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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

Low level of phosphorous concentration in terminal Paleoproterozoic shallow seawater: Evidence from Chuanlinggou ironstone on North China Platform

TL;DR: In this article , the authors performed fabric-specific analysis of dense laminasets in ooid cortices without cracks, and in stromatolitic columns, pointing to an extremely low phosphorus concentration (<0.002-0.016 μM) in ∼1.65 Ga shallow seawater.
Journal ArticleDOI

Effects of river damming on biogenic silica turnover: implications for biogeochemical carbon and nutrient cycles

TL;DR: In this article, the current understanding of the effects of river damming on the processes of biogeochemical Si cycle, especially the source, composition, and recycling process of biogenic silica (BSi).

Optimization and characterization of the bulk FDA viability assay to quantify living planktonic biomass

TL;DR: Optimization and characterization of the Bulk FDA viability assay to quantify living and its application in clinical practice and animal studies shows promising results.
Dissertation

The effect of nutrient enrichment on stream periphyton growth in the southern Coastal Plain of Georgia

TL;DR: Carey et al. as mentioned in this paper used periphyton biomass for treatments in the sun, measured as chlorophyll a, was significantly (p < 0.05) greater than corresponding treatments in a shade and algal growth was nutrient-limited at several sites where DO concentrations were below regulatory standards.

Water quality in Lake Illawarra, New South Wales: Groundwater contamination and migration from septic and nightsoil waste deposits in the coastal Windang unconfined sandy aquifer

Jack Palma
TL;DR: In this article, the unconfined aquifer in Windang around the south-western portion of Port Kembla Golf Course was assessed with the goal of identifying the characteristics of a known ammonia plume including migration, discharge and attenuation.
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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