time travelling to climates of the past

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Time travelling to climates of the past Mark Hodson, Emma Versteegh

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Presentation given with Mark at the Oxfordshire Science Festival

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Page 1: Time travelling to climates of the past

Time travelling to climates of the past Mark Hodson, Emma Versteegh

Page 2: Time travelling to climates of the past

Mark Hodson and Emma Versteegh, Time-travelling to climates of the past

How do we know that the climate is changing?

Page 3: Time travelling to climates of the past

Mark Hodson and Emma Versteegh, Time-travelling to climates of the past

How do we know that the climate is changing?

Page 4: Time travelling to climates of the past

Mark Hodson and Emma Versteegh, Time-travelling to climates of the past

How do we know that the climate is changing?

Page 5: Time travelling to climates of the past

Mark Hodson and Emma Versteegh, Time-travelling to climates of the past

How do we know that the climate is changing?

Page 6: Time travelling to climates of the past

Mark Hodson and Emma Versteegh, Time-travelling to climates of the past

How do we know what will happen in the future?

Page 7: Time travelling to climates of the past

Mark Hodson and Emma Versteegh, Time-travelling to climates of the past

How do we know what will happen in the future?

Page 8: Time travelling to climates of the past

Mark Hodson and Emma Versteegh, Time-travelling to climates of the past

How do we know what will happen in the future?

Page 9: Time travelling to climates of the past

Mark Hodson and Emma Versteegh, Time-travelling to climates of the past

How do we know what will happen in the future?

Page 10: Time travelling to climates of the past

Mark Hodson and Emma Versteegh, Time-travelling to climates of the past

How do we know what will happen in the future?

Page 11: Time travelling to climates of the past

Mark Hodson and Emma Versteegh, Time-travelling to climates of the past

How can we trust the models?

Present Day Cretaceous

Page 12: Time travelling to climates of the past

Mark Hodson and Emma Versteegh, Time-travelling to climates of the past

Looking into the past: calcium carbonate

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Page 13: Time travelling to climates of the past

Mark Hodson and Emma Versteegh, Time-travelling to climates of the past

Calcium carbonate

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Page 14: Time travelling to climates of the past

Mark Hodson and Emma Versteegh, Time-travelling to climates of the past

Calcium carbonate: stalagmites and stalactites

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Page 15: Time travelling to climates of the past

Mark Hodson and Emma Versteegh, Time-travelling to climates of the past

Calcium carbonate: stalagmites and stalactites

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Page 16: Time travelling to climates of the past

Mark Hodson and Emma Versteegh, Time-travelling to climates of the past

Calcium carbonate: shells

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Page 17: Time travelling to climates of the past

Mark Hodson and Emma Versteegh, Time-travelling to climates of the past

Calcium carbonate: shells

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Page 18: Time travelling to climates of the past

Mark Hodson and Emma Versteegh, Time-travelling to climates of the past

Earthworm calcium carbonate

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Image: Amy Stewart

Page 19: Time travelling to climates of the past

Mark Hodson and Emma Versteegh, Time-travelling to climates of the past

Earthworm calcium carbonate

Page 20: Time travelling to climates of the past

Mark Hodson and Emma Versteegh, Time-travelling to climates of the past

Earthworm calcium carbonate

Page 21: Time travelling to climates of the past

Mark Hodson and Emma Versteegh, Time-travelling to climates of the past

Earthworm calcium carbonate

Page 22: Time travelling to climates of the past

Mark Hodson and Emma Versteegh, Time-travelling to climates of the past

Earthworm calcium carbonate

Page 23: Time travelling to climates of the past

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

Page 24: Time travelling to climates of the past

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

Page 25: Time travelling to climates of the past

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

Page 26: Time travelling to climates of the past

Mark Hodson and Emma Versteegh, Time-travelling to climates of the past

Metal mobility

Page 27: Time travelling to climates of the past

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.

Page 28: Time travelling to climates of the past

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

Page 29: Time travelling to climates of the past

Mark Hodson and Emma Versteegh, Time-travelling to climates of the past

Production experiment

Page 30: Time travelling to climates of the past

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

Page 31: Time travelling to climates of the past

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

Page 32: Time travelling to climates of the past

Mark Hodson and Emma Versteegh, Time-travelling to climates of the past

Granules and climate change

I formed … years ago

and the temperature was…

Page 33: Time travelling to climates of the past

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

Page 34: Time travelling to climates of the past

Mark Hodson and Emma Versteegh, Time-travelling to climates of the past

Calcite chemistry

Page 35: Time travelling to climates of the past

Mark Hodson and Emma Versteegh, Time-travelling to climates of the past

Calcite chemistry

Page 36: Time travelling to climates of the past

Mark Hodson and Emma Versteegh, Time-travelling to climates of the past

U

Calcite chemistry

Page 37: Time travelling to climates of the past

Mark Hodson and Emma Versteegh, Time-travelling to climates of the past

Dating

234

230

92 U

90 Th

Page 38: Time travelling to climates of the past

Mark Hodson and Emma Versteegh, Time-travelling to climates of the past

Uranium-234 radioactive decay chain

Dating

Page 39: Time travelling to climates of the past

Mark Hodson and Emma Versteegh, Time-travelling to climates of the past

Dating

time

amou

nt

thorium

uranium / thorium

uranium

Page 40: Time travelling to climates of the past

Mark Hodson and Emma Versteegh, Time-travelling to climates of the past

Silbury Hill

Page 41: Time travelling to climates of the past

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

Page 42: Time travelling to climates of the past

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…

Page 43: Time travelling to climates of the past

Mark Hodson and Emma Versteegh, Time-travelling to climates of the past

Atomic structure

Page 44: Time travelling to climates of the past

Mark Hodson and Emma Versteegh, Time-travelling to climates of the past

Isotopes

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Page 45: Time travelling to climates of the past

Mark Hodson and Emma Versteegh, Time-travelling to climates of the past

Heavy water

Page 46: Time travelling to climates of the past

Mark Hodson and Emma Versteegh, Time-travelling to climates of the past

Forming calcite

calcium Ca2+

carbon dioxide CO2

water H2O

+ +

Page 47: Time travelling to climates of the past

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

Page 48: Time travelling to climates of the past

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

Page 49: Time travelling to climates of the past

Mark Hodson and Emma Versteegh, Time-travelling to climates of the past

Enrichment of heavy isotope decreases with temperature

49

enric

hmen

t in

heav

y ox

ygen

Page 50: Time travelling to climates of the past

Mark Hodson and Emma Versteegh, Time-travelling to climates of the past

Separating water molecules

Page 51: Time travelling to climates of the past

Mark Hodson and Emma Versteegh, Time-travelling to climates of the past

Separating water molecules

evaporation

Subtropics

Water vapour depleted in heavy water

Page 52: Time travelling to climates of the past

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

Page 53: Time travelling to climates of the past

Mark Hodson and Emma Versteegh, Time-travelling to climates of the past

Separating water molecules

condensation

Poles

Water vapour very depleted in heavy water

Page 54: Time travelling to climates of the past

Mark Hodson and Emma Versteegh, Time-travelling to climates of the past

Varying water composition

Page 55: Time travelling to climates of the past

Mark Hodson and Emma Versteegh, Time-travelling to climates of the past

Varying water composition

Page 56: Time travelling to climates of the past

Mark Hodson and Emma Versteegh, Time-travelling to climates of the past

Establishing a thermometer

3 temperatures

x 3 waters

x 2 soils

Page 57: Time travelling to climates of the past

Mark Hodson and Emma Versteegh, Time-travelling to climates of the past

Measuring isotopes

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granule

Oxygen isotope composition

Page 58: Time travelling to climates of the past

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

Page 59: Time travelling to climates of the past

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

Page 60: Time travelling to climates of the past

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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Page 61: Time travelling to climates of the past

Mark Hodson and Emma Versteegh, Time-travelling to climates of the past

A speleothem climate record

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← warmer - colder →

Page 62: Time travelling to climates of the past

Mark Hodson and Emma Versteegh, Time-travelling to climates of the past

A shell climate record

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Page 63: Time travelling to climates of the past

Mark Hodson and Emma Versteegh, Time-travelling to climates of the past

Applying the thermometer

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Page 64: Time travelling to climates of the past

Mark Hodson and Emma Versteegh, Time-travelling to climates of the past

Applying the thermometer

Page 65: Time travelling to climates of the past

Mark Hodson and Emma Versteegh, Time-travelling to climates of the past

Time travelling Boxgrove 500,000 years ago

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