Articles | Volume 18, issue 13
https://doi.org/10.5194/acp-18-9425-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/acp-18-9425-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
05 Jul 2018
Research article |
| 05 Jul 2018
| 05 Jul 2018
Disentangling the rates of carbonyl sulfide (COS) production and consumption and their dependency on soil properties across biomes and land use types
Aurore Kaisermann
CORRESPONDING AUTHOR
INRA/Bordeaux Science Agro, UMR 1391 ISPA, Villenave d'Ornon, 33140,
France
Jérôme Ogée
INRA/Bordeaux Science Agro, UMR 1391 ISPA, Villenave d'Ornon, 33140,
France
Joana Sauze
INRA/Bordeaux Science Agro, UMR 1391 ISPA, Villenave d'Ornon, 33140,
France
Steven Wohl
INRA/Bordeaux Science Agro, UMR 1391 ISPA, Villenave d'Ornon, 33140,
France
Sam P. Jones
INRA/Bordeaux Science Agro, UMR 1391 ISPA, Villenave d'Ornon, 33140,
France
Ana Gutierrez
INRA/Bordeaux Science Agro, UMR 1391 ISPA, Villenave d'Ornon, 33140,
France
Lisa Wingate
INRA/Bordeaux Science Agro, UMR 1391 ISPA, Villenave d'Ornon, 33140,
France
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Robbert Petrus Johannes Moonen, Getachew Agmuas Adnew, Jordi Vilà-Guerau de Arellano, Oscar Karel Hartogensis, David Joan Bonell Fontas, Shujiro Komiya, Sam P. Jones, and Thomas Röckmann
EGUsphere, https://doi.org/10.5194/egusphere-2025-452, https://doi.org/10.5194/egusphere-2025-452, 2025
This preprint is open for discussion and under review for Atmospheric Chemistry and Physics (ACP).
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Understory ejections are distinct turbulent features emerging in prime tall forest ecosystems. We share a method to isolate understory ejections based on H2O-CO2 anomalie quadrants. From these, we calculate the flux contributions of understory ejections and all flux quadrants. In addition we show that a distinctly depleted isotopic composition can be found in the ejected water vapour. Finally, we explored the role of clouds as a potential trigger for understory ejections.
Sophie L. Baartman, Steven M. Driever, Maarten Wassenaar, Linda M. J. Kooijmans, Nerea Ubierna Lopez, Leon Mossink, Maria E. Popa, Ara Cho, Lisa Wingate, Thomas Röckmann, Steven M. A. C. van Heuven, and Maarten C. Krol
EGUsphere, https://doi.org/10.5194/egusphere-2025-215, https://doi.org/10.5194/egusphere-2025-215, 2025
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Carbonyl sulfide (COS) and carbon dioxide (CO2) uptake fluxes and isotope discrimination was measured in sunflower and papyrus plants, using a plant chamber approach and varying light availability. COS and CO2 isotope discrimination in plants have never been jointly measured before. COS isotope discrimination did not differ between the species, nor with changing light. CO2 fluxes and isotope values provided additional useful information for data interpretation.
Guohua Liu, Mirco Migliavacca, Christian Reimers, Basil Kraft, Markus Reichstein, Andrew D. Richardson, Lisa Wingate, Nicolas Delpierre, Hui Yang, and Alexander J. Winkler
Geosci. Model Dev., 17, 6683–6701, https://doi.org/10.5194/gmd-17-6683-2024, https://doi.org/10.5194/gmd-17-6683-2024, 2024
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Our study employs long short-term memory (LSTM) networks to model canopy greenness and phenology, integrating meteorological memory effects. The LSTM model outperforms traditional methods, enhancing accuracy in predicting greenness dynamics and phenological transitions across plant functional types. Highlighting the importance of multi-variate meteorological memory effects, our research pioneers unlock the secrets of vegetation phenology responses to climate change with deep learning techniques.
Luiz A. T. Machado, Jürgen Kesselmeier, Santiago Botía, Hella van Asperen, Meinrat O. Andreae, Alessandro C. de Araújo, Paulo Artaxo, Achim Edtbauer, Rosaria R. Ferreira, Marco A. Franco, Hartwig Harder, Sam P. Jones, Cléo Q. Dias-Júnior, Guido G. Haytzmann, Carlos A. Quesada, Shujiro Komiya, Jost Lavric, Jos Lelieveld, Ingeborg Levin, Anke Nölscher, Eva Pfannerstill, Mira L. Pöhlker, Ulrich Pöschl, Akima Ringsdorf, Luciana Rizzo, Ana M. Yáñez-Serrano, Susan Trumbore, Wanda I. D. Valenti, Jordi Vila-Guerau de Arellano, David Walter, Jonathan Williams, Stefan Wolff, and Christopher Pöhlker
Atmos. Chem. Phys., 24, 8893–8910, https://doi.org/10.5194/acp-24-8893-2024, https://doi.org/10.5194/acp-24-8893-2024, 2024
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Composite analysis of gas concentration before and after rainfall, during the day and night, gives insight into the complex relationship between trace gas variability and precipitation. The analysis helps us to understand the sources and sinks of trace gases within a forest ecosystem. It elucidates processes that are not discernible under undisturbed conditions and contributes to a deeper understanding of the trace gas life cycle and its intricate interactions with cloud dynamics in the Amazon.
Clémence Paul, Clément Piel, Joana Sauze, Olivier Jossoud, Arnaud Dapoigny, Daniele Romanini, Frédérique Prié, Sébastien Devidal, Roxanne Jacob, Alexandru Milcu, and Amaëlle Landais
EGUsphere, https://doi.org/10.5194/egusphere-2024-1755, https://doi.org/10.5194/egusphere-2024-1755, 2024
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Our study investigated the influence of plant processes on oxygen dynamics, crucial for paleoclimatology. By examining maize respiration and photosynthesis using advanced techniques, we enhanced our understanding of past climates through ice core analysis.
Clémence Paul, Clément Piel, Joana Sauze, Nicolas Pasquier, Frédéric Prié, Sébastien Devidal, Roxanne Jacob, Arnaud Dapoigny, Olivier Jossoud, Alexandru Milcu, and Amaëlle Landais
Biogeosciences, 20, 1047–1062, https://doi.org/10.5194/bg-20-1047-2023, https://doi.org/10.5194/bg-20-1047-2023, 2023
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To improve the interpretation of the δ18Oatm and Δ17O of O2 in air bubbles in ice cores, we need to better quantify the oxygen fractionation coefficients associated with biological processes. We performed a simplified analogue of the terrestrial biosphere in a closed chamber. We found a respiration fractionation in agreement with the previous estimates at the microorganism scale, and a terrestrial photosynthetic fractionation was found. This has an impact on the estimation of the Dole effect.
Javier de la Casa, Adrià Barbeta, Asun Rodríguez-Uña, Lisa Wingate, Jérôme Ogée, and Teresa E. Gimeno
Hydrol. Earth Syst. Sci., 26, 4125–4146, https://doi.org/10.5194/hess-26-4125-2022, https://doi.org/10.5194/hess-26-4125-2022, 2022
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Recently, studies have been reporting mismatches in the water isotopic composition of plants and soils. In this work, we reviewed worldwide isotopic composition data of field and laboratory studies to see if the mismatch is generalised, and we found it to be true. This contradicts theoretical expectations and may underlie an non-described phenomenon that should be forward investigated and implemented in ecohydrological models to avoid erroneous estimations of water sources used by vegetation.
Linda M. J. Kooijmans, Ara Cho, Jin Ma, Aleya Kaushik, Katherine D. Haynes, Ian Baker, Ingrid T. Luijkx, Mathijs Groenink, Wouter Peters, John B. Miller, Joseph A. Berry, Jerome Ogée, Laura K. Meredith, Wu Sun, Kukka-Maaria Kohonen, Timo Vesala, Ivan Mammarella, Huilin Chen, Felix M. Spielmann, Georg Wohlfahrt, Max Berkelhammer, Mary E. Whelan, Kadmiel Maseyk, Ulli Seibt, Roisin Commane, Richard Wehr, and Maarten Krol
Biogeosciences, 18, 6547–6565, https://doi.org/10.5194/bg-18-6547-2021, https://doi.org/10.5194/bg-18-6547-2021, 2021
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The gas carbonyl sulfide (COS) can be used to estimate photosynthesis. To adopt this approach on regional and global scales, we need biosphere models that can simulate COS exchange. So far, such models have not been evaluated against observations. We evaluate the COS biosphere exchange of the SiB4 model against COS flux observations. We find that the model is capable of simulating key processes in COS biosphere exchange. Still, we give recommendations for further improvement of the model.
Rafael Poyatos, Víctor Granda, Víctor Flo, Mark A. Adams, Balázs Adorján, David Aguadé, Marcos P. M. Aidar, Scott Allen, M. Susana Alvarado-Barrientos, Kristina J. Anderson-Teixeira, Luiza Maria Aparecido, M. Altaf Arain, Ismael Aranda, Heidi Asbjornsen, Robert Baxter, Eric Beamesderfer, Z. Carter Berry, Daniel Berveiller, Bethany Blakely, Johnny Boggs, Gil Bohrer, Paul V. Bolstad, Damien Bonal, Rosvel Bracho, Patricia Brito, Jason Brodeur, Fernando Casanoves, Jérôme Chave, Hui Chen, Cesar Cisneros, Kenneth Clark, Edoardo Cremonese, Hongzhong Dang, Jorge S. David, Teresa S. David, Nicolas Delpierre, Ankur R. Desai, Frederic C. Do, Michal Dohnal, Jean-Christophe Domec, Sebinasi Dzikiti, Colin Edgar, Rebekka Eichstaedt, Tarek S. El-Madany, Jan Elbers, Cleiton B. Eller, Eugénie S. Euskirchen, Brent Ewers, Patrick Fonti, Alicia Forner, David I. Forrester, Helber C. Freitas, Marta Galvagno, Omar Garcia-Tejera, Chandra Prasad Ghimire, Teresa E. Gimeno, John Grace, André Granier, Anne Griebel, Yan Guangyu, Mark B. Gush, Paul J. Hanson, Niles J. Hasselquist, Ingo Heinrich, Virginia Hernandez-Santana, Valentine Herrmann, Teemu Hölttä, Friso Holwerda, James Irvine, Supat Isarangkool Na Ayutthaya, Paul G. Jarvis, Hubert Jochheim, Carlos A. Joly, Julia Kaplick, Hyun Seok Kim, Leif Klemedtsson, Heather Kropp, Fredrik Lagergren, Patrick Lane, Petra Lang, Andrei Lapenas, Víctor Lechuga, Minsu Lee, Christoph Leuschner, Jean-Marc Limousin, Juan Carlos Linares, Maj-Lena Linderson, Anders Lindroth, Pilar Llorens, Álvaro López-Bernal, Michael M. Loranty, Dietmar Lüttschwager, Cate Macinnis-Ng, Isabelle Maréchaux, Timothy A. Martin, Ashley Matheny, Nate McDowell, Sean McMahon, Patrick Meir, Ilona Mészáros, Mirco Migliavacca, Patrick Mitchell, Meelis Mölder, Leonardo Montagnani, Georgianne W. Moore, Ryogo Nakada, Furong Niu, Rachael H. Nolan, Richard Norby, Kimberly Novick, Walter Oberhuber, Nikolaus Obojes, A. Christopher Oishi, Rafael S. Oliveira, Ram Oren, Jean-Marc Ourcival, Teemu Paljakka, Oscar Perez-Priego, Pablo L. Peri, Richard L. Peters, Sebastian Pfautsch, William T. Pockman, Yakir Preisler, Katherine Rascher, George Robinson, Humberto Rocha, Alain Rocheteau, Alexander Röll, Bruno H. P. Rosado, Lucy Rowland, Alexey V. Rubtsov, Santiago Sabaté, Yann Salmon, Roberto L. Salomón, Elisenda Sánchez-Costa, Karina V. R. Schäfer, Bernhard Schuldt, Alexandr Shashkin, Clément Stahl, Marko Stojanović, Juan Carlos Suárez, Ge Sun, Justyna Szatniewska, Fyodor Tatarinov, Miroslav Tesař, Frank M. Thomas, Pantana Tor-ngern, Josef Urban, Fernando Valladares, Christiaan van der Tol, Ilja van Meerveld, Andrej Varlagin, Holm Voigt, Jeffrey Warren, Christiane Werner, Willy Werner, Gerhard Wieser, Lisa Wingate, Stan Wullschleger, Koong Yi, Roman Zweifel, Kathy Steppe, Maurizio Mencuccini, and Jordi Martínez-Vilalta
Earth Syst. Sci. Data, 13, 2607–2649, https://doi.org/10.5194/essd-13-2607-2021, https://doi.org/10.5194/essd-13-2607-2021, 2021
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Transpiration is a key component of global water balance, but it is poorly constrained from available observations. We present SAPFLUXNET, the first global database of tree-level transpiration from sap flow measurements, containing 202 datasets and covering a wide range of ecological conditions. SAPFLUXNET and its accompanying R software package
sapfluxnetrwill facilitate new data syntheses on the ecological factors driving water use and drought responses of trees and forests.
Sam P. Jones, Aurore Kaisermann, Jérôme Ogée, Steven Wohl, Alexander W. Cheesman, Lucas A. Cernusak, and Lisa Wingate
SOIL, 7, 145–159, https://doi.org/10.5194/soil-7-145-2021, https://doi.org/10.5194/soil-7-145-2021, 2021
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Understanding how the rate of oxygen isotope exchange between water and CO2 varies in soils is key for using the oxygen isotope composition of atmospheric CO2 as a tracer of biosphere CO2 fluxes at large scales. Across 44 diverse soils the rate of this exchange responded to pH, nitrate and microbial biomass, which are hypothesised to alter activity of the enzyme carbonic anhydrase in soils. Using these three soil traits, it is now possible to predict how this isotopic exchange varies spatially.
Regina T. Hirl, Hans Schnyder, Ulrike Ostler, Rudi Schäufele, Inga Schleip, Sylvia H. Vetter, Karl Auerswald, Juan C. Baca Cabrera, Lisa Wingate, Margaret M. Barbour, and Jérôme Ogée
Hydrol. Earth Syst. Sci., 23, 2581–2600, https://doi.org/10.5194/hess-23-2581-2019, https://doi.org/10.5194/hess-23-2581-2019, 2019
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We evaluated the system-scale understanding of the propagation of the oxygen isotope signal (δ18O) of rain through soil and xylem to leaf water in a temperate drought-prone grassland. Biweekly δ18O observations of the water pools made during seven growing seasons were accurately reproduced by the 18O-enabled process-based model MuSICA. While water uptake occurred from shallow soil depths throughout dry and wet periods, leaf water 18O enrichment responded to both soil and atmospheric moisture.
Adrià Barbeta, Sam P. Jones, Laura Clavé, Lisa Wingate, Teresa E. Gimeno, Bastien Fréjaville, Steve Wohl, and Jérôme Ogée
Hydrol. Earth Syst. Sci., 23, 2129–2146, https://doi.org/10.5194/hess-23-2129-2019, https://doi.org/10.5194/hess-23-2129-2019, 2019
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Plant water sources of a beech riparian forest were monitored using stable isotopes. Isotopic fractionation during root water uptake is usually neglected but may be more common than previously accepted. Xylem water was always more depleted in δ2H than all sources considered, suggesting isotopic discrimination during water uptake or within plant tissues. Thus, the identification and quantification of tree water sources was affected. Still, oxygen isotopes were a good tracer of plant source water.
Adrià Barbeta, Sam P. Jones, Laura Clavé, Lisa Wingate, Teresa E. Gimeno, Bastien Fréjaville, Steve Wohl, and Jérôme Ogée
Hydrol. Earth Syst. Sci. Discuss., https://doi.org/10.5194/hess-2018-402, https://doi.org/10.5194/hess-2018-402, 2018
Revised manuscript not accepted
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Plant-water sources of a beech riparian forest were monitored using stable isotopes. Isotopic fractionation during root water uptake is usually neglected but may be more common than previously accepted. Xylem water was always more depleted in δ2H than all sources considered, suggesting isotopic discrimination during water uptake or within plant tissues. Thus, the identification and quantification of tree water sources was affected. Still, oxygen isotopes were a good tracer of plant source water.
Mary E. Whelan, Sinikka T. Lennartz, Teresa E. Gimeno, Richard Wehr, Georg Wohlfahrt, Yuting Wang, Linda M. J. Kooijmans, Timothy W. Hilton, Sauveur Belviso, Philippe Peylin, Róisín Commane, Wu Sun, Huilin Chen, Le Kuai, Ivan Mammarella, Kadmiel Maseyk, Max Berkelhammer, King-Fai Li, Dan Yakir, Andrew Zumkehr, Yoko Katayama, Jérôme Ogée, Felix M. Spielmann, Florian Kitz, Bharat Rastogi, Jürgen Kesselmeier, Julia Marshall, Kukka-Maaria Erkkilä, Lisa Wingate, Laura K. Meredith, Wei He, Rüdiger Bunk, Thomas Launois, Timo Vesala, Johan A. Schmidt, Cédric G. Fichot, Ulli Seibt, Scott Saleska, Eric S. Saltzman, Stephen A. Montzka, Joseph A. Berry, and J. Elliott Campbell
Biogeosciences, 15, 3625–3657, https://doi.org/10.5194/bg-15-3625-2018, https://doi.org/10.5194/bg-15-3625-2018, 2018
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Measurements of the trace gas carbonyl sulfide (OCS) are helpful in quantifying photosynthesis at previously unknowable temporal and spatial scales. While CO2 is both consumed and produced within ecosystems, OCS is mostly produced in the oceans or from specific industries, and destroyed in plant leaves in proportion to CO2. This review summarizes the advancements we have made in the understanding of OCS exchange and applications to vital ecosystem water and carbon cycle questions.
Joana Sauze, Sam P. Jones, Lisa Wingate, Steven Wohl, and Jérôme Ogée
Biogeosciences, 15, 597–612, https://doi.org/10.5194/bg-15-597-2018, https://doi.org/10.5194/bg-15-597-2018, 2018
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Previous studies have shown that differences in soil carbonic anhydrase (CA) activity are found in different biomes and seasons, but our understanding of the drivers responsible for those patterns is still limited. We artificially increased the soil CA concentration to test how soil pH affected the relationship between soil CA activity and concentration. We found that soil pH was the primary driver of soil CA activity.
Sam P. Jones, Jérôme Ogée, Joana Sauze, Steven Wohl, Noelia Saavedra, Noelia Fernández-Prado, Juliette Maire, Thomas Launois, Alexandre Bosc, and Lisa Wingate
Hydrol. Earth Syst. Sci., 21, 6363–6377, https://doi.org/10.5194/hess-21-6363-2017, https://doi.org/10.5194/hess-21-6363-2017, 2017
Yiying Chen, James Ryder, Vladislav Bastrikov, Matthew J. McGrath, Kim Naudts, Juliane Otto, Catherine Ottlé, Philippe Peylin, Jan Polcher, Aude Valade, Andrew Black, Jan A. Elbers, Eddy Moors, Thomas Foken, Eva van Gorsel, Vanessa Haverd, Bernard Heinesch, Frank Tiedemann, Alexander Knohl, Samuli Launiainen, Denis Loustau, Jérôme Ogée, Timo Vessala, and Sebastiaan Luyssaert
Geosci. Model Dev., 9, 2951–2972, https://doi.org/10.5194/gmd-9-2951-2016, https://doi.org/10.5194/gmd-9-2951-2016, 2016
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In this study, we compiled a set of within-canopy and above-canopy measurements of energy and water fluxes, and used these data to parametrize and validate the new multi-layer energy budget scheme for a range of forest types. An adequate parametrization approach has been presented for the global-scale land surface model (ORCHIDEE-CAN). Furthermore, model performance of the new multi-layer parametrization was compared against the existing single-layer scheme.
Jérôme Ogée, Joana Sauze, Jürgen Kesselmeier, Bernard Genty, Heidi Van Diest, Thomas Launois, and Lisa Wingate
Biogeosciences, 13, 2221–2240, https://doi.org/10.5194/bg-13-2221-2016, https://doi.org/10.5194/bg-13-2221-2016, 2016
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Estimates of photosynthesis and respiration at large scales are needed to improve our predictions of the global CO2 cycle. Carbonyl sulfide (OCS) has been proposed as a new tracer of photosynthesis, as it was shown that the uptake of OCS from leaves is nearly proportional to photosynthesis. But soils also exchange OCS with the atmosphere. Here we propose a mechanistic model of this exchange and show, using this new model, how we are able to explain several observed features of soil OCS fluxes.
L. Wingate, J. Ogée, E. Cremonese, G. Filippa, T. Mizunuma, M. Migliavacca, C. Moisy, M. Wilkinson, C. Moureaux, G. Wohlfahrt, A. Hammerle, L. Hörtnagl, C. Gimeno, A. Porcar-Castell, M. Galvagno, T. Nakaji, J. Morison, O. Kolle, A. Knohl, W. Kutsch, P. Kolari, E. Nikinmaa, A. Ibrom, B. Gielen, W. Eugster, M. Balzarolo, D. Papale, K. Klumpp, B. Köstner, T. Grünwald, R. Joffre, J.-M. Ourcival, M. Hellstrom, A. Lindroth, C. George, B. Longdoz, B. Genty, J. Levula, B. Heinesch, M. Sprintsin, D. Yakir, T. Manise, D. Guyon, H. Ahrends, A. Plaza-Aguilar, J. H. Guan, and J. Grace
Biogeosciences, 12, 5995–6015, https://doi.org/10.5194/bg-12-5995-2015, https://doi.org/10.5194/bg-12-5995-2015, 2015
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The timing of plant development stages and their response to climate and management were investigated using a network of digital cameras installed across different European ecosystems. Using the relative red, green and blue content of images we showed that the green signal could be used to estimate the length of the growing season in broadleaf forests. We also developed a model that predicted the seasonal variations of camera RGB signals and how they relate to leaf pigment content and area well.
Related subject area
Subject: Biosphere Interactions | Research Activity: Laboratory Studies | Altitude Range: Troposphere | Science Focus: Chemistry (chemical composition and reactions)
Laboratory measurements of stomatal NO2 deposition to native California trees and the role of forests in the NOx cycle
A mechanism for biogenic production and emission of MEK from MVK decoupled from isoprene biosynthesis
H2O2 modulates the energetic metabolism of the cloud microbiome
The contribution of soil biogenic NO and HONO emissions from a managed hyperarid ecosystem to the regional NOx emissions during growing season
Carbonyl sulfide exchange in soils for better estimates of ecosystem carbon uptake
Urban stress-induced biogenic VOC emissions and SOA-forming potentials in Beijing
Plant surface reactions: an opportunistic ozone defence mechanism impacting atmospheric chemistry
Erin R. Delaria, Bryan K. Place, Amy X. Liu, and Ronald C. Cohen
Atmos. Chem. Phys., 20, 14023–14041, https://doi.org/10.5194/acp-20-14023-2020, https://doi.org/10.5194/acp-20-14023-2020, 2020
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Observations of NO2 deposition to vegetation have been widely reported, but the magnitude and mechanism remain uncertain. We use laboratory measurements to study NO2 deposition to leaves of 10 native California tree species. We report important differences in the uptake rates between species and find that this process is primarily diffusion-regulated. We suggest that processes within leaves at a cellular level represent a negligible limitation to NO2 deposition at the canopy level.
Luca Cappellin, Francesco Loreto, Franco Biasioli, Paolo Pastore, and Karena McKinney
Atmos. Chem. Phys., 19, 3125–3135, https://doi.org/10.5194/acp-19-3125-2019, https://doi.org/10.5194/acp-19-3125-2019, 2019
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MEK is an important VOC in atmospheric chemistry and recently it has been shown that biogenic sources are globally as important as anthropogenic ones. We unveiled the mechanism by which within-plant transformation of MVK is a source of biogenic MEK. Such transformation is observed in red oak for both exogenous MVK, taken up from the atmosphere, and endogenous MVK generated within plant when it experiences stress (e.g. heat stress). The new mechanism is important for inclusion in models.
Nolwenn Wirgot, Virginie Vinatier, Laurent Deguillaume, Martine Sancelme, and Anne-Marie Delort
Atmos. Chem. Phys., 17, 14841–14851, https://doi.org/10.5194/acp-17-14841-2017, https://doi.org/10.5194/acp-17-14841-2017, 2017
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This article highlights the interactions between H2O2 and microorganisms within the cloud system. Experiments performed in microcosms with bacterial strains isolated from clouds showed that H2O2 strongly impacted the microbial energetic state. The ATP depletion measured in the presence of H2O2 was not due to the loss of cell viability. The strong correlation between ATP and H2O2 based on the analysis of 37 real cloud samples confirmed that H2O2 modulates the metabolism of cloud microorganisms.
Buhalqem Mamtimin, Franz X. Meixner, Thomas Behrendt, Moawad Badawy, and Thomas Wagner
Atmos. Chem. Phys., 16, 10175–10194, https://doi.org/10.5194/acp-16-10175-2016, https://doi.org/10.5194/acp-16-10175-2016, 2016
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In this study, we focused on the contributions of soil biogenic NO and HONO emissions from a managed hyperarid ecosystem to the regional NOx emissions during growing season. In particular, the second maximum in summer provides substantial evidence to hypothesize that those biogenic emissions from soils of managed drylands in the growing period may be much more important contributors to regional NOx budgets of dryland regions than previously thought.
Mary E. Whelan, Timothy W. Hilton, Joseph A. Berry, Max Berkelhammer, Ankur R. Desai, and J. Elliott Campbell
Atmos. Chem. Phys., 16, 3711–3726, https://doi.org/10.5194/acp-16-3711-2016, https://doi.org/10.5194/acp-16-3711-2016, 2016
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We constructed a model of carbonyl sulfide soil exchange sufficient for predicting outcomes in terrestrial ecosystems. Empirical observations combined with soil gas exchange theory reveal simultaneous abiotic production and biotic uptake mechanisms. Measurement of atmospheric carbonyl sulfide is an emerging tool to quantify photosynthesis at important temporal and spatial scales.
Andrea Ghirardo, Junfei Xie, Xunhua Zheng, Yuesi Wang, Rüdiger Grote, Katja Block, Jürgen Wildt, Thomas Mentel, Astrid Kiendler-Scharr, Mattias Hallquist, Klaus Butterbach-Bahl, and Jörg-Peter Schnitzler
Atmos. Chem. Phys., 16, 2901–2920, https://doi.org/10.5194/acp-16-2901-2016, https://doi.org/10.5194/acp-16-2901-2016, 2016
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Trees can impact urban air quality. Large emissions of plant volatiles are emitted in Beijing as a stress response to the urban polluted environment, but their impacts on secondary particulate matter remain relatively low compared to those originated from anthropogenic activities. The present study highlights the importance of including stress-induced compounds when studying plant volatile emissions.
W. Jud, L. Fischer, E. Canaval, G. Wohlfahrt, A. Tissier, and A. Hansel
Atmos. Chem. Phys., 16, 277–292, https://doi.org/10.5194/acp-16-277-2016, https://doi.org/10.5194/acp-16-277-2016, 2016
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“Breathing” ozone can have harmful effects on sensitive vegetation when sufficient ozone enters the plant leaves through the stomatal pores. Here we show that cis-abienol, a semi-volatile organic compound secreted by the leaf hairs (trichomes) of various tobacco varieties, protects the leaves from breathing ozone. Ozone is efficiently removed by chemical reactions with cis-abienol at the plant surface, forming oxygenated VOC (formaldehyde and methyl vinyl ketone) that are released into the air.
Cited articles
Barnes, I., Becker, K. H., and Patroescu, I.: The tropospheric oxidation of
dimethyl sulfide: A new source of carbonyl sulfide, Geophys. Res. Lett.,
21, 2389–2392, https://doi.org/10.1029/94GL02499, 1994.
Barnes, I., Becker, K. H., and Patroescu, I.: FTIR product study of the OH
initiated oxidation of dimethyl sulphide: Observation of carbonyl sulphide
and dimethyl sulphoxide, Atmos. Environ., 30, 1805–1814,
https://doi.org/10.1016/1352-2310(95)00389-4, 1996.
Berry, J., Wolf, A., Campbell, J. E., Baker, I., Blake, N., Blake, D.,
Denning, A. S., Kawa, S. R., Montzka, S. A., Seibt, U., Stimler, K., Yakir,
D., and Zhu, Z.: A coupled model of the global cycles of carbonyl sulfide and
CO2: A possible new window on the carbon cycle, J. Geophys.
Res.-Biogeo., 118, 842–852, https://doi.org/10.1002/jgrg.20068, 2013.
Billesbach, D. P., Berry, J. A., Seibt, U., Maseyk, K., Torn, M. S.,
Fischer, M. L., Abu-Naser, M., and Campbell, J. E.: Growing season eddy
covariance measurements of carbonyl sulfide and CO2 fluxes: COS and
CO2 relationships in Southern Great Plains winter wheat, Agr.
Forest Meteorol., 184, 48–55, https://doi.org/10.1016/j.agrformet.2013.06.007,
2014.
Boyd, R. A., Gandin, A., and Cousins, A. B.: Temperature Responses of C4
Photosynthesis: Biochemical Analysis of Rubisco, Phosphoenolpyruvate
Carboxylase, and Carbonic Anhydrase in Setaria viridis, Plant Physiol.,
169, 1850–1861, https://doi.org/10.1104/pp.15.00586, 2015.
Borchers, H. W.: pracma: Practical Numerical Math Functions, R package
version 2.0.7, available at:
https://cran.r-project.org/web/packages/pracma/index.html, last access:
22 June 2017.
Bremner, J. M. and Steele, C. G.: Role of Microorganisms in the Atmospheric
Sulfur Cycle, in: Advances in Microbial Ecology, Springer,
Boston, MA, 155–201, 1978.
Bunk, R., Behrendt, T., Yi, Z., Andreae, M. O., and Kesselmeier, J.: Exchange
of carbonyl sulfide (OCS) between soils and atmosphere under various
CO2 concentrations, J. Geophys. Res.-Biogeo., 122, 2016JG003678,
https://doi.org/10.1002/2016JG003678, 2017.
Burnell, J. N. and Hatch, M. D.: Low Bundle Sheath Carbonic Anhydrase Is
Apparently Essential for Effective C4 Pathway Operation, Plant Physiol.,
86, 1252–1256, https://doi.org/10.1104/pp.86.4.1252, 1988.
Brühl, C., Lelieveld, J., Crutzen, P. J., and Tost, H.: The role of
carbonyl sulphide as a source of stratospheric sulphate aerosol and its
impact on climate, Atmos. Chem. Phys., 12, 1239–1253,
https://doi.org/10.5194/acp-12-1239-2012, 2012.
Campbell, J. E., Berry, J. A., Seibt, U., Smith, S. J., Montzka, S. A.,
Launois, T., Belviso, S., Bopp, L., and Laine, M.: Large historical growth in
global terrestrial gross primary production, Nature, 544, 22030
https://doi.org/10.1038/nature22030, 2017.
Castro, M. S. and Galloway, J. N.: A comparison of sulfur-free and ambient
air enclosure techniques for measuring the exchange of reduced sulfur gases
between soils and the atmosphere, J. Geophys. Res., 96, 15427–15437,
https://doi.org/10.1029/91JD01399, 1991.
Conrad, R.: Compensation concentration as critical variable for regulating
the flux of trace gases between soil and atmosphere, Biogeochemistry, 27,
155–170, https://doi.org/10.1007/BF00000582, 1994.
Conrad, R. and Meuser, K.: Soils contain more than one activity consuming
carbonyl sulfide, Atmos. Environ., 34, 3635–3639,
https://doi.org/10.1016/S1352-2310(00)00136-9, 2000.
de Mello, W. Z. and Hines, M. E.: Application of static and dynamic
enclosures for determining dimethyl sulfide and carbonyl sulfide exchange in
Sphagnum peatlands: Implications for the magnitude and direction of flux, J.
Geophys. Res., 99, 14601–14607, https://doi.org/10.1029/94JD01025, 1994.
Elleuche, S. and Pöggeler, S.: Carbonic anhydrases in fungi,
Microbiology, 156, 23–29, https://doi.org/10.1099/mic.0.032581-0, 2010.
Fabre, N., Reiter, I. M., Becuwe-Linka, N., Genty, B., and Rumeau, D.:
Characterization and expression analysis of genes encoding α and
β carbonic anhydrases in Arabidopsis, Plant Cell Environ., 30,
617–629, https://doi.org/10.1111/j.1365-3040.2007.01651.x, 2007.
Fried, A., Klinger, L. F., and Erickson, D. J.: Atmospheric carbonyl sulfide
exchange in bog microcosms, Geophys. Res. Lett., 20, 129–132,
https://doi.org/10.1029/93GL00062, 1993.
Geng, C. and Mu, Y.: Carbonyl sulfide and dimethyl sulfide exchange between
lawn and the atmosphere, J. Geophys. Res., 109, D12302,
https://doi.org/10.1029/2003JD004492, 2004.
Gimeno, T. E., Ogée, J., Royles, J., Gibon, Y., West, J. B., Burlett,
R., Jones, S. P., Sauze, J., Wohl, S., Benard, C., Genty, B., and Wingate,
L.: Bryophyte gas-exchange dynamics along varying hydration status reveal a
significant carbonyl sulphide (COS) sink in the dark and COS source in the
light, New Phytol., 215, 965–976, https://doi.org/10.1111/nph.14584, 2017.
Haney, R. L. and Haney, E. B.: Simple and Rapid Laboratory Method for
Rewetting Dry Soil for Incubations, Commun. Soil Sci. Plan., 41, 1493–1501,
https://doi.org/10.1080/00103624.2010.482171, 2010.
Haritos, V. S. and Dojchinov, G.: Carbonic anhydrase metabolism is a key
factor in the toxicity of CO2 and COS but not CS2 toward the flour
beetle Tribolium castaneum [Coleoptera: Tenebrionidae], Comp. Biochem.
Physiol., 140, 139–147, https://doi.org/10.1016/j.cca.2005.01.012, 2005.
Hines, M. E. and Morrison, M. C.: Emissions of biogenic sulfur gases from
Alaskan tundra, J. Geophys. Res., 97, 16703–16707, https://doi.org/10.1029/90JD02576,
1992.
Jarvis, P. G., Rey, A., Petsikos, C., Wingate, L., Rayment, M. B., Pereira,
J. S., Banza, J., David, J., Miglietta, F., Borgetti, M., and Valentini, R.:
Drying and wetting of Mediterranean soils stimulates decomposition and carbon
dioxide emission: the “Birch Effect”, Tree Physiol., 27, 929–940, 2007.
Katayama, Y., Narahara, Y., Inoue, Y., Amano, F., Kanagawa, T., and Kuraishi,
H.: A thiocyanate hydrolase of Thiobacillus thioparus. A novel enzyme
catalyzing the formation of carbonyl sulfide from thiocyanate, J. Biol.
Chem., 267, 9170–9175, 1992.
Kato, H., Saito, M., Nagahata, Y., and Katayama, Y.: Degradation of ambient
carbonyl sulfide by Mycobacterium spp. in soil, Microbiology, 154, 249–255,
https://doi.org/10.1099/mic.0.2007/011213-0, 2008.
Kesselmeier, J., Teusch, N., and Kuhn, U.: Controlling variables for the
uptake of atmospheric carbonyl sulfide by soil, J. Geophys. Res., 104,
11577–11584, https://doi.org/10.1029/1999JD900090, 1999.
Kettle, A. J., Kuhn, U., von Hobe, M., Kesselmeier, J., and Andreae, M. O.:
Global budget of atmospheric carbonyl sulfide: Temporal and spatial
variations of the dominant sources and sinks, J. Geophys. Res., 107, 4658,
https://doi.org/10.1029/2002JD002187, 2002.
Kim, S.-J. and Katayama, Y.: Effect of growth conditions on thiocyanate
degradation and emission of carbonyl sulfide by Thiobacillus thioparus
THI115, Water Res., 34, 2887–2894, https://doi.org/10.1016/S0043-1354(00)00046-4, 2000.
Kitz, F., Gerdel, K., Hammerle, A., Laterza, T., Spielmann, F. M., and
Wohlfahrt, G.: In situ soil COS exchange of a temperate mountain grassland
under simulated drought, Oecologia, 183, 851–860,
https://doi.org/10.1007/s00442-016-3805-0, 2017.
Kooijmans, L. M. J., Uitslag, N. A. M., Zahniser, M. S., Nelson, D. D.,
Montzka, S. A., and Chen, H.: Continuous and high-precision atmospheric
concentration measurements of COS, CO2, CO and H2O using a
quantum cascade laser spectrometer (QCLS), Atmos. Meas. Tech., 9, 5293–5314,
https://doi.org/10.5194/amt-9-5293-2016, 2016.
Launois, T., Belviso, S., Bopp, L., Fichot, C. G., and Peylin, P.: A new
model for the global biogeochemical cycle of carbonyl sulfide – Part 1:
Assessment of direct marine emissions with an oceanic general circulation and
biogeochemistry model, Atmos. Chem. Phys., 15, 2295–2312,
https://doi.org/10.5194/acp-15-2295-2015, 2015.
Lehmann, S. and Conrad, R.: Characteristics of turnover of carbonyl sulfide
in four different soils, J. Atmos. Chem., 23, 193–207,
https://doi.org/10.1007/BF00048260, 1996.
Le Mer, J. and Roger, P.: Production, oxidation, emission and consumption of
methane by soils: A review, Eur. J. Soil Biol., 37, 25–50,
https://doi.org/10.1016/S1164-5563(01)01067-6, 2001.
Li, W., Yu, L., Yuan, D., Wu, Y., and Zeng, X.: A study of the activity and
ecological significance of carbonic anhydrase from soil and its microbes from
different karst ecosystems of Southwest China, Plant Soil, 272, 133–141,
https://doi.org/10.1007/s11104-004-4335-9, 2005.
Liu, J., Geng, C., Mu, Y., Zhang, Y., Xu, Z., and Wu, H.: Exchange of
carbonyl sulfide (COS) between the atmosphere and various soils in China,
Biogeosciences, 7, 753–762, https://doi.org/10.5194/bg-7-753-2010, 2010.
Maire, V., Alvarez, G., Colombet, J., Comby, A., Despinasse, R., Dubreucq,
E., Joly, M., Lehours, A.-C., Perrier, V., Shahzad, T., and Fontaine, S.: An
unknown oxidative metabolism substantially contributes to soil CO2
emissions, Biogeosciences, 10, 1155–1167,
https://doi.org/10.5194/bg-10-1155-2013, 2013.
Manina, G. and McKinney, J. D.: A Single-Cell Perspective on Non-Growing but
Metabolically Active (NGMA) Bacteria, in: Pathogenesis of Mycobacterium
tuberculosis and its Interaction with the Host Organism,Springer, Berlin,
Heidelberg, 135–161, 2013.
Masaki, Y., Ozawa, R., Kageyama, K., and Katayama, Y.: Degradation and
emission of carbonyl sulfide, an atmospheric trace gas, by fungi isolated
from forest soil, FEMS Microbiol. Lett., 363, fnw197,
https://doi.org/10.1093/femsle/fnw197, 2016.
Maseyk, K., Berry, J. A., Billesbach, D., Campbell, J. E., Torn, M. S.,
Zahniser, M., and Seibt, U.: Sources and sinks of carbonyl sulfide in an
agricultural field in the Southern Great Plains, P. Natl. Acad. Sci. USA,
111, 9064–9069, https://doi.org/10.1073/pnas.1319132111, 2014.
Melillo, J. M. and Steudler, P. A.: The effect of nitrogen fertilization on
the COS and CS2 emissions from temperature forest soils, J. Atmos.
Chem., 9, 411–417, https://doi.org/10.1007/BF00114753, 1989.
Melillo, J. M., McGuire, A. D., Kicklighter, D. W., Moore, B., Vorosmarty,
C. J., and Schloss, A. L.: Global climate change and terrestrial net primary
production, Nature, 363, p. 234, 1993.
Minami, K. and Fukushi, S.: Detection of carbonyl sulfide among gases
produced by the decomposition of cystine in paddy soils, Soil Sci. Plant
Nutr., 27, 105–109, https://doi.org/10.1080/00380768.1981.10431259, 1981a.
Minami, K. and Fukushi, S.: Volatilization of carbonyl sulfide from paddy
soils treated with sulfur-containing substances, Soil Sci. Plant Nutr., 27,
339–345, https://doi.org/10.1080/00380768.1981.10431288, 1981b.
Moldrup, P., Yoshikawa, S., Olesen, T., Komatsu, T., and Rolston, D. E.: Gas
Diffusitivity in Undisturbed Volcanic Ash Soils, Soil Sci. Soc. Am. J., 67,
41–51, https://doi.org/10.2136/sssaj2003.3200, 2003.
Montzka, S. A., Calvert, P., Hall, B. D., Elkins, J. W., Conway, T. J.,
Tans, P. P., and Sweeney, C.: On the global distribution, seasonality, and
budget of atmospheric carbonyl sulfide (COS) and some similarities to
CO2, J. Geophys. Res., 112, D09302, https://doi.org/10.1029/2006JD007665, 2007.
Moroney, J. V., Bartlett, S. G., and Samuelsson, G.: Carbonic anhydrases in
plants and algae, Plant Cell Environ., 24, 141–153,
https://doi.org/10.1111/j.1365-3040.2001.00669.x, 2001.
Ogawa, T., Noguchi, K., Saito, M., Nagahata, Y., Kato, H., Ohtaki, A.,
Nakayama, H., Dohmae, N., Matsushita, Y., Odaka, M., Yohda, M., Nyunoya, H.,
and Katayama, Y.: Carbonyl Sulfide Hydrolase from Thiobacillus thioparus
Strain THI115 Is One of the β-Carbonic Anhydrase Family Enzymes, J.
Am. Chem. Soc., 135, 3818–3825, https://doi.org/10.1021/ja307735e, 2013.
Ogée, J., Sauze, J., Kesselmeier, J., Genty, B., Van Diest, H., Launois,
T., and Wingate, L.: A new mechanistic framework to predict OCS fluxes from
soils, Biogeosciences, 13, 2221–2240,
https://doi.org/10.5194/bg-13-2221-2016, 2016.
Protoschill-Krebs, G. and Kesselmeier, J.: Enzymatic Pathways for the
Consumption of Carbonyl Sulphide (COS) by Higher Plants, Bot. Acta, 105,
206–212, https://doi.org/10.1111/j.1438-8677.1992.tb00288.x, 1992.
Protoschill-Krebs, G., Wilhelm, C., and Kesselmeier, J.: Consumption of
carbonyl sulphide (COS) by higher plant carbonic anhydrase (CA), Atmos.
Environ., 30, 3151–3156, https://doi.org/10.1016/1352-2310(96)00026-X, 1996.
Raubuch, M., Dyckmans, J., Joergensen, R. G., and Kreutzfeldt, M.: Relation
between respiration, ATP content, and Adenylate Energy Charge (AEC) after
incubation at different temperatures and after drying and rewetting, J. Plant
Nutr. Soil Sc., 165, 435–440,
https://doi.org/10.1002/1522-2624(200208)165:4<435::AID-JPLN435>3.0.CO;2-3,
2002.
R Core Team: R: A Language and Environment for Statistical Computing, R
Foundation for Statistical Computing, Vienna, Austria, available at:
https://www.r-project.org/, last access: 7 March 2017.
Rhodes, C., Riddel, S. A., West, J., Williams, B. P., and Hutchings, G. J.:
The low-temperature hydrolysis of carbonyl sulfide and carbon disulfide: a
review, Catal. Today, 59, 443–464, https://doi.org/10.1016/S0920-5861(00)00309-6, 2000.
Roszak, D. B. and Colwell, R. R.: Survival strategies of bacteria in the
natural environment, Microbiol. Rev., 51, 365–379, 1987.
Saito, M., Honna, T., Kanagawa, T., and Katayama, Y.: Microbial Degradation
of Carbonyl Sulfide in Soils, Microbes Environ., 17, 32–38,
https://doi.org/10.1264/jsme2.2002.32, 2002.
Sandoval-Soto, L., Stanimirov, M., von Hobe, M., Schmitt, V., Valdes, J.,
Wild, A., and Kesselmeier, J.: Global uptake of carbonyl sulfide (COS) by
terrestrial vegetation: Estimates corrected by deposition velocities
normalized to the uptake of carbon dioxide (CO2), Biogeosciences, 2,
125–132, https://doi.org/10.5194/bg-2-125-2005, 2005.
Sauze, J., Ogée, J., Maron, P.-A., Crouzet, O., Nowak, V., Wohl, S.,
Kaisermann, A., Jones, S. P., and Wingate, L.: The interaction of soil
phototrophs and fungi with pH and their impact on soil CO2,
CO18O and OCS exchange, Soil Biol. Biochem., 115, 371–382,
https://doi.org/10.1016/j.soilbio.2017.09.009, 2017.
Sauze, J., Jones, S. P., Wingate, L., Wohl, S., and Ogée, J.: The role of
soil pH on soil carbonic anhydrase activity, Biogeosciences, 15, 597–612,
https://doi.org/10.5194/bg-15-597-2018, 2018.
Sharma, V. K. and Graham, H. J. D.: Oxidation of amino acids, peptides and
proteins by ozone: a review, Ozone: Science and Engineering, 32, 81–90,
https://doi.org/10.1080/01919510903510507, 2010.
Smith, K. S. and Ferry, J. G.: Prokaryotic carbonic anhydrases, FEMS
Microbiol. Rev., 24, 335–366, https://doi.org/10.1111/j.1574-6976.2000.tb00546.x, 2000.
Stimler, K., Berry, J. A., and Yakir, D.: Effects of Carbonyl Sulfide and
Carbonic Anhydrase on Stomatal Conductance, Plant Physiol., 158, 524–530,
https://doi.org/10.1104/pp.111.185926, 2012.
Sun, W., Maseyk, K., Lett, C., and Seibt, U.: A soil diffusion–reaction model
for surface COS flux: COSSM v1, Geosci. Model Dev., 8, 3055–3070,
https://doi.org/10.5194/gmd-8-3055-2015, 2015.
Sun, W., Maseyk, K., Lett, C., and Seibt, U.: Litter dominates surface fluxes
of carbonyl sulfide in a Californian oak woodland, J. Geophys. Res.-Biogeo.,
121, 2015JG003149, https://doi.org/10.1002/2015JG003149, 2016.
Suntharalingam, P., Kettle, A. J., Montzka, S. M., and Jacob, D. J.: Global
3-D model analysis of the seasonal cycle of atmospheric carbonyl sulfide:
Implications for terrestrial vegetation uptake, Geophys. Res. Lett., 35,
L19801, https://doi.org/10.1029/2008GL034332, 2008.
Ueno, Y., Johnson, M. S., Danielache, S. O., Eskebjerg, C., Pandey, A., and
Yoshida, N.: Geological sulfur isotopes indicate elevated OCS in the Archean
atmosphere, solving faint young sun paradox, P. Natl. Acad. Sci. USA, 106,
14784–14789, https://doi.org/10.1073/pnas.0903518106, 2009.
Van Diest, H. and Kesselmeier, J.: Soil atmosphere exchange of carbonyl
sulfide (COS) regulated by diffusivity depending on water-filled pore space,
Biogeosciences, 5, 475–483, https://doi.org/10.5194/bg-5-475-2008, 2008.
Van Veldhoven, P. P. and Mannaerts, G. P.: Inorganic and organic phosphate
measurements in the nanomolar range, Anal. Biochem., 161, 45–48,
https://doi.org/10.1016/0003-2697(87)90649-X, 1987.
Wei, T. and Simko, V.: R package “corrplot”: Visualization of a
Correlation Matrix, available at: https://github.com/taiyun/corrplot,
last access: 17 October 2017.
Whelan, M. E. and Rhew, R. C.: Carbonyl sulfide produced by abiotic thermal
and photodegradation of soil organic matter from wheat field substrate, J.
Geophys. Res.-Biogeo., 120, 2014JG002661, https://doi.org/10.1002/2014JG002661, 2015.
Whelan, M. E. and Rhew, R. C.: Reduced sulfur trace gas exchange between a
seasonally dry grassland and the atmosphere, Biogeochemistry, 128, 267–280,
https://doi.org/10.1007/s10533-016-0207-7, 2016.
Whelan, M. E., Min, D.-H., and Rhew, R. C.: Salt marsh vegetation as a
carbonyl sulfide (COS) source to the atmosphere, Atmos. Environ., 73,
131–137, https://doi.org/10.1016/j.atmosenv.2013.02.048, 2013.
Whelan, M. E., Hilton, T. W., Berry, J. A., Berkelhammer, M., Desai, A. R.,
and Campbell, J. E.: Carbonyl sulfide exchange in soils for better estimates
of ecosystem carbon uptake, Atmos. Chem. Phys., 16, 3711–3726,
https://doi.org/10.5194/acp-16-3711-2016, 2016.
Whelan, M. E., Lennartz, S. T., Gimeno, T. E., Wehr, R., Wohlfahrt, G., Wang,
Y., Kooijmans, L. M. J., Hilton, T. W., Belviso, S., Peylin, P., Commane, R.,
Sun, W., Chen, H., Kuai, L., Mammarella, I., Maseyk, K., Berkelhammer, M.,
Li, K.-F., Yakir, D., Zumkehr, A., Katayama, Y., Ogée, J., Spielmann, F.
M., Kitz, F., Rastogi, B., Kesselmeier, J., Marshall, J., Erkkilä, K.-M.,
Wingate, L., Meredith, L. K., He, W., Bunk, R., Launois, T., Vesala, T.,
Schmidt, J. A., Fichot, C. G., Seibt, U., Saleska, S., Saltzman, E. S.,
Montzka, S. A., Berry, J. A., and Campbell, J. E.: Reviews and Syntheses:
Carbonyl Sulfide as a Multi-scale Tracer for Carbon and Water Cycles,
Biogeosciences Discuss., https://doi.org/10.5194/bg-2017-427, in review,
2017.
Wilhelm, E., Battino, R., and Wilcock, R. J.: Low-pressure solubility of
gases in liquid water, Chem. Rev., 77, 219–262, https://doi.org/10.1021/cr60306a003,
1977.
Wingate, L., Ogée, J., Cuntz, M., Genty, B., Reiter, I., Seibt, U.,
Yakir, D., Maseyk, K., Pendall, E., Barbour, M. M., Mortazavi, B., Peylin,
P., Miller, J., Mencuccini, M., Burlett, R., Shim, J. H., Hunt, J., and
Grace, J.: The influence of soil micro-organisms on the oxygen isotope signal
of atmospheric CO2, P. Natl. Acad. Sci. USA, 106, 22411–22415,
https://doi.org/10.1073/pnas.0905210106, 2009
Yi, Z. and Wang, X.: Carbonyl sulfide and dimethyl sulfide fluxes in an
urban lawn and adjacent bare soil in Guangzhou, China, J. Environ. Sci., 23,
784–789, https://doi.org/10.1016/S1001-0742(10)60478-0, 2011.
Yi, Z., Wang, X., Sheng, G., Zhang, D., Zhou, G., and Fu, J.: Soil uptake of
carbonyl sulfide in subtropical forests with different successional stages in
south China, J. Geophys. Res., 112, D08302, https://doi.org/10.1029/2006JD008048, 2007.
Zoppini, A. and Marxsen, J.: Importance of Extracellular Enzymes for
Biogeochemical Processes in Temporary River Sediments during Fluctuating
Dry–Wet Conditions, in: Soil Enzymology, Springer, Berlin, Heidelberg,
103–117, 2010.
Short summary
Soils simultaneously produce and consume the trace gas carbonyl sulfide (COS). To understand the role of these processes, we developed a method to estimate their contribution to the soil–atmosphere COS exchange. Exchange was principally driven by consumption, but the influence of production increased at higher temperatures, lower soil moisture contents and lower COS concentrations. Across the soils studied, we found a strong interaction between soil nitrogen and COS exchange.
Soils simultaneously produce and consume the trace gas carbonyl sulfide (COS). To understand the...
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