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Diatom silicification changes in a high pCO 2 environment: a mesocosm experiment

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Diatom silicification changes in a high pCO 2 environment: a mesocosm experiment . Kiely Shutt University of Washington Friday Harbor Laboratories Spring 2013. Diatoms: A Brief Overview. Major primary producers Most common phytoplankton Single celled, some are chain forming - PowerPoint PPT Presentation
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Diatom silicification changes in a high pCO 2 environment: a mesocosm experiment Kiely Shutt University of Washington Friday Harbor Laboratories Spring 2013
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Page 1: Diatom  silicification  changes in  a high pCO 2  environment: a  mesocosm  experiment

Diatom silicification changes in a high pCO2 environment: a mesocosm

experiment

Kiely ShuttUniversity of Washington

Friday Harbor LaboratoriesSpring 2013

Page 2: Diatom  silicification  changes in  a high pCO 2  environment: a  mesocosm  experiment

Diatoms: A Brief Overview

•Major primary producers•Most common phytoplankton•Single celled, some are chain forming•Primary controllers of silica cycling in the ocean•Radial or bilateral symmetry•Diatoms have a silica requirement in order to build frustules

Page 3: Diatom  silicification  changes in  a high pCO 2  environment: a  mesocosm  experiment

Silicification

Dissolved H4SiO4

Biogenic Silica SiO2

Upt

ake

Page 4: Diatom  silicification  changes in  a high pCO 2  environment: a  mesocosm  experiment

MethodsBiogenic Silica Filtering

Rapid filter method by Paasche (1980)Prepped and ran on spectrometer using

Strickland and Parsons (1968)

Biogenic Silica/Diatom Cell CalculationBiogenic Silica

Liter

( Phytoplankton Cells

Liter

# Diatoms# Cells )

Page 5: Diatom  silicification  changes in  a high pCO 2  environment: a  mesocosm  experiment

Research Questions

• Does biogenic silica differ between pCO2 treatments?

• What stressors affected biogenic silica and silica per diatom cell?– Micronutrient limitation? (Iron, Zinc)– Macronutrient limitation? (Nitrate, Silicate)– Microzooplankton grazing pressure?– Light limitation?

Page 6: Diatom  silicification  changes in  a high pCO 2  environment: a  mesocosm  experiment

F(2,32)= 5.250, p=0.072

0 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17 18 19 202

4

6

8

10

12

14Control

High

Dock

Drift

Time (Days)

Med

ian

Biog

enic

Sili

ca (µ

mol

L-1

)Biogenic silica through time

Page 7: Diatom  silicification  changes in  a high pCO 2  environment: a  mesocosm  experiment

0 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17 18 19 200

5

10

15

20

25

0

5

10

15

20

25

Time (Days)

Med

ian

Nitr

ate

(µm

ol L-

1)

Med

ian

Biog

enic

Sili

ca (µ

mol

L-1)

Page 8: Diatom  silicification  changes in  a high pCO 2  environment: a  mesocosm  experiment

0 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17 18 19 200

5

10

15

20

25

0

5

10

15

20

25

Control Ni-trate

High Nitrate

Drift Nitrate

Dock Nitrate

Control BioS

High BioS

Drift BioS

Dock BioS

Time (Days)

Med

ian

Nitr

ate

(µm

ol L-

1)

Med

ian

Biog

enic

Sili

ca (µ

mol

L-1)

Statistically strong negative correlations for all treatment groups: ρ= -.923, -.913, -.884

Nitrate and biogenic silica through time

Page 9: Diatom  silicification  changes in  a high pCO 2  environment: a  mesocosm  experiment

0 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17 18 19 200

5

10

15

20

25

30

35

40

45

50

0

5

10

15

20

25

30

35

40

45

50

Time (Days)

Med

ian

Silic

ate

(µm

ol L-

1)

Med

ian

Biog

enic

Sili

ca (µ

mol

L-1

)

Page 10: Diatom  silicification  changes in  a high pCO 2  environment: a  mesocosm  experiment

0 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17 18 19 200

5

10

15

20

25

30

35

40

45

50

0

5

10

15

20

25

30

35

40

45

50

Control BioS

High BioS

Drift BioS

Dock BioS

Control Sil-icate

High Silicate

Drift Silicate

Dock Silicate

Time (Days)

Med

ian

Silic

ate

(µm

ol L-

1)

Med

ian

Biog

enic

Sili

ca (µ

mol

L-1

)

Biogenic silica and dissolved silicate through time

Statistically strong negative correlations for all treatment groups: ρ= -.939, -.897, -.854

Page 11: Diatom  silicification  changes in  a high pCO 2  environment: a  mesocosm  experiment

Grazing pressure

Treatment Spearman ρ

Control .382

High -.054

In order to show a significant association between silicification and grazing, our ρ value would need to be closer to -1 or 1.

Previous studies found increase in diatom silicification under grazing pressure (Pondaven et al 2007)

Page 12: Diatom  silicification  changes in  a high pCO 2  environment: a  mesocosm  experiment

0 20 40 60 80 100 120 1400.5

1

1.5

2

2.5

3

3.5

4

4.5 Irradiance (inside mesocosms) µmol m-2 s-1

Dept

h (m

)

Page 13: Diatom  silicification  changes in  a high pCO 2  environment: a  mesocosm  experiment

0 20 40 60 80 100 120 1400.5

1

1.5

2

2.5

3

3.5

4

4.5

T0 ControlT0 HighT0 DriftT11 ControlT11 HighT11 Drift

Irradiance (inside mesocosms) µmol m-2 s-1

Dept

h (m

)

Page 14: Diatom  silicification  changes in  a high pCO 2  environment: a  mesocosm  experiment

PAR

(Eie

nste

ins m

-2 d

-1)

Adapted from (Martin-jézéquel et al 2000)

Page 15: Diatom  silicification  changes in  a high pCO 2  environment: a  mesocosm  experiment

F(2,30)= 4.200, p=0.122

2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17 18 19 200

20

40

60

80

100

120

140

160

180ControlHighDrift

Time (Days)

Pico

mol

e Si

lica

Cell

-1Picomole Silica Per Cell Through Time

Page 16: Diatom  silicification  changes in  a high pCO 2  environment: a  mesocosm  experiment

Research Questions - Revisited

• Does biogenic silica differ between pCO2 treatments? Nope!

• What stressors affected biogenic silica and silica per diatom cell?– Micronutrient limitation? (Iron, Zinc)– Macronutrient limitation? (Nitrate, Silicate)– Grazing pressure?– Light limitation? Could be!

Page 17: Diatom  silicification  changes in  a high pCO 2  environment: a  mesocosm  experiment

Conclusions

• No significant differences between pCO2 treatments for biogenic silica or silicification in diatoms

• Macronutrient limitation and grazing pressure were not affecting silicification in diatoms

• Light limitation likely to be the reason why we see the trends in silicification data as well as other unmeasured variables within our mesocosm system

Page 18: Diatom  silicification  changes in  a high pCO 2  environment: a  mesocosm  experiment

Acknowledgements• Jim Murray• Robin Kodner• Kelsey Gaessner • Evelyn Lessard• Mike Foy• Barbara Paul• Amanda Fay• Molly Roberts• Kitae Park• Peers: Phil Gravinese, Kelly Govenar, Jen

Apple, Andrew Turner, Daneil Newcomb, Natsuko Porcino, Amy Stephens

• University of Washington - Friday Harbor Labs

• Mary Gates Endowment• Henry and Holly Wednt Endowment• Educational Foundation of America• Herbs Tavern


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