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High mountain lakes and their catchments are remote ecosystems in areas with low anthropogenic disturbance. High mountain lakes integrate changes in the atmosphere and catchment areas (e.g., acid rain, airborne pollutants, climate change). The present research analyses long-term datasets of meteorological and limnological variables representing two tropical high mountain lakes, El Sol and La Luna, in Central Mexico to identify the impacts of anthropogenic disturbance (i.e., sentinels of global/climate change). The 54-year meteorological analysis showed marked interannual variability with no statistically significant air temperature or rainfall trends. However, from 2000 to 2018, the air temperature increased by 0.5 °C. Accordingly, the lake water temperature increased (Lake El Sol: 0.8 °C, Lake La Luna: 0.6 °C). Although the rainfall displayed no change, the water level decreased in both lakes (1.5 m), most likely associated with increased evapotranspiration. Unexpectedly, the dissolved inorganic nitrogen (DIN) concentration in the lakes decreased. The initial acid pH rose to close neutrality in Lake La Luna and to alkaline values in Lake El Sol. The latter may be a consequence of the lowered SOx and NOx emissions from governmental regulations promulgated to control atmospheric pollution beginning in 2000 and probably resulting in less acidic deposition. An additional explanation for the lakes' deacidification is the increased deposition of alkaline ions derived from activities at the volcano slopes. Since the atmospheric supply is the primary nitrogen source to high mountain lakes, the DIN concentration decline could reflect the reduction in atmospheric HNO3. Thus, Lakes El Sol and La Luna evidenced global change. Both lakes are inside the same crater and are subjected to similar influences; thus, they showed similar responses to global change (increasing lake water temperatures, declining water levels, higher pH value, and lower DIN concentrations). Nevertheless, their differences (e.g., catchment size, surface area, water volume, water depth, trophic status) influenced the magnitude of the impacts, with higher pH increases recorded in Lake El Sol and higher DIN concentrations in Lake La Luna.

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This study simulated acidic habitat for different life stages of Clarias gariepinus to know the effect on survival, mortality, morphology and behaviour. The fish were exposed to pHs 3, 4, 5, 6 and 8.01 (control) for 35 days. 100% mortality was recorded for all the life stages in pH 3, and 80, 62 and 36% of mortality of fingerlings, juveniles and adults respectively were recorded in pH 4. In pH 5, 30, 26 and 12% mortalities of fingerlings, juveniles and adults respectively were recorded and at pH 6 mortalities of fingerlings, juveniles and adults were 12, 10 and 4% respectively. Control pH mortalities were 10, 6 and 2% for fingerlings, juveniles and adults respectively. Mortality was due to lack of oxygen uptake, stress and circulatory collapse. All these elicited the behavioural responses and morphological abnormalities like erratic swimming, gasping, dark body colouration and lethargy. The study showed that different life stages of C. gariepinus tolerate different acidic pH waters, with high mortalities of the fingerlings, juveniles and adults in pHs 3, pH 4 is sub-lethal to fingerlings, juveniles and adult, pH 5 sub-lethal to fingerlings and sub-optimal for juveniles, and pH 6 optimal for all life stages.(AU)

Este estudo simulou um habitat ácido para diferentes estágios de vida de Clarias gariepinus para conhecer o efeito na sobrevivência, mortalidade, morfologia e comportamento. Os peixes foram expostos aos pH 3, 4, 5, 6 e 8.01 (controle) por 35 dias. A mortalidade de 100% foi registrada em todos os estágios da vida em pH 3, e 80, 62 e 36% da mortalidade de alevinos, juvenis e adultos, respectivamente, foram registradas em pH 4. Em pH 5, 30, 26 e 12% de mortalidade de alevinos, juvenis e adultos, respectivamente, foram registrados e, a pH 6, a mortalidades de aletanas, juvenis e adultos foram 12, 10 e 4%, respectivamente. A mortalidade por pH de controle foi de 10, 6 e 2% para alevinos, juvenis e adultos, respectivamente. A mortalidade deveu-se à falta de absorção de oxigênio, estresse e colapso circulatório. Tudo isso provocou respostas comportamentais e anormalidades morfológicas como natação errática, ofegante, coloração do corpo escuro e letargia. O estudo evidenciou que diferentes estágios de vida de C. gariepinus toleram diferentes águas ácidas do pH, com alta mortalidade de alevinos, juvenis e adultos em pH 3, pH 4 é sub-letal para alevinos, juvenis e adultos, pH 5 sub-letal para alevinos e sub-ótima para juvenis, e pH 6 ideal para todos os estádios da vida.(AU)

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RESUMEN

This study simulated acidic habitat for different life stages of Clarias gariepinus to know the effect on survival, mortality, morphology and behaviour. The fish were exposed to pHs 3, 4, 5, 6 and 8.01 (control) for 35 days. 100% mortality was recorded for all the life stages in pH 3, and 80, 62 and 36% of mortality of fingerlings, juveniles and adults respectively were recorded in pH 4. In pH 5, 30, 26 and 12% mortalities of fingerlings, juveniles and adults respectively were recorded and at pH 6 mortalities of fingerlings, juveniles and adults were 12, 10 and 4% respectively. Control pH mortalities were 10, 6 and 2% for fingerlings, juveniles and adults respectively. Mortality was due to lack of oxygen uptake, stress and circulatory collapse. All these elicited the behavioural responses and morphological abnormalities like erratic swimming, gasping, dark body colouration and lethargy. The study showed that different life stages of C. gariepinus tolerate different acidic pH waters, with high mortalities of the fingerlings, juveniles and adults in pHs 3, pH 4 is sub-lethal to fingerlings, juveniles and adult, pH 5 sub-lethal to fingerlings and sub-optimal for juveniles, and pH 6 optimal for all life stages.

Este estudo simulou um habitat ácido para diferentes estágios de vida de Clarias gariepinus para conhecer o efeito na sobrevivência, mortalidade, morfologia e comportamento. Os peixes foram expostos aos pH 3, 4, 5, 6 e 8.01 (controle) por 35 dias. A mortalidade de 100% foi registrada em todos os estágios da vida em pH 3, e 80, 62 e 36% da mortalidade de alevinos, juvenis e adultos, respectivamente, foram registradas em pH 4. Em pH 5, 30, 26 e 12% de mortalidade de alevinos, juvenis e adultos, respectivamente, foram registrados e, a pH 6, a mortalidades de aletanas, juvenis e adultos foram 12, 10 e 4%, respectivamente. A mortalidade por pH de controle foi de 10, 6 e 2% para alevinos, juvenis e adultos, respectivamente. A mortalidade deveu-se à falta de absorção de oxigênio, estresse e colapso circulatório. Tudo isso provocou respostas comportamentais e anormalidades morfológicas como natação errática, ofegante, coloração do corpo escuro e letargia. O estudo evidenciou que diferentes estágios de vida de C. gariepinus toleram diferentes águas ácidas do pH, com alta mortalidade de alevinos, juvenis e adultos em pH 3, pH 4 é sub-letal para alevinos, juvenis e adultos, pH 5 sub-letal para alevinos e sub-ótima para juvenis, e pH 6 ideal para todos os estádios da vida.

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In the last 30 years, the Metropolitan Zone of Guadalajara (ZMG) has experienced a quick urban and industrial growth, situation which results in high rates of pollution and poor air quality harmful to the health of the population. The main purpose of this work was to analyze the SO2 and NO2 in the air, as well as ions H+, SO 4-2 and NO3- during the wet season of 2005. Results of the network of monitoring stations showed significant acidity in north-northwest and southeast of the study area. The maximum concentrations of SO 4-2 occurred in southeast and south, while the maximum NO3- was found in the south. Maximum levels of SO2 and NO2 occurred in the dry season, but it decreased in wet season. The higher frequency about acidity produced by NO2 is caused by mobile sources as the primary indicator.

En los últimos 30 años, la Zona Metropolitana de Guadalajara (ZMG) ha experimentado un acelerado crecimiento urbano-industrial, realidad traducida en contaminantes nocivos para la salud de la población. El objetivo de este trabajo fue analizar la concentración de dióxido de azufre (SO 2) y de nitrógeno (NO2) en el aire, así como, los iones hidrógeno (H+), sulfatos (SO 4-2) y nitratos (NO3-) durante la temporada de lluvias del año 2005. Mediante una red de estaciones de monitoreo, se obtuvieron resultados que revelaron acidez significativa al norte-noroeste y sureste. Las concentraciones máximas de SO4-2 ocurrieron al sureste y sur, mientras que, las de NO3- se localizaron al sur. Los niveles máximos de SO2 y NO2 sucedieron en el período seco, disminuyendo en el húmedo. Se observó mayor frecuencia de acidez por NO2 siendo el indicador principal las fuentes móviles.

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The purpose of this study is to assess the composition of wet precipitation in three sites of the metropolitan area of Porto Alegre. Besides the variables usually considered, such as pH, conductivity, major ions (Cl(-), NO(3)(-), F(-), SO(4)(2-), Na(+), K(+), Mg(2+), NH(4)(+) and Ca(2+)) and metallic elements (Cd, Co, Cr, Cu, Fe, Mn and Ni), the suspended matter was examined by X-ray diffraction (XRD) and scanning electron microscopy (SEM), with energy dispersive system (EDS), for better identification of possible anthropogenic material in this wet precipitation. Results showed an alkaline pH in the samples analyzed and higher concentrations for Na(+), Cl(-) and SO(4)(2-). The acidification and neutralization potential between anions (SO(4)(2-)+NO(3)(-)) and cations (Ca(2+)+Mg(2+)+K(+)+NH(4)(+)) showed a good correlation (0.922). The metallic elements with highest values were Zn, Fe and Mn. Results of XRD identified the presence of some minerals such as quartz, feldspar, mica, clay, carbonates and sulfates. In samples analyzed with SEM, we detected pyroxene, biotite, amphibole and oxides. Cluster analysis (CA) was applied to the data matrix to identify potential pollution sources of metals (natural or anthropogenic) and the association with minerals found in the analysis of SEM.

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Wet deposition and related rainwater chemistry were studied at the Itatiaia massif, on which is settled the Itatiaia National Park (INP). Samples were simultaneously collected on a weekly basis over 12 months, using automated wet and dry samplers, at the INP-Headquarters (INP-Hq; altitude=820 m) and the Itatiaia Plateau (It-Pt; altitude=2460 m). Conductivity, pH, Na(+), K(+), Mg(2+), Ca(2+), NH(4)(+), Cl(-), NO(3)(-) and SO(4)(2-) were determined in 36 rainwater samples. Volume-weighted mean (VWM) pH was lower at the INP-Hq (4.9) than at the It-Pt (5.3). Very strong correlation between Cl(-) and Na(+) was found for the INP-Hq (r=0.99). At the Itatiaia massif, SO(4)(2-), NO(3)(-), and NH(4)(+) comprised together about 60% of the total inorganic ions and appear to exert the major control on rainwater pH.

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Acid rain precipitation has become a major environmental concern. Many long-range projects in the United States and Europe are devoted to the problems associated with acid rain pollution. In Puerto Rico, there has been no formal study on acid rain. The rainfall pH values and the air-mass trajectory of the northeastern part of the island of Puerto Rico on the surface were analyzed from January 1998 to December 2000. The air-mass trajectory was classified in five different sectors, according to where it originates. The mean pH value measured during that period showed a tendency toward acidity. The 80% of the air-mass trajectory that arrived at the station occurred in Sector I, with a pH value of 4.30. The lowest pH value measured was 4.16, and it occurred in Sector V, where the air mass originates in the northwest part of the island.

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