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101 results for “dissolved organic matter”
Seasonal concentrations and fluxes of dissolved, soluble, and colloidal Fe and dissolved organic matter amount and composition (DOC and PARAFAC)
<p>These datasets accompany the following manuscript:</p> <p>Logozzo, L.A.*, Hosen, J.D., McArthur, J., and Raymond, P.A. Distinct drivers of two size fractions of operationally dissolved Fe in a temperate river. Limnology and Oceanography.</p> <p>*Corresponding Author: Laura A. Logozzo, laura.logozzo@uleth.ca</p> <p>Datasets:</p> <p>1- Fe-DOM-EMMA-merged.xlsx: this dataset includes operationally dissolved (<0.22 µm), colloidal (0.02-0.22 µm), and soluble (<0.02 µm) DOC concentrations, total Fe concentrations, PARAFAC component scores <0.22 µm, and end-member mixing model scores <0.22 µm. Samples were collected approximately bi-weekly from the Connecticut River at Thompsonville from April 2018 to March 2020.</p> <p>2- Loadest-merged.xlsx: this dataset includes LOADEST-modeled daily-average and monthly-average fluxes of operationally dissolved (<0.22 µm), colloidal (0.02-0.22 µm), and soluble (<0.02 µm) Fe, DOC <0.22 µm, and allochthonous-like DOC <0.22 µm.</p> <p>All methodology is described in the accompanied manuscript.</p>
Data from: Phosphorus limitation determines the quality of dissolved organic matter released by marine heterotrophic prokaryotes
<p>We determined phosphorus (P) limitation effect on the quantity and quality of dissolved organic matter (DOM) released by heterotrophic prokaryotes (HP). We grew 2 single bacterial strains, Photobacterium angustum and Sphingopyxis alaskensis, and natural HP communities collected in fall and spring from the Mediterranean Sea, on glucose under 2 treatments: P-replete vs. P-limiting. DOM release by HP comprised up to 30 % of the initial carbon provided for growth. P availability influenced carbon allocation to different cellular processes (respiration vs. growth), but did not significantly affect the quantity of DOM released by HP. However, using fluorescence spectroscopy, we demonstrated an effect of P-limitation on DOM quality, with a predominance of humic-like compounds under P-limitation but protein-like compounds under P-repletion. Our results suggest that P-limitation could determine the fate of HP-derived DOM in the ocean, thus affecting the microbial carbon pump.</p>
Soil microbial community, dissolved organic matter and nutrient cycling interactions change along an elevation gradient in subtropical China
<p>This table contains data on soil dissolved organic matter at different elevations in Wuyi Mountain, China, which is attached to the manuscript submitted to Journal of Environmental Management (Manuscript ID:JEMA-D-23-01912). </p>
Data for: Human activity coupled with climate change strengthens the role of lakes as an active pipe of dissolved organic matter
<p>This dataset contains data from an investigation to resolve the relative importance of multiple environmental drivers on the quantity and quality of chromophoric DOM in lakes at the continental scales. The study is described in the paper: "Du Y., Chen F., Zhang Y., He H., Wen S., Huang X., Song C., Li. K., Wang J., Kellings D., and Lu Y. 2023. Human activity coupled with climate change strengthens the role of lakes as an active pipe of dissolved organic matter, Earth's Future, in press". </p> <p>The primary objectives of the study were to (i) quantity the magnitude of environmental drivers modulating lacustrine DOM quantity and quality at a continental scale, including climate, land cover, societal development, and water retention time, and (ii) unravel individual and interactive effects of the environmental drivers.</p> <p>Firstly, we constructed a structural equation model framework that incorporated both direct and indirect pathways.</p> <p>Secondly, we collected a continental-scale dataset of lake DOM quantity and quality, along with the corresponding environmental driver variables from a group of carefully selected lakes (n=182).</p> <p>Lastly, we established structure equation models to analyze DOM quantity and quality variations as a function of the four environmental drivers.</p> <p>The main results include: (1) land cover and societal development both exhibit positive direct effects on lake CDOM quantity, highlighting the significant role of well-vegetated soils and anthropogenic activities as sources of lake DOM on a continental scale. (2) Climate has two strong but opposite effects –a warming and wet climate facilitates soil OM production and export but also enhances CDOM in-lake transformation. (3) Three proxies are proposed as indicators of the magnitude of biogeochemical drivers influencing lake DOM across ecoclimatic zones, including fluorescent DOM/DOC indicating economic activity, percentages of a degraded fluorescent DOM component indicating solar irradiation, and percent tyrosine-like DOM reflecting DOM processing time within the watershed and lake.</p>
The effects of dissolved organic matter supplements on the metabolism of corals under heat stress
<p><span>Octocorals represent a</span><span> major alternative group in the benthic community of reefs that have diverged from hexacoral dominance. Despite their phototrophic symbionts, supplementing their diet with heterotrophic sources may promote their growth, particularly when compared to hexacorals in bleaching conditions. However, limited comprehensive data exists on octocorals' trophic ecology, especially regarding their ability to feed on dissolved organic matter (DOM), which comprises the largest pool of organic matter in reefs. This study aims to investigate the ability of two octocorals (<em>Sarcophyton glaucum </em>and <em>Lobophytum sp.</em>) to feed on DOM and compare this ability to that of hexacorals, such as <em>Stylophora pistillata</em> and <em>Turbinaria reniformis. </em>The study measured the net fluxes of DOM under varying DOM concentrations and under heat stress. The results demonstrate that all coral species were net producers of DOM at ambient concentrations, but became net consumers once seawater was supplemented with DOM. Furthermore, our study highlights a relationship between coral physiological responses to heat stress and DOM uptake. Corals that increased (<em>S. pistillata</em>) or maintained (<em>S. glaucum</em> and <em>Lobophytum sp.)</em> their DOM uptake rates at high temperatures were the most resilient to heat stress. In contrast, <em>T. reniformis</em> exhibited lower DOM uptake rates at high temperatures, which was associated with significant bleaching. </span><span>Understanding the ability of corals to feed on DOM may therefore provide insight on the resilience of species under ocean warming conditions.</span></p>
Reactivity, fate and functional roles of dissolved organic matter in anoxic inland waters
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Nocturnal dissolved organic matter release by turf algae and its role in the microbialization of reefs
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Single-cell visualization indicates direct role of sponge host in uptake of dissolved organic matter
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Data from: The primacy of dissolved organic matter to aquatic light variability
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Data for: Human activity coupled with climate change strengthens the role of lakes as an active pipe of dissolved organic matter
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Oxygen availability regulates the quality of soil dissolved organic matter by mediating microbial metabolism and iron oxidation
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Water residence time and temperature drive the dynamics of dissolved organic matter in Alpine lakes in the Tibetan Plateau
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13C NMR data for the five dissolved organic matter
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Data for: Transformation of dissolved organic matter by two Indo-Pacific sponges
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The effects of dissolved organic matter supplements on the metabolism of corals under heat stress
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Phytoplankton assemblage shifts with dissolved organic matter properties: a functional perspective for sentinel lakes
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Data from: Phosphorus limitation determines the quality of dissolved organic matter released by marine heterotrophic prokaryotes
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Dataset for "Technical note: Effects of iron(II) on fluorescence properties of dissolved organic matter at circumneutral pH"
<p>This dataset contains fluorescence spectroscopy data (excitation-emission matrices and PARAFAC component analysis) from an experiment adding increasing concentrations of soluble reduced iron, Fe(II), to groundwater.</p>
Data from: Differential recycling of coral and algal dissolved organic matter via the sponge loop
Corals and macroalgae release large quantities of dissolved organic matter (DOM), one of the largest sources of organic matter produced on coral reefs. By rapidly taking up DOM and transforming it into particulate detritus, coral reef sponges are proposed to play a key role in transferring the energy and nutrients in DOM to higher trophic levels via the recently discovered sponge loop. DOM released by corals and algae differs in quality and composition, but the influence of these different DOM sources on recycling by the sponge loop has not been investigated. Here, we used stable isotope pulse‐chase experiments to compare the processing of naturally sourced coral‐ and algal‐derived DOM by three Red Sea coral reef sponge species: Chondrilla sacciformis, Hemimycale arabica and Mycale fistulifera. Incubation experiments were conducted to trace 13C‐ and 15N‐enriched coral‐ and algal‐derived DOM into the sponge tissue and detritus. Incorporation of 13C into specific phospholipid‐derived fatty acids (PLFAs) was used to differentiate DOM assimilation within the sponge holobiont (i.e. the sponge host vs. its associated bacteria). All sponges assimilated both coral‐ and algal‐derived DOM, but incorporation rates were significantly higher for algal‐derived DOM. The two DOM sources were also processed differently by the sponge holobiont. Algal‐derived DOM was incorporated into bacteria‐specific PLFAs at a higher rate while coral‐derived DOM was more readily incorporated into sponge‐specific PLFAs. A substantial fraction of the dissolved organic carbon (C) and nitrogen (N) assimilated by the sponges was subsequently converted into and released as particulate detritus (15–24% C and 27–49% N). However, algal‐derived DOM was released as detritus at a higher rate. The higher uptake and transformation rates of algal‐ compared with coral‐derived DOM suggest that reef community phase shifts from coral to algal dominance may stimulate DOM cycling through the sponge loop with potential consequences for coral reef biogeochemical cycles and food webs.
Global patterns and drivers of dissolved organic matter across Earth systems: Insights from H/C and O/C ratios
<p>Dissolved organic matter (DOM) is ubiquitous and contains a complex pool of thousands of distinct molecules, and their chemical characteristics help us inform the fate of global carbon. Yet, a more holistic perspective of molecular characteristics of DOM and underlying mechanisms across Earth systems and climates remain understudied. Here, we present a comprehensive analysis of the molecular characteristics of DOM using two abundance-weighted average indices, i.e., H/C and O/C ratios by compiling 2,995 samples from 317 studies covering the waters, land, plant, petroleum, and atmosphere systems, and the climatic regions from tropics to tundra. H/C ratios are lower on average in waters (H/C = 1.15 ± 0.005) and land (H/C = 1.20 ± 0.010) than the other systems, while their O/C ratios rank between plant and atmosphere. In the waters and land systems, the H/C ratios of DOM vary from the highest to the lowest in the habitats of land-to-ocean continuum generally as snow > glacier > marine ≥ freshwater/soil > groundwater. The H/C ratios show predictably U-shaped patterns along latitudinal gradients indicating the lowest abundance of more hydrogen saturated molecules at around mid-latitudes of 40°-50° in river water, lake water, and forest soil. The two ratios are primarily controlled by the environmental factors such as pH, dissolved oxygen, and carbon and nitrogen contents. We further unveil additional and considerable links between the ratios and the extremes of climatic factors such as precipitation of warmest quarter and maximum temperature of warmest month. Our synthesis provides molecular-level perspectives to characterize the global distribution and underlying drivers of DOM, which is complementary for our understanding global carbon cycle's processes under future global change.</p>
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Allen Brain Atlas
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International Brain Laboratory public data
The International Brain Laboratory public data releases expose standardized mouse decision-making experiments, including Neuropixels recordings, widefield calcium imaging, behavior, and session metadata accessed through the ONE API.
OpenNeuro
OpenNeuro is a free, open platform for sharing neuroimaging datasets, with public search, dataset pages, and download paths for web, S3, DataLad, and the OpenNeuro CLI.