ALL - seao2 · 2015. 3. 23. · sea ice open ocean coastal seas terrestrial biota atmosphere marine...
Transcript of ALL - seao2 · 2015. 3. 23. · sea ice open ocean coastal seas terrestrial biota atmosphere marine...
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ALL DEGLACIAL MODEL-DATA COMPARISONS ARE WRONG
SOME MAY BE USEFUL
Andy RidgwellUniversity of Bristol / University of California, Riverside
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0
Age (Ma)
-5.0
-4.0
-3.0
-2.0
-1.0
0.0
1.0
10 20 30 40 50 60
18
d0 (
‰)
Zachos et al. [2001, 2008]
Outline of talkQuantifying ‘time’ in
models and data
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0 50 100 150 200 2504000
4500
5000
5500
6000
6500
Age (kyr BP)
Depth
(m
)Outline of talk
Quantifying ‘time’ inmodels and data
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One (or more) of the following:
This is not relevant at all.
Too late – this was relevant 15 years ago.
There are potentially important implications for bulk carbonate and low sedimentation rate records. But no-one in their right mind uses these any more.
There are important implications for data-data (wiggle matching) and model-data analysis.
Meh
There are important questions raised of where in the sediments, and what fraction, of carbonate dissolves.
forget about itdrink beerbe happy
keep going
Quantifying ‘time’ inmodels and dataAnticipated outcome of talk
meh
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0
Age (Ma)
-5.0
-4.0
-3.0
-2.0
-1.0
0.0
1.0
10 20 30 40 50 60
18
d0 (
‰)
Zachos et al. [2001, 2008]
Quantifying ‘time’ inmodels and dataA deep time perspective on shallow time, time
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open oceansea ice coastal seas
terrestrialbiota
atmosphere
marine biota
sed
imen
ts
soils
land surface and rock weathering
icesheet
2D energy-moisture balance(no clouds, dynamics)
fully 3D (‘reducedphysics’)
ocean
surf
ace layer
bioturbatedzone of 1 cm
sedimentstack layers
partially-filledupper-most
layer
bio
turb
ati
on
al
mix
ing
non-bioturbated
zone ofburied layers
simplifiedthermo-dynamic
cGENIE
www.seao2.info/mycgenie.html
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-0.5
Age relative to the PETM (Ma)0.5 1.0 1.5-1.0 0.0-1.5-2.0
4.0
3.0
2.0
1.0
0.0
13
dC
(‰)
PE
TM
(ET
M1)
Age model artifacts -- lessons from deeper-time (1)Quantifying ‘time’ in
models and data
Consider: An event characterized by a (severe) reduction in carbonate preservation
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Age model artifacts -- lessons from deeper-time (1)Quantifying ‘time’ in
models and data
CaCO (wt%)3
13d C (‰)(CaCO3)
Depth
abo
ve r
efe
rence
leve
l (cm
)
0 50 100-70
-60
-40
-30
-20
-10
0
-50
0.0 4.52.25
?(model-data divide)
pCO (matm)2
low high
num
erica
l model t
ime-s
eries
or
ext
ern
al (
to o
cean)
reco
rd (
e.g
. ic
e c
ore
)
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‘lysocline’
‘carbonatecompensation
depth’
(reefs)
marine biota
oceanic crust
de
ep
-se
as
ed
ime
nts
surfaceoceanlayer
Ca
CO
ra
in f
lux
3
dis
so
lutio
n f
lux
de
trita
l ra
in f
lux
bioturbatedzone of
sedimentstack
layers
stack top
bio
turb
ati
on
al
mix
ing
non-bioturbated
zone ofsediment
stacklayers
Age model artifacts -- lessons from deeper-time (1)Quantifying ‘time’ in
models and data
current (model) time(to machine precision)
18d OI/Ca environmental
proxies
dissolution(of all tracers,including time,proportionally)
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Age model artifacts -- lessons from deeper-time (1)Quantifying ‘time’ in
models and data
CaCO (wt%)3
13d C (‰)(CaCO3)
Depth
abo
ve r
efe
rence
leve
l (cm
)
0 50 100-70
-60
-40
-30
-20
-10
0
-50
0.0 4.52.25 -85 0 0.0 2.01.0
pCO (matm)2
low high
num
erica
l model t
ime-s
eries
or
ext
ern
al (
to o
cean)
reco
rd (
e.g
. ic
e c
ore
)
Age (kyr) Sed rate-1(cm kyr )
-70
-60
-40
-30
-20
-10
0
-50
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Age model artifacts -- lessons from deeper-time (1)Quantifying ‘time’ in
models and data
CaCO (wt%)3
13d C (‰)(CaCO3)
0 50 100 0.0 4.52.25 0.0 2.01.0
pCO (matm)2
low high
num
erica
l model t
ime-s
eries
or
ext
ern
al (
to o
cean)
reco
rd (
e.g
. ic
e c
ore
)
Depth (cm) Sed rate-1(cm kyr )
Mean C
aC
O a
ge r
ela
tive to r
efe
rence
leve
l (ky
r)3
20
10
-10
-20
-30
-40
-50
0
-70
-60
-40
-30
-20
-10
0
-50
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Age model artifacts -- lessons from deeper-time (1)Quantifying ‘time’ in
models and data
CaCO (wt%)3
13d C (‰)(CaCO3)
0 50 100 0.0 4.52.25 0.0 2.01.0
pCO (matm)2
low high
Depth (cm) Sed rate-1(cm kyr )
Mean C
aC
O a
ge r
ela
tive to r
efe
rence
leve
l (ky
r)3
20
10
-10
-20
-30
-40
-50
0
20
10
-10
-20
-30
-40
-50
0
low high
13d C (‰)(pCO2)
-70
-60
-40
-30
-20
-10
0
-50
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CaCO (wt%)3
0.15
0.10
0.05
0.0
-0.05
20 40 60 80 1000
Mo
de
l-g
en
era
ted
syn
the
tic
se
dim
en
t c
ore
re
spo
nse
[R
idg
we
ll, 2
00
7]
54.75
54.80
54.85
54.90
54.95
55.00
CaCO (wt%)3
55.05
Age (M
a)
1500
m
3600 m
2600 m
20 40 60 80 1000
1266C1265A1263C/D
1262A1267B
Bu
lk s
ed
ime
nt
wt%
Ca
CO
co
nte
nt
[Za
ch
os
et
al.,
20
05
]3
Quantifying ‘time’ inmodels and dataAge model artifacts -- lessons from deeper-time (1)
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CaCO (wt%)3
0.15
0.10
0.05
0.0
-0.05
20 40 60 80 1000
Bu
lk s
ed
ime
nt
wt%
Ca
CO
co
nte
nt
[Za
ch
os
et
al.,
20
05
]3
54.75
54.80
54.85
54.90
54.95
55.00
CaCO (wt%)3
55.05
Age (M
a)
1500
m
3600 m
2600 m
20 40 60 80 1000
1266C1265A1263C/D
1262A1267B
CO perturbation22000 PgC
Mo
de
l-g
en
era
ted
syn
the
tic
se
dim
en
t c
ore
re
spo
nse
[R
idg
we
ll, 2
00
7]
Quantifying ‘time’ inmodels and dataAge model artifacts -- lessons from deeper-time (1)
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CaCO (wt%)3
0.15
0.10
0.05
0.0
-0.05
20 40 60 80 1000
54.75
54.80
54.85
54.90
54.95
55.00
CaCO (wt%)3
55.05
Age (M
a)
1500
m
3600 m
2600 m
20 40 60 80 1000
1266C1265A1263C/D
1262A1267B
Bu
lk s
ed
ime
nt
wt%
Ca
CO
co
nte
nt
[Za
ch
os
et
al.,
20
05
]3
4000 PgC CO perturbation2
Mo
de
l-g
en
era
ted
syn
the
tic
se
dim
en
t c
ore
re
spo
nse
[R
idg
we
ll, 2
00
7]
Quantifying ‘time’ inmodels and dataAge model artifacts -- lessons from deeper-time (1)
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CaCO (wt%)3
0.15
0.10
0.05
0.0
-0.05
20 40 60 80 1000
54.75
54.80
54.85
54.90
54.95
55.00
CaCO (wt%)3
55.05
Age (M
a)
1500
m
3600 m
2600 m
20 40 60 80 1000
1266C1265A1263C/D
1262A1267B
Bu
lk s
ed
ime
nt
wt%
Ca
CO
co
nte
nt
[Za
ch
os
et
al.,
20
05
]3
6000 PgC CO perturbation2
Mo
de
l-g
en
era
ted
syn
the
tic
se
dim
en
t c
ore
re
spo
nse
[R
idg
we
ll, 2
00
7]
Quantifying ‘time’ inmodels and dataAge model artifacts -- lessons from deeper-time (1)
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-0.5
Age relative to the PETM (Ma)0.5 1.0 1.5-1.0 0.0-1.5-2.0
4.0
3.0
2.0
1.0
0.0
13
dC
(‰)
ELM
O(E
TM
2)
Age model artifact lessons from deeper-time (2)Quantifying ‘time’ in
models and data
Consider: An event characterized by a (mild) reduction in carbonate preservation
@elm
o
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-0.5
Age relative to the PETM (Ma)0.5 1.0 1.5-1.0 0.0-1.5-2.0
4.0
3.0
2.0
1.0
0.0
13
dC
(‰)
ELM
O(E
TM
2)
0 50 100−20
0
20
40
60
80
100
wt%
Tim
e a
fte
r E
TM
2 o
nse
t (k
yr)
δ13C
-0.15 1.55
‰
Age model artifact lessons from deeper-time (2)Quantifying ‘time’ in
models and data
1262 (3500 m)
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Quantifying ‘time’ inmodels and dataAge model artifact lessons from deeper-time (2)
0.0 2.01.0
Depth (cm) Sed rate-1(cm kyr )
Mean C
aC
O a
ge r
ela
tive to r
efe
rence
leve
l (ky
r)3
20
10
-10
-20
-30
-40
-50
0
‘golden spike’(normalized conc)
model experiment starts,surface sediments ‘tagged’(instantaneous pulse of inert, conservative, numerical tracer)
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Quantifying ‘time’ inmodels and data
0.0 2.01.0
Depth (cm) Sed rate-1(cm kyr )
Mean C
aC
O a
ge r
ela
tive to r
efe
rence
leve
l (ky
r)3
20
10
-10
-20
-30
-40
-50
0
Age model artifact lessons from deeper-time (2)
‘golden spike’(normalized conc)
Depth above recorded ash maximum (cm)
020 10 -10 -2030
0.05
0.10
0.0
No
rma
lize
d a
sh c
on
cen
tra
tio
n
0.15
0.05
0.10
0.0
0.15-1
2.0-2.5 cm kyr
-10.5 cm kyr
RC17-126
E48-23
V29-39
V29-40
apparent offsetof event onset
apparent offsetof event onset
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0 50 100−20
0
20
40
60
80
100
wt%
Co
nst
an
t d
etr
ital f
lux
ag
e r
ela
tive
to
re
f le
ve
l (k
yr)
CaCO3
δ13C
2 3.25 4.5
‰
1250 2000−20
0
20
40
60
80
100
matm
pCO2 −6.5 −5.5 −4.5
δ13C
Model a
tmosp
heric
forc
ing
‰
1262 (3500 m)
Quantifying ‘time’ inmodels and dataAge model artifact lessons from deeper-time (2)
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0 50 100−20
0
20
40
60
80
100
wt%
Co
nst
an
t d
etr
ital f
lux
ag
e r
ela
tive
to
re
f le
ve
l (k
yr)
CaCO3
δ13C
2 3.25 4.5
‰
1262 (3500 m)
Quantifying ‘time’ inmodels and data‘Interface’ CaCO dissolution3
current (model) time(to machine precision)
18d OI/Ca environmental
proxies
1st, dissolution
2n
d,
bio
turb
ati
on
mix
ing
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Quantifying ‘time’ inmodels and data‘Homogeneous’ CaCO dissolution3
current (model) time(to machine precision)
18d OI/Ca environmental
proxies
1st,
bio
turb
ati
on
mix
ing
2nd, dissolution
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0 50 100−20
0
20
40
60
80
100
wt%
Co
nst
an
t d
etr
ital f
lux
ag
e r
ela
tive
to
re
f le
ve
l (k
yr)
CaCO3
δ13C
2 3.25 4.5
‰
1262 (3500 m)
Quantifying ‘time’ inmodels and data‘Homogeneous’ CaCO dissolution3
current (model) time(to machine precision)
18d OI/Ca environmental
proxies
1st,
bio
turb
ati
on
mix
ing
2nd, dissolution
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0
Age (Ma)
-5.0
-4.0
-3.0
-2.0
-1.0
0.0
1.0
10 20 30 40 50 60
18
d0 (
‰)
0.1
Ma
Shallow time, time (i.e. time in shallow time)Quantifying ‘time’ in
models and data
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Quantifying ‘time’ inmodels and dataShallow time, time (i.e. time in shallow time)
Farrell and Prell [1989]
60% CaCO3
?
mixing(bioturbation)
dissolution(peservation)
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Consider: Co-varying (glacial-interglacial) CaCO dissolution cycles and how 3
a (varying) stable isotope is recorded18Methodology: d O of planktic carbonate follows the LR04 stack, plus atmospheric pCO is 2
forced to follow the EPICA Dome C record, providing a varying preservation forcing on CaCO in marine sediments.3
Shallow time, time (i.e. time in shallow time)Quantifying ‘time’ in
models and data
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Quantifying ‘time’ inmodels and dataShallow time, time (i.e. time in shallow time)
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Consider: Co-varying (glacial-interglacial) CaCO dissolution cycles and how 3
a (varying) stable isotope is recorded18Methodology: d O of planktic carbonate follows the LR04 stack, plus atmospheric pCO is 2
forced to follow the EPICA Dome C record, providing a varying preservation forcing on CaCO in marine sediments.3
18Instead: d O of planktic carbonate follows SPECMAP while 500 PgC CO removed from 2
the atmosphere (to the terrestrial biosphere) across the deglacial transition (and then gradually added back again in a sawtooth shape).
Shallow time, time (i.e. time in shallow time)Quantifying ‘time’ in
models and data
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18color contours: d O in bulk CaCO3
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Shallow time, time (i.e. time in shallow time)Quantifying ‘time’ in
models and data
Implications
Once again, it matters ‘where’ CaCO dissolution occurs 3
(and what carbonate fraction) in accumulating sediments. Distortion of time-varying signals is likely minimized if a ‘homogeneous’ mode of dissolution dominates.
Use of multiple benthic individuals (even if single species) will avoid bulk sediment artifacts (other proxies will be differentially affected though), but give rise to an entertaining convolution of benthic foram population dynamics (driven by [O ] and Corg flux variability), with a 2
time-varying G-I environmental signal. (This would be an ‘interface’ like situation.)
Single foram analyses in which both age-scale and environmental proxy are simultaneously measured, is ideal.
18 14But e.g. d O would be adequate ( C not essential).
Modellers should learn some marine geology.
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One (or more) of the following:
This is not relevant at all.
Too late – this was relevant 15 years ago.
There are potentially important implications for bulk carbonate and low sedimentation rate records. But no-one in their right mind uses these any more.
There are important implications for data-data (wiggle matching) and model-data analysis.
There are important questions raised of where in the sediments, and what fraction, of carbonate dissolves.
Meh
forget about itdrink beerbe happy
keep going
Quantifying ‘time’ inmodels and data
meh
Outcome
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Answers to questionsQuantifying ‘time’ in
models and data