408
Walter et al.
Stuiver M, Quay PD, Ostlund HG (1984) Abyssal water
carbon-14 distributions and the age of the world
oceans. Science 219: 849-851
Suman DO, Bacon MP (1989) Variations in Holocene
sedimentation in the North American Basin determined from Th-23 0 measurements. Deep-Sea Res 36:
869-878
Taguchi K, Harada K, Tsunogai S (1989) Particulate removal of2JoTh and mPa in the biological productive
northern North Pacific. Earth Planet Sci Lett 93:
223-232
Vogler S, Scholten J, Rutgers van der LoeffM, Mangini
A (subm) 2 J OTh in the eastern North Atlantic: the importance of water mass ventilation in the balance of
2JOTh. Earth Planet Sci Lett, subm
Walter HJ, Rutgers van der LoeffMM, Hoeltzen H (1997)
Enhanced scavenging of 2J1 Pa relative to 2JOTh in the
South Atlantic south of the Polar Front. Implications for the use of the 2Jl Paj2JOTh ratio as a
paleoproductivity proxy. Earth Planet. Sci Lett 149:
85-100
WeferG (1989) Particle flux in the ocean: effects ofepisodic production. In: Berger WH, Smetacek V, Wefer
G (eds) Productivity of the Ocean: Present and Past.
J Wiley & Sons, Chichester, pp 139-154
Wefer G, Fischer G (1991) Annual primary production and
export flux in the Southern Ocean from sediment trap
data. MarChem35: 597-614
YangH-S, Nozaki Y, SakaiH, Masuda A (1986) The distribution 0[2 30 Th and 231 Pa in the deep-sea surface
sediments of the Pacific Ocean. Geochim Cosmochim
Acta 50: 81-89
Yang Y -L, Elderfeld H, Pederson TF (1995) Geochemical
record of the Panama basin during the last glacial
maximum carbon event shows that the glacial ocean
was not suboxic. Geology 23: 1115-1118
Yu EF (1994) Variations in the particulate flux 0[2 30 Th
and m Pa and paleoceanographic applications of the
mpa/ 2J oTh ratio. PhD Thesis, WHOI, Woods Hole,
MA,pp 1-269
Yu EF, Fran,
689-694
Walter et al.
Stuiver M, Quay PD, Ostlund HG (1984) Abyssal water
carbon-14 distributions and the age of the world
oceans. Science 219: 849-851
Suman DO, Bacon MP (1989) Variations in Holocene
sedimentation in the North American Basin determined from Th-23 0 measurements. Deep-Sea Res 36:
869-878
Taguchi K, Harada K, Tsunogai S (1989) Particulate removal of2JoTh and mPa in the biological productive
northern North Pacific. Earth Planet Sci Lett 93:
223-232
Vogler S, Scholten J, Rutgers van der LoeffM, Mangini
A (subm) 2 J OTh in the eastern North Atlantic: the importance of water mass ventilation in the balance of
2JOTh. Earth Planet Sci Lett, subm
Walter HJ, Rutgers van der LoeffMM, Hoeltzen H (1997)
Enhanced scavenging of 2J1 Pa relative to 2JOTh in the
South Atlantic south of the Polar Front. Implications for the use of the 2Jl Paj2JOTh ratio as a
paleoproductivity proxy. Earth Planet. Sci Lett 149:
85-100
WeferG (1989) Particle flux in the ocean: effects ofepisodic production. In: Berger WH, Smetacek V, Wefer
G (eds) Productivity of the Ocean: Present and Past.
J Wiley & Sons, Chichester, pp 139-154
Wefer G, Fischer G (1991) Annual primary production and
export flux in the Southern Ocean from sediment trap
data. MarChem35: 597-614
YangH-S, Nozaki Y, SakaiH, Masuda A (1986) The distribution 0[2 30 Th and 231 Pa in the deep-sea surface
sediments of the Pacific Ocean. Geochim Cosmochim
Acta 50: 81-89
Yang Y -L, Elderfeld H, Pederson TF (1995) Geochemical
record of the Panama basin during the last glacial
maximum carbon event shows that the glacial ocean
was not suboxic. Geology 23: 1115-1118
Yu EF (1994) Variations in the particulate flux 0[2 30 Th
and m Pa and paleoceanographic applications of the
mpa/ 2J oTh ratio. PhD Thesis, WHOI, Woods Hole,
MA,pp 1-269
Yu EF, Fran,
689-694