Gerd Gleixner
Gleixner, Gerd.
![Sudoc [ABES], France](/viaf/images/flags/SUDOC.png "Sudoc [ABES], France")
Gleixner, Gerd 1963-
VIAF ID: 165716055 (Personal)
Permalink: http://viaf.org/viaf/165716055
Preferred Forms
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100 0 _
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Gerd Gleixner
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100 1 _ ‡a Gleixner, Gerd
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100 1 _ ‡a Gleixner, Gerd (sparse)
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100 1 _
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Gleixner, Gerd
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100 1 _
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Gleixner, Gerd
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100 1 _ ‡a Gleixner, Gerd
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100 1 _ ‡a Gleixner, Gerd
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100 1 _
‡a
Gleixner, Gerd
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100 1 _
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Gleixner, Gerd
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1963-
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100 1 _ ‡a Gleixner, Gerd.
4xx's: Alternate Name Forms (11)
5xx's: Related Names (4)
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Friedrich-Schiller-Universität Jena
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Chemisch-Geowissenschaftliche Fakultät
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affi
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https://d-nb.info/standards/elementset/gnd#affiliation
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Affiliation
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Jena
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ortw
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https://d-nb.info/standards/elementset/gnd#placeOfActivity
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Max-Planck-Institut für Biogeochemie
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Jena
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affi
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https://d-nb.info/standards/elementset/gnd#affiliation
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Affiliation
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Uetersen
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ortg
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https://d-nb.info/standards/elementset/gnd#placeOfBirth
Works
| Title | Sources |
|---|---|
| Biomarkers in paleoenvironmental reconstructions novel applications and data-driven evaluation |
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| Biomineralization capabilities of streptomyces mirabilis P16B-1 insights into struvite and nickel-struvite synthesis and their implications |
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| dark side of primary production in temperate forest soils |
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| Effect of plant inputs and nutrient acquisition strategies on soil microbial community |
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| Environmental Control on Microbial Turnover of Leaf Carbon in Streams - Ecological Function of Phototrophic-Heterotrophic Interactions. |
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| Foliar and soil δ15N values reveal increased nitrogen partitioning among species in diverse grassland communities |
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| Grasshopper herbivory immediately affects element cycling but not export rates in an N‐limited grassland system |
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| Grazing triggers soil carbon loss by altering plant roots and their control on soil microbial community |
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| Growth-dependent stable carbon isotope fractionation by basidiomycete fungi: delta(13)C pattern and physiological process. |
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| How plant diversity impacts the coupled water, nutrient and carbon cycles |
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| How relevant is recalcitrance for the stabilization of organic matter in soils? |
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| Hydrogen isotope ratios of recent lacustrine sedimentary n-alkanes record modern climate variability |
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| Identification of ecosystem-specific markers in terrestrial dissolved organic matter (DOM) by Orbitrap mass spectrometry |
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| Identification of novel 7-methyl and cyclopentanyl branched glycerol dialkyl glycerol tetraethers in lake sediments |
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| Influence of litter diversity on dissolved organic matter release and soil carbon formation in a mixed beech forest. |
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| Isolation of Individual Saturated Fatty Acid Methyl Esters Derived From Groundwater Phospholipids by Preparative High‐Pressure Liquid Chromatography for Compound‐Specific Radiocarbon Analyses |
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| Isotopic evidences for microbiologically mediated and direct C input to soil compounds from three different leaf litters during their decomposition |
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| An isotopic method for testing the influence of leaf litter quality on carbon fluxes during decomposition |
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| Land use driven change in soil pH affects microbial carbon cycling processes |
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| Land use in mountain grasslands alters drought response and recovery of carbon allocation and plant-microbial interactions. |
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| Late quaternary hydrological changes at Tangra Yumco, Tibetan Plateau: a compound-specific isotope-based quantification of lake level changes |
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| Leaf wax n-alkane δD values of field-grown barley reflect leaf water δD values at the time of leaf formation |
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| Mangrove‐Derived Organic and Inorganic Carbon Exchanges Between the Sinnamary Estuarine System (French Guiana, South America) and Atlantic Ocean |
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| Microbial characteristics of soils on a latitudinal transect in Siberia |
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| The molecular composition of dissolved organic matter in forest soils as a function of pH and temperature |
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| Molecular turnover time of soil organic matter in particle-size fractions of an arable soil. |
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| Nematode grazing increases the allocation of plant-derived carbon to soil bacteria and saprophytic fungi, and activates bacterial species of the rhizosphere |
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| The New 14C Analysis Laboratory in Jena, Germany |
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| A new experimental approach to test why biodiversity effects strengthen as ecosystems age |
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| Old-growth forests : function, fate, and value |
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| An optimal defense strategy for phenolic glycoside production in Populus trichocarpa--isotope labeling demonstrates secondary metabolite production in growing leaves |
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| ORCHIDEE-SOM: modeling soil organic carbon (SOC) and dissolved organic carbon (DOC) dynamics along vertical soil profiles in Europe |
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| Organic carbon sequestration in earthworm burrows |
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| Organic matter quality structures benthic fatty acid patterns and the abundance of fungi and bacteria in temperate lakes |
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| Oxygen isotope ratios of sedimentary biogenic silica reflect the European transcontinental climate gradient |
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| Persistence of dissolved organic matter explained by molecular changes during its passage through soil |
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| Phosphorus Release from Mineral Soil by Acid Hydrolysis: Method Development, Kinetics, and Plant Community Composition Effects |
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| Pinus sylvestris switches respiration substrates under shading but not during drought |
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| Plant diversity and community age stabilize ecosystem multifunctionality |
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| Plant diversity effects on aboveground and belowground N pools in temperate grassland ecosystems: Development in the first 5 years after establishment |
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| Plant diversity enhances production and downward transport of biodegradable dissolved organic matter |
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| Plant diversity increases soil microbial activity and soil carbon storage |
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| Plant diversity shapes microbe-rhizosphere effects on P mobilisation from organic matter in soil |
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| Plant species diversity affects infiltration capacity in an experimental grassland through changes in soil properties |
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| Plant species richness and functional groups have different effects on soil water content in a decade-long grassland experiment |
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| Plants with arbuscular mycorrhizal fungi efficiently acquire Nitrogen from substrate additions by shaping the decomposer community composition and their net plant carbon demand |
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| Possible mechanisms underlying abundance and diversity responses of nematode communities to plant diversity |
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| Preparation of starch and soluble sugars of plant material for the analysis of carbon isotope composition: a comparison of methods |
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| Production of constitutive and induced secondary metabolites is coordinated with growth and storage in Norway spruce saplings |
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| Rapid northward shift of the Indian Monsoon on the Tibetan Plateau at the end of the Little Ice Age |
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| Reconstructing C 3 and C 4 vegetation cover using n -alkane carbon isotope ratios in recent lake sediments from Cameroon, Western Central Africa |
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| Reconstruction of palaeohydrological conditions in a lagoon during the 2nd Zechstein cycle through simultaneous use of ?D values of individual n-alkanes and ?18O and ?13C values of carbonates |
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| Reconstruction of the Late Holocene climate and environmental history from North Bolgoda Lake, Sri Lanka, using lipid biomarkers and pollen records |
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| Relative contribution of foliar and fine root pine litter to the molecular composition of soil organic matter after in situ degradation |
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| Reply to: Plant traits alone are good predictors of ecosystem properties when used carefully |
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| The results of biodiversity-ecosystem functioning experiments are realistic |
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| Rhizosphere activity in an old-growth forest reacts rapidly to changes in soil moisture and shapes whole-tree carbon allocation |
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| Rhizosphere bacterial carbon turnover is higher in nucleic acids than membrane lipids: implications for understanding soil carbon cycling |
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| Rhizospheric influence on soil respiration and decomposition in a temperate Norway spruce stand |
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| The role of biodiversity for element cycling and trophic interactions: an experimental approach in a grassland community |
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| Root chemistry and soil fauna, but not soil abiotic conditions explain the effects of plant diversity on root decomposition |
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| Seasonal changes in the soil microbial community in a grassland plant diversity gradient four years after establishment |
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| Seasonal drought reduces microbial diversity and functional richness in the Amazon |
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| Seasonal Patterns of Dominant Microbes Involved in Central Nutrient Cycles in the Subsurface |
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| Significant seasonal variation in the hydrogen isotopic composition of leaf-wax lipids for two deciduous tree ecosystems (Fagus sylvativa and Acerpseudoplatanus) |
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| Simultaneous determination of the quantity and isotopic signature of dissolved organic matter from soil water using high-performance liquid chromatography/isotope ratio mass spectrometry |
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| Soil-carbon preservation through habitat constraints and biological limitations on decomposer activity |
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| Soil Fungal:Bacterial Ratios Are Linked to Altered Carbon Cycling |
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| Soil microbial carbon turnover decreases with increasing molecular size |
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| Soil organic matter dynamics: a biological perspective derived from the use of compound-specific isotopes studies |
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| Source- and substrate-specific export of dissolved organic matter from permafrost-dominated forested watershed in central Siberia |
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| Special Issue dedicated to Professor Hanns-Ludwig Schmidt on the occasion of his 85th birthday |
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| Standardized protocols and procedures can precisely and accurately quantify non-structural carbohydrates |
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| Storage and stability of organic matter and fossil carbon in a Luvisol and Phaeozem with continuous maize cropping: A synthesis |
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| Storage of carbon reserves in spruce trees is prioritized over growth in the face of carbon limitation |
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| Towards a data-driven understanding of dissolved organic matter in the critical zone |
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| Trace element variability in single ostracod valves as a proxy for hydrochemical change in Nam Co, central Tibet, during the Holocene |
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| Tracking the autochthonous carbon transfer in stream biofilm food webs |
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| Variable effects of nitrogen additions on the stability and turnover of soil carbon |
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| Winter ecology of a subalpine grassland: Effects of snow removal on soil respiration, microbial structure and function |
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| δD values of individual n-alkanes from terrestrial plants along a climatic gradient – Implications for the sedimentary biomarker record |
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