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- Publisher Website: 10.1073/pnas.1819883116
- Scopus: eid_2-s2.0-85066781398
- PMID: 31097587
- WOS: WOS:000470136000042
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Article: Circumventing kinetics in biogeochemical modeling
Title | Circumventing kinetics in biogeochemical modeling |
---|---|
Authors | |
Keywords | geobiology reaction kinetics microbial system redox gradient marine anoxic region |
Issue Date | 2019 |
Publisher | National Academy of Sciences. The Journal's web site is located at http://www.pnas.org |
Citation | Proceedings of the National Academy of Sciences, 2019, v. 116 n. 23, p. 11329-11338 How to Cite? |
Abstract | Microbial metabolism drives biogeochemical fluxes in virtually every ecosystem. Modeling these fluxes is challenged by the incredible diversity of microorganisms, whose kinetic parameters are largely unknown. In poorly mixed systems, such as stagnant water columns or sediments, however, long-term bulk microbial metabolism may become limited by physical transport rates of substrates across space. Here we mathematically show that under these conditions, biogeochemical fluxes are largely predictable based on the system’s transport properties, chemical boundary conditions, and the stoichiometry of metabolic pathways, regardless of the precise kinetics of the resident microorganisms. We formalize these considerations into a predictive modeling framework and demonstrate its use for the Cariaco Basin subeuphotic zone, one of the largest anoxic marine basins worldwide. Using chemical concentration data solely from the upper boundary (depth 180 m) and lower boundary (depth 900 m), but without a priori knowledge of metabolite fluxes, chemical depth profiles, kinetic parameters, or microbial species composition, we predict the concentrations and vertical fluxes of biologically important substances, including oxygen, nitrate, hydrogen sulfide, and ammonium, across the entire considered depth range (180–900 m). Our predictions largely agree with concentration measurements over a period of 14 years (R2 = 0.78–0.92) and become particularly accurate during a period where the system was near biogeochemical steady state (years 2007–2009, R2 = 0.86–0.95). Our work enables geobiological predictions for a large class of ecosystems without knowledge of kinetic parameters or geochemical depth profiles. Conceptually, our work provides a possible explanation for the decoupling between microbial species composition and bulk metabolic function, observed in various ecosystems. |
Description | Bronze open access |
Persistent Identifier | http://hdl.handle.net/10722/290145 |
ISSN | 2023 Impact Factor: 9.4 2023 SCImago Journal Rankings: 3.737 |
PubMed Central ID | |
ISI Accession Number ID |
DC Field | Value | Language |
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dc.contributor.author | Louca, S | - |
dc.contributor.author | Scranton, MI | - |
dc.contributor.author | Taylor, GT | - |
dc.contributor.author | Astor, YM | - |
dc.contributor.author | Crowe, SA | - |
dc.contributor.author | Doebeli, M | - |
dc.date.accessioned | 2020-10-22T08:22:43Z | - |
dc.date.available | 2020-10-22T08:22:43Z | - |
dc.date.issued | 2019 | - |
dc.identifier.citation | Proceedings of the National Academy of Sciences, 2019, v. 116 n. 23, p. 11329-11338 | - |
dc.identifier.issn | 0027-8424 | - |
dc.identifier.uri | http://hdl.handle.net/10722/290145 | - |
dc.description | Bronze open access | - |
dc.description.abstract | Microbial metabolism drives biogeochemical fluxes in virtually every ecosystem. Modeling these fluxes is challenged by the incredible diversity of microorganisms, whose kinetic parameters are largely unknown. In poorly mixed systems, such as stagnant water columns or sediments, however, long-term bulk microbial metabolism may become limited by physical transport rates of substrates across space. Here we mathematically show that under these conditions, biogeochemical fluxes are largely predictable based on the system’s transport properties, chemical boundary conditions, and the stoichiometry of metabolic pathways, regardless of the precise kinetics of the resident microorganisms. We formalize these considerations into a predictive modeling framework and demonstrate its use for the Cariaco Basin subeuphotic zone, one of the largest anoxic marine basins worldwide. Using chemical concentration data solely from the upper boundary (depth 180 m) and lower boundary (depth 900 m), but without a priori knowledge of metabolite fluxes, chemical depth profiles, kinetic parameters, or microbial species composition, we predict the concentrations and vertical fluxes of biologically important substances, including oxygen, nitrate, hydrogen sulfide, and ammonium, across the entire considered depth range (180–900 m). Our predictions largely agree with concentration measurements over a period of 14 years (R2 = 0.78–0.92) and become particularly accurate during a period where the system was near biogeochemical steady state (years 2007–2009, R2 = 0.86–0.95). Our work enables geobiological predictions for a large class of ecosystems without knowledge of kinetic parameters or geochemical depth profiles. Conceptually, our work provides a possible explanation for the decoupling between microbial species composition and bulk metabolic function, observed in various ecosystems. | - |
dc.language | eng | - |
dc.publisher | National Academy of Sciences. The Journal's web site is located at http://www.pnas.org | - |
dc.relation.ispartof | Proceedings of the National Academy of Sciences | - |
dc.rights | Proceedings of the National Academy of Sciences. Copyright © National Academy of Sciences. | - |
dc.subject | geobiology | - |
dc.subject | reaction kinetics | - |
dc.subject | microbial system | - |
dc.subject | redox gradient | - |
dc.subject | marine anoxic region | - |
dc.title | Circumventing kinetics in biogeochemical modeling | - |
dc.type | Article | - |
dc.identifier.email | Crowe, SA: sacrowe@hku.hk | - |
dc.identifier.authority | Crowe, SA=rp02537 | - |
dc.description.nature | link_to_OA_fulltext | - |
dc.identifier.doi | 10.1073/pnas.1819883116 | - |
dc.identifier.pmid | 31097587 | - |
dc.identifier.pmcid | PMC6561284 | - |
dc.identifier.scopus | eid_2-s2.0-85066781398 | - |
dc.identifier.hkuros | 316140 | - |
dc.identifier.volume | 116 | - |
dc.identifier.issue | 23 | - |
dc.identifier.spage | 11329 | - |
dc.identifier.epage | 11338 | - |
dc.identifier.isi | WOS:000470136000042 | - |
dc.publisher.place | United States | - |
dc.identifier.issnl | 0027-8424 | - |