27 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. Understanding the causes and consequences of past marine carbon cycling variability through models D. Hülse et al. 10.1016/j.earscirev.2017.06.004
3. 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
4. Oceanic carbon and water masses during the Mystery Interval: A model‐data comparison study W. Huiskamp & K. Meissner 10.1029/2012PA002368
5. 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
6. A coupled model for carbon and radiocarbon evolution during the last deglaciation V. Mariotti et al. 10.1002/2015GL067489
7. Marine productivity response to Heinrich events: a model-data comparison V. Mariotti et al. 10.5194/cp-8-1581-2012
8. 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
9. Earth system response to Heinrich events explained by a bipolar convection seesaw M. Willeit et al. 10.1038/s41561-025-01814-0
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 CO2 and Southern Ocean winds in glacial abrupt climate change R. Banderas et al. 10.5194/cp-8-1011-2012
12. Millennial-scale atmospheric CO2 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. Multi-model assessment of the deglacial climatic evolution at high southern latitudes T. Obase et al. 10.5194/cp-21-1443-2025
15. Tightened constraints on the time-lag between Antarctic temperature and CO2 during the last deglaciation J. Pedro et al. 10.5194/cp-8-1213-2012
16. A potential feedback loop underlying glacial-interglacial cycles E. Weinans et al. 10.1007/s00382-021-05724-w
17. Evolution of the stable carbon isotope composition of atmospheric CO2 over the last glacial cycle S. Eggleston et al. 10.1002/2015PA002874
18. Atlantic-Pacific seesaw and its role in outgassing CO2during Heinrich events L. Menviel et al. 10.1002/2013PA002542
19. Two‐Timescale Carbon Cycle Response to an AMOC Collapse S. Nielsen et al. 10.1029/2018PA003481
20. Mechanisms of millennial-scale atmospheric CO2 change in numerical model simulations J. Gottschalk et al. 10.1016/j.quascirev.2019.05.013
21. Evaluating seasonal sea-ice cover over the Southern Ocean at the Last Glacial Maximum R. Green et al. 10.5194/cp-18-845-2022
22. 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
23. 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
24. 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
25. 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
26. New estimation of critical insolation–CO2 relationship for triggering glacial inception S. Talento et al. 10.5194/cp-20-1349-2024
27. Glacial CO2 cycle as a succession of key physical and biogeochemical processes V. Brovkin et al. 10.5194/cp-8-251-2012