Publication Index

1. A call for international soil experiment networks for studying, predicting, and managing global change impacts

2. A comment on “Appropriate experimental ecosystem warming methods by ecosystem, objective, and practicality” by Aronson and McNulty

3. A comprehensive data acquisition and management system for an ecosystem-scale peatland warming and elevated CO2 experiment

4. A method for experimental heating of intact soil profiles for application to climate change experiments

5. Across-model spread and shrinking in predicting peatland carbon dynamics under global change.

6. Advancing global change biology through experimental manipulations: Where have we been and where might we go?

7. Air Flow and Heat Transfer in a Temperature-Controlled Open Top Enclosure

8. An Integrative Model for Soil Biogeochemistry and Methane Processes. II: Warming and Elevated CO2 Effects on Peatland CH4 Emissions

9. An Integrative Model for Soil Biogeochemistry and Methane Processes: I. Model Structure and Sensitivity Analysis

10. An Integrative Model for Soil Biogeochemistry and Methane Processes: I. Model Structure and Sensitivity Analysis

11. Anaerobic oxidation of methane mitigates net methane production and responds to long-term experimental warming in a northern bog.

12. Attaining whole-ecosystem warming using air and deep-soil heating methods with an elevated CO<sub>2</sub> atmosphere

13. Biophysical drivers of seasonal variability in Sphagnum gross primary production in a northern temperate bog

14. Boreal conifers maintain carbon uptake with warming despite failure to track optimal temperatures.

15. Borg extrachromosomal elements of methane-oxidizing archaea have conserved and expressed genetic repertoires.

16. Can Sphagnum leachate chemistry explain differences in anaerobic decomposition in peatlands?

17. Characterizing Peatland Microtopography Using Gradient and Microform-Based Approaches

18. Climate drivers alter nitrogen availability in surface peat and decouple N2 fixation from CH4 oxidation in the Sphagnum moss microbiome.

19. Climate warming and elevated CO2 alter peatland soil carbon sources and stability.

20. Compositional stability of peat in ecosystem-scale warming mesocosms

21. Constraints on microbial communities, decomposition and methane production in deep peat deposits

22. Deciphering the shifting role of intrinsic and extrinsic drivers on moss decomposition in peatlands over a 5‐year period

23. Deep peat warming increases surface methane and carbon dioxide emissions in a black spruce‐dominated ombrotrophic bog

24. Defining the Sphagnum Core Microbiome across the North American Continent Reveals a Central Role for Diazotrophic Methanotrophs in the Nitrogen and Carbon Cycles of Boreal Peatland Ecosystems

25. Divergent species‐specific impacts of whole ecosystem warming and elevated CO2 on vegetation water relations in an ombrotrophic peatland

26. Divide and conquer: Using RhizoVision Explorer to aggregate data from multiple root scans using image concatenation and statistical methods.

27. Dynamic Vertical Profiles of Peat Porewater Chemistry in a Northern Peatland

28. Ecosystem warming extends vegetation activity but heightens vulnerability to cold temperatures

29. Elevated temperature alters microbial communities, but not decomposition rates, during 3 years of in situ peat decomposition.

30. Evaluating alternative ebullition models for predicting peatland methane emission and its pathways via data–model fusion

31. Evaluating the E3SM land model version 0 (ELMv0) at a temperate forest site using flux and soil water measurements

32. Experimental warming alters the community composition, diversity, and N2 fixation activity of peat moss (Sphagnum fallax) microbiomes

33. Experimental whole-ecosystem warming enables novel estimation of snow cover and depth sensitivities to temperature, and quantification of the snow-albedo feedback effect.

34. Experimental whole‐ecosystem warming enables novel estimation of snow cover and depth sensitivities to temperature, and quantification of the snow‐albedo feedback effect.

35. Extending a land-surface model with Sphagnum moss to simulate responses of a northern temperate bog to whole ecosystem warming and elevated CO2

36. Fine-root growth in a forested bog is seasonally dynamic, but shallowly distributed in nutrient-poor peat

37. Forecasting Responses of a Northern Peatland Carbon Cycle to Elevated CO2 and a Gradient of Experimental Warming

38. Forest phenology and a warmer climate - growing season extension in relation to climatic provenance

39. From systems biology to photosynthesis and whole-plant physiology

40. Gaseous mercury fluxes in peatlands and the potential influence of climate change

41. Habitat‐adapted microbial communities mediate Sphagnum peatmoss resilience to warming

42. High-throughput Fluorometric Measurement of Potential Soil Extracellular Enzyme Activities

43. High‐resolution minirhizotrons advance our understanding of root‐fungal dynamics in an experimentally warmed peatland

44. Host species–microbiome interactions contribute to Sphagnum moss growth acclimation to warming.

45. Hydrogenation of organic matter as a terminal electron sink sustains high CO2:CH4 production ratios during anaerobic decomposition

46. Hydrological feedbacks on peatland CH4 emission under warming and elevated CO2: A modeling study

47. Identification of shared viral sequences in peat moss metagenomes reveals elements of a possible Sphagnum core virome.

48. Incorporating Microtopography in a Land Surface Model and Quantifying the Effect on the Carbon Cycle

49. Intermediate-scale community-level flux of CO2 and CH4 in a Minnesota peatland: putting the SPRUCE project in a global context

50. Interrelationships among methods of estimating microbial biomass across multiple soil orders and biomes.

51. Large-scale experimental warming reduces soil faunal biodiversity through peatland drying

52. Long-term carbon and nitrogen dynamics at SPRUCE revealed through stable isotopes in peat profiles

53. Massive peatland carbon banks vulnerable to rising temperatures

54. Melanin mitigates the accelerated decay of mycorrhizal necromass with peatland warming

55. Methylotrophic methanogenesis in Sphagnum-dominated peatland soils

56. Microbial Community Stratification Linked to Utilization of Carbohydrates and Phosphorus Limitation in a Boreal Peatland at Marcell Experimental Forest, Minnesota, USA

57. Microbial Metabolic Potential for Carbon Degradation and Nutrient (Nitrogen and Phosphorus) Acquisition in an Ombrotrophic Peatland

58. Modeling the hydrology and physiology of Sphagnum moss in a northern temperate bog.

59. Molybdenum-Based Diazotrophy in a Sphagnum Peatland in Northern Minnesota

60. Near-real-time environmental monitoring and large-volume data collection over slow communication links

61. Needle age and season influence photosynthetic temperature response and total annual carbon uptake in mature Picea mariana trees

62. Nitrogen and phosphorus cycling in an ombrotrophic peatland: a benchmark for assessing change

63. Nitrogen and phosphorus cycling in an ombrotrophic peatland: a benchmark for assessing change

64. Northern peatland microbial communities exhibit resistance to warming and acquire electron acceptors from soil organic matter.

65. Novel climates reverse carbon uptake of atmospherically dependent epiphytes: Climatic constraints on the iconic boreal forest lichen Evernia mesomorpha

66. Novel metabolic interactions and environmental conditions mediate the boreal peatmoss-cyanobacteria mutualism

67. Organic matter transformation in the peat column at Marcell Experimental Forest: Humification and vertical stratification

68. Peatland plant community changes in annual production and composition through 8 years of warming manipulations under ambient and elevated CO2 atmospheres.

69. Peatland warming influences the abundance and distribution of branched tetraether lipids: Implications for temperature reconstruction.

70. Peatland warming strongly increases fine-root growth

71. Photosynthetic and Respiratory Responses of Two Bog Shrub Species to Whole Ecosystem Warming and Elevated CO2 at the Boreal-Temperate Ecotone

72. Photosynthetic capacity in middle-aged larch and spruce acclimates independently to experimental warming and elevated CO2.

73. Predation by a ciliate community mediates temperature and nutrient effects on a peatland prey prokaryotic community.

74. Radiocarbon Analyses Quantify Peat Carbon Losses With Increasing Temperature in a Whole Ecosystem Warming Experiment

75. Rapid loss of an ecosystem engineer: Sphagnum decline in an experimentally warmed bog

76. Rapid Net Carbon Loss From a Whole‐Ecosystem Warmed Peatland

77. Realized ecological forecast through an interactive Ecological Platform for Assimilating Data (EcoPAD, v1.0) into models

78. Representing northern peatland microtopography and hydrology within the Community Land Model

79. Responses of vascular plant fine roots and associated microbial communities to whole-ecosystem warming and elevated CO2 in northern peatlands

80. Responses of vascular plant fine roots and associated microbial communities to whole-ecosystem warming and elevated CO2 in northern peatlands.

81. Review of the influence of climate change on the hydrologic cycling and gaseous fluxes of mercury in Boreal peatlands: Implications for restoration.

82. Role of Ester Sulfate and Organic Disulfide in Mercury Methylation in Peatland Soils

83. Seasonal patterns of nonstructural carbohydrate reserves in four woody boreal species

84. Shading contributes to Sphagnum decline in response to warming.

85. Simulated projections of boreal forest peatland ecosystem productivity are sensitive to observed seasonality in leaf physiology

86. Simulation of carbon cycling, including dissolved organic carbon transport, in forest soil locally enriched with 14C

87. Small differences in ombrotrophy control regional-scale variation in methane cycling among Sphagnum-dominated peatlands

88. Soil metabolome response to whole-ecosystem warming at the Spruce and Peatland Responses under Changing Environments experiment

89. Soil thermal dynamics, snow cover, and frozen depth under five temperature treatments in an ombrotrophic bog: Constrained forecast with data assimilation

90. Sphagnum physiology in the context of changing climate: emergent influences of genomics, modelling and host–microbiome interactions on understanding ecosystem function

91. Springtime Drought Shifts Carbon Partitioning of Recent Photosynthates in 10-Year Old Picea mariana Trees, Causing Restricted Canopy Development

92. Stability of peatland carbon to rising temperatures

93. Temperature and CO2 interactively drive shifts in the compositional and functional structure of peatland protist communities.

94. Temperature and CO2 interactively drive shifts in the compositional and functional structure of peatland protist communities.

95. Temporal and Spatial Variation in Peatland Carbon Cycling and Implications for Interpreting Responses of an Ecosystem-Scale Warming Experiment

96. The challenging but unique eco-evolutionary aspects of Sphagnum moss.

97. The Ecology Underground coalition: building a collaborative future of belowground ecology and ecologists

98. The response of boreal peatland community composition and NDVI to hydrologic change, warming, and elevated carbon dioxide

99. The Sphagnum Genome Project: A New Model for Ecological and Evolutionary Genomics

100. The Sphagnum microbiome: new insights from an ancient plant lineage

101. The stable isotopes of natural waters at the Marcell Experimental Forest

102. The stable isotopes of natural waters at the Marcell Experimental Forest

103. Thermal acclimation of plant photosynthesis and autotrophic respiration in a northern peatland.

104. Uncertainty in Peat Volume and Soil Carbon Estimated Using Ground‐Penetrating Radar and Probing

105. Using long-term data from a whole ecosystem warming experiment to identify best spring and autumn phenology models.

106. Variation in peatland porewater chemistry over time and space along a bog to fen gradient

107. Vascular plant species response to warming and elevated carbon dioxide in a boreal peatland

108. Vertical Stratification of Peat Pore Water Dissolved Organic Matter Composition in a Peat Bog in Northern Minnesota

109. Warming and elevated CO ₂ promote rapid incorporation and degradation of plant‐derived organic matter in an ombrotrophic peatland

110. Warming and elevated CO2 induced shifts in carbon partitioning and lipid composition within an ombrotrophic bog plant community.

111. Warming drives a ‘hummockification’ of microbial communities associated with decomposing mycorrhizal fungal necromass in peatlands

112. Warming induces divergent stomatal dynamics in co‐occurring boreal trees

113. Warming response of peatland CO2 sink is sensitive to seasonality in warming trends

114. Warming Stimulates Iron-Mediated Carbon and Nutrient Cycling in Mineral-Poor Peatlands

115. Whole-Ecosystem Warming Increases Plant-Available Nitrogen and Phosphorus in an Ombrotrophic Bog