Cow

PALAEOECOLOGY

fossil cow dung

glacial refugia

hyena coprolites

forest ecology

cave palynology

extra-fossils

vegetation climate

taphonomy

abrupt climatic changes

bat guano

holocene global carbon

hyrax middens

pollen cave surface

ecological turnover and         Neanderthals

ALLERGICS

POLLEN MORPHOLOGY

BIO-CONSERVATION

HONEYS

 


RESEARCH: OUTCOMES, VIEWPOINTS & PERSPECTIVES

Iron Age cow dung is potentially useful in Palaeoenvironmental reconstruction. Examples from southern Africa

Trichuris

Thick accumulations of consolidated cow dung occur in ancient kraals (byres or corrals) in the bushveld and highveld areas of Zimbabwe, Botswana, and South Africa in the last 2000 years. They originated from long-term cattle herding by Iron Age people. The "vitrified" or baked dung deposits are thought to be a product of the burning of cow dung as fuel, either for domestic purposes or for iron smelting.

In order to establish the palaeoecological potential of this material, thirty-six samples of cow dung from archaeological sites within the present-day savanna and grassland biomes were analyzed for pollen and other microfossils. Twenty nine of the samples contained pollen together with other microfossils that support a faecal origin of the material such as sordariaceous ascospores, Thecaphora, Gelasinospora, and Chaetomium, and eggs of the intestinal parasite Trichuris. Similar microfossils were also found in recent fresh cow dung from the same study areas.

AcariThe presence of pollen grains and spores in most of the Iron Age samples lead to the assumption that they survived the burning because fire temperatures were not high enough to destroy them. Pollen in these cow dung pieces is apparently sealed and can be preserved under open-air conditions at sites under which pollen in other deposits like soils, will perish. Good pollen preservation and palynomorph diversity were found with mainly Poaceae, and secondly Chenopodiaceae and Cyperaceae as the most important pollen contributors, while tree and shrub indicators of savanna are rare. In the case of the samples that came from the subtropical savanna biome the latter result is unexpected and suggests that the cattle were kept in more open vegetation than the woody environments of today. Recent cow dung samples reflect the composition of present-day vegetation by showing considerably higher proportions of tree pollen than the fossil assemblages.

More in...

CARRIÓN, J.S., SCOTT, L., HUFFMAN, T. & DREYER, C. 2000. Pollen analysis of Iron Age cow dung in southern Africa. Vegetation History and Archaeobotany 9: 239-249


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