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Marine Botany Lesson 4 (continued from last week): The physical and chemical environment relevant to marine plant growth in the oceans…

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Presentation on theme: "Marine Botany Lesson 4 (continued from last week): The physical and chemical environment relevant to marine plant growth in the oceans…"— Presentation transcript:

1 Marine Botany Lesson 4 (continued from last week): The physical and chemical environment relevant to marine plant growth in the oceans…

2 Abiotic = Physical / Chemical Conditions affecting Plant Growth
Light – Irradiance Nutrients Temperature Salinity (ions, including CO2 >>> HCO3-) pH

3 Measuring Light (Ft. Candles) (Energy)
Photon Flux (mol photons m-2 s-1); [mol photons = Einstein (E)] Sunny day: ~ 2000 mmol photons m-2 s-1

4 Quantum Yield Absorption vs. Quantum Yield….

5 Blue-photon excitation level
Chlorophyll Heat Photosynthesis Fluorescence Ph Blue-photon excitation level Red-photon excitation level Ground state red orange yellow green blue Electron energy level

6 Measuring Light (Ft. Candles) (Energy)
Quantum E = h*c / λ Because the quantum yield for photosynthesis is equal for all wavelengths of PAR, we measure light as PHOTON FLUX (Ft. Candles) (Energy) Photon Flux (mol photons m-2 s-1); [mol photons = Einstein (E)] Sunny day: ~ 2000 mmol photons m-2 s-1

7 As light hits water surface: Reflectance Attenuation: Absorption
Irradiance Depth linear scale log scale As light hits water surface: Reflectance Attenuation: Absorption Scatter Absorption of low energy PAR (high wavelengths), Scatter of short wavelengths PAR (low wavelent Exponential attenuation!!! Attenuation

8 Light: Light is Reflected by the water surface, and Attenuated by the water column Reflection: 5-70% depending on Solar Angle and Roughness Attenuation: by Absorption and Scatter Absorption: Exponential, Selective [(Low-energy photons (red) are absorbed more than high-energy photons (blue)] Scatter: Short wavelengths (blue) are scattered more than long wavelengths (red)

9 Reflection: 5-70% depending on Solar Angle and Roughness
Clear Oceanic Water Light: Light is Reflected by the water surface, and Attenuated by the water column Reflection: 5-70% depending on Solar Angle and Roughness Attenuation: by Absorption and Scatter Absorption: Exponential, Selective (Red is absorbed more than Blue) Scatter: Short wavelengths (blue) are more scattered than Long wavelengths (red)

10

11 Light: Light is Reflected by the water surface, and Attenuated by the water column Reflection: 5-70% depending on Solar Angle and Roughness Attenuation: by Absorption and Scatter Absorption: Exponential, Selective (Red is absorbed more than Blue) Scatter: Short wavelengths (blue) are more scattered than Long wavelengths (red)

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13 Coastal Water

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15 Red algae and Cyanobacteria
Chlorophyll Chlorophyll Phycobilins

16 Red algae: Complementary chromatic adaptation (?)
Phycobilins

17 Zones according to LIGHT: Euphotic Disphotic Aphotic
Fig 2.5

18 1Compensation Irradiance (Ic) ~ 1% of full surface light
/ 2Compensation Depth = depth where 1% of surface light remains – depends on water clarity! Euphotic Zone ~1% 2 1 Photosynthesis and - Productivity +

19 Abiotic, Physical / Chemical Conditions
Light – Irradiance Nutrients Temperature Salinity pH

20 C:N = 6.6

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22 What determines nutrient uptake into plants?

23 How do we know if a nutrient is limiting?

24 Seawater Nitrogen* 0.05-1.0 mM (NO3-, NH4+) Phosphorous* 0.005-0.1 mM
(PO42-) Silica (Si) mM Iron (Fe) ?

25

26 Is it ethical? Is it leagal?

27 Abiotic, Physical / Chemical Conditions
Light – Irradiance Nutrients Temperature Salinity pH

28 Eurobiotic / Stenobiotic Eurothermic / Stenothermic
Controls rates of reactions Controls solubility of gasses Determines density Temperature “Isotherms” Fluctuations: <1o daily, 0-5o yearly in arctics / tropics, more in temp/subtr.

29 Temperature Usually 4oC at depths “Thermocline”

30 Abiotic, Physical / Chemical Conditions
Light – Irradiance Nutrients Temperature Salinity pH

31 measured in permill (o/oo, g/l), Usually ~ 35-40 o/oo (=3.5 - 4%)
Salinity measured in permill (o/oo, g/l), Usually ~ o/oo (= %) o/oo (or units) Open ocean Shallow coastal Estuary 0 – 30 brackish Semi-enclosed sea < 25 brackish Hypersaline sea > 40 Seawater ~0.5 M NaCl Salts mM NaCl 500 MgSO4 30 CaCl2 10 KCl 10 HCO3- ~2 mM

32 Salinity: Eurohaline / Stenohaline species
6 38 40 Salinity: Eurohaline / Stenohaline species

33 Usually 4oC at depths Temperature
“Halocline” = salinity boundary, can be saline on bottom water (usually) or top water (Med) “Thermocline”

34 Salinity can be toxic! Seawater ~0.5 M NaCl Salts mM NaCl 500 MgSO4 30
Open ocean Shallow coastal Estuary 0 – 30 brackish Semi-enclosed sea < 25 brackish Hypersaline sea > 40 Seawater ~0.5 M NaCl Salts mM NaCl 500 MgSO4 30 CaCl2 10 KCl 10 HCO3- ~2 mM

35 Na Cl K Internal Concentration of NaCl: ~ 80 mM (vs. 500 mM in seawater

36 Abiotic, Physical / Chemical Conditions
Light – Irradiance Nutrients Temperature Salinity pH? Carbon!

37 pH ~8.2 pH Seawater ~0.5 M NaCl Salts mM NaCl 500 MgSO4 30 CaCl2 10
KCl 10 HCO3- 2.2 pH ~8.2

38 350 ppm CO2 = 15 μM 10 μM CO2 CO2 + H2O > H2CO3 > HCO3- + H+ > CO32- + H+ pH 8.2: 10 μM μM μM Inorganic Carbon (Ci) ~2.1 mM HCO3-


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