Journal ArticleDOI
Oxidation‐reduction potentials in a salt marsh: Spatial patterns and interactions with primary production1
TLDR
In this article, a positive feedback loop was proposed to explain the sediment redox condition and S. aZterni$oru production in the tall form of Spurtina alterniflora.Abstract:
Spurtina alterniflora oxidizes the sediments in which it grows through both passive oxygen release and active metabolic processes. Eh is higher in the root zone of this grass than in the sediment below the root zone or in unvegetated sediments. Sediments underlying the tall form of S. aZterniJorcl are more oxidized than those under the short form, and sediment redox condition and S. aZterni$oru production are related through a positive feedback loop. Reducing conditions inhibit aboveground grass production. But also, more productive plants have a greater capacity for sediment oxidation, as shown by the increased Eh in fertilized plots. Waterlogged sediments inhibit plan growth by decreasing passive oxygen release and thereby lowering Eh.read more
Citations
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Journal ArticleDOI
Positive interactions among plants
TL;DR: The evidence for facilitation, the mechanisms by which facilitation operates, and the effects facilitation has on community structure are reviewed.
Journal ArticleDOI
Determinants of Pattern in a New England Salt Marsh Plant Community
TL;DR: Physical disturbance and interspecific competition appear to be major determinants of the spatial pattern of marsh plant communities.
Journal ArticleDOI
Phosphate-solubilizing microorganisms associated with the rhizosphere of mangroves in a semiarid coastal lagoon
TL;DR: The production of organic acids by these mangrove rhizosphere microorganisms as a possible mechanism involved in the solubilization of insoluble calcium phosphate is proposed.
Journal ArticleDOI
Salt Marsh Plant Zonation: The Relative Importance of Competition and Physical Factors
TL;DR: In Carpinteria Salt Marsh, Salicornia virginica (pickleweed) grows at lower marsh elevations than does Arthrocnemum subterminalis (Parish's glasswort), suggesting that conditions for plant growth were best here.
Journal ArticleDOI
Comparative ecology of tidal freshwater and salt marshes
TL;DR: Historically, tidal freshwater environments have been ignored by limnologists because of the presence of oceanic tidal influence, and neglected by marine ecologists because they are bathed by freshwater and inhabited primarily by freshwater organisms.
References
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Journal ArticleDOI
Sulfate reduction in a New England salt marsh1
Robert W. Howarth,John M. Teal +1 more
TL;DR: Sulfate reduction rates were measured for two years in the peat of a salt mars by a radiotracer technique as discussed by the authors, and the integrated annual rate is about 75 mol SO/sub 4/sup 2 -/.m/sup -2/yr/sup 1/
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Production and dynamics of experimentally enriched salt marsh vegetation: Belowground biomass1
Abstract: Root growth increased during the early growing season in Spartina alterniflora salt marsh plots. While fertilization with nitrogenous fertilizer did not affect initial growth, a marked decrease in root biomass followed the spring peak particularly where nutrient doses were highest. A sharp reduction in roots occurred in enriched areas covered by Spartina patens, although, as with S. alterniflora, aboveground biomass increased. Roots disappeared during autumn leaving rhizomes as the only part of the plants to overwinter. The maximum standing crop for roots was 0–2 cm deep, for rhizomes 2–5 cm. Net annual underground production was calculated from annual increments in dead matter belowground. Total production, underground and aboveground, exceeds that of any marine vegetation, ranging from 3,900 to 6,600 g m‒2 yr‒1 in S. alterniflora areas and 3,200 to 6,200 g m‒2 yr‒1 in S. patens areas. Fertilization increased production particularly aboveground where dead plant parts are subject to export.
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Factors Influencing Vascular Plant Zonation in North Carolina Salt Marshes
Journal ArticleDOI
Pyrite: Its Rapid Formation in a Salt Marsh and Its Importance In Ecosystem Metabolism
TL;DR: Pyrite formation in salt-marsh peat occurs more rapidly than is generally thought for any natural system, and the rates of sulfate reduction and ecosystem respiration may be grossly underestimated.