intro to heathland Flashcards

1
Q

devensian cold stage

A

115,000 ya

generally cold but has temp fluctuations

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2
Q

interstadial

A

embedded periods of temporarily warm conditions

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3
Q

stadial

A

embedded periods of cold conditions

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4
Q

chelford insterstadial

A

60,000 bp
rich vertebrate fauna
mean feb temp of -10
july mean temp 16

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5
Q

upton warren interstadial complex

A

42,000-38,000 bp
july mean of 16
species rich flora - thermophilous species, arctic alpines

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6
Q

dimlington stadial

A

maximum expansion of devensian ice

21,000 bp

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7
Q

windermere interstadial

A

rapid climatic warming after 13,000 bp
july mean temps 17-18
more continuous woodland
strong reduction in ice caps

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8
Q

loch lomond stadial

A

return to colder conditions for 1000years
july mean temps -10
ends with rapid temp rise

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9
Q

subdivision of the post glacial - periods:

A
pre boreal
boreal
atlantic 
sub boreal 
sub atlantic
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10
Q

pre boreal

A

sub arctic, godwin zone IV

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11
Q

boreal

A

warmer and dry, godwin zone V, VI

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12
Q

atlantic

A

warm and wet - oceanic, godwin zone V11a

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13
Q

sub boreal

A

warm and dry - continental, godwin zone V11b

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14
Q

sub atlantic

A

cool and wet - oceanic, VII

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15
Q

zones I-III

A

pre windermere
windermere interstadial
loch lomond stadial

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16
Q

zone IV

A

sub arctic climate

birch dominant

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17
Q

zone V

A

hazel expansion
birch dominant in NW despite warming
in south pine dominates
pollen evidence for thermophilous trees

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18
Q

zone VI

A

pine abundant everywhere
hazel still important
appearance of thermophilous trees in some quantity

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19
Q

zones VII

A
the forest maximum in britain
rapid increase in alder
oak relatively abundant
lime reaches peak
cooler and wetter
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20
Q

3 types of (semi) natural woodland

A

ancient
native
recent

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21
Q

native woodland

A

40% uk woodland native

mainly consists of native woodland

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22
Q

ancient woodland

A

continually wooded since 1600 AD

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23
Q

recent woodland

A

planted or established naturally

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24
Q

primary woodland

A

survived continually since ice age

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25
secondary woodland
planted or established since last ice age
26
why do communities occur
- environmental factors - community factors . competitive exclusion . co-existence through tolerance . co- existence through complementation . dependence
27
competitive exclusion
Gause's law - 2 species that compete for the exact same resources cannot stably coexist
28
structure
the spatial organisation of plant material within a community
29
structure includes 3 components
``` vertical structure (stratification) - grouped horizontal structure (pattern) species abundance ```
30
4 layers of woodland
``` ground layer field layer: - tall herbs and under shrubs - layer of low herbs shrub layer tree layer ```
31
horizontal structure - 3 distribution types
1. regular - overdispersed 2. random 3. clumped - underdispersed, most common type
32
pattern shown by a species is a product of:
morphology and growth characteristics seed dispersal mechanisms environmental heterogeneity species interactions
33
species abundance
the amount a species contributes to the vegetation
34
ways of measuring species abundance
density - number of individuals per unit area frequency - chance of finding a particular species in a sample of vegetation cover - generally expressed as a %
35
2 main approaches to survival
shade tolerance | complementation - growing when light intensity is relatively high
36
shade plants
large thin leaves leaves with singles palisade layer large surface area to weight ratio
37
shade tolerance - respiration
shade leaves may respire more slowly maintained at both high and light intensities have lower compensation points than sun leaves
38
phenology
the study of seasonal periodicity and timing of plant growth
39
vernal plant species
grow in spring
40
aestival species
grow in summer
41
autumnal species
grow in autumn
42
hiemal species
grow in winter
43
brown forest soil
mixing of organic and mineral matter no sharp boundaries between horizons less acidic - 5-7 pH
44
podzol soil
almost no mixing of mineral and organic matter by organisms sharp boundaries between horizons more acidic - <5.5 pH
45
heliophile
sun loving
46
pollen spectrum
distinctive decline in elm pollen
47
landnam clearances
small, temporary land clearances | for pasture or first cultivated then grazed
48
grassland adaptations
intercalary meristem adpressed growth low palatability ephemeral life history
49
intercalary meristem
meristems at internodes or stem regions between the places where leaves attach growing point not necessarily destroyed when grazed
50
adpressed growth
not easily grazed | leaves tightly adpressed to the ground
51
ephemeral life history
exploit bare patches of soil | grow during periods of limited grazing
52
calcifuge species
grow in acidic soils
53
calcicole species
in calcareous soils - containing calcium carbonate, chalky- limestone grassland = very species rich
54
rendzina soil
characteristic soil of limestone grasslands immature soil thin soil - due to purity of the bed rock high pH
55
heathland
typically needs low nutrient status and acidic soil | high conservation status
56
upland heath
up to montane zone - treeline 300-400m above sea level 75% worlds total
57
lowland heath
20% worlds total altitudes less than 300m 58,000 ha in uk
58
peatlands
largest carbon reserve in uk | 3 billion tonnes c
59
origin of heathland
in or after bronze age | dimbleby noted occurrence of brown earth underneath bronze age barrows yet surrounded by podzsol soil
60
broxa reforestation
possible to grow birch trees after 70 years small and contorted no real commercial value
61
important soil changes with planting
increase in earthworm numbers reversion of podsol soil to brown earth soil increase in pH