![]() ![]() Most of WCFs were established mainly for business and community services. Results showed that Tanzania has 28 active and 42 dormant WCFs. Descriptive statistics and Gross Profit Margin were used to analyze data on WCF status and cost-benefit analysis respectively. This study employed key informant interviews, participatory observations and counts to generate information on the status of WCFs in Tanzania. Tanzania harbours a number of these facilities, however, information on exact number, types, functioning status, size, composition and health is limited. Whether such arrival is in any ",ay connecteel me Neolithisation process of the Iberian Peninsula is an intriguing possibility impos"ibJe to verify with the data presently at hanel.Wildlife captive facilities (WCFs) are accommodations for ex-situ conservation of wild animals, they include wildlife ranches, farms, breeding facilities, orphanage centers, sanctuaries and zoos. The radiocarbon elating of horse bones from the leve] right aboye the one where the Beech J.Jarten fibula was retrieveel (5,310-5,010 caJ B.C.), suggests that the species reached Iberia coinciding with the Early Neolithic. In this paper we present the earliest evidence of the Beech Marten in the Iberian Peninsula along with a discriminant feature on the fíbula that sets apart both marten species. The matter is complicated by the fact that the postcranial bones of the Beech :Vlarten are easily misidentifíed with those of the Pine Manen (Martes martes). Its present distribution suggests that the species was a Holocene immigrant from sou thwest Asia but the details of its putative expansion remain poorly documented ro this day. The historical biogeography of the Beech marten (Martes foina) in Europe is still sparsely kIlown. The application of rapid methods to other assemblages is questioned, and finally, avenues for further research are explored. Discussion highlights the similarity of results and examines the biases in each system. New data from the rapid system is incorporated into previous investigation of animal management. The outcome of each method is presented and the arising differences interpreted. The original report, which identified as many specimens as possible, was then compared to new results derived from a rapid recording system. To test the limitations of a rapid recording and quantification system, the previously studied faunal assemblage from Bantycock Mine, Balderton (Nottinghamshire) was recorded and quantified a second time. Despite their increased usage, rapid techniques have rarely been directly evaluated and conditions concerning their appropriate application are generally undefined. ![]() Over the last few decades, methods that include only a restricted suite of skeletal parts have grown in popularity for their ability to rapidly record and analyze assemblages. ![]() Many methods of recording and quantification are currently employed in vertebrate faunal analysis. It could indicate the cooking of turtles directly on hearths or that carapaces were used as vessels to cook or heat food or other substances. In phase 4 only the carapace fragments are burned, whilst plastron elements are not. In particular most specimens related to the carapace and the plastron are carbonised or calcined. Burned specimens related to this taxon are very common, more than ones related to other taxa. Cut marks on limb bones testify the consumption of this reptile. Results of a taphonomic analysis conducted on Emys orbicularis remains are presented in this paper. Evidence of Cyprinid and Pike fishing and a great amount of beaver bones as well as presence of otter and Union testify an intense exploitation of wetland resources. (7705 -7478 BC caL), attesting that the si te was frequented by human groups between the final part of Preboreal and the midBoreal. The range of radiocarbon dating is betwt'en 926S ± 70 years BP uncal. It is located above a detritic cone near the wet environment in the va11ey bottom. The Early Mesolithic rockshelter site Gaigenbuhel/Dos de la Forca (Province of Bozen/Bolzano, Italy, Eastern Alps) lies in the Adige/Elsch Va11ey at the foot of a steep rock face that borders the va11ey.
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