@article {838,
	title = {Radiocarbon Chronology of Black-Sea Sediments},
	journal = {Deep-Sea Research Part I-Oceanographic Research Papers},
	volume = {41},
	year = {1994},
	note = {Nm252Times Cited:121Cited References Count:44},
	month = {Mar},
	pages = {531-557},
	abstract = {Accelerator Mass Spectrometer (AMS) radiocarbon analyses have been made on 102 samples from 12 sediment cores and 23 samples from two water column profiles. These materials, collected during the first leg of the 1988 joint U.S.-Turkish Black Sea Expedition, provide the most comprehensive radiocarbon chronology of Black Sea sediments vet attempted. Radiocarbon analyses from carefully collected box cores and a molluse shell collected live in 1931 suggest the prebomb surface waters had a DELTAC-14 value of -55 parts per thousand (460 years) and that the maximum detrital correction for radiocarbon ages of Unit I sediments is 580 years for the organic carbon and 260 years for the carbonate fractions. Evidence does not support the 1430-2000 year pre-bomb surface water and/or detrital corrections argued for in past studies. The best estimates for the age of the beginning of the final invasion of the coccolithophore Emiliania huxleyi (Unit 1/2 boundary of Ross and DEGENS, 1974, The Black Sea-geology, chemistry and biology, pp. 183-199) and the age of the first invasion of E. huxleyi (Unit I/II boundary of HAY et al., 1991, Deep-Sea Research, 38, S1211-S1235) are 1635 +/- 60 and 2720 +/- 160 years BP, respectively. Sapropel formation began at approximately 7540 +/- 130 years BP at all depths in the basin, a pattern in disagreement with those predicted by existing time-evolution models of sapropel formation for this basin. Our data suggest that the oxic-anoxic interface has remained relatively stable throughout the Holocene, is controlled largely by the physical oceanography of the basin, and has not evolved as assumed by previous workers.},
	issn = {0967-0637},
	doi = {10.1016/0967-0637(94)90094-9},
	author = {Jones, G. A. and Gagnon, A. R.}
}
@article {2371,
	title = {Rapid analysis of seawater samples at the National Ocean Sciences Accelerator Mass Spectrometry Facility, Woods Hole, MA},
	journal = {Radiocarbon},
	volume = {36},
	year = {1994},
	note = {id: 305},
	month = {1994},
	pages = {237-246},
	author = {McNichol, A. P. and Jones, G. A. and Hutton, D. L. and Gagnon, A. R. and Key, R. M.}
}
@article {2369,
	title = {The Rapid Preparation of Seawater Sigma-Co2 for Radiocarbon Analysis at the National Ocean Sciences Ams Facility},
	journal = {Radiocarbon},
	volume = {36},
	year = {1994},
	note = {Pz926Times Cited:61
Cited References Count:14
},
	month = {1994},
	pages = {237-246},
	abstract = {We have established a laboratory for extracting Sigma CO2 from seawater samples for AMS analysis of the radiocarbon content. The seawater samples are collected at sea, poisoned and stored until analysis in the laboratory. Each sample is acidified; the inorganic carbon is stripped out as CO2 with an inert carrier gas and then converted to graphite. We present results for Buzzards Bay surface H2O and Na2CO3 standards that demonstrate we strip > 98\% of inorganic carbon from seawater. Stable isotope analyses are performed to better than 0.2 parts per thousand, and the reproducibility of C-14 measurements on Buzzards Bay seawater is better than 13 parts per thousand. Finally, we compare data from samples collected in 1991 to those collected in the 1970s and to large volume samples.},
	keywords = {accelerator mass-spectrometry, C-14, samples},
	isbn = {0033-8222},
	author = {McNichol, A. P. and Jones, G. A. and Hutton, D. L. and Gagnon, A. R. and Key, R. M.}
}
@article {2389,
	title = {Radiocarbon ages from two submerged strandline features in the western Gulf of Maine and a sea-level curve for the northeastern Massachusetts coastal region},
	journal = {Quaternary Research},
	volume = {40},
	year = {1993},
	note = {id: 10},
	month = {1993},
	pages = {38-45},
	author = {Oldale, R. N. and Colman, S. M. and Jones, G. A.}
}
@article {2395,
	title = {Radiocarbon dating of Lake Baikal sediments--A progress report},
	journal = {Russian Geology and Geophysics},
	volume = {34},
	year = {1993},
	note = {id: 191},
	month = {1993},
	pages = {55-63},
	author = {Colman, S. M. and Kuptsov, V. M. and Jones, G. A. and Carter, S. J.}
}
@conference {1771,
	title = {Radiocarbon time histories from long-lived molluscs using accelerator mass-spectrometry},
	booktitle = {6th International Conference on Accelerator Mass Spectrometry},
	year = {1993},
	note = {id: 1296},
	month = {1993},
	pages = {133},
	address = {Sydney, Australia},
	author = {Weidman, C. R. and Jones, G. A.}
}
@conference {1780,
	title = {Role of the United States National Ocean Sciences Accelerator Mass Spectrometry Facility in Global Climate Change Studies},
	booktitle = {International Symposium on Applications of Isotope Techniques in Studying Past and Current Environmental Change in the Hydrosphere and the Atmosphere},
	year = {1993},
	note = {id: 928},
	month = {1993},
	address = {Vienna},
	author = {Jones, G. A. and Schneider, R. J. and von Reden, K. F. and McNichol, A. P.}
}
@article {2400,
	title = {Rapid Analysis of Seawater Inorganic Carbon at the National Ocean Sciences AMS Facility: Progress and Preliminary Results (abstract)},
	journal = {EOS, Transactions of the American Geophysical Union Meeting},
	volume = {72},
	year = {1992},
	note = {id: 1655},
	month = {1992},
	author = {McNichol, A. P. and Jones, G. A. and Schneider, R. J. and von Reden, K. F. and Key, R. M.}
}
@article {2408,
	title = {Response of G. quinqueloba to Hypsithermal warming in the Norwegian-Greenland Sea (abstract)},
	journal = {EOS, Transactions, American Geophysical Union},
	volume = {71},
	year = {1991},
	note = {id: 1759},
	month = {1991},
	author = {Jones, G. A. and Elder, K. L.}
}
@conference {1779,
	title = {Response of the Norwegian-Greenland Sea to Mid-Holocen warming (abstract)},
	booktitle = {20th Arctic Workshoip, INSTAAR},
	year = {1991},
	note = {id: 1760},
	month = {1991},
	address = {Fairbanks, AL},
	author = {Jones, G. A. and Elder, K. L.}
}
