New frontiers in calcium stable isotope geochemistry:Perspectives in present and past vertebrate biology

International audienc

Calcium isotopes in enamel of modern and Plio-Pleistocene East African mammals

Calcium isotope analyses show a depletion of heavy calcium isotopes in vertebrates, compared to food sources along each trophic step. Recent studies show considerable variability of the calcium isotopic composition of bone and teeth in modern mammals, leading to inconclusive interpretations regarding the utility of Ca isotopes for trophic inference in mammal-dominated terrestrial ecosystems. Here, we analyzed modern enamel samples from the Tsavo National Park (Kenya), and fossil enamel samples dated from ca. 4 Ma to 1.6 Ma from the Turkana Basin (Kenya). We found a constancy of taxa ordering between the modern and fossil datasets, suggesting that the diagenesis of calcium isotopes is minimal in fossils. In modern herbivore samples using similar digestive physiologies, browsers are enriched in Ca-44 compared to grazers. Both grazer and browser herbivore tooth enamel is enriched in Ca-44 relative to carnivores by about +0.30 parts per thousand. Used together, carbon and calcium isotope compositions may help refine the structure of the C-3 and C-4 trophic chains in the fossil record. Due to their high preservation potential, combining both carbon and calcium isotope systems represent a reliable approach to the reconstruction of the structure of past ecosystems. (C) 2018 Eisevier B.V. All rights reserved

Inferring odontocete life history traits in dentine using a multiproxy approach (δ15N, δ44/42Ca and trace elements)

Funding Information: The authors thank F. Demaret and W. Dabin (Observatoire Pelagis) for helping secure odontocete milk and tooth samples. This work was funded by the Conseil National de la Recherche Scientifique (CNRS) INSU INTERRVIE program (Early Whale Resource Use and Diet project) to J.E.M. The authors thank LGLTPE (UMR 5276) and ENS de Lyon for supporting the MC‐ICP mass spectrometry platform. Nitrogen isotope measurements were performed on the “Ecologie Isotopique” platform of LEHNA (UMR 5023). The authors thank F. Arnauld‐Godet and E. Albalat for technical support on the MC‐ICP platform of the LGLTPE. The authors thank the anonymous reviewers and the editor R. Bol for their constructive comments that helped improve the quality of this work. Funding Information: The authors thank F. Demaret and W. Dabin (Observatoire Pelagis) for helping secure odontocete milk and tooth samples. This work was funded by the Conseil National de la Recherche Scientifique (CNRS) INSU INTERRVIE program (Early Whale Resource Use and Diet project) to J.E.M. The authors thank LGLTPE (UMR 5276) and ENS de Lyon for supporting the MC-ICP mass spectrometry platform. Nitrogen isotope measurements were performed on the “Ecologie Isotopique” platform of LEHNA (UMR 5023). The authors thank F. Arnauld-Godet and E. Albalat for technical support on the MC-ICP platform of the LGLTPE. The authors thank the anonymous reviewers and the editor R. Bol for their constructive comments that helped improve the quality of this work. Publisher Copyright: © 2023 The Authors. Rapid Communications in Mass Spectrometry published by John Wiley & Sons Ltd.Peer reviewedPublisher PD

Calcium Isotopic Evidence for Vulnerable Marine Ecosystem Structure Prior to the K/Pg Extinction

International audienceThe collapse of marine ecosystems during the end-Cretaceous mass extinction involved the base of the food chain [1] up to ubiquitous vertebrate apex predators [2–5]. Large marine reptiles became suddenly extinct at the Cretaceous-Paleogene (K/Pg) boundary, whereas other contemporaneous groups such as bothremydid turtles or dyrosaurid crocodylomorphs, although affected at the familial, genus, or species level, survived into post-crisis environments of the Paleocene [5–9] and could have found refuge in freshwater habitats [10–12]. A recent hypothesis proposes that the extinction of plesiosaurians and mosasaurids could have been caused by an important drop in sea level [13]. Mosasaurids are unusually diverse and locally abundant in the Maastrichtian phosphatic deposits of Morocco, and with large sharks and one species of elasmosaurid plesiosaurian recognized so far, contribute to an overabundance of apex predators [3, 7, 14, 15]. For this reason, high local diversity of marine reptiles exhibiting different body masses and a wealth of tooth morphologies hints at complex trophic interactions within this latest Cretaceous marine ecosystem. Using calcium isotopes, we investigated the trophic structure of this extinct assemblage. Our results are consistent with a calcium isotope pattern observed in modern marine ecosystems and show that plesiosaurians and mosasaurids indiscriminately fall in the tertiary piscivore group. This suggests that marine reptile apex predators relied onto a single dietary calcium source, compatible with the vulnerable wasp-waist food webs of the modern world [16]. This inferred peculiar ecosystem structure may help explain plesiosaurian and mosasaurid extinction following the end-Cretaceous biological crisis

Calcium isotope physiology in mammals

L’environnement et la physiologie déterminent les compositions isotopiques du Ca de l’organisme des vertébrés et des mammifères en particulier. Ces constats ont permis de dégager des applications possibles de l’étude des isotopes du Ca, en biologie médicale pour le suivi de l’équilibre osseux chez les mammifères et en (paléo-)écologie pour l’étude des régimes alimentaires actuels et passés des vertébrés. Ces applications sont tributaires d’une meilleure compréhension fondamentale des causes de ces variations. Cette thèse a pour but de déterminer les principales causes de variabilité des compositions isotopiques du Ca chez les mammifères et l’humain. Un protocole d’analyse en solution par MC-ICP-MS est d’abord présenté puis deux méthodes d’échantillonnage sont comparées afin de réaliser des mesures de résolution spatiale accrue dans les tissus minéralisés. L’influence des sources alimentaires de Ca est ensuite discutée. La composition isotopique de l’alimentation humaine est variable du fait des compositions diverses des sources primaires de Ca et dépend particulièrement des proportions de produits laitiers dans l’alimentation. Il est démontré que les transitions nutritionnelles précoces, comme le sevrage du lait maternel, peuvent être tracées par les compositions de l’émail des dents de lait humaines. Les mécanismes des fractionnements isotopiques sont discutés sur la base d’observations chez l’humain et l’animal. Un modèle mathématique permet de dégager des mécanismes expliquant la distribution des isotopes du Ca à travers les tissus et les fluides de l’organisme et met en lumière le rôle prépondérant du rein dans la détermination de la composition isotopique de l’os.Environment influences the isotope compositions of body Ca and vertebrate physiology affects these compositions in turn. These observations have allowed recognition of possible applications for Ca isotopes, in the field of medical biology, with the assessment of bone mineral balance in human, and in (palaeo-)ecology for the study of past and present day diets in vertebrates. These applications depend on a better fundamental understanding of causes for these variations. This thesis aims at identifying the main mechanisms responsible for variability of Ca isotope compositions in mammals and human. A solution mode analysis protocol was first developed for MC-ICP-MS. Two methods for microsampling of tooth enamel were then compared in order to increase spatial resolution of mineralized tissues analysis. The influence of dietary Ca sources has been discussed. Isotope composition of human diet is variable because of the diversity of Ca primary sources but also due to variations in dairy products proportions in diet. Early dietary transitions, such as weaning, can be studied using the Ca isotope compositions of human deciduous tooth enamel.Based on observations in human and other mammals, the mechanisms responsible for Ca isotope fractionations are discussed. A mathematical model was developed, allowing the identification of some mechanisms responsible for Ca isotope distribution across organism reservoirs, and sheds light on the crucial role of kidney in determination of bone isotope compositions

Physiologie isotopique du Calcium chez les mammifères

Environment influences the isotope compositions of body Ca and vertebrate physiology affects these compositions in turn. These observations have allowed recognition of possible applications for Ca isotopes, in the field of medical biology, with the assessment of bone mineral balance in human, and in (palaeo-)ecology for the study of past and present day diets in vertebrates. These applications depend on a better fundamental understanding of causes for these variations. This thesis aims at identifying the main mechanisms responsible for variability of Ca isotope compositions in mammals and human. A solution mode analysis protocol was first developed for MC-ICP-MS. Two methods for microsampling of tooth enamel were then compared in order to increase spatial resolution of mineralized tissues analysis. The influence of dietary Ca sources has been discussed. Isotope composition of human diet is variable because of the diversity of Ca primary sources but also due to variations in dairy products proportions in diet. Early dietary transitions, such as weaning, can be studied using the Ca isotope compositions of human deciduous tooth enamel.Based on observations in human and other mammals, the mechanisms responsible for Ca isotope fractionations are discussed. A mathematical model was developed, allowing the identification of some mechanisms responsible for Ca isotope distribution across organism reservoirs, and sheds light on the crucial role of kidney in determination of bone isotope compositions.L’environnement et la physiologie déterminent les compositions isotopiques du Ca de l’organisme des vertébrés et des mammifères en particulier. Ces constats ont permis de dégager des applications possibles de l’étude des isotopes du Ca, en biologie médicale pour le suivi de l’équilibre osseux chez les mammifères et en (paléo-)écologie pour l’étude des régimes alimentaires actuels et passés des vertébrés. Ces applications sont tributaires d’une meilleure compréhension fondamentale des causes de ces variations. Cette thèse a pour but de déterminer les principales causes de variabilité des compositions isotopiques du Ca chez les mammifères et l’humain. Un protocole d’analyse en solution par MC-ICP-MS est d’abord présenté puis deux méthodes d’échantillonnage sont comparées afin de réaliser des mesures de résolution spatiale accrue dans les tissus minéralisés. L’influence des sources alimentaires de Ca est ensuite discutée. La composition isotopique de l’alimentation humaine est variable du fait des compositions diverses des sources primaires de Ca et dépend particulièrement des proportions de produits laitiers dans l’alimentation. Il est démontré que les transitions nutritionnelles précoces, comme le sevrage du lait maternel, peuvent être tracées par les compositions de l’émail des dents de lait humaines. Les mécanismes des fractionnements isotopiques sont discutés sur la base d’observations chez l’humain et l’animal. Un modèle mathématique permet de dégager des mécanismes expliquant la distribution des isotopes du Ca à travers les tissus et les fluides de l’organisme et met en lumière le rôle prépondérant du rein dans la détermination de la composition isotopique de l’os

Le pseudo-kyste du péritoine (un diagnostic trop souvent méconnu)

MONTPELLIER-BU Médecine UPM (341722108) / SudocPARIS-BIUM (751062103) / SudocMONTPELLIER-BU Médecine (341722104) / SudocSudocFranceF

Rehabilitation of LNID diversion headworks in southern Alberta

The Rehabilitation of the Diversion Headworks on the Oldman River is part of the improvement and expansion of the 60 year old Lethbridge Northern Irrigation District (LNID) water supply gravity system. Demand for increased capacity of the conveyance system, maintenance and operational problems experienced over the years and compliance with the Water Resources Act and Alberta Fish and Wildlife, are the factors which determined the new functional requirements of the Diversion Headworks.The works described in this paper involve the demolition and reconstruction of the Headgates and Sluicegate structures, the incorporation of a Fishway and Riparian Outlet works and the refurbishing of the existing concrete weir and footbridge