55 citations as recorded by crossref.

1. Northern Hemisphere forcing of Southern Hemisphere climate during the last deglaciation F. He et al. 10.1038/nature11822
2. Reconstructions of ground surface heat flux variations in the urals from geothermal and meteorological data D. Demezhko & A. Gornostaeva 10.1134/S0001433815070026
3. Delayed CO2 emissions from mid-ocean ridge volcanism as a possible cause of late-Pleistocene glacial cycles P. Huybers & C. Langmuir 10.1016/j.epsl.2016.09.021
4. Time’s arrow in stochastic characterization and simulation of atmospheric and hydrological processes D. Koutsoyiannis 10.1080/02626667.2019.1600700
5. Modeling enhanced firn densification due to strain softening F. Oraschewski & A. Grinsted 10.5194/tc-16-2683-2022
6. The Falkland Islands’ palaeoecological response to millennial‐scale climate perturbations during the Pleistocene–Holocene transition: Implications for future vegetation stability in the southern ocean islands R. Scaife et al. 10.1002/jqs.3150
7. A stratigraphic framework for abrupt climatic changes during the Last Glacial period based on three synchronized Greenland ice-core records: refining and extending the INTIMATE event stratigraphy S. Rasmussen et al. 10.1016/j.quascirev.2014.09.007
8. Atmospheric Temperature and CO2: Hen-Or-Egg Causality? D. Koutsoyiannis & Z. Kundzewicz 10.3390/sci2040083
9. A chironomid-inferred summer temperature reconstruction from subtropical Australia during the last glacial maximum (LGM) and the last deglaciation J. Chang et al. 10.1016/j.quascirev.2015.06.006
10. On Hens, Eggs, Temperatures and CO2: Causal Links in Earth’s Atmosphere D. Koutsoyiannis et al. 10.3390/sci5030035
11. Late Pleistocene–Holocene ground surface heat flux changes reconstructed from borehole temperature data (the Urals, Russia) D. Demezhko & A. Gornostaeva 10.5194/cp-11-647-2015
12. Breakpoint lead-lag analysis of the last deglacial climate change and atmospheric CO2 concentration on global and hemispheric scales Z. Liu et al. 10.1016/j.quaint.2018.05.021
13. Antarctic temperature and CO<sub>2</sub>: near-synchrony yet variable phasing during the last deglaciation J. Chowdhry Beeman et al. 10.5194/cp-15-913-2019
14. Synchronous Change of Atmospheric CO 2 and Antarctic Temperature During the Last Deglacial Warming F. Parrenin et al. 10.1126/science.1226368
15. Reconstruction du climat et de l’environnement des derniers 800 000 ans à partir des carottes de glace – variabilité orbitale et millénaire. A. Landais 10.4000/quaternaire.7664
16. Composition of planktonic foraminifera test-bound organic material and implications for carbon cycle reconstructions T. Paoloni et al. 10.3389/fmars.2023.1237440
17. The temperature–CO<sub>2</sub> climate connection: an epistemological reappraisal of ice-core messages P. Richet 10.5194/hgss-12-97-2021
18. Hydroclimate and vegetation changes in southeastern Amazonia over the past ∼25,000 years L. Reis et al. 10.1016/j.quascirev.2022.107466
19. Where to find 1.5 million yr old ice for the IPICS "Oldest-Ice" ice core H. Fischer et al. 10.5194/cp-9-2489-2013
20. Atmospheric Temperature and CO2: Hen-or-Egg Causality? D. Koutsoyiannis & Z. Kundzewicz 10.3390/sci2030081
21. Late Quaternary climatic and environmental conditions of northern Spain: An isotopic approach based on the mammalian record from La Paloma cave L. Domingo et al. 10.1016/j.palaeo.2015.09.017
22. Atmospheric Temperature and CO2: Hen-or-Egg Causality? D. Koutsoyiannis & Z. Kundzewicz 10.3390/sci2040077
23. Comment on “Synchronous records of pCO2 and Δ14C suggest rapid, ocean-derived pCO2 fluctuations at the onset of Younger Dryas” by Steinthorsdottir et al P. Köhler et al. 10.1016/j.quascirev.2014.09.024
24. Deglacial ice sheet meltdown: orbital pacemaking and CO<sub>2</sub> effects M. Heinemann et al. 10.5194/cp-10-1567-2014
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. Effect of Temperature in Experiments Involving Carbonated Beverages T. Kuntzleman & A. Sturgis 10.1021/acs.jchemed.0c00844
27. Atmospheric Temperature and CO2: Hen-or-Egg Causality? D. Koutsoyiannis & Z. Kundzewicz 10.3390/sci2030072
28. Measuring Quaternary time: A 50‐year perspective J. LOWE & M. WALKER 10.1002/jqs.2764
29. Interpolation methods for Antarctic ice-core timescales: application to Byrd, Siple Dome and Law Dome ice cores T. Fudge et al. 10.5194/cp-10-1195-2014
30. Resilience at the Transition to Agriculture: The Long-Term Landscape and Resource Development at the Aceramic Neolithic Tell Site of Chogha Golan (Iran) S. Riehl et al. 10.1155/2015/532481
31. Leads and Lags at the End of the Last Ice Age E. Brook 10.1126/science.1234239
32. Evaluation of biospheric components in Earth system models using modern and palaeo-observations: the state-of-the-art A. Foley et al. 10.5194/bg-10-8305-2013
33. Interglacials of the last 800,000 years 10.1002/2015RG000482
34. Two-phase change in CO2, Antarctic temperature and global climate during Termination II A. Landais et al. 10.1038/ngeo1985
35. Vegetation and Climate Change in Southwestern Australia During the Last Glacial Maximum J. Sniderman et al. 10.1029/2018GL080832
36. The last termination in the central South Atlantic K. Ljung et al. 10.1016/j.quascirev.2015.07.003
37. Reconstructions of long-term ground surface heat flux changes from deep-borehole temperature data D. Demezhko & A. Gornostaeva 10.1016/j.rgg.2014.11.011
38. Climate Sensitivity to an Increase in the Carbon Dioxide Concentration in the Atmosphere Decreases with an Increase in the Water Vapor Concentration upon Warming H. Abdussamatov 10.1134/S0016793221070021
39. Ice melt, sea level rise and superstorms: evidence from paleoclimate data, climate modeling, and modern observations that 2 °C global warming could be dangerous J. Hansen et al. 10.5194/acp-16-3761-2016
40. Similarities and dissimilarities between the last two deglaciations and interglaciations in the North Atlantic region B. Martrat et al. 10.1016/j.quascirev.2014.06.016
41. A review of the bipolar see–saw from synchronized and high resolution ice core water stable isotope records from Greenland and East Antarctica A. Landais et al. 10.1016/j.quascirev.2015.01.031
42. Multi-proxy constraints on Atlantic circulation dynamics since the last ice age F. Pöppelmeier et al. 10.1038/s41561-023-01140-3
43. Stochastic assessment of temperature–CO₂ causal relationship in climate from the Phanerozoic through modern times D. Koutsoyiannis 10.3934/mbe.2024287
44. Trans-pacific glacial response to the Antarctic Cold Reversal in the southern mid-latitudes E. Sagredo et al. 10.1016/j.quascirev.2018.01.011
45. Antarctic and global climate history viewed from ice cores E. Brook & C. Buizert 10.1038/s41586-018-0172-5
46. Climate reconstructions for the Last Glacial Maximum from a simple cirque glacier in Fiordland, New Zealand E. Moore et al. 10.1016/j.quascirev.2021.107281
47. Causal feedbacks in climate change E. van Nes et al. 10.1038/nclimate2568
48. The WAIS Divide deep ice core WD2014 chronology – Part 1: Methane synchronization (68–31 ka BP) and the gas age–ice age difference C. Buizert et al. 10.5194/cp-11-153-2015
49. Cosmogenic 10Be constraints on deglacial snowline rise in the Southern Alps, New Zealand L. Tielidze et al. 10.1016/j.quascirev.2022.107548
50. Carbon isotope records reveal precise timing of enhanced Southern Ocean upwelling during the last deglaciation G. Siani et al. 10.1038/ncomms3758
51. Changes in monsoon-driven upwelling in the South China Sea over glacial Terminations I and II: a multi-proxy record H. Sadatzki et al. 10.1007/s00531-015-1227-6
52. Antarctic Winds: Pacemaker of Global Warming, Global Cooling, and the Collapse of Civilizations W. Davis & W. Davis 10.3390/cli8110130
53. Unveiling the anatomy of Termination 3 using water and air isotopes in the Dome C ice core, East Antarctica C. Bréant et al. 10.1016/j.quascirev.2019.03.025
54. Siple Dome ice reveals two modes of millennial CO2 change during the last ice age J. Ahn & E. Brook 10.1038/ncomms4723
55. On the gas-ice depth difference (Δdepth) along the EPICA Dome C ice core F. Parrenin et al. 10.5194/cp-8-1239-2012