time travelling to climates of the past
DESCRIPTION
Presentation given with Mark at the Oxfordshire Science FestivalTRANSCRIPT
Time travelling to climates of the past Mark Hodson, Emma Versteegh
Mark Hodson and Emma Versteegh, Time-travelling to climates of the past
How do we know that the climate is changing?
Mark Hodson and Emma Versteegh, Time-travelling to climates of the past
How do we know that the climate is changing?
Mark Hodson and Emma Versteegh, Time-travelling to climates of the past
How do we know that the climate is changing?
Mark Hodson and Emma Versteegh, Time-travelling to climates of the past
How do we know that the climate is changing?
Mark Hodson and Emma Versteegh, Time-travelling to climates of the past
How do we know what will happen in the future?
Mark Hodson and Emma Versteegh, Time-travelling to climates of the past
How do we know what will happen in the future?
Mark Hodson and Emma Versteegh, Time-travelling to climates of the past
How do we know what will happen in the future?
Mark Hodson and Emma Versteegh, Time-travelling to climates of the past
How do we know what will happen in the future?
Mark Hodson and Emma Versteegh, Time-travelling to climates of the past
How do we know what will happen in the future?
Mark Hodson and Emma Versteegh, Time-travelling to climates of the past
How can we trust the models?
Present Day Cretaceous
Mark Hodson and Emma Versteegh, Time-travelling to climates of the past
Looking into the past: calcium carbonate
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Mark Hodson and Emma Versteegh, Time-travelling to climates of the past
Calcium carbonate
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Mark Hodson and Emma Versteegh, Time-travelling to climates of the past
Calcium carbonate: stalagmites and stalactites
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Mark Hodson and Emma Versteegh, Time-travelling to climates of the past
Calcium carbonate: stalagmites and stalactites
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Mark Hodson and Emma Versteegh, Time-travelling to climates of the past
Calcium carbonate: shells
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Mark Hodson and Emma Versteegh, Time-travelling to climates of the past
Calcium carbonate: shells
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Mark Hodson and Emma Versteegh, Time-travelling to climates of the past
Earthworm calcium carbonate
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Image: Amy Stewart
Mark Hodson and Emma Versteegh, Time-travelling to climates of the past
Earthworm calcium carbonate
Mark Hodson and Emma Versteegh, Time-travelling to climates of the past
Earthworm calcium carbonate
Mark Hodson and Emma Versteegh, Time-travelling to climates of the past
Earthworm calcium carbonate
Mark Hodson and Emma Versteegh, Time-travelling to climates of the past
Earthworm calcium carbonate
Mark Hodson and Emma Versteegh, Time-travelling to climates of the past
“It may be doubted whether there are many
other animals which have played so important a part in the history of the world,
as have these lowly organized creatures."
Darwin, 1881
Mark Hodson and Emma Versteegh, Time-travelling to climates of the past
…several small, or two or three larger, or a single very
large concretion of carbonate of lime as much as 1.5 mm in
diameter…they are often found in the gizzard, intestines and in
the castings of worms…
Darwin, 1881
Mark Hodson and Emma Versteegh, Time-travelling to climates of the past
What is the function of granules?
• Elimination of excess Ca • Neutralisation of gut pH • Fixing metabolic CO2
• Osmoregulation
Mark Hodson and Emma Versteegh, Time-travelling to climates of the past
Metal mobility
Mark Hodson and Emma Versteegh, Time-travelling to climates of the past
Material Science
(a) BSE image of a mixed calcite-ACC granule. (b) Corresponding EBSD orientation contrast map. Calcite generates good Kikuchi patterns (inset) and crystal orientations are colour coded. ACC lacks a Kikuchi pattern (inset), rendering it black in the EBSD map.
Mark Hodson and Emma Versteegh, Time-travelling to climates of the past
Production experiment
• 11 contrasting soils
• 1 earthworm per 300 g soil
• 27 days
Mark Hodson and Emma Versteegh, Time-travelling to climates of the past
Production experiment
Mark Hodson and Emma Versteegh, Time-travelling to climates of the past
Putting granules into perspective • Granule production =
65 x 103 – 5.7 x 106 tonnes CaCO3 a-1
9 – 840 Olympic swimming pools
Mark Hodson and Emma Versteegh, Time-travelling to climates of the past
Putting granules into perspective
• Granule production =
– 0.01 – 0.5 % UK C emissions
– Up to c. 5 % of C emitted from soils
– 0.04 – 3 % of C fixed by temperate grassland
– +100% Ca fixed by plants, released to soils from minerals,
in rainfall
Mark Hodson and Emma Versteegh, Time-travelling to climates of the past
Granules and climate change
I formed … years ago
and the temperature was…
Mark Hodson and Emma Versteegh, Time-travelling to climates of the past
Dating
You gotta check this out, Stuart. Vinnie’s over on the couch putting the moves on Zelda Schwartz – but he’s talkin’ to the wrong end
Mark Hodson and Emma Versteegh, Time-travelling to climates of the past
Calcite chemistry
Mark Hodson and Emma Versteegh, Time-travelling to climates of the past
Calcite chemistry
Mark Hodson and Emma Versteegh, Time-travelling to climates of the past
U
Calcite chemistry
Mark Hodson and Emma Versteegh, Time-travelling to climates of the past
Dating
234
230
92 U
90 Th
Mark Hodson and Emma Versteegh, Time-travelling to climates of the past
Uranium-234 radioactive decay chain
Dating
Mark Hodson and Emma Versteegh, Time-travelling to climates of the past
Dating
time
amou
nt
thorium
uranium / thorium
uranium
Mark Hodson and Emma Versteegh, Time-travelling to climates of the past
Silbury Hill
Mark Hodson and Emma Versteegh, Time-travelling to climates of the past
Silbury Hill
U-series isochron plot of multiple analyses of earthworm granules form Silbury hill. The earliest date for this is circa 4400 B.P. which is consistent with the U-series age for the carbonate granules, indicating they are contemporaneous with the soil formation.
230 Th/U age = 4.67 ± 0.44 ka MSWD = 63, probability = 0.000
230Th / 232Th
238U / 232Th
Mark Hodson and Emma Versteegh, Time-travelling to climates of the past
Granules and climate change
I formed 1000 years ago
and the temperature was…
Mark Hodson and Emma Versteegh, Time-travelling to climates of the past
Atomic structure
Mark Hodson and Emma Versteegh, Time-travelling to climates of the past
Isotopes
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Mark Hodson and Emma Versteegh, Time-travelling to climates of the past
Heavy water
Mark Hodson and Emma Versteegh, Time-travelling to climates of the past
Forming calcite
calcium Ca2+
carbon dioxide CO2
water H2O
+ +
Mark Hodson and Emma Versteegh, Time-travelling to climates of the past
Forming calcite at low temps
calcium Ca2+
carbon dioxide CO2
water H2O
+ +
light heavy
low temperature calcite enriched in heavy O
Mark Hodson and Emma Versteegh, Time-travelling to climates of the past
Forming calcite at high temps
calcium Ca2+
carbon dioxide CO2
water H2O
+ +
light heavy
higher temperature less heavy O enrichment
Mark Hodson and Emma Versteegh, Time-travelling to climates of the past
Enrichment of heavy isotope decreases with temperature
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enric
hmen
t in
heav
y ox
ygen
Mark Hodson and Emma Versteegh, Time-travelling to climates of the past
Separating water molecules
Mark Hodson and Emma Versteegh, Time-travelling to climates of the past
Separating water molecules
evaporation
Subtropics
Water vapour depleted in heavy water
Mark Hodson and Emma Versteegh, Time-travelling to climates of the past
Separating water molecules
condensation
Mid latitudes
Further depletion of heavy water in atmosphere Heavy water enriched water
Mark Hodson and Emma Versteegh, Time-travelling to climates of the past
Separating water molecules
condensation
Poles
Water vapour very depleted in heavy water
Mark Hodson and Emma Versteegh, Time-travelling to climates of the past
Varying water composition
Mark Hodson and Emma Versteegh, Time-travelling to climates of the past
Varying water composition
Mark Hodson and Emma Versteegh, Time-travelling to climates of the past
Establishing a thermometer
3 temperatures
x 3 waters
x 2 soils
Mark Hodson and Emma Versteegh, Time-travelling to climates of the past
Measuring isotopes
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granule
Oxygen isotope composition
Mark Hodson and Emma Versteegh, Time-travelling to climates of the past
Establishing a thermometer
58
enric
hmen
t in
heav
y ox
ygen
in c
alci
te
enrichment in heavy oxygen in water
Mark Hodson and Emma Versteegh, Time-travelling to climates of the past
Establishing a thermometer
temperature
enric
hmen
t in
heav
y ox
ygen
Earthworm calcite Stalagmites Mussels
Mark Hodson and Emma Versteegh, Time-travelling to climates of the past
Temperature equation
1000 ln α = 20.21 (103 T-1) - 38.58
α = (1000 + δ18OcVSMOW) / (1000 + δ18OwVSMOW)
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Mark Hodson and Emma Versteegh, Time-travelling to climates of the past
A speleothem climate record
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← warmer - colder →
Mark Hodson and Emma Versteegh, Time-travelling to climates of the past
A shell climate record
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Mark Hodson and Emma Versteegh, Time-travelling to climates of the past
Applying the thermometer
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Mark Hodson and Emma Versteegh, Time-travelling to climates of the past
Applying the thermometer
Mark Hodson and Emma Versteegh, Time-travelling to climates of the past
Time travelling Boxgrove 500,000 years ago
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