An Unexplored Realm in the Heartland of the Southern Gulf ... - Famsi

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shown that the initial appearance of this type occurred in the Late Formative period. This earlier development would explain its presence in the lower portions of Unit N8W3. To reiterate, a layer of highly disturbed soil was documented between the 0.4 to 1.1 m levels and contained chronologically mixed ceramics. This disturbance also included a few pieces of obsidian, small pieces of basalt, and some burned clay (Hernández and Barrera 2002). No chronologically identifiable ceramics or other cultural materials were recovered in any of the other excavated units. It was also noted that the disturbance of the soil and mixing of temporal ceramics did not breech Offering I or II, which were located immediately below the outer eastern edges of this disturbance. Collectively, these conditions suggest an approximately 2m wide, basin-like hole was dug at some point during the Late Classic period to a depth of 1.1 m. The hole was then re-filled with a mixture of the unearthed Formative period materials and Late Classic period wares. Finally, this digging event was limited to this specific area. Ceramics from the Test Unit Excavations In November 2002, Hernández reentered the field and directed the placement and excavation of seven, 1.5 x 1.5 m test units in Fields 1 and 2 (Figure 5.30). These locations were selected due to the high density of both Formative and Classic period in situ ceramics that were present in the upper 2 m of the nearby river cut bank as well as on the surface. Also, the surface features differed substantially from the Olmec throne complex over 750 m to the southwest, suggesting a divergent type of activity area. The following is a description of the chronologically diagnostic ceramic artifacts recovered and their depositional patterns (Table 5.2). 210
Figure 5.30. Map illustrating the location of the test unit excavations Unit 1 was located 3 m west of Structure 86. Three stratigraphic layers were encountered. Level I (0-20 cm) is a layer of soft to semi-compacted humus that contained few ceramics. Those present are small and, in most cases, diagnostically unrecognizable due to damage caused by repeated agricultural cultivation, cattle grazing, and erosional effects. This situation is true of Level I in all test units. Levels II and III of Unit 1 contained substantial quantities of ceramics. At a depth of 1 m, a layer of highly compacted, culturally sterile clay was encountered. The unit contained ceramics from the Unit Table 5.2. Ceramic artifacts recovered from test unit excavations Early Formative Middle Formative Late Formative Proto to Early Classic Late Classic Non- Diagnostic Totals 1 62 323 525 167 153 1040 2270 2 127 324 462 129 52 1034 2128 3 244 671 263 438 794 2368 4778 4 32 36 52 18 4 202 344 5 74 147 113 184 96 1036 1650 6 4 4 10 1 7 38 64 7 15 311 137 1965 75 614 3117 Totals 558 1816 1562 2902 1181 6332 14351 211
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An Unexplored Realm in the Heartlan
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“Note to Reader” The original o
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Confederacy Model 39 Feudalistic Mo
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Elemental Analysis of the Soils fro
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The Initial Occupation of El Marque
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List of Tables Table 5.1. Ceramic C
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Figure 3.14. Plan view of the Olmec
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Figure 5.7. Site map illustrating l
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Figure 5.53. El Marquesillo throne
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the resulting data do not fit many
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Furtherance of my academic career w
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Introduction Chapter 1. Archaeology
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esearch being conducted along the S
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its introduction to Mesoamerican ar
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participants. It is especially crit
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interpretations. Finally, I compare
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analogy (Diehl 1989:25; VanDerwarke
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change, fluctuates according to “
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embedded misconceptions about these
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The “Heartland” has been deline
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than a century after their occurren
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inference as opposed to evidence. T
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Sanders and Webster (1988:544) argu
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Park (1992:90) presents the Olmec a
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lowland subsistence economy until a
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Maya are lineal descendents of the
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continued to inhibit scientific inq
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describes this attempted conformanc
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The models used for evaluation of t
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number of archaeological correlates
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Confederacy Model Pool (2000:150;20
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Limitations and Cautions in the Use
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Lorenzo is considered the earliest
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Several lines of evidence suggest a
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turn, gave budding Olmec leaders co
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apid growth of settlements and thei
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techniques (Berger et al. 1967; Hei
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appear to characterize it as a “c
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iconographic detail, and appear to
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Formative period Southern Gulf Lowl
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Medellín-Zeníl (1960) found large
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de Agua, and the famous, iconograph
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egarding subsistence, settlement, p
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Introduction Chapter 3. El Marquesi
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300-900). Historical documentation
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The features of the San Juan are ch
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Figure 3.4. Aerial photograph of El
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At each of these three points of co
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El Marquesillo’s geographic locat
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of the location for more than 3,500
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The extensive Villa Alta architectu
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of constructions. This formal archi
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To achieve and maintain this elevat
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Figure 3.11. Map of the Southern Gu
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Teotihuacán and Aztec trade routes
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land was not in the form of gold an
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Huaspaltepec (Playa Vicente), betwe
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as listed in these records, include
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community members had to work the l
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The 1944 flood was a momentous even
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of ancient structures, including Ce
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to recover as much information as p
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Figure 3.17. Photograph of El Seño
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collection along the cut bank was a
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its termination line (Borstein 2001
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Figure 3.18. Illustration of San Lo
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is seated transitionally between th
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Introduction Chapter 4. El Marquesi
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Grove 1997; Tolstoy 1989). Landscap
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Determination of the Survey Area Th
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Surface Mapping and Terrain Modelin
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Global Positioning System (GPS) Map
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Figure 4.4. Map of El Marquesillo g
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have the potential to record points
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The topographic images and terrain
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Figure 4.8. Digital Terrain Model o
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Figure 4.11. View to the east of lo
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The western third of the platform h
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Figure 4.15. Elevated view of Field
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Figure 4.17. Topographic map of El
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Figure 4.19. Northwest view of spri
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Information Systems (GIS) approach
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Figure 4.21. Illustration of docume
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Magnetic Properties of Basalt The m
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Magnetic Data Collection, Condition
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The magnetometer was set to the bas
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Figure 4.23. Topographical base map
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of basalt, but instead, a body of s
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Figure 4.25. Topographic contour ma
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mercuric sulfide in the soil. There
Page 181 and 182: Coyote, Honduras (Terry et al. 2000
Page 183 and 184: intersection on the numbered rows a
Page 185 and 186: The results were reported in parts
Page 187 and 188: Figure 4.28b. Box plot summaries of
Page 189 and 190: Elemental Analysis of the Soils fro
Page 191 and 192: Summary of the Soil Analyses When t
Page 193 and 194: Figure 4.31a. Potassium distributio
Page 195 and 196: estriction prohibiting further exca
Page 197 and 198: The average depth of any observed a
Page 199 and 200: Figure 5.7. Site map illustrating l
Page 201 and 202: Figure 5.8. River cut profile 1A Le
Page 203 and 204: Figure 5.9. River cut profile 1B in
Page 205 and 206: Figure 5.10. River cut profile 2A L
Page 207 and 208: Figure 5.11. River cut profile 6B o
Page 209 and 210: Formative to Protoclassic ceramics
Page 211 and 212: fabrication methods, technologies,
Page 213 and 214: some of the Formative period wares
Page 215 and 216: The San Lorenzo Olmec Period (c. 11
Page 217 and 218: Figure 5.19. Examples of Middle For
Page 219 and 220: The Late Classic Period (c. AD 550-
Page 221 and 222: English annular ware (c. AD 1785-18
Page 223 and 224: Ceramic Collection Areas The identi
Page 225 and 226: Figure 5.26. Distribution of cerami
Page 227 and 228: Formative period accounted for 785
Page 229 and 230: The survey was conducted along the
Page 231: Figure 5.29. Diagram of Olmec thron
Page 235 and 236: Late Formative (263), Protoclassic
Page 237 and 238: demonstrates an analogous situation
Page 239 and 240: Offering I Figure 5.32. Locations o
Page 241 and 242: Figure 5.34. Offering I is at the c
Page 243 and 244: Figure 5.36. Two reconstructed plat
Page 245 and 246: crescent with its concave and conve
Page 247 and 248: The two figurine types are common t
Page 249 and 250: vessels that were deposited into a
Page 251 and 252: Figure 5.45. Two of three similar s
Page 253 and 254: Obsidian and Lithic Analyses The Ob
Page 255 and 256: Throne Units Test Units Offerings I
Page 257 and 258: inhabitants from other sites, or in
Page 259 and 260: Figure 5.50. Examples of stones tho
Page 261 and 262: Figure 5.51. El Marquesillo throne
Page 263 and 264: accomplished through violent blows
Page 265 and 266: Figure 5.56. Close-up of the figure
Page 267 and 268: Figure 5.58. Illustration of magnet
Page 269 and 270: Modifications to this pattern occur
Page 271 and 272: class occurred only in the presence
Page 273 and 274: appearance of ceramics occurred dur
Page 275 and 276: series of interrelated residential,
Page 277 and 278: The Early Formative period appearan
Page 279 and 280: Evidence of these constructions is
Page 281 and 282: and the excavated pit is not known,
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For the Gulf Olmec, monumental exhi
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precisely. This method would also m
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An earlier discussion suggested sty
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approximately 100 cm to 120 cm belo
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Nevertheless, the structural design
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discussion about the antiquity of t
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6.3). At La Venta equivalent basalt
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shamanistic ritual and rulership (F
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elevation provides an excellent ove
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further support to the idea that El
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Also contributing to the ceramic pr
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Another possible basalt deposition
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off is dramatic to say the least. T
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direction, a series of hills approx
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Finally, the selection and investig
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a metaphor for the movements of the
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plaza complex is also oriented to p
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the traditional communal ideology.
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where new diagnostic ceramic types
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Understanding of the early Postclas
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ceramics probably arrived at the en
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investigation before the direction
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Marquesillo, past and present. Fitt
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Through the integration of a sequen
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experienced an upward trend in popu
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prehispanic occupation would have b
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Assmann (2006) argues that prehisto
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1997:288). These changes in residen
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structures that could provide long-
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Analysis of these three components
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Early architectural units, specific
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activities and that these activitie
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political structure. Was it an inde
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subordinate to a nearby primary cen
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Explanation of Spatial Organization
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conjunction with other forms of arc
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Mesoamerican worldviews (Vogt 1981:
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Expanding the Boundaries and a Look
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to illustrate their power and wealt
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emains is striking. This disproport
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the earliest detectable occupation
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and Uxpanapa River Basins, I wonder
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Arnaiz-Villena, A., G. Vargas-Alarc
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Bassie, K. 2006 The Fire and Water
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Blake, M. and J. E. Clark 1999 The
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Butler, R. F. 1992 Paleomagnetism:
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2001 Gulf Lowlands: South Region. I
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Coe, M. D., D. Snow and E. Benson 1
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2003 Laguna de los Cerros: Una Capi
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2003 Analysis of Formative Period O
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Elachi, C. 1987 Introduction to the
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Foster, G. M. 1940 Notes on the Pop
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2001 La Venta, Tabasco, Mexico. In
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Halbwachs, M. 1992 On Collective Me
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Hester, T. R., H. J. Shafer and K.
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Johnston, K. J. and N. Gonlin 1998
Page 395 and 396:
Kruger, R. P. 1996 An Archaeologica
Page 397 and 398:
Madry, S. L. H. 1987 A Multiscalar
Page 399 and 400:
Middleton, W. D. 2004 Identifying C
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Ortíz, P. 1975 La Ceramica de los
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Plog, S. 1990 Agriculture, Sedentis
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Rapoport, A. 1990 History and Prece
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Rueda, H. G. 1989 Nuevas Exploracio
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Santley, R. S., S. A. Nelson, B. K.
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1989 Olmec Studies: A Status Report
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Stark, B. L. and P. J. Arnold 1997
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Tarling, D. H. 1983 Geomagnetism. C
Page 417 and 418:
Tykot, R. H. 2004 Stable Isotopes a
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Wallerstein, I. 1974 The Modern Wor
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2003 The Role of Kinship and Demogr
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Appendix 1a. Ceramic Analysis: Type
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Appendix 1b. Ceramic Analysis: Type
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Appendix 2. Ceramic Types and Count
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Appendix 2 Ceramic Types and Counts
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Appendix 3a. Obsidian from Test Uni
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Appendix 3b. Obsidian from Throne E
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Appendix 4a. Lithics from Surface C
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Appendix 4b. Lithics from River Cut
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Appendix 5a. Soil Survey I Element
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Appendix 5a. Soil Survey I Element
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Appendix 5b. Soil Survey II Element
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Appendix 5b. Soil Survey II Element
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About the Author Travis F. Doering
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An Unexplored Realm in the Heartland of the Southern Gulf ... - Famsi

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