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Yan S, Li W, Sun T, Cai Y, Pan Y, Yu J. Effects of the Hydroxy-Regulated Li-Montmorillonite Atomic Interface Arrangement on Li Cycle of Marine Sedimentation and pH. LANGMUIR : THE ACS JOURNAL OF SURFACES AND COLLOIDS 2024; 40:7375-7383. [PMID: 38497723 DOI: 10.1021/acs.langmuir.3c03619] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 03/19/2024]
Abstract
The reaction of ubiquitous clay is related to the global cycle of the key metals, but the relationship between the Li occurrence interface and the sedimentation in the Li cycle remains unclear. We investigated the atomic interface arrangement of Li-montmorillonite (Li-Mt) during low-temperature water-rock reactions and Li migration. The results show that, in Cl-rich systems, deprotonation and exposure of Na adsorption sites cause Li enrichment and O pairing, which lead to the weakening of the shielding effect of Mt on anions and the formation of a Mt-Li-Cl atomically interfacial arrangement. Only up to 20.3% of the Li is contained in the atomic interface of Li-Mt. In F-rich system, the dehydroxylation of F paired with Al in octahedral sites causes Li accumulation via local crystallization of LiF, and co-complexation of F and Li forms a Mt(Al)-F-Li atomic interface, in which up to 46.8% of the Li is enriched by the Mt. The participation of F and Cl in the complexation intensifies lattice collapse of the Li-Mt edge. The sedimentation velocity decreases with the smaller particle size affected by the Li loading. Lithium leached from igneous rocks serves as the marine Li source, which contributes up to 99.8% and 99.5% of the Li in Cl- and F-rich systems, respectively. The response of Mt(OH) to Li migration with a time accumulating effect may make an important regulatory of oceanic pH by either acidification or alkalization.
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Affiliation(s)
- Song Yan
- State Key Laboratory of Mineral Deposit Research, School of Earth and Engineering, Nanjing University, Nanjing 210023, China
| | - Wei Li
- State Key Laboratory of Mineral Deposit Research, School of Earth and Engineering, Nanjing University, Nanjing 210023, China
| | - Tao Sun
- State Key Laboratory of Mineral Deposit Research, School of Earth and Engineering, Nanjing University, Nanjing 210023, China
| | - Yuanfeng Cai
- State Key Laboratory of Mineral Deposit Research, School of Earth and Engineering, Nanjing University, Nanjing 210023, China
| | - Yuguan Pan
- State Key Laboratory of Mineral Deposit Research, School of Earth and Engineering, Nanjing University, Nanjing 210023, China
| | - Jinhai Yu
- State Key Laboratory of Mineral Deposit Research, School of Earth and Engineering, Nanjing University, Nanjing 210023, China
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Guo C, Guo L, Bass S, Manning AJ, Jin Z, Zhou Y. On the role of organic matter composition in fresh-water kaolinite flocculation. JOURNAL OF ENVIRONMENTAL MANAGEMENT 2023; 345:118576. [PMID: 37421719 DOI: 10.1016/j.jenvman.2023.118576] [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: 03/28/2023] [Revised: 06/18/2023] [Accepted: 07/02/2023] [Indexed: 07/10/2023]
Abstract
Organic matter has long been understood to affect fine sediment flocculation, yet the specific effects of different types of organic matter remain only partially understood. To address this knowledge gap, laboratory tank experiments were conducted in fresh water to investigate the sensitivity of kaolinite flocculation to varying organic matter species and contents. Three species of organic matter (xanthan gum, guar gum and humic acid) were investigated at varying concentrations. Results revealed a significant enhancement in kaolinite flocculation when organic polymers (xanthan gum and guar gum) were introduced. In contrast, the addition of humic acid had minimal influence on aggregation and floc structure. Notably, the nonionic polymer guar gum demonstrated greater efficacy in promoting the development of floc size compared to the anionic polymer, xanthan gum. We observed non-linear trends in the evolution of mean floc size (Dm) and boundary fractal dimension (Np) with increasing ratios of organic polymer concentration to kaolinite concentration. Initially, increasing polymer content facilitated the formation of larger and more fractal flocs. However, beyond a certain threshold, further increases in polymer content hindered flocculation and even led to the break-up of macro-flocs, resulting in the formation of more spherical and compact flocs. We further quantified the co-relationships between floc Np and Dm and found that larger Np values corresponded to larger Dm. These findings highlight the significant impact of organic matter species and concentrations on floc size, shape and structure, and shed light on the complex dynamics of fine sediment and associated nutrients and contaminants in fluvial systems.
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Affiliation(s)
- Chao Guo
- Changjiang River Scientific Research Institute of Changjiang Water Resources Commission, Wuhan, 430010, Hubei, China.
| | - Leicheng Guo
- State Key Laboratory of Estuarine and Coastal Research, East China Normal University, Shanghai, 200241, China
| | - Sarah Bass
- School of Biological and Marine Sciences, University of Plymouth, Drake Circus, Plymouth, Devon, PL4 8AA, United Kingdom
| | - Andrew J Manning
- School of Biological and Marine Sciences, University of Plymouth, Drake Circus, Plymouth, Devon, PL4 8AA, United Kingdom; HR Wallingford, Howbery Park, Wallingford, OX10 8BA, United Kingdom; Department of Civil and Environmental Engineering, Center for Applied Coastal Research, University of Delaware, Newark, 19716, DE, United States
| | - Zhongwu Jin
- Changjiang River Scientific Research Institute of Changjiang Water Resources Commission, Wuhan, 430010, Hubei, China
| | - Yinjun Zhou
- Changjiang River Scientific Research Institute of Changjiang Water Resources Commission, Wuhan, 430010, Hubei, China
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Birch SPD, Parker G, Corlies P, Soderblom JM, Miller JW, Palermo RV, Lora JM, Ashton AD, Hayes AG, Perron JT. Reconstructing river flows remotely on Earth, Titan, and Mars. Proc Natl Acad Sci U S A 2023; 120:e2206837120. [PMID: 37428909 PMCID: PMC10629578 DOI: 10.1073/pnas.2206837120] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 05/12/2022] [Accepted: 06/05/2023] [Indexed: 07/12/2023] Open
Abstract
Alluvial rivers are conveyor belts of fluid and sediment that provide a record of upstream climate and erosion on Earth, Titan, and Mars. However, many of Earth's rivers remain unsurveyed, Titan's rivers are not well resolved by current spacecraft data, and Mars' rivers are no longer active, hindering reconstructions of planetary surface conditions. To overcome these problems, we use dimensionless hydraulic geometry relations-scaling laws that relate river channel dimensions to flow and sediment transport rates-to calculate in-channel conditions using only remote sensing measurements of channel width and slope. On Earth, this offers a way to predict flow and sediment flux in rivers that lack field measurements and shows that the distinct dynamics of bedload-dominated, suspended load-dominated, and bedrock rivers give rise to distinct channel characteristics. On Mars, this approach not only predicts grain sizes at Gale Crater and Jezero Crater that overlap with those measured by the Curiosity and Perseverance rovers, it enables reconstructions of past flow conditions that are consistent with proposed long-lived hydrologic activity at both craters. On Titan, our predicted sediment fluxes to the coast of Ontario Lacus could build the lake's river delta in as little as ~1,000 y, and our scaling relationships suggest that Titan's rivers may be wider, slope more gently, and transport sediment at lower flows than rivers on Earth or Mars. Our approach provides a template for predicting channel properties remotely for alluvial rivers across Earth, along with interpreting spacecraft observations of rivers on Titan and Mars.
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Affiliation(s)
- Samuel P. D. Birch
- Department of Earth, Atmospheric and Planetary Sciences, Massachusetts Institute of Technology, Cambridge, MA02139
| | - Gary Parker
- Department of Geology, University of Illinois at Urbana-Champaign, Urbana, IL61820
- Department of Civil and Environmental Engineering, University of Illinois at Urbana-Champaign, Urbana, IL61820
| | - Paul Corlies
- Department of Earth, Atmospheric and Planetary Sciences, Massachusetts Institute of Technology, Cambridge, MA02139
| | - Jason M. Soderblom
- Department of Earth, Atmospheric and Planetary Sciences, Massachusetts Institute of Technology, Cambridge, MA02139
| | - Julia W. Miller
- Department of Earth, Planetary, and Space Sciences, University of California, Los Angeles, CA90095
| | - Rose V. Palermo
- Massachusetts Institute of Technology-Woods Hole Oceanographic Institute Joint Program in Oceanography/Applied Ocean Science and Engineering, Cambridge and Woods Hole, MA02139
| | - Juan M. Lora
- Department of Earth and Planetary Sciences, Yale University, New Haven, CT06520
| | - Andrew D. Ashton
- Department of Geology and Geophysics, Woods Hole Oceanographic Institution, Woods Hole, MA02543
| | | | - J. Taylor Perron
- Department of Earth, Atmospheric and Planetary Sciences, Massachusetts Institute of Technology, Cambridge, MA02139
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Mitchell RL, Kenrick P, Pressel S, Duckett J, Strullu-Derrien C, Davies N, McMahon WJ, Summerfield R. Terrestrial surface stabilisation by modern analogues of the earliest land plants: A multi-dimensional imaging study. GEOBIOLOGY 2023; 21:454-473. [PMID: 36779552 DOI: 10.1111/gbi.12546] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [Grants] [Track Full Text] [Subscribe] [Scholar Register] [Received: 09/13/2022] [Revised: 12/23/2022] [Accepted: 01/05/2023] [Indexed: 06/13/2023]
Abstract
The evolution of the first plant-based terrestrial ecosystems in the early Palaeozoic had a profound effect on the development of soils, the architecture of sedimentary systems, and shifts in global biogeochemical cycles. In part, this was due to the evolution of complex below-ground (root-like) anchorage systems in plants, which expanded and promoted plant-mineral interactions, weathering, and resulting surface sediment stabilisation. However, little is understood about how these micro-scale processes occurred, because of a lack of in situ plant fossils in sedimentary rocks/palaeosols that exhibit these interactions. Some modern plants (e.g., liverworts, mosses, lycophytes) share key features with the earliest land plants; these include uni- or multicellular rhizoid-like anchorage systems or simple roots, and the ability to develop below-ground networks through prostrate axes, and intimate associations with fungi, making them suitable analogues. Here, we investigated cryptogamic ground covers in Iceland and New Zealand to better understand these interactions, and how they initiate the sediment stabilisation process. We employed multi-dimensional and multi-scale imaging, including scanning electron microscopy (SEM) and X-ray Computed Tomography (μCT) of non-vascular liverworts (Haplomitriopsida and complex thalloids) and mosses, with additional imaging of vascular lycopods. We find that plants interact with their substrate in multiple ways, including: (1) through the development of extensive surface coverings as mats; (2) entrapment of sediment grains within and between networks of rhizoids; (3) grain entwining and adherence by rhizoids, through mucilage secretions, biofilm-like envelopment of thalli on surface grains; and (4) through grain entrapment within upright 'leafy' structures. Significantly, μCT imaging allows us to ascertain that rhizoids are the main method for entrapment and stabilisation of soil grains in the thalloid liverworts. This information provides us with details of how the earliest land plants may have significantly influenced early Palaeozoic sedimentary system architectures, promoted in situ weathering and proto-soil development, and how these interactions diversified over time with the evolution of new plant organ systems. Further, this study highlights the importance of cryptogamic organisms in the early stages of sediment stabilisation and soil formation today.
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Affiliation(s)
- Ria L Mitchell
- Science Group, The Natural History Museum, London, UK
- Sheffield Tomography Centre (STC), Kroto Research Institute, The University of Sheffield, Sheffield, UK
| | - Paul Kenrick
- Science Group, The Natural History Museum, London, UK
| | | | - Jeff Duckett
- Science Group, The Natural History Museum, London, UK
| | - Christine Strullu-Derrien
- Science Group, The Natural History Museum, London, UK
- Institut de Systématique, Evolution, Biodiversité (ISYEB), UMR7205, Muséum National d'Histoire naturelle, Sorbonne Université, CNRS, Paris, France
| | - Neil Davies
- Department of Earth Sciences, University of Cambridge, Cambridge, UK
| | - William J McMahon
- Department of Earth Sciences, University of Cambridge, Cambridge, UK
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Shen X, Huo H, Zhang Y, Zhu Y, Fettweis M, Bi Q, Lee BJ, Maa JPY, Chen Q. Effects of organic matter on the aggregation of anthropogenic microplastic particles in turbulent environments. WATER RESEARCH 2023; 232:119706. [PMID: 36773352 DOI: 10.1016/j.watres.2023.119706] [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: 09/03/2022] [Revised: 01/06/2023] [Accepted: 02/02/2023] [Indexed: 06/18/2023]
Abstract
Biofilm-coated microplastics are omnipresent in aquatic environments, carrying different organic matter (OM) that in turn influences the flocculation and settling of microplastic aggregates. In this study, the effects of chitosan, guar gum, humic acid, and xanthan gum on the flocculation of anthropogenic microplastics are examined under controlled shear through the mixing chamber experiments. The results show that all of the selected OMs have positive effects on biofilm culturing and thus enhance the growth of microplastic flocs, with more evident promoting effects for cationic and neutral OMs (i.e., chitosan and guar gum) than anionic OMs (i.e., humic acid and xanthan). No critical shear rate is observed in the size vs. shear relationship based on our measurements. In addition, the quadrature-based two-class population balance model is employed to track the development of bimodal floc size distributions (FSDs) composed of small and large microplastic flocs. The model predictions show reasonable agreement with the observed FSDs. The largest error of settling flux from the two-class model is 7.8% in contrast with the reference value measured by the camera-based FSDs with 30 bins. This study highlights the role of different OMs on microplastic flocculation and indicates that a two-class model may be sufficient to describe microplastic transport processes in estuaries.
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Affiliation(s)
- Xiaoteng Shen
- State Key Laboratory of Hydrology-Water Resources and Hydraulic Engineering, Hohai University, Nanjing 210024, China; Yangtze Institute for Conservation and Development, Hohai University, Nanjing 210024, China
| | - Hong Huo
- State Key Laboratory of Hydrology-Water Resources and Hydraulic Engineering, Hohai University, Nanjing 210024, China
| | - Ying Zhang
- College of Water Conservancy and Hydropower Engineering, Hohai University, Najing 210024, China; Jiangxi Water Resources Institute, Nanchang 330013, China
| | - Yuliang Zhu
- State Key Laboratory of Hydrology-Water Resources and Hydraulic Engineering, Hohai University, Nanjing 210024, China; Yangtze Institute for Conservation and Development, Hohai University, Nanjing 210024, China.
| | - Michael Fettweis
- Operational Directorate Natural Environment, Royal Belgian Institute of Natural Sciences, Rue Vautier 29, 1000 Brussels, Belgium
| | - Qilong Bi
- Hydraulics Laboratory, Department of Civil Engineering, KU Leuven, Kasteelpark Arenberg 40, B-3001 Leuven, Belgium; Flanders Hydraulics Research, Antwerp, Belgium
| | - Byung Joon Lee
- School of Construction and Environmental Engineering, Kyungpook National University, 2559 Gyeongsang-daero, Sangju, Gyeongbuk 742-711, South Korea
| | - Jerome P-Y Maa
- Virginia Institute of Marine Science, College of William & Mary, Glocuester Point VA23062, United States
| | - Qiqing Chen
- State Key Laboratory of Estuarine and Coastal Research, East China Normal University, Shanghai 200241, China
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Boyce CK, Ibarra DE, Nelsen MP, D'Antonio MP. Nitrogen-based symbioses, phosphorus availability, and accounting for a modern world more productive than the Paleozoic. GEOBIOLOGY 2023; 21:86-101. [PMID: 35949039 DOI: 10.1111/gbi.12519] [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: 04/05/2022] [Revised: 07/07/2022] [Accepted: 07/22/2022] [Indexed: 06/15/2023]
Abstract
Evolution of high-productivity angiosperms has been regarded as a driver of Mesozoic ecosystem restructuring. However, terrestrial productivity is limited by availability of rock-derived nutrients such as phosphorus for which permanent increases in weathering would violate mass balance requirements of the long-term carbon cycle. The potential reality of productivity increases sustained since the Mesozoic is supported here with documentation of a dramatic increase in the evolution of nitrogen-fixing or nitrogen-scavenging symbioses, including more than 100 lineages of ectomycorrhizal and lichen-forming fungi and plants with specialized microbial associations. Given this evidence of broadly increased nitrogen availability, we explore via carbon cycle modeling how enhanced phosphorus availability might be sustained without violating mass balance requirements. Volcanism is the dominant carbon input, dictating peaks in weathering outputs up to twice modern values. However, times of weathering rate suppression may be more important for setting system behavior, and the late Paleozoic was the only extended period over which rates are expected to have remained lower than modern. Modeling results are consistent with terrestrial organic matter deposition that accompanied Paleozoic vascular plant evolution having suppressed weathering fluxes by providing an alternative sink of atmospheric CO2 . Suppression would have then been progressively lifted as the crustal reservoir's holding capacity for terrestrial organic matter saturated back toward steady state with deposition of new organic matter balanced by erosion of older organic deposits. Although not an absolute increase, weathering fluxes returning to early Paleozoic conditions would represent a novel regime for the complex land biota that evolved in the interim. Volcanism-based peaks in Mesozoic weathering far surpass the modern rates that sustain a complex diversity of nitrogen-based symbioses; only in the late Paleozoic might these ecologies have been suppressed by significantly lower rates. Thus, angiosperms are posited to be another effect rather than proximal cause of Mesozoic upheaval.
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Affiliation(s)
- C Kevin Boyce
- Department of Geological Sciences, Stanford University, Stanford, California, USA
| | - Daniel E Ibarra
- Department of Geological Sciences, Stanford University, Stanford, California, USA
- Department of Earth and Planetary Science, University of California, Berkeley, California, USA
- Institute at Brown for Environment and Society and the Department of Earth, Environmental and Planetary Science, Brown University, Providence, Rhode Island, USA
| | - Matthew P Nelsen
- Negaunee Integrative Research Center, The Field Museum, Chicago, Illinois, USA
| | - Michael P D'Antonio
- Department of Geological Sciences, Stanford University, Stanford, California, USA
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Buatois LA, Davies NS, Gibling MR, Krapovickas V, Labandeira CC, MacNaughton RB, Mángano MG, Minter NJ, Shillito AP. The Invasion of the Land in Deep Time: Integrating Paleozoic Records of Paleobiology, Ichnology, Sedimentology, and Geomorphology. Integr Comp Biol 2022; 62:297-331. [PMID: 35640908 DOI: 10.1093/icb/icac059] [Citation(s) in RCA: 3] [Impact Index Per Article: 1.5] [Reference Citation Analysis] [Abstract] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 01/31/2022] [Revised: 04/19/2022] [Accepted: 05/24/2022] [Indexed: 11/13/2022] Open
Abstract
The invasion of the land was a complex, protracted process, punctuated by mass extinctions, that involved multiple routes from marine environments. We integrate paleobiology, ichnology, sedimentology, and geomorphology to reconstruct Paleozoic terrestrialization. Cambrian landscapes were dominated by laterally mobile rivers with unstable banks in the absence of significant vegetation. Temporary incursions by arthropods and worm-like organisms into coastal environments apparently did not result in establishment of continental communities. Contemporaneous lacustrine faunas may have been inhibited by limited nutrient delivery and high sediment loads. The Ordovician appearance of early land plants triggered a shift in the primary locus of the global clay mineral factory, increasing the amount of mudrock on the continents. The Silurian-Devonian rise of vascular land plants, including the first forests and extensive root systems, was instrumental in further retaining fine sediment on alluvial plains. These innovations led to increased architectural complexity of braided and meandering rivers. Landscape changes were synchronous with establishment of freshwater and terrestrial arthropod faunas in overbank areas, abandoned fluvial channels, lake margins, ephemeral lakes, and inland deserts. Silurian-Devonian lakes experienced improved nutrient availability, due to increased phosphate weathering and terrestrial humic matter. All these changes favoured frequent invasions to permament establishment of jawless and jawed fishes in freshwater habitats and the subsequent tetrapod colonization of the land. The Carboniferous saw rapid diversification of tetrapods, mostly linked to aquatic reproduction, and land plants, including gymnosperms. Deeper root systems promoted further riverbank stabilization, contributing to the rise of anabranching rivers and braided systems with vegetated islands. New lineages of aquatic insects developed and expanded novel feeding modes, including herbivory. Late Paleozoic soils commonly contain pervasive root and millipede traces. Lacustrine animal communities diversified, accompanied by increased food-web complexity and improved food delivery which may have favored permanent colonization of offshore and deep-water lake environments. These trends continued in the Permian, but progressive aridification favored formation of hypersaline lakes, which were stressful for colonization. The Capitanian and end-Permian extinctions affected lacustrine and fluvial biotas, particularly the invertebrate infauna, although burrowing may have allowed some tetrapods to survive associated global warming and increased aridification.
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Affiliation(s)
- Luis A Buatois
- Department of Geological Sciences, University of Saskatchewan, Saskatoon, Saskatchewan S7N 5E2, Canada
| | - Neil S Davies
- Department of Earth Sciences, University of Cambridge, Cambridge, Cambridgeshire CB2 3EQ, UK
| | - Martin R Gibling
- Department of Earth and Environmental Sciences, Dalhousie University, Halifax, Nova Scotia B3H 4R2, Canada
| | - Verónica Krapovickas
- Departamento de Ciencias Geológicas, Facultad de Ciencias Exactas y Naturales, Universidad de Buenos Aires, Intendente Güiraldes 2160, Ciudad Universitaria, C1428EGA, Argentina
| | - Conrad C Labandeira
- Department of Paleobiology, Smithsonian Institution, Washington DC 20013-7012, USA.,Department of Entomology and BEES Program, University of Maryland, College Park, Maryland 21740, USA.,College of Life Sciences, Capital Normal University, Beijing 100048, China
| | - Robert B MacNaughton
- Geological Survey of Canada (Calgary), Natural Resources Canada, Calgary, Alberta T2L 2A7, Canada
| | - M Gabriela Mángano
- Department of Geological Sciences, University of Saskatchewan, Saskatoon, Saskatchewan S7N 5E2, Canada
| | - Nicholas J Minter
- School of the Environment, Geography, and Geosciences, University of Portsmouth, Portsmouth, Hampshire PO1 3QL, UK
| | - Anthony P Shillito
- Department of Earth Sciences, University of Oxford, South Parks Road, Oxford, UK
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