49 citations as recorded by crossref.

1. Marine reservoir ages for coastal West Africa G. Soulet et al. 10.5194/gchron-5-345-2023
2. Late Pleistocene Carbon Cycle Revisited by Considering Solid Earth Processes P. Köhler & G. Munhoven 10.1029/2020PA004020
3. Mechanisms of millennial-scale atmospheric CO2 change in numerical model simulations J. Gottschalk et al. 10.1016/j.quascirev.2019.05.013
4. Evolution of the stable carbon isotope composition of atmospheric CO2 over the last glacial cycle S. Eggleston et al. 10.1002/2015PA002874
5. Understanding the causes and consequences of past marine carbon cycling variability through models D. Hülse et al. 10.1016/j.earscirev.2017.06.004
6. Quasi-100 ky glacial-interglacial cycles triggered by subglacial burial carbon release N. Zeng 10.5194/cp-3-135-2007
7. 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
8. A model‐based interpretation of low‐frequency changes in the carbon cycle during the last 120,000 years and its implications for the reconstruction of atmospheric Δ14C P. Köhler et al. 10.1029/2005GC001228
9. What caused Earth's temperature variations during the last 800,000 years? Data-based evidence on radiative forcing and constraints on climate sensitivity P. Köhler et al. 10.1016/j.quascirev.2009.09.026
10. Asynchrony between Antarctic temperature and CO2 associated with obliquity over the past 720,000 years R. Uemura et al. 10.1038/s41467-018-03328-3
11. Simulated radiocarbon cycle revisited by considering the bipolar seesaw and benthic 14C data P. Köhler et al. 10.1016/j.epsl.2024.118801
12. What drives the millennial and orbital variations of δ18Oatm? A. Landais et al. 10.1016/j.quascirev.2009.07.005
13. Atmosphericδ13CO2and its relation topCO2and deep oceanδ13C during the late Pleistocene P. Köhler et al. 10.1029/2008PA001703
14. The Southern Hemisphere at glacial terminations: insights from the Dome C ice core R. Röthlisberger et al. 10.5194/cp-4-345-2008
15. Changes in environment over the last 800,000 years from chemical analysis of the EPICA Dome C ice core E. Wolff et al. 10.1016/j.quascirev.2009.06.013
16. MODELLING GLOBAL CARBON AND RADIOCARBON CYCLES D. John et al. 10.1093/rpd/ncac137
17. Climate of the last million years: new insights from EPICA and other records C. Barbante et al. 10.1016/j.quascirev.2009.11.025
18. Evolution of Ocean Temperature and Ice Volume Through the Mid-Pleistocene Climate Transition H. Elderfield et al. 10.1126/science.1221294
19. Soil carbon sequestration in a changing global environment F. Macías & M. Camps Arbestain 10.1007/s11027-010-9231-4
20. Marine20—The Marine Radiocarbon Age Calibration Curve (0–55,000 cal BP) T. Heaton et al. 10.1017/RDC.2020.68
21. North Atlantic ventilation of “southern‐sourced” deep water in the glacial ocean E. Kwon et al. 10.1029/2011PA002211
22. On the application and interpretation of Keeling plots in paleo climate research – deciphering δ13C of atmospheric CO2 measured in ice cores P. Köhler et al. 10.5194/bg-3-539-2006
23. A RESPONSE TO COMMUNITY QUESTIONS ON THE MARINE20 RADIOCARBON AGE CALIBRATION CURVE: MARINE RESERVOIR AGES AND THE CALIBRATION OF 14C SAMPLES FROM THE OCEANS T. Heaton et al. 10.1017/RDC.2022.66
24. In and out of glacial extremes by way of dust−climate feedbacks G. Shaffer & F. Lambert 10.1073/pnas.1708174115
25. Deep Atlantic Carbonate Ion and CaCO3 Compensation During the Ice Ages S. Sosdian et al. 10.1029/2017PA003312
26. 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
27. Impact of terrestrial biosphere on the atmospheric CO2 concentration across Termination V G. Hes et al. 10.5194/cp-18-1429-2022
28. A reconstruction of atmospheric carbon dioxide and its stable carbon isotopic composition from the penultimate glacial maximum to the last glacial inception R. Schneider et al. 10.5194/cp-9-2507-2013
29. High-resolution carbon dioxide concentration record 650,000–800,000 years before present D. Lüthi et al. 10.1038/nature06949
30. 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
31. Glacial CO2 cycle as a succession of key physical and biogeochemical processes V. Brovkin et al. 10.5194/cp-8-251-2012
32. Migration of the Antarctic Polar Front through the mid-Pleistocene transition: evidence and climatic implications A. Kemp et al. 10.1016/j.quascirev.2010.04.027
33. Atmospheric CO2 Concentration Based on Boron Isotopes Versus Simulations of the Global Carbon Cycle During the Plio‐Pleistocene P. Köhler 10.1029/2022PA004439
34. Comment on “Magnetic effect on CO2 solubility in seawater: A possible link between geomagnetic field variations and climate” by Alexander Pazur and Michael Winklhofer P. Köhler et al. 10.1029/2008GL036133
35. Recent Developments in Calibration for Archaeological and Environmental Samples J. van der Plicht et al. 10.1017/RDC.2020.22
36. Application of sediment core modelling to interpreting the glacial-interglacial record of Southern Ocean silica cycling A. Ridgwell 10.5194/cp-3-387-2007
37. Centennial mineral dust variability in high-resolution ice core data from Dome C, Antarctica F. Lambert et al. 10.5194/cp-8-609-2012
38. The carbon cycle during the Mid Pleistocene Transition: the Southern Ocean Decoupling Hypothesis P. Köhler & R. Bintanja 10.5194/cp-4-311-2008
39. The influence of the ocean circulation state on ocean carbon storage and CO2 drawdown potential in an Earth system model M. Ödalen et al. 10.5194/bg-15-1367-2018
40. Regional patterns and temporal evolution of ocean iron fertilization and CO2 drawdown during the last glacial termination F. Lambert et al. 10.1016/j.epsl.2020.116675
41. Anthropogenic CO2 of High Emission Scenario Compensated After 3500 Years of Ocean Alkalinization With an Annually Constant Dissolution of 5 Pg of Olivine P. Köhler 10.3389/fclim.2020.575744
42. Constraint of the CO2 rise by new atmospheric carbon isotopic measurements during the last deglaciation A. Lourantou et al. 10.1029/2009GB003545
43. Carbon 13 Isotopes Reveal Limited Ocean Circulation Changes Between Interglacials of the Last 800 ka N. Bouttes et al. 10.1029/2019PA003776
44. Radiogenic isotopic and clay mineralogical signatures of terrigenous particles as water-mass tracers: New insights into South Atlantic deep circulation during the last termination F. Beny et al. 10.1016/j.quascirev.2019.106089
45. LOCAL MARINE RESERVOIR AGE (ΔR) RECONSTRUCTED BASED ON THE TSUNAMI DEPOSIT FROM PANGANI BAY (TANZANIA) G. Soulet & V. Maselli 10.1017/RDC.2021.47
46. The role of Southern Ocean processes in orbital and millennial CO2 variations – A synthesis H. Fischer et al. 10.1016/j.quascirev.2009.06.007
47. Deep water [CO32−] and circulation in the south China sea over the last glacial cycle S. Wan et al. 10.1016/j.quascirev.2020.106499
48. The Climate Response to the Astronomical Forcing M. Crucifix et al. 10.1007/s11214-006-9058-1
49. Glacial‐interglacial variations in marine phosphorus cycling: Implications for ocean productivity I. Tsandev et al. 10.1029/2007GB003054