299
Smith DJ, Eglinton G, Morris RJ (1983) Interfacial sediment and assessment of organic input
from a highly productive water column. Nature 304:259-262
Smith WO, Nelson DM (1985) Phytoplankton bloom produced by a receding ice edge in the
Ross Sea: spatial coherence with the density field. Science 227: 163-166
Sournia A, Birrien JL, Douville JL, Klein B, Viollier M (1987) A daily study of the diatom
spring bloom at Roscoff (France) in 1985. I. The spring bloom within the annual cycle.
Est Coast Shelf Sci 25:355-367
Southward AI (1974) Long term changes in abundance of eggs of the Cornish pilchard
(Sardina pilchardus Walbaum) off Plymouth. J Mar BioI Ass UK 54:641-649
Southward AI (1980) The western English Channel - an inconstant ecosystem? Nature
285 :361-366
Southward AI (1983) Fluctuations in the ecosystems of the Western Channel: a summary of
studies in progress. Oceanol Acta, Proceedings 17th European Marine Biology Symposium
(special issue): 187-189
Suess E (1973) Interaction of organic compounds with calcium carbonate.
II. Organo-carbonate association in recent sediments. Geochim Cosmochim Acta
37:2435-2447
Sugimura Y, Suzuki Y (1988) A high temperature catalytic oxidation method of non-volatile
dissolved organic carbon in seawater by direct injection of liquid samples. Mar Chern
24:105-131
Sundquist ET (1985) Geological perspectives on carbon dioxide and the carbon cycle. In:
Sundquist ET, Broecker WS (eds) The carbon cycle and atmospheric CO 2 : natural
variations archean to present. AGU Monograph 32, Amer Geophys Union, Washington
DC, 5-59
Sverdrup HU (1953) On conditions for the vernal blooming of phytoplankton. J Cons Int
Explor Mer 18:287-295
Sverdrup HU, Johnson MW, Fleming RH (1942) The oceans. Their physics, chemistry and
general biology. Prentice-Hall, Englewood Cliffs, NJ
Takahashi K, Be A WH (1984) Planktonic foraminifers: factors controlling sinking speeds.
Deep-Sea Res 31:1477-1500
Takahashi M, Hori T (1984) Abundance of picoplankton in the subsurface chlorophyll
maximum layer in subtropical and tropical waters. Mar BioI 79: 177-186.
Takahashi M, Seibert DL, Thomas WH (1977) Occasional blooms of phytoplankton during
summer in Saanich Inlet, B.C., Canada. Deep-Sea Res 24:775-780
Tett P (1987) The ecophysiology of exceptional blooms. Rapp P-V Reun Cons Int Explor Mer
187:47-60
Toggweiler JR (1989) Is the downward dissolved organic matter (DOM) flux important in
carbon transport? In: Berger WH, Smetacek VS, Wefer G (eds) Productivity ofthe ocean:
present and past, Wiley and Sons, Chichester, 65-83
Venrick EL (1974) The distribution and significance of Richelia intracellularis Schmidt in the
North Pacific Central Gyre. LimnolOceanogr 19:437-445
Yolk T (1989) Sensitivity of climate and atmospheric CO 2 to deep-ocean and shallow-ocean
carbonate burial. Nature 337:637-638
Yolk T, Hoffert MI (1985) Ocean carbon pumps: Analysis of relative strengths and
efficiencies in ocean driven CO2 changes. In: Sundquist ET, Broecker WS (eds) The
carbon cycle and atmospheric CO2: natural variations archean to present. AGU
Monograph 32, Amer Geophys Union, Washington DC, 99-110
Smith DJ, Eglinton G, Morris RJ (1983) Interfacial sediment and assessment of organic input
from a highly productive water column. Nature 304:259-262
Smith WO, Nelson DM (1985) Phytoplankton bloom produced by a receding ice edge in the
Ross Sea: spatial coherence with the density field. Science 227: 163-166
Sournia A, Birrien JL, Douville JL, Klein B, Viollier M (1987) A daily study of the diatom
spring bloom at Roscoff (France) in 1985. I. The spring bloom within the annual cycle.
Est Coast Shelf Sci 25:355-367
Southward AI (1974) Long term changes in abundance of eggs of the Cornish pilchard
(Sardina pilchardus Walbaum) off Plymouth. J Mar BioI Ass UK 54:641-649
Southward AI (1980) The western English Channel - an inconstant ecosystem? Nature
285 :361-366
Southward AI (1983) Fluctuations in the ecosystems of the Western Channel: a summary of
studies in progress. Oceanol Acta, Proceedings 17th European Marine Biology Symposium
(special issue): 187-189
Suess E (1973) Interaction of organic compounds with calcium carbonate.
II. Organo-carbonate association in recent sediments. Geochim Cosmochim Acta
37:2435-2447
Sugimura Y, Suzuki Y (1988) A high temperature catalytic oxidation method of non-volatile
dissolved organic carbon in seawater by direct injection of liquid samples. Mar Chern
24:105-131
Sundquist ET (1985) Geological perspectives on carbon dioxide and the carbon cycle. In:
Sundquist ET, Broecker WS (eds) The carbon cycle and atmospheric CO 2 : natural
variations archean to present. AGU Monograph 32, Amer Geophys Union, Washington
DC, 5-59
Sverdrup HU (1953) On conditions for the vernal blooming of phytoplankton. J Cons Int
Explor Mer 18:287-295
Sverdrup HU, Johnson MW, Fleming RH (1942) The oceans. Their physics, chemistry and
general biology. Prentice-Hall, Englewood Cliffs, NJ
Takahashi K, Be A WH (1984) Planktonic foraminifers: factors controlling sinking speeds.
Deep-Sea Res 31:1477-1500
Takahashi M, Hori T (1984) Abundance of picoplankton in the subsurface chlorophyll
maximum layer in subtropical and tropical waters. Mar BioI 79: 177-186.
Takahashi M, Seibert DL, Thomas WH (1977) Occasional blooms of phytoplankton during
summer in Saanich Inlet, B.C., Canada. Deep-Sea Res 24:775-780
Tett P (1987) The ecophysiology of exceptional blooms. Rapp P-V Reun Cons Int Explor Mer
187:47-60
Toggweiler JR (1989) Is the downward dissolved organic matter (DOM) flux important in
carbon transport? In: Berger WH, Smetacek VS, Wefer G (eds) Productivity ofthe ocean:
present and past, Wiley and Sons, Chichester, 65-83
Venrick EL (1974) The distribution and significance of Richelia intracellularis Schmidt in the
North Pacific Central Gyre. LimnolOceanogr 19:437-445
Yolk T (1989) Sensitivity of climate and atmospheric CO 2 to deep-ocean and shallow-ocean
carbonate burial. Nature 337:637-638
Yolk T, Hoffert MI (1985) Ocean carbon pumps: Analysis of relative strengths and
efficiencies in ocean driven CO2 changes. In: Sundquist ET, Broecker WS (eds) The
carbon cycle and atmospheric CO2: natural variations archean to present. AGU
Monograph 32, Amer Geophys Union, Washington DC, 99-110