2015
DOI: 10.1016/j.marpolbul.2015.03.026
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Microplankton dynamics under heavy anthropogenic pressure. The case of the Bahía Blanca Estuary, southwestern Atlantic Ocean

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Cited by 26 publications
(13 citation statements)
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“…In this study, the lower temperature and salinity registered at middle-shelf resulted from the influence of colder Subantarctic shelf waters diluted by low salinity discharges from the Magellan Strait (Palma and Matano, 2012), while the higher water temperatures in the shallow area of El Rincón were due to the northward outflow of high salinity and warmer waters from the San Matías Gulf into the inner-shelf (Palma et al, 2008). The freshwater discharges of the Negro and the Colorado Rivers (Lucas et al, 2005) were detected in situ at the coastal stations near their deltas, while the influence of the highly eutrophic and hypersaline Bahía Blanca Estuary (Guinder et al, 2010;López Abbate et al, 2015) was notable at stations 1 and 12, where the in situ salinities reached the maxima. A particular characteristic of El Rincón area is the formation of an anticyclone gyre in the center during winter, which looses intensification when nearing spring and summer (Palma et al, 2008).…”
Section: Environmental Conditions and Distribution Of Planktonmentioning
confidence: 99%
“…In this study, the lower temperature and salinity registered at middle-shelf resulted from the influence of colder Subantarctic shelf waters diluted by low salinity discharges from the Magellan Strait (Palma and Matano, 2012), while the higher water temperatures in the shallow area of El Rincón were due to the northward outflow of high salinity and warmer waters from the San Matías Gulf into the inner-shelf (Palma et al, 2008). The freshwater discharges of the Negro and the Colorado Rivers (Lucas et al, 2005) were detected in situ at the coastal stations near their deltas, while the influence of the highly eutrophic and hypersaline Bahía Blanca Estuary (Guinder et al, 2010;López Abbate et al, 2015) was notable at stations 1 and 12, where the in situ salinities reached the maxima. A particular characteristic of El Rincón area is the formation of an anticyclone gyre in the center during winter, which looses intensification when nearing spring and summer (Palma et al, 2008).…”
Section: Environmental Conditions and Distribution Of Planktonmentioning
confidence: 99%
“…Moreover, cultural eutrophication in the Bahía Blanca Estuary has been shown to reduce mesozooplankton biomass during summer (Dutto et al 2012) and the fertility of the copepod Eurytemora americana (Berasategui et al 2018). The negative effect on planktonic grazers was attributed to the combination of several factors, such as hypoxia (Dutto et al 2012) and toxicity of NH4 + and heavy metals (López-Abbate et al 2015, Fernández Severini et al 2017, Berasategui et al 2018.…”
Section: Eutrophication Effect On the Structure Of The Microbial Commmentioning
confidence: 99%
“…Dugdale et al (2007), conducted enclosure experiments in the San Francisco Bay and determined that NH4 + concentration exceeding 4 µM inhibits growth by preventing cells access to NO3 -, although other authors have reported a threshold value close to 10 µM in the Delaware Bay (Yoshiyama and Sharp 2006). NH4 + concentration near the sewage outflow in the Bahía Blanca Estuary can eventually exceed 150 µM (López-Abbate et al 2015), which is known to reduce chlorophyll content, cell abundance and productivity of estuarine phytoplankton (Livingston et al 2002, Yoshiyama andSharp 2006). Algal blooms resulting from cultural eutrophication are in fact associated with much lower NH4 + concentration.…”
Section: Eutrophication Effect On the Structure Of The Microbial Commmentioning
confidence: 99%
“…Actualmente, los estuarios exhiben una clara evidencia de eutrofización debido al aporte de nutrientes de origen antrópico (Nixon & Fulweiler, 2009;Spetter et al, 2015b;López Abbate et al, 2015) y juegan un rol primordial en donde los procesos biogeoquímicos modifican los flujos de nutrientes desde el continente hacia el mar (Lillebø et al, 2004, Van der Zee et al, 2007. En el ambiente acuático, el fósforo (P) disuelto es consumido durante el crecimiento del fitoplancton y luego es regenerado durante la descomposición de la materia orgánica (Sundby et al, 1992).…”
Section: Introductionunclassified