1. Petit, J. R. et al. Climate and atmospheric history of the past 420,000 years from the Vostok ice core, Antarctica. Nature 399, 429-436, doi:10.1038/20859 (1999).
2. Sigman, D. M. & Boyle, E. A. Glacial/interglacial variations in atmospheric carbon dioxide. Nature 407, 859-869 (2000).
3. Toggweiler, J. R., Russell, J. L. & Carson, S. R. Midlatitude westerlies, atmospheric CO2, and climate change during the ice ages. Paleoceanography 21 (2006).
4. Marshall, J. & Speer, K. Closure of the meridional overturning circulation through Southern Ocean upwelling. Nature Geoscience (2012).
5. Jaccard, S. L., Galbraith, E. D., Martínez-García, A. & Anderson, R. F. Covariation of deep Southern Ocean oxygenation and atmospheric CO2 through the last ice age. Nature 530, 207-210, doi:10.1038/nature16514 (2016).
6. Gottschalk, J. et al. Biological and physical controls in the Southern Ocean on past millennial-scale atmospheric CO2 changes. Nat Commun 7, doi:10.1038/ncomms11539 (2016).
7. Sigman, D. M., Hain, M. P. & Haug, G. H. The polar ocean and glacial cycles in atmospheric CO2 concentration. Nature 466, 47-55 (2010).
8. Ziegler, M., Diz, P., Hall, I. R. & Zahn, R. Millennial-scale changes in atmospheric CO2 levels linked to the Southern Ocean carbon isotope gradient and dust flux. Nature Geoscience 6, 457-461 (2013).
9. Jaccard, S. L. et al. Subarctic Pacific evidence for a glacial deepening of the oceanic respired carbon pool. Earth and Planetary Science Letters 277, 156-165 (2009).
10. Bradtmiller, L. I., Anderson, R. F., Sachs, J. P. & Fleisher, M. Q. A deeper respired carbon pool in the glacial equatorial Pacific Ocean. Earth and Planetary Science Letters 299, 417-425 (2010).
11. Menviel, L. et al. Poorly ventilated deep ocean at the Last Glacial Maximum inferred from carbon isotopes: A data-model comparison study. Paleoceanography 32, 2-17, doi:https://doi.org/10.1002/2016PA003024 (2017).
12. Talley, L. D. Closure of the global overturning circulation through the Indian, Pacific, and Southern Oceans: Schematics and transports. Oceanography 26, 80-97 (2013).
13. Talley, L. D. in Mechanisms of Global Climate Change at Millennial Time Scales. 1-22 (1999).
Duplessy, J.-C. et al. 13C record of benthic foraminifera in the last interglacial ocean: implications for the carbon cycle and the global deep water circulation. Quaternary Research 21, 225-243 (1984).
14. Lynch-Stieglitz, J., Valley, S. G. & Schmidt, M. W. Temperature-dependent ocean–atmosphere equilibration of carbon isotopes in surface and intermediate waters over the deglaciation. Earth and Planetary Science Letters 506, 466-475 (2019).
15. Sarmiento, J., Gruber, N., Brzezinski, M. & Dunne, J. High-latitude controls of thermocline nutrients and low latitude biological productivity. Nature 427, 56-60 (2004).
16. Charles, C. D. et al. Millennial scale evolution of the Southern Ocean chemical divide. Quaternary Science Reviews 29, 399-409 (2010).
17. Curry, W. B., Duplessy, J. C., Labeyrie, L. D. & Shackleton, N. J. Changes in the distribution of δ13C of deep water ΣCO2 between the Last Glaciation and the Holocene. Paleoceanography & Paleoclimatology 3, 317-341 (1988).
18. Kroopnick, P. The distribution of 13C of ΣCO2 in the world oceans. Deep Sea Research Part A. Oceanographic Research Papers 32, 57-84 (1985).
19. Menviel, L., Mouchet, A., Meissner, K. J., Joos, F. & England, M. H. Impact of oceanic circulation changes on atmospheric δ13CO2. Global Biogeochemical Cycles 29, 1944-1961, doi:https://doi.org/10.1002/2015GB005207 (2015).
20. Tsuchiya, M., Lukas, R., Fine, R. A., Firing, E. & Lindstrom, E. Source waters of the Pacific equatorial undercurrent. Progress in Oceanography 23, 101-147 (1989).
21. Xu, Z., Li, A., Jiang, F. & Xu, F. Geochemical character and material source of sediments in the eastern Philippine Sea. Chinese Science Bulletin 53, 923-931 (2008).
22. Xu, Z. et al. Evolution of East Asian monsoon: Clay mineral evidence in the western Philippine Sea over the past 700kyr. Journal of Asian Earth Sciences 60, 188-196 (2012).
23. Wan, S. et al. History of Asian eolian input to the West Philippine Sea over the last one million years. Palaeogeography, Palaeoclimatology, Palaeoecology 326-328, 152-159, doi:10.1016/j.palaeo.2012.02.015 (2012).
24. Hilde, T. W. & Chao-Shing, L. Origin and evolution of the West Philippine Basin: a new interpretation. Tectonophysics 102, 85-104 (1984).
25. Liu, Z., Zhao, Y., Colin, C., Siringan, F. P. & Wu, Q. Chemical weathering in Luzon, Philippines from clay mineralogy and major-element geochemistry of river sediments. Applied Geochemistry 24, 2195-2205 (2009).
26. Menviel, L. et al. Southern Hemisphere westerlies as a driver of the early deglacial atmospheric CO2 rise. Nature Communications 9, 2503, doi:10.1038/s41467-018-04876-4 (2018).
27. Goosse, H. et al. Description of the Earth system model of intermediate complexity LOVECLIM version 1.2. Geoscientific Model Development 3, 603-633 (2010).
28. Berger, A. Long-term variations of daily insolation and Quaternary climatic changes. Journal of Atmospheric Sciences 35, 2362-2367 (1978).
29. Abe-Ouchi, A., Segawa, T. & Saito, F. Climatic conditions for modelling the Northern Hemisphere ice sheets throughout the ice age cycle. Climate of the Past 3, 423-438 (2007).
30. Tang, Z., Li, T., Chang, F., Nan, Q. & Li, Q. Paleoproductivity evolution in the West Philippine Sea during the last 700 ka. Chinese Journal of Oceanology and Limnology 31, 435-444 (2013).
31. Lisiecki, L. E. & Raymo, M. E. A Pliocene-Pleistocene stack of 57 globally distributed benthic δ18O records. Paleoceanography 20, PA1003, doi:10.1029/2004pa001071 (2005).
32. Thompson, P. R., Be, A. W. H., Duplessy, J.-C. & Shackleton, N. J. Disappearance of pink-pigmented Globigerinoides ruber at 120,000 yr BP in the Indian and Pacific Oceans. Nature 280, 554-558 (1979).
33. Duplessy, J. et al. Deepwater source variations during the last climatic cycle and their impact on the global deepwater circulation. Paleoceanography 3, 343-360 (1988).
34. Graham, D. W., Corliss, B. H., Bender, M. L. & Keigwin Jr, L. D. Carbon and oxygen isotopic disequilibria of recent deep-sea benthic foraminifera. Marine micropaleontology 6, 483-497 (1981).
35. Herguera, J. C. Deep-sea benthic foraminifera and biogenic opal: glacial to postglacial productivity changes in the western equatorial Pacific. Marine Micropaleontology 19, 79-98 (1992).
36. Keigwin, L. D. Glacial‐age hydrography of the far northwest Pacific Ocean. Paleoceanography 13, 323-339 (1998).
37. Matsumoto, K., Oba, T., Lynch-Stieglitz, J. & Yamamoto, H. Interior hydrography and circulation of the glacial Pacific Ocean. Quaternary Science Reviews 21, 1693-1704 (2002).
38. Curry, W. B. & Oppo, D. W. Glacial water mass geometry and the distribution of δ13C of ΣCO2 in the western Atlantic Ocean. Paleoceanography 20 (2005).
39. McCorkle, D. C., Heggie, D. T. & Veeh, H. H. Glacial and Holocene stable isotope distributions in the southeastern Indian Ocean. Paleoceanography 13, 20-34 (1998).
40. Hodell, D. A., Venz, K. A., Charles, C. D. & Ninnemann, U. S. Pleistocene vertical carbon isotope and carbonate gradients in the South Atlantic sector of the Southern Ocean. Geochemistry, Geophysics, Geosystems 4, 1-19 (2003).
41. Ninnemann, U. S. & Charles, C. D. Changes in the mode of Southern Ocean circulation over the last glacial cycle revealed by foraminiferal stable isotopic variability. Earth and Planetary Science Letters 201, 383-396 (2002).
42. Hoogakker, B. A. A., Rohling, E. J., Palmer, M. R., Tyrrell, T. & Rothwell, R. G. Underlying causes for long-term global ocean δ13C fluctuations over the last 1.20 Myr. Earth and Planetary Science Letters 248, 15-29, doi:http://dx.doi.org/10.1016/j.epsl.2006.05.007 (2006).
43. Wolff, E. W. et al. Southern Ocean sea-ice extent, productivity and iron flux over the past eight glacial cycles. Nature 440, 491-496, doi:http://www.nature.com/nature/journal/v440/n7083 (2006).
44. WAIS Divide Project Members. Onset of deglacial warming in West Antarctica driven by local orbital forcing. Nature 500, 440-444 (2013).
45. Anderson, R. et al. Wind-driven upwelling in the Southern Ocean and the deglacial rise in atmospheric CO2. Science 323, 1443-1448 (2009).
46. Skinner, L. C., Fallon, S., Waelbroeck, C., Michel, E. & Barker, S. Ventilation of the deep Southern Ocean and deglacial CO2 rise. Science 328, 1147-1151 (2010).
47. Skinner, L. et al. Reduced ventilation and enhanced magnitude of the deep Pacific carbon pool during the last glacial period. Earth and Planetary Science Letters 411, 45-52, doi:http://dx.doi.org/10.1016/j.epsl.2014.11.024 (2015).
48. Sarnthein, M., Schneider, B. & Grootes, P. M. Peak glacial 14C ventilation ages suggest major draw-down of carbon into the abyssal ocean. Climate of the Past 9, 2595-2614 (2013).
49. Xu, Z. et al. Quantitative estimates of Asian dust input to the western Philippine Sea in the mid‐late Quaternary and its potential significance for paleoenvironment. Geochemistry, Geophysics, Geosystems 16, 3182-3196 (2015).
50. Xiong, Z. et al. Potential role of giant marine diatoms in sequestration of atmospheric CO2 during the Last Glacial Maximum: δ13C evidence from laminated Ethmodiscus rex mats in tropical West Pacific. Global and Planetary Change 108, 1-14 (2013).
51. Boyle, E. A. The role of vertical chemical fractionation in controlling late Quaternary atmospheric carbon dioxide. Journal of Geophysical Research: Oceans 93, 15701-15714, doi:https://doi.org/10.1029/JC093iC12p15701 (1988).
52. Curry, W. B. & Lohmann, G. Carbon isotopic changes in benthic foraminifera from the western South Atlantic: Reconstruction of glacial abyssal circulation patterns. Quaternary Research 18, 218-235 (1982).
53. Faul, K. L., Ravelo, A. C. & Delaney, M. Reconstructions of upwelling, productivity, and photic zone depth in the eastern equatorial Pacific Ocean using planktonic foraminiferal stable isotopes and abundances. The Journal of Foraminiferal Research 30, 110-125 (2000).
54. Spero, H. J. & Lea, D. W. The Cause of Carbon Isotope Minimum Events on Glacial Terminations. Science 296, 522-525, doi:10.1126/science.1069401 (2002).
55. Pena, L. D., Cacho, I., Ferretti, P. & Hall, M. A. El Niño-Southern Oscillation:like variability during glacial terminations and interlatitudinal teleconnections. Paleoceanography 23, PA3101, doi:10.1029/2008pa001620 (2008).
56. Chen, S. et al. Response of the northwestern Pacific upper water δ13C to the last deglacial ventilation of the deep Southern Ocean. Chinese Science Bulletin 56, 2628-2634, doi:10.1007/s11434-011-4590-0 (2011).
57. Shao, J. et al. The Atmospheric Bridge Communicated the δ 13 C Decline during the Last Deglaciation to the Global Upper Ocean. Climate of the Past Discussions, 1-28 (2020).
58. Siani, G. et al. Carbon isotope records reveal precise timing of enhanced Southern Ocean upwelling during the last deglaciation. Nature communications 4 (2013).
59. Schmitt, J. et al. Carbon isotope constraints on the deglacial CO2 rise from ice cores. Science 336, 711-714 (2012).
60. Okazaki, Y. et al. Deepwater formation in the North Pacific during the last glacial termination. Science 329, 200-204 (2010).
61. McManus, J. F., Francois, R., Gherardi, J. M., Keigwin, L. D. & Brown-Leger, S. Collapse and rapid resumption of Atlantic meridional circulation linked to deglacial climate changes. Nature 428, 834-837, doi:http://www.nature.com/nature/journal/v428/n6985/suppinfo/nature02494_S1.html (2004).
62. Zhang, X., Lohmann, G., Knorr, G. & Xu, X. Different ocean states and transient characteristics in Last Glacial Maximum simulations and implications for deglaciation. Clim. Past 9, 2319-2333, doi:10.5194/cp-9-2319-2013 (2013).
63. Ng, H. C. et al. Coherent deglacial changes in western Atlantic Ocean circulation. Nature Communications 9, 2947, doi:10.1038/s41467-018-05312-3 (2018).
64. Laepple, T., Werner, M. & Lohmann, G. Synchronicity of Antarctic temperatures and local solar insolation on orbital timescales. Nature 471, 91-94 (2011).
65. Stephens, B. B. & Keeling, R. F. The influence of Antarctic sea ice on glacial-interglacial CO2 variations. Nature 404, 171-174 (2000).
66. Law, M., Matear, J. & Francey, J, Comment on" Saturation of the Southern Ocean CO2 Sink Due to Recent Climate Change" Science 319, 570-570(2008).
67. Toggweiler, J. R. & Russell, J. Ocean circulation in a warming climate. Nature 451, 286-288 (2008).
68. Govin, A. et al. Evidence for northward expansion of Antarctic Bottom Water mass in the Southern Ocean during the last glacial inception. Paleoceanography 24 (2009).
69. Tang, Z. et al. Deglacial biogenic opal peaks revealing enhanced Southern Ocean upwelling during the last 513 ka. Quaternary International 425, 445-452, doi:https://doi.org/10.1016/j.quaint.2016.09.020 (2016).
70. Meckler, A. et al. Deglacial pulses of deep-ocean silicate into the subtropical North Atlantic Ocean. Nature 495, 495-498 (2013).
71. Rae, J. W. B. et al. Deep water formation in the North Pacific and deglacial CO2 rise. Paleoceanography 29, 645-667, doi:https://doi.org/10.1002/2013PA002570 (2014).
72. Barker, S. et al. Icebergs not the trigger for North Atlantic cold events. Nature 520, 333-336, doi:10.1038/nature14330 (2015)
73. Broecker, W., Clark, E. & Barker, S. Near constancy of the Pacific Ocean surface to mid-depth radiocarbon-age difference over the last 20 kyr. Earth and Planetary Science Letters 274, 322-326 (2008).
74. Hain, M. P., Sigman, D. M. & Haug, G. H. Shortcomings of the isolated abyssal reservoir model for deglacial radiocarbon changes in the mid‐depth Indo‐Pacific Ocean. Geophysical Research Letters 38 (2011).
75. Droxler, A. W., Alley, R. B., Howard, W. R., Poore, R. Z., & Burckle, L. H. Unique and exceptionally long interglacial marine isotope stage 11: Window into Earth warm future climate. Earth’s Climate and Orbital Eccentricity: The Marine Isotope Stage 11 Question., 1-14 (2003).
76. Martínez-Botí, M. A. et al. Boron isotope evidence for oceanic carbon dioxide leakage during the last deglaciation. Nature 518, 219-222, doi:10.1038/nature14155 (2015).
77. Boyle, E. A. Vertical oceanic nutrient fractionation and glacial/interglacial CO2 cycles. Nature 331, 55, doi:10.1038/331055a0 (1988b).
78. Qin, B., Li, T., Xiong, Z., Algeo, T. & Jia, Q. Deep‐Water Carbonate Ion Concentrations in the Western Tropical Pacific Since the Mid‐Pleistocene: A Major Perturbation During the Mid‐Brunhes. Journal of Geophysical Research: Oceans 123, 6876-6892 (2018).
79. Hodell, D. A., Charles, C. D. & Sierro, F. J. Late Pleistocene evolution of the ocean's carbonate system. Earth and Planetary Science Letters 192, 109, doi:10.1016/s0012-821x(01)00430-7 (2001).
80. Key, R. M. et al. A global ocean carbon climatology: Results from Global Data Analysis Project (GLODAP). Global biogeochemical cycles 18 (2004).
81. Schlitzer, R. Ocean Data View, https://odv.awi.de. (2020).
82. Martínez-Garcia, A. et al. Southern Ocean dust–climate coupling over the past four million years. Nature 476, 312-315 (2011).
83. Bazin, L. et al. An optimized multi-proxy, multi-site Antarctic ice and gas orbital chronology (AICC2012): 120–800 ka. Climate of the Past 9, 1715-1731 (2013).
84. Siegenthaler, U. et al. Stable Carbon Cycle : Climate Relationship During the Late Pleistocene. Science 310, 1313-1317, doi:10.1126/science.1120130 (2005).