AR101 Exam Two Flashcards
(100 cards)
archaeozoology
involves the identification and analysis of faunal species from archaeological sites, as an aid to the reconstruction of human diets and to an understanding of the contemporary environment at the time of deposition
australopithecus
a collective name for the earliest known hominids emerging about 5 million years ago in East Africa
context
usually consists of an artifact’s immediate matrix (the material around it e.g. gravel, clay or sand), its provenience (horizontal and vertical position in the matrix), and its association with other artifacts (with other archaeological remains, usually in the same matrix
coprolites
fossilized feces; contain food residues that can be used to reconstruct diet and subsistence activities
deep sea cores
drilled from the sea bed, provide the most coherent record of climate changes on a worldwide scale; contain shells of microscopic marine organisms (forminifera) laid down on the ocean floor through the continuous process of sedimentation. Variation in the ratio of two oxygen isotopes in the calcium carbonate of these shells give a sensitive indicator of sea temperature at the time the organisms were alive
diatom analysis
a method of environmental reconstruction based on plant microfossils; unicellular algae whose silica cell walls survive after the algae die, adn they accumulate in large numbers at the bottom of rivers and lakes. Assemblages directly reflect the floristic composition of the water’s extinct communities, as well as the water’s salinity, alkalinity, and nutrient status
diatoms
found in lake and shore sediments and thus useful for the analysis of past marine environments
domestication of wild plant species
various techniques can help to answer the crucial question of whether plant remains found in the archaeological record are from wild or domesticated species
flotations
a method of screening (sieving) excavated matrix in water so as to separate and recover small ecofacts and artifacts
ice cores
borings taken from the arctic and anarctic polar ice caps, containing layers of compacted ice useful for reconstructing paleoenvironments and as a method of absolute dating
information from animal resources
animal remains are often well-preserved on archaeological sites. It’s important to establish whether animal remains are present ona site through human agency or through other causes. We can sex and age animal bones, study their seasonality, and deduce whether the animals were wild or domesticated, all of which helps us to understand how humans were exploiting the animal environment
isotopic analysis
an important source of information on the reconstruction of prehistoric diets, this technique analyzes the ratios of the principal isiotopes preserved in human bone; in effect the method reads the chemical signatures left in the body by different foods; also used in characterization studies
macrobotanical remains
seeds and fruits, plant residues, wood; can give a good idea of what plants were present at a site, but there are problems of quantification and interpretation. It’s important to understand how a plant might have been processed and used
microbotanical remains
pollen, phytoliths, diatoms
microfauna
better indicators of climate and environmental change than macrofauna because they are much more sensitive to small variations in climate and adapt to them relatively quickly; tend to accumulate naturally on a site and refelct the immediate environment more accurately than the larger animals whose remains are often accumulated through human or animal predation
microwear analysis
the study of the patterns of wear or damage on the edge of stone tools, which provides valuable information on the way in which the tool was used
paleoethnobotany
the recovery and identification of plant remains from archaeological contextgs, used in reconstructing past environments and economies
paleoentomology
the study of insects from archaeological contexts. the survival of insect exoskeletons, which are quite resistant to decompositions, is important in the reconstruction of paleoenvironments
paleomagnetism
based on the fact that changes in the earth’s magnetic field over time can be recorded as remnant magnetism in materials such as baked clay structures (ovens, kilns, and hearths)
palynology
the study and analysis of fossil pollen as an aid to the reconstruction of past vegetation and climates
phytoliths
minute particles of silica in plant cells which survive after the rest of the plant has decomposed; some are specific to certain parts of the plant; survive very well in most archaeological sediments and can add to the picture of the environment built up from other sources
plant residues on artifacts
chemical traces of plants can be found on some artifacts (often pots and tools) and these can be tested and compared against a reference collection in order to identify a species
plant residues
can give some idea of what species were available
pollen
most useful for the study of minor fluctuations in climate over the last 12,000 years though can be preserved for millions of years in some contexts