Ecological vectors of carbon and biomineral export in the ... .fr

Sep 20, 2016 - Solubility pump. Timescale. 1 yr. 10 yr. 100 yr ... Solubility + circulation. Carbonate counter-pump ..... Fatty,acid,methyl, esters,(FAMEs). R3Si.
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Ecological vectors of carbon and biomineral export in the Southern Ocean

Mathieu Rembauville Supervized by Ian Salter and St´ephane Blain 20th September 2016 - Banyuls-sur-mer

Introduction - oceanic carbon pumps

Slow carbon cycle Million yr CO2

Carbonate rocks

Carbon fluxes from Le Qu´ er´ e et al. (2015)

1

Introduction - oceanic carbon pumps FastAcarbonAcycleA Century -GtACAyr-1) AtmosphericAgrowth

4.4AAA0.1

SlowAcarbonAcycle Million yr

LandAsink

3.0AAA0.8

Anthropogenic emissions

9.9AAA1 LandAuseA change

FossilAfuels, Aindustry

0.9AAA0.5

9.0AAA0.5

Ocean sink

CO2

2.6AAA0.5

Carbonate rocks

Carbon fluxes from Le Qu´ er´ e et al. (2015)

1

Introduction - oceanic carbon pumps Atmosphere

Timescale

CO2

CO2 DIC

1 yr

e Int

MLD

r ate ew iat n ed tio rm rma fo

10 yr

DIC ter wa n ep tio De rma fo

1000 m

100 yr > 1000 yr

DIC Seafloor

Geological Solubility pump

2

Introduction - oceanic carbon pumps Atmosphere

Timescale

CO2 Photosynthesis CO2 DIC

1 yr

r ate e+w iat n ed tio rm rma fo

Sinking+++active+transport+

e Int

MLD

POC Respiration

DIC r ate +w n ep tio De rma fo

1000+m

DIC Seafloor

100 yr > 1000 yr

POC Fossil+fuels

Solubility pump

10 yr

Geological

Soft tissue pump

2

Introduction - oceanic carbon pumps Atmosphere

Timescale

CO2 Photosynthesis CO2

r ate egw iat n ed tio rm rma fo

RDOC

+

LDOC

r ate gw n ep tio De rma fo

DIC Seafloor

POC Fossilgfuels

Solubility pump

Soft tissue pump

1 yr 10 yr

RDOC r ate gw n ep tio De rma fo

DIC 1000gm

+

Sinkingg+gactivegtransportg

e Int

MLD

POC Respiration

ter wa teg dia tion me a er form Int

DIC

100 yr > 1000 yr

RDOC Geological Microbial carbon pump

2

Introduction - oceanic carbon pumps Atmosphere

Photosynthesis

Precipitation 2HCO3-g+gCa2+

CaCO3g+gH2Og+ CO2

Dissolution

POC

r ate egw iat n ed tio rm rma fo

DIC

Carbonategrocks Carbonate pump

+

LDOC

POC Fossilgfuels

Solubility pump

Soft tissue pump

1 yr 10 yr

RDOC r ate gw n ep tio De rma fo

DIC r ate gw n ep tio De rma fo

PIC

RDOC

Sinkingg+gactivegtransportg

e Int

Sinking

1000gm

+

Respiration ter wa teg dia tion me a er form Int

DIC

PIC

MLD

Seafloor

Timescale

CO2

100 yr > 1000 yr

RDOC Geological Microbial carbon pump

2

Introduction - oceanic carbon pumps Atmosphere

Photosynthesis

Precipitation 2HCO3-g+gCa2+

CaCO3g+gH2Og+ CO2

Dissolution

POC

r ate egw iat n ed tio rm rma fo

DIC

Carbonategrocks Carbonate pump

+

LDOC

POC Fossilgfuels

Solubility pump

Soft tissue pump

1 yr 10 yr

RDOC r ate gw n ep tio De rma fo

DIC r ate gw n ep tio De rma fo

PIC

RDOC

Sinkingg+gactivegtransportg

e Int

Sinking

1000gm

+

Respiration ter wa teg dia tion me a er form Int

DIC

PIC

MLD

Seafloor

Timescale

CO2

100 yr > 1000 yr

RDOC Geological Microbial carbon pump

2

an

S

d G olu rub bi er, lity 20 + C 06 c Lé ar - L irc vy bo év ul et n y e at al. at ,2 e t a io 01 co l., n 20 3- u Le M 13 n M ge i illim te nd cr r an -p re ob et ia et um al. l al. p , 2 ca ,1 01 r 99 5 - bo 6 He ns L n é on vy pu et B et m al. io al. p , 2 lo ,2 01 g 01 2 - ic 3 La al ws pu et m al. p ,2 01 1

ien to

rm

Sa

Mixed layer carbon flux (Gt yr-1 )

Sink

15 10 5 0 5 10 15 Source

Introduction - oceanic carbon pumps Mixed layer MLD

Deep ocean

3

an

S

d G olu rub bi er, lity 20 + C 06 c Lé ar - L irc vy bo év ul et n y e at al. at ,2 e t a io 01 co l., n 20 3- u Le M 13 n M ge i illim te nd cr r an -p re ob et ia et um al. l al. p , 2 ca ,1 01 r 99 5 - bo 6 He ns L n é on vy pu et B et m al. io al. p , 2 lo ,2 01 g 01 2 - ic 3 La al ws pu et m al. p ,2 01 1

ien to

rm

Sa

Mixed layer carbon flux (Gt yr-1 )

Sink

15 10 5 0 5 10 15 Source

Introduction - oceanic carbon pumps Mixed layer MLD

Deep ocean

3

Introduction - biological pump

Legendre and Lef` evre (1989)

4

Introduction - biological pump

Legendre and Lef` evre (1989)

Ecosystem structure driving the [biological pump] process remains largely uncharacterized. - Guidi et al. (2016) 4

Introduction - export in the Southern Ocean

BP efficiency from NO3– field

5

Introduction - export in the Southern Ocean Westerlies

Katabatic

winds

PF

SAF

STF

BSi : PON Si(OH)4

: NO3-

Continental shelf

MidoceanOridge

Si(OH)4 : NO3-

ANTARCTICA

HighOlatitude

LowOlatitude

Redrawn from Marshall and Speer (2000) 5

Introduction - export in the Southern Ocean 0° 30°E

30°W

60°W

60°E

90°W

90°E

120°W

120°E

150°W

Sediment trap data POC/BSi/PIC Diatom Fecal pellets Foraminifers Pteropods Coccolithophores

150°E 180°

Hydrological fronts STF SAF PF

6

Introduction - export in the Southern Ocean

60°W

60°E

a

1.5

POC flux (mol m-2 yr-1 )

30°E

16

a

a

1.0

ab

12 8

b

Primary production (mol m-2 yr-1 )

2.0

0° 30°W

0.5

4

0.0

0

b 16 90°E

b

12 BSi:POC

90°W

8

a

4 0

120°E

150°W

Sediment trap data POC/BSi/PIC Diatom Fecal pellets Foraminifers Pteropods Coccolithophores

150°E 180°

Hydrological fronts STF SAF PF

2.0 PIC:POC

120°W

1.5

a

a c a

b

1.0 0.5 0.0

SAZ (n=9)

PFZ (n=16)

c

c

POOZ (n=16)

SIZ (n=47)

PP values from Moore and Abbott (2000)

6

Introduction - Objectives

How plankton export assemblage regulates : I - the magnitude and seasonality of POC export ? II - the BSi:POC and PIC:POC stoichiometry of export ? III - the lipid composition of export ?

7

Introduction - Objectives

80°W 30°S

60°W

40°W

20°W



20°E

40°E

60°E

80°E

1.4

40°S

Kerguelen

South Georgia PFZ

50°S

1.0 0.8

SAZ

0.6

AAZ

0.4

Chl ( g L-1 )

1.2

Crozet

0.2 0.0

60°S

M5

P3

KERFIX

A3

P2 M6

8

Introduction - Objectives

9

I - Magnitude and seasonality of POC export

I - Magnitude and seasonality of POC export

Rembauville et al., Biogeosciences, 2015 KEOPS2 - 290 m - October 2011 to September 2012 10

I - Magnitude and seasonality of POC export Imaging

Measurement

b

Specific.conversion

C.=.0.582.V0.811

a

a

C.=.0.039.V

b

a

b

C.=.0.036.V b

Diversity

a

Biovolume

Partitioned .POC.flux 11

POC flux (mmol m−2 d−1)

1.6

a)

CRS TRS Other diatoms Spherical faecal pellet Ovoid faecal pellet Cylindrical faecal pellet Ellipsoid faecal pellet Tabular faecal pellet

1.4 1.2 1 0.8 0.6 0.4 0.2 0

Oct

Nov 2011

Dec

Jan

Feb

Mar

Apr

May

Jun

Jul

Aug

Sep

Calculated POC flux (mmol m−2 d−1)

I - Magnitude and seasonality of POC export 2.5

b)

2 ρ = 0.84 p < 0.001 r² = 0.72

1.5

1

0.5

0

2012

0

0.5

1

1.5

Measured POC flux (mmol m−2 d−1)

Rembauville et al., Biogeosciences, 2015

12

POC flux (mmol m−2 d−1)

1.6

a)

CRS TRS Other diatoms Spherical faecal pellet Ovoid faecal pellet Cylindrical faecal pellet Ellipsoid faecal pellet Tabular faecal pellet

1.4 1.2 1 0.8 0.6 0.4 0.2 0

Oct

Nov 2011

Dec

Jan

Feb

Mar

Apr

May

Jun

Jul

Aug

Sep

Calculated POC flux (mmol m−2 d−1)

I - Magnitude and seasonality of POC export 2.5

b)

2 ρ = 0.84 p < 0.001 r² = 0.72

1.5

1

0.5

0

2012

0

0.5

1

1.5

Measured POC flux (mmol m−2 d−1)

Rembauville et al., Biogeosciences, 2015

12

I - Magnitude and seasonality of POC export

Auxospore (largest size) Vegetative cycle

Size reduction Sexual cycle

2n

2n Meiosis Zygote

n Gametes Fertilization

13

I - Magnitude and seasonality of POC export SporeRgermination (temperature,Rlight,Rdaylength) Auxospore (largestRsize) SporeRformation (nutrient,R lightRlimitation)

Mitosis

Vegetative cycle

SizeR reduction Resting cycle

Sexual cycle

2n

Physical, biological transport

MLD

2n Meiosis Zygote

n

RestingRspore

Gametes Fertilization

Seafloor

13

I - Magnitude and seasonality of POC export

Sediment CRS rel. ab. 50 % Spore dominant in sed. trap

Sediment data from Crosta et al. (1997) 14

I - Magnitude and seasonality of POC export

Sediment CRS rel. ab. 50 % Spore dominant in sed. trap

Rembauville et al., Deep Sea Research, 2016 Sediment data from Crosta et al. (1997) 14

II - BSi:POC and PIC:POC stoichiometry

II - BSi:POC and PIC:POC stoichiometry

Smetacek (1999)

F. kerguelensis Silica sinker BSi:POC

Wim van Egmond

Chaetoceros debilis Carbon sinker BSi:POC

15

II - BSi:POC and PIC:POC stoichiometry

Smetacek (1999)

Wim van Egmond

F. kerguelensis Silica sinker BSi:POC

Chaetoceros debilis Carbon sinker BSi:POC

How to link diversity with stoichiometry ?

15

II - BSi:POC and PIC:POC stoichiometry Micropal

Biological

16

II - BSi:POC and PIC:POC stoichiometry Biological technique: enumeration of full/empty cells

17

II - BSi:POC and PIC:POC stoichiometry Biological technique: enumeration of full/empty cells

Full > Empty

102

Empty > Full

Relative abundance (%)

CRS

101

F. kerguelensis

F. separanda/rhombica T. nitzschioides

Pseudo-nitzschia spp.

10

TRS

0

E. antarctica

T. lentiginosa

N. directa Thrix. antarctica

10-1

10-2

10-1

100 Empty:Full

101

102 17

II - BSi:POC and PIC:POC stoichiometry Micropaleontological technique: statistical relationship

18

II - BSi:POC and PIC:POC stoichiometry relationship a Micropaleontological technique: statistical b Fragilariopsis rhombica Fragilariopsis kerguelensis Thalassiosira gracilis Navicula directa Thalassionema nitzschioides Dactyliosolen antarcticus Pseudo-nitzshia heimii Pseudo-nitzchia lineola Thalassiosira oestrupii Chaetoceros (resting spore) Chaetoceros socialis 0.5 0.4 0.3 0.2 0.1 0.0 Bray-Curtis Distance

0.4

0.2 0.0 0.2 0.4 (BSi :POC)

0.6

Rembauville et al. (submitted) 18

II - BSi:POC and PIC:POC stoichiometry Silica vs. carbon sinker: validated with fluxes data ?

19

II - BSi:POC and PIC:POC stoichiometry Silica vs. carbon sinker: validated with fluxes data ?

19

II - BSi:POC and PIC:POC stoichiometry

2HCO3– + Ca2+ ←→ CaCO3 (PIC) + H2 O + CO2

20

II - BSi:POC and PIC:POC stoichiometry

2HCO3– + Ca2+ ←→ CaCO3 (PIC) + H2 O + CO2

CCpump =

CO2 ↑ PIC ↓ ∝ POC ↓ POC ↓

20

II - BSi:POC and PIC:POC stoichiometry

1/8th0wet0aliquot

Freeze-dried residue0 3700 m) Lins et al. (2015)

27

Conclusions

Conclusions I - Magnitude and seasonality of POC export • low POC flux in +Fe (