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Complementary Constraints from
Carbon and Nitrogen Isotopes on
the LGM Ocean’s Biological Pump
Andreas Schmittner and Christopher Somes
College of Earth, Ocean, and Atmospheric Sciences
Oregon State University
δ13C
I’ll tell you
about
circulation δ15N
I’ll tell you
about
iron
fertilization Δ14C
I’ll tell you
about
ventilation
Funded by NSF’s Marine Geology and Geophysics Program
IPODS Workshop Aug. 27, 2016, Utrecht
Goals
• Explore effects of changes in physics (e.g.
circulation, sea ice) and biology (e.g. iron
fertilization) on LGM distributions of δ13C, δ15N
• Compare model solutions to reconstructions
• Was the LGM biological pump stronger?
Schmittner and Somes (2016) Paleoceanography, doi:10.1002/2015PA002905.
Detritus
DIC
PO4
NO3
O2
Photosynthesis
Fast Recycling
13C
Water Column
Denitrification
Sinking
15N
15N
13C
Grazing
Mortality
Remineralization
Excretion
CO2O2
13C
N-Fixation
N2δ15NN2=0
Benthic
Denitrification
(Fe)
εBD ! −4‰
εWCD ! −25‰
εP ! −5‰
εP
εP
εE = −6‰
εAS
CaCO3
δ 13
C ! 2‰
13C
δ 13
CDIC ! 2‰
Phytoplankton
15N
13C δ 13
C ! −20‰
Diazotrophs
15N
13C δ 13
C ! −12‰
δ 13
C ! −20‰
Zooplankton
15N
13C δ 13
C ! −20‰
14C
Decay
δ 13
CCO2 ! −6.5‰
δ 13
CDIC ! 0.5‰
DOM
15N
13C δ 13
C ! −20‰
εP ! −20‰
εNF ! −1‰
δ 15
NNO3 ! 9‰
δ 15
NNO3 ! 5.5‰
δ 15
N ! −1‰
δ 15
N ! 4‰
δ 15
N ! 7‰
δ 15
N ! 5‰
δ 15
N ! 6‰
MOBI Model of Ocean Biogeochemistry and Isotopes
Somes et al. (2013, 2015)
Schmittner et al. (2015)
Numerical Experiments
• Pre-industrial Control (piCtrl) μmax = 0.6 d-1
• 6 idealized LGM experiments
• same physics: PMIP3-like boundary conditions
(ice sheets, CO2), δ13CCO2 = -6.5‰
• different maximum phytoplankton growth rates
μmax = 0.6 - 1.2 d-1 to mimic iron fertilization
(LGM0.6, LGM0.7, … LGM1.2)
Simplifications
• No spatial differences of iron fertilization effects
on growth rates
• No changes in winds or tides
• No sea level effects on benthic denitrification
• No interactive sediments (global ALK = const,
DIC will be too low)
Results (Physics)
• ΔSAT = -4.3 K
• Sea ice cover increased by 70%
• AMOC weaker (11 Sv) and shallower than piCtrl
(17 Sv)
• Deep 14C-ages increased by 600 years
Annan and Hargreaves (2013)
Roche et al. (2012)
Sarnthein et al. (2013)
Skinner et al. (previous IPODS mtg)
briefly: not inconsistent with reconstructions
Global Mean Quantities
Global Mean Vertical Profiles (horizontally averaged)
DIC = Cpre +
Corg + CCaCO3
δ13CDIC =
δ13Cpre +
δ13Corg
︷Biological
Pump
Corg=RC:OAOU
“Physics”
ΔCorg = 280 Pg
“Iron Fertilization”
ΔCorg = 400 Pg
ΔCorg vs Δδ13C R=-0.89
δ13C is a proxy of ΔCorg
ΔCorg vs Δδ13C R=-0.97
“Physics”
shallower AMOC
increases vertical
gradient in Atlantic
“Iron Fertilization”
further
increases vertical
gradient in Atlantic
and decreases
δ13C in Indian &
Pacific
δ13C
Oxygen
Similar to Corg
“Physics”
increased O2 in thermocline,
smaller suboxic zones (green
lines), decreased O2 in deep
ocean
“Iron Fertilization”
decreases oxygen in lower
thermocline and deep
ocean, increases suboxic
zones
Huge suboxic zone in North
Pacific inconsistent with
reconstructions (Jaccard
and Galbraith, 2011)
Nitrogen Cycle
“Physics”
decreases water-
column
denitrification and N-
fixation, increases N
inventory
“Iron Fertilization”
decreases surface
nutrients, increases
WCD and NF,
decreases N
inventory
“Physics”
decreases δ15N
“Iron Fertilization”
increases δ15N
δ15N
Comparison to
Reconstructions
• δ15N reconstructions from Nitrogen Cycle in the
Ocean Past and Present (NICOPP) compilation
(Galbraith et al., 2013)
• δ13C reconstructions from Peterson et al. (2014)
R RMSE
0.33 2.1
0.34 1.8
0.21 2.9
0.45 1.3
0.21 2.4
0.21 3.2
R RMSE
R RMSE
0.75 1.140.63 1.48
R RMSE
0.78 0.770.78 0.76
σobs=0.52‰
Conclusions
• N and C isotopes provide complementary
constraints on the biological pump
• Models with weaker and shallower AMOC and
moderately increased iron fertilization fit
observations best
• ΔCorg ~ 500 - 700 Pg
δ13C
I’ll tell you
about
Corg
δ15N
I’ll tell you
about
iron
fertilization
Ongoing and Future Work
• Effects on CO2 (Samar Khatiwala)
• Iron and Circulation (Juan Muglia)
• LGM Nitrogen Cycle (Somes et al., in prep for
Frontiers in Marine Sciences)
• Early Deglaciation
Dank je !
🌷
Schmittner ipods talk Aug. 27, 2016

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Schmittner ipods talk Aug. 27, 2016

  • 1. Complementary Constraints from Carbon and Nitrogen Isotopes on the LGM Ocean’s Biological Pump Andreas Schmittner and Christopher Somes College of Earth, Ocean, and Atmospheric Sciences Oregon State University δ13C I’ll tell you about circulation δ15N I’ll tell you about iron fertilization Δ14C I’ll tell you about ventilation Funded by NSF’s Marine Geology and Geophysics Program IPODS Workshop Aug. 27, 2016, Utrecht
  • 2. Goals • Explore effects of changes in physics (e.g. circulation, sea ice) and biology (e.g. iron fertilization) on LGM distributions of δ13C, δ15N • Compare model solutions to reconstructions • Was the LGM biological pump stronger? Schmittner and Somes (2016) Paleoceanography, doi:10.1002/2015PA002905.
  • 3. Detritus DIC PO4 NO3 O2 Photosynthesis Fast Recycling 13C Water Column Denitrification Sinking 15N 15N 13C Grazing Mortality Remineralization Excretion CO2O2 13C N-Fixation N2δ15NN2=0 Benthic Denitrification (Fe) εBD ! −4‰ εWCD ! −25‰ εP ! −5‰ εP εP εE = −6‰ εAS CaCO3 δ 13 C ! 2‰ 13C δ 13 CDIC ! 2‰ Phytoplankton 15N 13C δ 13 C ! −20‰ Diazotrophs 15N 13C δ 13 C ! −12‰ δ 13 C ! −20‰ Zooplankton 15N 13C δ 13 C ! −20‰ 14C Decay δ 13 CCO2 ! −6.5‰ δ 13 CDIC ! 0.5‰ DOM 15N 13C δ 13 C ! −20‰ εP ! −20‰ εNF ! −1‰ δ 15 NNO3 ! 9‰ δ 15 NNO3 ! 5.5‰ δ 15 N ! −1‰ δ 15 N ! 4‰ δ 15 N ! 7‰ δ 15 N ! 5‰ δ 15 N ! 6‰ MOBI Model of Ocean Biogeochemistry and Isotopes Somes et al. (2013, 2015) Schmittner et al. (2015)
  • 4. Numerical Experiments • Pre-industrial Control (piCtrl) μmax = 0.6 d-1 • 6 idealized LGM experiments • same physics: PMIP3-like boundary conditions (ice sheets, CO2), δ13CCO2 = -6.5‰ • different maximum phytoplankton growth rates μmax = 0.6 - 1.2 d-1 to mimic iron fertilization (LGM0.6, LGM0.7, … LGM1.2)
  • 5. Simplifications • No spatial differences of iron fertilization effects on growth rates • No changes in winds or tides • No sea level effects on benthic denitrification • No interactive sediments (global ALK = const, DIC will be too low)
  • 6. Results (Physics) • ΔSAT = -4.3 K • Sea ice cover increased by 70% • AMOC weaker (11 Sv) and shallower than piCtrl (17 Sv) • Deep 14C-ages increased by 600 years Annan and Hargreaves (2013) Roche et al. (2012) Sarnthein et al. (2013) Skinner et al. (previous IPODS mtg) briefly: not inconsistent with reconstructions
  • 8. Global Mean Vertical Profiles (horizontally averaged)
  • 9. DIC = Cpre + Corg + CCaCO3 δ13CDIC = δ13Cpre + δ13Corg ︷Biological Pump Corg=RC:OAOU
  • 10. “Physics” ΔCorg = 280 Pg “Iron Fertilization” ΔCorg = 400 Pg ΔCorg vs Δδ13C R=-0.89 δ13C is a proxy of ΔCorg ΔCorg vs Δδ13C R=-0.97
  • 11. “Physics” shallower AMOC increases vertical gradient in Atlantic “Iron Fertilization” further increases vertical gradient in Atlantic and decreases δ13C in Indian & Pacific δ13C
  • 12. Oxygen Similar to Corg “Physics” increased O2 in thermocline, smaller suboxic zones (green lines), decreased O2 in deep ocean “Iron Fertilization” decreases oxygen in lower thermocline and deep ocean, increases suboxic zones Huge suboxic zone in North Pacific inconsistent with reconstructions (Jaccard and Galbraith, 2011)
  • 13. Nitrogen Cycle “Physics” decreases water- column denitrification and N- fixation, increases N inventory “Iron Fertilization” decreases surface nutrients, increases WCD and NF, decreases N inventory
  • 15. Comparison to Reconstructions • δ15N reconstructions from Nitrogen Cycle in the Ocean Past and Present (NICOPP) compilation (Galbraith et al., 2013) • δ13C reconstructions from Peterson et al. (2014)
  • 16. R RMSE 0.33 2.1 0.34 1.8 0.21 2.9 0.45 1.3 0.21 2.4 0.21 3.2 R RMSE
  • 17. R RMSE 0.75 1.140.63 1.48 R RMSE 0.78 0.770.78 0.76 σobs=0.52‰
  • 18.
  • 19.
  • 20.
  • 21. Conclusions • N and C isotopes provide complementary constraints on the biological pump • Models with weaker and shallower AMOC and moderately increased iron fertilization fit observations best • ΔCorg ~ 500 - 700 Pg δ13C I’ll tell you about Corg δ15N I’ll tell you about iron fertilization
  • 22. Ongoing and Future Work • Effects on CO2 (Samar Khatiwala) • Iron and Circulation (Juan Muglia) • LGM Nitrogen Cycle (Somes et al., in prep for Frontiers in Marine Sciences) • Early Deglaciation