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Archaeological Investigations at Yourhaney Plantation (38GE18)

Archaeological Investigations at Yourhaney Plantation (38GE18)

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ARCHAEOLOGICAL INVESTIGATIONS AT YOURHANEY PLANTATION129VI. SUBSISTENCE STUDIESThe following chapter discusses the archaeobotanical and zooarchaeological remains recoveredfrom fe<strong>at</strong>ure contexts <strong>at</strong> the Yauhannah Bluff Site (<strong>38GE18</strong>). The first portion of the chapterdiscusses the analytical methodologies th<strong>at</strong> were utilized, which is followed by sections discussingthe archaeobotanical and zooarchaeological studies.ANALYSIS METHODSARCHAEOBOTANYMacroplant remains analyzed in this study were derived from 26 flot<strong>at</strong>ion samples from 25 culturalfe<strong>at</strong>ures and one general excav<strong>at</strong>ion fill sample (Table 14). The five to 10 liter samples wereflo<strong>at</strong>ed by New South Associ<strong>at</strong>es, Inc. staff members. The samples were subjected to machineassistedw<strong>at</strong>er separ<strong>at</strong>ion in a 55-gallon Shell Mound <strong>Archaeological</strong> Project (SMAP) type flot<strong>at</strong>ionmachine (Pearsall 1989; W<strong>at</strong>son 1976). The heavy fraction insert of the system was screened with0.8 mm mesh.In the labor<strong>at</strong>ory, each flot<strong>at</strong>ion sample was first weighed, and then passed through nestedgeologic sieves (2.0 mm, 1.0 mm, 0.71 mm, 0.5 mm). Each size-graded light fraction was fullysorted under low magnific<strong>at</strong>ion (10-25x). All charred plant remains th<strong>at</strong> were gre<strong>at</strong>er than 2.0 mmwere pulled from the sample m<strong>at</strong>rices and were quantified by m<strong>at</strong>erial type, by weight, and bycount. M<strong>at</strong>erial th<strong>at</strong> was smaller than 2.0 mm was fully sorted, but only charred seeds wereremoved. The gre<strong>at</strong>er than 2.0 mm fraction of each of the flot<strong>at</strong>ion heavy fractions was sorted inorder to check the flot<strong>at</strong>ion separ<strong>at</strong>ion, which was verified as excellent. Seeds and wood charcoalwere identified with standard reference texts (e.g. Martin and Barkley 1961, Montgomery 1977;USDA 1974) and a modern reference collection.Identific<strong>at</strong>ions were made of wood charcoal fragments from each flot<strong>at</strong>ion sample (Tables 17-18).Wood charcoal was separ<strong>at</strong>ed from other debris before <strong>at</strong>tempting specific identific<strong>at</strong>ion.Whenever possible, wood specimens were identified to genus. Segments th<strong>at</strong> were toofragmentary or poorly preserved to specifically identify were placed in the more general c<strong>at</strong>egoriesof conifer, monocot, indetermin<strong>at</strong>e hardwood, or unidentifiable. Wood taxa were identified bycomparison with charred and n<strong>at</strong>ural transverse, tangential, and radial thin sections of modernwood, as well as textbook illustr<strong>at</strong>ions. The transverse view was emphasized due to magnific<strong>at</strong>ionlimit<strong>at</strong>ions, size of the specimens, and time constraints. As needed, dichotomous keys wereemployed. Since these are geared toward fresh wood they are of limited use, but by employingboth the microscopic and macroscopic keys, following multiple p<strong>at</strong>hs, and with frequent referenceto the compar<strong>at</strong>ive collection, a genus can generally be determined.In this analysis, the macroplant d<strong>at</strong>a were quantified by individual fe<strong>at</strong>ure, time period (Woodland,Mississippian, Woodland/Mississippian, 18 th century, circa 1800, 19 th century, 18 th /19 th century,control), total prehistoric and historic, and total number of samples.

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