Environmental change and seasonal behavior of mastodons in the Great Lakes region inferred from stable isotope analysis

2014 ◽  
Vol 82 (2) ◽  
pp. 366-377 ◽  
Author(s):  
Jessica Z. Metcalfe ◽  
Fred J. Longstaffe

AbstractWe investigate seasonal variations in the diet and drinking water of four Great Lakes mastodon (Mammut americanum) specimens using stable isotope analysis of serially sampled inner-enamel bioapatite structural carbonate (δ13Csc, δ18Osc), and previously published bulk analyses. Isotopic analyses and thin section measurements showed that mastodon tooth enamel extension rates (~ 12–4 mm/yr, decreasing toward the cervix) were lower than those of mammoths or modern elephants. Mastodons had distinct and highly regular seasonal variations in δ13Csc and δ18Osc, which we interpret in the context of local glacial history and vegetation changes. Seasonal variations in δ18O were large but variations in δ13C were small, and may have been obscured if coarser sampling methods than our inner-enamel sampling approach were used. Thus, our approach may be particularly useful for understanding relatively small seasonal changes in δ13C within C3 environments. The seasonal patterns, though not entirely conclusive, suggest that the Ontario mastodons did not migrate over very long distances. Rather, the climate and seasonal dietary patterns of mastodons within the region changed over time, from ~ 12,400 to 10,400 14C yr BP (~ 15,000 – 12,000 cal yr BP). Insights gained using these methods can contribute to a better understanding of megafaunal extinctions and Paleoamerican lifeways.

Author(s):  
Katie A. Hemer ◽  
Jane A. Evans

Stable isotope analysis is firmly established as a method for the investigation of past population mobility. The distinction between local and non-local individuals within a cemetery population relies on identifying an individual’s place of childhood residence through the analysis of strontium and oxygen isotopes present in human tooth enamel. Traditionally, studies investigating mobility focus on the analysis of a single tooth. More recently, however, it has become apparent that in order to investigate the mobility of an individual during childhood—and thus to consider the importance of children in the migration process—it is necessary to analyse a series of teeth which form at different stages during the early years of life. This chapter will consider the potential of—and challenges surrounding—this scientific approach to the investigation of childhood mobility in the past.


Anthropology ◽  
2016 ◽  
Author(s):  
Eric Bartelink

Stable isotope analysis refers broadly to a series of chemical methods used to study phenomena such as earth systems, the hydrological cycle, and ecology. The use of stable isotopes in anthropology traces its beginnings to the late 1970s. Originally focused on geological, hydrological, and ecological problems, stable isotope analysis now is a major component of the anthropologist’s toolkit. Current applications within anthropology draw from the core scientific disciplines but adapt these methods for specific research questions within archaeology, bioarchaeology, paleoanthropology, and forensic anthropology. One major area of study is dietary reconstruction, which focuses on isotope analysis of human skeletons to examine temporal and regional dietary patterns, as well as variation associated with sex, age, mortuary patterns, and social status. More specialized approaches examine weaning and childhood diet patterns using serial sections of tooth enamel and dentin. Another major area of isotope research in anthropology is the study of past residence patterns (e.g., migration and mobility). Some stable isotopes record information about the local water and geology, and thus provide information regarding the place of origin or travel history of an individual. By examining multiple isotopes in different tissues, anthropologists can reconstruct changes in residence patterns. For example, isotopes in enamel bioapatite (mineral fraction) do not change throughout life, so teeth provide a record of where a person lived when a particular tooth formed. Bone collagen (organic fraction) and bioapatite (mineral fraction), in contrast, are constantly replaced through remodeling; thus, if a person moved to a new geographic region, the isotope values in their bones will shift toward the new location over time. By comparing the isotopes in teeth versus bones, anthropologists can detect whether a person was local or nonlocal to the area where they died. In instances where hair or nails are preserved (e.g., mummies, modern forensic cases), serial sections of these tissues can be used to provide a detailed record of diet or travel history in the months prior to death. More recently, forensic anthropologists have begun to examine stable isotopes in modern human remains to aid with medicolegal identification. These methods are especially useful when a decedent is nonlocal to the area where they died (for example, a recent traveler or foreign-born individual).


Author(s):  
Soichiro Kusaka

This chapter discusses the practice of ritual tooth ablation in Japan in relation to diet and migration. Ablation was practiced extensively among hunter-gatherers, and the tradition typically followed one of two patterns, type 4I and type 2C, depending on whether the lower incisors or canines were extracted, respectively. To test the hypothesis that a dependence on marine resources for food differed depending on ablation type during childhood and adulthood, stable isotope ratios of bone collagen and tooth enamel were measured. It was discovered that diets did vary among individuals with different ablation types in the Inariyama population. The findings provide important evidence that biocultural dietary differences were related to ablation type in the Jomon period.


2011 ◽  
Vol 25 (7) ◽  
pp. 910-916 ◽  
Author(s):  
A. Holobinko ◽  
W. Meier-Augenstein ◽  
H. F. Kemp ◽  
T. Prowse ◽  
S. M. Ford

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