2009
DOI: 10.1016/j.jmarsys.2008.10.005
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Strong bottom–up effects on phytoplankton community caused by a rainfall during spring and summer in Sagami Bay, Japan

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Cited by 42 publications
(42 citation statements)
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“…4). In Sagami Bay, high concentrations of NO 2 +NO 3 and Si(OH) 4 have been observed after heavy rainfall, when the supplies of these nutrients to the coastal regions are related to the increase in freshwater discharge due to precipitation (Fujiki et al 2004, Baek et al 2009). Thus, the significant negative relationships between NO 2 +NO 3 and Si(OH) 4 , and salinity indicate those nutrients were supplied by terrestrial runoff in the present study.…”
Section: Nutrient Originmentioning
confidence: 99%
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“…4). In Sagami Bay, high concentrations of NO 2 +NO 3 and Si(OH) 4 have been observed after heavy rainfall, when the supplies of these nutrients to the coastal regions are related to the increase in freshwater discharge due to precipitation (Fujiki et al 2004, Baek et al 2009). Thus, the significant negative relationships between NO 2 +NO 3 and Si(OH) 4 , and salinity indicate those nutrients were supplied by terrestrial runoff in the present study.…”
Section: Nutrient Originmentioning
confidence: 99%
“…During the study, a summer phytoplankton bloom occurred after 3-4 Satoh et al (2000) days of persistent precipitation of 200 mm or more, and the bloom was dominated by large-sized dinoflagellates, such as Ceratium furca Ehrenberg (Satoh et al 2000). Increase in freshwater discharge due to precipitation results in large loadings of nitrogen and silicate to the coastal area, which leads to phosphorus limitation of primary productivity from spring to summer (Fujiki et al 2004, Baek et al 2009). Although variability in phytoplankton communities and primary production has been documented in the nearshore, western part of Sagami Bay, information on the importance of episodic events remains limited.…”
Section: Introductionmentioning
confidence: 99%
“…Studies on Noctiluca in the coastal waters of Sagami Bay have dealt with aspects of red tides and/or red coloration phenomena, sometimes having originated in expanded from neighboring Tokyo Bay (Tanaka 1985, Yamada 1997, Kamataki 2005, predominance in the microphytoplankton assemblages (Tatara & Kikuchi 2003, Baek et al 2009, and seasonal and interannual variations in abundance in relation to environmental factors (Miyaguchi et al 2006). However, in these waters as well as other waters of the world, there has been no attempt to investigate the availability of nutrients regenerated by Noctiluca for phytoplankton growth or to evaluate the contribution of nutrient (N and P) supply by Noctiluca excretion to phytoplankton primary production.…”
Section: Introductionmentioning
confidence: 99%
“…; Baek et al . ). Solar radiation and wind influence ocean temperature and stratification, altering the availability of nutrients for phytoplankton (Behrenfeld et al .…”
Section: Introductionmentioning
confidence: 97%