47 citations as recorded by crossref.

1. Old carbon reservoirs were not important in the deglacial methane budget M. Dyonisius et al. 10.1126/science.aax0504
2. Excess methane in Greenland ice cores associated with high dust concentrations J. Lee et al. 10.1016/j.gca.2019.11.020
3. A detailed East Asian monsoon history surrounding the ‘Mystery Interval’ derived from three Chinese speleothem records W. Zhang et al. 10.1016/j.yqres.2014.01.010
4. Glacial/interglacial wetland, biomass burning, and geologic methane emissions constrained by dual stable isotopic CH 4 ice core records M. Bock et al. 10.1073/pnas.1613883114
5. Terrestrial methane emissions from the Last Glacial Maximum to the preindustrial period T. Kleinen et al. 10.5194/cp-16-575-2020
6. The penultimate deglaciation: protocol for Paleoclimate Modelling Intercomparison Project (PMIP) phase 4 transient numerical simulations between 140 and 127 ka, version 1.0 L. Menviel et al. 10.5194/gmd-12-3649-2019
7. Panarctic lakes exerted a small positive feedback on early Holocene warming due to deglacial release of methane L. Brosius et al. 10.1038/s43247-023-00930-2
8. Atmospheric Methane: Comparison Between Methane's Record in 2006–2022 and During Glacial Terminations E. Nisbet et al. 10.1029/2023GB007875
9. Impact of an abrupt cooling event on interglacial methane emissions in northern peatlands S. Zürcher et al. 10.5194/bg-10-1963-2013
10. A centrifugal ice microtome for measurements of atmospheric CO<sub>2</sub> on air trapped in polar ice cores B. Bereiter et al. 10.5194/amt-6-251-2013
11. Methane, Monsoons, and Modulation of Millennial‐Scale Climate K. Thirumalai et al. 10.1029/2020GL087613
12. Methane, ethane, and propane production in Greenland ice core samples and a first isotopic characterization of excess methane M. Mühl et al. 10.5194/cp-19-999-2023
13. Limited response of peatland CH<sub>4</sub> emissions to abrupt Atlantic Ocean circulation changes in glacial climates P. Hopcroft et al. 10.5194/cp-10-137-2014
14. N<sub>2</sub>O changes from the Last Glacial Maximum to the preindustrial – Part 1: Quantitative reconstruction of terrestrial and marine emissions using N<sub>2</sub>O stable isotopes in ice cores H. Fischer et al. 10.5194/bg-16-3997-2019
15. Methane emissions from floodplains in the Amazon Basin: challenges in developing a process-based model for global applications B. Ringeval et al. 10.5194/bg-11-1519-2014
16. Bipolar carbon and hydrogen isotope constraints on the Holocene methane budget J. Beck et al. 10.5194/bg-15-7155-2018
17. Evidence for elevated emissions from high‐latitude wetlands contributing to high atmospheric CH4 concentration in the early Holocene Z. Yu et al. 10.1002/gbc.20025
18. Synchronous volcanic eruptions and abrupt climate change ∼17.7 ka plausibly linked by stratospheric ozone depletion J. McConnell et al. 10.1073/pnas.1705595114
19. Continuous methane measurements from a late Holocene Greenland ice core: Atmospheric and in-situ signals R. Rhodes et al. 10.1016/j.epsl.2013.02.034
20. Climatic and insolation control on the high-resolution total air content in the NGRIP ice core O. Eicher et al. 10.5194/cp-12-1979-2016
21. NGRIP CH<sub>4</sub> concentration from 120 to 10 kyr before present and its relation to a δ<sup>15</sup>N temperature reconstruction from the same ice core M. Baumgartner et al. 10.5194/cp-10-903-2014
22. CH<sub>4</sub> and N<sub>2</sub>O fluctuations during the penultimate deglaciation L. Schmidely et al. 10.5194/cp-17-1627-2021
23. Reconstructing the last interglacial at Summit, Greenland: Insights from GISP2 A. Yau et al. 10.1073/pnas.1524766113
24. A 156 kyr smoothed history of the atmospheric greenhouse gases CO<sub>2</sub>, CH<sub>4</sub>, and N<sub>2</sub>O and their radiative forcing P. Köhler et al. 10.5194/essd-9-363-2017
25. Permafrost thawing as a possible source of abrupt carbon release at the onset of the Bølling/Allerød P. Köhler et al. 10.1038/ncomms6520
26. Ice Core Methane Analytical Techniques, Chronology and Concentration History Changes: A Review J. Song 10.3390/su15129346
27. Atmospheric methane variability through the Last Glacial Maximum and deglaciation mainly controlled by tropical sources B. Riddell-Young et al. 10.1038/s41561-023-01332-x
28. Abrupt changes in the global carbon cycle during the last glacial period T. Bauska et al. 10.1038/s41561-020-00680-2
29. The anatomy of past abrupt warmings recorded in Greenland ice E. Capron et al. 10.1038/s41467-021-22241-w
30. Climatic controls on the dynamic lateral expansion of northern peatlands and its potential implication for the ‘anomalous’ atmospheric CH4 rise since the mid-Holocene H. Peng et al. 10.1016/j.scitotenv.2023.168450
31. Climate in phase E. Wolff 10.1038/ngeo2165
32. The relative importance of methane sources and sinks over the Last Interglacial period and into the last glaciation A. Quiquet et al. 10.1016/j.quascirev.2015.01.004
33. Punctuated ASM strengthening in late Heinrich Stadial from speleothem records, southern China Y. Fang et al. 10.1007/s12665-019-8559-7
34. Divergent influences of the Greenland and Antarctica climates on the Asian monsoon during a stadial to interstadial cycle F. Duan et al. 10.1016/j.jseaes.2018.03.019
35. Extensive wetland development in mid-latitude North America during the Bølling–Allerød E. Byun et al. 10.1038/s41561-020-00670-4
36. The role of wetland expansion and successional processes in methane emissions from northern wetlands during the Holocene C. Treat et al. 10.1016/j.quascirev.2021.106864
37. A 3000-yr Annually Laminated Stalagmite Record of the Last Glacial Maximum from Hulu Cave, China F. Duan et al. 10.1016/j.yqres.2015.01.003
38. An ice core record of near-synchronous global climate changes at the Bølling transition J. Rosen et al. 10.1038/ngeo2147
39. Enhanced tropical methane production in response to iceberg discharge in the North Atlantic R. Rhodes et al. 10.1126/science.1262005
40. Evidence for a three-phase sequence during Heinrich Stadial 4 using a multiproxy approach based on Greenland ice core records M. Guillevic et al. 10.5194/cp-10-2115-2014
41. Response of methane emissions from wetlands to the Last Glacial Maximum and an idealized Dansgaard–Oeschger climate event: insights from two models of different complexity B. Ringeval et al. 10.5194/cp-9-149-2013
42. Europe on fire three thousand years ago: Arson or climate? P. Zennaro et al. 10.1002/2015GL064259
43. Tropical vegetation productivity and atmospheric methane over the last 40,000 years from model simulations and stalagmites in Sulawesi, Indonesia C. Krause et al. 10.1017/qua.2023.75
44. Atmospheric methane and nitrous oxide: challenges alongthe path to Net Zero E. Nisbet et al. 10.1098/rsta.2020.0457
45. High-resolution glacial and deglacial record of atmospheric methane by continuous-flow and laser spectrometer analysis along the NEEM ice core J. Chappellaz et al. 10.5194/cp-9-2579-2013
46. Hydrological changes in eastern europe during the last 40,000 yr inferred from biomarkers in Black Sea Sediments F. Rostek & E. Bard 10.1016/j.yqres.2013.07.003
47. Independent variations of CH4 emissions and isotopic composition over the past 160,000 years L. Möller et al. 10.1038/ngeo1922