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2019 The Lithic Analysis of an Early Floridian Archaeological Site in the Wacissa River Eric Calvin Vinh Jones
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THE FLORIDA STATE UNIVERSITY
COLLEGE OF ARTS & SCIENCES
THE LITHIC ANALYSIS OF AN EARLY FLORIDIAN ARCHAEOLOGICAL SITE IN THE
WACISSA RIVER
By
ERIC JONES
A Thesis submitted to the Department of Anthropology in partial fulfillment of the requirements for graduation with Honors in the Major
Degree Awarded: Spring, 2019
The members of the Defense Committee approve the thesis of Eric Jones defended on March 29, 2019. Signatures are on file with the Honors Program office.
Dr. Jessi Halligan Thesis Director
Dr. Seth Young Outside Committee Member
Dr. Jayur Mehta Committee Member i
Abstract
The Middle Paleoindian period of the North American Southeast is a problematic area in
American archaeology. The lack of well preserved sites, dateable materials, and the frequent discovery of artifacts out-of-context are all part of why this is such a poorly understood period.
The Ryan-Harley site is one of the few undisturbed Middle Paleoindian sites in Florida and
represents the remnants of a campsite inhabited by the Suwannee, a cultural group belonging to
this Paleoindian period, therefore making its study and analysis of the utmost importance.
This thesis presents the mass analysis of stone flakes and tools excavated in 2017 from a
discrete geologic layer at the Ryan-Harley site. This was completed in order to achieve a better
understanding of what types of tool production were taking place at the site, how that can
provide information regarding site function and human behaviors, and to support the findings of
past excavations conducted at the site.
The systematic analysis of the attributes and characteristics of 344 lithic artifacts showed
97% of the assemblage consisted of flake debitage, composed primarily of small biface thinning
flakes. Ten tools were also recovered, including multiple flake tools, scrapers, and a late-stage
biface combination tool. These findings represent late-stage tool reduction of local raw materials
at a small campsite occupation. This is in accordance with the conclusions of previous
excavations and provides a comparable study for future lithic analyses of Middle Paleoindian
sites in Florida.
ii
Acknowledgements
This thesis would not have been possible without the time and resources of multiple groups and individuals. My sincerest thanks to the following: Ryan and Harley Means, the
Center for the Study of the First Americans, Dr. Michael Waters, Morgan Smith, Adam Burke, the Florida Bureau of Archaeological Research, the Suwannee River Water Management
District, the Aucilla Wildlife Management Area, the FSU Archaeological Field School of 2017, and the FSU Department of Anthropology.
To all those with whom I have had the honor and pleasure to work with during this project – thank you. I am indebted to the members of my Thesis Committee, who have helped me complete this and have provided valuable feedback and discussion. I am especially grateful for Dr. Jessi Halligan, my advisor and director of the thesis committee. As my teacher and mentor, she has stimulated and inspired my interests in this field of study beyond measure and has taught me more than I could ever give her credit for here. Thank you for your time, great conversations, and never-ending encouragement. I would also not be where I am without Analise
Hollingshead, my graduate mentor and friend. With her constant hospitality and willingness to aid me in any capacity I have been taught so much. I am grateful for all she has done for me and for her patience and kindness over the past couple of years.
I would like to thank my family, whose love and excitement is with me in everything I
do. Their motivation and encouragement were, and continue to be, invaluable. I also wish to
thank my incredible partner, Jazmin. Her unwavering support and endless patience were
instrumental in this journey and through the many stressful and difficult times. Thank you for always being there for me. iii
Table of Contents
Page
Abstract i
Acknowledgments ii
Table of Contents iii
List of Figures v
List of Tables vi
Chapter I Introduction 1
Significance of Research 1 Research Questions and Organization of Thesis 2
Chapter II Background 4
Chapter III Methodology 10
Artifact Collection 12 Lithic Analysis 12 Flake Analyses 15 Flake Tool Analysis 19 Biface and Core Analysis 22 Microscopy 26
Chapter IV Results 30
Flake Debitage Results 30 Tool Results 39 Microscopic Analysis 46
Chapter V Discussion 49
Lithic Analysis 49 Tool Analysis 52 Site Function Analysis 53
iv
Chapter VI Conclusions and Future Research 59
Concluding Remarks 59 Future Research 59
References Cited 62
Appendix I 71
Appendix II 75
v
List of Figures
Page
Figure 1: The location of the Ryan-Harley site in Jefferson County, Florida 5
Figure 2. The diagnostic Suwannee points recovered from previous excavations 8
Figure 3. Profile of the 2017 Ryan-Harley Excavation 11
Figure 4. Site map of island and the three units excavated in the summer of 2017 by FSU SCUBA divers 12
Figure 5. Microscopic view of diagnostic miliolid (center) found in Suwannee chert 28
Figure 6. Classification of debitage by flake type 30
Figure 7. Classification of flake debitage by platform type 32
Figure 8. Classification of broken and fragmented flakes by portion 33
Figure 9. Classification of flake debitage by termination 33
Figure 10. The distribution of complete flake lengths in one centimeter increments 36
Figure 11. Weight distribution of complete flakes in one gram increments 36
Figure 12. Length to width ratio of complete flakes 37
Figure 13. Weight distributions based on all biface thinning and edge retouch flakes 37
Figure 14. Ratio of thickness to weight for biface thinning and edge retouch flakes 38
Figure 15. Composite image of the ten tools identified in the lithic analysis: (a) flake tool, (b) late stage biface/scraper, (c) early stage biface, (d) flake tool, (e) scraper, (f) core, (g) scraper, (h) flake tool, (i) flake tool, (j) flake tool/scraper 43
Figure 16. Percentage distribution of the raw material types of the Ryan-Harley assemblage 46
Figure 17. A diagnostic Miliolid foraminifera found in Suwannee chert 48
Figure 18. A V-shaped Dictyoconus diagnostic of Suwannee chert 48
vi
List of Tables
Page
Table 1. Lithic Analysis Characteristics and Attributes of Debitage 14
Table 2. Lithic Analysis Characteristics and Attributes of Flake Tools 20
Table 3. Lithic Analysis Characteristics and Attributes of Bifaces and Cores 23
Table 4. Classification of flake debitage by technological type 31
Table 5. Flake debitage by percent of cortex 34
Table 6. Tool attributes and characteristics by category 41
Table 7. Biface and core attributes and characteristics by category 42
Table 8. Values used in Simpson’s diversity index of technological artifact type 44
Table 9. Values used in Shannon’s diversity index of technological flake type 44
Table 10. Values used in Simpson’s diversity index of Ryan-Harley artifacts 45
Table 11. Data used to construct a Fisher Exact Test 45
Table 12. Chi-Square Test Values 45
1
Chapter I
Introduction
Significance of Research
The rise of lithic debitage as a viable medium through which to analyze prehistoric stone technology and human behavior only began within the last half century. It was once referred to and neglected as prehistoric trash and debris, but has since become an integral part of the analyses of lithic materials from archaeological sites. Arguably one of the most common artifacts found at sites worldwide, the variability and complexity of lithic debitage is what makes it such an important artifact to analyze in order to understand the processes that account for its complexity (Andrefsky 2001, 2005, 2007; Collins 2008; Eerkens et al. 2007; Goodyear 1979;
Kelly 1988; Pevny et al. 2012; Williams and Andrefsky 2011). Defined as the by-product flakes and chips removed by percussion or pressure from an objective piece, debitage provides researchers with a look into the technological and social aspects of stone tool production. This thesis discusses lithic analyses that involved the study of flake debitage and stone tools from a
Florida Paleoindian site and the behavioral patterns that can be interpreted from such analyses.
As stone artifacts, the lithic materials of archaeological sites are the most likely to
preserve and withstand the tests of time in many global conditions. This is what makes lithics such a common part of the artifact assemblages at archaeological sites. In the Southeast region of
North America, there is a heavy preservation bias that favors lithic materials, usually leaving
Paleoindian sites absent of organics that would be useful in the analysis of these prehistoric peoples (Dunbar and Vojnovski 2007; Halligan in press, 2012; Stojanowski et al. 2002; Stone et al. 1990). The artifact assemblages at the submerged Ryan-Harley site (8JE1004) are the 2 remnants of a Middle Paleoindian occupation in the Wacissa River that contains a valuable assortment of lithic artifacts that present evidence of the Suwannee culture complex. This paper is a discussion of a full lithic analysis completed on the most recent stone artifact assemblage recovered from Ryan-Harley.
The Ryan-Harley site is significant because it is the only archaeological site in the
American Southeast where diagnostic Suwannee material has been recovered in situ through extensive excavations. Dunbar and others (2005) suggest this site represents a Suwannee campsite post-dating the Clovis period (13,250-12,800 cal BP) based on Suwannee point morphology and relative dating methods. The analysis of the most recently recovered lithic
materials from three 1x1 meter excavation units provides further evidence of the Suwannee
occupation at Ryan-Harley and opens another window into the stone tool production and
behaviors of its inhabitants in a region where Paleoindian studies have recently become more defined.
Research Questions and Organization of Thesis
Three research questions were proposed at the beginning of this study: (1) what types of lithic manufacturing was taking place at the site, (2) what behavioral patterns can be derived
from this lithic analysis, and (3) do the results of this analysis support what previous conclusions
have been made about the Ryan-Harley site?
Through mass lithic analysis, the interpretation of what tools were being manufactured or
recycled could be achieved. The apparent presence or absence of formal or informal tools
indicates other activities happened at the site and allowed for the analyses of site functionality
and mobility strategies (Andrefsky 2005; Daniel and Wisenbaker 2017; Kelly 1988). The lithic
materials analyzed as a part of this assemblage are from the same cultural layer that Dunbar and 3 others (2005) previously excavated, so it was likely my research would reach similar conclusions.
This thesis presents the research of the Ryan-Harley lithic analysis in six chapters.
Chapter II describes Ryan-Harley, the conclusions of past excavations conducted at the site, and the most recent excavations that provided the lithic assemblage for this analysis. Chapter III provides in depth descriptions of the methods used to examine the flake debitage and tools recovered from the site. Chapter IV discusses the results of the lithic analysis, highlighting important aspects of our findings. Chapter V describes the interpretations of the results from the previous chapter, discussing residency models and site function analyses as it pertains to Ryan-
Harley. Chapter VI provides concluding remarks and potential directions of future research. 4
Chapter II
Background
The richness of Florida’s Paleoindian record has only been recognized in recent decades, and has since provided archaeologists a glimpse into the complex groups that once inhabited the
Southeast United States (Anderson 1990; Anderson and Sassaman 2012; Anderson et al. 2015;
Daniel and Wisenbaker, 2017; Dunbar et al. 2005; Dunbar and Vojnovsky 2007; Halligan in press, 2012; Smallwood 2012; Thulman 2009, 2012). While characterized by a unique and vast
Paleoindian record, the poor preservation and destruction of sites in the region are a common result of the changes made by the shifting climate and landscapes since the late Pleistocene.
Weathering and erosion has resulted in the general absence of datable organic material culture, and has rendered many of Florida’s discovered Paleoindian stone artifacts out of primary contexts and unable to be accurately dated (Halligan in press, 2012). This lack of accurate radiocarbon dates and in situ sites are among the many challenges archaeologists face in Florida when approaching the Paleoindian record of the Southeast.
Located in a spring-fed stream channel along the Wacissa River in the southern edge of
Jefferson County in North Florida, the submerged Ryan-Harley site (8JE1004) has provided researchers with a representation of a post-Clovis, Suwannee-point campsite (Dunbar et al. 2005;
Figure 1). It is unique in that it is the first Middle Paleoindian site where diagnostic Suwannee material has been recovered in situ with a large assemblage of faunal remains. Relative dating techniques based on stratigraphy and diagnostic artifact seriation has described Suwannee-age sites with a time frame ranging from ca. 10,900 14C cal BP to 10,500 14C cal BP (Balsillie et al.
2006). 5
Figure 1: The location of the Ryan-Harley site in Jefferson County, Florida.
Due to its undisturbed context, the Ryan-Harley site provides a specialized view into some aspects of the Suwannee point-makers’ lives. The large magnitude of faunal remains found at the site presented an opportunity for analyses of Middle Paleoindian subsistence and diet in
the North Florida region. The presence of several extinct fauna, such as horse and tapir, could
indicate that Pleistocene fauna survived in the Southeast past the Allerød/Younger Dryas
boundary ca 11,000 cal BP, unlike their southwestern counterparts (Dunbar et al. 2005; Dunbar
and Vojnovsky 2007; Balsillie et al. 2006; Pevny et al. 2018). Unfortunately, these remains are
most often leached of datable collagen, representing the most frustrating issue of Middle
Paleoindian sites in Florida (and therefore of Ryan-Harley) – the utter lack of absolute dates to
definitively date cultural materials (Balsillie et al. 2006; Halligan 2012).
This lack of dated material results in a serious theoretical concern regarding the true
identification of where Middle Paleoindian sites are in the chronological sequence of Florida’s 6 earliest inhabitants. Much of the literature on Middle Paleoindian sites state that Suwannee points are related to Clovis, which is rooted in the identification of similar traits in lithic reduction and toolkits between the two cultures. With these characteristics, Suwannee has been considered to represent a regionalized descendant population in an area where Pleistocene fauna survived longer (Basillie et al 2006; Dunbar and Vojnovsky 2007; Dunbar et al. 2005; Pevny et al. 2018). However, Suwannee could potentially be even older than it is currently thought and is perhaps contemporary with Clovis or even older (Anderson et al. 2015; Stanford 1991).
Paleoindian sites in Florida tend to show occupations that are localized around a resource rich area, focusing on nearby resources such as lithic raw materials, but even more so on dependable and potable water sources. During the terminal Pleistocene, inhabitants of Florida’s interior were presented with a xeric environment which would have made areas dry enough to motivate human groups to concentrate their occupations around or close to locales with reliable water sources (Pevny et al. 2018; Thulman 2009). This Oasis Model highlights the tendency of
Paleoindian sites to be concentrated around these terminal Pleistocene watering holes. These locations would also serve as excellent areas for food procurement, as local game would be drawn to the available water sources and provide Paleoindian peoples with dependable and expectable food and water resources. This provides researchers with an idea of where in Florida there might be concentrations of Paleoindian sites, so long as there is reliable landscape and environmental reconstructions that allow for greater potential in discovering these past surface water locations (Thulman 2009). These hypotheses grant archaeologists the ability to ask who the first Floridians were and how they lived, and how sites like Ryan-Harley are preserved or destroyed. It is in order to answer questions like these that the Ryan-Harley site must be researched and carefully studied. 7
After its discovery by Ryan and Harley Means in 1996, subsequent excavations in 1999 and 2015 found the site to be a baseline for the comparison of faunal and cultural remains to other Paleoindian sites in Florida (Dunbar and Vojnovsky 2007). The past excavations yielded a toolkit that includes a variety of scrapers, flake tools, and displaced diagnostic Suwannee points
(Figure 2), but one that is also hard to distinguish because the most reputable sites have not provided proper stratigraphic separation of Suwannee and other cultural materials, like the Bolen complex. This is seen at the Harney Flats site (8HI507), where Suwannee and Bolen materials are found in nearly the same stratigraphic levels at a Paleoindian base camp. What is seen in the
Ryan-Harley toolkit is a complete absence of the hafted unifacial and bifacial tools that are found in the Bolen and Dalton assemblages (Dunbar et al. 2005). This makes the Suwannee toolkit distinct among these other documented complexes and is why the Ryan-Harley lithic assemblages are unique. Unlike the Bolen toolkit, the Suwannee point assemblages at Ryan-
Harley do share some features found in Clovis assemblages (Dunbar et al. 2005). These similarities were identified by Dunbar and others (2005) as the occasional fluting, variation in size, and overshot flaking of uniface tools. With these apparent in the Ryan-Harley assemblage, and the similar morphological traits between the Suwannee and Clovis points, it is reasonable to suggest that Suwannee reflects a Middle Paleoindian toolkit that evolved from that of the Clovis complex.
The results of the past lithic analyses at the Ryan-Harley site concluded that tool production and maintenance occurred, and the concentrations of diagnostic artifacts and debitage reveal Ryan-Harley to be a campsite where a long enough occupation required its inhabitants to use a variety of tools and exploit the local fauna (Dunbar et al. 2005). After geoarchaeological analyses, it was evident that no post-depositional reworking of stable sections of the site 8 occurred, allowing Ryan-Harley to be classified as not only a Paleoindian campsite, but as one in an undisturbed context as well (Balsillie et al. 2005, 2006). The results from the excavations by
Dunbar and others (2005) present data that show how valuable of an archaeological site Ryan-
Harley is, and provides a foundation for future southeastern Paleoindian studies of Suwannee culture.
Figure 2. The diagnostic Suwannee points recovered from previous excavations.
In an effort to gather more data on Ryan-Harley and its Paleoindian inhabitants, the FSU archaeological field school returned to the site in 2017 to expand upon the previous excavations.
These excavations at Ryan-Harley had three main research goals: (1) to obtain absolute dates within the Suwannee assemblage at the site, and (2) to describe how Suwannee people were 9 utilizing the Ryan-Harley site in order to (3) expand the understanding of the Suwannee culture in the Southeast. The research presented in this paper is focused upon the latter two goals through an analysis of the lithic assemblage from the three 1x1 meter units the 2017 field school excavated. The literature on the lithic analyses of Suwannee materials is rare, due to its uncommon appearance in situ and at only some reputable sites, therefore making this research a relevant addition to the understanding of one of the Southeast’s Middle Paleoindian cultures.
As one of the most common artifact types found at archaeological sites, the analysis of
lithic debitage from the assemblage found at Ryan-Harley can provide a wealth of knowledge
when inferring upon the behavioral patterns and lifeways of the site’s past inhabitants. The value
of debitage analysis became increasingly important in the last 30 to 40 years, having gained
traction once its potential as an interpretive tool for examining prehistoric human technology,
economy, and organization was realized (Andrefsky 2001:6). Researchers are still refining and
adapting the ways in which lithic debitage is analyzed in order to make these higher level
inferences and theories of human behavior. As stone artifacts are the most likely to preserve, it is
imperative that as much information be derived from them as possible. By examining the entire
assemblage of debitage from the Ryan-Harley site by uniform criteria, the most popular form of
debitage analyses can be conducted, known as aggregate, or mass, analysis (Andrefsky 2001:7,
2007). This is the aim for analyzing the lithic assemblage recovered by the FSU field school at
Ryan-Harley, and for which this paper is being written.
10
CHAPTER III
Methodology
Artifact Collection
The three Ryan-Harley units were excavated by SCUBA divers in controlled 5 cm levels from May to June in 2017. These submerged units were located against the modern stream bank
(Figure 3). The observed artifacts were plotted in place, and the team used laser control points to determine Northing, Easting, and elevation (Figure 4). The strike (compass orientation) and dip
(angle of the artifact against the matrix) were also recorded by the excavators. All of the sediments that were removed from the units were screened through nested 1/4" and 1/16” screens on the surface via floating screen deck. The artifacts were then slowly dried post-fieldwork and all relevant excavation data were entered into Microsoft Excel sheets allowing for virtual reconstruction of the site in a GIS. 11
Figure 3. Profile of the 2017 Ryan-Harley Excavation
12
Figure 4. Site map of island and the three units excavated in the summer of 2017 by FSU
SCUBA divers.
Lithic Analysis
From January 2018 to March 2018, I conducted macroscopic analyses of the excavated stone artifacts under the direction of my graduate mentor, Analise Hollingshead. The systematic analyses of the lithic artifacts were performed in order to address our research questions: (1) what types of lithic manufacturing were taking place at the site, and (2) what behavioral patterns of Suwannee point-makers can be derived from debitage analysis in an effort to (3) further confirm what previous excavations have concluded. These laboratory analyses were all conducted in the Florida State University Anthropology Department building. Our research identified flakes and flake tools, recording values for a total of 21 and 20 attributes and 13 characteristics respectively (Tables 1, 2, and 3). For this debitage analysis an attribute is defined as “a measureable characteristic of an artifact or specimen, such as length, color, or weight”
(Andrefsky 2005:252). A “characteristic” will be considered any other value or description that is not an attribute, such as the debitage classification or flake portion of the artifact. A conscious effort was made during the analyses of the Ryan-Harley material to keep consistent the attribute definitions, characteristics, and data recording methods throughout the study and to be consistent with previous lithic analyses conducted at Ryan-Harley and other North Florida sites (Burke
2014; Halligan 2012). This will allow datasets to be compatible with one another through different projects and be valuable for future research. This chapter will contain in depth discussions of what was recorded and how, as a good foundation of knowledge about these were an important aspect of the lithic analysis as a whole.
In order to address the research questions of this study, each artifact was coded and recorded for the following attributes and characteristics based upon the morphological and technological classifications and guidelines determined by Andrefsky (2005): length, width, thickness, weight, bulb and midpoint thickness, application load, material color, technological class, platform type, platform width and thickness, debitage class, flake portion, termination type, percent of cortex, raw material type, burning, polish, retouch, and eraillure scars. Those classified as flake tools were separated and defined using several different attributes and characteristics including: tool blank, hafting wear, number of edges, edge shape, retouch face and type, edge angle, and the total and worked edge length. Bifaces and cores that were identified were separated further to analyze the following: estimated completeness, missing portions, biface stage, planview shape, base type, cross-section type, dominate flaking type, end 14 thinning, edge angles of side one and two, core type, and number of flake scars (Halligan 2012).
See Appendix I for the full coding sheets used during the analysis.
Table 1. Lithic analysis characteristics and attributes of debitage.
Attribute/Characteristic Descriptions/Attributes/Characteristics Length (mm) Measured relative to maximum dimensions Width (mm) Measured perpendicular to length Thickness (mm) Measured at the thickest point of specimen Weight (g) Measured on digital scale Bulb Thickness (mm) Measured at the bulb of percussion Midpoint Thickness (mm) Measured at the center of the specimen Debris/Shatter, Flake fragment, Broken flake, Debitage Classification Complete flake Flake Portion Proximal, Medial, Distal Biface Thinning Flake, Retouched Scraper Technological Class Flake, Bipolar Flake, Platform Preparation Flake, Pressure/Edge Retouch Flake Cortical, Flat, Complex/Multifacet, Platform Type Abraded/Ground Platform Width (mm) Measured relative to maximum dimensions Platform Thickness (mm) Measured perpendicular to platform width The difference between bulb thickness and Application Load (mm) midpoint thickness is the relative bulb size Termination Type Feather, Step, Hinge, Plunging/Overshot In relation to Dorsal Surface: 0%, .1-10%, 11- Cortex Percentage 49%, 50-90%, 91-100% Suwannee, St. Marks, Coastal Plains, Raw Material Type Quartzite, Other (Unidentifiable macroscopically) Burnt None, Present Use-wear analytics not as identifiable Polish/Rounding macroscopically Will signify modification post detachment, Retouch therefore representing tool use Eraillure Scar None, Present Rock Color Assigned with a Munsell Color Charts
Using digital calipers the length, width, and thickness were measured to the nearest .01
millimeter. Length was measured relative to the maximum dimensions of the artifact, and width
was measured perpendicular to length at the widest point (Andrefsky 2005:99). Thickness was 15 measured at the thickest point, most typically at the bulb of percussion if one was present
(Andrefsky 2005:101). The weights of all samples were recorded using a digital scale and rounded to the nearest .01 gram (Andrefsky 2005:104-106).
Flake Analyses
Debitage classification is an important aspect of this study, and is divided into four categories to classify flakes under: shatter, flake fragment, broken flake, and complete flake.
Shatter is a catchall term that includes all flakes that could not be identified as a flake fragment, broken, or complete flake. Samples classified as shatter are typically small unintentional detachments during lithic reduction processes, and are missing identifiable characteristics of flakes such as distinct dorsal and ventral surfaces and striking platforms. Flake fragments are flakes missing their striking platform. Broken flakes are the opposite, as their platform is present, but the termination is missing. Complete flakes are unbroken and not fragmented, containing all the necessary parts of a flake to analyze it. The flake portion classification is therefore inherently associated with flake fragments and broken flakes, as it deals with what part of the flake a sample is. The proximal section of a flake contains the striking platform, therefore always classified as a broken flake. The medial classification is for flakes missing both a striking platform and a termination, while the distal portion of a flake is always reflected by the termination of a flake opposite the striking platform. These two portion types are always flake fragments as the striking platform is missing on both occasions.
Technological classifications are a popular method of lithic debitage analyses, referring to a typology that separates the samples into groups based on some characteristic(s) of the stone tool technology (Andrefsky 2005:120). Biface thinning flakes are usually marked by a complex striking platform with some degree of lip and contain multiple dorsal scars (Andrefsky 2005; 16
Burke 2014; Halligan 2012). Retouched scraper flakes are generally small with small, flat striking platforms (Andrefsky 2005:125; Shott 1995:64). Bipolar flakes typically have no bulb of percussion and show evidence of application load on areas opposite of each other with the appearance of compression rings (Andrefsky 2005:124-125). Platform preparation flakes can have a dorsal surface of varying morphology and a distinct, flattened ventral surface, signifying the manufacturer’s want of a prepared core. Pressure/edge retouch flakes are produced through pressure flaking, resulting in small retouch flakes with, sometimes distinctly curved, flat or complex platforms.
Platform data analysis is useful in determining reduction techniques and stages, but can come in an extreme variety. After the identification of the striking platform, width and thickness were measured according to Andrefsky’s (2005:Figure 5.5) guidelines. Platform width was measured as the distance across the striking platform from corner to corner, and the length was perpendicular to that width (Andrefsky 2005:94). Andrefsky (2005) notes several striking platform attributes that can be used to define a simple typology that incorporates this large scale variety of different types. This typology can then be supplemented with the length and width of the platform to generate more meaningful analyses of lithic reduction stages. There are four platform types that samples can be grouped under: cortical, flat, complex, and abraded
(Andrefsky 2005:94-97). Cortical platforms are those that are simply composed of or contain the unmodified cortex of the original surface. Flat platforms are smooth flat surfaces that usually articulate with the dorsal surface at an angle approaching 75°-90°. Complex platforms are those with multiple flake scars and a relatively rounded surface, and abraded platforms are complex platforms that have undergone additional smoothing as a result of abrasion or rubbing. 17
In many cases the striking platform is accompanied by a raised hump on the ventral surface, located just below the platform. This hump, known as the bulb of percussion, can be extremely variable in morphology, and can be significant in determining the angle of applied force and the type of hammer used to remove the flake. Application load typologies aid researchers hoping to classify these flakes derived from lithic reduction strategies involving hard-hammer percussion, soft-hammer percussion, or pressure flaking. By recording the difference between the thickness at the bulb of percussion and the midpoint of the flake, one can obtain the relative bulb size (Andrefsky 2005:119). This would be considered the application load, where larger values are indicative of hard-hammer percussion and smaller values are evidence of soft-hammer percussion.
The termination typology is divided into four classes: feather, step, hinge, and overshot
(Andrefsky 2005:Figure 2.8). The feather termination is characterized by a smooth tapered distal portion that “feathers” out upon detachment. When a flake snaps during detachment, causing the distal portion to be relatively flat and abrupt, it is a considered a step termination. The hinge termination is when the force of the impact causes the distal portion to be slightly angled and rounded, a result of the force of impact rolling away from the objective piece and not fully across the core surface (Andrefsky 2005:20). A plunging termination is found when the force of impact rolls towards the objective piece and travels farther down, creating a slightly hook-shaped termination.
Another way of analyzing where in the reduction stage a tool or nontool was removed is determining the cortex percentage, as the cortex is the first to be removed. Cortex can vary depending on how chemical and physical weathering has affected the stone surface, and its percentage (according to the area it covered on the dorsal surface) was recorded in a five rank 18 system: 0%, 0.1-10%, 11-49%, 50-90%, and greater than 90%. The raw material type of an artifact is a tremendously important aspect of stone tool manufacturing, and can provide a window into the behaviors of stone tool users across time. The materials in this lithic assembly were all made of chert, and the type was cross referenced with photos of diagnostic cherts of multiple types found in this region of the North American southeast: Suwannee, St. Marks,
Coastal Plains, quartzite, and other (unidentifiable macroscopically).
Burnt flakes show evidence of more intensive heat treatment, typically discernible through the appearance of surface cracks, called crazing, and circular concave scars on the surface caused by the differential expansion and contraction of the material, known as a pot lid
(Andrefsky 2005:260). Polish and rounding on flakes are signs of use, caused by the grounding of the tool margins or dorsal ridges (Andrefsky 2005:171). Retouch on a flake edge is a sign of reworking the edge to make it sharper or thinner, signified by retouch scraper or edge retouch flakes. Since this is a sign of post-detachment modifications, it is therefore likely a flake tool that was used to carry out some form of activity. Erailure scars are another way of identifying the striking platform (or where it may have been if crushed) and bulb of percussion, as these are small concave scars from a chip or flake located on the ventral surface below the platform and on the bulb. It is the product of the original impact of flake removal, and while not always apparent, it becomes a good identifier of other attributes and characteristics of the flake.
By using the Munsell Rock Color Charts each sample was given a general rock color.
This was not an extremely crucial aspect of the analysis being conducted but allowed for a look into the patterns of staining and rock colors of the lithic assemblage. The color of the ventral side of the flakes typically showcased the interior of the core or original material it was struck from, and could aid in providing very general means of identifying material type. If the majority of the 19 sample was stained a particular color, it would be assigned a color closest to that staining. This should be accompanied by other analytical techniques, but for the purpose of this analysis served as a way of identifying an overall trend in the color of the samples.
Flake Tool Analyses
Flakes identified as flake tools were separated into a separate category with a total of nine different attributes and characteristics recorded (Table 2). These artifacts would have already been measured for length, width, thickness, and weight. Rock color, cortex percent, raw material type, burning, polish, and eraillure scar presence were also recorded for these samples. Using a separate code sheet, the following attributes and characteristics were measured: tool blank, hafting wear, number of edges worked, retouched edge shape, retouch face and type, edge angle, total edge length, and worked edge length.
20
Table 2. Lithic analysis characteristics and attributes of flake tools.
Attribute/Characteristic Descriptions/Attributes/Characteristics Length (mm) Measured relative to maximum dimensions Width (mm) Measured perpendicular to length Thickness (mm) Measured at the thickest point of specimen Weight (g) Measured on digital scale Indeterminate, Core reduction flake, Blade, Tool Blank Biface thinning flake, Cortical spall None evident, Dulling/Polishing along edge, Hafting Wear Crushing/Polishing along dorsal ridges, Abrupt change in edge wear Number of Edges Worked Number of worked edges in total Indeterminate, Pointed, Straight, Concave, Retouched Edge Shape Convex Indeterminate, Unifacial, Bi-marginal, Edge, Retouch Face Alternating Indeterminate, Nibbling, Scaly with feathered Retouch Type terminations, Stepped Edge Angle <30°, 30°-60°, >60° Measured length of specimen edge that the Total Edge Length (mm) worked edge is located on Worked Edge Length (mm) Measured length of worked edge only In relation to Dorsal Surface: 0%, .1-10%, 11- Cortex Percentage 49%, 50-90%, 91-100% Suwannee, St. Marks, Coastal Plains, Raw Material Type Quartzite, Other (unidentifiable macroscopically) Burnt None, Present Use-wear analytics not as identifiable Polish/Rounding macroscopically Eraillure Scar None, Present Rock Color Assigned with Munsell Rock Color Charts
The tool blank refers to the type of flake it was when detached from its core. The origin
of the tool blank could provide information on the shape of the flake tool and even the attributes
that relate to tool function (Andrefsky 2005:162). The hafting wear involves aspects of tools that were fitted into a socket or notch on a haft. The descriptions here provide different ways a tool could be worked in order to properly fit into a haft and the effects that has on the tool itself in 21 terms of polishing, edge reworking, or other abrupt changes in edge wear. The number of edges worked is simply defined as such, and recorded as however many edges were modified. From
this identification of the worked edge, the subsequent analyses must involve each worked edge
specifically. Retouched edge shape provides details on the overall morphological shape of the
edge being worked, and is described as pointed, straight, concave, or convex. The face(s) of
retouch on a flake is described as unifacial, bi-marginal, edge (i.e. burin), and alternating. An
edge’s retouch face is unifacial if it occurs only on the ventral or dorsal surface. Bi-marginal is retouch happening on both surfaces of an edge in the same location, and alternating is bi- marginal retouch but separated on the ventral and dorsal surfaces. The edge retouch face distinction is noticeable with burins and burin spalls, as the worked edge is populated by small flaking concentrated toward a pointed margin that was used for chiseling. Due to retouch type being so variable, its identification was limited to a small number of descriptors. We recognized them as either nibbled, scaly, or stepped. Nibbling is retouch that is primarily in a marginal line with flake scars ending with feathered terminations. Scaly retouch also had feathered terminations but flake scars were extended slightly away from the edge and intersecting one another. The stepped retouch consisted predominately of flake scars along the edge that
terminated with step fractures. These are considered to be proxies for intensity of use and
retouch, with nibbling representative of lightest use and stepped indicative of intensive use or use
on hard surfaces (Andrefsky 2005:174).
The edge angle is determined on a basis of gross shape, and is recorded in three states:
angles less than 30°, angles between 30° and 60°, and angles greater than 60° (Andrefsky
2005:172). This measurement of edge angle is also considered a proxy for function and intensity
of use, but is difficult to capture and replicate, therefore it is necessary to be scored in a classified 22 continuum (Andrefsky 2005:175-176; Kuhn 1990). The total edge length is measured in millimeters along the maximum linear distance of the edge of the flake tool with retouch occurring on it. To take into account any curved or sinuous edges, this attribute is measured with a string, followed by measuring the string length that matched up with the tool edge. Similarly, the worked edge length is measured in the same way with a string, except the string is only contoured along the actual worked edge of a flake tool.
Biface and Core Analysis
Bifaces are tools that have undergone extensive modification, having flakes removed from both sides, called faces, which meet at one edge around the margins of the artifact. Bifaces can serve several purposes depending on the task at hand, be it as a core (a source of usable flakes), or as chopping and cutting tools (Andrefky 2005:178-179; Kelly 1988). The analyses done for the bifaces and core found in this Ryan-Harley assemblage were measured according to
12 additional attributes and characteristics: estimated completeness, missing portions, biface stage, planview shape, base type, cross-section type, dominate flaking type, end thinning, edge angles of side one and two, core type, and number of core flake scars (Table 3). This coding system has been used in lithic analyses before and is used here in order to keep the data comparable and compatible (Halligan 2012).
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Table 3. Lithic analysis characteristics and attributes of bifaces and cores.
Attribute/Characteristic Descriptions/Attributes/Characteristics Length (mm) Measured relative to maximum dimensions Width (mm) Measured perpendicular to length Thickness (mm) Measured at the thickest point of specimen Weight (g) Measured on digital scale Indeterminate, 100%, 75-99%, 50-74%, 25- Estimated Completeness 49%, 1-25% None, Base, Tip, Base/mid, Tip/mid, Missing Portions Indeterminate Early, Middle, Late, Point, Fragment, Core, Biface Stage Chopper, Adze Circular, Lanceolate, Ovoid, Straight, Planview Shape Triangular, Corner-notched, Side-notched, Random Concave, Ovoid, Rounded, Square, Corner- Base Type notched, Side-notched Cross-Section Type Bi-convex, Bi-plano, Plano-convex, Diamond Indeterminate, Edge only, To midline, Past Dominate Flaking Type midline, Some overshots, Random End Thinned None, Present Edge Angle Side One Less than 30°. 30°-60°, more than 60° Edge Angle Side Two Less than 30°. 30°-60°, more than 60° Multidirectional random, Bifacial, Core Type Unidirectional, Conical, Wedge-shaped Core Flake Scars One, Two, Three, Four, Five or more Cortex Present None, One face, Both faces Suwannee, St. Marks, Coastal Plains, Raw Material Type Quartzite, Unidentifiable Macroscopically Burnt None, Present Use-wear analytics not as identifiable Polish/Rounding macroscopically Will signify modification post flaking, Retouch therefore reflecting use life Rock Color Assigned with a Munsell Rock Color Charts
Estimated completeness of a biface is recorded as a percent in a five state system: 100%,
75-99%, 50-74%, 25-49%, and 1-25%. Missing sections of the tool are recorded depending on the absence of the tip or base, or if the majority of the medial portion is absent along with the tip 24 or base, that was recorded as well. The stage of the biface was determined by estimated completeness, resulting in early, middle, late, or point stages, or if broken it was a fragmented biface. If none of the formerly mentioned identifiers were appropriate, then the stage of a biface was also determined by its use as a core, a chopper, or an adze, the only categories encountered in this dataset (Halligan 2012).
The planview shape was the overall outline that the stage of the biface has, resulting in multiple distinctions: circular, lanceolate, ovoid, straight, triangular, corner-notched, side- notched, or random (Halligan 2012). Biface bases are crucial to their identification and have an important role in determining what culture complex its producer was a part of. Bases can be variously shaped, including concave, ovoid, rounded, square, corner-notched, and side-notched.
The morphology of the cross-section of a biface was also recorded, resulting in the identification of four types: bi-convex, bi-plano, plano-convex, and diamond shaped (Halligan 2012).
Dominate flaking type reveals the reduction processes the artifact has undergone, and are recorded as indeterminate, edge flaking only, flaking to (or past) the tool midline, overshots, and random assortments of flaking. End thinning appears in later stage bifaces, and usually around the base of said biface. This can reflect the type of percussion used to detach the flakes, the stage at which it was, and is often considered diagnostic of Paleoindian reduction strategies (Collins
2008). Edge angles were measured on both sides of the biface in the same three state scale used for flake tools.
Cores reflect the end product of a sequence of tool preparation, reduction of flakes, and the continued preparation and reduction of tools (Andrefsky 2005:144). Cores that are identified are assigned a typology involving the both the general reduction technique used on them and the overall shape if significant enough. These include multidirectional random flaking, bifacial 25 flaking, unidirectional flaking, or if the core is primarily conical or wedge-shaped. The number of flake scars on the core itself was also scored, going up to a distinction of five or more scars. It is important to keep track of and analyze the detached pieces (or what those detached pieces may have been) from a core because its morphology represents the last stage of usage, and is pertinent for understanding the course of core reduction (Andrefsky 2005:144).
A method of statistical analysis was used during this study that involved artifact diversity
indices. While mostly utilized in ecological studies, Simpson’s and Shannon’s Diversity Indices
can also allow us to quantify the diversity of an archaeological site. The formulas for these
indices are as follows:
Simpson’s Diversity Index:
( 1) D = ( 1) Shannon’s Diversity Index and Evenness:
H= - [ ln( )]