346
GÉOCHIMIE MARINE
Baskaran M„ Swarzenski P.W. & Porcelli D. (2004). « Rôle of colloidal material in rhe removal of 234Th
in the Canada Basin of the Arctic Océan ». Deep-Sea Res. 50, 1353- 1373.
Battle M„ Bender M.L., Tans P.P., White J.W.C., Elus J.T., Conway T. & Francey R.J. (2000).
• Global Carbon Sinks and Their Variability Inferred from Atmospheric O2 and ô13 C ». Science 287,
2467-2470.
Beauvais S., Pedrotti M.L., Villa E. & Lemée R. (2003). « Transparent exopolymer particle (TEP)
dynamics in relation to trophic and hydrological conditions in the NW Mediterranean Sea ». Mar. Ecol.
Prog. Ser. 262, 97-109.
Behrenfeld M.J., O’Malley R.T., Siegel D.A., McClain C.R., Sarmiento J.L., Feldman G.C.,
Milligan A.J., Falkowski P.G., Letelier R.M. & Boss E.S. (2006). « Climate-driven trends in
contemporary océan productivity ». Nature 444,752-755.
Beining P. & Roether W. (1996). «Temporal évolution of CFC 11 and CFC 12 concentrations in the océan
interior ». J. Geophys. Res. 101, 16455-16464.
Bender M.L. (1990). «The dl8O of dissolved O, in seawater: A unique tracer of circulation and respiration in
the deep-sea ».J. Geophys. Res. 95,22243- 22252.
Blain S., Treguer P., Belviso S., Bucciarelli E., Denis M., Desabre S., Fiala M., Martin-Jézéque
L.V., Le Fèvre J., Mayzaud P, Marty J.-C. & Razouls S. (2001). « A biogeochemical study of the
island mass effect in the context of the iron hypothesis: Kerguelen Islands, Southern Océan ». Deep-Sea
Res. I 48, 163-187.
Bopp L, Kohfeld K.E., Le Quére C. & Aumont O. (2003). « Dust impact on marine biota and atmospheric
CO, during glacial periods ». Paleoceanography 18, doi:10.1029/2002PA000810.
Braungardt C.B., Achterberg E.P.,Elbaz-Poulichet F. & Morley N.H. (2003). « Métal geochemistry
in a mine-polluted estuarin System in Spain ». Appl. Geochem. 18, 1757-1771.
Broecker W.S., Blanton S., Smethie Jr. M. & Ostlund G. (1991). « Radiocarbon decay and oxygen
utilization in the deep Atlantic océan ». Global Biogeochem. Cycles 5,87-117.
Broecker W.S. & Maier-Reimer E. (1992). «The influence of air and sea exchange on the carbon isotope
distribution in the sea ». Global Biogeochemic. Cycles 6,315-320.
Broecker W.S. & PengT.H. (1982). Tracers in the Sea. Lamont-Doherty Geological Observatory, Columbia
University.
Broecker W.S. & PengT.H. (1998). Greenhouse Puzzles. Second édition. Eldigio Press.
Bruland K.W. & Lohan M.C. (2003). « Controls ofTrace Metals in Seawater ». In Treatise on Geochemistry,
Vol. 6 (ed. K.Turekian), Elsevier, 23-47.
Burkhardt S., Amorosa G., RiebesellU. & Sultermeyer D. (2001). « CO, and HCO3 uptakein Marine
diatoms to different CO, concentrations ». Limnol. Oceanogr. 46, 1378-1391.
Burton K.W., Ling H.-F. & O’Nions R.K. (1997). « Closure of the central American isthmus and its
impact on North Atlantic deepwater circulation ». Nature 386, 382-385.
Caldeira K. et al. (2007). « Comment on “Modern-age buildup of CO, and its effects on seawater acidity and
salinity” by Hugo A. Loaiciga ». Geophys. Res. Lett. 34, doi:10.1029/2006GL027288.
Canfield D.E. (1998). • A new mode! for proterozoic océan chemistry ». Nature 396, 450-453.
Caschetto S. & Wollast R. (1977). «Vertical distribution of dissolved aluminum in the mediterranean
sea ». Mar. Chem 7, 141-155.
Cazenave A., Lombard A. & Llovel W. (2008). • Present-day sea level rise: A synthesis ». C.R. Geoscience
340, 761-770.
Chereskin F.K. (1995). • Direct evidence for an Ekman balance in the California Current ». J. Geophys. Res.
100,18261-18269.
Choi M.S., François R., Si. ms K., Bacon M.P., Brown-Leger S., Fleer A.P., Ball L., Schneider
D. & Pichat S. (2001). « Rapid détermination of 2wTh and 23lPa in seawater by desolvated micronebulisation Inductiveiy Comupled Mass Spectrometry ». Mar. Chem. 76,99-112.
Chou L. & \X ollast R. (1997). « Biogeochemical behavior and mass balance of dissolved aluminum in the
western Mediterranean Sea ». Deep-Sea Res. 44,741-768.
Coai.e K.H. & Bruland K.W. (1987). • Oceanic stratified euphotic zone as elucidated by 2MTh: 238U
discquilibria ». Limnol. Oceanogr. 32, 189-200.
GÉOCHIMIE MARINE
Baskaran M„ Swarzenski P.W. & Porcelli D. (2004). « Rôle of colloidal material in rhe removal of 234Th
in the Canada Basin of the Arctic Océan ». Deep-Sea Res. 50, 1353- 1373.
Battle M„ Bender M.L., Tans P.P., White J.W.C., Elus J.T., Conway T. & Francey R.J. (2000).
• Global Carbon Sinks and Their Variability Inferred from Atmospheric O2 and ô13 C ». Science 287,
2467-2470.
Beauvais S., Pedrotti M.L., Villa E. & Lemée R. (2003). « Transparent exopolymer particle (TEP)
dynamics in relation to trophic and hydrological conditions in the NW Mediterranean Sea ». Mar. Ecol.
Prog. Ser. 262, 97-109.
Behrenfeld M.J., O’Malley R.T., Siegel D.A., McClain C.R., Sarmiento J.L., Feldman G.C.,
Milligan A.J., Falkowski P.G., Letelier R.M. & Boss E.S. (2006). « Climate-driven trends in
contemporary océan productivity ». Nature 444,752-755.
Beining P. & Roether W. (1996). «Temporal évolution of CFC 11 and CFC 12 concentrations in the océan
interior ». J. Geophys. Res. 101, 16455-16464.
Bender M.L. (1990). «The dl8O of dissolved O, in seawater: A unique tracer of circulation and respiration in
the deep-sea ».J. Geophys. Res. 95,22243- 22252.
Blain S., Treguer P., Belviso S., Bucciarelli E., Denis M., Desabre S., Fiala M., Martin-Jézéque
L.V., Le Fèvre J., Mayzaud P, Marty J.-C. & Razouls S. (2001). « A biogeochemical study of the
island mass effect in the context of the iron hypothesis: Kerguelen Islands, Southern Océan ». Deep-Sea
Res. I 48, 163-187.
Bopp L, Kohfeld K.E., Le Quére C. & Aumont O. (2003). « Dust impact on marine biota and atmospheric
CO, during glacial periods ». Paleoceanography 18, doi:10.1029/2002PA000810.
Braungardt C.B., Achterberg E.P.,Elbaz-Poulichet F. & Morley N.H. (2003). « Métal geochemistry
in a mine-polluted estuarin System in Spain ». Appl. Geochem. 18, 1757-1771.
Broecker W.S., Blanton S., Smethie Jr. M. & Ostlund G. (1991). « Radiocarbon decay and oxygen
utilization in the deep Atlantic océan ». Global Biogeochem. Cycles 5,87-117.
Broecker W.S. & Maier-Reimer E. (1992). «The influence of air and sea exchange on the carbon isotope
distribution in the sea ». Global Biogeochemic. Cycles 6,315-320.
Broecker W.S. & PengT.H. (1982). Tracers in the Sea. Lamont-Doherty Geological Observatory, Columbia
University.
Broecker W.S. & PengT.H. (1998). Greenhouse Puzzles. Second édition. Eldigio Press.
Bruland K.W. & Lohan M.C. (2003). « Controls ofTrace Metals in Seawater ». In Treatise on Geochemistry,
Vol. 6 (ed. K.Turekian), Elsevier, 23-47.
Burkhardt S., Amorosa G., RiebesellU. & Sultermeyer D. (2001). « CO, and HCO3 uptakein Marine
diatoms to different CO, concentrations ». Limnol. Oceanogr. 46, 1378-1391.
Burton K.W., Ling H.-F. & O’Nions R.K. (1997). « Closure of the central American isthmus and its
impact on North Atlantic deepwater circulation ». Nature 386, 382-385.
Caldeira K. et al. (2007). « Comment on “Modern-age buildup of CO, and its effects on seawater acidity and
salinity” by Hugo A. Loaiciga ». Geophys. Res. Lett. 34, doi:10.1029/2006GL027288.
Canfield D.E. (1998). • A new mode! for proterozoic océan chemistry ». Nature 396, 450-453.
Caschetto S. & Wollast R. (1977). «Vertical distribution of dissolved aluminum in the mediterranean
sea ». Mar. Chem 7, 141-155.
Cazenave A., Lombard A. & Llovel W. (2008). • Present-day sea level rise: A synthesis ». C.R. Geoscience
340, 761-770.
Chereskin F.K. (1995). • Direct evidence for an Ekman balance in the California Current ». J. Geophys. Res.
100,18261-18269.
Choi M.S., François R., Si. ms K., Bacon M.P., Brown-Leger S., Fleer A.P., Ball L., Schneider
D. & Pichat S. (2001). « Rapid détermination of 2wTh and 23lPa in seawater by desolvated micronebulisation Inductiveiy Comupled Mass Spectrometry ». Mar. Chem. 76,99-112.
Chou L. & \X ollast R. (1997). « Biogeochemical behavior and mass balance of dissolved aluminum in the
western Mediterranean Sea ». Deep-Sea Res. 44,741-768.
Coai.e K.H. & Bruland K.W. (1987). • Oceanic stratified euphotic zone as elucidated by 2MTh: 238U
discquilibria ». Limnol. Oceanogr. 32, 189-200.