Resolving the era of wet climates on Mars: Stratigraphy and paleohydrology of Aeolis Dorsa Edwin...
-
Upload
melanie-spindler -
Category
Documents
-
view
212 -
download
0
Transcript of Resolving the era of wet climates on Mars: Stratigraphy and paleohydrology of Aeolis Dorsa Edwin...
Resolving the era of wet climates on Mars:Stratigraphy and paleohydrology of Aeolis Dorsa
Edwin Kite (Princeton), Antoine Lucas (U. Paris), John Armstrong (Weber State University), Oded Aharonson (Weizmann), Michael Lamb (Caltech),
Alan Howard (U. Virginia)
Rationale: River-deposit dimensions constrain Early Mars hydrology, but stratigraphy is essential to constrain Mars climate evolution models Today, use measurements of Early Mars river-deposit dimensions versus stratigraphic elevation to:1) Constrain intermittency of wet
conditions2) Constrain climate models.
wavelength
width
River deposits record constraintssorely needed for Mars climate evolution models
Environmental scenarios for precipitation-fed runoff on Early Mars vary widely: e.g. Haberle et al. 2012, Kite et al. Icarus 2013, Mischna et al. 2013, Segura et al. 2012, Urata & Toon 2013, Wordsworth et al. 2013, Andrews-Hanna & Lewis 2011, Kite et al. Nature Geoscience 2014
102 mbar atmosphere needed to suppress evaporitic cooling Key geologic constraint – intermittency of wet conditions:
e.g. Burr et al. 2010, Palucis et al. 2014, Irwin et al. 2005, Hoke et al. 2011, Williams et al. 2011, Morgan et al. 2014, Grant & Wilson 2012, Fassett et al.2010, Hobley et al. 2014, Hauber et al. 2013.
Need error bars on geologic constraints to avert climate model overfitting
One-pass
Intermittent
Orbital forcingVolcanic forcingImpact-triggeredmetastable wetstatesImpact cataclysmThick early greenhouse
NAS
A/JP
L/M
SSS
Will
iam
s et
al.
Scie
nce
2013
Palu
cis
et a
l. JG
R 20
14
ESP_027807_1765PSP_008002_1750
F2
MSL rover
This Talk
)Elongitudela
titud
e
Thar
sis
Hellas
Early Mars water-availability model output (Kite et al., Icarus 2013a)
Zimbelman & Scheidt, Science 2012Kite et al., Nature Geosci. 2014
Aeolis Dorsa river deposits in global context:
Gale Aeolis Dorsaalluvial fans alluvial fans
Kite et al., in prep.geosci.uchicago.edu/~kite/stereo
1 cm
rhythmiterhythmite
Relatively young,post-Noachian (?)
0E 360E60S
60N
>108 yr time gap(embedded craters)
R-2
B20_
0175
48_1
739_
XI
R-1
How
ard
PNAS
200
9
400m
400m
e.g. Burr et al. 2009 & 2010 Kite et al. 2013 & in prep.
Stratigraphic context of river deposits suggests wet-dry alternations
Chan
nel d
epos
its
>3.2
km
stra
tigra
phic
thic
knes
s
rhythmitealluvial fans
rivers
>400 km E-W extent
Getting from stereopairs to stratigraphic logs
Errors: StratigraphicMeasurementOutcrop varianceMeasurement correlation
• Meander wavelengths tighten upwards• Small meanders rare/absent below 0m, common above 0m
(4-2
0) M
yr (
Kite
et a
l., Ic
arus
201
3b)
X transect 1(153.5ºE)transect 2(155ºE)transect 3(151ºE)
strat.error
1. Meander wavelengths (λ)
poor exposure
• Channel widths narrow upwards• Narrow channels rare/absent below 0m, common above 0m
strat.error
X transect 1(153.5ºE)transect 2(155ºE)transect 3(151ºE)
2. Channel widths (w)
(4
-20)
Myr
(Kite
et a
l., Ic
arus
201
3b)
poor exposure
# data points
Stra
tigra
phic
ele
vatio
n (m
)
0
Also: intermittency at 10m scale (correlatable basinwide using marker bed;Burr et al., 2010)
ESP_
0341
89_1
740
higher channel-depositproportion
lateral-accretion deposits
Logs show basin-wide discharge (Q) variability
Wavelength λ (m)
Width w (m)
Constraints on models of post-Noachian Mars climate evolution:
• Both short term intermittency and long-term intermittency.• A thicker atmosphere – and a way of removing it
Escape-to-space, or loss-to-ground (carbonate formation)?
Stochastic Mars climate evolution model:Uniform initial conditions: 3.5 Gya, 100 mbar
Liquid water availability model
(e.g. Kite et al. Icarus 2013)
Supply-limited carbonate
weathering in area of H2O(l)
update atmospheric pressure, solar luminosityescape to space scaled using ASPERA-3 data
scaled to UV flux of young Sunlike stars
Variable3.5 Gyr orbital
forcings(n = 100)
Armstrong et al. 2004
Ensemble approach
Obliquityeccentricity
Ls of perihelion
Obl
iqui
ty (°
) / P
atm
(mba
r)O
bliq
uity
(°) /
Pat
m
(mba
r)Late bursts of habitability on Mars-like planets: 1 example
atmosphericpressure
normalized areaof liquid-water
obliquity
Preliminary
long, globally-dryinterval
patchily,intermittently
wet
area of liquid w
ater
obliquity
atmospheric pressure
Metz et al. 2009, Edgar et al. 2014, Andrews-Hanna & Lewis 2011,
Head et al. 2009, Toon et al. 1980 …
Dry spells: Aeolian supply/ deflation?(e.g. Kocurek & Bridges, 2012)Wet spells: Cementation? (e.g. Milliken et al., 2014)
Obl
iqui
ty (°
) / P
atm
(mba
r)
Model Age (Gyr)
20 Myr
• Long dry intervals common– Laskar et al. Icarus 2004, Li &
Batygin ApJL 2014• Late-stage carbonate drawdown?
– 100x less carbonate than in Pollack et al. (1987), consistent with SAM δ13C
– Still need young, voluminous sedimentary reservoir for carbonate
longglobally-dry
interval
long, globally- dry interval
Preliminary
Late bursts of habitability on Mars-like planets: 3
different, equally likely scenarios
Obl
iqui
ty (°
) / P
atm
(mba
r)
wet
wet
Obl
iqui
ty (°
) / P
atm
(mba
r)
Obl
iqui
ty (°
) / P
atm
(mba
r)
Testing late-stage carbonate drawdown requires an extended Curiositytraverse
MAVEN
Test escape-to-space hypothesis
Upper Gale mound - above the sulfates: A representative sample
of the only geochemical reservoiradequate to explain the loss of habitability
via carbonate drawdown
Test loss-to-ground hypothesis:
Conclusions• Aeolis Dorsa records 1.5-2x reduction in river-deposit dimensions at or near
R-1/R-2 contact- Consistent with 3-4x reduction in peak discharge across the
contact.- 200m stratigraphy, (4-20) Myr total depositional interval
• Intermittency at multiple timescales (regional unconformities, river-deposit dimensions, marker beds).
• Constrains quantitative models linking sed. & strat. to climate evolution e.g. Kite et al., ‘Seasonal melting,’ Icarus 2013, Kite et al., ‘Growth and form …’, Geology
2013, Kite et al., ‘Low paleopressure …,’ Nature Geoscience 2014
With thanks to: Devon Burr, Kevin Lewis, Rebecca Williams, Robert Jacobsen, Lynn Carter, Bill Dietrich, Laura Kerber, Frederik Simons, Nicolas Mangold, Ross Irwin, Bill Dietrich, Alexandra Lefort, & Noah Finnegan for discussions, ideas, and inspiration.
More information: www.astro.princeton.edu/~ekite