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EOTRACES: Characterizing nit opes in South Atlantic water es (40°S). Robyn Tuerena, Raja Ganeshram, Anthony Fallick, Andrew Tait, Julie Dougans, Malcolm Woodward. ford 10 th -11 th September 2012

UK GEOTRACES: Characterizing nitrate isotopes in South Atlantic water masses (40°S). UK GEOTRACES: Characterizing nitrate isotopes in South Atlantic water

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UK GEOTRACES: Characterizing nitrate isotopes in South Atlantic water masses (40°S).

Robyn Tuerena, Raja Ganeshram,Anthony Fallick, Andrew Tait, Julie Dougans, Malcolm Woodward.

Oxford 10th-11th September 2012

Marine Nitrogen cycle

• N Limits on biological productionSigman et al., 2000; Difiore et al.,2008

• Trace N fluxesBrandes and Devol, 2002; Codispoti et al., 2001

• Changing productivity patternsDuce et al., 2008; Falkowski et al., 1998

Characterizing nitrate isotopes in South Atlantic water masses (40°S)Robyn Tuerena, Raja Ganeshram, Anthony Fallick, Andrew Tait, Julie Dougans, Malcolm Woodward.

Study area

D357, RRS DiscoveryJC068, RRS James Cook

NADW

AAIW

AABW

SACW AgulhasBrazil

Characterizing nitrate isotopes in South Atlantic water masses (40°S)Robyn Tuerena, Raja Ganeshram, Anthony Fallick, Andrew Tait, Julie Dougans, Malcolm Woodward.

δ15N (‰ vs. air) = x 1000

Stable isotope biogeochemistry

Characterizing nitrate isotopes in South Atlantic water masses (40°S)Robyn Tuerena, Raja Ganeshram, Anthony Fallick, Andrew Tait, Julie Dougans, Malcolm Woodward.

Spatially and temporallyintegrated value!

Sigman et al., 2009

N2

PP

Nitrate isotope cycling

1.

3.

4.

2.

ε ~ 25 ‰

ε ~5 ‰

~ -1 ‰

ε ~≤ 3 ‰

1. N2 fixation2. Remineralization3. Nitrate utilization4. Denitrification

4. ε ~0 ‰

NO3-

5‰

Characterizing nitrate isotopes in South Atlantic water masses (40°S)Robyn Tuerena, Raja Ganeshram, Anthony Fallick, Andrew Tait, Julie Dougans, Malcolm Woodward.

SURFACE

Characterizing water masses

Nitrate utilization, indicator of productivity

Tracer for N2 fixation, denitrification andpartially utilized nitrate

Isotope fractionation

Spatial pattern of δ15NNO3 and δ18ONO3

DEEP

Characterizing nitrate isotopes in South Atlantic water masses (40°S)Robyn Tuerena, Raja Ganeshram, Anthony Fallick, Andrew Tait, Julie Dougans, Malcolm Woodward.

Denitrifier method (Sigman et al., 2001, Casciotti et al., 2002)

NO3- converted to N2O

Isotope ratio mass spectrometry

Methods

Characterizing nitrate isotopes in South Atlantic water masses (40°S)Robyn Tuerena, Raja Ganeshram, Anthony Fallick, Andrew Tait, Julie Dougans, Malcolm Woodward.

0 2 4 6 8 10 12 14

Dep

th

(m

)

-5000

-4000

-3000

-2000

-1000

0

d15N d18O

-2 0 2 4 6 8 10 12Y

Dat

aPer mil (‰)

-15 -10 -5 0 5 10 15

Deep water masses

Characterizing nitrate isotopes in South Atlantic water masses (40°S)Robyn Tuerena, Raja Ganeshram, Anthony Fallick, Andrew Tait, Julie Dougans, Malcolm Woodward.

Station 3 Station 6 Station 10

δ15N 0.2 ‰δ18O 0.5 ‰

Deep water masses

Characterizing nitrate isotopes in South Atlantic water masses (40°S)Robyn Tuerena, Raja Ganeshram, Anthony Fallick, Andrew Tait, Julie Dougans, Malcolm Woodward.

Deep water masses

NADW

AAIWAABW

AABWNADW

AAIW

AABW 4.9 ± 0.1 ‰NADW 4.5 ± 0.2 ‰ AAIW 5.4 ± 0.4 ‰

Characterizing nitrate isotopes in South Atlantic water masses (40°S)Robyn Tuerena, Raja Ganeshram, Anthony Fallick, Andrew Tait, Julie Dougans, Malcolm Woodward.

Deep water massesAAIWIncorporation of NO3

- that has been partially consumed in Antarctic surface waters

AABWFormed on shelf, Weddell sea and entrainment of CDW (~ 4.8 ‰, Sigman 1999)

NADWRelease of lighter N through sinking particles?Depleted source values?

Characterizing nitrate isotopes in South Atlantic water masses (40°S)Robyn Tuerena, Raja Ganeshram, Anthony Fallick, Andrew Tait, Julie Dougans, Malcolm Woodward.

Surface water masses

Nitrate utilization enriches δ15N up to 13 ‰ at surface

Characterizing nitrate isotopes in South Atlantic water masses (40°S)Robyn Tuerena, Raja Ganeshram, Anthony Fallick, Andrew Tait, Julie Dougans, Malcolm Woodward.

SAMW

Surface water masses

Characterizing nitrate isotopes in South Atlantic water masses (40°S)Robyn Tuerena, Raja Ganeshram, Anthony Fallick, Andrew Tait, Julie Dougans, Malcolm Woodward.

D357

Surface water massesMixing dilutes δ15N values:Agulhas 6-8 ‰SACW 5-7‰

Characterizing nitrate isotopes in South Atlantic water masses (40°S)Robyn Tuerena, Raja Ganeshram, Anthony Fallick, Andrew Tait, Julie Dougans, Malcolm Woodward.

Nitrate Utilization

12

71619

5 µM12 ‰

30 µM5 ‰

17.5 µM6 ‰

Characterizing nitrate isotopes in South Atlantic water masses (40°S)Robyn Tuerena, Raja Ganeshram, Anthony Fallick, Andrew Tait, Julie Dougans, Malcolm Woodward.

15Nnr

-12 -10 -8 -6 -4 -2 0 2

Dep

th (

m)

0

200

400

600

800

1000

1200

1400

Station 2Station 6

15Nnr

-8 -6 -4 -2 0 2D

epth

(m

)

0

200

400

600

800

1000

1200

1400

Station 16Station 19

Mixing

δ15Nnr: Indicates deviations from expected enrichment related to NO3

- concentrations

Agulhas

SACW

Characterizing nitrate isotopes in South Atlantic water masses (40°S)Robyn Tuerena, Raja Ganeshram, Anthony Fallick, Andrew Tait, Julie Dougans, Malcolm Woodward.

Characterizing nitrate isotopes in South Atlantic water masses (40°S)Robyn Tuerena, Raja Ganeshram, Anthony Fallick, Andrew Tait, Julie Dougans, Malcolm Woodward.

Surface water masses

Δ15,18 = (δ15N -δ15Nm) -(15ε/18ε)x(δ18O-δ18Om)Sigman et al., (2005)

Deviations from δ15N:δ18O stoichiometry

Conclusions DeepAAIW: partially utilized NO3

- in surface watersNADW: Lighter values may indicate sinking of newly fixed OM

SurfaceWater mass mixing dilutes δ15N enrichment in surface waters

Future workFinish analysis of surface and Western basin samples

Finish particulate analyses

Arctic and Southern Ocean samples

Characterizing nitrate isotopes in South Atlantic water masses (40°S)Robyn Tuerena, Raja Ganeshram, Anthony Fallick, Andrew Tait, Julie Dougans, Malcolm Woodward.

High resolution deep ocean transect

δ15N and δ18O measurements of NO3- give an

integrated signal of N cycling processes over space and time

δ13C and δ15N of particulates can further constrain N cycling

Collaborations

• Aerosol data - Rosie Chance and Alex Baker• Mixing fluxes• Biological productivity in surface waters

AcknowledgementsSample collectionUK GEOTRACES team, Crew of the RRS Discovery and RRS James Cook, Sue Reynolds, Amandine Sabadel

Method developmentSian Henley, Jan Kaiser, Laura Campisi, Karen Casciotti, Matt McIlvin

R.Schlitzer, Ocean Data View, http://www.awi-bremerhaven.de/GEO/ODV, 2012

d15 NO3 (per mil)4 6 8 10 12 14

De

pth

(m

)

0

500

1000

1500

2000

2500

PN (uM)0.0 0.2 0.4 0.6 0.8 1.0 1.2 1.4

d15 PN1.0 1.5 2.0 2.5 3.0 3.5 4.0 4.5 5.0

NO3 (uM)0 5 10 15 20 25 30 35 40

d15NPN (uM)d15PON Nitrate [uM/L]

Particulates

Below 500 m

Station 3δ15PN increases to ~ 5 ‰ below1000 m

δ15NO3- source waters ~ 6 ‰

Characterizing nitrate isotopes in South Atlantic water masses (40°S)Robyn Tuerena, Raja Ganeshram, Anthony Fallick, Andrew Tait, Julie Dougans, Malcolm Woodward.

2D Graph 3

d15N PN (per mil)

0 1 2 3 4 5 6

Dep

th (m

)

0

50

100

150

200

250

d13C (per mil)-24.5 -24.0 -23.5 -23.0 -22.5 -22.0 -21.5 -21.0 -20.5

POC (uM)0 1 2 3 4 5

d15PN d13POC POC (uM)

Particulates…Surface

Station 9 or 1.5Enrichment in C-13 and N-15 at POC max

Enrichment with depth

Characterizing nitrate isotopes in South Atlantic water masses (40°S)Robyn Tuerena, Raja Ganeshram, Anthony Fallick, Andrew Tait, Julie Dougans, Malcolm Woodward.

Particulates