Week 2 - Intro To Environmental Change Flashcards

Concept of reconstructing environmental change

1
Q

Why study past climate change?

A

Understanding the past helps us understand how the climate works - climate models, computer programs can predict how it’s going to change in the future

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2
Q

What are Direct Societal Benefits and Academic Benefits of studying past climate change?

A

Direct - understanding the climate will help us predict future climate change

Academic - how climate influences, such as human evolution and civilisations collapses

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3
Q

Name an example of Analogues for the future in terms of studying past climates.

A

How high did temperatures reach in the past the last time CO2 levels were this high?

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4
Q

How do we benchmark climate models?

A

Run climate models backwards to see if they accurately predict past climate change (and how that compares to our palaeolimate reconstructions)

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5
Q

Why do grain harvest records infer climate?

A

A certain type of climate gets more grain in a year

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6
Q

What are proxies?

A

Physical, chemical or biological records that respond to changes in temperature or precipitation- in order to ‘reconstruct’ past climate change

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7
Q

What is an archive and name an example.

A

Something that accumulates material over time

Sediments at the bottom of the lake, accumulation of sediment

Tree rings

Ice cores

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8
Q

In a tree, what is the archive and what is the proxy?

A

The tree is the archive and the ring is the proxy (how wide it is could tell us about the climate at the time)

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9
Q

Name 5 examples of archives (geological and biological material)

A

Ocean sediments

Ice cores

Lake sediments

Bog sediments

Trees

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10
Q

Name 4 examples of proxies

A

Stable isotopes (18O, 13C)

Pollen

Diatom

Tree ring width

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11
Q

What is paleolimnology?

A

The study of lake sediments

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12
Q

How can a closed lake (one that has no flow of water) help us reconstruct past environmental change?

A

The lake level goes up if it gets ‘wetter’ (less evaporation and/or more precipitation) and goes down if it gets ‘drier’ (more evaporation and/or less precipitation).

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13
Q

In lake sediments there is a light layer and dark layer forming every year. What are they?

A

Light layer is calcium carbonate

Dark layer is algae

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14
Q

Though they have the same number of protons, what does Oxygen-18 have that Oxygen-16 does not have?

A

2 more neutrons

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15
Q

In a lake, what does a change in the ratio of O18 and O16 indicate?

A

Changes in lake level - caused by how wet or dry the climate is

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16
Q

What are Peatlands?

A

A mixture of more or less decomposed plant (humus) material

Accumulates in a water saturated environment

Absence of oxygen (anaerobic)

17
Q

Why does material not completely decompose in peatlands?

A

Because of anaerobic conditions as a result of no oxygen

18
Q

What are the two types of peatlands?

A

Ombrotrophic peatlands (bogs)

Minerotrophic peatlands (fens)

19
Q

What are ombrotrophic peatlands?

A

Receive water solely/mostly from mineral-poor precipitation falling onto their surface

20
Q

Minerotrophic peatlands (fens)

A

Influenced by mineral-rich groundwater from outside their own limits. Can turn into bogs

21
Q

What can ombrotrophic peatlands tell us about past environmental changes?

A

As they get most of their moisture from precipitation, any change in the hydrology of the bog (how much water there is) can tell us about precipitation and temperature

22
Q

What is Troels-Smith classification when analysing peat cores?

A

Visually identify stratigraphic units/layers (dark, lighter)

Mark the boundaries on the section/core

Record depth and nature of upper boundaries (sharp or diffuse)

Describe the physical components of each peat unit

23
Q

What are the 4 different peat components?

A

Turfa herbacea (stringy)

Turfa bryophytica (spongy)

Turfa lignosa (woody remains)

Substantia humosa (highly decomposed)

24
Q

What are the 3 components of Munsell Colour?

A

Munsell Hue (red, green, blue)

Munsell Value (light, dark)

Munsell Chroma (bright, vibrant)

25
Q

What proxies can be found in peatlands?

A

Plant macrofossils
Plant microfossils
Charcoal
Testate amoebae

Humification
Inorganic elemental chemistry
Isotopes - oxygen, hydrogen, carbon
Organic geochemistry

26
Q

What are plant macrofossils and plant microfossils?

A

Macro - vegetative parts, seeds, fruits

Micro - pollen, spores

27
Q

What is Humification?

A

A process of formation of humic substances (organic matter that has reached maturity) decomposed from plant remains

Decomposition of organic material in soils & peats

28
Q

What can Sphagnum (moss) tell us about past climate conditions?

A

Some species prefer wetter conditions and other species prefer dry conditions

29
Q

What are the 2 layers of peat bogs?

A

Upper acrotelm layer

Lower catotelm layer

30
Q

Which peat layer is below the water table (waterlogged)?

A

Catotelm layer

31
Q

When is a peat bog considered flooded?

A

When it rises above the acrotelm layer

32
Q

How does the water table influence decomposition rate in bogs?

A

Sediment in the acrotelm layer is exposed to oxygen in the air, aiding decomposition

Sediment in the catotelm layer is saturated in water, preventing peat from breaking down further

33
Q

What can higher water tables in peat bogs tell us about past climate?

A

Higher water tables are caused by wetter and or cooler (less evaporation) climatic conditions, resulting in less decomposed peats

34
Q

What can lower water tables tell us about past climatic conditions?

A

That the climate was warmer and/or drier, causing the peat to break down more as it sits in the acrotelm for longer

35
Q

As peat breaks down, what acids are produced?

A

Humic (dark brown)

36
Q

The more decomposition there is, the more ____ ____ will be produced

A

Humic acids

37
Q

What can a spectrophotometer tell us about peat samples?

A

It measures changes in colour over time, the darker the material is, the more humic acids there are (more decomposition), the less light will pass through.