Chapter 6 Flashcards
To asses previous enviromental conditions
look at them globally
Sediment of ocean floors accumulates
very slowly
Can trace changes in enviroment through time by studying
o Cores taken from the sea bed
o Fluctuations in the species
Morphology of single species through the sequence
Oxygen isotope technique
Cores come from stratified sheets of ice where the oxygen isotopic composition gives a guide to climate oscillations
Isostatic uplift/tectonic movement
the weight of ice is removed as the temp rise at the end of the ice age
WHY is the height of a raised beach above the present shoreline not always a straightforward indication of the former sea level height
o The land has been raised up through isostatic uplift
Raised beaches
- Location can be an indicator of earlier coastlines
Raised Beaches stratigraphy rather than vertical
can occur in horizontal stratigraphy rather than vertical
Coral reefs
Provides the position of previous shorelines and their organisms give info on local marine environment
Geoarchaeology
Area of study that uses methods and concepts of earth science to examine processes of earth formation and soil/sediment patterns
geoarchaeology aims
achieve the fullest possible reconstruction of the local area and set into the context of the region
Reconstruct glaciated landscapes is done through
varves, rivers and caves
VARVES
- Receive annual layers of sediment deposited after the spring thaw
Thick layers in varves
warm years with increased glacial melt
Thin layers in varves
cold conditions with less glacial melt
factors that affect varve readings
lakes that are
too shallow
have sediments that are easily disturbed
Form varves from other factors, violent storms
river show rapid change through
Erosion
Deposition of sediments
why are rivers important
often human occupation is close to a river and provided crucial rise of irrigation agriculture and urban civilization
Limestone caves
important because it can conserve a wide range of evidence about humans and the enviroment
The growth of tree rings varies with the climate
More moisture available = wider the annual rings
Growth was slow = which implies dense local forest cover
Growth was fast = which implies light forest cover
can record sudden and dramatic shocks to the climate
Tree rings
Sediments
the global term for material deposited on the earth’s surface
soils
the life-supporting, biologically and physically weathered upper layers of those sediments
Geomorphology
study of the form and development of the landscape
Sedimentology
the physical and chemical properties of sedimentary rocks and the processes involved in their formation
Two aspects combine to provide a detailed analysis of the composition and texture of sediments
o Petrography - detailed description of rock
o Granulometry - measurement of mineral rocks
Petrography
detailed description of rock
Granulometry
measurement of mineral rocks
Soil micromorphology
use of microscopic techniques to study the nature and organization of the components of soil
Karl Butzer
Distinguished three groups of cultural deposits
PRIMARY CULTURAL DEPOSIT
Those that accumulate on the surface from human activity
SECONDARY CULTURAL DEPOSIT
Primary deposits that have undergone modification
examples of secondary cultural deposit
Physical displacement
Change of use of the area
TERTIRAY CULTURAL DEPOSIT
- Those that have been completly removed from their original context
Plant studies are used to try and reconstruct
the vegetation that past people encountered at a particular time and place
Pollen analysis
can be applied to a wide range of sites and provides info on chronology and the enviroment
pollen gives ___________instead of _________
the idea of fluctuations in vegetation through time and an exact picture of past environments
Diatom analysis
· Diatoms are single-cell algae that have cell walls of silica instead of cellulose
what is important about silica
Silica cell walls survive after the algae die
Diatoms are used to identify
the period when lakes became isolated from the sea in areas of tectonic uplift
To locate the positions of past shorelines
Indicate marine transgressions
Reveal water pollution
Phytoliths
Minute particles of silica (plant opal) derived from the cells of plants and survive after the rest of the organism decomposes
where are phytoliths common
hearths and ash layers
why are phytoliths useful
o Produced in large numbers
o Survive well in ancient sediments
Have lots of distinctive shapes and sizes according to type
where do phytoliths survive
in sediments that are hostile to other preservation of fossil pollen
what can phytoliths inform us about
The use people made of particular plants
A simple presence that adds to the picture of the environment
phytoliths
Fossil cuticles
Cuticles are the outermost protective layer of skin (epidermis) of leaves or blades of grass
what are fossil cuticles made from
Made from cutin with different silica shapes and patterns
A useful complement to palynology where grass material, whole or fragmentary, needs to be identified
fossil cuticles
Rock varnishes are
natural accretions of manganese and iron oxides with clay minerals and organic matter
there is a strong correlation between _______ and their different local environments
relatively stable carbon isotopes
what provides information on changing conditions and the abundance of different plants
The ratios of these stable carbons found in the different layers of varnish on rock
first evidence used by archaeologists to characterize the climate of the prehistoric period
animal remains
different species were absent, present or abundant in certain layers would be
reflected in certain periods
Microfauna
Small animals that tend to be better indicators of climate and environmental changes than larger species
why are microfauna better at indicating climate changes
o They are more sensitive to small variations in climate
o Adapt better to them relatively quickly
what reflects the immediate environment
microfauna
what is an issue with larger animals
Animals killed by humans have been seen as prey and the bones cannot accurately reflect the full range of fauna present
Macrofauna is ideal when
animal remains brought by natural accident or catastrophe