Greenhouse gases and biogeochemical diel fluctuations in a high-altitude wetland

The landscapes of high-altitude wetland ecosystems are characterized by different kinds of aquatic sites, including ponds holding conspicuous microbial life. Here, we examined a representative pond of the wetland landscape for dynamics of greenhouse gases, and their association with other relevant b...

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Veröffentlicht in:The Science of the total environment 2021-05, Vol.768, p.144370, Article 144370
Hauptverfasser: Molina, Verónica, Eissler, Yoanna, Fernandez, Camila, Cornejo-D'Ottone, Marcela, Dorador, Cristina, Bebout, Brad M., Jeffrey, Wade H., Romero, Carlos, Hengst, Martha
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container_volume 768
creator Molina, Verónica
Eissler, Yoanna
Fernandez, Camila
Cornejo-D'Ottone, Marcela
Dorador, Cristina
Bebout, Brad M.
Jeffrey, Wade H.
Romero, Carlos
Hengst, Martha
description The landscapes of high-altitude wetland ecosystems are characterized by different kinds of aquatic sites, including ponds holding conspicuous microbial life. Here, we examined a representative pond of the wetland landscape for dynamics of greenhouse gases, and their association with other relevant biogeochemical conditions including diel shifts of microbial communities' structure and activity over two consecutive days. Satellite image analysis indicates that the area of ponds cover 238 of 381.3 Ha (i.e., 62.4%), representing a significant landscape in this wetland. Solar radiation, wind velocity and temperature varied daily and between the days sampled, influencing the biogeochemical dynamics in the pond, shifting the pond reservoir of inorganic versus dissolved organic nitrogen/phosphorus bioavailability, between day 1 and day 2. Day 2 was characterized by high dissolved organic nitrogen/phosphorus and N2O accumulation. CH4 presented a positive excess showing maxima at hours of high radiation during both days. The microbial community in the sediment was diverse and enriched in keystone active groups potentially related with GHG recycling including bacteria and archaea, such as Cyanobacteria, Verrucomicrobia, Rhodobacterales and Nanoarchaeaota (Woesearchaeia). Archaea account for the microbial community composition changes between both days and for the secondary productivity in the water measured during day 2. The results indicate that an intense recycling of organic matter occurs in the pond systems and that the activity of the microbial community is correlated with the availability of nutrients. Together, the above results indicate a net sink of CO2 and N2O, which has also been reported for other natural and artificial ponds. Overall, our two-day fluctuation study in a representative pond of a high-altitude wetland aquatic landscape indicates the need to explore in more detail the short-term besides the long-term biogeochemical variability in arid ecosystems of the Andes plateau, where wetlands are hotspots of life currently under high anthropogenic pressure. [Display omitted] •Ponds represent a significant landscape in this high-altitude wetland, covering 238 Ha, i.e., 62.4% of the flooded areas.•Weather conditions including solar radiation, temperature and wind velocity influence biogeochemical diel dynamics.•Microbial community structure and activity respond to changes mainly associated with nutrients and dissolved organic matter.•Changes between cons
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Here, we examined a representative pond of the wetland landscape for dynamics of greenhouse gases, and their association with other relevant biogeochemical conditions including diel shifts of microbial communities' structure and activity over two consecutive days. Satellite image analysis indicates that the area of ponds cover 238 of 381.3 Ha (i.e., 62.4%), representing a significant landscape in this wetland. Solar radiation, wind velocity and temperature varied daily and between the days sampled, influencing the biogeochemical dynamics in the pond, shifting the pond reservoir of inorganic versus dissolved organic nitrogen/phosphorus bioavailability, between day 1 and day 2. Day 2 was characterized by high dissolved organic nitrogen/phosphorus and N2O accumulation. CH4 presented a positive excess showing maxima at hours of high radiation during both days. The microbial community in the sediment was diverse and enriched in keystone active groups potentially related with GHG recycling including bacteria and archaea, such as Cyanobacteria, Verrucomicrobia, Rhodobacterales and Nanoarchaeaota (Woesearchaeia). Archaea account for the microbial community composition changes between both days and for the secondary productivity in the water measured during day 2. The results indicate that an intense recycling of organic matter occurs in the pond systems and that the activity of the microbial community is correlated with the availability of nutrients. Together, the above results indicate a net sink of CO2 and N2O, which has also been reported for other natural and artificial ponds. Overall, our two-day fluctuation study in a representative pond of a high-altitude wetland aquatic landscape indicates the need to explore in more detail the short-term besides the long-term biogeochemical variability in arid ecosystems of the Andes plateau, where wetlands are hotspots of life currently under high anthropogenic pressure. [Display omitted] •Ponds represent a significant landscape in this high-altitude wetland, covering 238 Ha, i.e., 62.4% of the flooded areas.•Weather conditions including solar radiation, temperature and wind velocity influence biogeochemical diel dynamics.•Microbial community structure and activity respond to changes mainly associated with nutrients and dissolved organic matter.•Changes between consecutive days indicate keystone microbial communities, such as Woesearchaeia and Verrucomicrobia.•This high-altitude wetland produced a net sink for CO2 and N2O, and a source of CH4 in the pond.</description><identifier>ISSN: 0048-9697</identifier><identifier>EISSN: 1879-1026</identifier><identifier>DOI: 10.1016/j.scitotenv.2020.144370</identifier><identifier>PMID: 33454466</identifier><language>eng</language><publisher>AMSTERDAM: Elsevier B.V</publisher><subject>Altitude ; Archaea ; Bacteria ; Biodiversity and Ecology ; C and N biogeochemical cycles ; Diel dynamics ; Environmental Sciences ; Environmental Sciences &amp; Ecology ; Greenhouse gases ; Greenhouse Gases - analysis ; High-altitude wetland ; Life Sciences &amp; Biomedicine ; Methane - analysis ; Microbial diversity ; Science &amp; Technology ; Wetlands</subject><ispartof>The Science of the total environment, 2021-05, Vol.768, p.144370, Article 144370</ispartof><rights>2020 Elsevier B.V.</rights><rights>Copyright © 2020 Elsevier B.V. All rights reserved.</rights><rights>Distributed under a Creative Commons Attribution 4.0 International License</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>true</woscitedreferencessubscribed><woscitedreferencescount>9</woscitedreferencescount><woscitedreferencesoriginalsourcerecordid>wos000625384700024</woscitedreferencesoriginalsourcerecordid><citedby>FETCH-LOGICAL-c405t-d68d54b1d3451608bb64019ae83c74e0164e722f7c3bb8916fd74ffe668861673</citedby><cites>FETCH-LOGICAL-c405t-d68d54b1d3451608bb64019ae83c74e0164e722f7c3bb8916fd74ffe668861673</cites><orcidid>0000-0001-5028-2542</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktohtml>$$Uhttps://dx.doi.org/10.1016/j.scitotenv.2020.144370$$EHTML$$P50$$Gelsevier$$H</linktohtml><link.rule.ids>230,315,781,785,886,3551,27929,27930,39263,46000</link.rule.ids><backlink>$$Uhttps://www.ncbi.nlm.nih.gov/pubmed/33454466$$D View this record in MEDLINE/PubMed$$Hfree_for_read</backlink><backlink>$$Uhttps://hal.science/hal-03097666$$DView record in HAL$$Hfree_for_read</backlink></links><search><creatorcontrib>Molina, Verónica</creatorcontrib><creatorcontrib>Eissler, Yoanna</creatorcontrib><creatorcontrib>Fernandez, Camila</creatorcontrib><creatorcontrib>Cornejo-D'Ottone, Marcela</creatorcontrib><creatorcontrib>Dorador, Cristina</creatorcontrib><creatorcontrib>Bebout, Brad M.</creatorcontrib><creatorcontrib>Jeffrey, Wade H.</creatorcontrib><creatorcontrib>Romero, Carlos</creatorcontrib><creatorcontrib>Hengst, Martha</creatorcontrib><title>Greenhouse gases and biogeochemical diel fluctuations in a high-altitude wetland</title><title>The Science of the total environment</title><addtitle>SCI TOTAL ENVIRON</addtitle><addtitle>Sci Total Environ</addtitle><description>The landscapes of high-altitude wetland ecosystems are characterized by different kinds of aquatic sites, including ponds holding conspicuous microbial life. 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The microbial community in the sediment was diverse and enriched in keystone active groups potentially related with GHG recycling including bacteria and archaea, such as Cyanobacteria, Verrucomicrobia, Rhodobacterales and Nanoarchaeaota (Woesearchaeia). Archaea account for the microbial community composition changes between both days and for the secondary productivity in the water measured during day 2. The results indicate that an intense recycling of organic matter occurs in the pond systems and that the activity of the microbial community is correlated with the availability of nutrients. Together, the above results indicate a net sink of CO2 and N2O, which has also been reported for other natural and artificial ponds. Overall, our two-day fluctuation study in a representative pond of a high-altitude wetland aquatic landscape indicates the need to explore in more detail the short-term besides the long-term biogeochemical variability in arid ecosystems of the Andes plateau, where wetlands are hotspots of life currently under high anthropogenic pressure. [Display omitted] •Ponds represent a significant landscape in this high-altitude wetland, covering 238 Ha, i.e., 62.4% of the flooded areas.•Weather conditions including solar radiation, temperature and wind velocity influence biogeochemical diel dynamics.•Microbial community structure and activity respond to changes mainly associated with nutrients and dissolved organic matter.•Changes between consecutive days indicate keystone microbial communities, such as Woesearchaeia and Verrucomicrobia.•This high-altitude wetland produced a net sink for CO2 and N2O, and a source of CH4 in the pond.</description><subject>Altitude</subject><subject>Archaea</subject><subject>Bacteria</subject><subject>Biodiversity and Ecology</subject><subject>C and N biogeochemical cycles</subject><subject>Diel dynamics</subject><subject>Environmental Sciences</subject><subject>Environmental Sciences &amp; Ecology</subject><subject>Greenhouse gases</subject><subject>Greenhouse Gases - analysis</subject><subject>High-altitude wetland</subject><subject>Life Sciences &amp; 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Here, we examined a representative pond of the wetland landscape for dynamics of greenhouse gases, and their association with other relevant biogeochemical conditions including diel shifts of microbial communities' structure and activity over two consecutive days. Satellite image analysis indicates that the area of ponds cover 238 of 381.3 Ha (i.e., 62.4%), representing a significant landscape in this wetland. Solar radiation, wind velocity and temperature varied daily and between the days sampled, influencing the biogeochemical dynamics in the pond, shifting the pond reservoir of inorganic versus dissolved organic nitrogen/phosphorus bioavailability, between day 1 and day 2. Day 2 was characterized by high dissolved organic nitrogen/phosphorus and N2O accumulation. CH4 presented a positive excess showing maxima at hours of high radiation during both days. The microbial community in the sediment was diverse and enriched in keystone active groups potentially related with GHG recycling including bacteria and archaea, such as Cyanobacteria, Verrucomicrobia, Rhodobacterales and Nanoarchaeaota (Woesearchaeia). Archaea account for the microbial community composition changes between both days and for the secondary productivity in the water measured during day 2. The results indicate that an intense recycling of organic matter occurs in the pond systems and that the activity of the microbial community is correlated with the availability of nutrients. Together, the above results indicate a net sink of CO2 and N2O, which has also been reported for other natural and artificial ponds. Overall, our two-day fluctuation study in a representative pond of a high-altitude wetland aquatic landscape indicates the need to explore in more detail the short-term besides the long-term biogeochemical variability in arid ecosystems of the Andes plateau, where wetlands are hotspots of life currently under high anthropogenic pressure. [Display omitted] •Ponds represent a significant landscape in this high-altitude wetland, covering 238 Ha, i.e., 62.4% of the flooded areas.•Weather conditions including solar radiation, temperature and wind velocity influence biogeochemical diel dynamics.•Microbial community structure and activity respond to changes mainly associated with nutrients and dissolved organic matter.•Changes between consecutive days indicate keystone microbial communities, such as Woesearchaeia and Verrucomicrobia.•This high-altitude wetland produced a net sink for CO2 and N2O, and a source of CH4 in the pond.</abstract><cop>AMSTERDAM</cop><pub>Elsevier B.V</pub><pmid>33454466</pmid><doi>10.1016/j.scitotenv.2020.144370</doi><tpages>12</tpages><orcidid>https://orcid.org/0000-0001-5028-2542</orcidid></addata></record>
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subjects Altitude
Archaea
Bacteria
Biodiversity and Ecology
C and N biogeochemical cycles
Diel dynamics
Environmental Sciences
Environmental Sciences & Ecology
Greenhouse gases
Greenhouse Gases - analysis
High-altitude wetland
Life Sciences & Biomedicine
Methane - analysis
Microbial diversity
Science & Technology
Wetlands
title Greenhouse gases and biogeochemical diel fluctuations in a high-altitude wetland
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