26
Carbon balance in a heterogeneous cutover bog in the Jura Mountains. Estelle Bortoluzzi, Daniel Epron, Daniel Gilbert, Alexandre Buttler

Carbon balance in a heterogeneous cutover bog in the Jura Mountains. Estelle Bortoluzzi, Daniel Epron, Daniel Gilbert, Alexandre Buttler

Embed Size (px)

Citation preview

Carbon balance in a heterogeneous cutover bog in the Jura Mountains.

Estelle Bortoluzzi,Daniel Epron,Daniel Gilbert, Alexandre Buttler

WP 02: Carbon sequestration by peatland vegetation

Objectives

1. Identify and compare the vegetation communities colonizing abandoned cut-over mire sites

2. Determine effects of key plant species used in peat restoration on carbon sequestration

3. Determine net primary production and biomass accumulation

4. Estimate net ecosystem productivity from seasonal determinations of photosynthesis and respiration in a transparent enclosure

WP 02: Carbon sequestration by peatland vegetation

Milestones:

M3: Site selection for survey and setting up of field experiment

M4: Survey of vegetation in cut-over sites and production measurements

M5: Rates of photosynthesis and respiration in cut-over sites (year1) and experiment (year 2-3)

M6: Biomass accumulation and growth biometry of keystone species in experiment (years 2-3)

WP 02: Carbon sequestration by peatland vegetation

Deliverables:

D5: Identification of key plant species successfully occupying abandoned sites and their potential for restoring peat accumulation

D6: Rates of carbon return from key species used in the restoration of cut-over sites

D7: Rates of C fixation on an area basis, evaluation of carbon sequestration through net primary production, estimation of hourly, daily and yearly net ecosystem productivity

=> Estelle thesis on June 15th

=> Manuscript under revision in New Phytologist

WP 02: Carbon sequestration by peatland vegetation

CO2

CH4CH4

PG - RA

CO2

CO2

RE

CO2CO2

Carbon sequestration

PPN

EEN

TOC

- RH - FCH4

Measurements

• A two year survey

• Open through flow transparent chamber (Ciras 1, PPSystems) for CO2 fluxes

• Closed darkened chambers for CH4 accumulation (micro-GC CP 4900, Varian)

• 11 collars on three vegetation types: bare peat, recent regeneration (Eriophorum) and advanced regeneration (Sphagnum)

• Environmental variables (air and peat temperature, global radiation and photosynthetic photon flux density, rainfall, water table level …)

•Biotic variables (Leaf Area Index, bryophyte density, dessication index) => Vegetation Index (VI) (0 to 1):

BImaxIFmax

DImaxDI

*BIIF

VI

Ecosystem respiration

0

2

4

6

8

10

0 90 180 270 360 450 540 630 720

Bare PeatRecentAdvanced

Days of years 2004 and 2005

RE (µmolCO2 m-2 s-1)

Air temperature, main determinant of RE

b

minrèf

minAE

TT

TT*R

TA (°C)

Bare peatRecent R.

Advanced R.

RE (µmolCO2 m-2 s-1)

Residuals of RE related to water table on bare peat

b

TT

TT*c

WT

WT*aR

minrèf

minA

rèfE

Bare Peat

WT (level of water table) (m)

Residuals of RE (µmolCO2 m-2 s-1)

Residuals of RE related to vegetation index

bed

minrèf

minA

rèfE

TT

TT*VI*

WT

WT*R

Residuals of RE (µmolCO2 m-2 s-1)

RecentAdvanced

VI (relative unit)

Predicted RE

RE predicted (µmolCO2 m-2 s-1)

Bare peatRecentAdvanced

RE measured (µmolCO2 m-2 s-1)

Net ecosystem exchange under saturating irradiance

-2

0

2

4

6

8

10

0 90 180 270 360 450 540 630 720Days of years 2004 and 2005

EENsat (µmolCO2 m-2 s-1)

RecentAdvanced

Gross photosynthesis under saturating irradiance

0

2

4

6

8

10

12

14

0 90 180 270 360 450 540 630 720

PBsat(µmol CO2 m-2 s-1)

RecentAdvanced

Days of years 2004 and 2005

PBsat = EENsat + RE

Air temperature, main determinant of PBsat

h

gA

Bsat

T

e*P

2

TA (°C)

PBsat(µmol CO2 m-2 s-1)

RecentAdvanced

Residuals of PBsat related to vegetation index

h

g

f

A

Bsat

T

e*VI*P

2

VI (relative unit)

RecentAdvanced

Residual of PBsat(µmolCO2 m-2 s-1)

Predicted EENsat

bedh

g

f

minrèf

minA

rèf

A

NsatTT

TT*VI*

WT

WT*

T

e*VI*EE

2

RecentAdvanced

EENsat measured (µmolCO2 m-2 s-1)

EENsat predicted (µmolCO2 m-2 s-1)

Light response curves of EEN

-6

-4

-2

0

2

4

6

8

0 500 1000 1500 2000

PPFD (µmol/m2/s)

EEN (µmolCO2 m-2 s-1)

Advanced collar 5,

j596

EBsat

BsatN R

PPFD*P

P*PPFD*EE

i

i

Predicted EEN

EEN predicted (µmolCO2 m-2 s-1)

EEN measured (µmolCO2 m-2 s-1)

RécentAdvanced

CH4 efflux

0

10

20

30

40

50

60

70

0 90 180 270 360 450 540 630 720Days of years 2004 and 2005

Bare peatRecent Advanced

FCH4 (nmole m-2 s-1)

CH4 efflux related to water table on bare peat

0

1

2

3

4

5

6

-0.15 -0.1 -0.05 0

FCH4 (nmol m-2 s-1)

WT (m )

Bare peat

WT*F 4CH j

CH4 efflux related to leaf area index of vasculars

0

20

40

60

80

0 0.2 0.4 0.6 0.8 1

FCH4 (nmol m-2 s-1)

LAI (m2 m-2 )

RecentAdvanced

IF*F 4CH k

Simulation:Knowing:

1. Half a hour global radiation and it conversion factor to photon flux density

2. Half a hour air and peat temperature

3. Seasonal variation of water table

4. Seasonal variation of leaf area index, bryophyte density and moss dessication index

=> Rates of net ecosystem productivity and methane efflux can be estimated at hourly, daily and yearly on an area basis and use to evaluate of carbon sequestration

Daily fluxes

-4

-3

-2

-1

0

1

2

3

4

5

6

0 90 180 270 360 450 540 630 720

FCO2 ( gC m-2 d-1)

Days of years 2004 and 2005

PB

RE

Advanced PB and RE

Advanced EN

Bare peat EEN

Recent PB and RE

Recent EN

Annual carbon balance (gC m-2 y-1)

2004 Bare peat Recent Advanced

PB 0.23 197 ~ 306 284 ~ 474

RE -22 -121~ -207 -186 ~ -297

FCH4 -0.4 -1.5 ~ -2.8 -0.7 ~ -2.3

Bilan -22 67 ~ 118 93 ~ 175

2005 Bare peat Recent Advanced

PB 279 ~ 379 359 ~ 525

RE -19 ~ -31 -199 ~ -214 -233 ~ -340

FCH4 -0.2 ~ -0.6 -1.8 ~ -3.9 -0.5 ~ -2.7

Bilan -19 ~ -32 78 ~ 166 122 ~ 183

Conclusions :

1. Bare peat is a weak carbon source and vegetated areas are strong carbon sinks

2. Net carbon exchange slightly higher for advanced than for recent regeneration

3. High variability among collars within a given stage of regeneration

4. Higher sensitivity to summer drought in Sphagnum covered plots (advanced regeneration)

5. Higher methane efflux in vascular covered plots ( recent regeneration)

Perspective : Site comparison, meta analysis …

Auteurs Country Type Method C balance (gC m-2 y-1)

Aurela et al., (2004) Finland Minerotrophic Eddy flux 22

Alm et al., (1997) Finland Ombrotrophic Chamber 73

Lafleur et al., (2001) Canada Ombrotrophic Eddy flux 68

Lafleur et al., (2003) Canada Ombrotrophic Eddy flux 71

Lafleur et al., (2003) Canada Ombrotrophic Eddy flux 9

Alm et al., (1999) Finland Ombrotrophic, very dry year

Chamber -90

Waddington et al., (2002) Quebec Ombrotrophic, after cutting

Chamber -88 ~ -112

This study Le Russey

Bare peat

Recent

Advanced

Chambers

-19 ~ -32

67 ~ 166

93 ~ 183