{"type": "FeatureCollection", "features": [{"id": "10.17863/cam.81466", "type": "Feature", "geometry": null, "properties": {"updated": "2026-07-25T16:19:58Z", "type": "Journal Article", "created": "2022-01-19", "title": "Multimodal correlative imaging and modelling of phosphorus uptake from soil by hyphae of mycorrhizal fungi", "description": "Summary<p>   <p>Phosphorus (P) is essential for plant growth. Arbuscular mycorrhizal fungi (AMF) aid its uptake by acquiring P from sources distant from roots in return for carbon. Little is known about how AMF colonise soil pore\uffe2\uff80\uff90space, and models of AMF\uffe2\uff80\uff90enhanced P\uffe2\uff80\uff90uptake are poorly validated.</p>  <p>We used synchrotron X\uffe2\uff80\uff90ray computed tomography to visualize mycorrhizas in soil and synchrotron X\uffe2\uff80\uff90ray fluorescence/X\uffe2\uff80\uff90ray absorption near edge structure (XRF/XANES) elemental mapping for P, sulphur (S) and aluminium (Al) in combination with modelling.</p>  <p>We found that AMF inoculation had a suppressive effect on colonisation by other soil fungi and identified differences in structure and growth rate between hyphae of AMF and nonmycorrhizal fungi. Our results showed that AMF co\uffe2\uff80\uff90locate with areas of high P and low Al, and preferentially associate with organic\uffe2\uff80\uff90type P species over Al\uffe2\uff80\uff90rich inorganic P.</p>  <p>We discovered that AMF avoid Al\uffe2\uff80\uff90rich areas as a source of P. Sulphur\uffe2\uff80\uff90rich regions were found to be correlated with higher hyphal density and an increased organic\uffe2\uff80\uff90associated P\uffe2\uff80\uff90pool, whilst oxidized S\uffe2\uff80\uff90species were found close to AMF hyphae. Increased S oxidation close to AMF suggested the observed changes were microbiome\uffe2\uff80\uff90related. Our experimentally\uffe2\uff80\uff90validated model led to an estimate of P\uffe2\uff80\uff90uptake by AMF hyphae that is an order of magnitude lower than rates previously estimated \uffe2\uff80\uff93 a result with significant implications for the modelling of plant\uffe2\uff80\uff93soil\uffe2\uff80\uff93AMF interactions.</p>  </p>", "keywords": ["580", "X-ray computed tomography", "570", "Research", "X-ray fluorescence", "Fungi", "Hyphae", "500", "Phosphorus", "mycorrhizas", "04 agricultural and veterinary sciences", "15. Life on land", "plant phosphorus uptake", "Plant Roots", "Soil", "rhizosphere modelling", "Mycorrhizae", "synchrotron", "0401 agriculture", " forestry", " and fisheries", "Soil Microbiology"]}, "links": [{"href": "https://eprints.soton.ac.uk/454110/1/Keyes_et_al_Myco_Paper_TR_04_01_2022_unmarked.pdf"}, {"href": "https://eprints.soton.ac.uk/454110/2/Figures_TR_22_12_2021.pdf"}, {"href": "https://eprints.soton.ac.uk/454110/3/SI_1_TR_22_12_2021_no_markup.pdf"}, {"href": "https://eprints.soton.ac.uk/454110/4/SI_2_TR_22_12_2021.pdf"}, {"href": "https://doi.org/10.17863/cam.81466"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/New%20Phytologist", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.17863/cam.81466", "name": "item", "description": "10.17863/cam.81466", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.17863/cam.81466"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2022-02-15T00:00:00Z"}}, {"id": "10.1155/2018/9736547", "type": "Feature", "geometry": null, "properties": {"updated": "2026-07-25T16:19:18Z", "type": "Journal Article", "created": "2018-05-09", "title": "Chronological Classification of Ancient Mortars Employing Spectroscopy and Spectrometry Techniques: Sagunto (Valencia, Spain) Case", "description": "<p>Forty-two mortar samples, from two archaeological excavations located in Sagunto (Valencian Community, Spain), were analysed by both portable energy dispersive X-ray fluorescence spectroscopy (pED-XRF) and inductively coupled plasma mass spectrometry (ICP-MS) to determine major and minor elements and traces including rare earth elements (REEs). Collected data were crossed with those previously obtained from Sagunto Castle mortars, and principal component analysis (PCA) was applied to discriminate the construction phases of the unearthed buildings. REE permitted to ascribe most of the masonries to the Roman Imperial period. Moreover, a statistical model was built by employing partial least squares discriminant analysis (PLS-DA) in order to classify the mortars from Roman Imperial period and from Islamic period due to the problematic overlapping between these two phases. Results confirmed the effectiveness of the developed indirect chronology method, based on REE data, to discriminate among historic mortars from different construction periods on a wide scale including different Sagunto archaeological sites.</p>", "keywords": ["2. Zero hunger", "0601 history and archaeology", "QC350-467", "06 humanities and the arts", "Optics. Light", "energy dispersive X-ray fluorescence spectroscopy (pED-XRF); inductively coupled plasma mass spectrometry (ICP-MS)", "Analytical Chemistry; Atomic and Molecular Physics", " and Optics; Spectroscopy"]}, "links": [{"href": "https://eprints.whiterose.ac.uk/130462/1/9736547.pdf"}, {"href": "https://iris.unica.it/bitstream/11584/248342/2/Ramacciotti%20et%20al%202018.pdf"}, {"href": "https://arpi.unipi.it/bitstream/11568/935316/1/P101%20Chronological%20Classification%20of%20Ancient%20Mortars.pdf"}, {"href": "https://doi.org/10.1155/2018/9736547"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Journal%20of%20Spectroscopy", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1155/2018/9736547", "name": "item", "description": "10.1155/2018/9736547", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1155/2018/9736547"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2018-01-01T00:00:00Z"}}, {"id": "10.1016/j.jasrep.2019.03.017", "type": "Feature", "geometry": null, "properties": {"updated": "2026-07-25T16:16:39Z", "type": "Journal Article", "created": "2019-03-25", "title": "Chemical and mineralogical analyses on stones from Sagunto Castle (Spain)", "description": "For the first time, an archaeometric study was carried out on the carbonate rock ashlars of the Sagunto Castle. The studied site is one of the most important and best preserved Spanish archaeological and architectural monuments, characterized by different construction phases from the Roman period to Modern Ages. Forty samples collected from thirteen different structures of Sagunto Castle and two quarries, located in the Sagunto's hill were used for comparative purposes. The samples were analyzed by X-ray diffraction, X-ray fluorescence and inductively coupled plasma mass spectrometry to determine their mineralogical and elemental composition. The obtained data show similar chemical and mineralogical features between the rocks outcropping in the city quarries and some of those employed to build the structures, suggesting that rocks could have been used to build the structures from different periods along the centuries.", "keywords": ["Building stone; Chemistry; Fortress; Middle ages; Mineralogy; Remains; Roman period", "Building stone; Fortress; Remains; Chemistry; Mineralogy; Roman period; Middle ages", "archaeometrics; carbonate rock ashlars; X-ray fluorescence and inductively coupled plasma mass spectrometry", "01 natural sciences", "0104 chemical sciences", "0105 earth and related environmental sciences"]}, "links": [{"href": "https://iris.unica.it/bitstream/11584/298931.2/3/Ramaciotti%20et%20al%202018_1-s2.0-S2352409X18307454-main.pdf"}, {"href": "https://doi.org/10.1016/j.jasrep.2019.03.017"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Journal%20of%20Archaeological%20Science%3A%20Reports", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1016/j.jasrep.2019.03.017", "name": "item", "description": "10.1016/j.jasrep.2019.03.017", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1016/j.jasrep.2019.03.017"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2019-04-01T00:00:00Z"}}, {"id": "10.1111/nph.17980", "type": "Feature", "geometry": null, "properties": {"updated": "2026-07-25T16:19:06Z", "type": "Journal Article", "created": "2022-01-19", "title": "Multimodal correlative imaging and modelling of phosphorus uptake from soil by hyphae of mycorrhizal fungi", "description": "Summary<p>   <p>Phosphorus (P) is essential for plant growth. Arbuscular mycorrhizal fungi (AMF) aid its uptake by acquiring P from sources distant from roots in return for carbon. Little is known about how AMF colonise soil pore\uffe2\uff80\uff90space, and models of AMF\uffe2\uff80\uff90enhanced P\uffe2\uff80\uff90uptake are poorly validated.</p>  <p>We used synchrotron X\uffe2\uff80\uff90ray computed tomography to visualize mycorrhizas in soil and synchrotron X\uffe2\uff80\uff90ray fluorescence/X\uffe2\uff80\uff90ray absorption near edge structure (XRF/XANES) elemental mapping for P, sulphur (S) and aluminium (Al) in combination with modelling.</p>  <p>We found that AMF inoculation had a suppressive effect on colonisation by other soil fungi and identified differences in structure and growth rate between hyphae of AMF and nonmycorrhizal fungi. Our results showed that AMF co\uffe2\uff80\uff90locate with areas of high P and low Al, and preferentially associate with organic\uffe2\uff80\uff90type P species over Al\uffe2\uff80\uff90rich inorganic P.</p>  <p>We discovered that AMF avoid Al\uffe2\uff80\uff90rich areas as a source of P. Sulphur\uffe2\uff80\uff90rich regions were found to be correlated with higher hyphal density and an increased organic\uffe2\uff80\uff90associated P\uffe2\uff80\uff90pool, whilst oxidized S\uffe2\uff80\uff90species were found close to AMF hyphae. Increased S oxidation close to AMF suggested the observed changes were microbiome\uffe2\uff80\uff90related. Our experimentally\uffe2\uff80\uff90validated model led to an estimate of P\uffe2\uff80\uff90uptake by AMF hyphae that is an order of magnitude lower than rates previously estimated \uffe2\uff80\uff93 a result with significant implications for the modelling of plant\uffe2\uff80\uff93soil\uffe2\uff80\uff93AMF interactions.</p>  </p", "keywords": ["580", "X-ray computed tomography", "570", "Research", "X-ray fluorescence", "Fungi", "Hyphae", "500", "Phosphorus", "mycorrhizas", "04 agricultural and veterinary sciences", "15. Life on land", "plant phosphorus uptake", "Plant Roots", "Soil", "rhizosphere modelling", "Mycorrhizae", "synchrotron", "0401 agriculture", " forestry", " and fisheries", "Soil Microbiology"]}, "links": [{"href": "https://eprints.soton.ac.uk/454110/1/Keyes_et_al_Myco_Paper_TR_04_01_2022_unmarked.pdf"}, {"href": "https://eprints.soton.ac.uk/454110/2/Figures_TR_22_12_2021.pdf"}, {"href": "https://eprints.soton.ac.uk/454110/3/SI_1_TR_22_12_2021_no_markup.pdf"}, {"href": "https://eprints.soton.ac.uk/454110/4/SI_2_TR_22_12_2021.pdf"}, {"href": "https://doi.org/10.1111/nph.17980"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/New%20Phytologist", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1111/nph.17980", "name": "item", "description": "10.1111/nph.17980", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1111/nph.17980"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2022-02-15T00:00:00Z"}}, {"id": "10.3389/feart.2021.703304", "type": "Feature", "geometry": null, "properties": {"updated": "2026-07-25T16:20:45Z", "type": "Journal Article", "created": "2021-09-04", "title": "Mineral Element Stocks in the Yedoma Domain: A Novel Method Applied to Ice-Rich Permafrost Regions", "description": "<p>With permafrost thaw, significant amounts of organic carbon (OC) previously stored in frozen deposits are unlocked and become potentially available for microbial mineralization. This is particularly the case in ice-rich regions such as the Yedoma domain. Excess ground ice degradation exposes deep sediments and their OC stocks, but also mineral elements, to biogeochemical processes. Interactions of mineral elements and OC play a crucial role for OC stabilization and the fate of OC upon thaw, and thus regulate carbon dioxide and methane emissions. In addition, some mineral elements are limiting nutrients for plant growth or microbial metabolic activity. A large ongoing effort is to quantify OC stocks and their lability in permafrost regions, but the influence of mineral elements on the fate of OC or on biogeochemical nutrient cycles has received less attention and there is an overall lack of mineral element content analyses for permafrost sediments. Here, we combine portable X-ray fluorescence (pXRF) with a bootstrapping technique to provide i) the first large-scale Yedoma domain Mineral Concentrations Assessment (YMCA) dataset, and ii) estimates of mineral element stocks in never thawed (since deposition) ice-rich Yedoma permafrost and previously thawed and partly refrozen Alas deposits. The pXRF method for mineral element quantification is non-destructive and offers a complement to the classical dissolution and measurement by optical emission spectrometry (ICP-OES) in solution. Using this method, mineral element concentrations (Si, Al, Fe, Ca, K, Ti, Mn, Zn, Sr and Zr) were assessed on 1,292 sediment samples from the Yedoma domain with lower analytical effort and lower costs relative to the ICP-OES method. The pXRF measured concentrations were calibrated using alkaline fusion and ICP-OES measurements on a subset of 144 samples (R2 from 0.725 to 0.996). The results highlight that i) the mineral element stock in sediments of the Yedoma domain (1,387,000\uffc2\uffa0km2) is higher for Si, followed by Al, Fe, K, Ca, Ti, Mn, Zr, Sr, and Zn, and that ii) the stock in Al and Fe (598 \uffc2\uffb1 213 and 288 \uffc2\uffb1 104\uffc2\uffa0Gt) is in the same order of magnitude as the OC stock (327\uffe2\uff80\uff93466\uffc2\uffa0Gt).</p>", "keywords": ["ddc:550", "late pleistocene- holocene", "thermokarst", "Science", "Q", "X-ray fluorescence", "01 natural sciences", "6. Clean water", "13. Climate action", "arctic", "alas", "Institut f\u00fcr Geowissenschaften", "thaw", "mineralogy", "late pleistocene \u2013 holocene", "bootstrapping technique", "0105 earth and related environmental sciences"]}, "links": [{"href": "https://doi.org/10.3389/feart.2021.703304"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Frontiers%20in%20Earth%20Science", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.3389/feart.2021.703304", "name": "item", "description": "10.3389/feart.2021.703304", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.3389/feart.2021.703304"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2021-09-03T00:00:00Z"}}, {"id": "11568/935316", "type": "Feature", "geometry": null, "properties": {"updated": "2026-07-25T16:25:03Z", "type": "Journal Article", "created": "2018-05-09", "title": "Chronological Classification of Ancient Mortars Employing Spectroscopy and Spectrometry Techniques: Sagunto (Valencia, Spain) Case", "description": "<?xml version='1.0' encoding='UTF-8'?><article><p>Forty-two mortar samples, from two archaeological excavations located in Sagunto (Valencian Community, Spain), were analysed by both portable energy dispersive X-ray fluorescence spectroscopy (pED-XRF) and inductively coupled plasma mass spectrometry (ICP-MS) to determine major and minor elements and traces including rare earth elements (REEs). Collected data were crossed with those previously obtained from Sagunto Castle mortars, and principal component analysis (PCA) was applied to discriminate the construction phases of the unearthed buildings. REE permitted to ascribe most of the masonries to the Roman Imperial period. Moreover, a statistical model was built by employing partial least squares discriminant analysis (PLS-DA) in order to classify the mortars from Roman Imperial period and from Islamic period due to the problematic overlapping between these two phases. Results confirmed the effectiveness of the developed indirect chronology method, based on REE data, to discriminate among historic mortars from different construction periods on a wide scale including different Sagunto archaeological sites.</p></article>", "keywords": ["2. Zero hunger", "0601 history and archaeology", "QC350-467", "06 humanities and the arts", "Optics. Light", "energy dispersive X-ray fluorescence spectroscopy (pED-XRF); inductively coupled plasma mass spectrometry (ICP-MS)", "Analytical Chemistry; Atomic and Molecular Physics", " and Optics; Spectroscopy"]}, "links": [{"href": "https://eprints.whiterose.ac.uk/130462/1/9736547.pdf"}, {"href": "https://iris.unica.it/bitstream/11584/248342/2/Ramacciotti%20et%20al%202018.pdf"}, {"href": "https://arpi.unipi.it/bitstream/11568/935316/1/P101%20Chronological%20Classification%20of%20Ancient%20Mortars.pdf"}, {"href": "https://doi.org/11568/935316"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Journal%20of%20Spectroscopy", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "11568/935316", "name": "item", "description": "11568/935316", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/11568/935316"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2018-01-01T00:00:00Z"}}, {"id": "2078.1/250558", "type": "Feature", "geometry": null, "properties": {"updated": "2026-07-25T16:25:36Z", "type": "Journal Article", "created": "2021-09-04", "title": "Mineral Element Stocks in the Yedoma Domain: A Novel Method Applied to Ice-Rich Permafrost Regions", "description": "<p>With permafrost thaw, significant amounts of organic carbon (OC) previously stored in frozen deposits are unlocked and become potentially available for microbial mineralization. This is particularly the case in ice-rich regions such as the Yedoma domain. Excess ground ice degradation exposes deep sediments and their OC stocks, but also mineral elements, to biogeochemical processes. Interactions of mineral elements and OC play a crucial role for OC stabilization and the fate of OC upon thaw, and thus regulate carbon dioxide and methane emissions. In addition, some mineral elements are limiting nutrients for plant growth or microbial metabolic activity. A large ongoing effort is to quantify OC stocks and their lability in permafrost regions, but the influence of mineral elements on the fate of OC or on biogeochemical nutrient cycles has received less attention and there is an overall lack of mineral element content analyses for permafrost sediments. Here, we combine portable X-ray fluorescence (pXRF) with a bootstrapping technique to provide i) the first large-scale Yedoma domain Mineral Concentrations Assessment (YMCA) dataset, and ii) estimates of mineral element stocks in never thawed (since deposition) ice-rich Yedoma permafrost and previously thawed and partly refrozen Alas deposits. The pXRF method for mineral element quantification is non-destructive and offers a complement to the classical dissolution and measurement by optical emission spectrometry (ICP-OES) in solution. Using this method, mineral element concentrations (Si, Al, Fe, Ca, K, Ti, Mn, Zn, Sr and Zr) were assessed on 1,292 sediment samples from the Yedoma domain with lower analytical effort and lower costs relative to the ICP-OES method. The pXRF measured concentrations were calibrated using alkaline fusion and ICP-OES measurements on a subset of 144 samples (R2 from 0.725 to 0.996). The results highlight that i) the mineral element stock in sediments of the Yedoma domain (1,387,000\uffc2\uffa0km2) is higher for Si, followed by Al, Fe, K, Ca, Ti, Mn, Zr, Sr, and Zn, and that ii) the stock in Al and Fe (598 \uffc2\uffb1 213 and 288 \uffc2\uffb1 104\uffc2\uffa0Gt) is in the same order of magnitude as the OC stock (327\uffe2\uff80\uff93466\uffc2\uffa0Gt).</p", "keywords": ["ddc:550", "late pleistocene- holocene", "thermokarst", "Science", "Q", "X-ray fluorescence", "01 natural sciences", "6. Clean water", "13. Climate action", "arctic", "alas", "Institut f\u00fcr Geowissenschaften", "thaw", "mineralogy", "late pleistocene \u2013 holocene", "bootstrapping technique", "0105 earth and related environmental sciences"]}, "links": [{"href": "https://doi.org/2078.1/250558"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Frontiers%20in%20Earth%20Science", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "2078.1/250558", "name": "item", "description": "2078.1/250558", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/2078.1/250558"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2021-09-03T00:00:00Z"}}, {"id": "2158/1353729", "type": "Feature", "geometry": null, "properties": {"updated": "2026-07-25T16:25:41Z", "type": "Journal Article", "created": "2019-03-25", "title": "Chemical and mineralogical analyses on stones from Sagunto Castle (Spain)", "description": "For the first time, an archaeometric study was carried out on the carbonate rock ashlars of the Sagunto Castle. The studied site is one of the most important and best preserved Spanish archaeological and architectural monuments, characterized by different construction phases from the Roman period to Modern Ages. Forty samples collected from thirteen different structures of Sagunto Castle and two quarries, located in the Sagunto's hill were used for comparative purposes. The samples were analyzed by X-ray diffraction, X-ray fluorescence and inductively coupled plasma mass spectrometry to determine their mineralogical and elemental composition. The obtained data show similar chemical and mineralogical features between the rocks outcropping in the city quarries and some of those employed to build the structures, suggesting that rocks could have been used to build the structures from different periods along the centuries.", "keywords": ["Building stone; Chemistry; Fortress; Middle ages; Mineralogy; Remains; Roman period", "Building stone; Fortress; Remains; Chemistry; Mineralogy; Roman period; Middle ages", "archaeometrics; carbonate rock ashlars; X-ray fluorescence and inductively coupled plasma mass spectrometry", "01 natural sciences", "0104 chemical sciences", "0105 earth and related environmental sciences"]}, "links": [{"href": "https://iris.unica.it/bitstream/11584/298931.2/3/Ramaciotti%20et%20al%202018_1-s2.0-S2352409X18307454-main.pdf"}, {"href": "https://doi.org/2158/1353729"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Journal%20of%20Archaeological%20Science%3A%20Reports", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "2158/1353729", "name": "item", "description": "2158/1353729", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/2158/1353729"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2019-04-01T00:00:00Z"}}, {"id": "3146683732", "type": "Feature", "geometry": null, "properties": {"updated": "2026-07-25T16:26:20Z", "type": "Dataset", "title": "Yedoma domain Mineral Concentrations Assessment (YMCA)", "description": "Mineral elements play a crucial role for organic carbon stabilization, which is key for organic carbon mineralization rates in soils. With thawing permafrost, especially in ice-rich regions such as the Yedoma domain, vast amounts of organic carbon previously stored in deep frozen deposits are unlocked and therefore available to undergo microbial mineralization leading to potential carbon dioxide and methane emissions. Mineral elements interfere with organic carbon degradation through various processes: i) mineral protection (aggregation, adsorption, and complexation) stabilizes organic carbon and mitigates its mineralization, and ii) change in mineral nutrients availability affects microorganisms growth and metabolic activity. Despite huge efforts to assess organic carbon stocks and lability in permafrost regions, there is a lack of studies on the mineral component assessment, which we aim to close with this dataset. Here, we provide a large-scale Yedoma domain Mineral Concentrations Assessment (YMCA) dataset of never thawed (since deposition) ice-rich Yedoma permafrost and previously thawed and partly refrozen Alas deposits. We used a portable X-ray fluorescence device (pXRF) for Si, Al, Fe, Ca, K, Ti, Mn, Zn, Sr and Zr concentration measurements on 1,292 sediment samples. Portable XRF measured concentrations trueness was calibrated using standard alkaline fusion and ICP-OES measurement from a subset of 144 samples (R\u00b2 from 0.725 to 0.996). This methodology lead to the creation of the Yedoma domain Mineral Concentration Assessment (YMCA) dataset, a necessary step to estimate mineral element stocks in never thawed Yedoma and previously thawed Alas deposits. Practically, the YMCA dataset is organized as follow: (i) all site and sample properties: sample ID, type of deposit, site location, profile ID, GPS coordinates, country, lithology, unconsolidated sediment type, geological epoch, samples depth below surface level (b.s.l) or height above sea/river level (a.s.l), sediment characteristics, bulk density, gravimetric and absolute ice content, total organic carbon content; (ii) the Si, Al, Fe, Ca, K, Ti, Mn, Zn, Sr and Zr concentrations (corrected based on linear regressions) in Yedoma and Alas deposits (n=1292).", "keywords": ["Density", "Permafrost", "Profile ID", "gravimetric", "Density", " bulk", " permafrost", "Aluminium", "total", "Sample code/label", "Portable X ray fluorescence device", "Titanium", "Mineral element", "Yedoma", "Portable X-ray fluorescence device", "Description", "Number", "Lithology/composition/facies", "Sample code label", "6. Clean water", "Deposit type", "Country", "sediment rock", "Zinc", "Earth System Research", "Alas", "Profile", "Silicon", "Lithology composition facies", "Height above sea level", "organic", "Iron", "Site", "DEPTH", " sediment/rock", "bulk", "Ice content", " gravimetric", "LONGITUDE", "Organic carbon", "Manganese", "Sediment type", "organic carbon", "15. Life on land", "Ice content", "Carbon", "Epoch", "Sample ID", "13. Climate action", "Strontium", "DEPTH", "LATITUDE", "Potassium", "Calcium", "Zirconium", "permafrost", "Carbon", " organic", " total"]}, "links": [{"href": "https://doi.org/3146683732"}, {"rel": "self", "type": "application/geo+json", "title": "3146683732", "name": "item", "description": "3146683732", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/3146683732"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2020-01-01T00:00:00Z"}}, {"id": "PMC9307049", "type": "Feature", "geometry": null, "properties": {"updated": "2026-07-25T16:28:14Z", "type": "Journal Article", "created": "2022-01-19", "title": "Multimodal correlative imaging and modelling of phosphorus uptake from soil by hyphae of mycorrhizal fungi", "description": "Summary<p>   <p>Phosphorus (P) is essential for plant growth. Arbuscular mycorrhizal fungi (AMF) aid its uptake by acquiring P from sources distant from roots in return for carbon. Little is known about how AMF colonise soil pore\uffe2\uff80\uff90space, and models of AMF\uffe2\uff80\uff90enhanced P\uffe2\uff80\uff90uptake are poorly validated.</p>  <p>We used synchrotron X\uffe2\uff80\uff90ray computed tomography to visualize mycorrhizas in soil and synchrotron X\uffe2\uff80\uff90ray fluorescence/X\uffe2\uff80\uff90ray absorption near edge structure (XRF/XANES) elemental mapping for P, sulphur (S) and aluminium (Al) in combination with modelling.</p>  <p>We found that AMF inoculation had a suppressive effect on colonisation by other soil fungi and identified differences in structure and growth rate between hyphae of AMF and nonmycorrhizal fungi. Our results showed that AMF co\uffe2\uff80\uff90locate with areas of high P and low Al, and preferentially associate with organic\uffe2\uff80\uff90type P species over Al\uffe2\uff80\uff90rich inorganic P.</p>  <p>We discovered that AMF avoid Al\uffe2\uff80\uff90rich areas as a source of P. Sulphur\uffe2\uff80\uff90rich regions were found to be correlated with higher hyphal density and an increased organic\uffe2\uff80\uff90associated P\uffe2\uff80\uff90pool, whilst oxidized S\uffe2\uff80\uff90species were found close to AMF hyphae. Increased S oxidation close to AMF suggested the observed changes were microbiome\uffe2\uff80\uff90related. Our experimentally\uffe2\uff80\uff90validated model led to an estimate of P\uffe2\uff80\uff90uptake by AMF hyphae that is an order of magnitude lower than rates previously estimated \uffe2\uff80\uff93 a result with significant implications for the modelling of plant\uffe2\uff80\uff93soil\uffe2\uff80\uff93AMF interactions.</p>  </p", "keywords": ["580", "X-ray computed tomography", "570", "Research", "X-ray fluorescence", "Fungi", "Hyphae", "500", "Phosphorus", "mycorrhizas", "04 agricultural and veterinary sciences", "15. Life on land", "plant phosphorus uptake", "Plant Roots", "Soil", "rhizosphere modelling", "Mycorrhizae", "synchrotron", "0401 agriculture", " forestry", " and fisheries", "Soil Microbiology"]}, "links": [{"href": "https://eprints.soton.ac.uk/454110/1/Keyes_et_al_Myco_Paper_TR_04_01_2022_unmarked.pdf"}, {"href": "https://eprints.soton.ac.uk/454110/2/Figures_TR_22_12_2021.pdf"}, {"href": "https://eprints.soton.ac.uk/454110/3/SI_1_TR_22_12_2021_no_markup.pdf"}, {"href": "https://eprints.soton.ac.uk/454110/4/SI_2_TR_22_12_2021.pdf"}, {"href": "https://doi.org/PMC9307049"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/New%20Phytologist", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "PMC9307049", "name": "item", "description": "PMC9307049", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/PMC9307049"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2022-02-15T00:00:00Z"}}], "links": [{"rel": "self", "type": "application/geo+json", "title": "This document as GeoJSON", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items?keywords=X-ray+fluorescence&f=json", "hreflang": "en-US"}, {"rel": "alternate", "type": "text/html", "title": "This document as HTML", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items?keywords=X-ray+fluorescence&f=html", "hreflang": "en-US"}, {"rel": "collection", "type": "application/json", "title": "Collection URL", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main", "hreflang": "en-US"}, {"type": "application/geo+json", "rel": "first", "title": "items (first)", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items?keywords=X-ray+fluorescence&", "hreflang": "en-US"}, {"rel": "last", "type": "application/geo+json", "title": "items (last)", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items?keywords=X-ray+fluorescence&offset=10", "hreflang": "en-US"}], "numberMatched": 10, "numberReturned": 10, "distributedFeatures": [], "timeStamp": "2026-07-26T13:05:31.466758Z"}