Lecture 2- Evolution of Australian Biomes Flashcards

1
Q

How does the Great Dividing Range affect the climate?

A

-much wetter on the east of it and drier in the west, more inland

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2
Q

What are the areas of plant species richness?

A

-the tropics, Nth Queensland

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3
Q

What are the areas of high plant species endemism?

A
  • tropics

- southwestern Australia is a hotspot

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4
Q

What are some examples of different habitat types across Australia?

A
  1. Rainforest
  2. Woodland
  3. Hammock grassland
  4. Tall shrubland
  5. Open Heath
  6. Tall open forest
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5
Q

What are the two parameters in how we classify plants?

A
  1. Height

2. Extent of canopy closure

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6
Q

What is the plant classification? (detail) up to a meter high

A

Tussocky or tufted grasses and graminoids

a) closure 70% is closed tussock grassland or closed sedgeland
b) closure 30-70% tussock grassland or sedgeland
c) closure 10-30% open tussock grassland

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7
Q

What is the plant classification? (detail) above 2 m, below 10m

A

Tall shrubs

a) 70% closure= closed shrub
b) 30-70% closure= open shrub
c) 10-30% closure= tall shrubland

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8
Q

What is the plant classification? (detail) 10-30m

A

Medium trees

a) 70% closure= closed forest
b) 30-70% closure= open forest
c) 10-30% closure= woodland

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9
Q

What is a closed forest also called?

A

Rainforest

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10
Q

What were the consequences of Australia drifting northwards during the Tertiary (Paleogene and Neogene)? (climate) (5)

A

Climate changed

  1. Warm, humid, rainforests initially widespread
  2. Circum-polar current: cooling of Antarctica
  3. Reduced wind-bearing rains over Australia and increased aridity from Oligocene (30my ago)
  4. Contraction of rainforest
  5. Evolution and expansion of more arid-adapted plants e.g. sclerophylls and animals adapted to them
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11
Q

What were the consequences of Australia drifting northwards during the Tertiary (Paleogene and Neogene)? (landforms changed) (5)

A
  1. Old land surface, little mountain building or volcanic activity
  2. Weathering during warm-wet periods leached nutrients from soils
  3. Soils became low in nutrients e.g. phosphorus
  4. Drier cooler periods increased wind erosion. Mobile dunes and inland lakes dried up and became salt plains
  5. Evolution further favoured arid-adapted flora and fauna
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12
Q

What were the consequences of Australia drifting northwards during the Tertiary (Paleogene and Neogene)? (fire) (5)

A
  1. Evidence from charcoal and pollen fossil record
  2. Infrequent but present in wetter periods
  3. Caused by lightning, volcanoes
  4. Increased frequency with aridity
  5. Rainforest contracted further sclerophylls fire-adapted
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13
Q

What were the Pleistocene ice ages and their effect on Australia?

A
  • World-wide fluctuating interglacial (warm) and glacial (cold) periods 2.5my to present
    1. Australia warm wet/cool dry periods, virtually no glaciation
    2. Mobilisation of sands and expansion of desert regions
    3. Changes in sea level= impact on dispersal
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14
Q

What is the history of human arrival to Australia?

A
  • number of immigrant groups (from Indonesia, China)
  • direct evidence: bones (Mungo man), tools, middens and paintings 40-50 000yr
  • indirect evidence: charcoal deposits 100 000yr?, due to fire stick farming (fire= charcoal left behind)
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15
Q

What happened in Australia during the last glacial period?

A
  • drier rainforest was replaced by fire tolerant vegetation (increased charcoal)
  • megafaunal extinctions (most between 35-15K years ago) due climate change? hunting? human use of fire?
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16
Q

What impact did human arrival have on Australian flora and fauna?

A

-increase in fire
-coincided a
with decrease in precipitation

17
Q

Why is there so much plant species richness in the tropics?

A

-due to the rainforest

18
Q

Why is there so much plant species endemism in the southwest of Australia?

A
  • long history of isolation due to marine incursions at times of higher sea levels
  • periods of high sea level 42-34, 27-21, 16-14 mya
  • limited deposits created soil edaphic barriers
  • isolation through climate due to lack of rain