Interactions between sunlight and microorganisms influence dissolved organic matter degradation along the aquatic continuum
CO2 emissions from inland surface waters to the atmosphere are almost as large as the net carbon transfer from the atmosphere to Earth's land surface. This large flux is supported by dissolved organic matter (DOM) from land and its complete oxidation to CO2 in freshwaters. A critical nexus in t...
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Published in | Limnology and oceanography letters Vol. 3; no. 3; pp. 102 - 116 |
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Main Authors | , |
Format | Journal Article |
Language | English |
Published |
Hoboken
John Wiley & Sons, Inc
01.06.2018
Wiley |
Subjects | |
Online Access | Get full text |
ISSN | 2378-2242 2378-2242 |
DOI | 10.1002/lol2.10060 |
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Abstract | CO2 emissions from inland surface waters to the atmosphere are almost as large as the net carbon transfer from the atmosphere to Earth's land surface. This large flux is supported by dissolved organic matter (DOM) from land and its complete oxidation to CO2 in freshwaters. A critical nexus in the global carbon cycle is the fate of DOM, either complete or partial oxidation. Interactions between sunlight and microbes control DOM degradation, but the relative importance of photodegradation vs. degradation by microbes is poorly known. The knowledge gaps required to advance understanding of key interactions between photochemistry and biology influencing DOM degradation include: (1) the efficiencies and products of DOM photodegradation, (2) how do photo‐products control microbial metabolism of photo‐altered DOM and on what time scales, and (3) how do water and DOM residence times and light exposure interact to determine the fate of DOM moving across the landscape to oceans? |
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AbstractList | CO
2
emissions from inland surface waters to the atmosphere are almost as large as the net carbon transfer from the atmosphere to Earth's land surface. This large flux is supported by dissolved organic matter (DOM) from land and its complete oxidation to CO
2
in freshwaters. A critical nexus in the global carbon cycle is the fate of DOM, either complete or partial oxidation. Interactions between sunlight and microbes control DOM degradation, but the relative importance of photodegradation vs. degradation by microbes is poorly known. The knowledge gaps required to advance understanding of key interactions between photochemistry and biology influencing DOM degradation include: (1) the efficiencies and products of DOM photodegradation, (2) how do photo‐products control microbial metabolism of photo‐altered DOM and on what time scales, and (3) how do water and DOM residence times and light exposure interact to determine the fate of DOM moving across the landscape to oceans? Abstract CO2 emissions from inland surface waters to the atmosphere are almost as large as the net carbon transfer from the atmosphere to Earth's land surface. This large flux is supported by dissolved organic matter (DOM) from land and its complete oxidation to CO2 in freshwaters. A critical nexus in the global carbon cycle is the fate of DOM, either complete or partial oxidation. Interactions between sunlight and microbes control DOM degradation, but the relative importance of photodegradation vs. degradation by microbes is poorly known. The knowledge gaps required to advance understanding of key interactions between photochemistry and biology influencing DOM degradation include: (1) the efficiencies and products of DOM photodegradation, (2) how do photo‐products control microbial metabolism of photo‐altered DOM and on what time scales, and (3) how do water and DOM residence times and light exposure interact to determine the fate of DOM moving across the landscape to oceans? CO2 emissions from inland surface waters to the atmosphere are almost as large as the net carbon transfer from the atmosphere to Earth's land surface. This large flux is supported by dissolved organic matter (DOM) from land and its complete oxidation to CO2 in freshwaters. A critical nexus in the global carbon cycle is the fate of DOM, either complete or partial oxidation. Interactions between sunlight and microbes control DOM degradation, but the relative importance of photodegradation vs. degradation by microbes is poorly known. The knowledge gaps required to advance understanding of key interactions between photochemistry and biology influencing DOM degradation include: (1) the efficiencies and products of DOM photodegradation, (2) how do photo‐products control microbial metabolism of photo‐altered DOM and on what time scales, and (3) how do water and DOM residence times and light exposure interact to determine the fate of DOM moving across the landscape to oceans? |
Author | Kling, George W. Cory, Rose M. |
Author_xml | – sequence: 1 givenname: Rose M. orcidid: 0000-0001-9867-7084 surname: Cory fullname: Cory, Rose M. email: rmcory@umich.edu organization: University of Michigan – sequence: 2 givenname: George W. surname: Kling fullname: Kling, George W. organization: University of Michigan |
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Notes | Edited by: Emily Stanley and Paul del Giorgio RMC and GWK led the manuscript effort and contributed equally to the literature synthesis, analysis of current evidence, and writing the manuscript. Data Availability Statement Data used in this paper is archived at the Arctic Data Center This article is an invited paper to the Special Issue: Carbon cycling in inland waters Author Contribution Statement https://arcticdata.io/catalog/#view/doi:10.18739/A2SV8Z . ObjectType-Article-1 SourceType-Scholarly Journals-1 ObjectType-Feature-2 content type line 14 |
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Snippet | CO2 emissions from inland surface waters to the atmosphere are almost as large as the net carbon transfer from the atmosphere to Earth's land surface. This... CO 2 emissions from inland surface waters to the atmosphere are almost as large as the net carbon transfer from the atmosphere to Earth's land surface. This... Abstract CO2 emissions from inland surface waters to the atmosphere are almost as large as the net carbon transfer from the atmosphere to Earth's land surface.... |
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SubjectTerms | Aquatic ecosystems Atmosphere Budgets Carbon cycle Carbon dioxide Creeks & streams Dissolved organic matter Gene expression Lakes Light Metabolism Microorganisms Oceans Oxidation Photochemistry Photodegradation Respiration Rivers Sunlight Surface water |
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Title | Interactions between sunlight and microorganisms influence dissolved organic matter degradation along the aquatic continuum |
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