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EVIDENCE FOR OLDER-THAN-CLOVIS AT THE GAULT SITE, TEXAS
Michael B. Collins with contributions by Sergio Ayala, Bruce Bradley, Steve Forman, Charles Frederick, Jennifer Gandy, Anna Gilmer, Robert Lassen, Brendan Nash, Jill Patton, Linda Perry, Jack Rink, Marilyn Shoberg, Charles A. Speer, Clark Wernecke, Tom Williams, and Nancy Velchoff
Figure 1. Regional setting of the Gault
site, Texas (41BL323)
Figure 2. Gault site map showing location of Area 15
and the positions of 2002 and 2007 test units
Figure 3. Photograph of a portion of the west wall of excavated
block in Area 15 with the approximate vertical distributions of
time-diagnostic artifacts as observed during excavation. The
excavation is ca. 3.6 meters deep, necessitating the stepped
excavation shown here
CLOVIS FIRSTERS—READ THIS:
An underlying question in this project is, does this site meet the criteria for acceptance as evidence
of “preClovis?” At Gault, there is no doubt that the more than 16,000 Older-than-Clovis artifacts are
of human manufacture; though sparse and poorly preserved, all fauna from the OTC component are
extinct Pleistocene species (horse and mammoth); there are more than 2.5 meters of alluvium with
stratified Clovis and younger components overlying this component; in places there is a break in
artifact frequencies immediately below Clovis before increasing again in the OTC deposit;
preliminary OSL dating of OTC includes two results (11-03, 11-04) that appear to be reversals, that
in fact, date fill in an disturbance (root?) and cut-and-fill feature and two results (11-05b, 11-06) that
we consider incongruously old (further efforts at dating are underway); luminescent dates above
OTC are in correct stratigraphic order, and are consistent with age estimates based on time-
diagnostic artifacts; numerous professional archaeologists witnessed and/or participated in this
excavation at all stages and a few have also been part of the laboratory analyses; multiple lines of
evidence indicate that downward movement of artifacts has been minimal; and, other than the OTC
blade technology, which is similar to that of Clovis, there are no technological or typological
continuities between the lower component and Clovis, nor any typological counterparts to the OTC
Figure 4. Bivariate plot of optically stimulated
luminescence dates by depth and cultural time
periods.
Figure 5. Synoptic geologic profile of west
wall of Area 15 excavation from elevations
92.05m to 93.55 m with the approximate
boundaries of the Clovis and Older-than-
Clovis components (from Gilmer 2013).
Figure 6. Comanche Peak limestone bedrock as
exposed in the floor of the Area 15 excavation
block. Fluting is interpreted as the result of
protracted stream flow of ancestral Buttermilk
Creek across the bedrock surface under three
different orientations of the stream, earliest
(green), intermediate (blue), and latest (red).
Photo by Gregg Cestaro.
Figure 7. Area 15 cultural chronology based
on time-diagnostic artifact distributions and
plotted against the available luminescent
dates.
Figure 8. 3-D plot of Clovis (green) and Older-
than-Clovis (red) artifacts, bedrock (gray), and
large limestone rocks (blue) in the lower 2
meters of excavated Area 15 (view is looking
south). Clovis artifacts are a point, blades,
diagnostic debitage, bifaces, core, and unifaces.
Older-than-Clovis component artifacts lacking
established age assignments consist of
potentially time-diagnostic blade cores, blades,
tools on blades, bifaces, flake cores, and tools
on flakes. The anomalous pile of large,
irregular limestone rocks measures 108 cm E-
W, 79cm N-S and 51cm high, consists of clasts
up to 35 cm across and 15 cm thick and lacking
in stream rounding, partly supported by soft
sediment, and neither clearly natural nor
human-made. A few non-diagnostic flakes
were present throughout. Stratigraphically, it
extends downward from the base of the Clovis
component through most of the underlying
deposits.
Figure 9. Vertical distributions of flakes by weight and
count below 93.00m elevation in the Clovis and Older-
than-Clovis components (modified from Gilmer 2013).
Figure 10. Backplot of diagnostic Andice,
Bell notching flakes, debitage, and point
fragments. At ca.6,000-5900 B.P. this is the
earliest Middle Archaic interval of Central
Texas.
Figure 11. Comparison of
representative Clovis and Older-
than-Clovis artifacts indicative of
blade technology.
Figure 12. Comparison of
representative Clovis and Older-
than-Clovis artifacts indicative
of biface technology.
Figure 13. Comparison of
representative Clovis and Older-
than-Clovis artifacts indicative of
flake technology.
Excavations, 2007-2014, in Area 15 of the Gault Site (Figures 1, 2) specifically targeted evidence
for an Older-Than-Clovis (OTC) occupation seen in two test units in 2002 and 2007 (Figure 2).
Excavation of a large block penetrated 3.5 meters from the surface to bedrock (Figures 3-6) through
culture-bearing alluvial fill. Physical and cultural stratigraphic evidence as well as luminescent dating
are consistent in showing a coherent sequence of Older-than-Clovis, Clovis, Late PaleoIndian, Early
Archaic, and Middle/Late Archaic occupations over an apparent span of more than 14,000 calendar
years (Figures 4, 7-9). This effort addressed seven specific questions: (1) What is the context and
integrity of the Clovis component? This component, roughly 35 cm in thickness, rests in largely
undisturbed alluvial deposits of high integrity (Figure 5). Twenty nine diagnostic stone artifacts and
30,000 waste flakes were recovered. (2) What is the depositional context and integrity of the underlying
component? This component, roughly 80 cm in thickness, is in minimally disturbed water-lain deposits
that yielded 45 formal artifacts and 16,000 waste flakes (Figures 5, 8). There is good separation
between Clovis and underlying material across 10 of the 12 excavated squares, but clearly some mixing
in one limited area; there is also an unexplained, anomalous stone pile near the eastern margin of the
excavation, extending downward from the base of the Clovis component (Figure 8). (3) What is the
nature of an apparent depositional discontinuity between the Clovis-bearing deposit and the one below
it? This discontinuity (Figures 5, 8, 9) is characterized by a decrease in artifacts and an increase in soil
carbonates in the 10 to 15 cm below Clovis, which appears to indicate a reduction in human activity and
possibly an environmental change. (4) What is the age and duration of the earlier component?
Preliminary luminescent dates on soils suggest an age range from greater than 14,000 to near 13,200
years for the early component (Figures 4,7,8). (5) What does the earlier assemblage indicate about
adaptive behavior? Details are lacking, but broadly, the OTC adaptations seem to be that of generalized
hunter-gatherers, a primary dependence on local tool-stone sources, and a generalized stone tool
production technology (Figures 11-13). The extreme contrast in projectile point forms between Clovis
and OTC (Figure 12) indicates contrasting weapons systems. Poor preservation of plant and animal
remains severely hampers interpretations of diet and perishable material culture, but meager evidence
suggests Clovis fauna (bone) and flora (starch grains) resources to be similar to OTC. Use wear on stone
tools are also similar. (6) Is the earlier component a possible technological progenitor of Clovis?
Evidently not. Although blade production technology seems to be somewhat similar in OTC and Clovis,
the production of bifaces and flake tools are entirely different, particularly the nature of the projectile
points. (7) What do differences or similarities between the Clovis and earlier components reveal about
possible alternative histories of occupation and cultural succession at this locality and beyond? Locally
there seems to be a break in the cultural succession between OTC and Clovis at Gault in addition to the
technological contrasts. In broader contexts of North America and the Western Hemisphere, this is not
a surprising finding given the complex mosaic of archaeological manifestations older than and
contemporary with Clovis.
Acknowledgements: Partial support from NSF Grant 0920549, a grant from Summerlee Foundation and from many
donors as well as volunteer efforts on the part of scores of individuals—all of which is greatly appreciated.
Clovis OTC Clovis OTC Clovis OTC
projectile points in any later cultures of this region.