@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 {2252,
	title = {High-precision radiocarbon age calibration for terrestrial and marine samples},
	journal = {Radiocarbon},
	volume = {40},
	year = {1998},
	note = {155qrTimes Cited:705
Cited References Count:31
},
	month = {1998},
	pages = {1127-1151},
	abstract = {Single-year and decadal radiocarbon tree-ring ages are tabulated and discussed in terms of C-14 age calibration. The single-year data form the basis of a detailed 14C age calibration curve for the cal AD 1510-1954 interval ("cal" denotes calibrated). The Seattle decadal data set (back to 11,617 cal sp, with 0 sp = AD 1950) is a component of the integrated decadal INTCAL98 C-14 age curve (Stuiver et al. 1998). Atmospheric C-14 ages can be transformed into C-14 ages of the global ocean using a carbon reservoir model. INTCAL98 C-14 ages, used for these calculations, yield global ocean C-14 ages differing slightly from previously published ones (Stuiver and Braziunas 1993b). We include discussions of offsets, error multipliers, regional C-14 age differences and marine C-14 age response to oceanic and atmospheric forcing.},
	keywords = {ad 1950-500 bc, c-14 data, decadal calibration, reservoir ages, time scale},
	isbn = {0033-8222},
	author = {Stuiver, M. and Reimer, P. J. and Braziunas, T. F.}
}
@article {2308,
	title = {Large-volume WOCE radiocarbon sampling in the Pacific Ocean},
	journal = {Radiocarbon},
	volume = {38},
	year = {1996},
	note = {Xd080Times Cited:12
Cited References Count:8
},
	month = {1996},
	pages = {519-561},
	abstract = {At the University of Miami Tritium Laboratory and the University of Washington Quaternary Isotope Laboratory, more than 1000 large-volume Pacific Ocean radiocarbon samples were measured for the WOCE program. Here we present a comprehensive data set, and a brief discussion of our findings.},
	keywords = {geosecs},
	isbn = {0033-8222},
	author = {Stuiver, M. and Ostlund, H. G. and Key, R. M. and Reimer, P. J.}
}
@article {965,
	title = {Ventilation of the deep Pacific Ocean},
	journal = {Supplement to Trans. American Geophysic. Union},
	volume = {76},
	year = {1995},
	note = {id: 41},
	pages = {0S40},
	author = {Key, R. M. and Rooth, C. and Ostlund, G. and Stuiver, M.}
}
