L9 Flashcards

1
Q

What is heathland and what is it dominated by?

A
  • Refers to a distinct type of vegetation dominated by ericoid dwarf shrubs
    • Normally dominated by Calluna vulgaris
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2
Q

What are the two types of heathland?

A

Upland heathland and lowland heaths

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3
Q

Upland heaths (moors)

A
  • 300-400m above sea level
  • up to montane zone (the tree-line)
  • 2-3 million hectares in the UK, which represents 75% of the global upland heath
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4
Q

Lowland heaths

A
  • altitudes less than 300m
  • 58,000 ha in the UK
  • 20% of the worlds total
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5
Q

Is heathland dry or wet?

A

Neither - it can be both

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6
Q

Eluviation definition

A

The transport of soil material from upper layers of soil to lower levels by downward precipitation of water across soil horizons

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7
Q

Podzol soils

A
  • characteristic of cool, wet climates
  • typical of boreal forests and heathland
  • intense eluviation of surface horizons
  • nutrients and bases leached from upper horizons
  • low nutrient, acidic soil
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8
Q

Podzol soil structure

A
  • Iron layer is characteristic
    • Iron oxides precipitates out and make it impermeable
    • Prevents water loss
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9
Q

Origins of heathland

A

Post glacial

  • Tundra-type vegetation included dwarf shrubs such as heather
  • Survived woodland development in glades, clearings, cliffs, above the treeline
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10
Q

Forest clearances

A

Occurred from 5000 y BP

-On poor soils … increased acidity and nutrient leaching
-good for heathers, gorse
-poor for for grassland / crops

-Heather pollen increases in the pollen record at this time

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11
Q

Bronze age onwards (3000 y BP)

A
  • Heathland established over significant areas
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12
Q

Why did heaths persist?

A

Poor soils, not converted to permanent agriculture - why don’t they become forest again?

Continued exploitation:
grazing / browsing (& fertilisation of fields)
heather thatch
turf fuel (turbary)
bracken: bedding, potash
gorse: fuel, fodder
sand & gravel

Coexisted with, and complementary to, agriculture

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