The fate of 13C15N labelled glycine in permafrost and surface soil at simulated thaw in mesocosms from high arctic and subarctic ecosystems

scholarly article by Nynne Marie Rand Ravn et al published 15 July 2017 in Plant and Soil

The fate of 13C15N labelled glycine in permafrost and surface soil at simulated thaw in mesocosms from high arctic and subarctic ecosystems is …
instance of (P31):
scholarly articleQ13442814

External links are
P356DOI10.1007/S11104-017-3322-X

P50authorBo ElberlingQ12303919
Anders MichelsenQ56808970
P2093author name stringNynne Marie Rand Ravn
P2860cites workWarming of subarctic tundra increases emissions of all three important greenhouse gases - carbon dioxide, methane, and nitrous oxide.Q31143266
Quantifying global soil carbon losses in response to warmingQ31146293
Climate change and the permafrost carbon feedback.Q35597913
Microbial control of soil organic matter mineralization responses to labile carbon in subarctic climate change treatmentsQ35968617
Site-dependent N uptake from N-form mixtures by arctic plants, soil microbes and ectomycorrhizal fungiQ46774628
Vascular plant 15N natural abundance in heath and forest tundra ecosystems is closely correlated with presence and type of mycorrhizal fungi in rootsQ48794446
Ecosystem carbon storage in arctic tundra reduced by long-term nutrient fertilization.Q50749197
High arctic heath soil respiration and biogeochemical dynamics during summer and autumn freeze-in - effects of long-term enhanced water and nutrient supply.Q51549302
Amount and timing of permafrost carbon release in response to climate warmingQ55951310
A frozen feast: thawing permafrost increases plant-available nitrogen in subarctic peatlandsQ56964146
Plot-scale evidence of tundra vegetation change and links to recent summer warmingQ57258314
Deeper snow alters soil nutrient availability and leaf nutrient status in high Arctic tundraQ57263649
Estimated stocks of circumpolar permafrost carbon with quantified uncertainty ranges and identified data gapsQ57263661
Long-term CO2 production following permafrost thawQ57263675
Recent dynamics of arctic and sub-arctic vegetationQ58239297
Preferential use of organic nitrogen for growth by a non-mycorrhizal arctic sedgeQ58381015
High Arctic Dry Heath CO2 Exchange During the Early Cold SeasonQ58897154
Nitrogen Uptake During Fall, Winter and Spring Differs Among Plant Functional Groups in a Subarctic Heath EcosystemQ58897177
Effects of shading on photosynthesis, plant organic nitrogen uptake, and root fungal colonization in a subarctic mire ecosystemQ58897291
Glycine uptake in heath plants and soil microbes responds to elevated temperature, CO2 and droughtQ58897295
Ecosystem partitioning of 15N-glycine after long-term climate and nutrient manipulations, plant clipping and addition of labile carbon in a subarctic heath tundraQ58897313
Nitrogen Uptake During One Year in Subarctic Plant Functional Groups and in Microbes After Long-Term Warming and FertilizationQ58897323
Uptake of pulse injected nitrogen by soil microbes and mycorrhizal and non-mycorrhizal plants in a species-diverse subarctic heath ecosystemQ58897358
Significance of cold-season respiration and photosynthesis in a subarctic heath ecosystem in Northern SwedenQ58897406
P433issue1-2
P921main subjectmesocosmQ3333382
permafrostQ179918
P1104number of pages18
P304page(s)201-218
P577publication date2017-07-15
P1433published inPlant and SoilQ2798768
P1476titleThe fate of 13C15N labelled glycine in permafrost and surface soil at simulated thaw in mesocosms from high arctic and subarctic ecosystems
P478volume419

Reverse relations

cites work (P2860)
Q56394959Biogenic volatile release from permafrost thaw is determined by the soil microbial sink
Q64065283Evaluation of an untargeted nano-liquid chromatography-mass spectrometry approach to expand coverage of low molecular weight dissolved organic matter in Arctic soil