@article {2070,
	title = {Changes of the 13C/12C of dissolved inorganic carbon in the ocean as a tracer of anthropogenic C)2 uptake},
	journal = {Global Biogeochemical Cycles},
	volume = {17},
	year = {2003},
	note = {id: 1689},
	month = {2003},
	author = {Quay, P. D. and Sonnerup, T. and Westby, J. and Stutsman, J. and McNichol, A. P.}
}
@article {2105,
	title = {Changes in the 13C/12C of dissolved inorganic carbon in the ocean as a tracer of anthropogenic CO2 uptake},
	journal = {Global Biogeochemical Cycles},
	volume = {17},
	year = {2002},
	note = {id: 1715},
	month = {2002},
	pages = {4-1 - 4-20},
	author = {Quay, P. D. and Sonnerup, R. and Westby, T. and Stutsman, J. and McNichol, A. P.}
}
@article {1522,
	title = {U. S. WOCE Indian Ocean survey: Final report for radiocarbon, Ocean Tracer Laboratory Tech. Report $\#$902-1},
	year = {2002},
	note = {id: 528},
	month = {2002},
	pages = {22 pp.},
	author = {Key, R. M. and Quay, P. D.}
}
@article {966,
	title = {WOCE radiocarbon IV: Pacific Ocean results; P10, P13N, P14C, P18, P19 \& S4P},
	journal = {Radiocarbon},
	volume = {44},
	year = {2002},
	note = {591keTimes Cited:33Cited References Count:56},
	pages = {239-392},
	abstract = {The World Ocean Circulation Experiment, carried out between 1990 and 1997, provided the most comprehensive oceanic survey of radiocarbon to date. Approximately 10,000 samples were collected in the Pacific Ocean by U.S. investigators for both conventional large volume P counting and small volume accelerator mass spectrometry analysis techniques. Results from six cruises are presented. The data quality is as good or better than previous large-scale surveys. The C-14 distribution for the entire WOCE Pacific data set is graphically described using mean vertical profiles and sections, and property-property plots.},
	issn = {0033-8222},
	url = {https://journals.uair.arizona.edu/index.php/radiocarbon/article/view/4097},
	author = {Key, R. M. and Quay, P. D. and Schlosser, P. and McNichol, A. P. and von Reden, K. F. and Schneider, R. J. and Elder, K. L. and Stuiver, M. and Ostlund, H. G.}
}
@article {2168,
	title = {The Indian Ocean 13C Suess effect},
	journal = {Global Biogeochemical Cycles},
	volume = {14},
	year = {2000},
	note = {id: 1816},
	month = {2000},
	pages = {903-916},
	author = {Sonnerup, R. E. and Quay, P. D. and McNichol, A. P.}
}
@conference {1716,
	title = {An ocean-wide DIC-13 data set},
	booktitle = {AGU Ocean Sciences Meeting},
	year = {2000},
	note = {id: 1444},
	month = {2000},
	address = {San Antonio, TX},
	author = {McNichol, A. P. and Quay, P. D. and Stuart, D. R. and Sonnerup, R. E. and Key, R. M.}
}
@conference {1767,
	title = {The radiocarbon gradient at the Antarctic Polar Front},
	booktitle = {AGU Ocean Sciences Meeting},
	year = {2000},
	note = {id: 317},
	month = {2000},
	address = {San Antonio, TX},
	author = {Schneider, R. J. and McNichol, A. P. and von Reden, K. F. and Elder, K. L. and Gagnon, A. R. and Key, R. M. and Quay, P. D. and Schlosser, P. M.}
}
@conference {1804,
	title = {Ten years after - the WOCE AMS radiocarbon program},
	booktitle = {Accelerator Mass Spectrometer Conference},
	year = {2000},
	note = {id: 316},
	month = {2000},
	author = {McNichol, A. P. and Schneider, R. J. and von Reden, K. F. and Gagnon, A. R. and Elder, K. L. and Key, R. M. and Quay, P. D.}
}
@article {810,
	title = {Ten years after - The WOCE AMS radiocarbon program},
	journal = {Nuclear Instruments \& Methods in Physics Research Section B-Beam Interactions with Materials and Atoms},
	volume = {172},
	year = {2000},
	note = {372jrTimes Cited:14Cited References Count:12},
	month = {Oct},
	pages = {479-484},
	abstract = {The National Ocean Sciences Accelerator Mass Spectrometry (NOSAMS) Facility is measuring all of the samples collected as part of the US WOCE Program - over 13,000 samples. We designed our extraction lines so that we also measure precise, oceanographically useful delta C-13-Sigma CO2 values. We have completed the analysis of samples from the Pacific and Southern Oceans and are processing those from the Indian Ocean now. At present, this constitutes the world{\textquoteright}s largest AMS data set. Reviews of the Pacific radiocarbon data are available and demonstrate the increased penetration of the "bomb signal" into the water column since the 1970s. Stable isotope data are being combined with those collected as part of NOAA{\textquoteright}s Ocean-Atmosphere Carbon Exchange Study to study the ocean{\textquoteright}s role in the anthropogenic CO2 cycle. The relationship of delta C-13 to other chemical tracers, e.g., PO4, O-2 and chlorofluorocarbons, will further our understanding of basic oceanographic processes. We present preliminary results from these studies as well as investigate the relationship of C-14 to C-13 in the ocean. (C) 2000 Elsevier Science B.V. All rights reserved.},
	issn = {0168-583x},
	doi = {10.1016/S0168-583x(00)00093-8},
	author = {McNichol, A. P. and Schneider, R. J. and von Reden, K. F. and Gagnon, A. R. and Elder, K. L. and Key, R. M. and Quay, P. D.}
}
@article {2212,
	title = {Reconstructing the oceanic 13C Suess effect},
	journal = {Global Biogeochemical Cycles},
	volume = {13},
	year = {1999},
	note = {id: 1710},
	month = {1999},
	pages = {857-872},
	author = {Sonnerup, R. E. and Quay, P. D. and McNichol, A. P. and Bullister, J. L. and Westby, T. A. and Anderson, H. L.}
}
@article {969,
	title = {P13N final report for AMS 14C samples},
	journal = {Ocean Tracer Laboratory Technical Report},
	volume = {97},
	year = {1997},
	note = {id: 1254},
	pages = {11},
	author = {Key, R. M. and Quay, P. D.}
}
@article {967,
	title = {WOCE AMS Radiocarbon I: Pacific Ocean results (P6, P16, and P17)},
	journal = {Radiocarbon},
	volume = {38},
	year = {1996},
	note = {id: 38},
	pages = {425-518},
	abstract = {AMS radiocarbon results from the World Ocean Circulation Experiment in the Pacific Ocean show dramatic changes in the inventory and distribution of bomb-produced 14C since the time of the GEOSECS survey (8/73-6/74). Nearsurface 4C values for the eastern portion of both the northern and southern subtropical gyres decreased by 25-50\%, with the change being greater in the north. Equatorial near-surface values have increased by ca. 25\%. Changes in the 250-750-m depth range are dramatically different between the northern and southern basins. The intermediate and mode waters of the
southern basin have increased by as much as 75\%o since GEOSECS. Waters of similar density in the northern hemisphere are not exposed to the Southern Ocean circulation regime and are significantly less ventilated, showing maximum changes of ca. 50\%.
},
	url = {https://journals.uair.arizona.edu/index.php/radiocarbon/article/view/1918},
	author = {Key, R. M. and Quay, P. D. and Jones, G. A. and McNichol, A. P. and von Reden, K. F. and Schneider, R. J.}
}
@article {1368,
	title = {Thermocline Ventilation Rates in the North Pacific},
	year = {1994},
	note = {id: 917},
	month = {1994},
	author = {Sonnerup, R. E. and Quay, P. D. and Bullister, J. L. and Key, R. M. and McNichol, A. P. and Jones, G. A.}
}
