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en Dissolved organic matter distribution in the water column and sediment pore water in a highly anthropized coastal lagoon (Mar Menor, Spain): Characteristics, sources, and benthic fluxes -
Modificado el valor del campo
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del recurso Distribución HTML a2026-06-25
(anteriormente2026-06-23
) en Dissolved organic matter distribution in the water column and sediment pore water in a highly anthropized coastal lagoon (Mar Menor, Spain): Characteristics, sources, and benthic fluxes
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| 95 | "notes": "Coastal lagoons are among the most productive and | 105 | "notes": "Coastal lagoons are among the most productive and | ||
| 96 | biodiverse systems in the world and are important sentinels of climate | 106 | biodiverse systems in the world and are important sentinels of climate | ||
| 97 | change. The Mar Menor is one of the largest coastal lagoons in the | 107 | change. The Mar Menor is one of the largest coastal lagoons in the | ||
| 98 | Mediterranean, providing a variety of ecosystem services and resources | 108 | Mediterranean, providing a variety of ecosystem services and resources | ||
| 99 | to the community. However, in recent decades this lagoon has suffered | 109 | to the community. However, in recent decades this lagoon has suffered | ||
| 100 | drastic changes and degradation caused by human activities. We | 110 | drastic changes and degradation caused by human activities. We | ||
| 101 | analyzed the concentration of dissolved organic carbon (DOC) and the | 111 | analyzed the concentration of dissolved organic carbon (DOC) and the | ||
| 102 | optical properties of dissolved organic matter (DOM) in the water | 112 | optical properties of dissolved organic matter (DOM) in the water | ||
| 103 | column and sediment pore water during the summer and winter of 2018 | 113 | column and sediment pore water during the summer and winter of 2018 | ||
| 104 | and during eighteen months from 2016 to 2018. Overall, we found that | 114 | and during eighteen months from 2016 to 2018. Overall, we found that | ||
| 105 | the composition of DOM is mainly related to and enhanced by | 115 | the composition of DOM is mainly related to and enhanced by | ||
| 106 | anthropogenic activities and microbial metabolism. DOM enters the | 116 | anthropogenic activities and microbial metabolism. DOM enters the | ||
| 107 | lagoon via urban and agricultural runoff, drainage systems, and | 117 | lagoon via urban and agricultural runoff, drainage systems, and | ||
| 108 | wastewater treatment plants. Additionally, strong microbial metabolism | 118 | wastewater treatment plants. Additionally, strong microbial metabolism | ||
| 109 | in sediments leads to differences in DOM composition between water and | 119 | in sediments leads to differences in DOM composition between water and | ||
| 110 | sediments. In the water column, humic-like components accounted for 71 | 120 | sediments. In the water column, humic-like components accounted for 71 | ||
| 111 | % of the total DOM, while protein-like compounds were most abundant in | 121 | % of the total DOM, while protein-like compounds were most abundant in | ||
| 112 | sediment pore water. We observed a strong seasonal variability | 122 | sediment pore water. We observed a strong seasonal variability | ||
| 113 | associated with precipitation and the system collapse in 2016 | 123 | associated with precipitation and the system collapse in 2016 | ||
| 114 | (phytoplankton bloom), which resulted in the death of 80 % of | 124 | (phytoplankton bloom), which resulted in the death of 80 % of | ||
| 115 | macrophytes. The sediments act as a source of DOM to the overlying | 125 | macrophytes. The sediments act as a source of DOM to the overlying | ||
| 116 | water, likely due to relatively high organic matter content and | 126 | water, likely due to relatively high organic matter content and | ||
| 117 | intense microbial activity, primarily through anaerobic pathways. | 127 | intense microbial activity, primarily through anaerobic pathways. | ||
| 118 | Benthic fluxes of DOC ranged from 5.24 to 33.30 mmol m\u22122 | 128 | Benthic fluxes of DOC ranged from 5.24 to 33.30 mmol m\u22122 | ||
| 119 | d\u22121, being higher in winter than summer 2018 and decreasing from | 129 | d\u22121, being higher in winter than summer 2018 and decreasing from | ||
| 120 | north to south, likely related to lower residence time in the northern | 130 | north to south, likely related to lower residence time in the northern | ||
| 121 | basin, groundwater discharge and accumulation of organic matter from | 131 | basin, groundwater discharge and accumulation of organic matter from | ||
| 122 | the dead meadows. We estimate a net flux of DOC from the Mar Menor | 132 | the dead meadows. We estimate a net flux of DOC from the Mar Menor | ||
| 123 | toward the Mediterranean Sea of 1.57 \u00d7 107 mol yr\u22121.", | 133 | toward the Mediterranean Sea of 1.57 \u00d7 107 mol yr\u22121.", | ||
| 124 | "notes_translated": { | 134 | "notes_translated": { | ||
| 125 | "es": "Coastal lagoons are among the most productive and | 135 | "es": "Coastal lagoons are among the most productive and | ||
| 126 | biodiverse systems in the world and are important sentinels of climate | 136 | biodiverse systems in the world and are important sentinels of climate | ||
| 127 | change. The Mar Menor is one of the largest coastal lagoons in the | 137 | change. The Mar Menor is one of the largest coastal lagoons in the | ||
| 128 | Mediterranean, providing a variety of ecosystem services and resources | 138 | Mediterranean, providing a variety of ecosystem services and resources | ||
| 129 | to the community. However, in recent decades this lagoon has suffered | 139 | to the community. However, in recent decades this lagoon has suffered | ||
| 130 | drastic changes and degradation caused by human activities. We | 140 | drastic changes and degradation caused by human activities. We | ||
| 131 | analyzed the concentration of dissolved organic carbon (DOC) and the | 141 | analyzed the concentration of dissolved organic carbon (DOC) and the | ||
| 132 | optical properties of dissolved organic matter (DOM) in the water | 142 | optical properties of dissolved organic matter (DOM) in the water | ||
| 133 | column and sediment pore water during the summer and winter of 2018 | 143 | column and sediment pore water during the summer and winter of 2018 | ||
| 134 | and during eighteen months from 2016 to 2018. Overall, we found that | 144 | and during eighteen months from 2016 to 2018. Overall, we found that | ||
| 135 | the composition of DOM is mainly related to and enhanced by | 145 | the composition of DOM is mainly related to and enhanced by | ||
| 136 | anthropogenic activities and microbial metabolism. DOM enters the | 146 | anthropogenic activities and microbial metabolism. DOM enters the | ||
| 137 | lagoon via urban and agricultural runoff, drainage systems, and | 147 | lagoon via urban and agricultural runoff, drainage systems, and | ||
| 138 | wastewater treatment plants. Additionally, strong microbial metabolism | 148 | wastewater treatment plants. Additionally, strong microbial metabolism | ||
| 139 | in sediments leads to differences in DOM composition between water and | 149 | in sediments leads to differences in DOM composition between water and | ||
| 140 | sediments. In the water column, humic-like components accounted for 71 | 150 | sediments. In the water column, humic-like components accounted for 71 | ||
| 141 | % of the total DOM, while protein-like compounds were most abundant in | 151 | % of the total DOM, while protein-like compounds were most abundant in | ||
| 142 | sediment pore water. We observed a strong seasonal variability | 152 | sediment pore water. We observed a strong seasonal variability | ||
| 143 | associated with precipitation and the system collapse in 2016 | 153 | associated with precipitation and the system collapse in 2016 | ||
| 144 | (phytoplankton bloom), which resulted in the death of 80 % of | 154 | (phytoplankton bloom), which resulted in the death of 80 % of | ||
| 145 | macrophytes. The sediments act as a source of DOM to the overlying | 155 | macrophytes. The sediments act as a source of DOM to the overlying | ||
| 146 | water, likely due to relatively high organic matter content and | 156 | water, likely due to relatively high organic matter content and | ||
| 147 | intense microbial activity, primarily through anaerobic pathways. | 157 | intense microbial activity, primarily through anaerobic pathways. | ||
| 148 | Benthic fluxes of DOC ranged from 5.24 to 33.30 mmol m\u22122 | 158 | Benthic fluxes of DOC ranged from 5.24 to 33.30 mmol m\u22122 | ||
| 149 | d\u22121, being higher in winter than summer 2018 and decreasing from | 159 | d\u22121, being higher in winter than summer 2018 and decreasing from | ||
| 150 | north to south, likely related to lower residence time in the northern | 160 | north to south, likely related to lower residence time in the northern | ||
| 151 | basin, groundwater discharge and accumulation of organic matter from | 161 | basin, groundwater discharge and accumulation of organic matter from | ||
| 152 | the dead meadows. We estimate a net flux of DOC from the Mar Menor | 162 | the dead meadows. We estimate a net flux of DOC from the Mar Menor | ||
| 153 | toward the Mediterranean Sea of 1.57 \u00d7 107 mol yr\u22121." | 163 | toward the Mediterranean Sea of 1.57 \u00d7 107 mol yr\u22121." | ||
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| 338 | Menor, Spain): Characteristics, sources, and benthic fluxes", | 348 | Menor, Spain): Characteristics, sources, and benthic fluxes", | ||
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| 340 | "es": "Dissolved organic matter distribution in the water column | 350 | "es": "Dissolved organic matter distribution in the water column | ||
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| 342 | Menor, Spain): Characteristics, sources, and benthic fluxes" | 352 | Menor, Spain): Characteristics, sources, and benthic fluxes" | ||
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