| P50 | author | David Beerling | Q16404688 |
| | Vincent Gauci | Q56433498 |
| | Stephen Blake | Q57903533 |
| | Jonathan S. Watson | Q58129564 |
| P2093 | author name string | Carl P Boardman | |
| P2860 | cites work | High-resolution carbon dioxide concentration record 650,000-800,000 years before present | Q28280161 |
| | Carbon starvation in glacial trees recovered from the La Brea tar pits, southern California | Q28770036 |
| | Atmospheric oxidation capacity sustained by a tropical forest | Q29353925 |
| | Tropical temperature variations since 20,000 years ago: modulating interhemispheric climate change | Q31123320 |
| | Effects of temperature on the diversity and community structure of known methanogenic groups and other archaea in high Arctic peat. | Q31142211 |
| | Orbital and millennial-scale features of atmospheric CH4 over the past 800,000 years | Q31155450 |
| | Methanogen communities and Bacteria along an ecohydrological gradient in a northern raised bog complex. | Q33223176 |
| | Late Holocene methane rise caused by orbitally controlled increase in tropical sources | Q34162549 |
| | Root Exudation and Rhizosphere Biology | Q34196780 |
| | Export of dissolved organic carbon from peatlands under elevated carbon dioxide levels | Q34331967 |
| | Hydrogenotrophic methanogenesis by moderately acid-tolerant methanogens of a methane-emitting acidic peat | Q34877438 |
| | The role of terrestrial plants in limiting atmospheric CO(2) decline over the past 24 million years | Q34990248 |
| | Pathways for methanogenesis and diversity of methanogenic archaea in three boreal peatland ecosystems | Q41787144 |
| | shift from acetoclastic to H2-dependent methanogenesis in a west Siberian peat bog at low pH values and isolation of an acidophilic Methanobacterium strain | Q41971709 |
| | Changing boreal methane sources and constant biomass burning during the last termination | Q43532575 |
| | Trends in Stomatal Density and 13C/12C Ratios of Pinus flexilis Needles During Last Glacial-Interglacial Cycle | Q47339179 |
| | Effects of elevated CO2 on fen peat biogeochemistry. | Q51342334 |
| | Shifts of soil enzyme activities in wetlands exposed to elevated CO(2). | Q51559975 |
| | The role of Sphagnum mosses in the methane cycling of a boreal mire. | Q51620278 |
| | Quantifying the effect of vegetation dynamics on the climate of the Last Glacial Maximum | Q57089826 |
| | Methanotrophic symbionts provide carbon for photosynthesis in peat bogs | Q57139392 |
| | A process-based model to derive methane emissions from natural wetlands | Q57242397 |
| | Leaf isoprene emission rate as a function of atmospheric CO2concentration | Q57262292 |
| | Climate and CO2 controls on global vegetation distribution at the last glacial maximum: analysis based on palaeovegetation data, biome modelling and palaeoclimate simulations | Q57264440 |
| | Growth responses of African savanna trees implicate atmospheric [CO2] as a driver of past and current changes in savanna tree cover | Q57264609 |
| | Methane fluxes from three ecosystems in tropical peatland of Sarawak, Malaysia | Q57267447 |
| | Global prevalence of methane oxidation by symbiotic bacteria in peat-moss ecosystems | Q57273415 |
| | Wetland methane emissions during the Last Glacial Maximum estimated from PMIP2 simulations: Climate, vegetation, and geographic controls | Q57518976 |
| | The effects of glacial atmospheric CO2 concentrations and climate on isoprene emissions by vascular plants | Q58071094 |
| | The ice age methane budget | Q58071098 |
| | The role of endophytic methane-oxidizing bacteria in submerged Sphagnum in determining methane emissions of Northeastern Siberian tundra | Q58101948 |
| | Changes in the atmospheric CH4gradient between Greenland and Antarctica during the Last Glacial and the transition to the Holocene | Q58265569 |
| | Changes in the atmospheric CH4gradient between Greenland and Antarctica during the Holocene | Q58265616 |
| | Role of methane and biogenic volatile organic compound sources in late glacial and Holocene fluctuations of atmospheric methane concentrations | Q58397246 |
| | Belowground carbon turnover in a temperate ombrotrophic bog | Q58412870 |
| | Effects of elevated CO2and N deposition on CH4emissions from European mires | Q58841370 |
| | Increase in C3 plant water-use efficiency and biomass over Glacial to present C02 concentrations | Q59072146 |
| | Stimulation of methane emission by carbon dioxide enrichment of marsh vegetation | Q59076802 |
| | Primary production control of methane emission from wetlands | Q59090721 |
| P433 | issue | 4 | |
| P407 | language of work or name | English | Q1860 |
| P921 | main subject | methane | Q37129 |
| P1104 | number of pages | 14 | |
| P304 | page(s) | 898-911 | |
| P577 | publication date | 2011-09-07 | |
| P1433 | published in | New Phytologist | Q13548580 |
| P1476 | title | Contrasting wetland CH4 emission responses to simulated glacial atmospheric CO2 in temperate bogs and fens | |
| P478 | volume | 192 | |