66 citations as recorded by crossref.

1. Burial-nutrient feedbacks amplify the sensitivity of carbon dioxide to changes in organic matter remineralisation R. Roth et al. 10.5194/esdd-5-473-2014
2. Atlantic Meridional Overturning Circulation and δ 13 C Variability During the Last Interglacial A. Kessler et al. 10.1029/2019PA003818
3. Coupled climate–carbon cycle simulation of the Last Glacial Maximum atmospheric CO<sub>2</sub> decrease using a large ensemble of modern plausible parameter sets K. Kemppinen et al. 10.5194/cp-15-1039-2019
4. North Atlantic ventilation of “southern-sourced” deep water in the glacial ocean E. Kwon et al. 10.1029/2011PA002211
5. Controls on the spatial distribution of oceanic δ<sup>13</sup>C<sub>DIC</sub> P. Holden et al. 10.5194/bg-10-1815-2013
6. Timing and magnitude of Southern Ocean sea ice/carbon cycle feedbacks K. Stein et al. 10.1073/pnas.1908670117
7. Variable C∕P composition of organic production and its effect on ocean carbon storage in glacial-like model simulations M. Ödalen et al. 10.5194/bg-17-2219-2020
8. Deciphering the spatio-temporal complexity of climate change of the last deglaciation: a model analysis D. Roche et al. 10.5194/cp-7-591-2011
9. Sea ice contribution to the air–sea CO2 exchange in the Arctic and Southern Oceans R. Søren et al. 10.1111/j.1600-0889.2011.00571.x
10. Including a full carbon cycle into the <i>i</i>LOVECLIM model (v1.0) N. Bouttes et al. 10.5194/gmdd-7-3937-2014
11. Inorganic Carbon and p CO 2 Variability During Ice Formation in the Beaufort Gyre of the Canada Basin M. DeGrandpre et al. 10.1029/2019JC015109
12. Impact of oceanic processes on the carbon cycle during the last termination N. Bouttes et al. 10.5194/cpd-7-1887-2011
13. Marine productivity response to Heinrich events: a model-data comparison V. Mariotti et al. 10.5194/cpd-8-557-2012
14. Connecting Antarctic sea ice to deep-ocean circulation in modern and glacial climate simulations A. Marzocchi & M. Jansen 10.1002/2017GL073936
15. High-resolution mineral dust and sea ice proxy records from the Talos Dome ice core S. Schüpbach et al. 10.5194/cp-9-2789-2013
16. Role of sea ice in global biogeochemical cycles: emerging views and challenges M. Vancoppenolle et al. 10.1016/j.quascirev.2013.04.011
17. On the Sensitivity of the Devonian Climate to Continental Configuration, Vegetation Cover, Orbital Configuration, CO 2 Concentration, and Insolation J. Brugger et al. 10.1029/2019PA003562
18. Quaternary glaciations: from observations to theories D. Paillard 10.1016/j.quascirev.2014.10.002
19. A coupled model for carbon and radiocarbon evolution during the last deglaciation V. Mariotti et al. 10.1002/2015GL067489
20. Global cooling linked to increased glacial carbon storage via changes in Antarctic sea ice A. Marzocchi & M. Jansen 10.1038/s41561-019-0466-8
21. Marine productivity response to Heinrich events: a model-data comparison V. Mariotti et al. 10.5194/cp-8-1581-2012
22. Including an ocean carbon cycle model into <i>i</i>LOVECLIM (v1.0) N. Bouttes et al. 10.5194/gmd-8-1563-2015
23. The Origin and Propagation of the Antarctic Centennial Oscillation W. Davis et al. 10.3390/cli7090112
24. Evaluating Southern Ocean sea-ice for the Last Glacial Maximum and pre-industrial climates: PMIP-2 models and data evidence D. Roche et al. 10.1016/j.quascirev.2012.09.020
25. Quantifying the ocean's role in glacial CO<sub>2</sub> reductions M. Chikamoto et al. 10.5194/cp-8-545-2012
26. Simulating atmospheric CO2, 13C and the marine carbon cycle during the Last Glacial–Interglacial cycle: possible role for a deepening of the mean remineralization depth and an increase in the oceanic nutrient inventory L. Menviel et al. 10.1016/j.quascirev.2012.09.012
27. On Quaternary glaciations, observations and theories D. Paillard 10.1016/j.quascirev.2015.05.017
28. Impact of oceanic processes on the carbon cycle during the last termination N. Bouttes et al. 10.5194/cp-8-149-2012
29. The role of ocean cooling in setting glacial southern source bottom water salinity M. Miller et al. 10.1029/2012PA002297
30. The Impact of the Oceanic Biological Pump on Atmospheric CO2and Its Link to Climate Change E. Kwon & Y. Cho 10.7850/jkso.2013.18.4.266
31. Simulation of climate, ice sheets and CO<sub>2</sub> evolution during the last four glacial cycles with an Earth system model of intermediate complexity A. Ganopolski & V. Brovkin 10.5194/cp-13-1695-2017
32. Modeling the interplay between sea ice formation and the oceanic mixed layer: Limitations of simple brine rejection parameterizations A. Barthélemy et al. 10.1016/j.ocemod.2014.12.009
33. Hydrographic variations in deep ocean temperature over the mid-Pleistocene transition S. Bates et al. 10.1016/j.quascirev.2014.01.020
34. Burial-nutrient feedbacks amplify the sensitivity of atmospheric carbon dioxide to changes in organic matter remineralisation R. Roth et al. 10.5194/esd-5-321-2014
35. Two-phase change in CO2, Antarctic temperature and global climate during Termination II A. Landais et al. 10.1038/ngeo1985
36. Modulation of ice ages via precession and dust-albedo feedbacks R. Ellis & M. Palmer 10.1016/j.gsf.2016.04.004
37. The control of atmosphericpCO2by ocean ventilation change: The effect of the oceanic storage of biogenic carbon E. Kwon et al. 10.1029/2011GB004059
38. Evolution of South Atlantic density and chemical stratification across the last deglaciation J. Roberts et al. 10.1073/pnas.1511252113
39. Assessment of the sea-ice carbon pump: Insights from a three-dimensional ocean-sea-ice-biogeochemical model (MPIOM/HAMOCC) R. Grimm et al. 10.12952/journal.elementa.000136
40. Interglacials of the last 800,000 years 10.1002/2015RG000482
41. The Biological Pump During the Last Glacial Maximum E. Galbraith & L. Skinner 10.1146/annurev-marine-010419-010906
42. Systematic study of the impact of fresh water fluxes on the glacial carbon cycle N. Bouttes et al. 10.5194/cp-8-589-2012
43. Controls on the spatial distribution of oceanic δ<sup>13</sup>C<sub>DIC</sub> P. Holden et al. 10.5194/bgd-9-11843-2012
44. Carbon 13 Isotopes Reveal Limited Ocean Circulation Changes Between Interglacials of the Last 800 ka N. Bouttes et al. 10.1029/2019PA003776
45. Centennial mineral dust variability in high-resolution ice core data from Dome C, Antarctica F. Lambert et al. 10.5194/cp-8-609-2012
46. The “MIS 11 paradox” and ocean circulation: Role of millennial scale events N. Vázquez Riveiros et al. 10.1016/j.epsl.2013.03.036
47. Glacial marine carbon cycle sensitivities to Atlantic ocean circulation reorganization by coupled climate model simulations M. Chikamoto et al. 10.5194/cpd-7-1261-2011
48. The evolution of deep-ocean flow speeds and δ13C under large changes in the Atlantic overturning circulation: Toward a more direct model-data comparison P. Bakker et al. 10.1002/2015PA002776
49. Southern Ocean buoyancy forcing of ocean ventilation and glacial atmospheric CO2 A. Watson et al. 10.1038/ngeo2538
50. Understanding the causes and consequences of past marine carbon cycling variability through models D. Hülse et al. 10.1016/j.earscirev.2017.06.004
51. Sources and transport of dust to East Antarctica: new insights from high-resolution terrestrial and marine aerosol records from the Talos Dome ice core S. Schüpbach et al. 10.5194/cpd-9-3321-2013
52. An improved land biosphere module for use in the DCESS Earth system model (version 1.1) with application to the last glacial termination R. Eichinger et al. 10.5194/gmd-10-3481-2017
53. A synthesis of the arctic terrestrial and marine carbon cycles under pressure from a dwindling cryosphere F. Parmentier et al. 10.1007/s13280-016-0872-8
54. Deciphering the spatio-temporal complexity of climate change of the last deglaciation: a model analysis D. Roche et al. 10.5194/cpd-6-2593-2010
55. Mechanisms of millennial-scale atmospheric CO2 change in numerical model simulations J. Gottschalk et al. 10.1016/j.quascirev.2019.05.013
56. A Seasonal Model of Nitrogen Isotopes in the Ice Age Antarctic Zone: Support for Weakening of the Southern Ocean Upper Overturning Cell P. Kemeny et al. 10.1029/2018PA003478
57. Temporal evolution of mechanisms controlling ocean carbon uptake during the last glacial cycle K. Kohfeld & Z. Chase 10.1016/j.epsl.2017.05.015
58. Modeling the contribution of dissolved organic carbon to carbon sequestration during the last glacial maximum W. Ma & J. Tian 10.1007/s00367-014-0378-y
59. Last Glacial - Holocene climate variability in the Atlantic sector of the Southern Ocean W. Xiao et al. 10.1016/j.quascirev.2016.01.023
60. Response of a comprehensive climate model to a broad range of external forcings: relevance for deep ocean ventilation and the development of late Cenozoic ice ages E. Galbraith & C. de Lavergne 10.1007/s00382-018-4157-8
61. Last Glacial Maximum CO2andδ13C successfully reconciled N. Bouttes et al. 10.1029/2010GL044499
62. Simulated Last Glacial Maximum Δ14Catm and the Deep Glacial Ocean Carbon Reservoir V. Mariotti et al. 10.1017/S0033822200048517
63. The Last Glacial Maximum at 44°S documented by a 10Be moraine chronology at Lake Ohau, Southern Alps of New Zealand A. Putnam et al. 10.1016/j.quascirev.2012.10.034
64. Systematic study of the fresh water fluxes impact on the carbon cycle N. Bouttes et al. 10.5194/cpd-7-1363-2011
65. Fitting the last Pleistocene δ¹⁸O and CO₂ time series with simple box models A. García-Olivares & C. Herrero 10.3989/scimar.03617.19H
66. Deep water formation in the North Pacific and deglacial CO2rise J. Rae et al. 10.1002/2013PA002570