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The yield of chlorophyll from dissolved inorganic nitrogen (DIN) has been shown to be a potentially useful parameter for predicting eutrophication, particularly, in the northerly, coastal waters of the North East Atlantic (NEA). This study investigates whether this parameter might also be appropriat...

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Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.582.1739
http://w3.ualg.pt/~anewton/docs/Publications/Edwards et al 2005.pdf
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spelling ftciteseerx:oai:CiteSeerX.psu:10.1.1.582.1739 2023-05-15T17:38:37+02:00 r n The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.582.1739 http://w3.ualg.pt/~anewton/docs/Publications/Edwards et al 2005.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.582.1739 http://w3.ualg.pt/~anewton/docs/Publications/Edwards et al 2005.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://w3.ualg.pt/~anewton/docs/Publications/Edwards et al 2005.pdf chlorophyll nitrogen cyanobacteria phytoplankton microcosms eutr text ftciteseerx 2016-08-28T00:02:23Z The yield of chlorophyll from dissolved inorganic nitrogen (DIN) has been shown to be a potentially useful parameter for predicting eutrophication, particularly, in the northerly, coastal waters of the North East Atlantic (NEA). This study investigates whether this parameter might also be appropriate for the southerly, coastal waters of the NEA. Nitrogen enrichment experiments were carried out using microcosms to determine the microplanktonic yield of chlorophyll from DIN in waters from the Ria Formosa (April 2002) and from Sagres (September 2002) on the south coast of Portugal. Continuous culture techniques enabled experiments to be run for 7 days after enrichment so that changes in the cumulative yield over time could be calculated. Yields from the Sagres experiment were consistently higher than those from the Ria Formosa experiment, with respective maximum yields of 4.7 and 2.1 mg chl (mmol N)1, and respective steady-state yields of 3.1 and 0.9 mg chl (mmol N)1. In addition, regressions carried out on historical data sets from the two study sites showed poor correlation between chlorophyll and nitrate. Other differences between the microcosm experiments at the two sites, included: background concentrations of DIN, silicate and phosphate that were, respectively, 5.6 mM, 8.1 mM, and 0.3 mM higher in the Ria; chlorophyll concentrations at Sagres that were double those of the Ria; accumulation of particulate nitrogen that was both more rapid and more substantial at Sagres; a different community structure for the diatoms at the two sites; more numerous autotrophic dinoflagellates, flagellates and cyanobacteria, as well as more numerous protozoan grazers, at Sagres. These differences may explain why the yield of chlorophyll from DIN at Sagres is one of the highest reported in Text North East Atlantic Unknown
institution Open Polar
collection Unknown
op_collection_id ftciteseerx
language English
topic chlorophyll
nitrogen
cyanobacteria
phytoplankton
microcosms
eutr
spellingShingle chlorophyll
nitrogen
cyanobacteria
phytoplankton
microcosms
eutr
r n
topic_facet chlorophyll
nitrogen
cyanobacteria
phytoplankton
microcosms
eutr
description The yield of chlorophyll from dissolved inorganic nitrogen (DIN) has been shown to be a potentially useful parameter for predicting eutrophication, particularly, in the northerly, coastal waters of the North East Atlantic (NEA). This study investigates whether this parameter might also be appropriate for the southerly, coastal waters of the NEA. Nitrogen enrichment experiments were carried out using microcosms to determine the microplanktonic yield of chlorophyll from DIN in waters from the Ria Formosa (April 2002) and from Sagres (September 2002) on the south coast of Portugal. Continuous culture techniques enabled experiments to be run for 7 days after enrichment so that changes in the cumulative yield over time could be calculated. Yields from the Sagres experiment were consistently higher than those from the Ria Formosa experiment, with respective maximum yields of 4.7 and 2.1 mg chl (mmol N)1, and respective steady-state yields of 3.1 and 0.9 mg chl (mmol N)1. In addition, regressions carried out on historical data sets from the two study sites showed poor correlation between chlorophyll and nitrate. Other differences between the microcosm experiments at the two sites, included: background concentrations of DIN, silicate and phosphate that were, respectively, 5.6 mM, 8.1 mM, and 0.3 mM higher in the Ria; chlorophyll concentrations at Sagres that were double those of the Ria; accumulation of particulate nitrogen that was both more rapid and more substantial at Sagres; a different community structure for the diatoms at the two sites; more numerous autotrophic dinoflagellates, flagellates and cyanobacteria, as well as more numerous protozoan grazers, at Sagres. These differences may explain why the yield of chlorophyll from DIN at Sagres is one of the highest reported in
author2 The Pennsylvania State University CiteSeerX Archives
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url http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.582.1739
http://w3.ualg.pt/~anewton/docs/Publications/Edwards et al 2005.pdf
genre North East Atlantic
genre_facet North East Atlantic
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http://w3.ualg.pt/~anewton/docs/Publications/Edwards et al 2005.pdf
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