| scholarly article | Q13442814 |
| P356 | DOI | 10.1007/S11104-017-3252-7 |
| P50 | author | Nigel T. Roulet | Q57263712 |
| P2093 | author name string | Zheng Wang | |
| P2860 | cites work | Degradation changes stable carbon isotope depth profiles in palsa peatlands | Q57236560 |
| Stable carbon isotopes as indicators for environmental change in palsa peats | Q57236584 | ||
| Source- and substrate-specific export of dissolved organic matter from permafrost-dominated forested watershed in central Siberia | Q57250159 | ||
| Estimated stocks of circumpolar permafrost carbon with quantified uncertainty ranges and identified data gaps | Q57263661 | ||
| Long-term CO2 production following permafrost thaw | Q57263675 | ||
| The Limits to Peat Bog Growth | Q57379371 | ||
| Vulnerability of high-latitude soil organic carbon in North America to disturbance | Q58078736 | ||
| Environmental change in the Great Whale River region, Hudson Bay: Five decades of multidisciplinary research by Centre d'études nordiques (CEN) | Q58192234 | ||
| Dissolved Organic Carbon in Alaskan Boreal Forest: Sources, Chemical Characteristics, and Biodegradability | Q58240280 | ||
| Vegetation and climate controls on potential CO2, DOC and DON production in northern latitude soils | Q58240300 | ||
| Moisture modulates rhizosphere effects on C decomposition in two different soil types | Q58264988 | ||
| Dissolved organic carbon and total dissolved nitrogen production by boreal soils and litter: the role of flooding, oxygen concentration, and temperature | Q58412805 | ||
| Effects of permafrost and hydrology on the composition and transport of dissolved organic carbon in a subarctic peatland complex | Q58412832 | ||
| Modeling Northern Peatland Decomposition and Peat Accumulation | Q58412912 | ||
| Temperature sensitivity of organic matter decomposition of permafrost-region soils during laboratory incubations | Q58653380 | ||
| Dissolved organic matter in small streams along a gradient from discontinuous to continuous permafrost | Q58816520 | ||
| Changes in properties of soil-derived dissolved organic matter induced by biodegradation | Q58816526 | ||
| Carbon respiration from subsurface peat accelerated by climate warming in the subarctic | Q59072344 | ||
| Changes in peat chemistry associated with permafrost thaw increase greenhouse gas production | Q28658270 | ||
| Permafrost Thaw Accelerates in Boreal Peatlands During Late-20th Century Climate Warming | Q29037934 | ||
| Thawing permafrost increases old soil and autotrophic respiration in tundra: partitioning ecosystem respiration using δ(13) C and ∆(14) C. | Q30601394 | ||
| Temperature and peat type control CO2 and CH4 production in Alaskan permafrost peats. | Q30774891 | ||
| Stoichiometry and temperature sensitivity of methanogenesis and CO2 production from saturated polygonal tundra in Barrow, Alaska | Q30859492 | ||
| Evaluation of specific ultraviolet absorbance as an indicator of the chemical composition and reactivity of dissolved organic carbon | Q30883289 | ||
| Decadal warming causes a consistent and persistent shift from heterotrophic to autotrophic respiration in contrasting permafrost ecosystems | Q30978993 | ||
| Similar response of labile and resistant soil organic matter pools to changes in temperature | Q30979879 | ||
| The effect of permafrost thaw on old carbon release and net carbon exchange from tundra | Q33455418 | ||
| Methane emissions from wetlands: biogeochemical, microbial, and modeling perspectives from local to global scales. | Q34625115 | ||
| Temperature response of litter and soil organic matter decomposition is determined by chemical composition of organic material | Q34888750 | ||
| Climate change and the permafrost carbon feedback. | Q35597913 | ||
| Ancient low-molecular-weight organic acids in permafrost fuel rapid carbon dioxide production upon thaw | Q36300451 | ||
| Microbial stress-response physiology and its implications for ecosystem function | Q39436356 | ||
| Nutrient-specific solubility patterns of leaf litter across 41 lowland tropical woody species | Q39439067 | ||
| Biodegradability of fractions of dissolved organic carbon leached from decomposing leaf litter | Q43320702 | ||
| Long-term warming restructures Arctic tundra without changing net soil carbon storage | Q48243346 | ||
| Experimental warming shows that decomposition temperature sensitivity increases with soil organic matter recalcitrance. | Q51677780 | ||
| Rapid turnover of DOC in temperate forests accounts for increased CO2 production at elevated temperatures. | Q51704632 | ||
| Soil organic carbon pools in the northern circumpolar permafrost region | Q55894469 | ||
| Accelerated thawing of subarctic peatland permafrost over the last 50 years | Q56004170 | ||
| Soil-carbon response to warming dependent on microbial physiology | Q56942726 | ||
| Warming alters potential enzyme activity but precipitation regulates chemical transformations in grass litter exposed to simulated climatic changes | Q56959108 | ||
| Modeling the effects of temperature and moisture on soil enzyme activity: Linking laboratory assays to continuous field data | Q56959161 | ||
| Vulnerability of Permafrost Carbon to Climate Change: Implications for the Global Carbon Cycle | Q57017549 | ||
| On the Temperature Dependence of Soil Respiration | Q57199933 | ||
| P433 | issue | 1-2 | |
| P921 | main subject | permafrost | Q179918 |
| peatland | Q36449705 | ||
| P1104 | number of pages | 20 | |
| P304 | page(s) | 197-216 | |
| P577 | publication date | 2017-04-11 | |
| P1433 | published in | Plant and Soil | Q2798768 |
| P1476 | title | Comparison of plant litter and peat decomposition changes with permafrost thaw in a subarctic peatland | |
| P478 | volume | 417 |
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