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Title: Reviews and syntheses: Carbonyl sulfide as a multi-scale tracer for carbon and water cycles

Abstract

Abstract. For the past decade, observations of carbonyl sulfide (OCS or COS)have been investigated as a proxy for carbon uptake by plants. OCS is destroyed by enzymes that interact with CO2 during photosynthesis, namely carbonic anhydrase (CA) and RuBisCO, where CA is the more important one. The majority of sources of OCS to the atmosphere are geographically separated from this large plant sink,whereas the sources and sinks of CO2 are co-located in ecosystems. The draw down of OCS can therefore be related to the uptake of CO2 without the added complication of co-located emissions comparable in magnitude. Here we review the state of our understanding of the global OCS cycle and its applications to ecosystem carbon cycle science. OCS uptake is correlated well toplant carbon uptake, especially at the regional scale. OCS can be used in conjunction with other independent measures of ecosystem function, like solar-induced fluorescence and carbon and water isotope studies. More work needs to be done to generate global coverage for OCS observations and to link this powerful atmospheric tracer to systems where fundamental questions concerning the carbon and water cycle remain.

Authors:
ORCiD logo [1];  [2]; ORCiD logo [3];  [4]; ORCiD logo [5];  [6]; ORCiD logo [7]; ORCiD logo [8];  [9];  [9]; ORCiD logo [10]; ORCiD logo [11]; ORCiD logo [7];  [12];  [13];  [14]; ORCiD logo [15]; ORCiD logo [16];  [17];  [18] more »;  [19]; ORCiD logo [3]; ORCiD logo [5];  [5];  [20];  [21]; ORCiD logo [22]; ORCiD logo [13]; ORCiD logo [3]; ORCiD logo [4]; ORCiD logo [7]; ORCiD logo [21];  [3];  [13]; ORCiD logo [23];  [24];  [11];  [4]; ORCiD logo [25]; ORCiD logo [26]; ORCiD logo [27];  [8] « less
  1. Carnegie Institution for Science, Stanford, CA (United States); Univ. of California, Los Angeles, CA (United States)
  2. GEOMAR Helmholtz-Centre for Ocean Research Kiel, Kiel (Germany)
  3. INRA, Villenave d'Ornon (France)
  4. Univ. of Arizona, Tucson, AZ (United States)
  5. Univ. of Innsbruck, Innsbruck (Austria)
  6. Univ. of Bremen, Bremen (Germany)
  7. Univ. of Groningen, Groningen (The Netherlands)
  8. Univ. of California, Santa Cruz, CA (United States)
  9. Lab des Sciences du Climat et de l’Environnement, Gif-sur-Yvette (France)
  10. Harvard School of Engineering and Applied Sciences, Cambridge, MA (United States)
  11. Univ. of California, Los Angeles, CA (United States)
  12. UCLA Joint Institute for Regional Earth System Science and Engineering (JIFRESSE), Pasadena, CA (United States)
  13. Univ. of Helsinki, Helsinki (Finland)
  14. The Open Univ., Milton Keynes (United Kingdom)
  15. Univ. of Illinois at Chicago, Chicago, IL (United States)
  16. Univ. of California, Riverside, CA (United States)
  17. Weizmann Inst. of Science, Rehovot (Israel)
  18. Univ. of California, Merced, CA (United States)
  19. Tokyo National Research Institute for Cultural Properties, Tokyo (Japan)
  20. Oregon State Univ., Corvallis, OR (United States)
  21. Max Planck Institute for Chemistry, Mainz (Germany)
  22. Max Planck Institute for Biogeochemistry, Jena (Germany)
  23. Univ. of Copenhagen, Copenhagen (Denmark)
  24. Boston Univ., Boston, MA (United States)
  25. Univ. of California, Irvine, CA (United States)
  26. NOAA/ESRL/GMD, Boulder, CO (United States)
  27. Carnegie Institution for Science, Stanford, CA (United States)
Publication Date:
Research Org.:
Lawrence Berkeley National Laboratory (LBNL), Berkeley, CA (United States). National Energy Research Scientific Computing Center (NERSC)
Sponsoring Org.:
USDOE
OSTI Identifier:
1544102
Resource Type:
Accepted Manuscript
Journal Name:
Biogeosciences (Online)
Additional Journal Information:
Journal Name: Biogeosciences (Online); Journal Volume: 15; Journal Issue: 12; Journal ID: ISSN 1726-4189
Publisher:
European Geosciences Union
Country of Publication:
United States
Language:
English
Subject:
54 ENVIRONMENTAL SCIENCES; Environmental Sciences & Ecology; Geology

Citation Formats

Whelan, Mary E., Lennartz, Sinikka T., Gimeno, Teresa E., Wehr, Richard, Wohlfahrt, Georg, Wang, Yuting, Kooijmans, Linda M. J., Hilton, Timothy W., Belviso, Sauveur, Peylin, Philippe, Commane, Róisín, Sun, Wu, Chen, Huilin, Kuai, Le, Mammarella, Ivan, Maseyk, Kadmiel, Berkelhammer, Max, Li, King -Fai, Yakir, Dan, Zumkehr, Andrew, Katayama, Yoko, Ogée, Jérôme, Spielmann, Felix M., Kitz, Florian, Rastogi, Bharat, Kesselmeier, Jürgen, Marshall, Julia, Erkkilä, Kukka -Maaria, Wingate, Lisa, Meredith, Laura K., He, Wei, Bunk, Rüdiger, Launois, Thomas, Vesala, Timo, Schmidt, Johan A., Fichot, Cédric G., Seibt, Ulli, Saleska, Scott, Saltzman, Eric S., Montzka, Stephen A., Berry, Joseph A., and Campbell, J. Elliott. Reviews and syntheses: Carbonyl sulfide as a multi-scale tracer for carbon and water cycles. United States: N. p., 2018. Web. doi:10.5194/bg-15-3625-2018.
Whelan, Mary E., Lennartz, Sinikka T., Gimeno, Teresa E., Wehr, Richard, Wohlfahrt, Georg, Wang, Yuting, Kooijmans, Linda M. J., Hilton, Timothy W., Belviso, Sauveur, Peylin, Philippe, Commane, Róisín, Sun, Wu, Chen, Huilin, Kuai, Le, Mammarella, Ivan, Maseyk, Kadmiel, Berkelhammer, Max, Li, King -Fai, Yakir, Dan, Zumkehr, Andrew, Katayama, Yoko, Ogée, Jérôme, Spielmann, Felix M., Kitz, Florian, Rastogi, Bharat, Kesselmeier, Jürgen, Marshall, Julia, Erkkilä, Kukka -Maaria, Wingate, Lisa, Meredith, Laura K., He, Wei, Bunk, Rüdiger, Launois, Thomas, Vesala, Timo, Schmidt, Johan A., Fichot, Cédric G., Seibt, Ulli, Saleska, Scott, Saltzman, Eric S., Montzka, Stephen A., Berry, Joseph A., & Campbell, J. Elliott. Reviews and syntheses: Carbonyl sulfide as a multi-scale tracer for carbon and water cycles. United States. https://doi.org/10.5194/bg-15-3625-2018
Whelan, Mary E., Lennartz, Sinikka T., Gimeno, Teresa E., Wehr, Richard, Wohlfahrt, Georg, Wang, Yuting, Kooijmans, Linda M. J., Hilton, Timothy W., Belviso, Sauveur, Peylin, Philippe, Commane, Róisín, Sun, Wu, Chen, Huilin, Kuai, Le, Mammarella, Ivan, Maseyk, Kadmiel, Berkelhammer, Max, Li, King -Fai, Yakir, Dan, Zumkehr, Andrew, Katayama, Yoko, Ogée, Jérôme, Spielmann, Felix M., Kitz, Florian, Rastogi, Bharat, Kesselmeier, Jürgen, Marshall, Julia, Erkkilä, Kukka -Maaria, Wingate, Lisa, Meredith, Laura K., He, Wei, Bunk, Rüdiger, Launois, Thomas, Vesala, Timo, Schmidt, Johan A., Fichot, Cédric G., Seibt, Ulli, Saleska, Scott, Saltzman, Eric S., Montzka, Stephen A., Berry, Joseph A., and Campbell, J. Elliott. Mon . "Reviews and syntheses: Carbonyl sulfide as a multi-scale tracer for carbon and water cycles". United States. https://doi.org/10.5194/bg-15-3625-2018. https://www.osti.gov/servlets/purl/1544102.
@article{osti_1544102,
title = {Reviews and syntheses: Carbonyl sulfide as a multi-scale tracer for carbon and water cycles},
author = {Whelan, Mary E. and Lennartz, Sinikka T. and Gimeno, Teresa E. and Wehr, Richard and Wohlfahrt, Georg and Wang, Yuting and Kooijmans, Linda M. J. and Hilton, Timothy W. and Belviso, Sauveur and Peylin, Philippe and Commane, Róisín and Sun, Wu and Chen, Huilin and Kuai, Le and Mammarella, Ivan and Maseyk, Kadmiel and Berkelhammer, Max and Li, King -Fai and Yakir, Dan and Zumkehr, Andrew and Katayama, Yoko and Ogée, Jérôme and Spielmann, Felix M. and Kitz, Florian and Rastogi, Bharat and Kesselmeier, Jürgen and Marshall, Julia and Erkkilä, Kukka -Maaria and Wingate, Lisa and Meredith, Laura K. and He, Wei and Bunk, Rüdiger and Launois, Thomas and Vesala, Timo and Schmidt, Johan A. and Fichot, Cédric G. and Seibt, Ulli and Saleska, Scott and Saltzman, Eric S. and Montzka, Stephen A. and Berry, Joseph A. and Campbell, J. Elliott},
abstractNote = {Abstract. For the past decade, observations of carbonyl sulfide (OCS or COS)have been investigated as a proxy for carbon uptake by plants. OCS is destroyed by enzymes that interact with CO2 during photosynthesis, namely carbonic anhydrase (CA) and RuBisCO, where CA is the more important one. The majority of sources of OCS to the atmosphere are geographically separated from this large plant sink,whereas the sources and sinks of CO2 are co-located in ecosystems. The draw down of OCS can therefore be related to the uptake of CO2 without the added complication of co-located emissions comparable in magnitude. Here we review the state of our understanding of the global OCS cycle and its applications to ecosystem carbon cycle science. OCS uptake is correlated well toplant carbon uptake, especially at the regional scale. OCS can be used in conjunction with other independent measures of ecosystem function, like solar-induced fluorescence and carbon and water isotope studies. More work needs to be done to generate global coverage for OCS observations and to link this powerful atmospheric tracer to systems where fundamental questions concerning the carbon and water cycle remain.},
doi = {10.5194/bg-15-3625-2018},
journal = {Biogeosciences (Online)},
number = 12,
volume = 15,
place = {United States},
year = {Mon Jun 18 00:00:00 EDT 2018},
month = {Mon Jun 18 00:00:00 EDT 2018}
}

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The temporal trend of stratospheric carbonyl sulfide
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In situ soil COS exchange of a temperate mountain grassland under simulated drought
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Bryophyte gas-exchange dynamics along varying hydration status reveal a significant carbonyl sulphide (COS) sink in the dark and COS source in the light
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Microbial life in the phyllosphere
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A thiocyanate hydrolase of Thiobacillus thioparus. A novel enzyme catalyzing the formation of carbonyl sulfide from thiocyanate.
journal, May 1992


Carbonyl sulfide: an alternate substrate for but not an activator of ribulose-1,5-bisphosphate carboxylase
journal, February 1989


Measurements of the exchange of carbonyl sulfide (OCS) and carbon disulfide (<mml:math altimg="si33.gif" overflow="scroll" xmlns:xocs="http://www.elsevier.com/xml/xocs/dtd" xmlns:xs="http://www.w3.org/2001/XMLSchema" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xmlns="http://www.elsevier.com/xml/ja/dtd" xmlns:ja="http://www.elsevier.com/xml/ja/dtd" xmlns:mml="http://www.w3.org/1998/Math/MathML" xmlns:tb="http://www.elsevier.com/xml/common/table/dtd" xmlns:sb="http://www.elsevier.com/xml/common/struct-bib/dtd" xmlns:ce="http://www.elsevier.com/xml/common/dtd" xmlns:xlink="http://www.w3.org/1999/xlink" xmlns:cals="http://www.elsevier.com/xml/common/cals/dtd"><mml:msub><mml:mrow><mml:mi>CS</mml:mi></mml:mrow><mml:mrow><mml:mn>2</mml:mn></mml:mrow></mml:msub></mml:math>) between soil and atmosphere in a spruce forest in central Germany
journal, November 2004


Works referencing / citing this record:

Higher than expected CO 2 fertilization inferred from leaf to global observations
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The influence of dissolved organic matter on the marine production of carbonyl sulfide (OCS) and carbon disulfide (CS2) in the Peruvian upwelling
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Carbonyl sulfide (COS) and carbon disulfide (CS2) exchange fluxes between cotton fields and the atmosphere in the arid area in Xinjiang, China
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Partitioning net carbon dioxide fluxes into photosynthesis and respiration using neural networks
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Ecosystem transpiration and evaporation: Insights from three water flux partitioning methods across FLUXNET sites
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Stomatal control of leaf fluxes of carbonyl sulfide and CO 2 in a Typha freshwater marsh
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Soil–atmosphere exchange of carbonyl sulfide in a Mediterranean citrus orchard
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Influences of light and humidity on carbonyl sulfide-based estimates of photosynthesis
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Nitrogen Fertilization Reduces the Capacity of Soils to Take up Atmospheric Carbonyl Sulphide
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Coupled Biological and Abiotic Mechanisms Driving Carbonyl Sulfide Production in Soils
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Gross Primary Productivity of Four European Ecosystems Constrained by Joint CO 2 and COS Flux Measurements
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Reviews and syntheses: Turning the challenges of partitioning ecosystem evaporation and transpiration into opportunities
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