| scholarly article | Q13442814 |
| P819 | ADS bibcode | 2007Sci...318..633W |
| P356 | DOI | 10.1126/SCIENCE.1142924 |
| P698 | PubMed publication ID | 17962561 |
| P5875 | ResearchGate publication ID | 5882548 |
| P50 | author | F. Stuart Chapin III | Q5424051 |
| Sergey Zimov | Q7454139 | ||
| Guido Grosse | Q42657013 | ||
| P2093 | author name string | M E Edwards | |
| K M Walter | |||
| P2860 | cites work | Methane bubbling from Siberian thaw lakes as a positive feedback to climate warming | Q24289337 |
| Ice record of delta13C for atmospheric CH4 across the Younger Dryas-Preboreal transition | Q28260007 | ||
| Late Quaternary atmospheric CH4 isotope record suggests marine clathrates are stable | Q28296516 | ||
| Abrupt climate change at the end of the last glacial period inferred from trapped air in polar Ice | Q30583475 | ||
| Climate change. Permafrost and the global carbon budget | Q31044392 | ||
| Siberian peatlands a net carbon sink and global methane source since the early Holocene | Q34290251 | ||
| Rapid early development of circumarctic peatlands and atmospheric CH4 and CO2 variations | Q46605636 | ||
| Timing of abrupt climate change at the end of the Younger Dryas interval from thermally fractionated gases in polar ice | Q55921479 | ||
| North Siberian Lakes: A Methane Source Fueled by Pleistocene Carbon | Q56679630 | ||
| Changes in the atmospheric CH4gradient between Greenland and Antarctica during the Last Glacial and the transition to the Holocene | Q58265569 | ||
| PALEOCLIMATE:"Frozen" Methane Escapes from the Sea Floor | Q58265573 | ||
| Synchronous changes in atmospheric CH4 and Greenland climate between 40 and 8 kyr BP | Q58265646 | ||
| P433 | issue | 5850 | |
| P407 | language of work or name | English | Q1860 |
| P921 | main subject | lake | Q23397 |
| methane | Q37129 | ||
| thermokarst | Q1367339 | ||
| deglaciation | Q3707848 | ||
| P304 | page(s) | 633-6 | |
| P577 | publication date | 2007-10-26 | |
| P1433 | published in | Science | Q192864 |
| P1476 | title | Thermokarst lakes as a source of atmospheric CH4 during the last deglaciation | |
| P478 | volume | 318 |
| Q46431488 | 14CH4 measurements in Greenland ice: investigating last glacial termination CH4 sources. |
| Q56394989 | 21st-century modeled permafrost carbon emissions accelerated by abrupt thaw beneath lakes |
| Q45000792 | A shift of thermokarst lakes from carbon sources to sinks during the Holocene epoch. |
| Q57494329 | Basin evolution and palaeoenvironmental variability of the thermokarst lake El'gene-Kyuele, Arctic Siberia |
| Q43532575 | Changing boreal methane sources and constant biomass burning during the last termination |
| Q35597913 | Climate change and the permafrost carbon feedback. |
| Q51426476 | Climate science: cold carbon storage. |
| Q57235195 | Cryogenic Displacement and Accumulation of Biogenic Methane in Frozen Soils |
| Q57070771 | Deglacial mobilization of pre-aged terrestrial carbon from degrading permafrost |
| Q57662558 | Environmental feedbacks in temperate aquatic ecosystems under global change: why do we need to consider chemical stressors? |
| Q57235196 | Estimation and Sensitivity of Carbon Storage in Permafrost of North-Eastern Yakutia |
| Q58388775 | Evidence of multiple thermokarst lake generations from an 11 800-year-old permafrost core on the northern Seward Peninsula, Alaska |
| Q58264050 | Expansion rate and geometry of floating vegetation mats on the margins of thermokarst lakes, northern Seward Peninsula, Alaska, USA |
| Q58078600 | Expert assessment of vulnerability of permafrost carbon to climate change |
| Q59095940 | Extensive loss of past permafrost carbon but a net accumulation into present-day soils |
| Q58388840 | Fossil organic matter characteristics in permafrost deposits of the northeast Siberian Arctic |
| Q34794852 | Glacial demise and methane's rise |
| Q38695401 | Glacial/interglacial wetland, biomass burning, and geologic methane emissions constrained by dual stable isotopic CH4 ice core records |
| Q33615699 | Hydrogen isotopes preclude marine hydrate CH4 emissions at the onset of Dansgaard-Oeschger events |
| Q58261713 | Impacts of disturbance on the terrestrial carbon budget of North America |
| Q58053636 | Independent variations of CH4 emissions and isotopic composition over the past 160,000 years |
| Q58650641 | Is the subarctic landscape still a carbon sink? Evidence from a detailed catchment balance |
| Q31060380 | Isotopic insights into methane production, oxidation, and emissions in Arctic polygon tundra |
| Q28589195 | Massive remobilization of permafrost carbon during post-glacial warming |
| Q58101939 | Methane emissions from permafrost thaw lakes limited by lake drainage |
| Q30601080 | Methane emissions from rice paddies natural wetlands, and lakes in China: synthesis and new estimate |
| Q56141063 | Methane production and bubble emissions from arctic lakes: Isotopic implications for source pathways and ages |
| Q105426325 | Methane, Monsoons, and Modulation of Millennial‐Scale Climate |
| Q58388778 | Mid-Wisconsin to Holocene Permafrost and Landscape Dynamics based on a Drained Lake Basin Core from the Northern Seward Peninsula, Northwest Alaska |
| Q38637850 | Minimal geological methane emissions during the Younger Dryas-Preboreal abrupt warming event |
| Q58264080 | Modern thermokarst lake dynamics in the continuous permafrost zone, northern Seward Peninsula, Alaska |
| Q34033724 | Multi-decadal changes in tundra environments and ecosystems: synthesis of the International Polar Year-Back to the Future project (IPY-BTF). |
| Q34721054 | Northern peatland initiation lagged abrupt increases in deglacial atmospheric CH4. |
| Q92157616 | Organic Carbon and Nitrogen Stocks Along a Thermokarst Lake Sequence in Arctic Alaska |
| Q58650131 | Particulate organic carbon and nitrogen export from major Arctic rivers |
| Q30989412 | Permafrost collapse alters soil carbon stocks, respiration, CH4 , and N2O in upland tundra. |
| Q47416595 | Presidential address. Reflections on: our planet and its life, origins, and futures |
| Q46525088 | Rapid carbon loss and slow recovery following permafrost thaw in boreal peatlands |
| Q28752266 | Rapid deglacial and early Holocene expansion of peatlands in Alaska |
| Q57395564 | Reply to ‘Methane and megafauna’ |
| Q72993204 | Response of CO2exchange in a tussock tundra ecosystem to permafrost thaw and thermokarst development |
| Q28660447 | Role of megafauna and frozen soil in the atmospheric CH4 dynamics |
| Q63645528 | Sedimentology and geochemistry of thermokarst ponds in discontinuous permafrost, subarctic Quebec, Canada |
| Q57150855 | Shallow carbon storage in ancient buried thermokarst in the South Kara Sea |
| Q21093481 | Spatial distribution of pingos in northern Asia |
| Q34762371 | The impacts of climate change and human activities on biogeochemical cycles on the Qinghai-Tibetan Plateau |
| Q43105215 | Two metagenomes from late pleistocene northeast siberian permafrost |
| Q58388837 | Using the deuterium isotope composition of permafrost meltwater to constrain thermokarst lake contributions to atmospheric CH4during the last deglaciation |
| Q58388851 | Vulnerability and feedbacks of permafrost to climate change |
| Q57017549 | Vulnerability of Permafrost Carbon to Climate Change: Implications for the Global Carbon Cycle |
| Q58078736 | Vulnerability of high-latitude soil organic carbon in North America to disturbance |
| Q104155994 | Warming-induced destabilization of peat plateau/thermokarst lake complexes |
Search more.