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

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Figure 3.7. Stratigraphic river cut bank. Arrow indicates undercut line that led to the collapse of the upper wall. Note portions of a contemporary concrete house foundation remain atop cut bank (upper circle). Remainder of the slab has fallen to the bottom of the bank (lower circle). Figure 3.8. Aerial photograph illustrating areas impacted by river channel. ‘D’ indicates the Classic period constructions being impacted and ‘E’ illustrates the location in the contemporary ejido of El Marquesillo, which included numerous precolumbian constructions as well (INEGI 2000). 74
El Marquesillo’s geographic location on the San Juan River provided strategic socioeconomic advantages. For people living in riverine environments, such as those in the Tonala, Coatzacoalcos, Papaloapan, and San Juan River basins, it has been established through archaeological and ethnohistoric data that water transport was the most effective and efficient mode of conveyance (Berdan and Anawalt 1997:113; Coe and Diehl 1980b:54-59; Doering 2002:97; Navarrete 1978; Rust and Sharer 1988; Scholes and Warren 1965:779). Grove (1968:182) contends that Formative period trade nodes were located on constricted passes along routes that were positioned to monitor the flow of goods. A cursory examination of the river network around El Marquesillo demonstrates that its position was a natural hub or focal point for multiple routes that connected a variety of localities, both nearby and distant. Figure 3.9 illustrates that the tributaries of the San Juan create a broad network linking numerous regional ecological regions. One of the two primary tributaries of the San Juan is the Río La Lana whose headwaters begin at Cerro Mirador, Oaxaca (1536 m asl). La Lana’s principal tributary is the Colorado River, which extends to the slopes of Nudo de Zempoaltépetl, Oaxaca (3412 m asl), both of these sources are deep in the Sierra de Juarez in Oaxaca. The second principal tributary to the San Juan is the Trinidad River, which is fed by the Chisme and Puxmetacán rivers. These waters drain the northern slope of Cerro Casa de Piedra (2348 m asl), which is less than 15 km north of the Tehuantepec River. The Tehuantepec flows out of the eastern end of the Valley of Oaxaca and empties into the Pacific Ocean at Salina Cruz. To the northeast of El Marquesillo, Arroyo Zanja Grande and Arroyo Zanja Prieta flowed past either side of Laguna de los Cerros. These paleochannels resulted from 75
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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
Page 45 and 46: Sanders and Webster (1988:544) argu
Page 47 and 48: Park (1992:90) presents the Olmec a
Page 49 and 50: lowland subsistence economy until a
Page 51 and 52: Maya are lineal descendents of the
Page 53 and 54: continued to inhibit scientific inq
Page 55 and 56: describes this attempted conformanc
Page 57 and 58: The models used for evaluation of t
Page 59 and 60: number of archaeological correlates
Page 61 and 62: Confederacy Model Pool (2000:150;20
Page 63 and 64: Limitations and Cautions in the Use
Page 65 and 66: Lorenzo is considered the earliest
Page 67 and 68: Several lines of evidence suggest a
Page 69 and 70: turn, gave budding Olmec leaders co
Page 71 and 72: apid growth of settlements and thei
Page 73 and 74: techniques (Berger et al. 1967; Hei
Page 75 and 76: appear to characterize it as a “c
Page 77 and 78: iconographic detail, and appear to
Page 79 and 80: Formative period Southern Gulf Lowl
Page 81 and 82: Medellín-Zeníl (1960) found large
Page 83 and 84: de Agua, and the famous, iconograph
Page 85 and 86: egarding subsistence, settlement, p
Page 87 and 88: Introduction Chapter 3. El Marquesi
Page 89 and 90: 300-900). Historical documentation
Page 91 and 92: The features of the San Juan are ch
Page 93 and 94: Figure 3.4. Aerial photograph of El
Page 95: At each of these three points of co
Page 99 and 100: of the location for more than 3,500
Page 101 and 102: The extensive Villa Alta architectu
Page 103 and 104: of constructions. This formal archi
Page 105 and 106: To achieve and maintain this elevat
Page 107 and 108: Figure 3.11. Map of the Southern Gu
Page 109 and 110: Teotihuacán and Aztec trade routes
Page 111 and 112: land was not in the form of gold an
Page 113 and 114: Huaspaltepec (Playa Vicente), betwe
Page 115 and 116: as listed in these records, include
Page 117 and 118: community members had to work the l
Page 119 and 120: The 1944 flood was a momentous even
Page 121 and 122: of ancient structures, including Ce
Page 123 and 124: to recover as much information as p
Page 125 and 126: Figure 3.17. Photograph of El Seño
Page 127 and 128: collection along the cut bank was a
Page 129 and 130: its termination line (Borstein 2001
Page 131 and 132: Figure 3.18. Illustration of San Lo
Page 133 and 134: is seated transitionally between th
Page 135 and 136: Introduction Chapter 4. El Marquesi
Page 137 and 138: Grove 1997; Tolstoy 1989). Landscap
Page 139 and 140: Determination of the Survey Area Th
Page 141 and 142: Surface Mapping and Terrain Modelin
Page 143 and 144: Global Positioning System (GPS) Map
Page 145 and 146: 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
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Coyote, Honduras (Terry et al. 2000
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intersection on the numbered rows a
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The results were reported in parts
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Figure 4.28b. Box plot summaries of
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Elemental Analysis of the Soils fro
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Summary of the Soil Analyses When t
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Figure 4.31a. Potassium distributio
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estriction prohibiting further exca
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The average depth of any observed a
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Figure 5.7. Site map illustrating l
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Figure 5.8. River cut profile 1A Le
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Figure 5.9. River cut profile 1B in
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Figure 5.10. River cut profile 2A L
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Figure 5.11. River cut profile 6B o
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Formative to Protoclassic ceramics
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fabrication methods, technologies,
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some of the Formative period wares
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The San Lorenzo Olmec Period (c. 11
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Figure 5.19. Examples of Middle For
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The Late Classic Period (c. AD 550-
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English annular ware (c. AD 1785-18
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Ceramic Collection Areas The identi
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Figure 5.26. Distribution of cerami
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Formative period accounted for 785
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The survey was conducted along the
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Figure 5.29. Diagram of Olmec thron
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Figure 5.30. Map illustrating the l
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Late Formative (263), Protoclassic
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demonstrates an analogous situation
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Offering I Figure 5.32. Locations o
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Figure 5.34. Offering I is at the c
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Figure 5.36. Two reconstructed plat
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crescent with its concave and conve
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The two figurine types are common t
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vessels that were deposited into a
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Figure 5.45. Two of three similar s
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Obsidian and Lithic Analyses The Ob
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Throne Units Test Units Offerings I
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inhabitants from other sites, or in
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Figure 5.50. Examples of stones tho
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Figure 5.51. El Marquesillo throne
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accomplished through violent blows
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Figure 5.56. Close-up of the figure
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Figure 5.58. Illustration of magnet
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Modifications to this pattern occur
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class occurred only in the presence
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appearance of ceramics occurred dur
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series of interrelated residential,
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The Early Formative period appearan
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Evidence of these constructions is
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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
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Kruger, R. P. 1996 An Archaeologica
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Madry, S. L. H. 1987 A Multiscalar
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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
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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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