Lecture 5: Ancient impacts of people on climate change Flashcards

1
Q

Anthropocene: Human impacts push the Earth system (particularly ___ system) beyond its

A

climate system

natural range of variation

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2
Q

when did the anthropocene begin?

A

DEBATE

  • pre-industrial? (fire & hunting, origins of agriculture)
  • industrial ? (industrial revolution, nuclear age?)
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3
Q

holocene

A

last 10,000 years

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4
Q

Industrial effects are obvious (CO2 + Methane)

A

Huge ‘hockey stick’ curves showing increase following industrial revolution

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5
Q

earliest impacts of humans on the planet (4 points)

A

1) hunters and the megafaunal extinction
2) deglaciation & origins of agriculture
3) pre-industrial spread of agriculture
4) Climatic impacts of early agriculture

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6
Q

Hunters & megafaunal extinction

A
  • loss of wooly mammals etc
  • on every continent (Johnson 2009)
  • big animals more bias (more threatened)
  • small animals thriving in modern world
  • population sizes smaller in large animals, slower growth rates, breeding slower = more vulnerable to extinction
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7
Q

causes of megafaunal extinction?

A

debate, extinction correlated with human arrival

Johnson 2009

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8
Q

Agriculture: began? where? what does it allow?

A
  • 10-12 thousand years ago
  • began in multiple independent regions across the world
  • allows society to support high no. of people in one place
  • allows people to have diff jobs in society (farmers, not farmers, tax collectors)
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9
Q

modern agriculture

A
  • industrialised
  • support cities (importation)
  • free from need to go out and work and collect (hunter & gatherer)
  • tech innovations stem from agriculture (people have time on their hands)
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10
Q

hypothesis into why agriculture began?

A
  • DEBATABLE –> lots of hypothesis

- - i.e. local resource availability, population growth, tech innovation, dietary breadth etc

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11
Q

hunter gatherers ate …

A
    • were farming!
  • a broad spectrum of wild grains
  • Ohalo II, 10,000years BEFORE agriculture
  • tool use (weapons, grindstones)
  • wheat, barley & other things
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12
Q

transition to agriculture involved specialisation from a large pool of wild species

A

to a few crops

- wheat, barley, pulses etc

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13
Q

deglaciation probably allowed __ to begin

A

agriculture

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14
Q

Was agriculture impossible during the glacial?

A

YES,
-necessary tech & intellect:
low & unpredictable plant productivity made it impossible to specialise on a narrow range of crops
- picking a few crops = runs risk of high crop loss

  • so they go out, collect things in season, buffers you to environmental change
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15
Q

domestication of crops allowed

A
  • greater yields
    wild crops disperse their own seeds
  • domesticated dont
    – they rely on us, we do them
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16
Q

agriculture began & spread =

A
fertile crescent (iraq, iran, israel etc) and then spread through Europe and England in 5000 year ago 
- agriculture spread from where it began
17
Q

agriculture spread meant the __ of trees

A

deforestation

18
Q

from beginning agriculture (10,000) to now. Has tech innovations changed per capita land-use?

A
  • productivity of crops has improved,
  • shrinking per capita land-use
  • land change occurred further back in time
  • early anthropogenic view supports pre-industrial deforestation
19
Q

technological innovations in food production

A
  • hunter-gatherer management of landscapes by fire
  • food processing methods
  • cultivation of sown seeds in intensive gardens
  • agricultural economies (manuring, ploughing)
  • irrigation, multiple cropping, rotations, fertilisers,
  • industrial evolution
  • green revolution

Ellis et al 2013

20
Q

indirect climatic impacts of pre-industrial agriculture

A

comparison of CO2 & CH4 in current interglacial (holocene) and past (eemian)
- Now in holocene, increase in CO2 and CH4 (slightly more recently)

21
Q

reasons for CO2 and CH4 holocene interglacial levels

A
  • CH4 emissions from paddy rice & livestock
  • CO2 emission from deforestation for agriculture
  • RUDDIMAN 2013
  • – debatable though!
    • prior to 3000 years ago, only half CO2 was from deforestation
    • CH4 nature variation explains CH4 conc changes