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| .p073 ref [[ https://www.nature.com/articles/41457 | CO2 increases oceanic primary production ]] Mette Hein & Kaj Sand-Jensen Nature volume 388, pages 526–527 (1997) | .p073 ref [[ https://www.nature.com/articles/41457 | CO₂ increases oceanic primary production ]] Mette Hein & Kaj Sand-Jensen Nature volume 388, pages 526–527 (1997) |
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| .p109 [[ | ]] .p111 [[ | ]] .p156 [[ | ]] .p157 [[ | ]] .p161 [[ | ]] .p163 [[ | ]] .p163 [[ | ]] .p170 [[ | ]] .plate 7.1 Global annual net primary production .p182 ref [[ | ]] |
.p109 DBL Diffusive Boundary Layer .p111 [[ https://en.wikipedia.org/wiki/Redfield_ratio | Redfield Ratio ]] C:N:P 106:16:1 .p156 <2002 fossil fuel consumption 6e15 grams carbon / year .2002 2.6e16g CO₂, 2022 3.8e16g CO₂, 2022 land use and deforestation adds 6e15g CO₂ .GCM Global Climate Models? Or [[ https://en.wikipedia.org/wiki/General_circulation_model | general circulation model? ]] .p157 biosphere net primary productivity 12e16g carbon .p157 APAR absorbed photsynthetically active radiation .p157 NDVI normalized difference vegetation index .p159 DIMs Depth Integrated Models calculate ΣNPP .p159 TIMs Time Integrated Models .p159 WIMs Wavelength Integrated Models .p159 WRMs Wavelength Resolved Models, subsurface irradiance .p163 TIMs variability of depth dependent carbon fixation as a function of daily surface PAR .p163 TIMs integrated into daily DIMs .p170 [[ https://en.wikipedia.org/wiki/Vertically_Generalized_Production_Model | VGPM ]] global NPP 59e15 gC/year .plate 7.1 Global annual net primary production - 500 gC/m²y on continental shelves, <200 elsewhere .p182 ref [[ https://www.researchgate.net/profile/Zbigniew-Kolber-3/publication/13356425_Widespread_Iron_Limitation_of_Phytoplankton_in_the_South_Pacific_Ocean/links/0c9605304320f403da000000/Widespread-Iron-Limitation-of-Phytoplankton-in-the-South-Pacific-Ocean.pdf | Widespread Iron Limitation of Phytoplankton in the South Pacific Ocean ]] Michael J. Behrenfeld* and Zbigniew S. Kolber @Rutgers, Science 5 Feb 1999 p840 |
- wiki.keithl.com/Phytoplankton
Phytoplankton Books
Algal Cultures and Phytoplankton Ecology
p158 Viruses (cyanophages) and myxobacteria causing lysis of blue-green algae
p226 ref J. A. Bassham and M. Calvin 1957 The Path of Carbon in Photosynthesis @PSU QK882.B3
p228 The seasonal variation in oceanic production as a problem in population dynamics D. H. Cushing 1959
- p229 Cushing 1959 no online source
- p229 M. R. Droop Heterotrophy of carbon 1974 Algal Physiology and Biochemistry
p232 E. Fogg et. al. 1973 459p The Blue-Green Algae WSU Vancouver Library purchased $16.08
p233 W.W.C. Gieskes Current 14C methods for measuring primary production: Gross underestimates in oceanic waters
p236 O Holm-Hansen, K Nishida, V Moses, M Calvin Journal of Experimental Botany, 1959 [[ https://escholarship.org/content/qt42q33467/qt42q33467_noSplash_4e281a8d4b5fc18255d66c9cee28ec22.pdf | Effects of Mineral Salts on Short-term Incorporation of Carbon Dioxide inChlorella] ]
p245 Trevor Platt D. V. Subba Rao 1970 Primary Production Measurements on a Natural Plankton Bloom
p245 Karen Glaus Porter 1976 https://www.science.org/doi/abs/10.1126/science.192.4246.1332
p260i Perspectives in Marine Biology 1958 PSU QH91.S8 1956 p299-322 Rohde& The Primary Production and Standing Crop of Phytoplankton
- p265i Oligotrophic refers to environments, particularly lakes and other aquatic systems, that have very low concentrations of nutrients such as nitrates, phosphates, and organic matter, resulting in limited biological productivity.
p266i Phagotrophy
p266i Primary Productivity
Phytoplankton 2nd Ed 1989 - Arthur Donald Boney Emeritus Professor of Botany University of Glasgow
- PSU QK933.B66 1989
- pelagic zone: water column of the open ocean
p001 thallus, no organization into tissues such as vascular structure
p001 all algae contain chlorophyll a, a poor absorber of green light
p003 Red tides toxic dinoflagellates
p013 coccolith plates of calcium carbonate, perhaps protective against predation
p016 Primary production autotroph produces own food heterotroph consumes producers
- p017 Global primary production 1.4e14 to 1.8e14 kg/year dry matter, oceans only 35% of the total
why not 70%, proportional to ocean/land ratio? If land production remained the same, the total land plus ocean productivity could increase by a factor of 2.16 ... and that's before improving predation resistance and engineering new photosynthetic processes.
p018 PAR Photosynthetically active radiation
- p018 Clear winter's day light intensity 20% of summer, 10% with clouds
p019 thylakoids membrane-bound compartments inside chloroplasts and cyanobacteria
p019 stroma
p019 pyrenoids
p019 phycobilin
p019 carotenes absorb UV, violet, and blue light
p019 xanthrophyll yellow pigments
- p019 Sun vertical, 2% light reflection, near horizon 90% reflection
p021 humic acids
p021 gilvin colored humic substances
- p023 depth d at which lowered white disk disappears
- p023 surface inhibition, light too intense for phytoplankton
- p024 continuous sunlight and prolonged calm injures Arctic phytoplankton and inhibits photosynthesis
p026 epilimnion surface layer hypolimnion depths metalimnion between
p026 sieche standing wave in body of water
p029 photosynthetic activity will increase pH in favor of bicarbonate users
p032 orthosilicic acid makes silica cell walls, 26% to 63%
p033 desmid green algae, progenitors of land plants
p034 Iron fertilization
- p034 primary production may be limited by the availability of iron and other trace elements
- p034 manganous = +2 oxidation state
p035 copper in plastocyanin mediates electron-transfer
p035 cyancobalamine B12 thiamine biotin B7 required by plantonic algae
p036 auxotrophs dependent on other sources of vitamins
p036 auxospores in growth processes, sexual reproduction, or dormancy
- p036 coastal phytoplankton excrete 35% of fixed carbon CITATION NEEDED
p036 eutrophication can be long term enrichment of aging process in natural waters
p037 heterotrophs deplete water of oxygen -> high biochemical oxygen demand (BOD)
p037 euryhaline species adapt to varied salinities, stenohaline (i.e. freshwater fish) cannot
p037 stenohaline in fresh water suffer cell distortion/rupture, freshwater algae in seawater plasmolysed
p038 regions enriched with phosphate -> dense algae within two months, not with nitrate and sucrose
- p041 cell must keep moving for continuing nutrient supply, phytoplankyton tend to sink
- p041 net production nil if mixed zone 5x deeper than euphotic zone
- p043 small cells with high surface to volume ratio have higher friction and sink slowest
- p079 Extracellular products pass from cell to medium, photo-synthetically derived organic carbon, PDOC
- p079 dm³ =decimeter cubed = liter
- p094 Measuring Primary Productivity
- p105 phytoplankton "farm" in liquid tubes, 12.5 tonnes per hectare. Better radiation input could triple that, eightfold increase over cultivated land. Edibility questionable, taste barrier, animal feed? Cell wall lowers food value
- KL can cell wall be "designed out" with genetic engineering in a pathogen-free environment?
Phytoplankton Productivity
Carbon assimilation in marine and freshwater ecosystems
- P.J. le B. Williams, D.N. Thomas, C.S. Reynolds . . PSU QK933 .P52 2002
p073 ref CO₂ increases oceanic primary production Mette Hein & Kaj Sand-Jensen Nature volume 388, pages 526–527 (1997)
- pxxx numerically abundant groups of phytoplankton live hours to days
- p086 first trophic transition between autotrophs and grazers, 10% to 20% efficiency, 2x errors in net primary productivity
- p109 DBL Diffusive Boundary Layer
p111 Redfield Ratio C:N:P 106:16:1
p156 <2002 fossil fuel consumption 6e15 grams carbon / year
- 2002 2.6e16g CO₂, 2022 3.8e16g CO₂, 2022 land use and deforestation adds 6e15g CO₂
GCM Global Climate Models? Or general circulation model?
- p157 biosphere net primary productivity 12e16g carbon
- p157 APAR absorbed photsynthetically active radiation
- p157 NDVI normalized difference vegetation index
- p159 DIMs Depth Integrated Models calculate ΣNPP
- p159 TIMs Time Integrated Models
- p159 WIMs Wavelength Integrated Models
- p159 WRMs Wavelength Resolved Models, subsurface irradiance
- p163 TIMs variability of depth dependent carbon fixation as a function of daily surface PAR
- p163 TIMs integrated into daily DIMs
p170 VGPM global NPP 59e15 gC/year
plate 7.1 Global annual net primary production - 500 gC/m²y on continental shelves, <200 elsewhere
p182 ref Widespread Iron Limitation of Phytoplankton in the South Pacific Ocean Michael J. Behrenfeld* and Zbigniew S. Kolber @Rutgers, Science 5 Feb 1999 p840
p374 ref78 1953 Carbon dioxide concentration and maximum quantum yield in photosynthesis Nature volume 171, pages 1106–1108 (1953)
p375 An effect of antibiotics produced by plankton algae E. Steemann Nielsen Nature 1955
