| nr |
titel |
auteur |
tijdschrift |
jaar |
jaarg. |
afl. |
pagina('s) |
type |
| 1 |
Analysis of mycosporine-like amino acids in plankton by liquid chromatography electrospray ionization mass spectrometry
|
Whitehead, Kenia
|
|
2002
|
80 |
1 |
p. 27-39
13 p.
|
artikel
|
| 2 |
Calibration of sediment traps and particulate organic carbon export using 234Th in the Barents Sea
|
Coppola, L
|
|
2002
|
80 |
1 |
p. 11-26
16 p.
|
artikel
|
| 3 |
Editorial Board
|
|
|
2002
|
80 |
1 |
p. iii-
1 p.
|
artikel
|
| 4 |
Influence of thermal and photochemical reactions upon the redox cycling of Pu between solid and solution phases in seawater
|
McCubbin, David
|
|
2002
|
80 |
1 |
p. 61-77
17 p.
|
artikel
|
| 5 |
Isotopic composition of fatty acids of extremely piezophilic bacteria from the Mariana Trench at 11,000 m
|
Fang, Jiasong
|
|
2002
|
80 |
1 |
p. 1-9
9 p.
|
artikel
|
| 6 |
New TIMS constraints on the uranium-238 and uranium-234 in seawaters from the main ocean basins and the Mediterranean Sea 1 1 Throughout the paper we use the δ 234U notation which represents the deviation of the measured 234U/238U atomic ratio from the 234U/238U atomic ratio at secular equilibrium: δ 234U=1000×[(234U/238U)/(234U/238U)eq−1], where (234U/238U)eq is the ratio of the two decay constants: λ 238=1.5513×10−10 year−1 (Jaffey et al., 1971) and λ 234=2.826×10−6 year−1 recently revised by Cheng et al. (2000). Therefore, an activity ratio of 1 equals (234U/238U)eq=λ 238/λ 234=54.89×10−6 in atomic ratio. This latter value is ∼3‰ different than the one previously used and thus data from the literature have been recalculated accordingly. All U concentrations are expressed in pmol/g (to be multiplied by 0.2380274 for comparison with some previous works which used ng/g; e.g. Chen et al., 1986).
|
Delanghe, Doriane
|
|
2002
|
80 |
1 |
p. 79-93
15 p.
|
artikel
|
| 7 |
The distribution of Mo, U, and Cd in relation to major redox species in muddy sediments of the Bay of Biscay
|
Chaillou, Gwénaëlle
|
|
2002
|
80 |
1 |
p. 41-59
19 p.
|
artikel
|
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