@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.}
}
