348
GÉOCHIMIE MARINE
Flecker R., de Villiers S. & Ellam R. M. (2002). « Modelling the effect of évaporation on the salinity87Sr/86Sr relationship in modem and ancient marginal-marine Systems: the Mediterranean Messinian
Salinity Crisis ». Earth Planet. Sci. Lett. 203, 221-233.
François R., Altabet M.A., Goericke R., McCorkle D.C., Brunet C. & Poisson A. (1993). « Changes
in the d'3C of surface water particulate organic matter across the subtropical convergence in the SW
Indian Océan ». Global Biogeochem. Cycles 7,627-644.
François R., Frank M., Rutgers van der Loeff M. & Bacon M.P. (2004). « 230Th normalization: An
essential tool for interpreting sedimentary fluxes during the late Quaternary », Paleoceanography, 19,
PA 1018, doi: 10.1029/2003PA000939.
Freudenthal S. & Andrié C. (2002). «The arrivai of a «new» Labrador SeaWater signal in the tropical
Atlantic in 1996 ». Geophys. Res. Lett. 29.
Friedli H., Lôtscher H., Oeschger H., Siegenthaler U. & Stauffer B. (1986). « Ice core record of the
13C/12C ratio of atmospheric CO, in the past two centuries ». Nature 324, 237-238.
Gruber N., Keeling C.D. & Bâtes N.R. (2002). « Interannual Variability in the North Atlantic Océan
Carbon Sink ». Science 298,2374-2378.
Guieu C., Roy-Barman M., Leblond N., Jeandel C., Souhaut M., Le Cann B., Dufour A. &
Bournot C. (2005). «Vertical particle flux in the North-East Atlantic Océan (POMME experiment) ».
J. Geophys. Res. 110., doi:10.1029/2004JC002672.
Habitch K.S., Gabe M., Thamdrup B., Berg P. & Canfield D.E. (2002). « Calibration of sulfate levels
in the archean océan ». Science 298,2372-2374.
Hamelin B., Ferrand J.L., Alleman L., Nicolas E. & Veron A. (1997). « Isotopic evidence of pollutant
lead transport from North America to the Subtropical North Atlantic Gyre ». Geochim. Cosmochim. Acta
61(22), 4423-4428.
Hansell D.A. & Carlson C.A. (1998). « Deep-ocean gradients in the concentration of dissolved organic
carbon ». Nature 395,263-266.
Hautala S.L., Roemmich D.H. & Schmitz Jr. WJ. (1994). « Is the Nor± Pacific in Sverdrup balance à
24°N ». J. Geophys. Res. 99,16041-16052.
Hayes G.C., Richardson A.J. & Robinson C. (2005). « Climate change and marine plankton ». Trends in
Ecology and Evolution 20, 337-344.
Hellerman S. & Rosenstein M. (1983). « Normal monthly wind stress over the world océan with error
estimate ». J. Phys. Oceanogr. 13,1093-1104.
Hendricks M.B., Bender M. & Barnett B. (2004). « Net and gross O, production in the Southern Océan
from measurements of biological O2 saturation and its triple isotope composition ». Deep Sea Res. 151,
1541- 1561.
Hensen C., Pfeifer K., Wenzhôfer F., Volbers A., Schulz S., Romero O. & Seiter K. (2004).
• Fluxes at the benthic boundary layer - A global view from the South Atlantic ». In The South Atlantic
in the Late Quaternary (eds. G. Wefer, S. Mulitza, and C. Rühlemann). Springer.
Hogg N.G. & Owens W. B. (1999). « Direct measurement of the deep circulation within the Brasil basin ».
Deep Sea Res. 46, 335-353.
Holm E., Aakorg A., Ballestra S. & Dalghaard H. (1986). « Origin and isotopic ratios of plutonium in
the Barents and Greenlan Seas ». Earth Planet. Sci. lett. 79,27-32.
Honeyman B.D. & Santschi P.H. (1989). « A Brownian-pumping model for trace métal scavenging:
evidence from Th isotopes ». J. Mar. Res. 47,950-995.
Hltchins D.A. & Bruland K.W. (1998). « Iron-limited diatom growth andSi:N uptake ratios in a Coastal
upwelling régime ». Nature 393, 561-564.
Intergovernmental Panel on Climate Change (2007). The IPCC 4th Assessment Report, Climate
Change 2007: Synthesis Report. Contribution ofWorking Groups I, II and III to the Fourth Assessment Report
of the Intergovernmental Panel on Climate Change (eds Team CW, Pauchauri RK, Reisinger A (IPCC,
Geneva)), 104.
Jahnke R.A. & Jahnke D.B. (2000). • Rates of C, N, P and Si recycling and dénitrification at the US MidAtlantic continental slope depocenter ». Deep-Sea Res. I 47,1405-1428.
Jarman W.M., Hobson K.H., Sydeman W.J., Bacon C.E. & McLaren E.B. (1996). « Influence of trophic
position abd feeding location on contaminant levels in the Gulf of the Farallones food web revealed by
stable isotooe analvsis • Fh^
™
GÉOCHIMIE MARINE
Flecker R., de Villiers S. & Ellam R. M. (2002). « Modelling the effect of évaporation on the salinity87Sr/86Sr relationship in modem and ancient marginal-marine Systems: the Mediterranean Messinian
Salinity Crisis ». Earth Planet. Sci. Lett. 203, 221-233.
François R., Altabet M.A., Goericke R., McCorkle D.C., Brunet C. & Poisson A. (1993). « Changes
in the d'3C of surface water particulate organic matter across the subtropical convergence in the SW
Indian Océan ». Global Biogeochem. Cycles 7,627-644.
François R., Frank M., Rutgers van der Loeff M. & Bacon M.P. (2004). « 230Th normalization: An
essential tool for interpreting sedimentary fluxes during the late Quaternary », Paleoceanography, 19,
PA 1018, doi: 10.1029/2003PA000939.
Freudenthal S. & Andrié C. (2002). «The arrivai of a «new» Labrador SeaWater signal in the tropical
Atlantic in 1996 ». Geophys. Res. Lett. 29.
Friedli H., Lôtscher H., Oeschger H., Siegenthaler U. & Stauffer B. (1986). « Ice core record of the
13C/12C ratio of atmospheric CO, in the past two centuries ». Nature 324, 237-238.
Gruber N., Keeling C.D. & Bâtes N.R. (2002). « Interannual Variability in the North Atlantic Océan
Carbon Sink ». Science 298,2374-2378.
Guieu C., Roy-Barman M., Leblond N., Jeandel C., Souhaut M., Le Cann B., Dufour A. &
Bournot C. (2005). «Vertical particle flux in the North-East Atlantic Océan (POMME experiment) ».
J. Geophys. Res. 110., doi:10.1029/2004JC002672.
Habitch K.S., Gabe M., Thamdrup B., Berg P. & Canfield D.E. (2002). « Calibration of sulfate levels
in the archean océan ». Science 298,2372-2374.
Hamelin B., Ferrand J.L., Alleman L., Nicolas E. & Veron A. (1997). « Isotopic evidence of pollutant
lead transport from North America to the Subtropical North Atlantic Gyre ». Geochim. Cosmochim. Acta
61(22), 4423-4428.
Hansell D.A. & Carlson C.A. (1998). « Deep-ocean gradients in the concentration of dissolved organic
carbon ». Nature 395,263-266.
Hautala S.L., Roemmich D.H. & Schmitz Jr. WJ. (1994). « Is the Nor± Pacific in Sverdrup balance à
24°N ». J. Geophys. Res. 99,16041-16052.
Hayes G.C., Richardson A.J. & Robinson C. (2005). « Climate change and marine plankton ». Trends in
Ecology and Evolution 20, 337-344.
Hellerman S. & Rosenstein M. (1983). « Normal monthly wind stress over the world océan with error
estimate ». J. Phys. Oceanogr. 13,1093-1104.
Hendricks M.B., Bender M. & Barnett B. (2004). « Net and gross O, production in the Southern Océan
from measurements of biological O2 saturation and its triple isotope composition ». Deep Sea Res. 151,
1541- 1561.
Hensen C., Pfeifer K., Wenzhôfer F., Volbers A., Schulz S., Romero O. & Seiter K. (2004).
• Fluxes at the benthic boundary layer - A global view from the South Atlantic ». In The South Atlantic
in the Late Quaternary (eds. G. Wefer, S. Mulitza, and C. Rühlemann). Springer.
Hogg N.G. & Owens W. B. (1999). « Direct measurement of the deep circulation within the Brasil basin ».
Deep Sea Res. 46, 335-353.
Holm E., Aakorg A., Ballestra S. & Dalghaard H. (1986). « Origin and isotopic ratios of plutonium in
the Barents and Greenlan Seas ». Earth Planet. Sci. lett. 79,27-32.
Honeyman B.D. & Santschi P.H. (1989). « A Brownian-pumping model for trace métal scavenging:
evidence from Th isotopes ». J. Mar. Res. 47,950-995.
Hltchins D.A. & Bruland K.W. (1998). « Iron-limited diatom growth andSi:N uptake ratios in a Coastal
upwelling régime ». Nature 393, 561-564.
Intergovernmental Panel on Climate Change (2007). The IPCC 4th Assessment Report, Climate
Change 2007: Synthesis Report. Contribution ofWorking Groups I, II and III to the Fourth Assessment Report
of the Intergovernmental Panel on Climate Change (eds Team CW, Pauchauri RK, Reisinger A (IPCC,
Geneva)), 104.
Jahnke R.A. & Jahnke D.B. (2000). • Rates of C, N, P and Si recycling and dénitrification at the US MidAtlantic continental slope depocenter ». Deep-Sea Res. I 47,1405-1428.
Jarman W.M., Hobson K.H., Sydeman W.J., Bacon C.E. & McLaren E.B. (1996). « Influence of trophic
position abd feeding location on contaminant levels in the Gulf of the Farallones food web revealed by
stable isotooe analvsis • Fh^
™