Paleoparasitology of Merovingian Corpses Buried in Stone Sarcophagi in the Saint-Martin-au-Val Church (Chartres, France).

Paleoparasitological analysis was carried on 4 Merovingian skeletons, dated from the late-5th to the late-9th centuries, and recovered in the church of Saint-Martin-au-Val in Chartres (Center region, France). The corpses were buried in stone sarcophagi, which were still sealed at the time of excavation. Parasite marker extraction was conducted on sediment samples taken from the abdominal and pelvic regions, but also on samples taken from under the head and the feet as control samples. Microscopic observation revealed the presence of 3 gastrointestinal parasites, namely the roundworm (Ascaris lumbricoides), the whipworm (Trichuris trichiura) and the fish tapeworm (genus Diphyllobothrium). This analysis contributes to a better knowledge of the health status and the lifestyle of ancient medieval populations during the Merovingian period, for which very few paleoparasitological data were available, up until now. It demonstrates the presence of the fish tapeworm for the first time during this period.

Benthic foraminifera assemblages as elemental pollution bioindicator in marine sediments around fish farm (Vrgada Island, Central Adriatic, Croatia).

Effects on sediments of fish farming activity near Vrgada Island was analysed through living and total foraminiferal assemblages and concentration of major, minor and trace elements from three sediment cores. Elemental concentrations of sediments are in accordance with carbonate characteristics of the surrounding area and show mostly natural element variations between sampling locations and throughout the cores, with no significant increases due to fish farming activity. Only phosphorus concentration shows elevate values below the fish cage, assigned to fish pellets. Foraminiferal communities are dominated by epifaunal and stress tolerant species, while diversity indices point to normal marine conditions. The type of substrate and phosphorus content in sediments principally influence foraminiferal community composition, while other elemental concentrations have no perceptible effect on the assemblages. Some foraminiferal species Ammoniatepida, Ammoniabeccarii, Elphidiumcrispum, Elphidiummacellum and genus Haynesina are confirmed to be tolerant to elevated nutrient (phosphorus) content, while Ammonia parkinsoniana shows sensitivity to pollution. Postmortem processes cause decrease of foraminiferal density and species richness with core depth. All results point to negligible influence of fish farming and relatively stable environmental conditions at all sampling locations.

Effects of deposit-feeding tubificid worms and filter-feeding bivalves on benthic-pelagic coupling: implications for the restoration of eutrophic shallow lakes.

Benthic-pelagic coupling is a key factor in the dynamics of shallow lakes. A 12-week mesocosm experiment tested the hypothesis that deposit-feeding tubificid worms stimulate the growth of pelagic algae while filter-feeding bivalves promote the growth of benthic algae, using the deposit-feeding tubificid Limnodrilus hoffmeisteri and the filter-feeding bivalve Anodonta woodiana. A tube-microcosm experiment using a (32)P radiotracer tested for differential effects of tubificids and bivalves on the release of sediment phosphorus (P). In this experiment A. woodiana was replaced by Corbicula fluminea, a smaller bivalve from the same functional group whose size was more appropriate to the experimental tubes needed for the tracer study. The first experiment recorded greater nutrient concentrations in the overlying water, higher biomass of pelagic algae as measured by chlorophyll a (Chl a), lower light intensity at the sediment and lower biomass of benthic algae in the worm treatments than in the controls, while nutrients and Chl a of pelagic algae were lower and the light intensity and Chl a of benthic algae were higher in the bivalve treatments than in the controls. In the second experiment, (32)P activity in the overlying water was higher in both treatments than in the controls, but highest in the worm treatment indicating that both animals accelerated P release from the sediment, with the biggest effect associated with the presence of worms. Our study demonstrates that worms promote pelagic algal growth by enhancing the release of sediment nutrients, while bivalves, likely through their grazing on pelagic algae increasing available light levels, stimulate benthic algal growth despite enhanced P release from the sediment and thus aid the establishment of clear water states. The rehabilitation of native bivalve populations may therefore enhance the recovery of eutrophic shallow lakes.

Resíduos alimentares, infecções parasitárias e evidência do uso de plantas medicinais em grupos pré-históricos das Américas / Food waste, parasitic infections and evidence of the use of medicinal plants in groups of prehistoric Americas

A paleoparasitologia utiliza como principal instrumento de estudo a análise de coprólitos e sedimentos retirados do solo de sítios arqueológicos, latrinas e da área pélvica de esqueletos. Associando-se dados da arqueologia, antropologia e paleoparasitologia, entre outras ciências, é possível obter resultados consistentes sobre modo de vida e saúde das populações no passado. Neste trabalho foram analisadas amostras de três regiões diferentes das Américas. Um total de 59 amostras de coprólitos e sedimentos provenientes de sítios arqueológicos localizados na área arqueológica de São Raimundo Nonato, que engloba o Parque Nacional Serra da Capivara (PNSC), Piauí, Brasil, foram analisadas. Esta região apresenta sítios com datações bastante antigas obtidas na área do Parque, com evidência de atividades humanas datadas aproximadamente de 50.000 anos; 12 amostras provenientes do sítio arqueológico Antelope Cave, localizado no Arizona, EUA. Assim como o PNSC, este sítio possui a presença de cerâmica e a iniciação da agricultura pelos grupos pré-históricos naquela região; e 15 amostras retiradas diretamente da região pélvica de sepultamentos provenientes do sambaqui Cubatão I, localizado em Joinville, Santa Catarina, Brasil. Este sítio arqueológico é, na verdade, um desafio metodológico devido ao clima e a atividade biótica do solo da região que não permitem boas condições de preservação do material arqueológico. A análise de resíduos alimentares destas diferentes regiões arqueológicas forneceu dados a respeito da dieta de populações antigas e a relação entre a presença de parasitos e o encontro de plantas com propriedades anti-helmínticas, e ainda foi possível a determinação de casos de falso parasitismo.

Paleoparasitology uses, as the main tool to study, the analysis of coprolites andsediments removed from the land of archaeological sites, latrines and the pelvic area of skeletons. Joining data from archeology, anthropology and paleoparasitology, among other sciences, it is possible to obtain solid results on livelihoods and health of people in the past. On this study were analyzed samples from three different regions of the Americas. A total of 59 samples of coprolites and sediments from archaeological sites located in thearchaeological area of São Raimundo Nonato, which includes the National Park Serra da Capivara (PNSC), located in Pernambuco, Brazil, were analyzed. This region has sites with the oldest dating obtained in the Park, with human activities recorded from 50.000 years BP; 12 samples from the archaeological site of Antelope Cave, located in Arizona, USA. This site, just like PNSC, has features such as the presence of pottery and the initiation of agriculture by prehistoric groups in the region, and 15 samples taken directly from the pelvic region of burials from the sambaqui Cubatão I, located in Joinville, Santa Catarina, Brazil. This archaeological site is actually a methodological challenge due to the climate and soil biotic activity in the region that don't allow good conditions of preservation of the archeological material. The analysis of alimentary residues of these different archaeological areas supplied dataregarding the diet of old populations and the relationship between the presence ofparasites and the encounter of plants with anthelminthic properties, and it was still possible the determination of cases of false parasitism.

Protozoan grazing increases mineralization of naphthalene in marine sediment.

Bacterial decomposition of organic matter is frequently enhanced when protozoa are present. Various mechanisms have been proposed to account for this phenomenon, including effects associated with grazing by protozoa (such as increased recycling of limiting nutrients, removal of senescent cells, or reduction of competition among bacteria) and indirect effects of grazers (such as excretion of bacterial growth factors). Few studies have examined the role of protozoa in bacterial degradation of xenobiotic compounds in sediment containing a natural community of microbes. The effect of protozoa on mineralization of naphthalene was investigated in this study. Laboratory experiments were conducted using field-contaminated estuarine sediment, with the indigenous microbial populations. Mineralization of naphthalene was up to four times greater in treatments with actively grazing protozoa than in treatments containing the grazing inhibitor cytochalasin B. Control experiments confirmed that the grazing inhibitor was not toxic to ciliates but did prevent them from grazing. The grazing inhibitor did not affect growth rates of a mixed culture of sediment bacteria or a pure polycyclic-aromatic-hydrocarbon-degrading strain. Once grazing had been inhibited, supplementing treatments with inorganic N and P, glucose, or additional protozoa failed to stimulate naphthalene mineralization. Naphthalene-degrading bacteria were four to nine times less abundant when protozoan grazing was suppressed. We suggest that protozoa enhance naphthalene mineralization by selectively grazing on those sediment bacteria that ordinarily would outcompete naphthalene-degrading bacteria.

Diphyllobothrium: Neolithic parasite?

During paleoparasitological analyses on several Neolithic sites in Switzerland (Arbon-Bleiche 3) and southwestern Germany (Hornstaad-Hörnle I, Torwiesen II, and Seekirch-Stockwiesen), numerous eggs of Diphyllobothrium sp. were recovered. This is one of the earliest occurrences of this parasite during the prehistoric period in the Old World. The prevalence of this helminth in the samples studied raises the question as to how important parasitic diseases were during the Neolithic period and what their actual consequences were.