Ecosystem dynamics based on plankton functional types for global ocean biogeochemistry models

Global Change Biology

Volumn 11, Issue 11, 2005, Pages 2016-2040

  Le Quéré, Corinne ^a,h,i   Harrison, Sandy P ^a,b   Prentice, I Colin ^a,b   Buitenhuis, Erik T ^a   Aumont, Olivier ^c   Bopp, Laurent ^d   Claustre, Hervé ^e   Cotrim Da Cunha, Leticia ^a   Geider, Richard ^f   Giraud, Xavier ^a,k   Klaas, Christine ^a,g   Kohfeld, Karen E ^a,l   Legendre, Louis ^e   Manizza, Manfredi ^a,h   Platt, Trevor ⁱ   Rivkin, Richard B ^j   Sathyendranath, Shubha ⁱ   Uitz, Julia ^e   Watson, Andy J ^h   Wolf Gladrow, Dieter ^g  

^a MAX PLANCK INSTITUTE FOR BIOGEOCHEMISTRY   (Germany)

^b UNIVERSITY OF BRISTOL   (United Kingdom)

^c SORBONNE UNIVERSITÉ   (France)

^d LABORATOIRE DES SCIENCES DU CLIMAT ET DE L ENVIRONNEMENT   (France)

^e LABORATOIRE D OCÉANOGRAPHIE DE VILLEFRANCHE   (France)

^f UNIVERSITY OF ESSEX   (United Kingdom)

^g ALFRED WEGENER INSTITUTE FOR POLAR AND MARINE RESEARCH   (Germany)

^h UNIVERSITY OF EAST ANGLIA   (United Kingdom)

ⁱ DALHOUSIE UNIVERSITY   (Canada)

^j MEMORIAL UNIVERSITY OF NEWFOUNDLAND   (Canada)

^k UNIVERSITY OF BREMEN   (Germany)

^l CITY UNIVERSITY OF NEW YORK   (United States)

more..

Author keywords

Carbon cycle; Climate change; Ecosystem; Functional types; Glacial interglacial cycles; Modeling; Ocean; Plankton

Indexed keywords

BIOGEOCHEMISTRY; CARBON CYCLE; CLIMATE CHANGE; ECOSYSTEM DYNAMICS; MODELING; PLANKTON;

EID: 20444469410     PISSN: 13541013     EISSN: 13652486     Source Type: Journal    
DOI: 10.1111/j.1365-2486.2005.1004.x     Document Type: Article

References (190)

1. Alvain S, Moulin C, Dandonneau Y et al. (2005) Remote sensing of phytoplankton groups in case 1 waters from global sea WiFS imagery. Deep Sea Research, in press.
2. Antia AN, Maassen J, Herman P et al. (2001) Spatial and temporal variability of particle flux at the NW European continental margin. Deep-Sea Research Part II-Topical Studies in Oceanography, 48, 3083-3106.
3. Archer DE, Johnson K (2000) A model of the iron cycle in the ocean. Global Biogeochemical Cycles, 14, 269-279.
4. Archer SD, Gilbert FJ, Nightingale PD et al. (2002) Transformation of dimethylsulphoniopropionate to dimethyl sulphide during summer in the North Sea with an examination of key processes via a modelling approach. Deep-Sea Research Part II-Topical Studies in Oceanography, 49, 3067-3101.
5. Armstrong RA (2003a) A hybrid spectral representation of phytoplankton growth and zooplankton response: The 'control rod' model of plankton interaction. Deep-Sea Research Part II-Topical Studies in Oceanography, 50, 2895-2916.
6. Armstrong RA (2003b) Representing biogeochemical diversity and size spectra in ecosystem models of the ocean carbon cycle. In Models in Ecosystem Science (eds Canham CD, Cole JJ, Laurenroth WK), pp. 254-271. Princeton University Press, Princeton, NJ, USA.
7. Aumont O, Belviso S, Monfray P (2002) Dimethylsulfoniopropionate (DMSP) and dimethylsulfide (DMS) sea surface distributions simulated from a global three-dimensional ocean carbon cycle model. Journal of Geophysical Research-Oceans, 107, doi: 10.1029/1999JC000111.
8. Aumont O, Maier-Reimer E, Blain S et al. (2003) An ecosystem model of the global ocean including Fe, Si, P colimitations. Global Biogeochemical Cycles, 17, 1060 (doi: 10.1029/2001GB001745).
9. Banse K (1991) Rates of phytoplankton cell division in the field and in iron enrichment experiments. Limnology and Oceanography, 36, 1886-1898.
10. Baretta JW, Ebenhoh W, Ruardij P (1995) The European-Regional-Seas-Ecosystem-Model, a complex marine ecosystem model. Netherlands Journal of Sea Research, 33, 233-246.
11. 2. Nature, 329, 408-414.
12. 2 and biogeochemical properties in the Western North Atlantic subtropical gyre. Deep-Sea Research Part II-Topical Studies in Oceanography, 48, 1507-1528.
13. Beaugrand G, Reid PC, Ibañez F et al. (2002) Reorganization of North Atlantic marine copepod biodiversity and climate. Science, 296, 1692-1694.
14. Behrenfeld MJ, Randerson JT, McClain et al. (2001) Biospheric primary production during an ENSO transition. Science, 291, 2594-2597.
15. Bender M (2003) Climate-biosphere interactions on glacial-interglacial timescales. Global Biogeochemical Cycles, 17, 1082 (doi: 10.1029/ 2002GB001932).
16. Benner R (2002) Chemical composition and reactivity. In: Biogeochemistry of Dissolved Organic Matter (eds Hansell D, Carlson C), pp. 59-90. Academic Press, Amsterdam.
17. Berelson WM (2002) Particle settling rates increase with depth in the ocean. Deep-Sea Research Part II-Topical Studies in Oceanography, 49, 237 -251.
18. Berges JA, Falkowski PG (1998) Physiological stress and cell death in marine phytoplankton: Induction of proteases in response to nitrogen or light limitation. Limnology and Oceanography, 43, 129 -135.
19. Bidle KD, Azam F (1999) Accelerated dissolution of diatom silica by marine bacterial assemblages. Nature, 397, 508-512.
20. Blackford JC, Burkill PH (2002) Planktonic community structure and carbon cycling in the Arabian Sea as a result of monsoonal forcing: The application of a generic model. Journal of Marine Systems, 36, 239-267.
21. 2 during glacial periods. Paleoceanography, 18, 1046 (doi: 10.1029/2002PA 000810).
22. Bopp L, Le Quéré C, Heimann M et al. (2002) Climate-induced oceanic oxygen fluxes: Implications for the contemporary carbon budget. Global Biogeochemical Cycles, 16, doi: 10.1029/ 2001GB001445.
23. Bopp L, Monfray P, Aumont O et al. (2001) Potential impact of climate change on marine export production. Global Biogeochemical Cycles, 15, 81 -99.
24. Bouman HA, Platt T, Sathyendranath S et al. (2003) Temperature as indicator of optical properties and community structure of marine phytoplankton: Implications for remote sensing. Marine Ecology Progress Series, 258, 19 -30.
25. Boyd P, Doney SC (2003) The impact of climate change and feedback process on the ocean carbon cycle. In: Ocean Biogeochemistry: The Role of the Ocean Carbon Cycle in Global Change (ed. Fasham MJR), pp. 157-187. Springer, Berlin.
26. Boyd PW, Doney SC (2002) Modelling regional responses by marine pelagic ecosystems to global climate change. Geophysical Research Letters, 29, doi: 10.1029/2001GL014130.
27. Boyd PW, Law CS, Wong CS et al. (2004) The decline and fate of an iron-induced subarctic phytoplankton bloom. Nature, 428, 549-553.
28. Boyd PW, Watson AJ, Law CS et al. (2000) A mesoscale phytoplankton bloom in the polar Southern Ocean stimulated by iron fertilization. Nature, 407, 695-702.
29. Brix H, Gruber N, Keeling CD (2004) Interannual variability in the surface ocean carbon cycle at station ALOHA near Hawaii. Global Biogeochemical Cycles, 18, GB4019 (doi: 10.1029/2004GB002245).
30. Broecker WS (1991) Keeping global change honest. Global Biogeochemical Cycles, 5, 191-192.
31. 2 changes. Paleoceanography, 13, 352-364.
32. Brown BE, Dunne RP, Goodson MS et al. (2000) Bleaching patterns in reef corals. Nature, 404, 142-143.
33. Brown CW, Yoder JA (1994) Coccolithophorid blooms in the global ocean. Journal of Geophysical Research-Oceans, 99, 7467-7482.
34. Brussaard CPD, Noordeloos AAM, Riegman R (1997) Autolysis kinetics of the marine diatom Ditylum brightwellii (Bacillariophyceae) under nitrogen and phosphorus limitation and starvation. Journal of Phycology, 33, 980-987.
35. Buesseler KO, Andrews JE, Pike SM et al. (2004) The effects of iron fertilization on carbon sequestration in the Southern Ocean. Science, 304, 414-417.
36. Buffle J (1988) Complexation Reactions in Aquatic Systems: An Analytical Approach. Ellis Horwood, Chichester.
37. Buitenhuis E, van Bleijswijk J, Bakker D et al. (1996) Trends in inorganic and organic carbon in a bloom of Emiliania huxleyi in the North Sea. Marine Ecology Progress Series, 143, 271-282.
38. Catubig NR, Archer DE, Francois R et al. (1998) Global deep-sea burial rate of calcium carbonate during the last glacial maximum. Paleoceanography, 13, 298-310.
39. Claustre H (1994) The trophic status of various oceanic provinces as revealed by phytoplankton pigment signatures. Limnology and Oceanography, 39, 1206-1210.
40. Coale KH, Johnson KS, Chavez FP et al. (2004) Southern ocean iron enrichment experiment: Carbon cycling in high- and low-Si waters. Science, 304, 408 -414.
41. Coale KH, Johnson KS, Fitzwater SE et al. (1996) A massive phytoplankton bloom induced by an ecosystem-scale iron fertilization experiment in the equatorial Pacific Ocean. Nature, 383, 495-501.
42. Conkright ME (2002) World Ocean Database 2001. Volume 1: Introduction. NOAA Atlas NESDIS, Vol. 42. U.S. Government Printing Office, Washington, DC.
43. Copin-Montégut C, Copin-Montégut G (1983) Stoichiometry of carbon, nitrogen, and phosphorus in marine particulate matter. Deep-Sea Research Part A-Oceanographic Research Papers, 30, 31-46.
44. Cox PM, Betts RA, Jones CD et al. (2000) Acceleration of global warming due to carbon-cycle feedbacks in a coupled climate model. Nature, 408, 184-187.
45. 2 and climate change: Results from six dynamic global vegetation models. Global Change Biology, 7, 357-373.
46. Crosta X, Pichon J-J, Burckle LH (1998) Reappraisal of Antarctic seasonal sea-ice at the Last Glacial Maximum. Geophysical Research Letters, 25, 2703-2706.
47. de Baar HJW, Boyd PW (2000) The role of iron in plankton ecology and carbon dioxide transfer of the global oceans. In: The Changing Ocean Carbon Cycle: A Midterm Synthesis of the Joint Global Ocean Flux Study (eds Hanson RB, Ducklow HW, Field JG), pp. 61-140. Cambridge University Press, Cambridge.
48. de Vernal A, Hillaire-Marcel C, Turon JL et al. (2000) Reconstruction of sea-surface temperature, salinity, and sea-ice cover in the northern North Atlantic during the last glacial maximum based on dinocyst assemblages. Canadian Journal of Earth Sciences, 37, 725-750.
49. Denman K, Hofmann E, Marchant H et al. (1996) Marine biotic responses to environmental change and feedbacks to climate. In: Climate change 1995: Contribution of Working Group I to the Second Assessment of the Intergovernmental Panel on Climate Change (eds Houghton JT, Meira LG, Filho BA et al.), pp.485-516. Cambridge University Press, Cambridge.
50. Doerffer R, Fischer J (1994) Concentrations of chlorophyll, suspended matter, and gelbstoff in case II waters derived from satellite coastal zone color scanner data with inverse modeling methods. Journal of Geophysical Research-Oceans, 99, 7457-7466.
51. Doney SC (1999) Major challenges confronting marine biogeochemical modeling. Global Biogeochemical Cycles, 13, 705-714.
52. Doney SC, Lindsay K, Caldeira K et al. (2004) Evaluating global ocean carbon models: The importance of realistic physics. Global Biogeochemical Cycles, 18, GB3017 (doi: 10.1029/2003GB002150).
53. Dutay JC, Bullister JL, Doney SC et al. (2002) Evaluation of ocean model ventilation with CFC-11: Comparison of 13 global ocean models. Ocean Modelling, 4, 89-120.
54. Engel A, Thoms S, Riebesell U et al. (2004) Polysaccharide aggregation as a potential sink of marine dissolved organic carbon. Nature, 428, 929 -932.
55. EPICA community members (2004) Eight glacial cycles from an Antarctic ice core. Nature, 429, 623-628.
56. Eppley RW (1972) Temperature and phytoplankton growth in the sea. Fishery Bulletin, 70, 1063-1085.
57. 2 in the ocean. Nature, 387, 272-275.
58. Falkowski PG, Barber RT, Smetacek V (1998) Biogeochemical controls and feedbacks on ocean primary production. Science, 281, 200-206.
59. Falkowski PG, Laws EA, Barber RT et al. (2003) Phytoplankton and their role in primary, new, and export production. In: Ocean Biogeochemistry: The Role of the Ocean Carbon Cycle in Global Change (ed. Fasham MJR), pp. 99-121. Springer, Berlin.
60. 3 species. Planta, 149, 78-90.
61. Farrera I, Harrison SP, Prentice IC et al. (1999) Tropical climates at the Last Glacial Maximum: A new synthesis of terrestrial palaeoclimate data. I. Vegetation, lake-levels and geochemistry. Climate Dynamics, 15, 823-856.
62. Fasham MJR, Sarmiento JL, Slater RD et al. (1993) Ecosystem behavior at Bermuda Station 'S' and Ocean Weather Station 'India': A general circulation model and observational analysis. Global Biogeochemical Cycles, 7, 379-415.
63. 2 in the equatorial Pacific. Deep-Sea Research Part II-Topical Studies in Oceanography, 49, 2443-2469.
64. 3 system in the oceans. Science, 305, 362-366.
65. 2 accumulation. Nature, 398, 597-601.
66. Finenko ZZ, Piontkovski SA, Williams R et al. (2003) Variability of phytoplankton and mesozooplankton biomass in the subtropical and tropical Atlantic Ocean. Marine Ecology Progess Series, 250, 125-144.
67. Francois R, Honjo S, Krishfield R et al. (2002) Factors controlling the flux of organic carbon to the bathypelagic zone of the ocean. Global Biogeochemical Cycles, 16, doi: 10.1029/2001GB001722.
68. Fung IY, Meyn SK, Tegen I et al. (2000) Iron supply and demand in the upper ocean. Global Biogeochemical Cycles, 14, 281-295.
69. Gasol JM, del Giorgio PA, Duarte CM (1997) Biomass distribution in marine planktonic communities. Limnology and Oceanography, 42, 1353-1363.
70. Geider RJ, La Roche J (2002) Redfield revisited: Variability of C: N: P in marine microalgae and its biochemical basis. European Journal of Phycology, 37, 1-17.
71. Geider RJ, MacIntyre HL, Kana TM (1997) Dynamic model of phytoplankton growth and acclimation: Responses of the balanced growth rate and the chlorophyll a: Carbon ratio to light, nutrient-limitation and temperature. Marine Ecology Progress Series, 148, 187-200.
72. Geider RJ, MacIntyre HL, Kana TM (1998) A dynamic regulatory model of phytoplanktonic acclimation to light, nutrients, and temperature. Limnology and Oceanography, 43, 679-694.
73. Gentleman W, Leising A, Frost B et al. (2003) Functional responses for zooplankton feeding on multiple resources: A review of assumptions and biological dynamics. Deep-Sea Research Part II-Topical Studies in Oceanography, 50, 2847-2875.
74. Gnanadesikan A, Dunne JP, Key RM et al. (2004) Oceanic ventilation and biogeochemical cycling: Understanding the physical mechanisms that produce realistic distributions of tracers and productivity. Global Biogeochemical Cycles, 18, GB4010 (doi: 10.1029/2003GB002097).
75. Gnanadesikan A, Sarmiento JL, Slater RD (2003) Effects of patchy ocean fertilization on atmospheric carbon dioxide and biological production. Global Biogeochemical Cycles, 17, 1050 (doi: 10.1029/2002GB001940).
76. Grassl H (2000) Status and improvements of coupled general circulation models. Science, 288, 1991-1997.
77. Gregg WW, Ginoux P, Schopf PS et al. (2003) Phytoplankton and iron: validation of a global three-dimensional ocean biogeochemical model. Deep-Sea Research Part II-Topical Studies in Oceanography, 50, 3143 -3169.
78. Grossart HP, Ploug H (2001) Microbial degradation of organic carbon and nitrogen on diatom aggregates. Limnology and Oceanography, 46, 267-277.
79. Gruber N, Keeling CD, Bates NR (2002) Interannual variability in the North Atlantic Ocean carbon sink. Science, 298, 2374-2378.
80. Hansen B, Bjørnsen PK, Hansen PJ (1994) The size ratio between planktonic predators and their prey. Limnology and Oceanography, 39, 395-403.
81. Harrison SP, Braconnot P, Joussaume S et al. (2002) Comparison of palaeoclimate simulations enhances confidence in models. EOS, Transactions, American Geophysical Union, 83, 447.
82. Hartmann DL (1994) Global Physical Climatology. Academic Press, San Diego.
83. Hildebrand M, Dahlin K (2000) Nitrate transporter genes from the diatom Cylindrotheca fusiformis (Bacillariophyceae): MRNA levels controlled by nitrogen source and by the cell cycle. Journal of Phycology, 36, 702-713.
84. Hirst AG, Bunker AJ (2003) Growth of marine planktonic copepods: Global rates and patterns in relation to chlorophyll a, temperature, and body weight. Limnology and Oceanography, 48, 1988-2010.
85. Hirst AG, Kiørboe T (2002) Mortality of marine planktonic copepods: Global rates and patterns. Marine Ecology Progress Series, 230, 195-209.
86. 2. Global Change Biology, 8, 1047-1052.
87. Iglesias-Rodríguez MD, Brown CW, Doney SC et al. (2002) Representing key phytoplankton functional groups in ocean carbon cycle models: Coccolithophorids. Global Biogeochemical Cycles, 16, 1100 (doi: 10.1029/2001GB001454).
88. Jackson GA (1990) A model of the formation of marine algal flocs by physical coagulation processes. Deep-Sea Research Part A-Oceanographic Research Papers, 37, 1197-1211.
89. Jahnke RA (1996) The global ocean flux of particulate organic carbon: areal distribution and magnitude. Global Biogeochemical Cycles, 10, 71-88.
90. Jansen H, Wolf-Gladrow DA (2001) Carbonate dissolution in copepod guts: a numerical model. Marine Ecology Progress Series, 221, 199-207.
91. 3 in the ocean. Global Biogeochemical Cycles, 16, doi: 10.1029/2000GB001279.
92. Johnson KS, Gordon RM, Coale KH (1997) What controls dissolved iron concentrations in the world ocean? Marine Chemistry, 57, 137-161.
93. Joos F, Gerber S, Prentice IC et al. (2004) Transient simulations of Holocene atmospheric carbon dioxide and terrestrial carbon since the last glacial maximum. Global Biogeochemical Cycles, 18, GB2002 (doi: 10.1029/2003GB002156).
94. 2. Science, 284, 464-467.
95. Joussaume S, Taylor KE (2000) The paleoclimate modeling intercomparison project. In: Paleoclimate Modelling Intercomparison Project (PMIP). Proceedings of the third PMIP workshop, 4-8 October 1999 (ed. Braconnot P), pp. 9-24. WCRP, Canada, La Huardière.
96. Karl DM (1999) A sea of change: Biogeochemical variability in the North Pacific Subtropical Gyre. Ecosystems, 2, 181-214.
97. Kettle AJ, Andreae MO (2000) Flux of dimethylsulfide from the oceans: A comparison of updated data seas and flux models. Journal of Geophysical Research-Atmospheres, 105, 26793 -26808.
98. Key RM, Kozyr A, Sabine CL et al. (2004) A global ocean carbon climatology: Results from GLODAP. Global Biogeochemical Cycles, 19 (submitted, doi: 10.1029/2004GB002247).
99. Klaas C, Archer DE (2002) Association of sinking 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).
100. Kohfeld KE, Harrison SP (2001) DIRTMAP: The geological record of dust. Earth-Science Reviews, 54, 81-114.
101. 2 cycles. Science 308, 74 -78.
102. Kriest I, Evans GT (1999) Representing phytoplankton aggregates in biogeochemical models. Deep-Sea Research Part I-Oceanographic Research Papers, 46, 1841-1859.
103. Kustka A, Carpenter EJ, Sañudo-Wilhelmy SA (2002) Iron and marine nitrogen fixation: Progress and future directions. Research in Microbiology, 153, 255-262.
104. Kustka AB, Sañudo-Wilhelmy SA, Carpenter EJ et al. (2003) Iron requirements for dinitrogen- and ammonium-supported growth in cultures of Trichodesmium (IMS 101): Comparison with nitrogen fixation rates and iron: Carbon ratios of field populations. Limnology and Oceanography, 48, 1869-1884.
105. Labeyrie LD, Duplessy J-C, Duprat J et al. (1992) Changes in the vertical structure of the North Atlantic Ocean between glacial and modern times. Quaternary Science Reviews, 11, 401-413.
106. Ladner S, Arnone RA, Gould RW Jr et al. (2002) Evaluation of sea WiFS optical products in coastal regions. Sea Technology, 43, 29-35.
107. Laroche D, Vezina AF, Levasseur M et al. (1999) DMSP synthesis and exudation in phytoplankton: A modeling approach. Marine Ecology Progress Series, 180, 37-49.
108. LaRoche J, Breitbarth E (2005) Importance of the diazotrophs as a source of new nitrogen in the ocean. Journal of Sea Research, 53, 67-91.
109. Le Quéré C, Bopp L, Tegen I (2002) Antarctic circumpolar wave impact on marine biology: A natural laboratory for climate change study. Geophysical Research Letters, 29 (doi: 10.1029/2001GL014585).
110. Le Vu B (2005) Le rôle de la biocalcification dans l'océan actuel àtravers l'organisme modèle Emiliania huxleyi. Quand la mer devient blanche. PhD Thesis, UniversitéPierre et Marie Curie -Paris VI.
111. Lee K (2001) Global net community production estimated from the annual cycle of surface water total dissolved inorganic carbon. Limnology and Oceanography, 46, 1287-1297.
112. Li H, Veldhuis MJW, Post AF (1998) Alkaline phosphatase activities among planktonic communities in the northern Red Sea. Marine Ecology Progress Series, 173, 107-115.
113. Liss PS, Hatton AD, Malin G et al. (1997) Marine sulphur emissions. Philosophical Transactions of the Royal Society of London Series B-Biological Sciences, 352, 159-169.
114. Loisel H, Nicolas J-M, Deschamps P-Y et al. (2002) Seasonal and inter-annual variability of particulate organic matter in the global ocean. Geophysical Research Letters, 29, 2196 (doi: 10.1029/ 2002GL015948).
115. Lucht W, Prentice IC, Myneni RB et al. (2002) Climatic control of the high-latitude vegetation greening trend and Pinatubo effect. Science, 296, 1687-1689.
116. MacIntyre HL, Kana TM, Anning T et al. (2002) Photoacclimation of photosynthesis irradiance response curves and photosynthetic pigments in microalgae and cyanobacteria. Journal of Phycology, 38, 17-38.
117. Maier-Reimer E (1993) Geochemical cycles in an ocean general circulation model: Preindustrial tracer distributions. Global Biogeochemical Cycles, 7, 645-677.
118. 2 in the ocean: An inorganic ocean-circulation carbon cycle model. Climate Dynamics, 2, 63-90.
119. 2: Interaction between ocean circulation and biology. Climate Dynamics, 12, 711-721.
120. Makino W, Cotner JB, Sterner RW et al. (2003) Are bacteria more like plants or animals? Growth rate and resource dependence of bacterial C:N: P stoichiometry. Functional Ecology, 17, 121-130.
121. Manizza M, Le QuéréC, Watson AJ et al. (2005) Bio-optical feedbacks among phytoplankton, upper ocean physics and sea-ice in a global model. Geophysical Research Letters (in press).
122. 2 uptake. Tellus Series B-Chemical and Physical Meteorology, 51, 722-733.
123. Milliman JD (1993) Production and accumulation of calcium carbonate in the ocean: Budget of a nonsteady state. Global Biogeochemical Cycles, 7, 927-957.
124. Milliman JD, Troy PJ, Balch WM et al. (1999) Biologically mediated dissolution of calcium carbonate above the chemical lysocline? Deep-Sea Research Part I-Oceanographic Research Papers, 46, 1653-1669.
125. Mills MM, Ridame C, Davey M et al. (2004) Iron and phosphorus co-limit nitrogen fixation in the eastern tropical North Atlantic. Nature, 429, 292-294.
126. Mitchell JMJ (1990) Climatic variability: Past, present and future. Journal of Atmospheric and Terrestrial Physics, 52, 231-246.
127. Mix AC, Morey AE, Pisias NG et al. (1999) Foraminiferal faunal estimates of paleotemperature: Circumventing the no-analog problem yields cool ice age tropics. Paleoceanography, 14, 350-359.
128. Moore JK, Doney SC, Kleypas JA et al. (2002) An intermediate complexity marine ecosystem model for the global domain. Deep-Sea Research Part II-Topical Studies in Oceanography, 49, 403-462.
129. Morel A, Berthon JF (1989) Surface pigments, algal biomass profiles, and potential production of the euphotic layer: Relationships reinvestigated in view of remote-sensing applications. Limnology and Oceanography, 34, 1545-1562.
130. Najjar RG, Sarmiento JL, Toggweiler JR (1992) Downward transport and fate of organic matter in the ocean: Simulations with a general circulation model. Global Biogeochemical Cycles, 6, 45-76.
131. 2O due to intensifying anoxia on the Indian continental shelf. Nature, 408, 346-349.
132. O'Brien TD, Conkright ME, Boyer TP et al. (2002) World Ocean Atlas 2001, Vol. 5: Plankton, NOAA Atlas NESDIS 53 (ed. Levitus S.), U.S. Government Printing Office, Washington, DC (Available at: http://www.nodc.noaa.gov/ OC5/indpub.html#pub2002).
133. Ohman MD, Hirche HJ (2001) Density-dependent mortality in an oceanic copepod population. Nature, 412, 638-641.
134. Passow U, Alldredge AL (1995) Aggregation of a diatom bloom in a mesocosm -the role of transparent exopolymer particles (TEP). Deep-Sea Research Part II-Topical Studies in Oceanography, 42, 99-109.
135. Petit JR, Jouzel J, Raynaud D et al. (1999) Climate and atmospheric history of the past 4 20 000 years from the Vostok ice core, Antarctica. Nature, 399, 429-436.
136. Ploug H (2001) Small-scale oxygen fluxes and remineralization in sinking aggregates. Limnology and Oceanography, 46, 1624-1631.
137. Prentice IC, Farquhar GD, Fasham MJR et al. (2001) The carbon cycle and atmospheric carbon dioxide. In: Climate Change 2001: The Scientific Basis. Contribution of Working Group I to the Third Assessment Report of the Intergovernmental Panel on Climate Change (eds Houghton JT, Ding Y, Griggs DJ et al.), pp. 183-237. Cambridge University Press, Cambridge.
138. Prentice IC, Heimann M, Sitch S (2000) The carbon balance of the terrestrial biosphere: Ecosystem models and atmospheric observations. Ecological Applications, 10, 1553-1573.
139. Prentice IC, Le QuéréC, Buitenhuis ET et al. (2004) Biosphere dynamics: Questions for Earth system modelling. In: The State of the Planet: Frontiers and Challenges. Geophysical Monograph Series, Vol. 150 (eds Hawkesworth C, Sparks R), AGU.
140. Raven JA, Kübler JE (2002) New light on the scaling of metabolic rate with the size of algae. Journal of Phycology, 38, 11-16.
141. Redfield AC (1934) On the proportions of organic derivatives in sea water and their relation to the composition of plankton. In: James Johnstone Memorial Volume (ed. Johnstone J), pp. 176-192. University Press of Liverpool, Liverpool.
142. Rickert D, Schludie;ter M, Wallmann K (2002) Dissolution kinetics of biogenic silica from the water column to the sediments. Geochimica Et Cosmochimica Acta, 66, 439-455.
143. Riebesell U, Wolf-Gladrow DA (1992) The relationship between physical aggregation of phytoplankton and particle flux: A numerical model. Deep-Sea Research Part A-Oceanographic Research Papers, 39, 1085-1102.
144. Riebesell U, Zondervan I, Rost B et al. (2000) Reduced calcification of marine plankton in response to increased atmospheric CO 2. Nature, 407, 364-367.
145. Riegman R, Stolte W, Noordeloos AAM et al. (2000) Nutrient uptake, and alkaline phosphate (ec 3:1:3:1) activity of Emiliania huxleyi (prymnesiophyceae) during growth under N and P limitation in continuous cultures. Journal of Phycology, 36, 87-96.
146. Rivkin RB, Legendre L (2001) Biogenic carbon cycling in the upper ocean: effects of microbial respiration. Science, 291, 2398-2400.
147. Rivkin RB, Legendre L (2002) Roles of food web and heterotrophic microbial processes in upper ocean biogeochemistry: Global patterns and processes. Ecological Research, 17, 151-159.
148. Rivkin RB, Legendre L, Deibel D et al. (1996) Vertical flux of biogenic carbon in the ocean: Is there food web control? Science, 272, 1163-1166.
149. K' index: Comparison with GCMs. Geophysical Research Letters, 31, L03208 (doi: 10.1029/2003GL018151).
150. Ruiz J, Prieto L, Ortegon F (2002) Diatom aggregate formation and fluxes: A modeling analysis under different size-resolution schemes and with empirically determined aggregation kernels. Deep-Sea Research Part I-Oceanographic Research Papers, 49, 495-515.
151. Sabine CL, Feely RA, Key RM et al. (2002) Distribution of anthropogenic CO 2 in the Pacific Ocean. Global Biogeochemical Cycles, 16, 1083 (doi: 10.1029/2001GB001639).
152. Sañudo-Wilhelmy SA, Kustka AB, Gobler CJ et al. (2001) Phosphorus limitation of nitrogen fixation by Trichodesmium in the central Atlantic Ocean. Nature, 411, 66-69.
153. 3 to organic carbon export ratio. Global Biogeochemical Cycles, 16, 1107 (doi: 10.1029/2002GB001919).
154. Sarmiento JL, Gruber N, Brzezinski MA et al. (2004) High-latitude controls of thermocline nutrients and low latitude biological productivity. Nature, 427, 56-60.
155. Sarmiento JL, Hughes TMC, Stouffer RJ et al. (1998) Simulated response of the ocean carbon cycle to anthropogenic climate warming. Nature, 393, 245-249.
156. Sarmiento JL, Le QuéréC (1996) Oceanic carbon dioxide uptake in a model of century-scale global warming. Science, 274, 1346-1350.
157. Sarthou G, Timmermans KR, Blain S et al. (2005) Growth physiology and fate of diatoms in the ocean: A review. Journal of Sea Research, 53, 25-42.
158. Sathyendranath S, Gouveia AD, Shetye SR et al. (1991) Biological control of surface temperature in the Arabian sea. Nature, 349, 54-56.
159. Sathyendranath S, Watts L, Devred E et al. (2004) Discrimination of diatoms from other phytoplankton using ocean-colour data. Marine Ecology Progress Series, 272, 59-68.
160. Schiebel R (2002) Planktic foraminiferal sedimentation and the marine calcite budget. Global Biogeochemical Cycles, 16, 1065 (doi: 10.1029/ 2001GB001459).
161. Schlitzer R (2000) Applying the adjoint method for biogeochemical modeling: Export of particulate organic matter in the world ocean. In: Inverse Methods in Global Biogeochemical Cycles (eds Kasibhatla P, Heimann M, Rayner P et al.), pp. 107-124. AGU, Washington, DC.
162. Schlitzer R (2002) Carbon export fluxes in the Southern Ocean: Results from inverse modeling and comparison with satellite-based estimates. Deep-Sea Research Part II-Topical Studies in Oceanography, 49, 1623-1644.
163. Schneider B, Schlitzer R, Fischer G et al. (2003) Depth-dependent elemental compositions of particulate organic matter (POM) in the ocean. Global Biogeochemical Cycles, 17 (doi: 10.1029/2002GBC001871).
164. Schoemann V, Becquevort S, Stefels J (2005) Phaeocystis blooms in the global ocean and their controlling mechanisms: A review. Journal of Sea Research, 53, 43-66.
165. Schulz KG, Zondervan I, Gerringa LJA et al. (2004) Effect of trace metal availability on coccolithophorid calcification. Nature, 430, 673-676.
166. Sciare J, Mihalopoulos N, Dentener FJ (2000) Interannual variability of atmospheric dimethylsulfide in the southern Indian Ocean. Journal of Geophysical Research-Atmospheres, 105, 26369-26377.
167. 15 N of nitrate in the Southern Ocean: Nitrogen cycling and circulation in the ocean interior. Journal of Geophysical Research-Oceans, 105, 19599-19614.
168. Six KD, Maier-Reimer E (1996) Effects of plankton dynamics on seasonal carbon fluxes in an ocean general circulation model. Global Biogeochemical Cycles, 10, 559-583.
169. Smith B, Prentice IC, Sykes MT (2001) Representation of vegetation dynamics in the modelling of terrestrial ecosystems: Comparing two contrasting approaches within European climate space. Global Ecology and Biogeography, 10, 621-637.
170. Sonzogni C, Bard E, Rostek F (1998) Tropical sea-surface temperatures during the last glacial period: A view based on alkenones in Indian
171. Staal M, Meysman FJR, Stal LJ (2003) Temperature excludes N 2 -fixing heterocystous cyanobacteria in the tropical oceans. Nature, 425, 504-507.
172. Stefels J, Dijkhuizen L, Gieskes WWC (1995) DMSP-lyase activity in a spring phytoplankton bloom off the Dutch coast, related to Phaeocystis sp. abundance. Marine Ecology Progress Series, 123, 235-243.
173. Steffen WL (1996) A periodic table for ecology? A chemist's view of plant functional types. Journal of Vegetation Science, 7, 425-430.
174. Stemmann L, Jackson GA, Gorsky G (2004) A vertical model of particle size distributions and fluxes in the midwater column that includes biological and physical processes -Part II: Application to a three year survey in the NW Mediterranean Sea. Deep-Sea Research Part I-Oceanographic Research Papers, 51, 885-908.
175. Stihl A, Sommer U, Post AF (2001) Alkaline phosphatase activities among populations of the colony-forming diazotrophic cyanobacterium Trichodesmium spp. (cyanobacteria) in the Red Sea. Journal of Phycology, 37, 310-317.
176. Strom S (2002) Novel interactions between phytoplankton and microzooplankton: Their influence on the coupling between growth and grazing rates in the sea. Hydrobiologia, 480, 41-54.
177. Subramaniam A, Brown CW, Hood RR et al. (2002) Detecting Trichodesmium blooms in SeaWiFS imagery. Deep-Sea Research Part II-Topical Studies in Oceanography, 49, 107-121.
178. Subramaniam A, Carpenter EJ, Falkowski PG (1999) Bio-optical properties of the marine diazotrophic cyanobacteria Trichodesmium spp. II. A reflectance model for remote sensing. Limnology and Oceanography, 44, 618-627.
179. 2, and seasonal biological and temperature effects. Deep-Sea Research Part II-Topical Studies in Oceanography, 49, 1601-1622.
180. Thingstad TF, Lignell R (1997) Theoretical models for the control of bacterial growth rate, abundance, diversity and carbon demand. Aquatic Microbial Ecology, 13, 19-27.
181. Tyrrell T (1999) The relative influences of nitrogen and phosphorus on oceanic primary production. Nature, 400, 525-531.
182. van Cappellen P, Dixit S, van Beusekom J (2002) Biogenic silica dissolution in the oceans: Reconciling experimental and field-based dissolution rates. Global Biogeochemical Cycles, 16, 1075 (doi: 10.1029/ 2001GB001431).
183. Veldhuis MJW, Admiraal W (1987) Influence of phosphate depletion on the growth and colony formation of Phaeocystis pouchetii. Marine Biology, 95, 47-54.
184. Veldhuis MJW, Timmermans KR, Croot P et al. (2005) Picophytoplankton; a comparative study of their biochemical composition and photosynthetic properties. Journal of Sea Research, 53, 7-24.
185. Vidussi F, Claustre H, Manca BB et al. (2001) Phytoplankton pigment distribution in relation to upper thermocline circulation in the eastern Mediterranean Sea during winter. Journal of Geophysical Research-Oceans, 106, 19939-19956.
186. Wefer G, Berger WH, Bijma J (1999) Clues to ocean history: A brief overview of proxies. In: Use of Proxies in Paleoceanography: Examples from the South Atlantic (eds Fischer G, Wefer G), pp. 1-68. Springer, Berlin.
187. Weinelt M, Sarnthein M, Pflaumann U et al. (1996) Ice-free nordic seas during the last glacial maximum? Potential sites of deepwater formation. Palaeoclimates: Data and Modelling, 1, 283-309.
188. Whitman WB, Coleman DC, Wiebe WJ (1998) Prokaryotes: The unseen majority. Proceedings of the National Academy of Sciences of the United States of America, 95, 6578-6583.
189. Yoder JA, Kennelly MA (2003) Seasonal and ENSO variability in global ocean phytoplankton chlorophyll derived from 4 years of SeaWiFS measurements. Global Biogeochemical Cycles, 17, 1112 (doi: 10.1029/ 2002GB001942).
190. Zehr JP, Waterbury JB, Turner PJ et al. (2001) Unicellular cyanobacteria fix N 2 in the subtropical North Pacific Ocean. Nature, 412, 635-638.