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- SPIN enables high throughput species identification of archaeological bone by proteomicsPublication . Rüther, Patrick Leopold; Husic, Immanuel Mirnes; Bangsgaard, Pernille; Gregersen, Kristian Murphy; Pantmann, Pernille; Carvalho, Milena; Godinho, Ricardo Miguel; Friedl, Lukas; Cascalheira, João; Taurozzi, Alberto John; Jørkov, Marie Louise Schjellerup; Benedetti, Michael; Haws, Jonathan; Bicho, Nuno; Welker, Frido; Cappellini, Enrico; Olsen, Jesper VelgaardSpecies determination based on genetic evidence is an indispensable tool in archaeology, forensics, ecology, and food authentication. Most available analytical approaches involve compromises with regard to the number of detectable species, high cost due to low throughput, or a labor-intensive manual process. Here, we introduce “Species by Proteome INvestigation” (SPIN), a shotgun proteomics workflow for analyzing archaeological bone capable of querying over 150 mammalian species by liquid chromatography-tandem mass spectrometry (LC-MS/MS). Rapid peptide chromatography and data-independent acquisition (DIA) with throughput of 200 samples per day reduce expensive MS time, whereas streamlined sample preparation and automated data interpretation save labor costs. We confirm the successful classification of known reference bones, including domestic species and great apes, beyond the taxonomic resolution of the conventional peptide mass fingerprinting (PMF)-based Zooarchaeology by Mass Spectrometry (ZooMS) method. In a blinded study of degraded Iron-Age material from Scandinavia, SPIN produces reproducible results between replicates, which are consistent with morphological analysis. Finally, we demonstrate the high throughput capabilities of the method in a high-degradation context by analyzing more than two hundred Middle and Upper Palaeolithic bones from Southern European sites with late Neanderthal occupation. While this initial study is focused on modern and archaeological mammalian bone, SPIN will be open and expandable to other biological tissues and taxa.
- A stalagmite test of North Atlantic SST and Iberian hydroclimate linkages over the last two glacial cyclesPublication . Denniston, Rhawn F.; Houts, Amanda N.; Asmerom, Yemane; Wanamaker Jr., Alan D.; Haws, Jonathan; Polyak, Victor J.; Thatcher, Diana L.; Altan-Ochir, Setsen; Borowske, Alyssa C.; Breitenbach, Sebastian F. M.; Ummenhofer, Caroline C.; Regala, Frederico T.; Benedetti, Michael M.; Bicho, Nuno Gonçalo Viana Pereira FerreiraClose coupling of Iberian hydroclimate and North Atlantic sea surface temperature (SST) during recent glacial periods has been identified through the analysis of marine sediment and pollen grains co-deposited on the Portuguese continental margin. While offering precisely correlatable records, these time series have lacked a directly dated, site-specific record of continental Iberian climate spanning multiple glacial cycles as a point of comparison. Here we present a high-resolution, multi-proxy (growth dynamics and delta C-13, delta O-18, and delta U-234 values) composite stalagmite record of hydroclimate from two caves in western Portugal across the majority of the last two glacial cycles (similar to 220 ka). At orbital and millennial scales, stalagmite-based proxies for hydroclimate proxies covaried with SST, with elevated delta C-13, delta O-18, and delta U-234 values and/or growth hiatuses indicating re-duced effective moisture coincident with periods of lowered SST during major ice-rafted debris events, in agreement with changes in palynological reconstructions of continental climate. While in many cases the Portuguese stalagmite record can be scaled to SST, in some intervals the magnitudes of stalagmite isotopic shifts, and possibly hydroclimate, appear to have been somewhat decoupled from SST.
- Human adaptive responses to climate and environmental change during the Gravettian of Lapa do Picareiro (Portugal)Publication . Haws, Jonathan; Benedetti, Michael; Carvalho, Milena; Ellis, Grace; Pereira, Telmo; Cascalheira, João; Bicho, Nuno; Friedl, LukasOn the Iberian Peninsula, abrupt climate shifts during the Late Pleistocene impacted human and natural systems. Our knowledge of human adaptive responses to these climatic perturbations has improved in recent years with the development of new radiocarbon techniques that have increased the temporal resolution of cultural chronologies. At the same time, new high-resolution paleoclimatic records from Greenland ice cores, deep-sea sediment cores, speleothems, and microfaunal assemblages have permitted detailed paleoenvironmental reconstructions. Combined with the archaeological record of culture change, these data sets allow for a better understanding of the nature of human socio-ecological systems during the Late Pleistocene. Here we present new data on the Gravettian occupations at Lapa do Picareiro, a cave site in Portugal with a long continuous stratigraphic sequence spanning MIS 3 and 2. The ongoing excavation of Lapa do Picareiro has revealed at least three Gravettian levels with very different patterns of raw material use and technological reduction. The Early Gravettian levels contain a quartzite flake assemblage with several refitting clusters and a small chert assemblage with nosed endscrapers and bladelet technology. The Late or Terminal Gravettian level contains carinated endscraper/core-bladelet technology, mainly quartz, with chert blade production, and a few bone tools. The faunal assemblages also have a different character. Both contain a similar range of medium and large ungulates but the earlier Gravettian has a much richer and more diverse assemblage of small animals. These combined archaeological data sets provide a new perspective on Gravettian human adaptations in response to climate shifts, especially Heinrich Event 3 and Greenland Interstadials 4 and 3.
- Middle and late stone age of the Niassa region, Northern Mozambique. Preliminary resultsPublication . Bicho, Nuno Gonçalo Viana Pereira Ferreira; Haws, Jonathan; Raja, Mussa; Madime, Omar; Gonçalves, Célia; Cascalheira, João; Benedetti, Michael M.; Pereira, Telmo; Aldeias, VeraLocated between modern-day South Africa and Tanzania, both of which have well-known and extensive Stone Age records, Mozambique's Stone Age sequence remains largely unknown in the broader context of African Pleistocene prehistory. Such lack of data occurs despite the key geographical location of the country, in southern Africa at the southeastern tip of the Great Rift Valley. As such, Mozambique is an area of interest to evaluate the origins and dispersion of Homo sapiens within Africa, particularly in relation to Middle Stone Age contexts and associated early modern human ecology and cognition.This paper focuses on preliminary survey results from the Niassa District, near Lake Niassa (also known as Lake Malawi) in northern Mozambique. The results include the discovery and location of more than 80 new surface lithic concentration localities, as well as data from two new sites, the open air surface site of Ncuala and the rock shelter of Chicaza. For Chicaza we provide a series of new radiocarbon dates for the Iron Age and Late Stone Age occupations based on preliminary testing carried out at the site. (C) 2015 Elsevier Ltd and INQUA. All rights reserved.
- Late Pleistocene Landscape and Settlement Dynamics of Portuguese EstremaduraPublication . Haws, Jonathan; Benedetti, Michael; Funk, Caroline L.; Bicho, Nuno; Pereira, Telmo; Marreiros, Joao; Daniels, J. Michael; Forman, Steven L.; Minckley, Thomas A.; Denniston, Rhawn F.Here we report the results of an integrated geoarchaeological survey to study Palaeolithic human settlement dynamics in the coastal region of Portuguese Estremadura. The region has been an important focus of human occupation across multiple glacial-interglacial cycles, including periods of well-documented abrupt climate instability during MIS 3 and 2. The pedestrian survey covered a roughly 10 km wide strip of land between Sao Pedro de Muel and Peniche. The survey intensively targeted three landscape settings with Pleistocene-age surfaces and sediments: the coastal bluffs with exposed aeolian, fluvial, and colluvial sands; the Caldas da Rainha diapiric valley and associated fluvial/estuarine fills; and, Cretaceous chert-rich limestone uplands that bound the inland margin of the study area. We discovered dozens of new Palaeolithic sites, analyzed numerous Pleistocene sedimentary sections, and applied widespread OSL-dating to establish age control that allowed us to build a regional geomorphic history to contextualize Late Pleistocene human settlement across the region.
- Portable art and personal ornaments from Txina-Txina: a new later stone age site in the Limpopo River Valley, southern MozambiquePublication . Bicho, Nuno Gonçalo Viana Pereira Ferreira; Cascalheira, João; André, Lino; Haws, Jonathan; Gomes, Ana; Gonçalves, Célia; Raja, Mussa; Benedetti, Michael M.This paper reports on preliminary fieldwork at the Later Stone Age site of Txina-Txina in Mozambique. Excavation yielded a long stratigraphic sequence, a large lithic assemblage, a unique decorated gastropod shell fragment and two ostrich eggshell beadsthe first of their type recovered from a Stone Age context in Mozambique.