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Archaeological Investigations at Yourhaney Plantation (38GE18)

Archaeological Investigations at Yourhaney Plantation (38GE18)

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ARCHAEOLOGICAL INVESTIGATIONS AT YOURHANEY PLANTATION131Fragment<strong>at</strong>ion can result from such taphonomic factors such as differential destruction during thebutchering of carcasses, breaking of bone during processing, and scavenger activity (Grayson1984: 17). Factors outside the realm of intentional breakage th<strong>at</strong> infl<strong>at</strong>e NISP include trampling,breakage during excav<strong>at</strong>ion, and careless handling of specimens. (Lyman 1994: 101).When NISP is used as a measure of abundance of taxa <strong>at</strong> a site, its use causes the analyst toassume all fragment<strong>at</strong>ion, be it cultural or the result of some other force, is uniform and th<strong>at</strong> all taxaare being represented, recovered, and counted equally (Reitz and Wing 1999: 192). In this vein,NISP does not account for differential survivability of bones and is unable to determine the howmany of the bones belong to one individual organism. It also affects the identifiability of aspecimen, which varies from taxa to taxa. While NISP has a few limit<strong>at</strong>ions, it was utilized in thisanalysis.Bone weight, which represents quantities of bone present, is useful for comparing rel<strong>at</strong>ive size ofspecimens, as well as degree of fragment<strong>at</strong>ion (Jackson and Scott 2001: 189; Reitz and Wing1999: 200; Erlandson 1994: 151, 154; Zeder 1991: 107, 219). It can also be used to comparein a rel<strong>at</strong>ive way the quantities of bone representing different taxa (Reitz and Wing 1999: 200;Driesch 1993; Stahl 1995: 158). While it cannot account for differential densities of bone, it doeselimin<strong>at</strong>e the neg<strong>at</strong>ive effects fragment<strong>at</strong>ion has on assemblages (Jackson and Scott 2001: 189).Due to its strengths and the fact th<strong>at</strong> it provides the most robust quantit<strong>at</strong>ive measure, weight d<strong>at</strong>awas obtained during this analysis.The size ranges of the fish from the site were examined to infer wh<strong>at</strong> procurement methods werepossibly used. Species percentages for fish were analyzed to determine wh<strong>at</strong> environments weretargeted for resource acquisition.Burned bones were recorded, as were bones th<strong>at</strong> exhibit calcin<strong>at</strong>ion. The percentages of burntbones were looked <strong>at</strong> in rel<strong>at</strong>ion to species. Calcined bones were noted as it provided inform<strong>at</strong>ionon the intensity and dur<strong>at</strong>ion of exposure to fire.ARCHAEOBOTANICAL STUDYThis archaeobotanical analysis focuses upon macroplant remains collected by flot<strong>at</strong>ion from 12prehistoric N<strong>at</strong>ive American fe<strong>at</strong>ures (5 Woodland, 3 Mississippian, 4 indetermin<strong>at</strong>eWoodland/Mississippian), 14 historic Euro-American fe<strong>at</strong>ures (3-18 th century, 4-circa 1800, 2-19 thcentury, 5-indetermin<strong>at</strong>e 18 th /19 th century), and 1 non-fe<strong>at</strong>ure control sample (Bag 417). Thesampled fe<strong>at</strong>ures (Tables 1-2) consisted of historic hearths (N=3), historic postholes (N=5),indetermin<strong>at</strong>e pits (N=9), pits containing smashed prehistoric pottery vessels (N=4), an historicbuilder’s trench (N=1), an historic root/storage pit (N=1), an historic clay extraction pit (N=1), aprehistoric human burial (N=1), and an historic midden deposit (N=1) from the Yauhannah BluffSite (38GE19). The non-fe<strong>at</strong>ure context (Bag 417) was a control sample collected from generalexcav<strong>at</strong>ion fill.Prehistoric occup<strong>at</strong>ion of this multi-component site consisted of Early through L<strong>at</strong>e Woodland Periodand Mississippian Period occup<strong>at</strong>ions. Five of the fe<strong>at</strong>ures th<strong>at</strong> were sampled for archaeobotanicalremains clearly d<strong>at</strong>e to the Woodland Period (Table 14).

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