64 citations as recorded by crossref.

1. Ventilation of Northern and Southern Sources of Aged Carbon in the Eastern Equatorial Pacific During the Younger Dryas Rise in Atmospheric CO 2 S. Bova et al. 10.1029/2018PA003386
2. Mysteriously high Δ<sup>14</sup>C of the glacial atmosphere: influence of <sup>14</sup>C production and carbon cycle changes A. Dinauer et al. 10.5194/cp-16-1159-2020
3. A Three-Dimensional Model of the Marine Nitrogen Cycle during the Last Glacial Maximum Constrained by Sedimentary Isotopes C. Somes et al. 10.3389/fmars.2017.00108
4. Deglacial subarctic Pacific surface water hydrography and nutrient dynamics and links to North Atlantic climate variability and atmospheric CO2 E. Maier et al. 10.1002/2014PA002763
5. On Quaternary glaciations, observations and theories D. Paillard 10.1016/j.quascirev.2015.05.017
6. Trace metal evidence for a poorly ventilated glacial Southern Ocean M. Wagner & I. Hendy 10.1016/j.quascirev.2017.06.014
7. Changes in monsoon-driven upwelling in the South China Sea over glacial Terminations I and II: a multi-proxy record H. Sadatzki et al. 10.1007/s00531-015-1227-6
8. Large Variability of Dissolved Inorganic Radiocarbon in the Kuroshio Extension of the Northwest North Pacific L. Ding et al. 10.1017/RDC.2017.143
9. The Biological Pump During the Last Glacial Maximum E. Galbraith & L. Skinner 10.1146/annurev-marine-010419-010906
10. Deglacial weakening of the oceanic soft tissue pump: global constraints from sedimentary nitrogen isotopes and oxygenation proxies E. Galbraith & S. Jaccard 10.1016/j.quascirev.2014.11.012
11. Ice sheet dynamics on the Lofoten–Vesterålen shelf, north Norway, from Late MIS-3 to Heinrich Stadial 1 J. Brendryen et al. 10.1016/j.quascirev.2015.03.015
12. Enhanced δ13C and δ18O Differences Between the South Atlantic and South Pacific During the Last Glaciation: The Deep Gateway Hypothesis E. Sikes et al. 10.1002/2017PA003118
13. Comparing dust flux records from the Subarctic North Pacific and Greenland: Implications for atmospheric transport to Greenland and for the application of dust as a chronostratigraphic tool S. Serno et al. 10.1002/2014PA002748
14. Burial-nutrient feedbacks amplify the sensitivity of atmospheric carbon dioxide to changes in organic matter remineralisation R. Roth et al. 10.5194/esd-5-321-2014
15. Poorly ventilated deep ocean at the Last Glacial Maximum inferred from carbon isotopes: A data-model comparison study L. Menviel et al. 10.1002/2016PA003024
16. Deep‐Sea Oxygen Depletion and Ocean Carbon Sequestration During the Last Ice Age R. Anderson et al. 10.1029/2018GB006049
17. Deep water formation in the North Pacific and deglacial CO2rise J. Rae et al. 10.1002/2013PA002570
18. Impact of North Atlantic Freshwater Forcing on the Pacific Meridional Overturning Circulation under Glacial and Interglacial Conditions H. Kim & S. An 10.1175/JCLI-D-19-0065.1
19. Increased reservoir ages and poorly ventilated deep waters inferred in the glacial Eastern Equatorial Pacific M. de la Fuente et al. 10.1038/ncomms8420
20. Deep water exchanges between the South China Sea and the Pacific since the last glacial period S. Wan & Z. Jian 10.1002/2013PA002578
21. Complementary constraints from carbon ( 13 C) and nitrogen ( 15 N) isotopes on the glacial ocean's soft‐tissue biological pump A. Schmittner & C. Somes 10.1002/2015PA002905
22. Modeling the contribution of dissolved organic carbon to carbon sequestration during the last glacial maximum W. Ma & J. Tian 10.1007/s00367-014-0378-y
23. Radiocarbon evidence for enhanced respired carbon storage in the Atlantic at the Last Glacial Maximum E. Freeman et al. 10.1038/ncomms11998
24. Radiocarbon constraints on the extent and evolution of the South Pacific glacial carbon pool T. Ronge et al. 10.1038/ncomms11487
25. Deep Pacific storage of respired carbon during the last ice age: Perspectives from bottom water oxygen reconstructions A. Jacobel et al. 10.1016/j.quascirev.2019.106065
26. Refined modeling and14C plateau tuning reveal consistent patterns of glacial and deglacial14C reservoir ages of surface waters in low-latitude Atlantic S. Balmer et al. 10.1002/2016PA002953
27. Pulses of enhanced North Pacific Intermediate Water ventilation from the Okhotsk Sea and Bering Sea during the last deglaciation L. Max et al. 10.5194/cp-10-591-2014
28. North Pacific Intermediate Water circulation enhanced by the closure of the Bering Strait K. Knudson & A. Ravelo 10.1002/2015PA002840
29. 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
30. Bottom water variability in the subtropical northwestern Pacific from 26 kyr BP to present based on Mg / Ca and stable carbon and oxygen isotopes of benthic foraminifera Y. Kubota et al. 10.5194/cp-11-803-2015
31. Integrating palaeoclimate time series with rich metadata for uncertainty modelling: strategy and documentation of the PalMod 130k marine palaeoclimate data synthesis L. Jonkers et al. 10.5194/essd-12-1053-2020
32. Evolution of the Global Overturning Circulation since the Last Glacial Maximum based on marine authigenic neodymium isotopes J. Du et al. 10.1016/j.quascirev.2020.106396
33. Air-sea disequilibrium enhances ocean carbon storage during glacial periods S. Khatiwala et al. 10.1126/sciadv.aaw4981
34. Burial-nutrient feedbacks amplify the sensitivity of carbon dioxide to changes in organic matter remineralisation R. Roth et al. 10.5194/esdd-5-473-2014
35. Trace metal evidence for a poorly ventilated glacial Southern Ocean M. Wagner & I. Hendy 10.5194/cpd-11-637-2015
36. A Synthesis of Deglacial Deep-Sea Radiocarbon Records and Their (In)Consistency With Modern Ocean Ventilation N. Zhao et al. 10.1002/2017PA003174
37. Deglacial upwelling, productivity and CO2 outgassing in the North Pacific Ocean W. Gray et al. 10.1038/s41561-018-0108-6
38. Authigenic Nd isotope record of North Pacific Intermediate Water formation and boundary exchange on the Bering Slope K. Jang et al. 10.1016/j.quascirev.2016.11.032
39. Weak overturning circulation and high Southern Ocean nutrient utilization maximized glacial ocean carbon J. Muglia et al. 10.1016/j.epsl.2018.05.038
40. Planktic and Benthic 14C Reservoir Ages for Three Ocean Basins, Calibrated by a Suite of 14C Plateaus in the Glacial-to-Deglacial Suigetsu Atmospheric 14C Record M. Sarnthein et al. 10.2458/azu_rc.57.17916
41. Laminated sediments in the Bering Sea reveal atmospheric teleconnections to Greenland climate on millennial to decadal timescales during the last deglaciation H. Kuehn et al. 10.5194/cp-10-2215-2014
42. Refining the Icelandic tephrachronology of the last glacial period – The deep-sea core PS2644 record from the southern Greenland Sea A. Voelker & H. Haflidason 10.1016/j.gloplacha.2015.05.001
43. Phasing of millennial-scale climate variability in the Pacific and Atlantic Oceans M. Walczak et al. 10.1126/science.aba7096
44. The glacial mid-depth radiocarbon bulge and its implications for the overturning circulation A. Burke et al. 10.1002/2015PA002778
45. Late Glacial to Holocene radiocarbon constraints on North Pacific Intermediate Water ventilation and deglacial atmospheric CO2 sources M. Davies-Walczak et al. 10.1016/j.epsl.2014.04.004
46. Whole‐Ocean Changes in Silica and Ge/Si Ratios During the Last Deglacial Deduced From Long‐Lived Giant Glass Sponges K. Jochum et al. 10.1002/2017GL073897
47. Coupled climate–carbon cycle simulation of the Last Glacial Maximum atmospheric CO<sub>2</sub> decrease using a large ensemble of modern plausible parameter sets K. Kemppinen et al. 10.5194/cp-15-1039-2019
48. Persistently well-ventilated intermediate-depth ocean through the last deglaciation T. Chen et al. 10.1038/s41561-020-0638-6
49. Effects of eustatic sea-level change, ocean dynamics, and iron fertilization on atmospheric <i>p</i>CO<sub>2</sub> and seawater composition over the last 130 000 years K. Wallmann et al. 10.5194/cpd-11-2405-2015
50. Effects of eustatic sea-level change, ocean dynamics, and nutrient utilization on atmospheric <i>p</i>CO<sub>2</sub> and seawater composition over the last 130 000 years: a model study K. Wallmann et al. 10.5194/cp-12-339-2016
51. Low terrestrial carbon storage at the Last Glacial Maximum: constraints from multi-proxy data A. Jeltsch-Thömmes et al. 10.5194/cp-15-849-2019
52. Deep-water carbonate dissolution in the northern South China Sea during Marine Isotope Stage 3 N. Wang et al. 10.1016/j.jop.2015.11.004
53. Biological and physical controls in the Southern Ocean on past millennial-scale atmospheric CO2 changes J. Gottschalk et al. 10.1038/ncomms11539
54. Magnetic Fingerprints of Modern Sediments in the South China Sea Resulting From Source‐to‐Sink Processes C. Kissel et al. 10.1029/2018GC007571
55. Rapid Loss of CO 2 From the South Pacific Ocean During the Last Glacial Termination K. Allen et al. 10.1029/2019PA003766
56. Laminated sediments in the Bering Sea reveal atmospheric teleconnections to Greenland climate on millennial to decadal timescales during the last deglaciation H. Kuehn et al. 10.5194/cpd-10-2467-2014
57. Selection and Treatment of Data for Radiocarbon Calibration: An Update to the International Calibration (IntCal) Criteria P. Reimer et al. 10.2458/azu_js_rc.55.16955
58. Radiocarbon constraints on the glacial ocean circulation and its impact on atmospheric CO2 L. Skinner et al. 10.1038/ncomms16010
59. 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 10.1007/s00382-018-4157-8
60. Stratigraphic gaps at northern South China Sea margin reflect changes in Pacific deepwater inflow at glacial Termination II M. Sarnthein et al. 10.1007/s11430-013-4678-2
61. Glacial-to-deglacial changes in North Atlantic meltwater advection and deep-water formation – Centennial-to-millennial-scale 14C records from the Azores plateau S. Balmer & M. Sarnthein 10.1016/j.gca.2018.03.001
62. IntCal13 and Marine13 Radiocarbon Age Calibration Curves 0–50,000 Years cal BP P. Reimer et al. 10.2458/azu_js_rc.55.16947
63. Pulses of enhanced North Pacific Intermediate Water ventilation from the Okhotsk Sea and Bering Sea during the last deglaciation L. Max et al. 10.5194/cpd-9-6221-2013
64. Reduced ventilation and enhanced magnitude of the deep Pacific carbon pool during the last glacial period L. Skinner et al. 10.1016/j.epsl.2014.11.024