We are pleased to introduce a component of the TARL family, the
Center for Archaeological and Tropical Studies (CATS). The CATS
research facility is primarily focused in tropical Central America,
but has research interests in broader regions of the neotropics.
This interdisciplinary research unit has been operating for several
decades with a sister facility in Belize, the Programme for Belize
Archaeological Project (PfBAP). PfBAP research has been conducted on over 60 Maya sites within the research focus defined by the nature reserve covering 260,000 acres at the Rio Bravo Conservation and Management Area.
While this comment serves to Introduce CATS, forthcoming
newsletters will provide specific research interests and findings
of CATS as well as ongoing research right here at CATS Corner!
Serving as Director of CATS is Dr. Fred Valdez of the Department
of Anthropology (UT-Austin) and may be reached at
Over the past two years, the Houston Archeological Society (HAS) has been working with the Sam Houston Regional Library and Research Center in Liberty, Texas to assess the contents of the extensive Andy Kyle Archeological Collection currently curated at the Center. The collection was donated to the Center by the late Mr. Andy Kyle and consists of well over 30,000 artifacts collected from 95 sites in 9 Southeast Texas counties. One of the more prolific sites represented in the collection is the Savoy site (41LB27) located in northeastern Liberty County. Artifacts from the Savoy site range from Middle Archaic to Late Prehistoric, with an extensive collection from the Woodland period (Crook et al. 2017).
A number of exotic items are present in the site collections including two broken bannerstones made from lithic material not native to Texas, a broken boatstone, and a large partial bowl of the rare Lower Mississippian ceramic type Mabin Stamped, var. Joe’sBayou. Recently, several previously unknown boxes of material from the Savoy site were located by Ms. Alana Inman, Director of the Sam Houston Regional Library. In these boxes was a small, cone-shaped ceramic artifact which could not be readily identified. The artifact has been shown to a number of colleagues both from Texas and Louisiana without any success in identification. It is hoped that this short paper will prompt someone to contact the author and assist in the artifact’s identification and functional use.
The Savoy Site (41LB27)
The Savoy site is located approximately 4.2 km southwest of the community of Moss Hill in northeastern Liberty County. The site is bisected by County Road 2099 and hand written notes left by Mr. Kyle in the boxes of artifacts in the collection indicate that the unknown ceramic artifact described herein was found on the part of the site that occurs south of CR 2099, known locally as the “Stone Field” after the property’s original owner. The Savoy site is part of a series of four sites that occur parallel to one another along a 600 meter southeast-to-northwest stretch of land. Site 41LB26 lies 215 meters to the southeast; site 41LB28 is 225 meters to the northwest; and site 41LB29 is 400 meters to the northwest. All four sites contain similar cultural material ranging from the Middle Archaic to the Woodland period and into the Late Prehistoric period as well (Kindall and Patterson 1987; Crook et al. 2017). The nearest source of permanent water to the Savoy site is Knight’s Bayou, which is located 1.2 km to the west. Knight’s Bayou is a tributary of the Trinity River which currently lies 2.5 km to the west of the site.
The Savoy site was originally recorded in 1973 by the University of Texas during the Louisiana Loop Survey (Elton R. Prewitt, personal communication, 2019). A second survey was conducted in the mid-1980s by members of the HAS in conjunction with Mr. Andy Kyle who showed them where his artifacts were found (Kindall and Patterson 1987; Sheldon Kindall, personal communication, 2017). A third exploration of the area was conducted in 2014 by TRC Environmental Corporation as part of a pipeline right-of-way survey. TRC conducted 21 shovel tests over both the north and southern portions of the site. Nine of the 21 shovel tests contained cultural materials including a Gary point, an Alba point, and numerous ceramic sherds (TRC notes on file with the Texas Archeological Research Laboratory).
Occupational material at the Savoy site covers at least 0.7 acres today, however, based on information given to the HAS by Mr. Kyle, this area represents only about 20 percent of the original site size. Much of the site was destroyed by the construction of CR 2099 coupled with farming and house construction in the area (Sheldon Kindall, personal communication, 2017). Soils covering the area of the Savoy site belong to the Spurger-Bienville-Kennefick complex, specifically a mix of Bienville and Kennefick soils (Griffen 1996). The typical soil profile at the site consists of about 13 cm of a dark brown loamy fine sand underlain by 200+ cm of a very fine-grain dark yellowish-brown loamy sand (Griffen 1996). The artifact horizon extends to at least one meter or more in depth.
Artifacts from the site generally represent the following archeological periods: (1) Archaic – 6000-2000 B.P. (marked by Ellis, Yarbrough, Kent, Ensor, and Gary points), (2) Woodland phase – 2000-1400 B.P. (marked by Gary and Kent points and both plain and decorated sandy paste ceramics), and (3) Late Prehistoric 1400-500 B.P. (marked by Alba, Catahoula, Friley, and Perdiz points, and both locally manufactured and imported Caddo ceramics) (Crook et al. 2017; Suhm et al. 1954; Suhm and Jelks 1962; Turner and Hester 1985, 1993, 1999; Turner et al. 2011).
The Mystery Artifact
As mentioned above, the artifact in question is a cone-shaped ceramic made from a sandy clay paste. It appears that the object is intentionally made and has not been repurposed from a broken sherd. It has been well-fired and is not friable, unlike most of the Goose Creek type ceramics from the site. Color varies from very pale brown (10YR 7/3-7/4) to pale brown (10YR 6/3). Length of the cone is 36.0 mm (Figure 1). Width is 15.0 mm at the wide end tapering to 6.1 mm at the pointed end. A small perforation approximately 1.5 mm in diameter transits through the entire length of the artifact (Figure 2).
At the wide end of the cone, the end is recessed to a depth of about 8 mm. Examination under a under high power (20-80x) Dino-Lite AM4111-T digital microscope shows the walls of the recessed end are slightly darkened and there is some unknown black residue on one side (Figure 3). No other wear was observed. To date, none of the darkened material has been removed for potential chemical analysis.
The cone-shaped ceramic artifact described herein is not only unique among all the artifacts recovered from the Savoy site, it is also completely unique among the entire Andy Kyle Archeological collection. Most of the artifacts collected by Mr. Kyle from the Savoy site were found on the surface so any artifact association with the object is unknown. However, given the composition of the ceramic and the fact that similar sandy paste ceramics have been recovered from the site, it is likely that the cone-shaped object is Woodland in age. Elton Prewitt (personal communication, 2019) postulated that the object was of Mississippian origin which is certainly possible given the presence of bannerstones made from exotic materials and the Mabin Stamped, var. Joe’s Bayou bowl from the same area of the site.
As to function, this remains problematical. The most common suggestions given to the author by colleagues is that it is either a perforated ornament of some type or a type of tubular pipe. Neither explanation is convincing, especially give the very small diameter (1.5 mm) of the perforation. If anyone from the Texas archeological community has seen something similar, please contact the author at: email@example.com.
The author is grateful to Ms. Alana Inman, Manager of the Sam Houston Regional Library and Research Center in Liberty, Texas for inviting the Houston Archeological Society to participate in the development of the new prehistory exhibit at the Center and thus affording us the opportunity to study in detail all the artifacts contained in the Andy Kyle Archeological Collection. Alana not only provided open access to study the collection but also allowed for the study of artifacts outside the Center. I am also grateful to HAS colleague, Robert Sewell, who helped me take the high resolution digital photomicrograph which appears in this paper.
Crook, Wilson W., III, Robert J. Sewell, Linda C. Gorski and Louis F. Aulbach
2017 The Andy Kyle Archeological Collection. Report of the Houston Archeological Society, 29:13-56. Houston.
Griffen, Kirby L.
1996 Soil Survey of Liberty County, Texas. United States Department of Agriculture, Soil Conservation Service, in cooperation with the Texas Agricultural and Experiment Station and the Harris County Flood Control District.
Kindall, Sheldon and Leland W. Patterson
1987 The Andy Kyle Archeological Collection, Southeast Texas. The Journal 86:14-21. Houston Archeological Society, Houston.
Suhm, Dee Ann and Alex D. Krieger, with the collaboration of Edward B. Jelks
1954 An Introductory Handbook of Texas Archeology. Bulletin of the Texas Archeological Society 25:1-562.
Suhm, Dee Ann and Edward B. Jelks (editors)
1962 Handbook of Texas Archeology: Type Descriptions. Special Publication No. 1, Texas Archeological Society and Bulletin No. 4, Texas Memorial Museum.
Turner, Ellen Sue and Thomas R. Hester
1985 A Field Guide to Stone Artifacts of Texas Indians. Gulf Publishing, Lanham, Maryland.
1993 A Field Guide to Stone Artifacts of Texas Indians. 2nd Edition. Gulf Publishing, Lanham, Maryland.
1999 A Field Guide to Stone Artifacts of Texas Indians. 3rd Edition. Gulf Publishing, Lanham, Maryland.
Turner, Ellen Sue, Thomas R. Hester, and Richard L. McReynolds
2011 Stone Artifacts of Texas Indians. Taylor Trade Publishing, Lanham, Maryland.
Myself and Caroline Znachko, Ph.D. students from the University of Tennessee – Knoxville, have been collecting skeletal data from the Ernest Witte mortuary site. The site is an Archaic cemetery from east-central Texas and was utilized by a semi-sedentary indigenous group between 2,700 B.C.E. and 1,500 C.E. The Archaic period is known for increasing population and drastic climate change in Texas. This information, coupled with an analysis of the developmental timing of linear enamel hypoplasia (LEH), leads to a meaningful consideration of the impact of a changing environment on the life course of Middle and Late Archaic Texas hunter-gatherers. Out of 191 individuals analyzed, 40 were affected by LEH with more males affected than females overall. Age-at-formation analyses indicate a slightly earlier first age-at-onset of LEH for females than males and an earlier age-at-onset for young adults. These results provide further insight into populational patterns of the skeletal embodiment of early childhood stress in hunter-gatherers and can offer additional insight into health and stress patterns in the Texas Archaic.
We were invited to present this research by Marybeth Tomka at the TARL Renovations, Rehabilitation, Reorganization, and Research symposium at the 2018 Texas Archeological Society meeting and have recently offered a workshop through TARL to train students in dental pathology data collection. In the future, we plan to work with TARL to offer more workshops like this for students of all experiences completely free!
In addition, through this workshop, we identified two students with strong potential for future success in the field. These students are helping us to collect more LEH data from the Morhiss site and Crestmont site this summer. They will be collecting their own data and asking their own research questions as well and will be presenting posters at next year’s conferences on dental abscesses, caries, and their relation to LEH. Our aim is to ultimately yield research that helps with our understanding of the climate change and population increase that occurred during the Texas Archaic.
1981 Allens Creek: A study in the Cultural Prehistory of the Lower Brazos River Valley, Texas. Texas Archeological Survey Research Report NO. 61, The University of Texas at Austin.
In the June, 2018 issue of this newsletter, I reviewed some of the reasoning and methods that underpin paleoenvironmental research involving snails, and I pointed out that the southwestern quadrant of Texas (basically, west of longitude 100º W and south of latitude 32ºN) is almost a blank slate for archeomalacologists. We know that the better-watered eastern half of the state often produces abundant and informative snail faunas from sites in alluvial deposits, but what about sites in dryland alluvial settings? Dryland floodplains often lack fringing gallery forests and are essentially open habitats with high insolation, constant exposure to wind, and a conspicuous lack of leaf litter from deciduous tree canopy. Trees, if present at all, are likely to be represented only by scrub brush. Woody species in desert settings tend to be small-leaved, because high insolation makes photosynthesis very efficient, so leaf litter is often scarce or absent. Ground cover may be sparse, unless there is good grass cover in wet years, or rock rubble in sloping areas. Conditions like these are challenging for snails, which are highly moisture-sensitive.
One of the earliest studies in the state was done by Cheatum (1966) as part of the Amistad paleoecological project at Eagle Cave, Bonfire Shelter, Devil’s Mouth, and Devil’s Rockshelter, but the number of samples, volumetric size of samples, and number of specimens are not disclosed and intrasite provenience is reported only by stratum. In the entire vast area of the Big Bend (more than 12,300 square miles, not counting parts of Culberson, Hudspeth, and Reeves counties), no formal archeomalacological studies have been done until recently, as far as I know.
The Genevieve Lykes Duncan site (41 BS 2615, Early Holocene to present, Brewster County)
This site lies 54 km south of Alpine, toward the western side of the sprawling O2 Ranch, a 272,000-acre ranch that actually sprawls over into Presidio County (Fig. 1). This is the eastern part of the Basin and Range province, and the site sits at the north end of Green Valley, on an interfluve between Terlingua Creek and Davenport Draw. Both streams have contributed sediment in the past, and the deepest component consists of stratified Late Paleoindian (Early Holocene) occupations: sparse artifact scatters associated with rock-lined hearths or small earth ovens. An earlier occupation at about 10,400-11,080 cal BP lies about 2.3 to 2.5 m below the ground surface, with two rock-lined features, and five smaller rock-lined features dating about 8630-9535 cal BP are somewhat later. There are also two undated (but presumably Late Paleoindian) features that lack charcoal. As of 2016, at least 11 features had been found exposed in the walls of the recent arroyo that revealed the site, over a distance of about 24 meters (since then, three more have been found). There are also a few Middle and Late Holocene features exposed in more distant parts of the arroyo (Cloud et al. 2016:Fig. 6).
An extensive series of radiocarbon assays (chiefly on saltbush, mesquite, and creosote charcoal) ranging from 7934±25 to 9545±25 RCYBP places these Late Paleoindian occupations in the Early Holocene; Cloud et al. 2016:Table 2). These early occupations are buried by Allostratigraphic Unit 1, a thick deposit of clay loam that began accumulating sometime before 10,730 RCYBP and continued until the Middle Holocene. The Paleoindian deposits lie in a dark paleosol bracketed by two sheet gravel deposits (the lower one probably laid down by Terlingua Creek and the upper one by Davenport Draw; Cloud et al 2016:27). Allostratigraphic Units 2 (Middle to Late Holocene) and 3 (Late Holocene) overlie this unit. There is a series of global post-Younger Dryas cold events that punctuate the Early Holocene, but for the most part they do not seem to correspond to the Paleoindian occupations here, which follow the Preboreal Oscillation and precede the well-known 8200 cal cold event.
In July, 2013, I visited the site for several days with the auspices of the Center for Big Bend Studies, and with the assistance of Sam Cason (who did most of the work), collected a continuous column of matrix samples 60 cm wide and 2.74 m high from the southeast wall of the arroyo, immediately adjacent to the main excavation block (Fig. 2). The original plan was to collect samples in 5 cm increments, but the clay and silt-rich alluvium was so thoroughly indurated that this proved impossible, so the sampling interval was increased to 10 cm. Altogether 30 samples were collected (there are two extra samples because intervals were subdivided where stratigraphic breaks were crossed). The lowest sample cut only 10 cm into the lower gravel deposit (Fig. 2). This level is unassayed, but Andy Cloud (personal communication) estimates it dates to about 10,200 RCYBP, based on assays from the adjacent excavation block. Thus, the sample column documents the entire span of the Holocene (including the Late Paleoindian component), but presumably includes no Younger Dryas sediments.
In all, 465.6 kg (about half a ton) of sediment was collected. For the entire column, the mean sample size processed was 14.3 liters (range, 13-15 liters) and the mean analyzed weight was 15.05 kg; the total weight of sediment used in the analysis was 451 kg (a few samples had excess amounts). Samples were soaked overnight in tapwater, then passed through nested 18-inch geologic sieves with mesh sizes of 2 mm, 1 mm, and 0.5 mm. Residue from each grade was dried and bagged for picking. All snails, snail shell fragments, charcoal, seeds, animal bones, and possible microdebitage were saved and counted or weighed. After picking, the remaining residue was turned over to Brittney Gregory for heavy mineral separation studies at LSU.
Despite the fact that nearly half a ton of sediment was processed, only 843 specimens (many of them damaged or fragmentary) were recovered. This amounts to a density of only about two specimens per liter of sediment, compared to about 10-130 per liter from other sites in the eastern half of Texas where the same methods have been used. There are only four kinds of terrestrial snails: Succineidae, Gastrocopta pellucida, Helicodiscus singleyanus (= Lucilla singleyana), and Pupoides albilabris. The Succineidae are unidentified. Although succineids are usually considered to be wetland fringe inhabitants, there are perhaps a couple of borderland species (Succinea luteola and S. solastra) that are found in arid upland areas. Thus, it is not clear whether the succineids indicate wet or dry conditions (but perhaps the latter). There are only two kinds of aquatic snails: a planorbid, believed to be juvenile Planorbella trivolvis, and Physa sp., probably Physa acuta. A few examples of a third aquatic species, Gyraulus parvus, was not found in the sample column but was recovered in wet-screening by the field crew.
All of these snails are resilient habitat generalists, and all appear to be very arid-tolerant species (although the identity of the succineids is uncertain). Almost all the Succineidae, the Helicodiscus, and the aquatic snails are juveniles, hinting at high juvenile mortality. Generally speaking, the aquatic taxa are tolerant of sluggish, poorly oxygenated, warm water with high solute levels. All of the aquatic snails are confined to the bottom half of the column, disappearing in the upper gravel, just before the midpoint of the Holocene; otherwise, the same kinds of snails are found throughout the column, although fluctuating in abundance.
The Genevieve Lykes Duncan snail assemblage is characterized by low specimen density, low taxonomic diversity, apparently high juvenile mortality for many taxa, and a preponderance of arid-tolerant, resilient habitat generalists. When I began sampling this site, I expected to find lingering evidence of greater moisture conditions from the Younger Dryas at the base of the column. My expectation was that despite mounting aridification in the Early Holocene, one or two samples at the base of the column would yield greater numbers of snails, more diversity, and perhaps some taxa that are more moisture-dependant. This proved not to be the case. Instead, the snail assemblage suggests local conditions were already arid by the start of the Holocene. This is consistent with the saltbush, mesquite, and cholla identified in charcoal, and the Cheno-Ams, Artemisia, thistle, Asteraceae, and Ephedra identified in a pollen sample overlying Feature 1 (Cloud et al. 2016:55-56). My sampling stopped in the top of the lower gravel (a depositional event that might signal significant climatic reorganization), and if there is an assemblage adapted to wetter conditions, it must lie in the unsampled sediments under that gravel bed.
The Sayles Adobe site (41 VV 2239, Late Holocene, Val Verde County)
In May, 2016, I visited the Sayles Adobe site in Eagle Nest Canyon (Fig. 3) near Langtry. Eagle Nest Canyon is a narrow, deep, rock-floored canyon that drains southward into the Rio Grande, and two famous sites, Eagle Cave and Bonfire Shelter, lie farther upstream in the canyon. Sayles Adobe is a sandy terrace site that sits perched high (about 11 meters) above the canyon floor not far from the confluence with the Rio Grande. It sits at the foot of the talus slope descending from Skiles Shelter (41 VV 165) and may have served as an adjunct area during the occupation of that site. Tori Pagano, a Texas State University graduate student, has been excavating Sayles Adobe for her MA thesis in geoarcheology, and my report on the snails is to appear as an appendix in her thesis. Tori collected a discontinuous series of eight pilot samples for me from two separate excavation blocks, representing about a 2500-year span of the Late Holocene. Here, instead of a continuous column, the goal was simply to find out if microsnails were present in these sediments, and if so, what kind and in what quantity.
The thick package of alluvium at this site consists of sandy sediments derived from limestone terrain in the canyon watershed, along with some fine-grained sediments (including mud drapes) contributed by backflooding from the nearby Rio Grande. Two of the samples were box-shaped removals 20 cm thick (“borrow pit” block), and six were 22-42 cm in thickness (“sandbox” block; Fig. 4). The samples come from two separate excavation blocks and represent a maximum elevation difference of about 2.9 m. These samples cover about a 2500-year span of the Late Holocene, from about 3167 cal BP at the lowest sample to a point somewhat later than 675 cal BP for the uppermost sample (Tori Pagano, personal communication 2018). This uppermost sample, at about 1275 AD, occurs well into the Medieval Climatic Anomaly. Sedimentation rates were high at this site. An Early Holocene radiocarbon assay of 8236±34 RCYBP was obtained on guajillo charcoal from an auger test at a depth of 5.7 m, so there are sediments equivalent in age to the Lykes Duncan site, but no excavation or snail sampling has been done at this depth. Late Holocene sedimentation rates were evidently high at this site, so the unusually thick samples obtained (up to 42 cm) probably do not imply much time-averaging.
For the 8 pilot samples, average volume was 12.7 liters (range, 11.3-15.0). The processing methods used were the same as those at the Lykes Duncan site. From the 101.35 liters of sediment processed, only 559 specimens were recovered; almost 81% of these came from the 0.5 mm mesh sieve. Specimen density is fairly low, about 5.51 specimens per liter. This is much lower than the 15.7 specimens per liter at Bonfire Shelter, doubtless reflecting the much higher depositional rates at Sayles Adobe. Low specimen density could be a result of poor habitat quality, the diluting effect of rapid sediment deposition, or both.
The samples produced one adult Rabdotus (species indeterminate), three juveniles, and some spires of indeterminate age. Other than this, the snail fauna is very similar to that from Genevieve Lykes Duncan. The assemblage includes Gastrocopta pellucida adults and juveniles, Succineidae adults and (mostly) juveniles, Helicodiscus singleyanus (Lucilla singleyana) of indeterminate age, a few Pupoides albilabris adults, and perhaps two aquatic species: small, mostly juvenile snails tentatively identified as Gyraulus parvus (but with a somewhat anomalous shape), and two small planorbids that look different from Gyraulus (an embryo and a columellar fragment) and suggest the possibility of one or more different species.
Except for the presence of a few Rabdotus and the absence of Physa, this assemblage is much the same as that at Genevieve Lykes Duncan. The succineids are mostly very tiny embryos, and I suspect represent one of the two upland, arid-adapted species in the Succineidae family.
Overview: Snails in Dryland Alluvium
These two sites differ in many ways. Genevieve Lykes Duncan lies in an open, lowland basin at about 1180 meters, in sediments generated from igneous and metamorphic bedrock, and spans the entire Holocene, at the confluence of two meandering, unconstrained streams. Sayles Adobe lies in a narrow, rock-floored limestone canyon at 350 meters, partially sheltered from wind and insolation, with samples that are limited to the Late Holocene (although older but unsampled sediments are at the base), with sediments produced both by limestone bedrock terrain and by Rio Grande backflooding (although the there seems to be no particular evidence of a Rio Grande influence in the snail assemblage).
Annual precipitation is similar in the two areas, but it is distributed differently. At Langtry under the current climatic regime, it is about 37.26 cm/year (based on 1981-200 normals) with 32% occurring in the summer. There is no permanent weather station on the O2 Ranch, but average annual precipitation was about 36 cm in 1914-1928, and 42 cm in 2015-2016. May to October are the wettest months, with August the peak, and 44% of precipitation occurring in the summer months (June to August). Insolation rates are very high here and evapotranspiration exceeds precipitation for 11 out of every 12 months. Although the antiquity of the North American Monsoon system is not entirely certain, Genevieve Lykes Duncan participates in this system today, receiving Pacific moisture, often from convectional thunderstorms, mostly in the summer, when plant growth and snail activity are enhanced, but evaporation rates are higher. Sayles Adobe lies farther east and receives more moisture from the Gulf of Mexico, so its precipitation pattern is a hybrid of the West Texas monsoon pattern and the bimodal eastern Texas pattern of rainfall peaks in May and September. At Langtry, April-May and September-October are the rainiest months, but significant rainfall also occurs in June-August (Fig. 5).
Despite these differences, both sites have similar snail assemblages, characterized by low specimen density, a very limited range of resilient, arid-adapted taxa, and apparent high juvenile mortality in some of the species. Both assemblages seem to indicate arid, drought-prone (and probably variable) conditions that only resilient habitat generalists can tolerate. These findings raise an interesting question: if the fauna consists entirely of resilient habitat generalists, can we rely on it to register small-scale fluctuations in past climates? In faunal studies, it is often the rare, infrequent species with specialized habitat preferences that carry the most paleoenvironmental information payload. If none of these are present, can we rely on fluctuating specimen counts to indicate changing environmental conditions?
We probably need to apply the FRIN principle (Further Research Is Needed).
Cheatum, E. P.
1966 Report on Mollusk Shells Recovered From Four Archeological Sites in the Amistad Reservoir. Pages 227-243 in Dee Ann Story and Vaughn M. Bryant, Jr. (assemblers), A Preliminary Study of the Paleoecology of the Amistad Reservoir Area. Final Report of Research Under the Auspices of the National Science Foundation (GS-667).
Cloud, William A., Richard W. Walter, Charles D. Frederick and Robert Mallouf
2016 Late Paleoindian Occupations at the Genevieve Lykes Duncan Site, Brewster County, Texas. The Journal of Big Bend Studies 28:1-82. Center for Big Bend Studies, Alpine.
Manuscripts Resulting from This Research
Brown, Kenneth M.
n.d.a Analysis of a Column of Snail Samples from the Genevieve Lykes Duncan Site. Manuscript in progress, estimated length about 80 pages, to be published by the Center for Big Bend Studies.
n.d.b Appendix G: Pilot Sampling of the Snail Fauna at Sayles Adobe. Appendix to appear in
MA thesis (2019) by Victoria Pagano, Texas State University, estimated length about 25 pages.
The A. C. Saunders site (41AN19) is an important ancestral Caddo settlement in the upper Neches River basin in East Texas (Figure 1a). The site is one of only a few ancestral Caddo sites with mound features in the upper Neches River basin, particularly those that are known to date after ca. A.D. 1400, but this part of the upper Neches River basin, including its many tributaries, such as Caddo Creek just to the south and west (see Perttula and Walters 2016), was widely settled by Caddo farmers after that time. These Caddo groups left behind evidence of year-round occupied settlements with house structures, middens, and outdoor activity areas, impressive artifact assemblages, as well as the creation of numerous cemeteries (Figure 1b), most apparently the product of use by families or lineage groups.
Figure 1. The A. C. Saunders site in the upper Neches River basin: a, important excavated Caddo sites in the Caddo Creek valley and surrounding drainages in Anderson and Henderson counties, Texas; b, known Caddo cemetery and domestic sites.
What makes the A. C. Saunders site unique in upper Neches River basin Caddo archaeology are the two mound features there, situated on a broad upland landform less than a mile west of the Neches River and a comparable distance north of the confluence of Caddo Creek with the Neches River. The first mound (Feature 1) is an ash mound that has been linked with the use of fire temples and perpetual fires by the xinesi of Hasinai Caddo groups in historic times (Jackson 1936; Kleinschmidt 1982, 1984; Perttula 1992; Wyckoff and Baugh 1980). The second mound, not far to the southeast (Figure 2a), is a thick midden mound (Feature 2) that was deliberately accumulated over a large structure (Feature 3, Figure 2b). The concentrated midden accumulation near the ash mound suggests it may represent the remains of multiple feasting events and other ritual activities where large amounts of food were consumed, clay pipes were smoked, and cooking and serving vessels were used, and thus the discarded fragments of these activities creating the midden deposits. These items constitute a discrete and substantial corpus of material culture remains that have played a large role in defining and framing the archaeological character of what has come to be known as the Late Caddo period Frankston phase (ca. A.D. 1400-1680); the A. C. Saunders site is the quintessential Frankston phase site in East Texas. As such, these material culture remains curated at the Texas Archeological Research Laboratory at The University of Texas at Austin—in particular the large number of ceramic vessel sherds and ceramic pipe sherds from Feature 2 at the A. C. Saunders site—warrant continued archaeological study as a means to better understand the stylistic and technological character of the ceramic vessels and pipes made and used by ancestral Caddo peoples in the upper Neches River basin (Perttula 2011, 2013, 2019). The remainder of the material culture assemblage included Perdiz arrow points, stone drills, mussel shell digging tools, an assortment of bone tools (awls, needles, and beamers), and shell columnella beads.
Figure 2. A. C. Saunders site: a, plan map of the site; b, plan map of Feature 3 underneath the midden mound.
Ceramic Vessel Sherds
A total of 7344 ceramic sherds have been recovered from Feature 2 at the A. C. Saunders site from plain ware, utility ware, and fine ware vessels; of these, approximately 82 percent (n=6001) are from a known arbitrary level in Feature 2. The plain rim, body, and base sherds comprise approximately 21 percent of the vessel sherd assemblage, and the fine ware sherds account for another 8.8 percent of the assemblage. Utility ware sherds are by far the most common in Feature 2 at the site, representing approximately 70 percent of the ceramic wares. The plain to decorated sherd ratio for the Feature 2 assemblage is a low 0.27.
Defined utility ware types identified in the ceramic vessel sherds (from jars) include Bullard Brushed, Killough Pinched, La Rue Neck Banded, Lindsey Grooved, and Maydelle Incised, as well as sherds from two new types: Mann Punctated (with tool punctated elements on the rim and /or body), and Saunders Punctated (with fingernail punctated elements on the rim and/or body). Based on the number of rim sherds, the most common utility wares are Maydelle Incised (n=64, Figure 3a), Bullard Brushed (n=56, Figure 3b), Saunders Punctated (n=38, Figure 3c), and Mann Punctated (n=26, Figure 3d).
Figure 3. Common utility ware types at the A. C. Saunders site: a, Maydelle Incised; b, Bullard Brushed; c, Saunders Punctated; d, Mann Punctated.
The fine ware sherds are from carinated bowls primarily from a number of varieties of Poynor Engraved (n=68 rim sherds), particularly var. Cook (n=32 rim sherds) (Figure 4a) and var. Hood (n=13 rim sherds) (Figure 4b), as well as Hood Engraved and Hume Engraved vessels. The predominance of var. Cook and var. Hood vessels suggests that Feature 2 at the A. C. Saunders site accumulated between the early 15th century and the mid-late 16th century (see Perttula 2011:Table 6-37). Hood Engraved effigy bowls were also most commonly manufactured by Caddo potters during that era in the upper Neches River basin.
Figure 4. Most common Poynor Engraved varieties at the A. C. Saunders site: a, var. Cook; b, var. Hood.
The sherds from the A. C. Saunders site are from vessels tempered almost exclusively with grog (i.e., fired clay and/or crushed sherds). Between 98.3-98.6 percent of the sherds by ware have grog temper inclusions. Other temper inclusions, such as burned bone and hematite, were commonly added to the grog-tempered paste, and with regularity in the case of hematite in all three wares (11.7-21.1 percent). The few sherds in the different wares that have crushed and burned bone range from 9.1 percent in the plain wares, 9.9 percent in the utility wares, and 9.0 percent in the fine wares.
In addition to the 7300+ sherds from plain ware, utility ware, and fine ware vessels, there are other distinctive characteristics of the Frankston phase assemblage at the A. C. Saunders site. These include strap and lug handles (n=85) on utility ware jars, pedestal legs and bases (n=13) from Killough Pinched jars, spindle whorls (n=29), and one ceramic bead.
Ceramic Pipe Sherds
The A. C. Saunders artifact assemblage from Feature 2 has one complete ceramic pipe and 89 stem and bowl sherds. These pipes are from several defined pipe varieties in the upper Neches River basin (see Perttula 2011). Two of the pipe sherds in the assemblage are part of two different circular platform pipes that have either a series of upper and lower large excised pendant triangles or hatched engraved triangles on either side of the platform.
The remainder of the ceramic pipes and pipe sherds are from elbow pipes, including sherds from Var. A (n=7), Var. B (n=16), Var. C (n=5), Var. D (n=1), and Var. G (n=14), the Neches pipe (Jackson 1933). Another 45 sherds cannot be assigned to a defined Upper Neches River basin elbow pipe variety.
The Var. A elbow pipe sherds have plain stems and bowls. They range from at least 64-76.0 mm in length, have smoothed exterior surfaces, and have rounded lips; one Var. A pipe has a flat distal knob. Var. B elbow pipes have between two to six horizontal incised or engraved lines on the stem (Figure 5a), and several examples also have horizontal incised lines on the lower bowl and stem or the distal stem knob, or engraved lines on the pipe bowl.
Figure 5. Selected ceramic pipe sherds and pipes from the A. C. Saunders site: a, Var. B. pipe sherd (No. 62); b, Var. C pipe sherd (No. 14); c, Var. G pipe (No. 50) with punctated rows on the collared bowl rim, at the stem, and at the lower stem.
Four of the Var. C pipe sherds have two to five horizontal incised lines on the stem as well as vertical incised lines on the lower stem (see Figure 5b). One pipe sherd has both horizontal and vertical incised lines on the stem as well as a row of tool punctations adjacent to the vertical incised lines. The one Var. D elbow pipe sherd in the A. C. Saunders assemblage is grog-bone-tempered and smoothed on its exterior surface. The stem is decorated with five horizontal incised lines while the lower stem has at least two vertical rows of tool punctations.
The Var. G elbow pipes and pipe sherds have several different decorative element combinations, including incised or engraved lines on the stem between punctated rows beneath the lip or with rows of circular punctations on the lower stem. Other Var. G pipes have punctated rows on the stem or on the lower stem, or have tool punctated rows on both the stem and lower stem. The one complete Var. G elbow pipe (see Figure 5c) is decorated on the bowl, the stem, and the lower stem. There are small circular punctated rows on the bowl lip, five rows of circular punctations at the base of the stem and bowl, and five rows of circular punctations on the stem below the lip. Several of these circular punctations have a kaolin-rich clay pigment rubbed in the punctations.
Jackson, A. T.
1933 Some Pipes of East Texas. Bulletin of the Texas Archeological and Paleontological Society 5:69-86.
1936 A Perpetual Fire Site. Bulletin of the Texas Archeological and Paleontological Society 8:134-174.
1982 Review and Analysis of the A. C. Saunders Site, 41AN19, Anderson County, Texas. Master’s thesis, Department of Anthropology, The University of Texas at Austin.
1984 The A. C. Saunders Site Revisited: A Hasinai Fire Temple? Paper presented at the 26th Caddo Conference, Nacogdoches.
Perttula, T. K.
1992 “The Caddo Nation”: Archaeological & Ethnohistoric Perspectives. University of Texas Press, Austin.
2011 The Ceramic Artifacts from the Lang Pasture Site (41AN38) and the Place of the Site within an Upper Neches River Basin Caddo Ceramic Tradition. In Archeological Investigations at the Lang Pasture Site (41AN38) in the Upper Neches River Basin of East Texas, assembled and edited by Timothy K. Perttula, David B. Kelley, and Robert A. Ricklis, pp. 145-320. Archeological Studies Program Report No. 129, Texas Department of Transportation, Environmental Affairs Division, Austin.
2013 Caddo Ceramics in East Texas. Bulletin of the Texas Archeological Society 84:181-212.
2019 East Texas Caddo Ceramic Traditions. In Ancestral Caddo Ceramic Traditions, edited by D. P. McKinnon, J. S. Girard, and T. K. Perttula. Louisiana State University Press, Baton Rouge, in press.
Perttula, T. K. and M. Walters
2016 Caddo Archaeology in the Caddo Creek Valley of the Upper Neches River basin, Anderson and Henderson Counties, Texas. Special Publication No. 43. Friends of Northeast Texas Archaeology, Austin and Pittsburg.
Wyckoff, D. G. and T. G. Baugh
1980 Early Historic Hasinai Elites: A Model for the Material Culture of Governing Elites. Midcontinental Journal of Archaeology 5:225-283.
Erin is a Master of Science in Information Studies student working on a data management project in the human osteology collection. Erin’s undergraduate degree in anthropology sparked an interest in forensic science and she was eager to engage with a physical collection that touched on her information studies coursework, specifically records management and conservation. In an effort to help fulfill the federal law NAGPRA (the Native American Graves Protection and Repatriation Act), she is assisting in processing
the original records from the burial excavations as well as subsequent skeletal analyses to promote research access and to facilitate the repatriation of the human remains to extant Native tribes. A portion of the paper records will be digitized and linked so that original data can be accessed and viewed by researchers through a searchable database interface. We congratulate Erin on her pending graduation at the end of the summer!
Megan Steele and Sam Lowrance
Congratulations to our two recent Masters graduates from the Master of Science in Information Studies program! TARL has had the pleasure of working with Megan Steele and Sam Lowrance as they both complete their Capstone professional experience and project focused on the digitization of records and photographs from the 1930’s excavations and surveys conducted under the Works Program Administration. We are further pleased to announce that Megan Steele will continue to work with us here at TARL as our new archival Curatorial Assistant! We are excited to see what wonderful work both Sam and Megan go on to do!