24 citations as recorded by crossref.

1. Enhanced vertical mixing in the glacial ocean inferred from sedimentary carbon isotopes S. Wilmes et al. 10.1038/s43247-021-00239-y
2. Two‐Timescale Carbon Cycle Response to an AMOC Collapse S. Nielsen et al. 10.1029/2018PA003481
3. Carbon Capture and Utilization Technology without Carbon Dioxide Purification and Pressurization: A Review on Its Necessity and Available Technologies H. Ho et al. 10.1021/acs.iecr.9b01213
4. 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
5. Meridional Ocean Carbon Transport A. Aldama‐Campino et al. 10.1029/2019GB006336
6. Paleoredox conditions of bottom water in the northern Indian Ocean since 39 ka R. Nambiar et al. 10.1016/j.palaeo.2021.110766
7. Climate pathways behind phytoplankton-induced atmospheric warming R. Asselot et al. 10.5194/bg-19-223-2022
8. Mechanisms of millennial-scale atmospheric CO2 change in numerical model simulations J. Gottschalk et al. 10.1016/j.quascirev.2019.05.013
9. Evaluating the biological pump efficiency of the Last Glacial Maximum ocean using δ13C A. Morée et al. 10.5194/cp-17-753-2021
10. Prediction of CO2 solubility in NaCl brine under geological conditions with an improved binary interaction parameter in the Søreide-Whitson model Z. Liu et al. 10.1016/j.geothermics.2022.102544
11. The atmospheric bridge communicated the δ13C decline during the last deglaciation to the global upper ocean J. Shao et al. 10.5194/cp-17-1507-2021
12. 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
13. Asymmetric dynamical ocean responses in warming icehouse and cooling greenhouse climates K. Kvale et al. 10.1088/1748-9326/aaedc3
14. Investigation of Mineral Carbonation with Direct Bubbling into Concrete Sludge M. Abe et al. 10.1021/acsomega.0c04758
15. The Biological Pump During the Last Glacial Maximum E. Galbraith & L. Skinner 10.1146/annurev-marine-010419-010906
16. The devil's in the disequilibrium: multi-component analysis of dissolved carbon and oxygen changes under a broad range of forcings in a general circulation model S. Eggleston & E. Galbraith 10.5194/bg-15-3761-2018
17. Global cooling linked to increased glacial carbon storage via changes in Antarctic sea ice A. Marzocchi & M. Jansen 10.1038/s41561-019-0466-8
18. Reduced CO2 uptake and growing nutrient sequestration from slowing overturning circulation Y. Liu et al. 10.1038/s41558-022-01555-7
19. A First Intercomparison of the Simulated LGM Carbon Results Within PMIP‐Carbon: Role of the Ocean Boundary Conditions F. Lhardy et al. 10.1029/2021PA004302
20. Linking Glacial‐Interglacial States to Multiple Equilibria of Climate D. Ferreira et al. 10.1029/2018GL077019
21. Carbon burial in deep-sea sediment and implications for oceanic inventories of carbon and alkalinity over the last glacial cycle O. Cartapanis et al. 10.5194/cp-14-1819-2018
22. Feedbacks of CaCO3 dissolution effect on ocean carbon sink and seawater acidification: a model study H. Zhang et al. 10.1088/2515-7620/aca9ac
23. Retracted: Earth System Model Analysis of How Astronomical Forcing Is Imprinted Onto the Marine Geological Record: The Role of the Inorganic (Carbonate) Carbon Cycle and Feedbacks P. Vervoort et al. 10.1029/2020PA004090
24. The Relative Importance of Phytoplankton Light Absorption and Ecosystem Complexity in an Earth System Model R. Asselot et al. 10.1029/2020MS002110