/chl a)) and metabolism via nutrient-diffusing substrate bioassays (control, nitrogen (N), phosphorus (P), and N + P treatments)
at 11 sites in the Upper Snake River basin (southeast Idaho, USA) that differed in the magnitude and extent of human-caused
impacts. Water temperature, turbidity, and dissolved inorganic N concentrations all changed seasonally at the study sites,
while turbidity and dissolved inorganic N and P also varied with impact level. Chl a and AI on control treatments suggested that the most heavily impacted sites supported more autotrophic biofilms than less-impacted
sites, and that across all sites biofilms were more heterotrophic in autumn than in summer. Nutrient stimulation or suppression
of biofilm biomass was observed for chl a in 59% of the experiments and for AFDM in 33%, and the most frequent response noted across all study sites was N limitation.
P suppression of chl a was observed only at the most-impacted sites, while AFDM was never suppressed by nutrients. When nutrient additions did have
significant effects on metabolism, they were driven by differences in biomass rather than by changes in metabolic rates. Our
study demonstrated that biofilms in southeast Idaho rivers were primarily limited by N, but nutrient limitation was more frequent
at sites with good water quality than at those with poor water quality. Additionally, heterotrophic and autotrophic biofilm
components may respond differently to nutrient enrichment, and nutrient limitation of biofilm biomass should not be considered
a surrogate for metabolism in these rivers.
Handling editor: D. Ryder 相似文献
9.
KATHERINE C. MARTIN DAN BRUHN CATHERINE E. LOVELOCK ILKA C. FELLER JOHN R. EVANS MARILYN C. BALL 《Plant, cell & environment》2010,33(3):344-357
Effects of salinity and nutrients on carbon gain in relation to water use were studied in the grey mangrove, Avicennia marina, growing along a natural salinity gradient in south‐eastern Australia. Tall trees characterized areas of seawater salinities (fringe zone) and stunted trees dominated landward hypersaline areas (scrub zone). Trees were fertilized with nitrogen (+N) or phosphorus (+P) or unfertilized. There was no significant effect of +P on shoot growth, whereas +N enhanced canopy development, particularly in scrub trees. Scrub trees maintained greater CO2 assimilation per unit water transpired (water‐use efficiency, WUE) and had lower nitrogen‐use efficiency (NUE; CO2 assimilation rate per unit leaf nitrogen) than fringe trees. The CO2 assimilation rates of +N trees were similar to those in other treatments, but were achieved at lower transpiration rates, stomatal conductance and intercellular CO2 concentrations. Maintaining comparable assimilation rates at lower stomatal conductance requires greater ribulose 1·5‐bisphosphate carboxylase/oxygenase activity, consistent with greater N content per unit leaf area in +N trees. Hence, +N enhanced WUE at the expense of NUE. Instantaneous WUE estimates were supported by less negative foliar δ13C values for +N trees and scrub control trees. Thus, nutrient enrichment may alter the structure and function of mangrove forests along salinity gradients. 相似文献
10.
Consistent nutrient storage and supply mediated by diverse fish communities in coral reef ecosystems
Jacob E. Allgeier Craig A. Layman Peter J. Mumby Amy D. Rosemond 《Global Change Biology》2014,20(8):2459-2472
Corals thrive in low nutrient environments and the conservation of these globally imperiled ecosystems is largely dependent on mitigating the effects of anthropogenic nutrient enrichment. However, to better understand the implications of anthropogenic nutrients requires a heightened understanding of baseline nutrient dynamics within these ecosystems. Here, we provide a novel perspective on coral reef nutrient dynamics by examining the role of fish communities in the supply and storage of nitrogen (N) and phosphorus (P). We quantified fish‐mediated nutrient storage and supply for 144 species and modeled these data onto 172 fish communities (71 729 individual fish), in four types of coral reefs, as well as seagrass and mangrove ecosystems, throughout the Northern Antilles. Fish communities supplied and stored large quantities of nutrients, with rates varying among ecosystem types. The size structure and diversity of the fish communities best predicted N and P supply and storage and N : P supply, suggesting that alterations to fish communities (e.g., overfishing) will have important implications for nutrient dynamics in these systems. The stoichiometric ratio (N : P) for storage in fish mass (~8 : 1) and supply (~20 : 1) was notably consistent across the four coral reef types (but not seagrass or mangrove ecosystems). Published nutrient enrichment studies on corals show that deviations from this N : P supply ratio may be associated with poor coral fitness, providing qualitative support for the hypothesis that corals and their symbionts may be adapted to specific ratios of nutrient supply. Consumer nutrient stoichiometry provides a baseline from which to better understand nutrient dynamics in coral reef and other coastal ecosystems, information that is greatly needed if we are to implement more effective measures to ensure the future health of the world's oceans. 相似文献