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Faunal remains are parts of animals that have been left in the material record, which archaeologists study. 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 ]
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 ...
Zooarchaeology which is the study of animal remains from archaeological sites is able to provide insight into the diet of both humans and animals, resource use, the economy, climate, technological adaptations, human demography, urbanisation and a wide variety of information about how humans operated within their environment.
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 ...
The abundance of faunal remains recovered at the site, totaling approximately 20,000 bones and bone fragments, exhibited the importance of animal resources in the diets of the past inhabitants. Findings revealed the presence of diverse fauna, including fallow deer, deer, wild pigs, and wild cattle, indicative of intensive hunting practices.
Often biostratigraphic correlations are based on a faunal assemblage, rather than an individual species — this allows greater precision as the time span in which all of the species in the assemblage existed together is narrower than the time spans of any of the members. Furthermore, if only one species is present in a sample, it can mean ...
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.