Geoscience Reference
In-Depth Information
Huesemann, M.H., Skillman, A.D., and Crecelius, E.A. (2002).
The inhibition of marine nitrii cation by ocean disposal
of carbon dioxide.
Marine Pollution Bulletin
,
44
, 142-8.
Hutchins, D.A., Fu, F.-X., Zhang, Y.
et al.
(2007). CO
2
con-
trol of
Trichodesmium
N
2
i xation, photosynthesis, growth
rates and elemental ratios: implications for past, present
and future ocean biogeochemistry.
Limnology and
Oceanography
,
52
, 1293-304.
Hutchins, D.A., Mulholland, M.R., and Fu, F. (2009).
Nutrient cycles and marine microbes in a CO
2
-enriched
ocean.
Oceanography
,
22
, 128-45.
Iglesias-Rodriguez, M.D., Halloran, P.R., Rickaby, R.E.M.
et al.
(2008). Phytoplankton calcii cation in a high-CO
2
world.
Science
,
320
, 336-40.
Jenkins, B.D. and Zehr, J.P. (2008). Molecular approaches
to the nitrogen cycle. In: D.G. Capone, D.A. Bronk, M.R.
Mulholland, and E.J. Carpenter (eds),
Nitrogen in the
marine environment
, pp. 1303-44. Elsevier, Amsterdam.
Jin, X. and Gruber, N. (2003). Offsetting the radiative ben-
ei t of ocean iron fertilization by enhancing N
2
O emis-
sions.
Geophysical Research Letters
,
Montoya, J.P., Holl, C.M., Zehr, J.P., Hansen, A., Villareal,
T.A., and Capone, D.G. (2004). High rates of N
2
-i xation
by unicellular diazotrophs in the oligotrophic Pacii c.
Nature
,
430
, 1027-32.
Morse, J.W., Arvidson, R.S., and Lüttge, A. (2007). Calcium
carbonate formation and dissolution.
Chemical Reviews
,
107
, 342-81.
Moore, L.R., Post, A.F., Rocap, G., and Chisholm, S.W.
(2002). Utilization of different nitrogen sources by the
marine cyanobacteria
Prochlorococcus
and
Synechococcus
.
Limnology and Oceanography
,
47
, 989-96.
Oschlies, A. (2009). Impact of atmospheric and terrestrial
CO
2
feedbacks on fertilization-induced marine carbon
uptake.
Biogeosciences
,
6
, 1603-13.
Oschlies, A., Schulz, K.G., Riebesell, U., and Schmittner, A.
(2008). Simulated 21st century's increase in oceanic sub-
oxia by CO
2
enhanced biotic carbon export.
Global
Biogeochemical
Cycles
,
22
,
GB4008,
doi:
10.1029/2007GB003147.
Pahlow, M., Vezina, A.F., Casault, B.
et al.
(2008). Adaptive
model of plankton dynamics for the North Atlantic.
Progress in Oceanography
,
76
, 151-91.
Passow, U. and De La Rocha, C.L. (2006). Accumulation of
mineral ballast on organic aggregates.
Global
Biogeochemical
30
, 2249, doi:
10.1029/2003GL018458.
Jin, X., Gruber, N., Frenzel, H., Doney, S.C., and
McWilliams, J.C. (2008). The impact on atmospheric
CO
2
of iron fertilization induced changes in the ocean's
biological pump.
Biogeosciences
,
5
, 385-406.
Keeling, R.F., Körtzinger, A., and Gruber, N. (2010). Ocean
deoxygenation in a warming world.
Annual Review of
Marine Science
,
2
, 199-229.
Keir, R.S. (1980). The dissolution kinetics of biogenic car-
bonate in seawater.
Geochimica et Cosmochimica Acta
,
44
,
241-52.
Khatiwala, S., Primeau, F., and Hall, T. (2009).
Reconstruction of the history of anthropogenic CO
2
con-
centrations in the ocean.
Nature
,
462
, 346-9.
Klaas, C. and Archer, D.E. (2002). Association of sinking
organic matter with various types of mineral ballast in
the deep sea: implications for the rain ratio.
Global Biogeo-
chemical Cycles
,
16
, 1116, doi:10.1029/2001GB001765.
Kranz, S.A., Sültemeyer, D., Richter, K.-U., and Rost, B.
(2009). Carbon acquisition by
Trichodesmium
: the
effect of
p
CO
2
and diurnal changes.
Limnology and
Oceanography
,
54
, 548-59.
Levitan, O., Rosenberg, G., Setlik, I.
et al.
(2007). Elevated
CO
2
enhances nitrogen i xation and growth in the
marine cyanobacterium
Trichodesmium
.
Global Change
Biology
,
13
, 531-8.
Middelburg, J.J., Soetaert, K., Herman, P.M.J., and Heip,
C.H.R. (1996). Denitrii cation in marine sediments: a
model study.
Global Biogeochemical Cycles
,
10
, 661-73.
Moisander, P.H., Beinart, R.A., Hewson, I.
et al.
(2010).
Unicellular cyanobacterial distributions broaden the
oceanic N
2
i xation domain.
Science
,
327
, 1512-14.
Cycles
,
20
,
GB1013,
doi:10.1029/2005GB002579.
Ridgwell, A. and Hargreaves, J.C. (2007). Regulation of atmos-
pheric CO
2
by deep-sea sediments in an Earth System
Model.
Global Biogeochemical Cycles
,
21
, GB2008, doi:
10.1029/2006GB002764.
Ridgwell, A., Zondervan, I., Hargreaves, J.C., Bijma, J.,
and Lenton, T.M. (2007). Assessing the potential long-
term increase of oceanic fossil fuel CO
2
uptake due to
CO
2
-calcii cation feedback.
Biogeosciences
,
4
, 481-92.
Ridgwell, A., Schmidt, D.N., Turley, C.
et al.
(2009). From
laboratory manipulations to Earth system models: scal-
ing calcii cation impacts of ocean acidii cation.
Biogeosciences
,
6
, 2611-23.
Riebesell, U., Schulz, K.G., Bellerby, R.G.J.
et al.
(2007).
Enhanced biological carbon consumption in a high CO
2
ocean.
Nature
,
450
, 545-8.
Rost, B., Zondervan, I., and Wolf-Gladrow, D. (2008).
Sensitivity of phytoplankton to future changes in ocean
carbonate chemistry: current knowledge, contradictions
and research directions.
Marine Ecology Progress Series
,
373
, 227-37.
Sarmiento, J.L., Le Quéré, C., and Pacala, S.W. (1995).
Limiting future atmospheric carbon dioxide.
Global
Biogeochemical Cycles
,
9
, 121-37.
Sarmiento, J.L., Hughes, T.M.C., Stouffer, R.J., and
Manabe, S. (1998). Simulated response of the ocean car-
bon cycle to anthropogenic climate warming.
Nature
,
393
, 245-9.
