108 citations as recorded by crossref.

1. Mathematics of the total alkalinity–pH equation – pathway to robust and universal solution algorithms: the SolveSAPHE package v1.0.1 G. Munhoven 10.5194/gmd-6-1367-2013
2. Tectonic degassing drove global temperature trends since 20 Ma T. Herbert et al. 10.1126/science.abl4353
3. The seawater carbon inventory at the Paleocene–Eocene Thermal Maximum L. Haynes & B. Hönisch 10.1073/pnas.2003197117
4. Radiolarian size and silicification across the Paleocene-Eocene boundary and into the early Eocene S. Westacott et al. 10.1016/j.palaeo.2022.111287
5. 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
6. Ocean biogeochemistry in the warm climate of the late Paleocene M. Heinze & T. Ilyina 10.5194/cp-11-63-2015
7. Orbitally Paced Carbon and Deep‐Sea Temperature Changes at the Peak of the Early Eocene Climatic Optimum V. Lauretano et al. 10.1029/2018PA003422
8. History of carbonate ion concentration over the last 100 million years II: Revised calculations and new data R. Zeebe & T. Tyrrell 10.1016/j.gca.2019.02.041
9. Understanding long-term carbon cycle trends: The late Paleocene through the early Eocene N. Komar et al. 10.1002/palo.20060
10. Late Lutetian Thermal Maximum—Crossing a Thermal Threshold in Earth's Climate System? T. Westerhold et al. 10.1002/2017GC007240
11. Climatic fluctuations modeled for carbon and sulfur emissions from end-Triassic volcanism J. Landwehrs et al. 10.1016/j.epsl.2020.116174
12. Anthropogenic carbon release rate unprecedented during the past 66 million years R. Zeebe et al. 10.1038/ngeo2681
13. Marine siliceous ecosystem decline led to sustained anomalous Early Triassic warmth T. Isson et al. 10.1038/s41467-022-31128-3
14. Modeling 400–500-kyr Pleistocene carbon isotope cyclicity through variations in the dissolved organic carbon pool W. Ma et al. 10.1016/j.gloplacha.2017.04.001
15. All aboard! Earth system investigations with the CH2O-CHOO TRAIN v1.0 T. Kukla et al. 10.5194/gmd-16-5515-2023
16. Silicate weathering as a feedback and forcing in Earth's climate and carbon cycle D. Penman et al. 10.1016/j.earscirev.2020.103298
17. A Cenozoic record of the equatorial Pacific carbonate compensation depth H. Pälike et al. 10.1038/nature11360
18. Origin of the long-term increase in coccolith size and its implication for carbon cycle and climate over the past 2 Myr X. Jin et al. 10.1016/j.quascirev.2022.107642
19. Reverse weathering as a long-term stabilizer of marine pH and planetary climate T. Isson & N. Planavsky 10.1038/s41586-018-0408-4
20. The [simple carbon project] model v1.0 C. O'Neill et al. 10.5194/gmd-12-1541-2019
21. Coupled dolomite and silica precipitation from continental weathering during deglaciation of the Marinoan Snowball Earth Y. Fang & H. Xu 10.1016/j.precamres.2022.106824
22. Reconciling atmospheric CO 2 , weathering, and calcite compensation depth across the Cenozoic N. Komar & R. Zeebe 10.1126/sciadv.abd4876
23. Cracking the palaeoclimate code S. Meyers 10.1038/nature22501
24. Eutrophication and Deoxygenation Forcing of Marginal Marine Organic Carbon Burial During the PETM N. Papadomanolaki et al. 10.1029/2021PA004232
25. Terrestrial records of two hyperthermal events in the Cretaceous-Paleogene boundary suggest different control mechanisms M. Ma et al. 10.1038/s43247-024-01425-4
26. Geologic history of seawater: A MAGic approach to carbon chemistry and ocean ventilation R. Arvidson et al. 10.1016/j.chemgeo.2013.10.012
27. Ocean acidification and the Permo-Triassic mass extinction M. Clarkson et al. 10.1126/science.aaa0193
28. Calcium and calcium isotope changes during carbon cycle perturbations at the end-Permian N. Komar & R. Zeebe 10.1002/2015PA002834
29. Geochronological Constraints on the Evolution and Petrogenesis of the Malwa Plateau Subprovince of the Deccan Traps A. Tholt et al. 10.1029/2023GC011137
30. Middle Eocene greenhouse warming facilitated by diminished weathering feedback R. van der Ploeg et al. 10.1038/s41467-018-05104-9
31. Constraints on the volume and rate of Deccan Traps flood basalt eruptions using a combination of high-resolution terrestrial mercury records and geochemical box models I. Fendley et al. 10.1016/j.epsl.2019.115721
32. Atmospheric CO2 Concentration Based on Boron Isotopes Versus Simulations of the Global Carbon Cycle During the Plio‐Pleistocene P. Köhler 10.1029/2022PA004439
33. Surface ocean warming and acidification driven by rapid carbon release precedes Paleocene-Eocene Thermal Maximum T. Babila et al. 10.1126/sciadv.abg1025
34. CASCADE: Dataset of extant coccolithophore size, carbon content and global distribution J. de Vries et al. 10.1038/s41597-024-03724-z
35. Orbital Signals in Carbon Isotopes: Phase Distortion as a Signature of the Carbon Cycle J. Laurin et al. 10.1002/2017PA003143
36. Effects of Dynamic Topography on the Cenozoic Carbonate Compensation Depth S. Campbell et al. 10.1002/2017GC007386
37. The 405 kyr and 2.4 Myr eccentricity components in Cenozoic carbon isotope records I. Kocken et al. 10.5194/cp-15-91-2019
38. Rapid coupling between solid earth and ice volume during the Quaternary Y. Kuwahara et al. 10.1038/s41598-021-84448-7
39. New constraints on massive carbon release and recovery processes during the Paleocene-Eocene Thermal Maximum D. Penman & J. Zachos 10.1088/1748-9326/aae285
40. Carbonate dissolution rates at the deep ocean floor B. Boudreau 10.1029/2012GL054231
41. Understanding the causes and consequences of past marine carbon cycling variability through models D. Hülse et al. 10.1016/j.earscirev.2017.06.004
42. Thermogenic carbon release from the Central Atlantic magmatic province caused major end-Triassic carbon cycle perturbations T. Heimdal et al. 10.1073/pnas.2000095117
43. Lithium isotope evidence for enhanced weathering and erosion during the Paleocene-Eocene Thermal Maximum P. Pogge von Strandmann et al. 10.1126/sciadv.abh4224
44. Interpreting the Difference in Magnitudes of PETM Carbon Isotope Excursions in Paleosol Carbonate and Organic Matter: Oxidation of Methane in Soils Versus Elevated Soil Respiration Rates T. Gallagher et al. 10.1029/2019PA003596
45. Late Pleistocene Carbon Cycle Revisited by Considering Solid Earth Processes P. Köhler & G. Munhoven 10.1029/2020PA004020
46. A protracted Mesoproterozoic carbon cycle perturbation in response to volcanism at ∼ 1.39 Ga Y. Lyu et al. 10.1016/j.palaeo.2024.112355
47. Bentho‐Pelagic Decoupling: The Marine Biological Carbon Pump During Eocene Hyperthermals E. Griffith et al. 10.1029/2020PA004053
48. Constraints on the onset duration of the Paleocene–Eocene Thermal Maximum S. Turner 10.1098/rsta.2017.0082
49. Biogeochemical significance of pelagic ecosystem function: an end-Cretaceous case study M. Henehan et al. 10.1098/rstb.2015.0510
50. Effect of the Atlantic Meridional Overturning Circulation on atmospheric pCO2 variations A. Boot et al. 10.5194/esd-13-1041-2022
51. The Magnitude of Surface Ocean Acidification and Carbon Release During Eocene Thermal Maximum 2 (ETM‐2) and the Paleocene‐Eocene Thermal Maximum (PETM) D. Harper et al. 10.1029/2019PA003699
52. Orbital forcing of the Paleocene and Eocene carbon cycle R. Zeebe et al. 10.1002/2016PA003054
53. Estimating the impact of the cryptic degassing of Large Igneous Provinces: A mid-Miocene case-study D. Armstrong McKay et al. 10.1016/j.epsl.2014.06.040
54. Severity of ocean acidification following the end-Cretaceous asteroid impact T. Tyrrell et al. 10.1073/pnas.1418604112
55. Early and late phases of the Permian–Triassic mass extinction marked by different atmospheric CO2 regimes J. Shen et al. 10.1038/s41561-022-01034-w
56. A climate threshold for ocean deoxygenation during the Early Cretaceous K. Bauer et al. 10.1038/s41586-024-07876-1
57. Unravelling the land source: an investigation of the processes contributing to the oceanic input of DIC and alkalinity J. Hieronymus & G. Walin 10.3402/tellusb.v65i0.19683
58. Aptian–Albian clumped isotopes from northwest China: cool temperatures, variable atmospheric <i>p</i>CO<sub>2</sub> and regional shifts in the hydrologic cycle D. Harper et al. 10.5194/cp-17-1607-2021
59. A Simple Thousand-Year Prognosis for Oceanic and Atmospheric Carbon Change A. Fowler 10.1007/s00024-014-0892-x
60. Peak intervals of equatorial Pacific export production during the middle Miocene climate transition S. Carter et al. 10.1130/G38290.1
61. Sequential changes in ocean circulation and biological export productivity during the last glacial–interglacial cycle: a model–data study C. O'Neill et al. 10.5194/cp-17-171-2021
62. A middle Eocene carbon cycle conundrum A. Sluijs et al. 10.1038/ngeo1807
63. What caused the long duration of the Paleocene‐Eocene Thermal Maximum? R. Zeebe 10.1002/palo.20039
64. Quantifying the volcanic emissions which triggered Oceanic Anoxic Event 1a and their effect on ocean acidification K. Bauer et al. 10.1111/sed.12335
65. Secular variations in the carbonate chemistry of the oceans over the Cenozoic B. Boudreau et al. 10.1016/j.epsl.2019.02.004
66. The effects of bathymetry on the long-term carbon cycle and CCD M. Bogumil et al. 10.1073/pnas.2400232121
67. Atlantic Deep‐Sea Cherts Associated With Eocene Hyperthermal Events D. Penman et al. 10.1029/2018PA003503
68. The Influence of Warming on Phosphorus Burial in Continental Margin Sediments M. Zhao et al. 10.2475/001c.85110
69. Differential weathering of basaltic and granitic catchments from concentration–discharge relationships D. Ibarra et al. 10.1016/j.gca.2016.07.006
70. No Cretaceous‐Paleogene Boundary in Exposed Rajahmundry Traps: A Refined Chronology of the Longest Deccan Lava Flows From40Ar/39Ar Dates, Magnetostratigraphy, and Biostratigraphy I. Fendley et al. 10.1029/2020GC009149
71. Long-term legacy of massive carbon input to the Earth system: Anthropocene versus Eocene R. Zeebe & J. Zachos 10.1098/rsta.2012.0006
72. Enhanced clay formation key in sustaining the Middle Eocene Climatic Optimum A. Krause et al. 10.1038/s41561-023-01234-y
73. Oxygen isotope ensemble reveals Earth’s seawater, temperature, and carbon cycle history T. Isson & S. Rauzi 10.1126/science.adg1366
74. Cenozoic carbon cycle imbalances and a variable weathering feedback J. Caves et al. 10.1016/j.epsl.2016.06.035
75. On impact and volcanism across the Cretaceous-Paleogene boundary P. Hull et al. 10.1126/science.aay5055
76. Reconciling early Deccan Traps CO 2 outgassing and pre-KPB global climate A. Hernandez Nava et al. 10.1073/pnas.2007797118
77. Enhanced metamorphic CO 2 release on the Proterozoic Earth E. Stewart & D. Penman 10.1073/pnas.2401961121
78. Data-model comparison reveals key environmental changes leading to Cenomanian-Turonian Oceanic Anoxic Event 2 Y. Joo et al. 10.1016/j.earscirev.2020.103123
79. Thermogenic methane release as a cause for the long duration of the PETM J. Frieling et al. 10.1073/pnas.1603348113
80. The role of conceptual models in climate research H. Dijkstra 10.1016/j.physd.2023.133984
81. Increased Biogenic Calcification and Burial Under Elevated pCO2 During the Miocene: A Model‐Data Comparison W. Si et al. 10.1029/2022GB007541
82. Coupled carbon and silica cycle perturbations during the Marinoan snowball Earth deglaciation D. Penman & A. Rooney 10.1130/G45812.1
83. Control of CaCO3 dissolution at the deep seafloor and its consequences B. Boudreau et al. 10.1016/j.gca.2019.09.037
84. On the role of chemical weathering of continental arcs in long-term climate regulation: A case study of the Peninsular Ranges batholith, California (USA) H. Jiang & C. Lee 10.1016/j.epsl.2019.115733
85. Long- and short-term coupling of sea surface temperature and atmospheric CO 2 during the late Paleocene and early Eocene D. Harper et al. 10.1073/pnas.2318779121
86. Relationships between CO2, thermodynamic limits on silicate weathering, and the strength of the silicate weathering feedback M. Winnick & K. Maher 10.1016/j.epsl.2018.01.005
87. Global Extent of Early Eocene Hyperthermal Events: A New Pacific Benthic Foraminiferal Isotope Record From Shatsky Rise (ODP Site 1209) T. Westerhold et al. 10.1029/2017PA003306
88. Redox-controlled carbon and phosphorus burial: A mechanism for enhanced organic carbon sequestration during the PETM N. Komar & R. Zeebe 10.1016/j.epsl.2017.09.011
89. Intensified continental chemical weathering and carbon-cycle perturbations linked to volcanism during the Triassic–Jurassic transition J. Shen et al. 10.1038/s41467-022-27965-x
90. Marine anoxia linked to abrupt global warming during Earth’s penultimate icehouse J. Chen et al. 10.1073/pnas.2115231119
91. Intrusions induce global warming before continental flood basalt volcanism X. Tian & W. Buck 10.1038/s41561-022-00939-w
92. Modeling hyperthermal events in the Mesozoic-Paleogene periods: a review Y. Zhang et al. 10.3389/fevo.2023.1226349
93. A Bayesian inversion for emissions and export productivity across the end-Cretaceous boundary A. Cox & C. Keller 10.1126/science.adh3875
94. Carbonate weathering, CO2 redistribution, and Neogene CCD and pCO2 evolution L. Derry 10.1016/j.epsl.2022.117801
95. Time-dependent climate sensitivity and the legacy of anthropogenic greenhouse gas emissions R. Zeebe 10.1073/pnas.1222843110
96. Reply to Pearson and Nicholas, Stassen et al., and Zeebe et al.: Teasing out the missing piece of the PETM puzzle J. Wright & M. Schaller 10.1073/pnas.1321876111
97. Scaling laws for perturbations in the ocean–atmosphere system following large CO<sub>2</sub> emissions N. Towles et al. 10.5194/cp-11-991-2015
98. Oxygenation of the Earth aided by mineral–organic carbon preservation M. Zhao et al. 10.1038/s41561-023-01133-2
99. What Models Tell Us About the Evolution of Carbon Sources and Sinks over the Phanerozoic Y. Goddéris et al. 10.1146/annurev-earth-032320-092701
100. Up in smoke: A role for organic carbon feedbacks in Paleogene hyperthermals G. Bowen 10.1016/j.gloplacha.2013.07.001
101. iLOSCAR: interactive Long-term Ocean-atmosphere-Sediment CArbon cycle Reservoir model v1.0 S. Li et al. 10.1016/j.gloplacha.2024.104413
102. What the future ocean has in common with an asthma attack G. Aloisi 10.1177/20530196231204340
103. A critical trade-off between nitrogen quota and growth allows Coccolithus braarudii life cycle phases to exploit varying environment J. de Vries et al. 10.5194/bg-21-1707-2024
104. An abyssal carbonate compensation depth overshoot in the aftermath of the Palaeocene–Eocene Thermal Maximum D. Penman et al. 10.1038/ngeo2757
105. Can organic matter flux profiles be diagnosed using remineralisation rates derived from observed tracers and modelled ocean transport rates? J. Wilson et al. 10.5194/bg-12-5547-2015
106. Magmatic Forcing of Cenozoic Climate? P. Sternai et al. 10.1029/2018JB016460
107. Constraining oceanic carbonate chemistry evolution during the Cretaceous-Paleogene transition: Combined benthic and planktonic calcium isotope records from the equatorial Pacific Ocean A. Jouini et al. 10.1016/j.epsl.2023.118305
108. History of Seawater Carbonate Chemistry, Atmospheric CO2, and Ocean Acidification R. Zeebe 10.1146/annurev-earth-042711-105521