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Clark & Aravena Tracing Tracing the the carbon carbon cycle cycle

Tracing the carbon cycle

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Tracing the carbon cycle. Fe: produit dans la dernière phase de fusion. CNO. Éléments > Fe: activation par neutrons. Éléments fissionable. Instable. Vostok – a 500 ka record of climate in an ice core. Expanded carbon cycling in the boreal, temperate and tropical forests. - PowerPoint PPT Presentation

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Page 1: Tracing the carbon cycle

Clark & Aravena

Tracing Tracing thethe

carbon carbon cyclecycle

Page 2: Tracing the carbon cycle

-2

0

2

4

6

8

10

12

0 10 20 30 40 50 60 70 80 90 100

log

ab

on

da

nce

(ato

me

s / 1

06 Si)

H

He

Li

Be

B

Fe

Ca

Sc

CO

UTh

PbPt

Ni

Tc Pm

N

NeSiS

Fe:produit dans la dernière phase

de fusionÉléments > Fe:activation par

neutrons

Instable

CNO

Éléments fissionable

Page 3: Tracing the carbon cycle
Page 4: Tracing the carbon cycle

Clark & Aravena

Page 5: Tracing the carbon cycle

Vostok – a 500 ka

record of climate inan ice core

Page 6: Tracing the carbon cycle

-500

-490

-480

-470

-460

-450

-440

-430

-420

-410

0 100000 200000 300000 400000

Years before present

Deu

teriu

m ‰

VS

MO

W

D T

°C

Page 7: Tracing the carbon cycle

-64

-62

-60

-58

-56

-54

-52

0 100000 200000 300000 400000

Years before present

d18 O

‰ V

SM

OW

-14

-12

-10

-8

-6

-4

-2

0

2

4

D T

°C

Page 8: Tracing the carbon cycle

160

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340

0 100000 200000 300000 400000

Years before present

Atm

osp

he

ric

CO

2 p

pm

v

-14

-12

-10

-8

-6

-4

-2

0

2

D T

°C

Page 9: Tracing the carbon cycle

Expanded carbon cycling in the boreal, temperate and tropical forests

160

180

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220

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260

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300

320

340

0 100000 200000 300000 400000

Years before present

Atm

osp

he

ric

CO

2 p

pm

v

-14

-12

-10

-8

-6

-4

-2

0

2

D T

°C

Page 10: Tracing the carbon cycle

CO2 from increased respiration in soils at higher T

Page 11: Tracing the carbon cycle
Page 12: Tracing the carbon cycle

150

200

250

300

350

0 5 10 15 20 25 30 35 40

Temperature

CO

2 p

pm

CO2 atmosphèrique en equilibre avec

des eaux marines CO2 degassing withincreased T

Page 13: Tracing the carbon cycle
Page 14: Tracing the carbon cycle

0.00001

0.0001

0.001

0.01

0.1

1

10

100

1000

10000

100000

1000000

Li Be B C N F Na Mg Al Si P S Cl K Ca Sc Ti V Cr Mn Fe Co Ni Cu Zn Ga Ge As Se Br Rb Sr

pp

m

Croûte

Rivières

Eau marine

Page 15: Tracing the carbon cycle

0.001

0.01

0.1

1

10

100

1000

10000

100000

1000000

10000000

100000000

1000000000

Li Be B C N F Na Mg Al Si P S Cl K Ca Sc Ti V Cr Mn Fe Co Ni Cu Zn Ga Ge As Se Br Rb Sr

Facteur d'enrichissement

Temps de résidence océanique

Page 16: Tracing the carbon cycle

Solanki et al., 2004, Nature 431, 1084

Anthropogenic COAnthropogenic CO22 is is increasing during a time of increasing during a time of maximum solar activity – maximum solar activity –

the highest in 10,000 the highest in 10,000 years.years.

250

270

290

310

330

350

370

390

CO

2 p

pm

Page 17: Tracing the carbon cycle

Tracing the Sulfur Cycle

Page 18: Tracing the carbon cycle

Sulfate Cycle in Groundwater

Page 19: Tracing the carbon cycle

34S composition of Geological Materials of Different Origin

Page 20: Tracing the carbon cycle