intro to heathland Flashcards
devensian cold stage
115,000 ya
generally cold but has temp fluctuations
interstadial
embedded periods of temporarily warm conditions
stadial
embedded periods of cold conditions
chelford insterstadial
60,000 bp
rich vertebrate fauna
mean feb temp of -10
july mean temp 16
upton warren interstadial complex
42,000-38,000 bp
july mean of 16
species rich flora - thermophilous species, arctic alpines
dimlington stadial
maximum expansion of devensian ice
21,000 bp
windermere interstadial
rapid climatic warming after 13,000 bp
july mean temps 17-18
more continuous woodland
strong reduction in ice caps
loch lomond stadial
return to colder conditions for 1000years
july mean temps -10
ends with rapid temp rise
subdivision of the post glacial - periods:
pre boreal boreal atlantic sub boreal sub atlantic
pre boreal
sub arctic, godwin zone IV
boreal
warmer and dry, godwin zone V, VI
atlantic
warm and wet - oceanic, godwin zone V11a
sub boreal
warm and dry - continental, godwin zone V11b
sub atlantic
cool and wet - oceanic, VII
zones I-III
pre windermere
windermere interstadial
loch lomond stadial
zone IV
sub arctic climate
birch dominant
zone V
hazel expansion
birch dominant in NW despite warming
in south pine dominates
pollen evidence for thermophilous trees
zone VI
pine abundant everywhere
hazel still important
appearance of thermophilous trees in some quantity
zones VII
the forest maximum in britain rapid increase in alder oak relatively abundant lime reaches peak cooler and wetter
3 types of (semi) natural woodland
ancient
native
recent
native woodland
40% uk woodland native
mainly consists of native woodland
ancient woodland
continually wooded since 1600 AD
recent woodland
planted or established naturally
primary woodland
survived continually since ice age