Abstract:The invasive freshwater dino agellate Ceratium furcoides is extending its distribution in South America with increasing environmental impacts associated with its blooms. We here report two events related to C. furcoides distribution expansion in Uruguay: 1) the rst appearance and main environmental drivers (physico-chemical variables, extreme wind events and zooplankton composition) of the bloom of C. furcoides in 2012 in a subtropical eutrophic shallow lake (Lake Blanca, Uruguay), and 2) the sh kill event of … Show more
“…Other studies have shown the success of the invasion of C. furcoides in aquatic bodies in the subtropical region(Cavalcante et al, 2013(Cavalcante et al, , 2016Silva et al, 2018;Silva et al, 2019).Although high temperatures may bene t Ceratium, this is not a determining factor for its expansion, as the dino agellate maintains intermediate densities in later years (2016 onwards). This coincides with other studies, such as in Lake Blanca, Uruguay(Pacheco et al, 2021), where high temperatures were important during the initial stages of a bloom but not necessary to maintain it. C. furcoides has complex distribution and expansion patterns, usually colonizing freshwaters from basins that are geographically close(Moreira et al, 2015;Silva et al, 2018;Pacheco et al, 2021).Common phytoplankton dispersants such as wind, animals, and humans could play a part on the expansion of the dino agellate as they can be a very effective disperse…”
supporting
confidence: 91%
“…This coincides with other studies, such as in Lake Blanca, Uruguay(Pacheco et al, 2021), where high temperatures were important during the initial stages of a bloom but not necessary to maintain it. C. furcoides has complex distribution and expansion patterns, usually colonizing freshwaters from basins that are geographically close(Moreira et al, 2015;Silva et al, 2018;Pacheco et al, 2021).Common phytoplankton dispersants such as wind, animals, and humans could play a part on the expansion of the dino agellate as they can be a very effective disperse…”
supporting
confidence: 91%
“…With regard to environmental variables, only in Dom Pedrito cyanobacteria and Ceratium were correlated with maximum temperature (0.48 and 0.45, respectively). The results also suggest that the temperature range for the occurrence of the species is much wider than expected (between 18 and 22°C, according to Meichtry-de-Zaburlin et al, 2016), as we found the species in environments with temperatures as high as 34,5°C and as low as 3,6°C, provide that the spatial and temporal scales are expanded, as in this study Pacheco et al (2021). showed the species in temperatures ranging from 18 to 28,4°C in a Uruguayan lakes; however, in tropical area in Brazil, where the temperature variation is short, Severiano et al (2022) evidenced C. furcoides in warm environments (around 26-28°C).Furthermore, seems that high temperatures associated with high precipitation rates may spark the growth of Ceratium in these spring, as large densities occurred in years where these meteorological variables were high (2013 to 2015).…”
Ceratium furcoides is a dinoflagellate that exhibits invasive behavior in aquatic ecosystems of Southern Brazil. Because of this, the study had as objectives to determine the factors that drive dinoflagellate populations as well as identifying temporal and spatial patterns of these populations, relating to Microcystis and propose actions against the invasion and establishment of Ceratium. Data (physical and chemical water and phytoplankton density) came from the monitoring carried out by CORSAN (Riograndense Sanitation Company), in reservoirs in the Hydrographic Region (HR) of Uruguay, from 2013 to 2019 (weekly to monthly sampling); climatic data were obtained through INMET (National Meteorological Institute). Seasonally, maximum precipitation occurred in autumn and spring, temperatures followed a subtropical pattern. Regarding phytoplankton, maximum density occurred in autumn and summer, in 2018 and 2013 (except Ceratium, with maximum in 2014). The analysis indicated that the highest values of density of phytoplankton, cyanobacteria, and Microcystis occurred in U20 basin, in Erechim (autumn 2018) and Passo Fundo (summer 2013); Ceratium peaks were found at U70 in Dom Pedrito (summer 2014) and U80 in Aceguá (autumn 2015). Usually, the populations of dinoflagellate and Microcystis did tend to stabilization, however showed classic relations, such as competition and coexistence, and dominance of the dinoflagellate. The results suggest that local environmental characteristics (temperature, phosphorus, nitrate, organic matter, pH) are key for the development of C. furcoides in this HR, and as is in an environment susceptible to its invasion, studies like this are important in understanding and eventually combating species with this character.
“…Other studies have shown the success of the invasion of C. furcoides in aquatic bodies in the subtropical region(Cavalcante et al, 2013(Cavalcante et al, , 2016Silva et al, 2018;Silva et al, 2019).Although high temperatures may bene t Ceratium, this is not a determining factor for its expansion, as the dino agellate maintains intermediate densities in later years (2016 onwards). This coincides with other studies, such as in Lake Blanca, Uruguay(Pacheco et al, 2021), where high temperatures were important during the initial stages of a bloom but not necessary to maintain it. C. furcoides has complex distribution and expansion patterns, usually colonizing freshwaters from basins that are geographically close(Moreira et al, 2015;Silva et al, 2018;Pacheco et al, 2021).Common phytoplankton dispersants such as wind, animals, and humans could play a part on the expansion of the dino agellate as they can be a very effective disperse…”
supporting
confidence: 91%
“…This coincides with other studies, such as in Lake Blanca, Uruguay(Pacheco et al, 2021), where high temperatures were important during the initial stages of a bloom but not necessary to maintain it. C. furcoides has complex distribution and expansion patterns, usually colonizing freshwaters from basins that are geographically close(Moreira et al, 2015;Silva et al, 2018;Pacheco et al, 2021).Common phytoplankton dispersants such as wind, animals, and humans could play a part on the expansion of the dino agellate as they can be a very effective disperse…”
supporting
confidence: 91%
“…With regard to environmental variables, only in Dom Pedrito cyanobacteria and Ceratium were correlated with maximum temperature (0.48 and 0.45, respectively). The results also suggest that the temperature range for the occurrence of the species is much wider than expected (between 18 and 22°C, according to Meichtry-de-Zaburlin et al, 2016), as we found the species in environments with temperatures as high as 34,5°C and as low as 3,6°C, provide that the spatial and temporal scales are expanded, as in this study Pacheco et al (2021). showed the species in temperatures ranging from 18 to 28,4°C in a Uruguayan lakes; however, in tropical area in Brazil, where the temperature variation is short, Severiano et al (2022) evidenced C. furcoides in warm environments (around 26-28°C).Furthermore, seems that high temperatures associated with high precipitation rates may spark the growth of Ceratium in these spring, as large densities occurred in years where these meteorological variables were high (2013 to 2015).…”
Ceratium furcoides is a dinoflagellate that exhibits invasive behavior in aquatic ecosystems of Southern Brazil. Because of this, the study had as objectives to determine the factors that drive dinoflagellate populations as well as identifying temporal and spatial patterns of these populations, relating to Microcystis and propose actions against the invasion and establishment of Ceratium. Data (physical and chemical water and phytoplankton density) came from the monitoring carried out by CORSAN (Riograndense Sanitation Company), in reservoirs in the Hydrographic Region (HR) of Uruguay, from 2013 to 2019 (weekly to monthly sampling); climatic data were obtained through INMET (National Meteorological Institute). Seasonally, maximum precipitation occurred in autumn and spring, temperatures followed a subtropical pattern. Regarding phytoplankton, maximum density occurred in autumn and summer, in 2018 and 2013 (except Ceratium, with maximum in 2014). The analysis indicated that the highest values of density of phytoplankton, cyanobacteria, and Microcystis occurred in U20 basin, in Erechim (autumn 2018) and Passo Fundo (summer 2013); Ceratium peaks were found at U70 in Dom Pedrito (summer 2014) and U80 in Aceguá (autumn 2015). Usually, the populations of dinoflagellate and Microcystis did tend to stabilization, however showed classic relations, such as competition and coexistence, and dominance of the dinoflagellate. The results suggest that local environmental characteristics (temperature, phosphorus, nitrate, organic matter, pH) are key for the development of C. furcoides in this HR, and as is in an environment susceptible to its invasion, studies like this are important in understanding and eventually combating species with this character.
“…and a permanent clear water regime. The dominant phytoplankton taxonomic groups, in this lake, have changed through the years from cyanobacteria to chlorophytes (Kruk et al, 2006;Pacheco et al, 2010), with one event of a Ceratium furcoides (Levander) bloom in 2012 (Pacheco et al, 2021). The community of consumers in the clear-vegetated lake is diverse; the zooplankton community is dominated by small-bodied cladocerans and copepods, with occasional occurrence of Daphnia spp.…”
Section: Methodsmentioning
confidence: 99%
“…The community of consumers in the clear-vegetated lake is diverse; the zooplankton community is dominated by small-bodied cladocerans and copepods, with occasional occurrence of Daphnia spp. and other larger-bodied species, the diverse fish community dominated by small-bodied species with a high biomass (Pacheco et al, 2021). Lake Capilla (location: 34°49 0 18.5 00 S-54°37 0 48.7 00 W, area: 1 ha), hereinafter referred to as 'phytoplankton-turbid', is a small, young (less than 15 years) artificially constructed lake that is in a turbid state due to high phytoplankton biomass.…”
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