Evaluation de la pénétration du carbone anthropique en Méditerranée | Bibliographie
118
(2005). Anthropogenic ocean acidification over the twenty-first century and its impact on
calcifying organisms. Nature. Vol. 437, pp. 681-686.
ORR, J. C., MAIER-REIMER, E., MIKOLAJEWICZ, U., MONFRAY, P., SARMIENTO,
J. L., TOGGWEILER, J. R., TAYLOR, N. K., PALMER, J., GRUBER, N., SABINE, C. L.,
LE QUÉRÉ, C., KEY, R. M., BOUTIN, J. (2001). Estimates of anthropogenic carbon uptake
from four tree-dimensional global ocean models. Global Biogeochimical Cycles. Vol. 15, 1, pp.
43-60.
PALMIÉRI, J., ORR, J. C., DUTAY, J.-C., BÉRANGER, K., SCHNEIDER, A., BEUVIER,
J., SOMOT, S. (2014). Simulated anthropogenic CO2 uptake and acidification of the
Mediterranean Sea. Biogeosciences Discussions. pp. 1-55.
PENG, T.-H. et BROECKER, W. S. (1985). The utility of Multiple tracer distribution in the
calibrating models for uptake of anthropogenic CO2 by the ocean thermocline. Journal of
Geophysical Research. The American Geophysical Union. Vol. 90, C4, pp. 7023-7035.
PENG, T.-H., WANNINKHOF, R., BULLISTER, J. L., FEELY, R. A., TAKAHASHI , T.
(1998). Quantification of decadal anthropogenic CO2 uptake in the ocean based on dissolved
inorganic carbon measurements. Vol. 396, pp. 560-563.
PNUE/PAM. (2012). Etat de l'environnement marin et côtier de la Méditerranée. Athènes :
PNUE/PAM - Convention de Barcelone.
POISSON, A. et CHEN, C.-T. A. (1987). Why is there little anthropogenic CO2 in the Antarctique
bottom water ? Deep-Sea Research. Pergamon journals Ltd. Vol. 34, 7, pp. 1255-1275.
QUÉGUINER, B. (2008). Le cycle océanique de l'azote. Centre d'Océanographie de Marseille.
pp. 21-22.
RAMETTE, R.W., CULBERSON, C.H. et BATES, R.G. (1977). Acid-Base Properties of
Tris(hydroxymethyl)aminomethane (Tris) Buffers in Seawater from 5 to 40 °C. Analytical
Chemistry. Vol. 49, 6, pp. 867-870.
RAVEN, J., CALDEIRA, K., ELDERFIELD, H., HOEGH-GULDBERG, O., LISS, P.,
RIEBESELL, U., SHEPHERD, J., TURLEY, C., WATSON, A. (2005). Ocean acidification
due to increasing atmospheric carbon dioxide. London : The Clyvedon Press Ltd, Cardiff, UK.
RAYNAUD, S., AUMONT, O., RODGERS, K. B., YIOU, P., ORR, J. C. (2005). Interannualto-decadal variability of North Atlantic air-sea CO2 fluxes. Ocean Science Discussions. Vol. 2, pp.
437-472.
REDFIELD, A.C., KETCHUM, B.H. et RICHARDS, F.A. (1963). The influence of organisms
on the composition of seawater. in The Sea. M. N. Hill, Interscience, New York. Vol. 2.
RIBERA D’ALCALA, M., CIVITARESE, G., CONVERSANO, F., LAVEZZA, R. (2003).
Nutrient ratios and fluxes hint at overlooked processes in the Mediterranean Sea. Journal od
Geophysical Research. The American Geophysical Union. Vol. 108, C9.
118
(2005). Anthropogenic ocean acidification over the twenty-first century and its impact on
calcifying organisms. Nature. Vol. 437, pp. 681-686.
ORR, J. C., MAIER-REIMER, E., MIKOLAJEWICZ, U., MONFRAY, P., SARMIENTO,
J. L., TOGGWEILER, J. R., TAYLOR, N. K., PALMER, J., GRUBER, N., SABINE, C. L.,
LE QUÉRÉ, C., KEY, R. M., BOUTIN, J. (2001). Estimates of anthropogenic carbon uptake
from four tree-dimensional global ocean models. Global Biogeochimical Cycles. Vol. 15, 1, pp.
43-60.
PALMIÉRI, J., ORR, J. C., DUTAY, J.-C., BÉRANGER, K., SCHNEIDER, A., BEUVIER,
J., SOMOT, S. (2014). Simulated anthropogenic CO2 uptake and acidification of the
Mediterranean Sea. Biogeosciences Discussions. pp. 1-55.
PENG, T.-H. et BROECKER, W. S. (1985). The utility of Multiple tracer distribution in the
calibrating models for uptake of anthropogenic CO2 by the ocean thermocline. Journal of
Geophysical Research. The American Geophysical Union. Vol. 90, C4, pp. 7023-7035.
PENG, T.-H., WANNINKHOF, R., BULLISTER, J. L., FEELY, R. A., TAKAHASHI , T.
(1998). Quantification of decadal anthropogenic CO2 uptake in the ocean based on dissolved
inorganic carbon measurements. Vol. 396, pp. 560-563.
PNUE/PAM. (2012). Etat de l'environnement marin et côtier de la Méditerranée. Athènes :
PNUE/PAM - Convention de Barcelone.
POISSON, A. et CHEN, C.-T. A. (1987). Why is there little anthropogenic CO2 in the Antarctique
bottom water ? Deep-Sea Research. Pergamon journals Ltd. Vol. 34, 7, pp. 1255-1275.
QUÉGUINER, B. (2008). Le cycle océanique de l'azote. Centre d'Océanographie de Marseille.
pp. 21-22.
RAMETTE, R.W., CULBERSON, C.H. et BATES, R.G. (1977). Acid-Base Properties of
Tris(hydroxymethyl)aminomethane (Tris) Buffers in Seawater from 5 to 40 °C. Analytical
Chemistry. Vol. 49, 6, pp. 867-870.
RAVEN, J., CALDEIRA, K., ELDERFIELD, H., HOEGH-GULDBERG, O., LISS, P.,
RIEBESELL, U., SHEPHERD, J., TURLEY, C., WATSON, A. (2005). Ocean acidification
due to increasing atmospheric carbon dioxide. London : The Clyvedon Press Ltd, Cardiff, UK.
RAYNAUD, S., AUMONT, O., RODGERS, K. B., YIOU, P., ORR, J. C. (2005). Interannualto-decadal variability of North Atlantic air-sea CO2 fluxes. Ocean Science Discussions. Vol. 2, pp.
437-472.
REDFIELD, A.C., KETCHUM, B.H. et RICHARDS, F.A. (1963). The influence of organisms
on the composition of seawater. in The Sea. M. N. Hill, Interscience, New York. Vol. 2.
RIBERA D’ALCALA, M., CIVITARESE, G., CONVERSANO, F., LAVEZZA, R. (2003).
Nutrient ratios and fluxes hint at overlooked processes in the Mediterranean Sea. Journal od
Geophysical Research. The American Geophysical Union. Vol. 108, C9.