Evaluation de la pénétration du carbone anthropique en Méditerranée | Bibliographie
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BETHOUX, J. P., MORIN, P. et RUIZ-PINO, D. P. (2002). Temporal trends in nutrient ratios:
chemical evidence of Mediterranean ecosystem changes driven by human activity. Deep-Sea
Research II. Elsevier Science Ltd. Vol. 49, pp. 2007-2016.
BÉTHOUX, J. P., MORIN, P., CHAUMERY, C., CONNAN, O., GENTILI, B., RUIZ-PINO,
D. (1998). Nutrients in the Mediterranean Sea, mass balance and statistical analysis of
concentrations with respect to environmental change. Marine Chemistry. Elsevier Science B.V.
Vol. 63, pp. 155-169.
BETHOUX, J.P., GENTILI, B., MORIN, P., NICOLAS, E., PIERRE, C., RUIZ-PINO, D.
(1999). The Mediterranean Sea: a miniature ocean for climatic and environmental studies and a
key for the climatic functioning of the North Atlantic. Progress in Oceanography. Elsevier Science
Ltd. Vol. 44, pp. 131-146.
BOUDJAKDJI, M. (2008). Etude du cycle biogéochimique du carbone dans le bassin algéroprovençal. ENSSMAL. Mémoire de Magister.
BOULAHDID, M. et MINSTER, J.-F. (1989). Oxygen consumption and nutrient regeneration
ratios along isopycnal horizons in the Pacific Ocean. Marine Chemistry. sevier Science Publishers
B.V., Amsterdam. Vol. 26, pp. 133-153.
BREWER, P. G. (1978). Direct observation of the oceanic CO2 increase. Geophysical Research
Letters. The American Geophysical Union. Vol. 5, 12, pp. 997-1000.
BROECKER, W. S. (1974). "NO", a conservative water-mass tracer. Earth and Planetary Science
Letters. North-Holland Publishing Company. Vol. 23, pp. 100-107.
BROECKER, W. S. et PENG, T-H. (1982). Tracers in the sea. New York : Lamont-Doherty
Geological Observatory.
BROECKER, W. S., TAKAHASHI, T. et TAKAHASHI, T. (1985). Sources and flow patterns
of deep-ocean waters as deduced from potential temperature, salinity, ans initial phosphate
concentration. Journal of Geophysical Research. Vol. 90, C4, pp. 6925-6939.
BRYDEN, H. L., MCDONAGH, E. L. et KING, B. A. (2003). Changes in Ocean Water Mass
Properties: Oscillations or Trends? Science. Vol. 300.
BULLISTER, J. L., WISEGARVER, D. P. et MENZIA, F. A. (2002). The solubilité of surfure
hexafluoride in water and sea water. Deep-Sea Research I. Pergamon. Vol. 49, pp. 175-187.
CALDEIRA, K. et WICKETT, M. E. (2003). Anthropogenic carbon and ocean pH. Nature. Vol.
425, p. 365.
CDIAC. (2014). Carbon Dioxide Information Analysis Center. [En ligne]. [Citation : 28 Novembre
2014.] http://cdiac.ornl.gov/.
CDIAC. (2010). Carbon Dioxide Information Analysis Center. [En ligne]. http://cdiac.ornl.gov/.
111
BETHOUX, J. P., MORIN, P. et RUIZ-PINO, D. P. (2002). Temporal trends in nutrient ratios:
chemical evidence of Mediterranean ecosystem changes driven by human activity. Deep-Sea
Research II. Elsevier Science Ltd. Vol. 49, pp. 2007-2016.
BÉTHOUX, J. P., MORIN, P., CHAUMERY, C., CONNAN, O., GENTILI, B., RUIZ-PINO,
D. (1998). Nutrients in the Mediterranean Sea, mass balance and statistical analysis of
concentrations with respect to environmental change. Marine Chemistry. Elsevier Science B.V.
Vol. 63, pp. 155-169.
BETHOUX, J.P., GENTILI, B., MORIN, P., NICOLAS, E., PIERRE, C., RUIZ-PINO, D.
(1999). The Mediterranean Sea: a miniature ocean for climatic and environmental studies and a
key for the climatic functioning of the North Atlantic. Progress in Oceanography. Elsevier Science
Ltd. Vol. 44, pp. 131-146.
BOUDJAKDJI, M. (2008). Etude du cycle biogéochimique du carbone dans le bassin algéroprovençal. ENSSMAL. Mémoire de Magister.
BOULAHDID, M. et MINSTER, J.-F. (1989). Oxygen consumption and nutrient regeneration
ratios along isopycnal horizons in the Pacific Ocean. Marine Chemistry. sevier Science Publishers
B.V., Amsterdam. Vol. 26, pp. 133-153.
BREWER, P. G. (1978). Direct observation of the oceanic CO2 increase. Geophysical Research
Letters. The American Geophysical Union. Vol. 5, 12, pp. 997-1000.
BROECKER, W. S. (1974). "NO", a conservative water-mass tracer. Earth and Planetary Science
Letters. North-Holland Publishing Company. Vol. 23, pp. 100-107.
BROECKER, W. S. et PENG, T-H. (1982). Tracers in the sea. New York : Lamont-Doherty
Geological Observatory.
BROECKER, W. S., TAKAHASHI, T. et TAKAHASHI, T. (1985). Sources and flow patterns
of deep-ocean waters as deduced from potential temperature, salinity, ans initial phosphate
concentration. Journal of Geophysical Research. Vol. 90, C4, pp. 6925-6939.
BRYDEN, H. L., MCDONAGH, E. L. et KING, B. A. (2003). Changes in Ocean Water Mass
Properties: Oscillations or Trends? Science. Vol. 300.
BULLISTER, J. L., WISEGARVER, D. P. et MENZIA, F. A. (2002). The solubilité of surfure
hexafluoride in water and sea water. Deep-Sea Research I. Pergamon. Vol. 49, pp. 175-187.
CALDEIRA, K. et WICKETT, M. E. (2003). Anthropogenic carbon and ocean pH. Nature. Vol.
425, p. 365.
CDIAC. (2014). Carbon Dioxide Information Analysis Center. [En ligne]. [Citation : 28 Novembre
2014.] http://cdiac.ornl.gov/.
CDIAC. (2010). Carbon Dioxide Information Analysis Center. [En ligne]. http://cdiac.ornl.gov/.