Department of Human Evolution
Max Planck Institute for Evolutionary Anthropology
Deutscher Platz 6
phone: +49 (341) 3550 - 350
fax: +49 (0341) 3550 - 399
We use the methods of virtual paleoanthropology to study how differences in growth and development before and after birth contribute to the large shape differences observed between adult Neandertals and modern humans.
Dental material represents a large portion of the hominin fossil record. Using microCT scans of fossil teeth and jaws allows us to test different hypotheses related to the evolution of hominin dental morphology, masticatory biomechanics and tooth decay.
Our isotope studies on Neandertal diet, as well as studies of the vegetal particles preserved in dental calculus reveal that Neandertals had a varied diet largely depending on local climate and landscape throughout their vast geographical and chronological range.
Lately there has been great renewed interest in the question of when hominins first controlled and produced fire. We are working on this topic from a number of perspectives. First, to better understand what temperatures are needed to leave an impact on proxies for fire such as stone tools, bones and sediments, we built a heating apparatus to do a set of controlled experiments heating various sediment types to different temperatures of varying durations. The results (see Aldeias et al., 2016a; Aldeias, in press) show that average fires produce subsurface temperatures high enough to cause thermal alteration of objects up to 10 cm below the surface (with maximum temperatures at this depth ranging from 85°C up to ~250°C). This apparatus is available for additional experiments.
Second, we have also started to investigate the effects of cooking, namely concerning the exploitation of marine resources. We have conducted a series of experiments on shellfish roasting fires (Aldeias et al., 2016b). In this work, we use FTIR to trace the transformation of aragonitic shells to calcite and we show that this transformation can start at fairly low temperatures (around 250 °C). This research highlights potential issues of using altered shells for radiocarbon and isotope analysis. Additional papers, focusing on using microFTIR to map the location of the aragonite>calcite transformation within a shell and application of this new methodology in archaeological sediments, are in preparation.
Third, in our excavations we continue to document the relative presence of fire related activities through, where possible, the documentation of fire features (including the application of micromorphology and microFTIR) and also through the quantification of fire proxies such as heated stone and heated bones. We are quite interested in expanding this data set to have a better understanding of when hominins were making use of fire in part to better understand the origins of the controlled use and production of fire.
We are interested in reconstructing Neandertal (and more generally hominin) adaptations through direct studies of their stone and bone tools. In addition to studying the materials that derive from our excavations and some key collections, we also emphasize here an experimental approach to better understand some factors that contribute to stone and bone tool variability.
Our approach to stone tool studies is mainly quantitative with an emphasis on what is typically called attribute analysis. More recently we have started to work with three dimensional data and the application of geometric morphometrics to these data. We are interested in how these methods might help us better document and understand the structure of variability in certain key artifact types in the archaeological record, but we are also interested in how these methods might be more widely applicable to stone tool studies. We have a number of scanners in the department for collecting these data.