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Journal ArticleDOI

Nutrient Limitation of Net Primary Production in Marine Ecosystems

Robert W. Howarth
- 01 Jan 1988 - 
- Vol. 19, Iss: 1, pp 89-110
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TLDR
There is a feeling among many limnologists and environmental engineers who study lakes that marine ecosystems also probably are phosphorus limited, and environmental management agencies often assume that phosphorus limitation in marine ecosystems is the rule.
Abstract
The question of nutrient limitation of primary production in estuaries and other marine ecosystems has engendered a great deal of debate. Although nitrogen is often named as the primary limiting nutrient in seawater (3, 17-19, 50, 52, 55, 61, 76, 80), this is by no means universally accepted. Many workers have argued that phosphorus is limiting (58, 71), that both nitrogen and phosphorus can simultaneously be limiting (9), or that primary production can switch seasonally from being nitrogen-limited to phosphorus-limited (6, 46). Others argue that nutrients are not limiting at all in many marine ecosystems, including highly oligotrophic waters (15). To some extent these disagreements result from poor communication due to different definitions of nutrient limitation. Considerable argument also occurs over the various methods and approaches used to estimate nutrient limitation. Limnologists in particular have tended to be critical of the methods often used to study nutrient limitation in marine ecosystems (23). Nutrient limitation in lakes has historically received more study than that in estuaries, and most mesotrophic and eutrophic north-temperate lakes are phosphorus limited (8, 62, 63, 66, 81). Thus, there is a feeling among many limnologists and environmental engineers who study lakes that marine ecosystems also probably are phosphorus limited. Lacking strong mechanistic arguments to explain why nutrient limitation might be different in estuaries than in lakes, environmental management agencies often assume that phosphorus limitation in marine ecosystems is the rule.

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Citations
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Journal ArticleDOI

Net anthropogenic phosphorus inputs: spatial and temporal variability in the Chesapeake Bay region

TL;DR: In this article, the authors estimated net anthropogenic phosphorus inputs (NAPI) in the Chesapeake Bay region and found that large positive NAPI values were associated with agricultural and developed land cover, and the developed land component of NAPI had a strong direct correlation with measured phosphorus discharges from major rivers draining to the Bay.
Journal ArticleDOI

Sulfur, iron and organic carbon fluxes in the Black Sea: sulfur isotopic evidence for origin of sulfur fluxes

TL;DR: A sulfur isotope-based box model for sulfur cycling between dissolved and particulate phases in the water column and sediments is presented in this paper, where sulfides in surface sediments are often isotopically similar to dissolved sulfide at the top of the sulfide zone and to sediment trap fluxes.
Journal ArticleDOI

Nutrient limitation and the eutrophication of coastal lagoons

TL;DR: Comparison of the N-alone and combined N + P treatments indicated that when enriched with N alone, the limitation of the systems shifted to P limitation of total system metabolism and of phytoplankton production and standing crop, and to light limitation of eelgrass and macroalgal growth.
Journal ArticleDOI

Nitrogen inputs to a marine embayment: the importance of groundwater

TL;DR: In this paper, the importance of nitrogen inputs from groundwater and runoff in a small coastal marine cove on Cape Cod, MA, USA, was examined 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.
Journal ArticleDOI

Isotopic characterization of atmospheric nitrogen inputs as sources of enhanced primary production in coastal Atlantic Ocean waters

TL;DR: To investigate the effects of significant atmospheric N loading with stable isotope tracers, the δ15N of the>1 μm fraction from surrounding coastal waters was measured to emphasize the contribution of atmospheric nitrogen deposition to “new” production in coastal waters.
References
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Journal ArticleDOI

Particulate organic matter flux and planktonic new production in the deep ocean

TL;DR: The primary production in the oceans results from allochthonous nutrient inputs to the euphotic zone (new production) and from nutrient recycling in the surface waters (regenerated production) as discussed by the authors.
Journal ArticleDOI

Nitrogen, Phosphorus, and Eutrophication in the Coastal Marine Environment

TL;DR: Removal of phosphate from detergents is not likely to slow the eutrophication of coastal marine waters, and its replacement with nitrogen-containing nitrilotriacetic acid may worsen the situation.
Journal ArticleDOI

Nutrient limitation of phytoplankton in freshwater and marine environments: A review of recent evidence on the effects of enrichment1

TL;DR: It is concluded that the extent and severity of N limitation in the marine environment remain an open question, despite the fact that by the late seventies the evidence for P limitation had become so great that phosphorus control was recommended as the legislated basis for controlling eutrophication in North American and European inland waters.
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