[1]Abrantes F. 2000. 200,000 yr diatom records from Atlantic upwelling sites reveal maximum productivity during LGM and a shift in phytoplankton community structure at 185,000 yr. Earth and Planetary Science Letters 176(1):7.16.
[2]Ascough PL, Cook GT, Dugmore AJ. 2009. North Atlantic marine 14C reservoir effects: implications for late- Holocene chronological studies. Quaternary Geochronology 4(3):171.80.
[3]Austin WEN, Wilson LJ, Hunt JB. 2004. The age and chronostratigraphical significance of North Atlantic Ash Zone II. Journal of Quaternary Science 19(2): 137.46.
[4]Austin WEN, Abbott PM. In press. Comment: .Were last glacial climate events simultaneous between Greenland and France? A quantitative comparison using non-tuned chronologies. by Blaauw M, Wohlfarth B, Christen JA, Ampel L, Veres D, Hughen K, Preusser F, Svensson A. Journal of Quaternary Science doi: 10.1002/jqs.1366.
[5]Bard E, Arnold M, Hamelin B, Tisnerat-Laborde N, Cabioch G. 1998. Radiocarbon calibration by means of mass spectrometric 230Th/234U and 14C ages of corals: an updated database including samples from Barbados, Mururoa and Tahiti. Radiocarbon 40(3):1085. 92.
[6]Bard E, Ménot-Combes G, Rostek F. 2004a. Present status of radiocarbon calibration and comparison records based on Polynesian corals and Iberian Margin sediments. Radiocarbon 46(3):1189.202.
[7]Bard E, Rostek F, Ménot-Combes G. 2004b. A better radiocarbon clock. Science 303(5655):178.9.
[8]Bard E, Rostek F, Ménot-Combes G. 2004c. Radiocarbon calibration beyond 20,000 14C yr B.P. by means of planktonic foraminifera of the Iberian Margin. Quaternary Research 61(2):204.14.
[9]Bard E, Menot G, Licari L. 2009. Radiocarbon calibration- comparison records based on marine sediments from the Pakistan and Iberian Margins. Geophysical Research Abstracts 11:EGU2009-6985.
[10]Beck JW, Richards DA, Edwards RL, Silverman BW, Smart PL, Donahue DJ, Herrera-Osterheld S, Burr GS, Calsoyas L, Jull AJT, Biddulph D. 2001. Extremely large variations of atmospheric 14C concentration during the last glacial period. Science 292(5526): 2453.8.
[11]Björck S, Koç N, Skog G. 2003. Consistently large marine reservoir ages in the Norwegian Sea during the Last Deglaciation. Quaternary Science Reviews 22(5.7):429.35.
[12]Blaauw M, Wohlfarth B, Christen JA, Ampel L, Veres D, Hughen KA, Preusser F, Svensson A. 2009. Were last glacial climate events simultaneous between Greenland and France? A quantitative comparison using non-tuned chronologies. Journal of Quaternary Science 24: doi: 10.1002/jqs.330.
[13]Blackwell PG, Buck CE. 2008a. Estimating radiocarbon calibration curves: rejoinder. Bayesian Analysis 3(2): 263.8.
[14]Blackwell PG, Buck CE. 2008b. Estimating radiocarbon calibration curves. Bayesian Analysis 3(2):225.48.
[15]Blockley SPE, Housley RA. 2009. Calibration commentary. Radiocarbon 51(1):287.90.