7: Soil and Loess Flashcards
What is the main problem with using soils as global paleoclimate archives?
Not very well preserved usually
What are the two main special situations of high accumulation rates which can preserve soil in the paleoclimate record?
Floodplains, windblown dust (loess)
What is the primary location of paleoclimatic archives of soil, and why is this location timeless?
South of the furthest reach of glacial ice sheets, thus band across asia – glaciers do not reach to erode archive
Where is loess most often formed?
Periglacial regions – marginal to ice cover
When is loess most readily formed in periglacial conditions?
Cold periods
Besides periglacial sources of loess, what would be the other potential source?
Desert derived
What are the two factors of loess grains?
Usually silt sized, tend to be the same size – well sorted
What colour dust does goethite produce?
Orange
What colour dust does haematite produce?
Red
What mineral produces red dust?
Haematite
What mineral produces orangey dust?
Goethite
What are the most common magnetic minerals in loess?
Haematite/goethite, yet still not very common
What are the three main factors of loess source areas?
Extensive, Seasonally dry, Non-vegetated
Pedogenisis is a function of what 5 main things?
Time, Climate, Parent material, Organic activity, Relief
For the Chinese case study, soil formed from loess after how many years?
~100 years (quick for soil formation)