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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

Biogeochemical processes in a small California estuary. 1. Benthic fluxes and pore water constituents reflect high nutrient freshwater inputs

TL;DR: In this article, the effect of nutrient loading on ecosystem processes, rates of sediment oxygen consumption, benthic nutrient fluxes, pore water ammonium (NH4 + ), dissolved inorganic phosphate (DIP) and sulfide (S 2 - ) concentrations were measured at 5 sites several times each year between 1998 and 1999.
Journal ArticleDOI

Denitrification measured by a direct N2 flux method in sediments of Waquoit Bay, MA

TL;DR: Denitrification was directly estimated in estuarine sediments of Waquoit Bay, Cape Cod, MA by detection of N2 increases above ambient in the water overlying sediment cores as discussed by the authors.
Book ChapterDOI

Chapter 18 – Estuaries

TL;DR: In this paper, an overview of advances during the past 20 years in our understanding of nitrogen (N) in estuarine ecosystems and suggests some fruitful directions future research is provided.
Journal ArticleDOI

The composition and bioavailability of phosphorus transport through the Changjiang (Yangtze) River during the 1998 flood

Weijin Yan, +1 more
- 07 Jun 2003 - 
TL;DR: Wang et al. as mentioned in this paper collected water and suspended sediment (SS) samples from the Changjiang River at the Datong Hydrological Station (DHS) five times from May 1997 through January 1999 in order to evaluate transport, composition and bioavailability of phosphorus (P) during a 1998 flood.
Journal ArticleDOI

A kelp with integrity: Macrocystis pyrifera prioritises tissue maintenance in response to nitrogen fertilisation

TL;DR: Patterns in physiological parameters suggest that M. pyrifera displays functional differentiation between canopy and basal tissues that may aid in nutrient-tolerance strategies, similar to those seen in higher plants and unlike thoseseen in more simple algae (i.e. non-kelps).
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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