25 citations as recorded by crossref.

1. Response of the carbon cycle in an intermediate complexity model to the different climate configurations of the last nine interglacials N. Bouttes et al. 10.5194/cp-14-239-2018
2. Carbon Fluxes during Dansgaard–Oeschger Events as Simulated by an Earth System Model M. Jochum et al. 10.1175/JCLI-D-21-0713.1
3. Understanding the causes and consequences of past marine carbon cycling variability through models D. Hülse et al. 10.1016/j.earscirev.2017.06.004
4. Ice sheet and terrestrial input impacts on the 100-kyr ocean carbon cycle during the Middle Miocene X. Ma et al. 10.1016/j.gloplacha.2021.103723
5. Oceanic carbon and water masses during the Mystery Interval: A model‐data comparison study W. Huiskamp & K. Meissner 10.1029/2012PA002368
6. Southern Ocean link between changes in atmospheric CO2 levels and northern-hemisphere climate anomalies during the last two glacial periods J. Gottschalk et al. 10.1016/j.quascirev.2019.106067
7. A coupled model for carbon and radiocarbon evolution during the last deglaciation V. Mariotti et al. 10.1002/2015GL067489
8. Marine productivity response to Heinrich events: a model-data comparison V. Mariotti et al. 10.5194/cp-8-1581-2012
9. Lead–lag relationships between global mean temperature and the atmospheric CO 2 content in dependence of the type and time scale of the forcing K. Muryshev et al. 10.1016/j.gloplacha.2016.11.005
10. Deglacial weakening of the oceanic soft tissue pump: global constraints from sedimentary nitrogen isotopes and oxygenation proxies E. Galbraith & S. Jaccard 10.1016/j.quascirev.2014.11.012
11. Role of CO<sub>2</sub> and Southern Ocean winds in glacial abrupt climate change R. Banderas et al. 10.5194/cp-8-1011-2012
12. Millennial-scale atmospheric CO<sub>2</sub> variations during the Marine Isotope Stage 6 period (190–135 ka) J. Shin et al. 10.5194/cp-16-2203-2020
13. Tracking δ13C and δ18O fluctuations uncovers stable modes and key patterns of paleoclimate S. Sun et al. 10.1016/j.gsf.2024.101805
14. Tightened constraints on the time-lag between Antarctic temperature and CO<sub>2</sub> during the last deglaciation J. Pedro et al. 10.5194/cp-8-1213-2012
15. A potential feedback loop underlying glacial-interglacial cycles E. Weinans et al. 10.1007/s00382-021-05724-w
16. Evolution of the stable carbon isotope composition of atmospheric CO2 over the last glacial cycle S. Eggleston et al. 10.1002/2015PA002874
17. Atlantic-Pacific seesaw and its role in outgassing CO2during Heinrich events L. Menviel et al. 10.1002/2013PA002542
18. Two‐Timescale Carbon Cycle Response to an AMOC Collapse S. Nielsen et al. 10.1029/2018PA003481
19. Mechanisms of millennial-scale atmospheric CO2 change in numerical model simulations J. Gottschalk et al. 10.1016/j.quascirev.2019.05.013
20. Evaluating seasonal sea-ice cover over the Southern Ocean at the Last Glacial Maximum R. Green et al. 10.5194/cp-18-845-2022
21. Contribution of enhanced Antarctic Bottom Water formation to Antarctic warm events and millennial-scale atmospheric CO2 increase L. Menviel et al. 10.1016/j.epsl.2014.12.050
22. Past Carbonate Preservation Events in the Deep Southeast Atlantic Ocean (Cape Basin) and Their Implications for Atlantic Overturning Dynamics and Marine Carbon Cycling J. Gottschalk et al. 10.1029/2018PA003353
23. 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
24. Assessing transient changes in the ocean carbon cycle during the last deglaciation through carbon isotope modeling H. Kobayashi et al. 10.5194/cp-20-769-2024
25. Glacial CO<sub>2</sub> cycle as a succession of key physical and biogeochemical processes V. Brovkin et al. 10.5194/cp-8-251-2012