90 citations as recorded by crossref.

1. Organic carbon burial drivers in the northeastern South China Sea since the last glacial X. Huang et al.
2. Temporal evolution of mechanisms controlling ocean carbon uptake during the last glacial cycle K. Kohfeld & Z. Chase
3. Sequential changes in ocean circulation and biological export productivity during the last glacial–interglacial cycle: a model–data study C. O'Neill et al.
4. Sensitivity simulations with direct shortwave radiative forcing by aeolian dust during glacial cycles E. Bauer & A. Ganopolski
5. Critical insolation–CO2 relation for diagnosing past and future glacial inception A. Ganopolski et al.
6. Coupled climate–carbon cycle simulation of the Last Glacial Maximum atmospheric CO2 decrease using a large ensemble of modern plausible parameter sets K. Kemppinen et al.
7. Modeling the evolution of pulse-like perturbations in atmospheric carbon and carbon isotopes: the role of weathering–sedimentation imbalances A. Jeltsch-Thömmes & F. Joos
8. Synchronization phenomena observed in glacial–interglacial cycles simulated in an Earth system model of intermediate complexity T. Mitsui et al.
9. Rejuvenating the ocean: mean ocean radiocarbon, CO2 release, and radiocarbon budget closure across the last deglaciation L. Skinner et al.
10. Deglacial weakening of the oceanic soft tissue pump: global constraints from sedimentary nitrogen isotopes and oxygenation proxies E. Galbraith & S. Jaccard
11. The role of land weathering in carbon consumption and its impact on global carbon cycling since the Last Interglacial period S. Xu et al.
12. Timing of a future glaciation in view of anthropogenic climate change C. Kaufhold et al.
13. Permafrost-carbon mobilization in Beringia caused by deglacial meltwater runoff, sea-level rise and warming V. Meyer et al.
14. Transient climate simulations of the deglaciation 21–9 thousand years before present (version 1) – PMIP4 Core experiment design and boundary conditions R. Ivanovic et al.
15. Deglacial carbon cycle changes observed in a compilation of 127 benthic δ13C time series (20–6 ka) C. Peterson & L. Lisiecki
16. On the Cause of the Mid‐Pleistocene Transition C. Berends et al.
17. In and out of glacial extremes by way of dust−climate feedbacks G. Shaffer & F. Lambert
18. FESOM2.1-REcoM3-MEDUSA2: an ocean–sea ice–biogeochemistry model coupled to a sediment model Y. Ye et al.
19. Earth system response to Heinrich events explained by a bipolar convection seesaw M. Willeit et al.
20. Testing the reliability of global surface temperature reconstructions of the Last Glacial Cycle with pseudo-proxy experiments J. Baudouin et al.
21. Dynamic storage of glacial CO2 in the Atlantic Ocean revealed by boron [CO32−] and pH records T. Chalk et al.
22. Covariation of deep Southern Ocean oxygenation and atmospheric CO2 through the last ice age S. Jaccard et al.
23. Surface fertilisation and organic matter delivery enhanced carbonate dissolution in the western South Atlantic J. Suárez-Ibarra et al.
24. Quantifying the influence of the terrestrial biosphere on glacial–interglacial climate dynamics T. Davies-Barnard et al.
25. Response of Atmospheric pCO2 to Glacial Changes in the Southern Ocean Amplified by Carbonate Compensation H. Kobayashi & A. Oka
26. Impact of iron fertilisation on atmospheric CO2 during the last glaciation H. Saini et al.
27. Simulated radiocarbon cycle revisited by considering the bipolar seesaw and benthic 14C data P. Köhler et al.
28. An 800-kyr record of global surface ocean δ18O and implications for ice volume-temperature coupling J. Shakun et al.
29. Monsoon- and ENSO-driven surface-water pCO2 variation in the tropical West Pacific since the Last Glacial Maximum Z. Xiong et al.
30. Reduced-complexity model for the impact of anthropogenic CO2 emissions on future glacial cycles S. Talento & A. Ganopolski
31. Nonlinear climate dynamics: From deterministic behaviour to stochastic excitability and chaos D. Alexandrov et al.
32. Assessing transient changes in the ocean carbon cycle during the last deglaciation through carbon isotope modeling H. Kobayashi et al.
33. Coupling of a sediment diagenesis model (MEDUSA) and an Earth system model (CESM1.2): a contribution toward enhanced marine biogeochemical modelling and long-term climate simulations T. Kurahashi-Nakamura et al.
34. Impact of Greenland Ice Sheet disintegration on atmosphere and ocean disentangled M. Andernach et al.
35. The role of orbital forcing in the Early Middle Pleistocene Transition M. Maslin & C. Brierley
36. Antarctic sea ice over the past 130 000 years – Part 1: a review of what proxy records tell us X. Crosta et al.
37. Sea level fall during glaciation stabilized atmospheric CO2 by enhanced volcanic degassing J. Hasenclever et al.
38. A reconstruction of radiocarbon production and total solar irradiance from the Holocene 14C and CO2 records: implications of data and model uncertainties R. Roth & F. Joos
39. Effects of eustatic sea-level change, ocean dynamics, and nutrient utilization on atmospheric pCO2 and seawater composition over the last 130 000 years: a model study K. Wallmann et al.
40. On the effect of orbital forcing on mid-Pliocene climate, vegetation and ice sheets M. Willeit et al.
41. Carbon Cycle Responses to Changes in Weathering and the Long‐Term Fate of Stable Carbon Isotopes A. Jeltsch‐Thömmes & F. Joos
42. Simulation of climate, ice sheets and CO2 evolution during the last four glacial cycles with an Earth system model of intermediate complexity A. Ganopolski & V. Brovkin
43. Carbon cycle implications of terrestrial weathering changes since the last glacial maximum M. Brault et al.
44. The influence of the ocean circulation state on ocean carbon storage and CO2 drawdown potential in an Earth system model M. Ödalen et al.
45. Radiocarbon as a Dating Tool and Tracer in Paleoceanography L. Skinner & E. Bard
46. Pattern scaling of simulated vegetation change in northern Africa during glacial cycles M. Duque-Villegas et al.
47. Interglacials of the last 800,000 years
48. 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.
49. Ice-sheet configuration in the CMIP5/PMIP3 Last Glacial Maximum experiments A. Abe-Ouchi et al.
50. The Role of Enthalpy of Reaction in the Process of Global Warming: What Can We Learn from Basic Thermodynamics* W. Vogelsberger
51. Reconstructing the evolution of ice sheets, sea level, and atmospheric CO2 during the past 3.6 million years C. Berends et al.
52. Deglacial ice sheet meltdown: orbital pacemaking and CO2 effects M. Heinemann et al.
53. Model of Early Diagenesis in the Upper Sediment with Adaptable complexity – MEDUSA (v. 2): a time-dependent biogeochemical sediment module for Earth system models, process analysis and teaching G. Munhoven
54. A First Intercomparison of the Simulated LGM Carbon Results Within PMIP‐Carbon: Role of the Ocean Boundary Conditions F. Lhardy et al.
55. Mid-Pleistocene transition in glacial cycles explained by declining CO 2 and regolith removal M. Willeit et al.
56. Low terrestrial carbon storage at the Last Glacial Maximum: constraints from multi-proxy data A. Jeltsch-Thömmes et al.
57. Strong increase in thawing of subsea permafrost in the 22nd century caused by anthropogenic climate change S. Wilkenskjeld et al.
58. Sediment fluxes dominate glacial–interglacial changes in ocean carbon inventory: results from factorial simulations over the past 780 000 years M. Adloff et al.
59. Radiocarbon constraints on the glacial ocean circulation and its impact on atmospheric CO2 L. Skinner et al.
60. Modelled interglacial carbon cycle dynamics during the Holocene, the Eemian and Marine Isotope Stage (MIS) 11 T. Kleinen et al.
61. Long-term deglacial permafrost carbon dynamics in MPI-ESM T. Schneider von Deimling et al.
62. The Biological Pump During the Last Glacial Maximum E. Galbraith & L. Skinner
63. An Analytical Framework for the Steady State Impact of Carbonate Compensation on Atmospheric CO2 A. Omta et al.
64. Toward generalized Milankovitch theory (GMT) A. Ganopolski
65. Traditional and novel approaches to palaeoclimate modelling M. Crucifix
66. Mysteriously high Δ14C of the glacial atmosphere: influence of 14C production and carbon cycle changes A. Dinauer et al.
67. Assessing future ice-sheet variability for long-term safety of deep geological repositories J. Liakka et al.
68. Is late Quaternary climate change governed by self-sustained oscillations in atmospheric CO2? K. Wallmann
69. The Earth system model CLIMBER-X v1.0 – Part 2: The global carbon cycle M. Willeit et al.
70. The role of CO2 decline for the onset of Northern Hemisphere glaciation M. Willeit et al.
71. Atmospheric methane underestimated in future climate projections T. Kleinen et al.
72. Sea level and ground water table depth (WTD): A biogeochemical pacemaker for glacial-interglacial cycling S. Cowling
73. CO2 drawdown due to particle ballasting by glacial aeolian dust: an estimate based on the ocean carbon cycle model MPIOM/HAMOCC version 1.6.2p3 M. Heinemann et al.
74. A lower limit to atmospheric CO2 concentrations over the past 800,000 years E. Galbraith & S. Eggleston
75. Glacial carbon cycle changes by Southern Ocean processes with sedimentary amplification H. Kobayashi et al.
76. On the potential role of marine calcifiers in glacial‐interglacial dynamics A. Omta et al.
77. CO2 and summer insolation as drivers for the Mid-Pleistocene Transition M. Scherrenberg et al.
78. Comparative carbon cycle dynamics of the present and last interglacial V. Brovkin et al.
79. 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
80. Role of the Deglacial Buildup of the Great Barrier Reef for the Global Carbon Cycle T. Felis et al.
81. Last glacial-interglacial productivity and associated changes in the eastern Arabian Sea D. Naik et al.
82. Understanding the causes and consequences of past marine carbon cycling variability through models D. Hülse et al.
83. Glacial CO2 decrease and deep-water deoxygenation by iron fertilization from glaciogenic dust A. Yamamoto et al.
84. Deglacial climate, carbon cycle and ocean chemistry changes in response to a terrestrial carbon release C. Simmons et al.
85. Sensitivity of simulations of Plio–Pleistocene climate with the CLIMBER-2 Earth System Model to details of the global carbon cycle J. Carrillo et al.
86. Mechanisms of millennial-scale atmospheric CO2 change in numerical model simulations J. Gottschalk et al.
87. Late Pleistocene Carbon Cycle Revisited by Considering Solid Earth Processes P. Köhler & G. Munhoven
88. Organic Matter DYnamic model (OMDY) predicts the wood debris decomposition of ten Mediterranean species S. Spigno et al.
89. Variations in mid-ocean ridge CO2 emissions driven by glacial cycles J. Burley & R. Katz
90. Path-dependence of the Plio–Pleistocene glacial/interglacial cycles J. Carrillo et al.