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  • 1
    Electronic Resource
    Electronic Resource
    Springer
    Biogeochemistry 1 (1985), S. 383-386 
    ISSN: 1573-515X
    Source: Springer Online Journal Archives 1860-2000
    Topics: Chemistry and Pharmacology , Geosciences
    Type of Medium: Electronic Resource
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  • 2
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] Ecologists have long been intrigued by the ways co-occurring species divide limiting resources. Such resource partitioning, or niche differentiation, may promote species diversity by reducing competition. Although resource partitioning is an important determinant of species diversity and ...
    Type of Medium: Electronic Resource
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  • 3
    Electronic Resource
    Electronic Resource
    Springer
    Biodegradation 10 (1990), S. 309-328 
    ISSN: 1572-9729
    Keywords: estuaries ; groundwater ; nitrogen ; nitrogen cycle ; nitrogen loading
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology , Energy, Environment Protection, Nuclear Power Engineering , Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
    Notes: Abstract We examined the importance of nitrogen inputs from groundwater and runoff in a small coastal marine cove on Cape Cod, MA, USA. We evaluated groundwater inputs by three different methods: a water budget, assuming discharge equals recharge; direct measurements of discharge using bell jars; and a budget of water and salt at the mouth of the Cove over several tidal cycles. The lowest estimates were obtained by using a water budget and the highest estimates were obtained using a budget of water and salt at the Cove mouth. Overall there was more than a five fold difference in the freshwater inputs calculated by using these methods. Nitrogen in groundwater appears to be largely derived from on site septic systems. Average nitrate concentrations were highest in the region where building density was greatest. Nitrate in groundwater appeared to behave conservatively in sandy sediments where groundwater flow rates were high (〉 11/m2/h), indicating that denitrification was not substantially reducing external nitrogen loading to the Cove. Nitrogen inputs from groundwater were approximately 300 mmol-N/m3/y of Cove water. Road runoff contributed an additional 60 mmol/m3/y. Total nitrogen inputs from groundwater and road runoff to this cove were similar in magnitude to river dominated estuaries in urbanized areas in the United States.
    Type of Medium: Electronic Resource
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  • 4
    ISSN: 1573-515X
    Keywords: 34S ; sulfate reduction ; sulfide oxidation ; SO4 addition
    Source: Springer Online Journal Archives 1860-2000
    Topics: Chemistry and Pharmacology , Geosciences
    Notes: Abstract We investigated the effects of sulfate concentration on sulfate reduction and net S storage in lake sediments using34S as a tracer. The water overlying intact sediment cores from the hypolimnion of Mares Pond, MA, was replaced with two Na2 34SO4 solutions at either ambient (70 μM) or elevated (260 μM) sulfate concentrations. The δ34S of the added sulfate was 4974 ‰. Over two months, the net sulfate reduction rate in the ambient sulfate treatment was zero, while the net rate for the high sulfate treatment was 140 μmoles/m2/d. The water overlying the cores was kept under oxic conditions and the sediment received no fresh carbon inputs, thus the net rate reported may underestimate the in situ rate. Gross sulfate reduction rates calculated by isotope dilution were approximately 350 μmoles/m2/d for both treatments. While the calculation of gross sulfate reduction rates in intact sediment cores can be complicated by differential diffusion of34S and32S, isotopic fractionation, and the possible formation of ester sulfates, we believe these effects to be small. The results suggest that sulfate reduction is not strongly sulfate-limited in Mares Pond. The difference in net sulfate reduction rates between treatments resulted from a decrease in sulfide oxidation and suggests the importance of reoxidation in controlling net S storage in lake sediments. In both treatments the CRS and organic S fractions were measurably labelled in34S. Below the sediment surface, the CRS fraction was the more heavily labelled storage product for reduced sulfides.
    Type of Medium: Electronic Resource
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  • 5
    Electronic Resource
    Electronic Resource
    Springer
    Biogeochemistry 35 (1996), S. 235-260 
    ISSN: 1573-515X
    Keywords: benthic mineralization ; continental shelf ; denitrification ; global N cycle ; nitrogen ; North Atlantic ; nutrients ; onwelling ; phytoplankton ; sediments
    Source: Springer Online Journal Archives 1860-2000
    Topics: Chemistry and Pharmacology , Geosciences
    Notes: Abstract A model of coupled nitrification/denitrification was developed for continental shelf sediments to estimate the spatial distribution of denitrification throughout shelf regions in the North Atlantic basin. Using data from a wide range of continental shelf regions, we found a linear relationship between denitrification and sediment oxygen uptake. This relationship was applied to specific continental shelf regions by combining it with a second regression relating sediment oxygen uptake to primary production in the overlying water. The combined equation was: denitrification (mmol N m−2 d−1)=0.019* phytoplankton production (mmol C m−2 d−1). This relationship suggests that approximately 13% of the N incorporated into phytoplankton in shelf waters is eventually denitrified in the sediments via coupled nitrification/denitrification, assuming a C:N ratio of 6.625:1 for phytoplankton. The model calculated denitrification rates compare favorably with rates reported for several shelf regions in the North Atlantic. The model-predicted average denitrification rate for continental shelf sediments in the North Atlantic Basin is 0.69 mmol N m− 2 d−1. Denitrification rates (per unit area) predicted by the model are highest for the continental shelf region in the western North Atlantic between Cape Hatteras and South Florida and lowest for Hudson Bay, the Baffin Island region, and Greenland. Within latitudinal belts, average denitrification rates were lowest in the high latitudes, intermediate in the tropics and highest in the mid-latitudes. Although denitrification rates per unit area are lowest in the high latitudes, the total N removal by denitrification (53 × 1010 mol N y−1) is similar to that in the mid-latitudes (60 × 1010 mol N y−1) due to the large area of continental shelf in the high latitudes. The Gulf of St. Lawrence/Grand Banks area and the North Sea are responsible for seventy-five percent of the denitrification in the high latitude region. N removal by denitrification in the western North Atlantic (96 × 1010 mol N y−1) is two times greater than in the eastern North Atlantic (47 × 1010 mol N y−1). This is primarily due to differences in the area of continental shelf in the two regions, as the average denitrification rate per unit area is similar in the western and eastern North Atlantic. We calculate that a total of 143 × 1010 mol N y−1 is removed via coupled nitrification/denitrification on the North Atlantic continental shelf. This estimate is expected to underestimate total sediment denitrification because it does not include direct denitrification of nitrate from the overlying water. The rate of coupled nitrification/denitrification calculated is greater than the nitrogen inputs from atmospheric deposition and river sources combined, and suggests that onwelling of nutrient rich slope water is a major source of N for denitrification in shelf regions. For the two regions where N inputs to a shelf region from onwelling have been measured, onwelling appears to be able to balance the denitrification loss.
    Type of Medium: Electronic Resource
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  • 6
    Electronic Resource
    Electronic Resource
    Springer
    Water, air & soil pollution 20 (1983), S. 81-98 
    ISSN: 1573-2932
    Source: Springer Online Journal Archives 1860-2000
    Topics: Energy, Environment Protection, Nuclear Power Engineering
    Type of Medium: Electronic Resource
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  • 7
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    Unknown
    PANGAEA
    Publication Date: 2023-02-24
    Keywords: BC; BH02-1; Boston Harbor; Box corer; DEPTH, sediment/rock; Giblin_BH02-1_BC; Gyre; Gyre9007; ORFOIS; Origin and Fate of Biogenic Particle Fluxes in the Ocean; Oxygen, flux, sediment oxygen demand; Temperature, water
    Type: Dataset
    Format: text/tab-separated-values, 2 data points
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  • 8
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    Unknown
    PANGAEA
    Publication Date: 2023-02-24
    Keywords: BC; BH02-11; Boston Harbor; Box corer; DEPTH, sediment/rock; Giblin_BH02-11_BC; Gyre; Gyre9007; Nitrate, flux; ORFOIS; Origin and Fate of Biogenic Particle Fluxes in the Ocean; Oxygen, flux, sediment oxygen demand; Temperature, water
    Type: Dataset
    Format: text/tab-separated-values, 3 data points
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  • 9
    facet.materialart.
    Unknown
    PANGAEA
    Publication Date: 2023-02-24
    Keywords: BC; BH02-10; Boston Harbor; Box corer; DEPTH, sediment/rock; Giblin_BH02-10_BC; Gyre; Gyre9007; Nitrate, flux; ORFOIS; Origin and Fate of Biogenic Particle Fluxes in the Ocean; Oxygen, flux, sediment oxygen demand; Temperature, water
    Type: Dataset
    Format: text/tab-separated-values, 3 data points
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  • 10
    facet.materialart.
    Unknown
    PANGAEA
    Publication Date: 2023-02-24
    Keywords: BC; BH02-2; Boston Harbor; Box corer; DEPTH, sediment/rock; Giblin_BH02-2_BC; Gyre; Gyre9007; ORFOIS; Origin and Fate of Biogenic Particle Fluxes in the Ocean; Oxygen, flux, sediment oxygen demand; Temperature, water
    Type: Dataset
    Format: text/tab-separated-values, 2 data points
    Location Call Number Limitation Availability
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