Phytoplankton and primary production-2 Marine pelagic ecology BIO 4400 k

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Marine pelagic ecology BIO 4400

Phytoplankton and primary production-2

Bente Edvardsen 2009

Content

1.

Nutrients (N, P and Si)

2.

Growth

3.

Effects of temperature and salinity for growth

4.

Methods to measure primary production and algal biomass

Elemental composition of algal cells

99% of the living biomass is made up of C, H, O and N

Nutrients needed by algal cells

• Macronutrients : N, P, Si, S, K, Na

• Micronutrients: Fe, Zn, Cu, Mn, Se

• Vitamins: B

12

, biotin, thiamine

• In most marine environments algal growth is limited by N or P. The absolute levels are low, the demand high and concentrations very variable.

• But trace elements (e.g. Fe) may limit growth in some areas

HNLC

Parts of the Pacific and the Southern Ocean have areas with high nutrient and low chlorophyll levels where iron limit the growth

Nitrogen uptake in the algal cell

Uptake of [NO

3

] as a function of [NH

4

+ ]

Ammonium is preferred by phytoplankton at [NH4+] >1-2

µM

Enzyme nitrate reductase

( NR ) inhibited by [NH4+] >2

µM and is induced

Nitrogen cycle in the sea

Some N2 fixing cyanobacteria

Chemoautotrophic bacteria

After Paasche 2005

Anaerobic bacteria

Nitrogen cycle in the sea

Arrigo, K.R. 2005.

Nature 437: 349-355

Changes in [NO

3

] and [NH

4

+

Oslofjord (0-4 m depth)

] in the inner

From deep water from land

Paasche 2005

[NO

3

] and [NH

4

+ ] and particular N in the inner Oslofjord

(0-8 m depth)

Paasche 2005

short

Short and long cycle of N

Recycled production long

New production

New and recycled production ffactor = production based on NO

3

-

_______________________________ production based on NH

4

+ + NO

3

+ urea

Can be determined by a N 15 -method , but not well in coastal waters with supply of both NH

4

+ + NO

3

from land

Average f-factor is ~0.3 globally and ~0.5 in coastal waters

Phosphorus cycle

Paasche 2005

Phosphorus (P)

Phosphorus is rapidly remineralized to ortophosphate

Can be stored in cell

(polyphosphate, luxury uptake)

May limit production when fresh water influence is high

Paasche 2005

Elemental composition of algal cells

Silicate

Redfield ratio

• Albert Redfield noticed that elemental composition of plankton is strikingly similar to that in the deep ocean

• Nitrate:phosphate ratio 16:1 in the sea is controlled by the requirements of phytoplankton

• ..which subsequently release N and P to the environment at this ratio when remineralized

Redfield ratio

C:N:P : 106:16:1 = Redfield ratio

= average content in phytoplankton

Primary production:

106 CO

2

->

+ 16 NO

3

+ HPO

4

2+ 122H

2

O + 18 H +

C

106

H

263

O

110

N

16

P + 138 O

2

Nitrogen limitation in the sea

Mediterranean

NO 3+ / PO

4

3-

<16 in deep water support nitrogen limitation

Falkowski & Raven 1997.

Aquatic photosynthesis

Global balance between N

2 fixation and denitrification and anammox

Arrigo, K.R. 2005.

Nature 437: 349-355

Uptake rate (V) as a function of nutrient concentration (S)

Nutrient limitation

Michaelis-Menten

V = V max

.

S / (K s

+S)

No nutrient limitation

The affinity for a substrate increases with decreasing concentration

Photosynthesis and effect of temperature

Photosynthesis decrease with decreasing temperatures

The metabolic rate (enzymatic reactions) increase with temperature

From photosynthesis to growth

Respiration

• All organisms carry out respiration

• When oxygen is present :

6 O

2

+ C

6

H

12

O

6

-> 6CO

2

+ 6H

2

O + ATP

(energy)

• Anaerobic respiration :

• NO

3

, SO

4

2, CO

3

as electron donors or organic compounds

Growth curves- exponential growth

Most phytoplankton grow by two-division

Exponential growth

Population growth : nett growth rate (r) = growth rate (

μ

) – loss rate (

λ

) dN =

μ

N

0 dt

N = number of ind. in population

N t

= N

0 e

μ t

μ

= ln (N t

/N

0

) / t exponential growth

µ = specific growth rate (d -1 ) k = growth rate (divisions d -1 ) ln 2 = 0.69

k = 1.44

.

µ (or k= µ/ 0.69)

Maximal growth rate in response to temperature

Eppleys curve

• Eppleys curve: maximal growth rate at a given T

• Cold water species grow slowly

Growth rate as a function of salinity

Growth rate

(divisions/day)

Cell size and growth rate

Small cells growth faster than large

Growth rate and cell size diatome Diatomes: higher

Chl a: C -ratio

Dino: higher respiration, Ic dinoflagellate

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