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Selden CR, LaBrie R, Ganley LC, Crocker DR, Peleg O, Perry DC, Reich HG, Sasaki M, Thibodeau PS, Isanta-Navarro J. Is our understanding of aquatic ecosystems sufficient to quantify ecologically driven climate feedbacks? GLOBAL CHANGE BIOLOGY 2024; 30:e17351. [PMID: 38837306 DOI: 10.1111/gcb.17351] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Grants] [Track Full Text] [Subscribe] [Scholar Register] [Received: 01/01/2024] [Revised: 05/02/2024] [Accepted: 05/13/2024] [Indexed: 06/07/2024]
Abstract
The Earth functions as an integrated system-its current habitability to complex life is an emergent property dependent on interactions among biological, chemical, and physical components. As global warming affects ecosystem structure and function, so too will the biosphere affect climate by altering atmospheric gas composition and planetary albedo. Constraining these ecosystem-climate feedbacks is essential to accurately predict future change and develop mitigation strategies; however, the interplay among ecosystem processes complicates the assessment of their impact. Here, we explore the state-of-knowledge on how ecological and biological processes (e.g., competition, trophic interactions, metabolism, and adaptation) affect the directionality and magnitude of feedbacks between ecosystems and climate, using illustrative examples from the aquatic sphere. We argue that, despite ample evidence for the likely significance of many, our present understanding of the combinatorial effects of ecosystem dynamics precludes the robust quantification of most ecologically driven climate feedbacks. Constraining these effects must be prioritized within the ecological sciences for only by studying the biosphere as both subject and arbiter of global climate can we develop a sufficiently holistic view of the Earth system to accurately predict Earth's future and unravel its past.
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Affiliation(s)
- Corday R Selden
- Department of Marine and Coastal Sciences, Rutgers University, New Brunswick, New Jersey, USA
- Department of Earth and Planetary Sciences, Rutgers University, Piscataway, New Jersey, USA
| | - Richard LaBrie
- Interdisciplinary Environmental Research Centre, TU Bergakademie Freiberg, Freiberg, Germany
| | - Laura C Ganley
- Anderson Cabot Center for Ocean Life, New England Aquarium, Boston, Massachusetts, USA
| | - Daniel R Crocker
- Department of Earth and Planetary Sciences, Harvard University, Cambridge, Massachusetts, USA
| | - Ohad Peleg
- School of Biological Sciences, Victoria University of Wellington, Wellington, New Zealand
| | - Danielle C Perry
- Department of Natural Resources Science, University of Rhode Island, Kingston, Rhode Island, USA
| | - Hannah G Reich
- Department of Biological Sciences, Biological Sciences, University of New Hampshire, Durham, New Hampshire, USA
| | - Matthew Sasaki
- Department of Marine Sciences, University of Connecticut, Mansfield, Connecticut, USA
| | - Patricia S Thibodeau
- School of Marine and Environmental Programs, University of New England, Biddeford, Maine, USA
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2
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Zhang J, Hou X, Zhang K, Deng Y, Xiao Q, Gao Y, Zhou X, Yan B. Deciphering fluorescent and molecular fingerprint of dissolved organic matter leached from microplastics in water. WATER RESEARCH 2024; 250:121047. [PMID: 38154343 DOI: 10.1016/j.watres.2023.121047] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 11/02/2023] [Revised: 12/12/2023] [Accepted: 12/19/2023] [Indexed: 12/30/2023]
Abstract
Despite extensive research into the presence and behavior of microplastics (MPs) in the environment, limited attention has been given to the investigation of the characteristics of dissolved organic matter (DOM) that leaches from MPs (MPs-DOM). Herein, two frequently encountered plastic particles in aquatic environments, specifically polyethylene terephthalate (PET)- and polyethylene (PE)-MPs, were subjected to leaching in the aquatic settings for seven days, both in the absence of light and under UV irradiation. Measurements of dissolved organic carbon (DOC) indicated that UV exposure enhanced the liberation of DOM from PET-MPs, while PE-MPs did not exhibit such leaching. After UV treatment for seven days, the DOM released from PET-MPs increased by 25 times, while that from PE-MPs remained almost unchanged. Then, the molecular diversity and the evolving formation of DOM originating from different MPs were comprehensively analyzed with fluorescence excitation-emission matrix (EEM) and Fourier transform ion cyclotron resonance mass spectrometry (FT-ICR-MS). Specifically, both PET- and PE-DOM exhibited three fluorescence signatures, with the predominant C1 (tryptophan-like) component showing a decline in PET-DOM and a rise in PE-DOM during aging. The FT-ICR-MS analysis unveiled that PET-DOM grew more recalcitrant under UV exposure, while PE-DOM became increasingly labile. In brief, UV irradiation influences MPs-DOM release and transformation differently, depending on the plastic composition. This highlights the significance of exploring MPs-DOM transformation in securing environmental safety.
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Affiliation(s)
- Jie Zhang
- School of Environmental Science and Engineering, Shandong University, Qingdao 266237, China
| | - Xianfeng Hou
- National-Regional Joint Engineering Research Center for Soil Pollution Control and Remediation in South China, Guangdong Key Laboratory of Integrated Agro-Environmental Pollution Control and Management, Institute of Eco-Environmental and Soil Sciences, Guangdong Academy of Sciences, Guangzhou 510650, China
| | - Kena Zhang
- School of Environmental Science and Engineering, Shandong University, Qingdao 266237, China
| | - Youwei Deng
- Institute of Environmental Research at the Greater Bay Area, Key Laboratory for Water Quality and Conservation of the Pearl River Delta, Ministry of Education, Guangzhou University, Guangzhou 510006, China
| | - Quanzhi Xiao
- Institute of Environmental Research at the Greater Bay Area, Key Laboratory for Water Quality and Conservation of the Pearl River Delta, Ministry of Education, Guangzhou University, Guangzhou 510006, China
| | - Yan Gao
- Institute of Environmental Research at the Greater Bay Area, Key Laboratory for Water Quality and Conservation of the Pearl River Delta, Ministry of Education, Guangzhou University, Guangzhou 510006, China
| | - Xiaoxia Zhou
- National-Regional Joint Engineering Research Center for Soil Pollution Control and Remediation in South China, Guangdong Key Laboratory of Integrated Agro-Environmental Pollution Control and Management, Institute of Eco-Environmental and Soil Sciences, Guangdong Academy of Sciences, Guangzhou 510650, China.
| | - Bing Yan
- School of Environmental Science and Engineering, Shandong University, Qingdao 266237, China; Institute of Environmental Research at the Greater Bay Area, Key Laboratory for Water Quality and Conservation of the Pearl River Delta, Ministry of Education, Guangzhou University, Guangzhou 510006, China
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3
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Spiegel CJ, Mladenov N, Wall CB, Hollman K, Tran CH, Symons CC, Shurin JB. Life after a fiery death: Fire and plant biomass loading affect dissolved organic matter in experimental ponds. GLOBAL CHANGE BIOLOGY 2024; 30:e17061. [PMID: 38273537 DOI: 10.1111/gcb.17061] [Citation(s) in RCA: 1] [Impact Index Per Article: 1.0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Grants] [Track Full Text] [Subscribe] [Scholar Register] [Received: 03/02/2023] [Revised: 10/19/2023] [Accepted: 11/02/2023] [Indexed: 01/27/2024]
Abstract
Drier and hotter conditions linked with anthropogenic climate change can increase wildfire frequency and severity, influencing terrestrial and aquatic carbon cycles at broad spatial and temporal scales. The impacts of wildfire are complex and dependent on several factors that may increase terrestrial deposition and the influx of dissolved organic matter (DOM) from plants into nearby aquatic systems, resulting in the darkening of water color. We tested the effects of plant biomass quantity and its interaction with fire (burned vs. unburned plant biomass) on dissolved organic carbon (DOC) concentration and degradation (biological vs. photochemical) and DOM composition in 400 L freshwater ponds using a gradient experimental design. DOC concentration increased nonlinearly with plant biomass loading in both treatments, with overall higher concentrations (>56 mg/L) in the unburned treatment shortly after plant addition. We also observed nonlinear trends in fluorescence and UV-visible absorbance spectroscopic indices as a function of fire treatment and plant biomass, such as greater humification and specific UV absorbance at 254 nm (a proxy for aromatic DOM) over time. DOM humification occurred gradually over time with less humification in the burned treatment compared to the unburned treatment. Both burned and unburned biomass released noncolored, low molecular weight carbon compounds that were rapidly consumed by microbes. DOC decomposition exhibited a unimodal relationship with plant biomass, with microbes contributing more to DOC loss than photodegradation at intermediate biomass levels (100-300 g). Our findings demonstrate that the quantity of plant biomass leads to nonlinear responses in the dynamics and composition of DOM in experimental ponds that are altered by fire, indicating how disturbances interactively affect DOM processing and its role in aquatic environments.
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Affiliation(s)
- Cody J Spiegel
- Department of Ecology, Behavior and Evolution, School of Biological Sciences, University of California, San Diego, California, USA
| | - Natalie Mladenov
- Department of Civil, Construction and Environmental Engineering, San Diego State University, San Diego, California, USA
| | - Christopher B Wall
- Department of Ecology, Behavior and Evolution, School of Biological Sciences, University of California, San Diego, California, USA
| | - Kelly Hollman
- Department of Civil, Construction and Environmental Engineering, San Diego State University, San Diego, California, USA
| | - Cindy H Tran
- Department of Ecology, Behavior and Evolution, School of Biological Sciences, University of California, San Diego, California, USA
| | - Celia C Symons
- Department of Ecology and Evolutionary Biology, University of California, Irvine, California, USA
| | - Jonathan B Shurin
- Department of Ecology, Behavior and Evolution, School of Biological Sciences, University of California, San Diego, California, USA
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4
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Plamper P, Lechtenfeld OJ, Herzsprung P, Groß A. A Temporal Graph Model to Predict Chemical Transformations in Complex Dissolved Organic Matter. ENVIRONMENTAL SCIENCE & TECHNOLOGY 2023; 57:18116-18126. [PMID: 37159837 PMCID: PMC10666529 DOI: 10.1021/acs.est.3c00351] [Citation(s) in RCA: 3] [Impact Index Per Article: 3.0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Grants] [Track Full Text] [Subscribe] [Scholar Register] [Received: 01/20/2023] [Revised: 04/25/2023] [Accepted: 04/25/2023] [Indexed: 05/11/2023]
Abstract
Dissolved organic matter (DOM) is a complex mixture of thousands of natural molecules that undergo constant transformation in the environment, such as sunlight induced photochemical reactions. Despite molecular level resolution from ultrahigh resolution mass spectrometry (UHRMS), trends of mass peak intensities are currently the only way to follow photochemically induced molecular changes in DOM. Many real-world relationships and temporal processes can be intuitively modeled using graph data structures (networks). Graphs enhance the potential and value of AI applications by adding context and interconnections allowing the uncovering of hidden or unknown relationships in data sets. We use a temporal graph model and link prediction to identify transformations of DOM molecules in a photo-oxidation experiment. Our link prediction algorithm simultaneously considers educt removal and product formation for molecules linked by predefined transformation units (oxidation, decarboxylation, etc.). The transformations are further weighted by the extent of intensity change and clustered on the graph structure to identify groups of similar reactivity. The temporal graph is capable of identifying relevant molecules subject to similar reactions and enabling to study their time course. Our approach overcomes previous data evaluation limitations for mechanistic studies of DOM and leverages the potential of temporal graphs to study DOM reactivity by UHRMS.
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Affiliation(s)
- Philipp Plamper
- Anhalt
University of Applied Sciences, Department Computer Science and Languages, Lohmannstraße 23, Köthen 06366, Germany
| | - Oliver J. Lechtenfeld
- Helmholtz
Centre for Environmental Research − UFZ, Department of Analytical Chemistry, Research Group
BioGeoOmics, Permoserstraße
15, Leipzig 04318, Germany
- ProVIS
- Centre for Chemical Microscopy, Helmholtz Centre for Environmental
Research - UFZ, Permoserstraße
15, Leipzig 04318, Germany
| | - Peter Herzsprung
- Helmholtz
Centre for Environmental Research − UFZ, Department of Lake Research, Brückstraße 3a, Magdeburg 39114, Germany
| | - Anika Groß
- Anhalt
University of Applied Sciences, Department Computer Science and Languages, Lohmannstraße 23, Köthen 06366, Germany
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5
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Li Z, Xu W, Kang L, Kuzyakov Y, Chen L, He M, Liu F, Zhang D, Zhou W, Liu X, Yang Y. Accelerated organic matter decomposition in thermokarst lakes upon carbon and phosphorus inputs. GLOBAL CHANGE BIOLOGY 2023; 29:6367-6382. [PMID: 37695465 DOI: 10.1111/gcb.16938] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [Grants] [Track Full Text] [Subscribe] [Scholar Register] [Received: 12/05/2022] [Revised: 08/23/2023] [Accepted: 08/27/2023] [Indexed: 09/12/2023]
Abstract
Mineralization of dissolved organic matter (DOM) in thermokarst lakes plays a non-negligible role in the permafrost carbon (C) cycle, but remains poorly understood due to its complex interactions with external C and nutrient inputs (i.e., aquatic priming and nutrient effects). Based on large-scale lake sampling and laboratory incubations, in combination with 13 C-stable-isotope labeling, optical spectroscopy, and high-throughput sequencing, we examined large-scale patterns and dominant drivers of priming and nutrient effects of DOM biodegradation across 30 thermokarst lakes along a 1100-km transect on the Tibetan Plateau. We observed that labile C and phosphorus (P) rather than nitrogen (N) inputs stimulated DOM biodegradation, with the priming and P effects being 172% and 451% over unamended control, respectively. We also detected significant interactive effects of labile C and nutrient supply on DOM biodegradation, with the combined labile C and nutrient additions inducing stronger microbial mineralization than C or nutrient treatment alone, illustrating that microbial activity in alpine thermokarst lakes is co-limited by both C and nutrients. We further found that the aquatic priming was mainly driven by DOM quality, with the priming intensity increasing with DOM recalcitrance, reflecting the limitation of external C as energy sources for microbial activity. Greater priming intensity was also associated with higher community-level ribosomal RNA gene operon (rrn) copy number and bacterial diversity as well as increased background soluble reactive P concentration. In contrast, the P effect decreased with DOM recalcitrance as well as with background soluble reactive P and ammonium concentrations, revealing the declining importance of P availability in mediating DOM biodegradation with enhanced C limitation but reduced nutrient limitation. Overall, the stimulation of external C and P inputs on DOM biodegradation in thermokarst lakes would amplify C-climate feedback in this alpine permafrost region.
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Affiliation(s)
- Ziliang Li
- State Key Laboratory of Vegetation and Environmental Change, Institute of Botany, Chinese Academy of Sciences, Beijing, China
- China National Botanical Garden, Beijing, China
- University of Chinese Academy of Sciences, Beijing, China
| | - Weijie Xu
- State Key Laboratory of Vegetation and Environmental Change, Institute of Botany, Chinese Academy of Sciences, Beijing, China
- China National Botanical Garden, Beijing, China
- University of Chinese Academy of Sciences, Beijing, China
| | - Luyao Kang
- State Key Laboratory of Vegetation and Environmental Change, Institute of Botany, Chinese Academy of Sciences, Beijing, China
- China National Botanical Garden, Beijing, China
- University of Chinese Academy of Sciences, Beijing, China
| | - Yakov Kuzyakov
- Department of Soil Science of Temperate Ecosystems, University of Göttingen, Göttingen, Germany
- Department of Agricultural Soil Science, University of Göttingen, Göttingen, Germany
- Peoples Friendship University of Russia (RUDN University), Moscow, Russia
| | - Leiyi Chen
- State Key Laboratory of Vegetation and Environmental Change, Institute of Botany, Chinese Academy of Sciences, Beijing, China
- China National Botanical Garden, Beijing, China
| | - Mei He
- State Key Laboratory of Vegetation and Environmental Change, Institute of Botany, Chinese Academy of Sciences, Beijing, China
- China National Botanical Garden, Beijing, China
| | - Futing Liu
- Key Laboratory of Forest Ecology and Environment of National Forestry and Grassland Administration, Ecology and Nature Conservation Institute, Chinese Academy of Forestry, Beijing, China
| | - Dianye Zhang
- State Key Laboratory of Vegetation and Environmental Change, Institute of Botany, Chinese Academy of Sciences, Beijing, China
- China National Botanical Garden, Beijing, China
| | - Wei Zhou
- State Key Laboratory of Vegetation and Environmental Change, Institute of Botany, Chinese Academy of Sciences, Beijing, China
- China National Botanical Garden, Beijing, China
- University of Chinese Academy of Sciences, Beijing, China
| | - Xuning Liu
- State Key Laboratory of Vegetation and Environmental Change, Institute of Botany, Chinese Academy of Sciences, Beijing, China
- China National Botanical Garden, Beijing, China
| | - Yuanhe Yang
- State Key Laboratory of Vegetation and Environmental Change, Institute of Botany, Chinese Academy of Sciences, Beijing, China
- China National Botanical Garden, Beijing, China
- University of Chinese Academy of Sciences, Beijing, China
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6
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Grasset C, Groeneveld M, Tranvik LJ, Robertson LP, Hawkes JA. Hydrophilic Species Are the Most Biodegradable Components of Freshwater Dissolved Organic Matter. ENVIRONMENTAL SCIENCE & TECHNOLOGY 2023; 57:13463-13472. [PMID: 37646447 PMCID: PMC10501193 DOI: 10.1021/acs.est.3c02175] [Citation(s) in RCA: 1] [Impact Index Per Article: 1.0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Grants] [Track Full Text] [Subscribe] [Scholar Register] [Received: 03/22/2023] [Revised: 07/29/2023] [Accepted: 07/31/2023] [Indexed: 09/01/2023]
Abstract
Aquatic dissolved organic matter (DOM) is a crucial component of the global carbon cycle, and the extent to which DOM escapes mineralization is important for the transport of organic carbon from the continents to the ocean. DOM persistence strongly depends on its molecular properties, but little is known about which specific properties cause the continuum in reactivity among different dissolved molecules. We investigated how DOM fractions, separated according to their hydrophobicity, differ in biodegradability across three different inland water systems. We found a strong negative relationship between hydrophobicity and biodegradability, consistent for the three systems. The most hydrophilic fraction was poorly recovered by solid-phase extraction (SPE) (3-28% DOC recovery) and was thus selectively missed by mass spectrometry analysis during SPE. The change in DOM composition after incubation was very low according to SPE-ESI (electrospray ionization)-mass spectrometry (14% change, while replicates had 11% change), revealing that this method is sub-optimal to assess DOM biodegradability, regardless of fraction hydrophobicity. Our results demonstrate that SPE-ESI mass spectrometry does not detect the most hydrophilic and most biodegradable species. Hence, they question our current understanding of the relationships between DOM biodegradability and its molecular composition, which is built on the use of this method.
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Affiliation(s)
- Charlotte Grasset
- Department
of Ecology and Genetics, Limnology, Uppsala
University, Uppsala 75236, Sweden
| | - Marloes Groeneveld
- Department
of Ecology and Genetics, Limnology, Uppsala
University, Uppsala 75236, Sweden
| | - Lars J. Tranvik
- Department
of Ecology and Genetics, Limnology, Uppsala
University, Uppsala 75236, Sweden
| | - Luke P. Robertson
- Department
of Pharmaceutical Biosciences, Uppsala University, Uppsala 75237, Sweden
| | - Jeffrey A. Hawkes
- Department
of Chemistry, BMC, Uppsala University, Uppsala 75237, Sweden
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7
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Kurek MR, Garcia-Tigreros F, Nichols NA, Druschel GK, Wickland KP, Dornblaser MM, Striegl RG, Niles SF, McKenna AM, Aukes PJK, Kyzivat ED, Wang C, Smith LC, Schiff SL, Butman D, Spencer RGM. High Voltage: The Molecular Properties of Redox-Active Dissolved Organic Matter in Northern High-Latitude Lakes. ENVIRONMENTAL SCIENCE & TECHNOLOGY 2023. [PMID: 37235632 DOI: 10.1021/acs.est.3c01782] [Citation(s) in RCA: 2] [Impact Index Per Article: 2.0] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 05/28/2023]
Abstract
Redox-active functional groups in dissolved organic matter (DOM) are crucial for microbial electron transfer and methane emissions. However, the extent of aquatic DOM redox properties across northern high-latitude lakes and their relationships with DOM composition have not been thoroughly described. We quantified electron donating capacity (EDC) and electron accepting capacity (EAC) in lake DOM from Canada to Alaska and assessed their relationships with parameters from absorbance, fluorescence, and ultrahigh resolution mass spectrometry (FT-ICR MS) analyses. EDC and EAC are strongly tied to aromaticity and negatively related to aliphaticity and protein-like content. Redox-active formulae spanned a range of aromaticity, including highly unsaturated phenolic formulae, and correlated negatively with many aliphatic N and S-containing formulae. This distribution illustrates the compositional diversity of redox-sensitive functional groups and their sensitivity to ecosystem properties such as local hydrology and residence time. Finally, we developed a reducing index (RI) to predict EDC in aquatic DOM from FT-ICR MS spectra and assessed its robustness using riverine DOM. As the hydrology of the northern high-latitudes continues to change, we expect differences in the quantity and partitioning of EDC and EAC within these lakes, which have implications for local water quality and methane emissions.
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Affiliation(s)
- Martin R Kurek
- Department of Earth, Ocean and Atmospheric Science, Florida State University, 1011 Academic Way, Tallahassee, Florida 32304, United States
- National High Magnetic Field Laboratory Geochemistry Group, 1800 E Paul Dirac Drive, Tallahassee, Florida 32310, United States
| | - Fenix Garcia-Tigreros
- School of Environmental and Forest Sciences, University of Washington, 3715 W Stevens Way NE, Seattle, Washington 98195, United States
| | - Natalie A Nichols
- Department of Earth Sciences, Indiana University-Purdue University Indianapolis, 723 W Michigan Street, Indianapolis, Indiana 46202, United States
| | - Gregory K Druschel
- Department of Earth Sciences, Indiana University-Purdue University Indianapolis, 723 W Michigan Street, Indianapolis, Indiana 46202, United States
| | - Kimberly P Wickland
- Geosciences and Environmental Change Science Center, United States Geological Survey, Denver Federal Center, Denver, Colorado 80225-0046, United States
| | - Mark M Dornblaser
- Water Resources Mission Area, United States Geological Survey, 3215 Marine Street, Boulder, Colorado 80303, United States
| | - Robert G Striegl
- Water Resources Mission Area, United States Geological Survey, 3215 Marine Street, Boulder, Colorado 80303, United States
| | - Sydney F Niles
- National High Magnetic Field Laboratory Ion Cyclotron Resonance Facility, 1800 E Paul Dirac Drive, Tallahassee, Florida 32310, United States
| | - Amy M McKenna
- National High Magnetic Field Laboratory Ion Cyclotron Resonance Facility, 1800 E Paul Dirac Drive, Tallahassee, Florida 32310, United States
- Department of Soil & Crop Sciences, Colorado State University, 307 University Avenue, Fort Collins, Colorado 80521, United States
| | - Pieter J K Aukes
- Department of Earth & Environmental Studies, University of Waterloo, 200 University Avenue W, Waterloo, Ontario N2L 3G1, Canada
- Geography & Environmental Studies, Wilfrid Laurier University, 75 University Avenue W, Waterloo, Ontario N2L 3C5, Canada
| | - Ethan D Kyzivat
- Department of Earth, Environmental & Planetary Sciences and Institute at Brown for Environment & Society, Brown University, 324 Brook Street, Providence, Rhode Island 02912, United States
| | - Chao Wang
- Department of Earth, Marine and Environmental Sciences, University of North Carolina, 104 South Road, CB#3315, Chapel Hill, North Carolina 27514, United States
| | - Laurence C Smith
- Department of Earth, Environmental & Planetary Sciences and Institute at Brown for Environment & Society, Brown University, 324 Brook Street, Providence, Rhode Island 02912, United States
| | - Sherry L Schiff
- Department of Earth & Environmental Studies, University of Waterloo, 200 University Avenue W, Waterloo, Ontario N2L 3G1, Canada
| | - David Butman
- School of Environmental and Forest Sciences, University of Washington, 3715 W Stevens Way NE, Seattle, Washington 98195, United States
- Department of Civil and Environmental Engineering, University of Washington, 201 More Hall, Seattle, Washington 98195-2700, United States
| | - Robert G M Spencer
- Department of Earth, Ocean and Atmospheric Science, Florida State University, 1011 Academic Way, Tallahassee, Florida 32304, United States
- National High Magnetic Field Laboratory Geochemistry Group, 1800 E Paul Dirac Drive, Tallahassee, Florida 32310, United States
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8
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Anderson KJ, Kominoski JS, Nocentini A, Hoffman S. Dissolved organic matter in peat and marl marshes varies with nutrient enrichment and restored hydrology. Restor Ecol 2023. [DOI: 10.1111/rec.13905] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 04/05/2023]
Affiliation(s)
- Kenneth J. Anderson
- Institute of Environment & Department of Biological Sciences Florida International University, Miami, FL 33199 U.S.A
| | - John S. Kominoski
- Institute of Environment & Department of Biological Sciences Florida International University, Miami, FL 33199 U.S.A
| | - Andrea Nocentini
- Institute of Environment & Department of Biological Sciences Florida International University, Miami, FL 33199 U.S.A
- South Florida Natural Resource Center, National Park Service, Homestead, FL 33034 U.S.A
| | - Sophia Hoffman
- Institute of Environment & Department of Biological Sciences Florida International University, Miami, FL 33199 U.S.A
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9
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Zhang S, Yin Y, Yang P, Yao C, Tian S, Lei P, Jiang T, Wang D. Using the end-member mixing model to evaluate biogeochemical reactivities of dissolved organic matter (DOM): autochthonous versus allochthonous origins. WATER RESEARCH 2023; 232:119644. [PMID: 36736245 DOI: 10.1016/j.watres.2023.119644] [Citation(s) in RCA: 8] [Impact Index Per Article: 8.0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 09/04/2022] [Revised: 01/02/2023] [Accepted: 01/16/2023] [Indexed: 06/18/2023]
Abstract
Dissolved organic matter (DOM) is an essential component of environmental systems. It usually originates from two end-members, including allochthonous and autochthonous sources. Previously, links have been established between DOM origins/sources and its biogeochemical reactivities. However, the influence of changes in DOM characteristics driven by end-member mixing on DOM biogeochemical reactivities has not been clarified. In this study, we investigated variations of DOM reactivities responding to the dynamics of DOM characteristics induced by different mixing ratios of two DOM end-members derived from humic acid (HA) and algae, respectively. Four biogeochemical reactivities of DOM were evaluated, including biodegradation, ·OH production, photodegradation, and redox capacity. Results showed that the variations of DOM characteristics due to the two end-members mixing significantly impact its biogeochemical reactivities. However, not all spectral parameters and reactivities followed the conservative mixing behavior. In contrast to reactivities of ·OH production and redox capacity, mixed samples showed apparent deviations from conservative linear relationships in biodegradation and photodegradation due to the interaction between the two end-members. Regarding the role of DOM properties influencing reactivity changes, peak A and M were recognized as the most stable parameters. However, peak C and SUVA254 were identified as the most vital contributors for explaining DOM reactivity variations. These findings suggest that a general model for describing the dynamic relationship between DOM source and reactivity cannot be proposed. Thus, the dynamics of DOM reactivity in diverse ecosystems cannot be estimated simply by the "plus or minus" of the reactivity from individual end-member. The effect of end-member mixing should be evaluated in a given reactivity instead of generalization. This study provides important insights for further understanding the dynamics of DOM's environmental role in different ecosystems influenced by variations of source inputs. In future, more field investigations are needed to further verify our findings in this study, especially in the scenario of end-member mixing.
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Affiliation(s)
- Siqi Zhang
- Interdisciplinary Research Centre for Agriculture Green Development in Yangtze River Basin, Department of Environmental Sciences and Engineering, College of Resources and Environment, Southwest University, Chongqing 400716, China
| | - Yongguang Yin
- Laboratory of Environmental Nanotechnology and Health Effect, Research Center for Eco-Environmental Sciences, Chinese Academy of Sciences, Beijing 100085, China; Institute of Environment and Health, Jianghan University, Wuhan 430056, China
| | - Peijie Yang
- Laboratory of Environmental Nanotechnology and Health Effect, Research Center for Eco-Environmental Sciences, Chinese Academy of Sciences, Beijing 100085, China
| | - Cong Yao
- Interdisciplinary Research Centre for Agriculture Green Development in Yangtze River Basin, Department of Environmental Sciences and Engineering, College of Resources and Environment, Southwest University, Chongqing 400716, China
| | - Shanyi Tian
- Interdisciplinary Research Centre for Agriculture Green Development in Yangtze River Basin, Department of Environmental Sciences and Engineering, College of Resources and Environment, Southwest University, Chongqing 400716, China
| | - Pei Lei
- School of Environment, Nanjing Normal University, Nanjing 210023, China
| | - Tao Jiang
- Interdisciplinary Research Centre for Agriculture Green Development in Yangtze River Basin, Department of Environmental Sciences and Engineering, College of Resources and Environment, Southwest University, Chongqing 400716, China; Institute of Environment and Health, Jianghan University, Wuhan 430056, China.
| | - Dingyong Wang
- Interdisciplinary Research Centre for Agriculture Green Development in Yangtze River Basin, Department of Environmental Sciences and Engineering, College of Resources and Environment, Southwest University, Chongqing 400716, China
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