{"type": "FeatureCollection", "features": [{"id": "10.1007/s00248-011-9897-5", "type": "Feature", "geometry": null, "properties": {"updated": "2026-05-31T06:55:22Z", "type": "Journal Article", "created": "2011-06-29", "title": "Impacts Of Organic And Inorganic Fertilizers On Nitrification In A Cold Climate Soil Are Linked To The Bacterial Ammonia Oxidizer Community", "description": "The microbiology underpinning soil nitrogen cycling in northeast China remains poorly understood. These agricultural systems are typified by widely contrasting temperature, ranging from -40 to 38\u00b0C. In a long-term site in this region, the impacts of mineral and organic fertilizer amendments on potential nitrification rate (PNR) were determined. PNR was found to be suppressed by long-term mineral fertilizer treatment but enhanced by manure treatment. The abundance and structure of ammonia-oxidizing bacterial (AOB) and archaeal (AOA) communities were assessed using quantitative polymerase chain reaction and denaturing gradient gel electrophoresis techniques. The abundance of AOA was reduced by all fertilizer treatments, while the opposite response was measured for AOB, leading to a six- to 60-fold reduction in AOA/AOB ratio. The community structure of AOA exhibited little variation across fertilization treatments, whereas the structure of the AOB community was highly responsive. PNR was correlated with community structure of AOB rather than that of AOA. Variation in the community structure of AOB was linked to soil pH, total carbon, and nitrogen contents induced by different long-term fertilization regimes. The results suggest that manure amendment establishes conditions which select for an AOB community type which recovers mineral fertilizer-suppressed soil nitrification.", "keywords": ["DNA", " Bacterial", "2. Zero hunger", "China", "Bacteria", "04 agricultural and veterinary sciences", "15. Life on land", "Cold Climate", "Archaea", "Nitrification", "6. Clean water", "Genes", " Archaeal", "Soil", "DNA", " Archaeal", "Ammonia", "Genes", " Bacterial", "13. Climate action", "0401 agriculture", " forestry", " and fisheries", "Fertilizers", "Oxidoreductases", "Soil Microbiology"]}, "links": [{"href": "https://doi.org/10.1007/s00248-011-9897-5"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Microbial%20Ecology", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1007/s00248-011-9897-5", "name": "item", "description": "10.1007/s00248-011-9897-5", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1007/s00248-011-9897-5"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2011-06-29T00:00:00Z"}}, {"id": "10.1007/s00442-009-1427-5", "type": "Feature", "geometry": null, "properties": {"license": "Closed Access", "updated": "2026-05-31T06:55:31Z", "type": "Journal Article", "created": "2009-08-22", "title": "Herbivore Impacts To The Moss Layer Determine Tundra Ecosystem Response To Grazing And Warming", "description": "Herbivory and climate are key environmental drivers, shaping ecosystems at high latitudes. Here, we focus on how these two drivers act in concert, influencing the high arctic tundra. We aim to investigate mechanisms through which herbivory by geese influences vegetation and soil processes in tundra ecosystems under ambient and warmed conditions. To achieve this, two grazing treatments, clipping plus faecal additions and moss removal, were implemented in conjunction with passive warming. Our key finding was that, in many cases, the tundra ecosystem response was determined by treatment impacts on the moss layer. Moss removal reduced the remaining moss layer depth by 30% and increased peak grass biomass by 27%. These impacts were probably due to observed higher soil temperatures and decomposition rates associated with moss removal. The positive impact of moss removal on grass biomass was even greater with warming, further supporting this conclusion. In contrast, moss removal reduced dwarf shrub biomass possibly resulting from increased exposure to desiccating winds. An intact moss layer buffered the soil to increased air temperature and as a result there was no response of vascular plant productivity to warming over the course of this study. In fact, moss removal impacts on soil temperature were nearly double those of warming, suggesting that the moss layer is a key component in controlling soil conditions. The moss layer also absorbed nutrients from faeces, promoting moss growth. We conclude that both herbivory and warming influence this high arctic ecosystem but that herbivory is the stronger driver of the two. Disturbance to the moss layer resulted in a shift towards a more grass-dominated system with less abundant mosses and shrubs, a trend that was further enhanced by warming. Thus herbivore impacts to the moss layer are key to understanding arctic ecosystem response to grazing and warming.", "keywords": ["0106 biological sciences", "Arctic Regions", "Bryophyta", "Feeding Behavior", "15. Life on land", "Cold Climate", "Poaceae", "Global Warming", "01 natural sciences", "Soil", "13. Climate action", "Geese", "Animals", "Biomass", "Ecosystem"]}, "links": [{"href": "https://doi.org/10.1007/s00442-009-1427-5"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Oecologia", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1007/s00442-009-1427-5", "name": "item", "description": "10.1007/s00442-009-1427-5", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1007/s00442-009-1427-5"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2009-08-23T00:00:00Z"}}, {"id": "10.1038/nature02887", "type": "Feature", "geometry": null, "properties": {"license": "Closed Access", "updated": "2026-05-31T06:58:27Z", "type": "Journal Article", "created": "2004-09-22", "title": "Ecosystem Carbon Storage In Arctic Tundra Reduced By Long-Term Nutrient Fertilization", "description": "Global warming is predicted to be most pronounced at high latitudes, and observational evidence over the past 25 years suggests that this warming is already under way. One-third of the global soil carbon pool is stored in northern latitudes, so there is considerable interest in understanding how the carbon balance of northern ecosystems will respond to climate warming. Observations of controls over plant productivity in tundra and boreal ecosystems have been used to build a conceptual model of response to warming, where warmer soils and increased decomposition of plant litter increase nutrient availability, which, in turn, stimulates plant production and increases ecosystem carbon storage. Here we present the results of a long-term fertilization experiment in Alaskan tundra, in which increased nutrient availability caused a net ecosystem loss of almost 2,000 grams of carbon per square meter over 20 years. We found that annual aboveground plant production doubled during the experiment. Losses of carbon and nitrogen from deep soil layers, however, were substantial and more than offset the increased carbon and nitrogen storage in plant biomass and litter. Our study suggests that projected release of soil nutrients associated with high-latitude warming may further amplify carbon release from soils, causing a net loss of ecosystem carbon and a positive feedback to climate warming.", "keywords": ["Greenhouse Effect", "0106 biological sciences", "Time Factors", "Arctic Regions", "Nitrogen", "Plants", "15. Life on land", "Cold Climate", "01 natural sciences", "Carbon", "Soil", "13. Climate action", "Biomass", "Fertilizers", "Ecosystem", "0105 earth and related environmental sciences"]}, "links": [{"href": "https://doi.org/10.1038/nature02887"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Nature", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1038/nature02887", "name": "item", "description": "10.1038/nature02887", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1038/nature02887"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2004-09-01T00:00:00Z"}}, {"id": "10.1038/nature12129", "type": "Feature", "geometry": null, "properties": {"license": "Closed Access", "updated": "2026-05-31T06:58:27Z", "type": "Journal Article", "created": "2013-05-14", "title": "Long-Term Warming Restructures Arctic Tundra Without Changing Net Soil Carbon Storage", "description": "High latitudes contain nearly half of global soil carbon, prompting interest in understanding how the Arctic terrestrial carbon balance will respond to rising temperatures. Low temperatures suppress the activity of soil biota, retarding decomposition and nitrogen release, which limits plant and microbial growth. Warming initially accelerates decomposition, increasing nitrogen availability, productivity and woody-plant dominance. However, these responses may be transitory, because coupled abiotic-biotic feedback loops that alter soil-temperature dynamics and change the structure and activity of soil communities, can develop. Here we report the results of a two-decade summer warming experiment in an Alaskan tundra ecosystem. Warming increased plant biomass and woody dominance, indirectly increased winter soil temperature, homogenized the soil trophic structure across horizons and suppressed surface-soil-decomposer activity, but did not change total soil carbon or nitrogen stocks, thereby increasing net ecosystem carbon storage. Notably, the strongest effects were in the mineral horizon, where warming increased decomposer activity and carbon stock: a 'biotic awakening' at depth.", "keywords": ["Food Chain", "Time Factors", "Nitrogen", "Rain", "Global Warming", "History", " 21st Century", "01 natural sciences", "Carbon Cycle", "Soil", "Animals", "Biomass", "Photosynthesis", "Ecosystem", "Soil Microbiology", "0105 earth and related environmental sciences", "Arctic Regions", "Temperature", "Discriminant Analysis", "04 agricultural and veterinary sciences", "History", " 20th Century", "Plants", "15. Life on land", "Cold Climate", "Carbon", "13. Climate action", "0401 agriculture", " forestry", " and fisheries"], "contacts": [{"organization": "Gaius R. Shaver, John C. Moore, Joshua P. Schimel, Seeta A. Sistla, Rodney T. Simpson, Laura Gough,", "roles": ["creator"]}]}, "links": [{"href": "https://doi.org/10.1038/nature12129"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Nature", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1038/nature12129", "name": "item", "description": "10.1038/nature12129", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1038/nature12129"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2013-05-01T00:00:00Z"}}, {"id": "10.1111/j.1461-0248.2007.01051.x", "type": "Feature", "geometry": null, "properties": {"license": "Closed Access", "updated": "2026-05-31T06:59:42Z", "type": "Journal Article", "created": "2007-05-14", "title": "Global Negative Vegetation Feedback To Climate Warming Responses Of Leaf Litter Decomposition Rates In Cold Biomes", "description": "Abstract<p>Whether climate change will turn cold biomes from large long\uffe2\uff80\uff90term carbon sinks into sources is hotly debated because of the great potential for ecosystem\uffe2\uff80\uff90mediated feedbacks to global climate. Critical are the direction, magnitude and generality of climate responses of plant litter decomposition. Here, we present the first quantitative analysis of the major climate\uffe2\uff80\uff90change\uffe2\uff80\uff90related drivers of litter decomposition rates in cold northern biomes worldwide. Leaf litters collected from the predominant species in 33 global change manipulation experiments in circum\uffe2\uff80\uff90arctic\uffe2\uff80\uff90alpine ecosystems were incubated simultaneously in two contrasting arctic life zones. We demonstrate that longer\uffe2\uff80\uff90term, large\uffe2\uff80\uff90scale changes to leaf litter decomposition will be driven primarily by both direct warming effects and concomitant shifts in plant growth form composition, with a much smaller role for changes in litter quality within species. Specifically, the ongoing warming\uffe2\uff80\uff90induced expansion of shrubs with recalcitrant leaf litter across cold biomes would constitute a negative feedback to global warming. Depending on the strength of other (previously reported) positive feedbacks of shrub expansion on soil carbon turnover, this may partly counteract direct warming enhancement of litter decomposition.</p>", "keywords": ["Greenhouse Effect", "Sweden", "0106 biological sciences", "Analysis of Variance", "Plant Development", "04 agricultural and veterinary sciences", "Plants", "15. Life on land", "Cold Climate", "Models", " Biological", "01 natural sciences", "Carbon", "Plant Leaves", "Species Specificity", "13. Climate action", "SDG 13 - Climate Action", "0401 agriculture", " forestry", " and fisheries", "Alpine; carbon; circum-arctic; global change; growth form; litter turnover; mass loss; vegetation change.", "Ecosystem"]}, "links": [{"href": "https://doi.org/10.1111/j.1461-0248.2007.01051.x"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Ecology%20Letters", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1111/j.1461-0248.2007.01051.x", "name": "item", "description": "10.1111/j.1461-0248.2007.01051.x", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1111/j.1461-0248.2007.01051.x"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2007-05-14T00:00:00Z"}}], "links": [{"rel": "self", "type": "application/geo+json", "title": "This document as GeoJSON", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items?keywords=Cold+Climate&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=Cold+Climate&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=Cold+Climate&", "hreflang": "en-US"}, {"rel": "last", "type": "application/geo+json", "title": "items (last)", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items?keywords=Cold+Climate&offset=5", "hreflang": "en-US"}], "numberMatched": 5, "numberReturned": 5, "distributedFeatures": [], "timeStamp": "2026-05-31T09:58:25.207145Z"}