Geoscience Reference
In-Depth Information
Feng, Y., Warner, M., Zhang, Y.
et al.
(2008). Interactive
effects of increased
p
CO
2
, temperature and irradiance
on the marine coccolithophore
Emiliania huxleyi
(Prymnesiophyceae).
European Journal of Phycology
,
43
,
87-98.
Feng, Y., Hare, C.E., Leblanc, K.
et al.
(2009). The effects of
increased
p
CO
2
and temperature on the North Atlantic
spring bloom: I. phytoplankton community and biogeo-
chemical response.
Marine Ecology Progress Series
,
388
,
13-25.
Feng, Y., Hare, C.E., Rose, J.M.
et al.
(2010). Interactive
effects of iron, irradiance and CO
2
on Ross Sea phyto-
plankton.
Deep-Sea Research Part I: Oceanographic Research
Papers
,
57
, 368-83.
Fu, F.-X., Mulholland, M.R., Garcia, N.S.
et al.
(2008a).
Interactions between changing
p
CO
2
, N
2
i xation, and Fe
limitation in the marine unicellular cyanobacterium
Crocosphaera
.
Limnology and Oceanography
,
53
, 2472-84.
Fu, F., Zhang, Y., Warner, M.E., Feng, Y., and Hutchins,
D.A. (2008b). A comparison of future increased CO
2
and
temperature effects on sympatric
Heterosigma akashiwo
and
Prorocentrum minimum
.
Harmful Algae
,
7
, 76-90.
Gao K., Ruan Z., Villafane V.E., Gattuso J.-P., and Helbling,
W. (2009). Ocean acidii cation exacerbates the effect of
UV radiation on the calcifying phytoplankter
Emiliania
huxleyi
.
Limnology and Oceanography
,
54
, 1855-62.
Gervais, F. and Riebesell, U. (2001). Effect of phosphorus
limitation on elemental composition and stable car-
bon isotope fractionation in a marine diatom growing
under different CO
2
concentrations.
Limnology and
Oceanography
,
46
, 497-504.
Giordano, M., Beardall, J., and Raven, J.A. (2005). CO
2
con-
centrating mechanisms in algae: mechanisms, environ-
mental modulation, and evolution.
Annual Review of
Plant Biology
,
56
, 99-131.
del Giorgio, P.A. and Cole, J.J. (1998). Bacterial growth efi -
ciency in natural aquatic systems.
Annual Review of
Ecology and Systematics
,
29
, 503-41.
Glibert, P.M. (1982). Regional studies of daily, seasonal
and size fraction variability in ammonium reminerali-
zation.
Marine Biology
,
70
, 209-22.
Gruber, N. and Galloway, J.N. (2008). An Earth-system
perspective of the global nitrogen cycle.
Nature
,
451
,
293-6.
Gruber, N. and Sarmiento, J.L. (2002). Large-scale biogeo-
chemical/physical interactions in elemental cycles. In:
A.R. Robinson, J.J. McCarthy, and B.J. Rothschild (eds),
The sea: biological-physical interactions in the oceans
, pp.
337-99. John Wiley and Sons, New York.
Hansell, D.A. and Carlson, C.A. (2002).
Biogeochemistry of
marine dissolved organic matter
, 745 pp. Academic Press,
New York.
Hare, C.E., Leblanc, K., DiTullio, G.R.
et al.
(2007).
Consequences of increased temperature and CO
2
for
phytoplankton community structure in the Bering Sea.
Marine Ecology Progress Series
,
352
, 9-16.
Hein, M. and Sand-Jensen, K. (1997). CO
2
increases oce-
anic primary production.
Nature
,
388
, 526-7.
Heinze, C., Maier-Reimer, E. and Winn, K. (1991). Glacial
p
CO
2
reduction by the world ocean: experiments with
the Hamburg carbon cycle model.
Paleoceanography
,
6
,
395-430.
Hinga, K.R. (1992). Co-occurrence of dinol agellate blooms
and high pH in marine enclosures.
Marine Ecology
Progress Series
,
86
, 181-7.
Hinga, K.R. (2002). Effects of pH on coastal marine
phytoplankton.
Marine Ecology Progress Series
,
238
,
281-300.
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-Rodríguez, M.D., Schoi eld, O.M., Batley, J.,
Medlin, L.K., and Hayes, P.K. (2006). Intraspecii c gene-
tic diversity in the marine coccolithophore
Emiliania
huxleyi
(Prymnesiophyceae): the use of microsatellite
analysis in marine phytoplankton population studies.
Journal of Phycology
,
42
, 526-36.
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.
Joint, I., Doney, S.C., and Karl, D.M. (2011). Will ocean
acidii cation affect marine microbes?
The ISME Journal
,
5
, 1-7.
Kim, J.-M., Lee, K., Shin, K.
et al.
(2006). The effect of sea-
water CO
2
concentration on growth of a natural phyto-
plankton assemblage in a controlled mesocosm
experiment.
Limnology and
Oceanography
,
51
, 1629-36.
Klaas, C. and Archer, D.A. (2002). Association of sink-
ing organic matter with various types of mineral
ballast in the deep sea: implications for the rain
ratio.
Global
Biogeochemical
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.
Kranz, S.A., Levitan, O., Richter, K.-U., Prášil, O., Berman-
Frank, I., and Rost, B. (2010). Combined effects of CO
2
and light on the N
2
-i xing cyanobacterium
Trichodesmium
