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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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Source of silica and silicification of the lowermost Cambrian Yanjiahe Formation in the Three Gorges area, South China

TL;DR: In this article, the authors provided a petrographic study supplemented by elemental concentration, SEM and Raman spectral data on the siliceous rocks from the Yanjiahe Formation (the Three Gorges area, South China), in order to ascertain the origin of included silica and discuss the involved processes of silica deposition.
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Assessment of the Spatial and Temporal Variations of Water Quality for Agricultural Lands with Crop Rotation in China by Using a HYPE Model.

TL;DR: Results show that the parameters related to the effective soil porosity were highly sensitive to hydrological modeling, and N balance was largely controlled by soil denitrification processes and P balance was influenced by the sedimentation rate and production/decay of P in rivers and lakes.
Journal ArticleDOI

Tracking changes to a microplankton community in a North Atlantic sea loch using the microplankton index PI(mp)

TL;DR: The PI(mp) is shown to be a useful and robust method to visualize and quantify changes in the underlying structure of the microplankton community and is a powerful addition to the toolbox of techniques needed to determine the health of the authors' seas.
Journal ArticleDOI

Controls on the organic carbon content of the lower Cambrian black shale in the southeastern margin of Upper Yangtze

TL;DR: In this paper, the authors investigated the influence of various factors, including mineral components, primary productivity and redox level on the total organic carbon (TOC) in the lower Cambrian black shale from southeastern margin of Upper Yangtze (Taozichong, Longbizui and Yanbei areas) is discussed in detail.
Journal Article

Evaluation of trophic state of Lake Uluabat, Turkey.

TL;DR: According to calculated nutrient ratios, phosphorus was found to be the primary limiting nutrient in lake Uluabat and Carlson's trophic state index values indicated that lake ULUabat is an eutrophic system.
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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