Coles Creek fauna procurement strategies: subsistence diversity among late prehistoric hunter-gatherer-horticulturalists in the Lower Mississippi Valley

In the late 1980s, a collaborative effort between Harvard University’s Lower Mississippi Survey and Tulane University’s Center for Archaeology launched a study examining the causes and consequences of subsistence change in the Lower Mississippi Valley. The Osceola Project contributed the first formal study of late prehistoric faunal remains within the Alluvial Plain, becoming the standard against which all subsequent Coles Creek faunal assemblages have been measured. Recent evidence recovered from three sites located in the Eastern Uplands presented the opportunity to compare and contrast vertebrate subsistence in these two distinct physiographic regions. We hypothesize that a clear distinction exists between lowland and upland Coles Creek procurement strategies. This article evaluates this claim by examining species diversity, spatial patterns, and temporal trends evident within an eight-site sample. The results suggest that the primary factor influencing Coles Creek fauna procurement was the immediate environment, and that the composition of Late Woodland period diets may be a reflection of efficiency of effort rather than food access or scarcity.     

Early Paleoindian Mobility and Watercraft: An Assessment from the Mississippi River Valley

Several researchers have suggested use of watercraft during the Early Paleoindian period 11,500 and 10,800 rcybp (13,400–12,700 cal B.P.), but none have brought empirical data to bear on this possibility. This paper addresses the potential for fluted point-making groups to have made and used boats circa 11,000 rcybp (13,000–12,800 cal B.P.). Fluted point data from a large region of the upper and central Mississippi River valley strongly suggest that the Mississippi River was a barrier to movement and that Early Paleoindians in the midcontinent did not routinely use watercraft.     

Precipitation of lead–zinc ores in the Mississippi Valley‐type deposit at Trèves,Cévennes region of southern France

The Trèves zinc–lead deposit is one of several Mississippi Valley‐type (MVT) deposits in the Cévennes region of southern France. Fluid inclusion studies show that the ore was deposited at temperatures between approximately 80 and 150°C from a brine that derived its salinity mainly from the evaporation of seawater past halite saturation. Lead isotope studies suggest that the metals were extracted from local basement rocks. Sulfur isotope data and studies of organic matter indicate that the reduced sulfur in the ores was derived from the reduction of Mesozoic marine sulfate by thermochemical sulfate reduction or bacterially mediated processes at a different time or place from ore deposition. The large range of δ³⁴S values determined for the minerals in the deposit (12.2–19.2‰ for barite, 3.8–13.8‰ for sphalerite and galena, and 8.7 to ?21.2‰ for pyrite), are best explained by the mixing of fluids containing different sources of sulfur. Geochemical reaction path calculations, based on quantitative fluid inclusion data and constrained by field observations, were used to evaluate possible precipitation mechanisms. The most important precipitation mechanism was probably the mixing of fluids containing different metal and reduced sulfur contents. Cooling, dilution, and changes in pH of the ore fluid probably played a minor role in the precipitation of ores. The optimum results that produced the most metal sulfide deposition with the least amount of fluid was the mixing of a fluid containing low amounts of reduced sulfur with a sulfur‐rich, metal poor fluid. In this scenario, large amounts of sphalerite and galena are precipitated, together with smaller quantities of pyrite precipitated and dolomite dissolved. The relative amounts of metal precipitated and dolomite dissolved in this scenario agree with field observations that show only minor dolomite dissolution during ore deposition. The modeling results demonstrate the important control of the reduced sulfur concentration on the Zn and Pb transport capacity of the ore fluid and the volumes of fluid required to form the deposit. The studies of the Trèves ores provide insights into the ore‐forming processes of a typical MVT deposit in the Cévennes region. However, the extent to which these processes can be extrapolated to other MVT deposits in the Cévennes region is problematic. Nevertheless, the evidence for the extensive migration of fluids in the basement and sedimentary cover rocks in the Cévennes region suggests that the ore forming processes for the Trèves deposit must be considered equally viable possibilities for the numerous fault‐controlled and mineralogically similar MVT deposits in the Cévennes region.     

Determination of warfare and interpersonal conflict in the protohistoric period: a case study from Mississippi

Analysis of a bundle burial of a young male recovered from 22OK905, a late prehistoric/protohistoric site located near Starkville, Mississippi, is discussed. AMS dating of the burial places it between AD 1640 and AD 1814, a time when Native American and European conflicts are well documented. One interesting finding is the presence of cut marks on the frontal bone of this individual. These marks were determined to be the result of scalping rather than defleshing marks associated with secondary burial treatment. Comparisons of bone element frequency among several bundle burials suggest that this individual died away from his village and the body was later collected for burial. A second study indicates that a stone tool may have been used to scalp the victim. Copyright © 2005 John Wiley & Sons, Ltd.     

The New York and the Josephine: two steamships of the Charles Morgan Line

Charles Morgan (1795 to 1882) was one of the most important figures in the development of steam packet service in the United States. Morgan's career spanned over a half century, during which he controlled some 117 steamships. Of the three known wrecks of Morgan Line steamers, two, the New York (1837–1845) and the Josephine (1867–1881), have been documented by the Minerals Management Service, a Federal agency responsible for overseeing the extraction of mineral resources on the Outer Continental Shelf. The two vessels document the changing technology of steam navigation through the middle part of the 19th century.     

HISTORIOGRAPHY: A FIELD IN SEARCH OF A HISTORIAN?

Richard Kirkendall's collection of essays, The Organization of American Historians and the Writing and Teaching of American History, examines the history of the Organization of American Historians (OAH) from its founding to the present, using that history to illuminate how the writing of American history has changed over the last hundred years. The book provides coverage of all the major dimensions of the Mississippi Valley Historical Association's (MVHA) and the OAH's activities, ranging from the work of its scholarly publications, the Mississippi Historical Valley Review and the Journal of American History, to its role in promoting the teaching of American history. Overall, the essays in the volume tell a story of the organization's progress toward greater inclusion and democracy, falling prey to a Whig interpretation of historiography. In doing so, the book is part of a larger tendency in the way that historians have approached historiography, which in turn reflects their ambivalence about their relationship to the historical process. Thus, even as the very enterprise of historiography is premised on the recognition of how historians are themselves the products of the historical process, historians have revealed the limits to that recognition in their approach to the subject. This essay shows how deeply rooted this duality has been in the study of American historiography and illuminates some of its sources by placing Kirkendall's book in the context of how the MVHA and the OAH have treated historiography over the course of the organization's history.     

Formal analyses and functional accounts of groundstone “plummets” from Poverty Point, Louisiana

Groundstone plummets of magnetite or hematite are commonly found artifacts of the Late Archaic period in Louisiana. While often assumed to have functioned as weights for fishnets or as thrown objects used to catch waterfowl, relatively little empirical evidence has been generated to explain their form and features relative to hypothesized performance in prehistoric behavior. To address this deficiency, we provide a morphometric analysis of the variability in plummet shape as a means for studying the performance constraints inherent to their use. Based on our analyses, we find that plummet form is well explained as a component of weighted looms, supporting the early use weaving technology in the Late Archaic of Eastern North America.     

THE SHELBY FOREST SITE IN SOUTHWEST TENNESSEE AND EARLY MISSISSIPPIAN RED-FILMED POTTERY IN THE CENTRAL MISSISSIPPI VALLEY

Abstract

The Shelby Forest site in southwest Tennessee is an Early Mississippian component characterized by Varney Red Filmed ceramics. Comparison to other sites in the Reelfoot Lake area of west Tennessee and the Upper St. Francis Basin of Missouri and Arkansas allows refinement of the direction, timing, and characteristics of influences from these areas northeastward to American Bottom and southward into the Yazoo Basin of Mississippi. Subsequent influences from the Cahokia area into the southern Yazoo Basin and northeast Louisiana are also discussed.     

The DaVincis of dirt: Geoarchaeological perspectives on Native American mound building in the Mississippi River basin

The complexity of mound construction, as revealed through geoarchaeological analyses, indicates the cultural significance of mounds may be as well reflected in the earthen construction materials and their arrangement, as it is in the artifacts abandoned on their summits. We use geoarchaeological examples from three sites in the Mississippi River basin, Shiloh Mounds, Cahokia, and Poverty Point, to advocate a geoarchaeological approach that considers multiple scales from the regional soils and geomorphology, field observation of lithostratigraphic units, to the micro-scale identification of the mineralogy and soil development in order to decipher the source and processing of the soils and sediments. We focus on the use of five types of construction referred to here as: sod blocks, soil blocks, loaded fills, zoned fills and veneers. Also we address the selection and transportation of soils and sediments used in mound building and what these types of deposits reveal about the methods used to build mounds. These data can be used to evaluate and understand organization of labor, pace of construction, and mound appearance. We hold there is a considerable (although unquantified) difference between earth moving and mound building and that the construction of these important monuments required considerable knowledge, skill, planning, hard work, and attention to symbolic and ritual meaning.