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Vincon-Laugier, A.

Publications and source records attributed to Vincon-Laugier, A..

2 recordsLinked to original sources

Towards a tracking of bird migratory behaviour through geological time: an isotopic and histological approach

O_LIBird seasonal migration is a remarkable biogeographic phenomenon, yet its deep-time origin(s) and evolutionary history remain poorly understood, with the bird fossil record largely overlooked. This study explores the predictability of bird migratory behaviour from the oxygen isotope composition of their bone apatite phosphate ({delta}18Op), a promising approach in this regard because: (i) sedentary and migratory birds tend to occupy distinct climatic niches year-round; (ii) their {delta}18Op values primarily reflect the climate-driven isotopic composition of their drinking water; and (iii) this isotopic signature can persist through fossilisation. C_LIO_LIBone tissues were categorised based on their potential to yield spatio-temporally distinct climatic records: Early Bone Tissues (EBT), deposited before somatic maturity, and Late Bone Tissues (LBT), formed through bone remodelling over the lifespan. The predictability of migratory behaviour was theoretically assessed by modelling tissue-specific {delta}18Op values for thousands of birds across 77 migratory and sedentary species, using tracking and observational data along with a revised phosphate-water fractionation equation. These theoretical results were confronted with data from 11 extant bird species, obtained using a new experimental framework combining histological and isotopic analyses. C_LIO_LIA significantly positive correlation between {delta}18Op and the proportion of LBT in bone samples was observed both theoretically and experimentally in migratory birds - particularly in long-distance migrants - and is predicted to be virtually absent in sedentary species at temperate latitudes. Migratory birds that died outside their natal sites can also be identified when their {delta}18Op,EBT values fall outside the range observed in local juvenile and sedentary birds. C_LIO_LIWe conclude that bird migratory behaviour can be inferred from the {delta}18Op values of their skeletal remains, provided the individuals migrated across sufficiently contrasting climatic zones. While this approach cannot detect all migratory behaviours - such as short-distance or longitudinal movements - it is unlikely to misclassify sedentary birds as migratory at temperate latitudes. We therefore argue that this approach can be extended to well-preserved fossil bones to infer past bird migratory behaviours, as long as the palaeoclimatic context is carefully considered. More broadly, this study establishes a framework for inferring migratory behaviour in any vertebrate from non-fully remodelled biomineralised remains. C_LI

evolutionary biology↗

High δ15N values in Predynastic Egyptian archeological remains: A potential indicator for localised soil fertilisation practices in extreme conditions

Predynastic Egypt arose around 5700 BC when nomadic people settled in the Nile Valley. Without voluntary practice related to anthropic mummification, as will be seen with the Egyptian Dynastic empires, human remains from this period were naturally mummified because of the natural environmental conditions, possibly enveloped in plant mats and animal skins. This study focuses on four mummies from the Natural History Museum of Musee des Confluences in Lyon (France). The geographic origin of the mummies and climatic conditions at that time were deduced from o18O measurements on teeth and bones. These measurements confirm that the primary source of drinking water was the Nile, and that one mummy of unknown origin also originated from Upper Egypt like the other three. The diet and life habits of these individuals were inferred from carbon (o13C), nitrogen (o15N) and sulfur (o34S) isotope compositions of their skins and bone collagens. Our study is of particular interest as we were able to analyse the animal skins and plant material enveloping the mummies using the same isotopic systems. The mean o15N values obtained in human skins (17.9{+/-}2.4{per thousand}, AIR) were found to be high, and consistent with the values measured in animal skins (16.0{+/-}2.9{per thousand}, AIR). The analysed plants have even higher values, with an average of 22.1{+/-}2.2{per thousand}, AIR. The most probable explanation for the markedly elevated {delta}15N values observed in all the materials investigated is localised soil amendment practices. This is corroborated by the consistent nitrogen isotopic signatures across all the examined tissues, with a notable prevalence in plant tissues.

ecology↗