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These remains are important to the record because they can show cultural practices, such as what food they were eating, based on the remains left behind. [11] Zooarcheologists can find out information like the species the animal is, the age the animal was when it died, and what its sex was.
Animal remains have the potential to be both an ecofact and artifact and their classification is dependent on the context in which they may have been used. If not deliberately altered, animal remains can be classified as an ecofact, and can often reveal the dietary habits of a past group of people.
In archaeology and paleontology a faunal assemblage is a group of animal fossils found together in a given stratum. [1] In a non-deformed deposition, fossils are organized by stratum following the laws of uniformitarianism [2] and superposition, [3] which state that the natural phenomena observable today (such as death, decay, or post-mortem transport) also apply to the paleontological record ...
Animal remains were the first evidence used by 19th century archaeologists. Today, archaeologists use faunal remains as a guide to the environment. It helps archaeologists understand whether the fauna were present naturally or through activities of carnivores or people. [4] Archaeologists deal with macrofauna and microfauna. Microfauna are ...
Faunal remains are considered to include both fish, birds, and mammals. These remains are used to reconstruct past environments and identify how animals impacted human economies. The study of ancient animal remains is referred to as zooarchaeology. Once bones are collected, cleaned, and labeled, specialists begin to identify the type of bone ...
Additionally, faunal analysis exists to study artifacts in the form of animal remains. Just as with lithic artifacts, faunal remains are extremely common within the field of archaeology. Faunal analysis provides insight to trade due to animals being exchanged in different markets over time and being traded over long distances.
The Isimila Prehistoric Site has yielded various faunal remains that provide valuable insights into the environment and ecosystem during the middle Pleistocene occupation. Due to the acidic nature of sediments in the Lisamagalasi formation and upper Lukingi level, [1] most faunal remains were recovered in the middle Luking level (sand 4).
Taphonomy is the study of how organisms decay and become fossilized or preserved in the paleontological record. The term taphonomy (from Greek táphos, τάφος 'burial' and nomos, νόμος 'law') was introduced to paleontology in 1940 [1] by Soviet scientist Ivan Efremov to describe the study of the transition of remains, parts, or products of organisms from the biosphere to the lithosphere.