[3]Dunbar R B, Cole J E.Annual records of tropical systems(ARTS) recommendations for research. PAGES Workshop Report, 1999(1): 27-29, 49-50
[4]
[4]何学贤,彭子成.珊瑚的古环境信息研究进展.地球科学进展,1999,14(5):505-511
[5]
[5]Druffel E R M, Griffin S. Large variations of surface ocean radiocarbon: evidence of circulation changes in the Southwestern Pacific. Journal of Geophysical Research, 1993(98) :20 249- 20 259
[6]
[6]Toggweiler J R, Dixon K. The Peru upwelling and the ventilation of the South Pacific thermocline. Joumal of Geophysical Research, 1991(96): 20 467- 20 497
[7]
[7]Guiderson T P, Schrag D P. Radiocarbon variability in the western equatorial Pacific inferred from a high - resolution coral record from Nauru Island. Journal of Geophysical Research, 1998(103): 24 641 - 24 650
[8]
[8]Brown T A. Intra - annual variability of the radiocarbon content of corals from the Galapagos Islands. Radiocarbon, 1993(35):245 - 251
[9]
[9]Moore M D, Schrag D P. Coral radiocarbon constraints on the source of the Indonesian throughflow. Journal of Geophysical Research, 1997(102): 12 359- 12 365
[10]
[10]Rodgers K B,Cane MA. Seasonal variability of sea surface 14C in the equatorial Pacific in an ocean circulation model. Journal of Geophysical Research, 1997(102): 18 627- 18 639