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Biogeochemical Controls and Feedbacks on the Ocean Primary Production. Carbon Cycle. Marine Biota. Export Production. Export Production of Organic Carbon. Ocean Ecosystem Structure. Trophic levels and dynamics. Ocean Ecosystem Structure. Example of a more complex Food Web.
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Biogeochemical Controls and Feedbacks on the Ocean Primary Production
Carbon Cycle Marine Biota Export Production
Ocean Ecosystem Structure Trophic levels and dynamics
Ocean Ecosystem Structure Example of a more complex Food Web
Ocean Ecosystem Structure Energy Transfer between Trophic Levels is not efficient
Trophic levels and dynamics Food Web Energy
Large scale Eddies 200 km
A useful way to keep track of biomass in the lower trophic levels is to follow the path of MACRONUTRIENTS Carbon C Nitrogen N Phosphorus P
Redfield Ratio C : N : P 106 : 16 : 1 Redfield A.C.,On the proportions of organic derivations in seawater and their relation to the composition of plankton. In James Johnson Memorial Volume. (ed. R.J. Daniel). University Press of Liverpool, pp. 177-192.
C : N : P source 1) atmosphere source 1) from N2 atmosphere gas2) ocean subsurface3) remineralization of dead organic matter 4) biological (e.g. excretions) source 1) not biological, not atmospheric2) fluvial Nitrogen appears to be the limiting factorin ocean productivity in todays oceans
Description of the oceanic ecosystem based on Nitrogen exchanges Fixation N2 Nitrification Mineralization NH4 NO3 Uptake Phytoplankton Grazing Mix Layer depth Chlorophyll Zooplankton Mortality Large detritus Water column Susp. particles Nitrification N2 NH4 NO3 Denitrification Aerobic mineralization Organic matter Sediment
Carbon Cycle Marine Biota Export Production
What are the controls on Export Production? Nutrient Sources for Primary Production The fluxed of organic carbon must be sustained by an adeguate flux of macronutrients If macronutrients are unavailable then the CO2 flux is reduced!
What are the controls on Export Production? • Ocean nutrient inventory • 2) Utilization of nutrients in HNLC • 3) Change Redfield Ratio
Surface CHL-A 1) Central Gyres 2) Upwelling Regions
What are the controls on Export Production? • Ocean nutrient inventory Nitrogen appears to be the control duringmodern time. (but was not always this way e.g. duringlat glacial maxima)
Modern TIME N2 fixation Denitrification N = 25790 N* = N – 16 P (Gruber & Sarmiento 1997)
What are the controls on Export Production? 2) Utilization of nutrients in HNLC
High Nutrient, Low (Medium) Chlorophyll Regions Why aren’t the nutrients being completely utilized by phytoplankton? Phosphorous Chlorophyll Conkright et al., 1994 µm SeaWiFs
What are the controls on Export Production? 3) Change Redfield Ratio Do not know much about this!
Biologically Mediated Exchange of CO2 Between the Ocean and Atmosphere The fluxed of organic carbon must be sustained by an adeguate flux of macronutrients
Phytoplankton Blooms Bands of the dionflagellate Lingulodinium polyedrum moving onshore over the troughs of a series of internal waves
Trophic levels and dynamics Food Web Energy