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Browning of boreal freshwaters coupled to carbon-iron interactions along the aquatic continuum
The color of freshwaters, often measured as absorbance, influences a number of ecosystem services including biodiversity, fish production, and drinking water quality. Many countries have recently reported on increasing trends of water color in freshwaters, for which drivers are still not fully under...
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Published in: | PloS one 2014-02, Vol.9 (2), p.e88104 |
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description | The color of freshwaters, often measured as absorbance, influences a number of ecosystem services including biodiversity, fish production, and drinking water quality. Many countries have recently reported on increasing trends of water color in freshwaters, for which drivers are still not fully understood. We show here with more than 58000 water samples from the boreal and hemiboreal region of Sweden and Canada that absorbance of filtered water (a₄₂₀) co-varied with dissolved organic carbon (DOC) concentrations (R² = 0.85, P |
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Many countries have recently reported on increasing trends of water color in freshwaters, for which drivers are still not fully understood. We show here with more than 58000 water samples from the boreal and hemiboreal region of Sweden and Canada that absorbance of filtered water (a₄₂₀) co-varied with dissolved organic carbon (DOC) concentrations (R² = 0.85, P<0.0001), but that a₄₂₀ relative to DOC is increased by the presence of iron (Fe). We found that concentrations of Fe significantly declined with increasing water retention in the landscape, resulting in significantly lower Fe concentrations in lakes compared to running waters. The Fe loss along the aquatic continuum corresponded to a proportional loss in a₄₂₀, suggesting a tight biogeochemical coupling between colored dissolved organic matter and Fe. Since water is being flushed at increasing rates due to enhanced runoff in the studied regions, diminished loss of Fe along the aquatic continuum may be one reason for observed trends in a₄₂₀, and in particular in a₄₂₀/DOC increases. If trends of increased Fe concentrations in freshwaters continue, water color will further increase with various effects on ecosystem services and biogeochemical cycles.</description><identifier>ISSN: 1932-6203</identifier><identifier>EISSN: 1932-6203</identifier><identifier>DOI: 10.1371/journal.pone.0088104</identifier><identifier>PMID: 24505396</identifier><language>eng</language><publisher>United States: Public Library of Science</publisher><subject>Absorbance ; Aquatic sciences ; Biodiversity ; Biogeochemical cycles ; Biology ; Browning ; Carbon - analysis ; Chemistry ; Color ; Creeks & streams ; Dissolved organic carbon ; Dissolved organic matter ; Drinking water ; Earth Sciences ; Ecosystem assessment ; Ecosystem services ; Ecosystems ; Environmental Monitoring ; Fresh water ; Fresh Water - analysis ; Geochemistry ; Iron ; Iron - analysis ; Laboratories ; Lakes ; Limnology ; Materials Science ; Oceanography ; Organic carbon ; Precipitation ; Respiration ; Rivers ; Running waters ; Runoff ; Trends ; Water analysis ; Water color ; Water purification ; Water quality ; Water sampling</subject><ispartof>PloS one, 2014-02, Vol.9 (2), p.e88104</ispartof><rights>COPYRIGHT 2014 Public Library of Science</rights><rights>2014 Weyhenmeyer et al. This is an open-access article distributed under the terms of the Creative Commons Attribution License: http://creativecommons.org/licenses/by/4.0/ (the “License”), which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited. 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Many countries have recently reported on increasing trends of water color in freshwaters, for which drivers are still not fully understood. We show here with more than 58000 water samples from the boreal and hemiboreal region of Sweden and Canada that absorbance of filtered water (a₄₂₀) co-varied with dissolved organic carbon (DOC) concentrations (R² = 0.85, P<0.0001), but that a₄₂₀ relative to DOC is increased by the presence of iron (Fe). We found that concentrations of Fe significantly declined with increasing water retention in the landscape, resulting in significantly lower Fe concentrations in lakes compared to running waters. The Fe loss along the aquatic continuum corresponded to a proportional loss in a₄₂₀, suggesting a tight biogeochemical coupling between colored dissolved organic matter and Fe. Since water is being flushed at increasing rates due to enhanced runoff in the studied regions, diminished loss of Fe along the aquatic continuum may be one reason for observed trends in a₄₂₀, and in particular in a₄₂₀/DOC increases. If trends of increased Fe concentrations in freshwaters continue, water color will further increase with various effects on ecosystem services and biogeochemical cycles.</description><subject>Absorbance</subject><subject>Aquatic sciences</subject><subject>Biodiversity</subject><subject>Biogeochemical cycles</subject><subject>Biology</subject><subject>Browning</subject><subject>Carbon - analysis</subject><subject>Chemistry</subject><subject>Color</subject><subject>Creeks & streams</subject><subject>Dissolved organic carbon</subject><subject>Dissolved organic matter</subject><subject>Drinking water</subject><subject>Earth Sciences</subject><subject>Ecosystem assessment</subject><subject>Ecosystem services</subject><subject>Ecosystems</subject><subject>Environmental Monitoring</subject><subject>Fresh water</subject><subject>Fresh Water - analysis</subject><subject>Geochemistry</subject><subject>Iron</subject><subject>Iron - analysis</subject><subject>Laboratories</subject><subject>Lakes</subject><subject>Limnology</subject><subject>Materials Science</subject><subject>Oceanography</subject><subject>Organic carbon</subject><subject>Precipitation</subject><subject>Respiration</subject><subject>Rivers</subject><subject>Running waters</subject><subject>Runoff</subject><subject>Trends</subject><subject>Water analysis</subject><subject>Water color</subject><subject>Water purification</subject><subject>Water quality</subject><subject>Water sampling</subject><issn>1932-6203</issn><issn>1932-6203</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2014</creationdate><recordtype>article</recordtype><sourceid>PIMPY</sourceid><sourceid>DOA</sourceid><recordid>eNqNU2uLEzEUHURx1-o_EB0QBMHWvGYm-SLU9VVYWPCxHw13Mpk2ZZp0k4nVf2_azi4dUJAQ8rjnHG5O7s2ypxjNMK3wm7WL3kI32zqrZwhxjhG7l51jQcm0JIjeP9mfZY9CWCNUUF6WD7Mzwoq0F-V59uOddztr7DJ3bV47r6HLW6_Dage99iFXLm473eS9yxX42tmp8c7mxqYoqN44G3LoXOL3K53DTYTeqMSyvbExbh5nD1rogn4yrJPs-8cP3y4-Ty-vPi0u5pdTVYmin1Koi1pTgSkSwFTLMHCejoLzijUEUN3ofUBwQbioaEkE47gqilbgsgFNJ9nzo-62c0EO1gSZBCjDBUnLJFscEY2Dtdx6swH_Wzow8nDh_FKCT7l3WiaXcMtEQRpUMwSKq7YqSl2BbhgluEpar49aYae3sR6pvTfX84NajJIQVHGR4G-H5GK90Y3StvfQjVjjiDUruXQ_ZXKACVokgReDgHc3UYf-Hy8cUEtIjzC2dUlMbUxQcs4qzkma-2Rmf0Gl0eiNSf-mW5PuR4RXI8L-b_WvfgkxBLn4-uX_sVfXY-zLE-wqFV6_Cq6Lh5oaA9kRqLwLwev2zjmM5L4Vbt2Q-1aQQysk2rNT1-9It7VP_wDmrASK</recordid><startdate>20140205</startdate><enddate>20140205</enddate><creator>Weyhenmeyer, Gesa A</creator><creator>Prairie, Yves T</creator><creator>Tranvik, Lars J</creator><general>Public Library of Science</general><general>Public Library of Science (PLoS)</general><scope>CGR</scope><scope>CUY</scope><scope>CVF</scope><scope>ECM</scope><scope>EIF</scope><scope>NPM</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>IOV</scope><scope>ISR</scope><scope>3V.</scope><scope>7QG</scope><scope>7QL</scope><scope>7QO</scope><scope>7RV</scope><scope>7SN</scope><scope>7SS</scope><scope>7T5</scope><scope>7TG</scope><scope>7TM</scope><scope>7U9</scope><scope>7X2</scope><scope>7X7</scope><scope>7XB</scope><scope>88E</scope><scope>8AO</scope><scope>8C1</scope><scope>8FD</scope><scope>8FE</scope><scope>8FG</scope><scope>8FH</scope><scope>8FI</scope><scope>8FJ</scope><scope>8FK</scope><scope>ABJCF</scope><scope>ABUWG</scope><scope>AEUYN</scope><scope>AFKRA</scope><scope>ARAPS</scope><scope>ATCPS</scope><scope>AZQEC</scope><scope>BBNVY</scope><scope>BENPR</scope><scope>BGLVJ</scope><scope>BHPHI</scope><scope>C1K</scope><scope>CCPQU</scope><scope>D1I</scope><scope>DWQXO</scope><scope>FR3</scope><scope>FYUFA</scope><scope>GHDGH</scope><scope>GNUQQ</scope><scope>H94</scope><scope>HCIFZ</scope><scope>K9.</scope><scope>KB.</scope><scope>KB0</scope><scope>KL.</scope><scope>L6V</scope><scope>LK8</scope><scope>M0K</scope><scope>M0S</scope><scope>M1P</scope><scope>M7N</scope><scope>M7P</scope><scope>M7S</scope><scope>NAPCQ</scope><scope>P5Z</scope><scope>P62</scope><scope>P64</scope><scope>PATMY</scope><scope>PDBOC</scope><scope>PIMPY</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>PRINS</scope><scope>PTHSS</scope><scope>PYCSY</scope><scope>RC3</scope><scope>5PM</scope><scope>ACNBI</scope><scope>ADTPV</scope><scope>AOWAS</scope><scope>D8T</scope><scope>DF2</scope><scope>ZZAVC</scope><scope>DOA</scope></search><sort><creationdate>20140205</creationdate><title>Browning of boreal freshwaters coupled to carbon-iron interactions along the aquatic continuum</title><author>Weyhenmeyer, Gesa A ; Prairie, Yves T ; Tranvik, Lars J</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c795t-3ab5be391309a4cf41a8839198874d2a0bde9a4c98928973629481755f916dae3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2014</creationdate><topic>Absorbance</topic><topic>Aquatic sciences</topic><topic>Biodiversity</topic><topic>Biogeochemical cycles</topic><topic>Biology</topic><topic>Browning</topic><topic>Carbon - 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Many countries have recently reported on increasing trends of water color in freshwaters, for which drivers are still not fully understood. We show here with more than 58000 water samples from the boreal and hemiboreal region of Sweden and Canada that absorbance of filtered water (a₄₂₀) co-varied with dissolved organic carbon (DOC) concentrations (R² = 0.85, P<0.0001), but that a₄₂₀ relative to DOC is increased by the presence of iron (Fe). We found that concentrations of Fe significantly declined with increasing water retention in the landscape, resulting in significantly lower Fe concentrations in lakes compared to running waters. The Fe loss along the aquatic continuum corresponded to a proportional loss in a₄₂₀, suggesting a tight biogeochemical coupling between colored dissolved organic matter and Fe. Since water is being flushed at increasing rates due to enhanced runoff in the studied regions, diminished loss of Fe along the aquatic continuum may be one reason for observed trends in a₄₂₀, and in particular in a₄₂₀/DOC increases. If trends of increased Fe concentrations in freshwaters continue, water color will further increase with various effects on ecosystem services and biogeochemical cycles.</abstract><cop>United States</cop><pub>Public Library of Science</pub><pmid>24505396</pmid><doi>10.1371/journal.pone.0088104</doi><tpages>e88104</tpages><oa>free_for_read</oa></addata></record> |
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subjects | Absorbance Aquatic sciences Biodiversity Biogeochemical cycles Biology Browning Carbon - analysis Chemistry Color Creeks & streams Dissolved organic carbon Dissolved organic matter Drinking water Earth Sciences Ecosystem assessment Ecosystem services Ecosystems Environmental Monitoring Fresh water Fresh Water - analysis Geochemistry Iron Iron - analysis Laboratories Lakes Limnology Materials Science Oceanography Organic carbon Precipitation Respiration Rivers Running waters Runoff Trends Water analysis Water color Water purification Water quality Water sampling |
title | Browning of boreal freshwaters coupled to carbon-iron interactions along the aquatic continuum |
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