4 results on '"Bernard, Anaëlle"'
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2. Exploring the Genetic Structure and Phylogeographic Patterns of the Copepod Genus Eurytemora in Europe.
- Author
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Mouth, Céleste, Ferreira, Flavien, Sukhikh, Natalia, Bou, Elisa, Bernard, Anaëlle, Tackx, Michèle, Azémar, Fréderic, Meire, Patrick, Maris, Tom, and Legal, Luc
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MAXIMUM likelihood statistics ,CYTOCHROME oxidase ,GENETIC variation ,BIOGEOGRAPHY ,PHYLOGENY - Abstract
The genus Eurytemora is a diverse group of copepods found in coastal, estuarine, brackish, and freshwater environments. The main research has focused on Eurytemora affinis (Poppe, 1880) and revealed it to be a species complex. Eurytemora velox (Liljeborg, 1853) has only recently been characterized in the Scheldt estuary but never within a global phylogenetic context. This study integrated nearly all European Eurytemora species sequences available, along with original ones from the Scheldt. A total of 351 sequences were analyzed using one mitochondrial gene (CO1) and one nuclear gene (nITS), with sequencing performed specifically on the CO1 gene. Phylogenetic reconstructions were performed using the Maximum Likelihood method, along with haplowebs and genetic diversity indices. A significant subdivision between six European species was observed. The monophyletic clade status of the E. affinis complex was confirmed alongside the existence of three geographically isolated lineages of the E. affinis species, the East Atlantic, the North Sea/English Channel, and the Baltic lineages, each exhibiting pronounced genetic differentiation. The population of E. velox from the Urals differs significantly from the European ones. These results provide both an overview of the genetic structure of the genus in geographic Europe as well as new insights on E. velox. [ABSTRACT FROM AUTHOR]
- Published
- 2024
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3. Zooplankton and suprabenthos of the upstream part of the Seine estuary (France)
- Author
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Chauvel, Nathan, Bernard, Anaëlle, Bou, Elisa, Azémar, Frédéric, Dauvin, Jean-Claude, Tackx, Michèle, Pezy, Jean-Philippe, Morphodynamique Continentale et Côtière (M2C), Université de Caen Normandie (UNICAEN), Normandie Université (NU)-Normandie Université (NU)-Institut national des sciences de l'Univers (INSU - CNRS)-Université de Rouen Normandie (UNIROUEN), Normandie Université (NU)-Centre National de la Recherche Scientifique (CNRS), Laboratoire Ecologie Fonctionnelle et Environnement (LEFE), Institut Ecologie et Environnement (INEE), Centre National de la Recherche Scientifique (CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université Toulouse III - Paul Sabatier (UT3), Université de Toulouse (UT)-Université de Toulouse (UT)-Observatoire Midi-Pyrénées (OMP), Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3), Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales [Toulouse] (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France -Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales [Toulouse] (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France -Centre National de la Recherche Scientifique (CNRS)-Institut National Polytechnique (Toulouse) (Toulouse INP), and Université de Toulouse (UT)
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[SDE.BE]Environmental Sciences/Biodiversity and Ecology - Abstract
International audience
- Published
- 2022
4. Seeking alternative stable states in a deep lake
- Author
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Bruel, Rosalie, Marchetto, Aldo, Bernard, Anaëlle, Lami, Andrea, Sabatier, Pierre, Frossard, Victor, Perga, Marie Elodie, Istituto per lo Studio degli Ecosistemi, Consiglio Nazionale delle Ricerche [Roma] (CNR), Environnements, Dynamiques et Territoires de la Montagne (EDYTEM), Centre National de la Recherche Scientifique (CNRS)-Université Savoie Mont Blanc (USMB [Université de Savoie] [Université de Chambéry]), Centre Alpin de Recherche sur les Réseaux Trophiques et Ecosystèmes Limniques (CARRTEL), Institut National de la Recherche Agronomique (INRA)-Université Savoie Mont Blanc (USMB [Université de Savoie] [Université de Chambéry]), University Savoie-Mont Blanc, Region Auvergne-Rhone-Alpes, Université Savoie Mont Blanc (USMB [Université de Savoie] [Université de Chambéry])-Centre National de la Recherche Scientifique (CNRS), and Université Savoie Mont Blanc (USMB [Université de Savoie] [Université de Chambéry])-Institut National de la Recherche Agronomique (INRA)
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0106 biological sciences ,[SDE.IE]Environmental Sciences/Environmental Engineering ,010604 marine biology & hydrobiology ,[SDE.MCG]Environmental Sciences/Global Changes ,spatial heterogeneity ,[SHS.GEO]Humanities and Social Sciences/Geography ,15. Life on land ,Aquatic Science ,010603 evolutionary biology ,01 natural sciences ,[SDE.ES]Environmental Sciences/Environmental and Society ,Aquatic organisms ,alternative stable state ,Oceanography ,eutrophication ,13. Climate action ,Alternative stable state ,Environmental science ,14. Life underwater ,palaeo-ecology ,[SDE.BE]Environmental Sciences/Biodiversity and Ecology ,early warnings - Abstract
International audience; Hysteresis linked to alternative stable states may explain delays in water quality recovery despite reduced nutrient loadings in shallow lakes. Because deep lakes are assumed to be less prone to critical transitions, similar delays are attributed to the confounding effects of additional environmental disturbances, such as climate warming. Herein, we hypothesised that the lack of evidence of nutrient‐driven alternative stable states in a deep lake arises from the fact that the nutrient threshold that causes the critical transition is lower than the nutrient threshold in shallow lakes. Thereby, it might have been crossed much earlier in the lake history. To test this hypothesis, we focused on the palaeo‐ecological trajectory of Lake Varese, which is a deep, hypereutrophicated peri‐alpine lake undergoing restoration. Proxies for drivers of ecological state (i.e. total phosphorus—TP—through diatoms and pigments) and ecological responses (Cladocera), as well as a repeatable analysis, were used to identify transitions and to distinguish hysteretic delays from those of the ecosystems responding to additional constraints over the past century. Our results suggest spatial heterogeneity in the ecological response. The littoral habitats changed abruptly and prematurely for a low TP threshold, causing a shift that met many criteria of a flickering‐type critical transition. Soon after the littoral shift, a striking increase in the lake phosphorous concentration was recorded and drove the pelagic assemblage towards a new state. This transition was abrupt, and the pelagic communities exhibited limited evidence of recovery; however, we found no evidence of hysteresis. Therefore, the modern ecological trajectory of the pelagic communities is currently driven by climate warming. This detailed analysis allowed us to go beyond the general pattern that links ecological responses to drivers and suggest that a nonlinear transition following eutrophication can take place in a deep lake synchronously with linear transitions. Instead of triggering a new regime shift, climate warming, to which pelagic habitats are more sensitive than littoral ones, has driven the lake further from its safe operating space.
- Published
- 2018
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