2016
DOI: 10.1016/j.csr.2016.07.006
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Spatio-temporal variability of phytoplankton (Chlorophyll-a) in relation to salinity, suspended sediment concentration, and light intensity in a macrotidal estuary

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Cited by 56 publications
(13 citation statements)
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“…In the spring and summer seasons, independently of the tide, chlorophyll a peaked in the upstream oligohaline area of the estuary (salinity 0.5-5), whereas in the fall it peaked in freshwater, and during winter in the downstream polyhaline area. The observed patterns during the warmest period of the year at the interface between freshwater and saltwater, were also reported previously [13], as well as for the fall [41]. Moreover, chlorophyll a peaks may also occur in higher salinity areas [40,42].…”
Section: Chlorophyll a And Bacteria Dynamicssupporting
confidence: 87%
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“…In the spring and summer seasons, independently of the tide, chlorophyll a peaked in the upstream oligohaline area of the estuary (salinity 0.5-5), whereas in the fall it peaked in freshwater, and during winter in the downstream polyhaline area. The observed patterns during the warmest period of the year at the interface between freshwater and saltwater, were also reported previously [13], as well as for the fall [41]. Moreover, chlorophyll a peaks may also occur in higher salinity areas [40,42].…”
Section: Chlorophyll a And Bacteria Dynamicssupporting
confidence: 87%
“…For the box model, the obtained salinity values at each sampling site were used to classify water masses according to the Venice System [30] and the Water Framework Directive [31], i.e., freshwater (salinity < 0.5), brackish water (0.5-30), and seawater or euhaline water (>30), with brackish water subdivided into three groups, oligohaline (0.5-5), mesohaline (5)(6)(7)(8)(9)(10)(11)(12)(13)(14)(15)(16)(17)(18), and polyhaline (18-30).…”
Section: The Box Modelmentioning
confidence: 99%
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“…In macrotidal zones, physical processes control the system dynamics with large amounts of organic and inorganic compounds being reworked and transported within the estuary (Burford et al, 2008). In turbid estuaries under strong mixing conditions, tidal force is the most dominant factor, which can vary over time (diurnally, fortnightly or seasonally) (Azhikodan and Yokoyama, 2016). Wind force also promotes continuous vertical mixing of the water column allowing the translocation of oxygen-saturated water and protecting proximate coastal water bodies from eutrophication since macrotidal currents decrease the response of primary production to enhanced nutrient inputs (Cloern, 2001).…”
Section: Introductionmentioning
confidence: 99%
“…Studies on CHL-A have been conducted in various water bodies from coastal estuarine areas to oceanic, mainly focusing on the spatial and temporal changes, size distribution, and relationships with environmental factors (Iriarte & Purdie, 1994;Agawin, Duarte, & Agustí, 2000;Calvo-Díaz, Morán, & Suárez, 2008;Azhikodan & Yokoyama 2016). However, presently there are still limited information on the CHL-A in sea cucumber culture pond.…”
Section: Introductionmentioning
confidence: 99%