Distinguishing intraplate from megathrust earthquakes using lacustrine turbidites
Subduction zone seismicity arises from megathrust, crustal, and intraslab earthquakes, and understanding the recurrence patterns of each type is crucial for hazard assessments. Lake sediments can record earthquakes from all three seismogenic sources. Here, we studied the turbidite record of Lo Encañado, an Andean lake located in central Chile. We show that Lo Encañado turbidites can be attributed to (1) subaquatic slope failure by earthquake shaking (coseismic phase), (2) floods or human impact, and (3) postseismic catchment response. All historical events with shaking intensities >VI (modified Mercalli intensity) have triggered coseismic turbidites, but only the intraplate earthquakes triggered subaerial slope failures followed by postseismic turbidites. We argue that this contrasting result is due to different spectra of seismic waves from these earthquake sources: higher-frequency accelerations from intraplate earthquakes are hardly attenuated in rocks around the lake, whereas lower-frequency accelerations from megathrust earthquakes are amplified in soft lake sediments. We tested our findings by comparing acceleration response spectra of recent and historical intraslab and megathrust earthquakes along a longitudinal profile. Results suggest that the location of Andean lakes is ideal to distinguish earthquake sources.
(Geology. vol. 47, n° 0091-7613, pp. 127-130, 01/02/2019)
RCMG, UGent, EPOC, EPHE, PSL, UB, INSU - CNRS, CNRS
Retrotransposon methylation and activity in wild fish (A. anguilla): A matter of size
Understanding how organisms cope with global change is a major question in many fields of biology. Mainly, understanding the molecular mechanisms supporting rapid phenotypic changes of organisms in response to stress and linking stress-induced molecular events to adaptive or adverse outcomes at the individual or population levels remain a major challenge in evolutionary biology, ecology or ecotoxicology. In this view, the present study aimed to test (i) whether environmental factors, especially pollutants, can trigger changes in the activity of retrotransposons (RTs) in wild fish and (ii) if changes in RT DNA methylation or transcription levels can be linked to modifications at the individual level. RTs are genetic elements that have the ability to replicate and integrate elsewhere in the genome. Although RTs are mainly quiescent during normal development, they can be experimentally activated under life-threatening conditions, affecting the fitness of their host. Wild eels were collected in four sampling sites presenting differing levels of contamination. The methylation level and the transcriptional activity of two RTs and two genes involved in development and cell differentiation were analyzed in fish liver in addition to the determination of fish contaminants levels and diverse growth and morphometric indices. An up-regulation of RTs associated to lower methylation levels and lower growth indices were observed in highly contaminated fish. Our results suggest that RT activation in fish experiencing stress conditions could have both detrimental and beneficial implications, affecting fish growth but promoting resistance to environmental stressors such as pollutants. Retrotransposons could represent interesting environment-sensitive molecular markers allowing to link stress-induced molecular events to adverse outcomes at higher levels.
(Environmental Pollution. vol. 245, n° 0269-7491, pp. 494-503, 01/02/2019)
EPOC, EPHE, PSL, UB, INSU - CNRS, CNRS, UR EABX, IRSTEA, INRS - ETE, INRS
Two-dimensional ammonium distribution in sediment pore waters using a new colorimetric diffusive equilibration in thin-film technique
This study presents a new gel based technique to describe the pore water ammonium distribution through the sediment-water interface in two dimensions at a millimeter scale. The technique is an adaptation of the classical colorimetric method based on the Berthelot's reaction. After the thin film of the gel probe was equilibrated by diffusion either in standard solutions or in pore waters, a colorimetric reagent gel was set on the gel probe, allowing development of the characteristic green color. A flatbed scanner and subsequent densitometry image analysis allowed to determine the concentration distribution of ammonium. The gel probe was tested in the laboratory for two media, deionized water and seawater, within the range 0e3000 mM in NH 4 þ. Detection limit is about 20 mM and accuracy about ±25 mM. The field validation was realized in a tidal mudflat of the French Atlantic coast by comparison with conventional pore water extraction and colorimetric analysis. The large range of concentrations and its applicability in continental and marine sediments suggest a wide range of applications of the technique for a reasonable cost.
(Water Research X. vol. 2, n° 2589-9147, pp. 100023, 01/02/2019)
BIAF, UA, IPGP, INSU - CNRS, UPD7, UR, IPG Paris, CNRS, EPOC, EPHE, PSL, UB, INSU - CNRS, CNRS
Écologie des foraminifères benthiques en domaine arctique dans un contexte de changements climatiques : cas des mers de Chukchi, Barents et Baffin
Les foraminifères benthiques sont largement utilisés en océanographie comme bio-indicateurs paléoclimatiques et paléoenvironnementaux du fait de leur présence dans tous les milieux marins, leur sensibilité aux changements environnementaux et leur grande capacité de fossilisation. Néanmoins, leur utilisation nécessite une connaissance approfondie de leur écologie et des paramètres contrôlant leur distribution. Si les connaissances sur l’écologie des foraminifères benthiques sont de plus en plus complètes, elles demeurent très sporadiques dans la zone arctique, système complexe caractérisé par des interactions multiples entre l'atmosphère, l'océan et la cryosphère, pourtant au coeur du changement climatique global. L'amplification polaire du changement climatique conduit les régions des hautes latitudes à se réchauffer près de deux fois plus vite que les régions tempérées. Dans ce contexte, cette thèse s'attache à mieux comprendre l'écologie des foraminifères benthiques vivants dans plusieurs régions arctiques et définir l'importance du contrôle des paramètres environnementaux sur les faunes tels que les propriétés des masses d'eau, la productivité primaire et le flux de matière organique ainsi que la dynamique de la glace de mer. Les foraminifères benthiques vivants ont été analysés dans les premiers centimètres de sédiment de 21 carottes d’interfaces prélevées dans trois régions arctiques durant les étés 2014 et 2015 : la mer de Barents, la baie de Baffin et la mer de Chukchi. Ces trois régions présentent des particularités en termes de couvert de banquise, de circulation des masses d’eau ou de dynamique de la production primaire. Nos résultats montrent que ces facteurs influencent la distribution des foraminifères benthiques. Le flux de matière organique qui résulte de la forte productivité primaire printanière aux abords des fronts polaires hydrographiques, des bordures de glace de mer (zones marginales de glace) et dans la polynie des eaux du nord (baie de Baffin) impacte la densité et la diversité des faunes et favorise le développement de certaines espèces. Nonionellina labradorica dans les eaux arctiques froides et Cassidulina neoteretis associée aux eaux atlantiques répondent aux apports de matière organique fraîche tandis que Melonis barleeanus s’accommode des milieux riches en matière organique plus dégradée. Dans les environnements oligotrophes plus profonds, Oridorsalis tenerus est une espèce ubiquiste. Cette espèce est associée à Cibicidoides wuellerstorfi sur la marge ouest de la mer de Barents et Ioanella tumidula dans le bassin plus profond au nord de la mer de Chukchi. Les propriétés physiques et chimiques des masses d’eau contraignent également la distribution faunistique. En baie de Baffin et sur le plateau de la mer de Chukchi, les eaux corrosives engendrent la dissolution des carbonates, favorisant la dominance des espèces agglutinées. Les études menées dans le cadre de cette thèse permettent de calibrer l'outil foraminifère benthique dans l'actuel et d'affiner leur utilisation en tant que proxy paléoclimatique et paléoenvironnemental en Arctique. Enfin, une étude préliminaire sur les foraminifères benthiques fossiles de trois carottes de la mer de Barents a permis de montrer les variations des conditions paléoenvironnementales au cours des deux derniers siècles.
(28/01/2019)
EPOC, EPHE, PSL, UB, INSU - CNRS, CNRS
Moonlight cycles synchronize oyster behaviour
Organisms possess endogenous clock mechanisms that are synchronized to external cues and orchestrate biological rhythms. Internal timing confers the advantage of being able to anticipate environmental cycles inherent in life on Earth and to prepare accordingly. Moonlight-entrained rhythms are poorly described, being much less investigated than circadian and circannual rhythms synchronized by sunlight. Yet focus on these lunar rhythms is highly relevant to understanding temporal organization of biological processes. Here, we investigate moonlight cycle effects on valve activity behaviour of the oyster Crassostrea gigas. Our results show that oysters modulate valve behaviour according to both intensity and direction of the lunar illumination cycle. As a consequence, valve opening amplitude is significantly increased at third quarter Moons (decreasing lunar illumination) compared with first quarter Moons (increasing lunar illumination) despite identical lunar illumination, and this indicates that oyster modulation of valve behaviour by moonlight cycles is not a direct response to lunar illumination. We propose that oysters use moonlight cycles to synchronize behaviour and also other physiological and ecological aspects of this benthic mollusc bivalve.
(Biology Letters. vol. 15, n° 1744-9561, pp. 20180299, 23/01/2019)
EPOC, EPHE, PSL, UB, INSU - CNRS, CNRS
AMOC as the key driver of the spread in Mid-Holocene winter temperature patterns over Europe in PMIP3 models
The mid-Holocene (6,000 years before present) was a warmer period than today in summer in most places of the Northern Hemisphere. In winter, over Europe, reconstructions of temperature based on pollen data show a dipole of temperature anomalies as compared to present-day, with warmer conditions in the north and colder in the south. It has been proposed that this pattern of temperature anomaly could be explained by a persisting positive phase of the North Atlantic Oscillation during this period, which was, however, not reproduced in general by climate models. Indeed, PMIP3 models show a large spread in their response to the mid-Holocene insolation changes, the physical origins of which are not understood. To improve the understanding of the reconstructed temperature changes and of the PMIP3 model spread, we analyze the dynamical response of these model simulations in the North Atlantic for mid-Holocene conditions as compared to pre-industrial. We focus on the European pattern of temperature in winter, which allows comparing the simulations with a pollen-based reconstruction. We find that some of the model simulations yield a similar pattern to the reconstructed one, with lower amplitude, but which remains within the reconstruction uncertainty. We attribute the northern warm part of the latitudinal dipole of temperature anomaly in winter to a lower sea-ice cover in the Nordic Seas. The decrease of sea ice in winter indeed reduces the sea-ice insulation effect there, allowing the ocean heat released in winter to reach the continental northern Europe. This decrease in winter sea-ice cover is related to an increase in the Atlantic meridional overturning circulation (AMOC) and its associated ocean heat transport, as well as the effect of insolation changes on sea ice in summer, which persists until winter. Concerning the cooling of southern Europe, we only find a slight cooling signal mainly related to the insolation-induced cooling in winter over Africa. We show that the models that failed to reproduce any AMOC increase under mid-Holocene conditions are also the ones that do not reproduce the temperature pattern over Europe. The change in sea level pressure is not sufficient to explain the spread among the models. The ocean-sea ice mechanisms that we proposed constitute an alternative explanation to the pattern of changes in winter temperatures over Europe in the mid-Holocene, which is in better agreement with available model simulations of this period. Finally, we argue that this period can provide interesting emerging constraints on key changes in European climate, and indirectly of AMOC response to radiative changes.
(21/01/2019)
EPOC, EPHE, PSL, UB, INSU - CNRS, CNRS, LSCE, UVSQ, INSU - CNRS, CNRS, DRF (CEA), CEA, LOCEAN-VARCLIM, LOCEAN, MNHN, IRD, INSU - CNRS, SU, CNRS, IPSL (FR_636), ENS-PSL, UVSQ, CEA, INSU - CNRS, X, CNES, SU, CNRS, UPCité
Mercury(II) Binding to Metallothionein in Mytilus edulis revealed by High Energy-Resolution XANES Spectroscopy
Of all divalent metals, mercury (Hg(II)) has the highest affinity for metallothioneins. Hg(II) is considered to be enclosed in the and domains as tetrahedral -type Hg4Cys11-12 and -type Hg3Cys9 clusters similarly to Cd(II) and Zn(II). However, neither the four-fold coordination of Hg nor the existence of Hg-Hg atomic pairs have ever been demonstrated, and the Hg(II) partitioning among the two protein domains is unknown. Using high energy-resolution XANES spectroscopy, MP2 geometry optimization, and biochemical analysis, we provide evidence for the coexistence of two-coordinate Hg-thiolate complex and four-coordinate Hg-thiolate cluster with a metacinnabar-type (β-HgS) structure in the α domain of separate metallothionein molecules from blue mussel under in vivo exposure. The findings suggest that the CXXC claw setting of thiolate donors, which only exists in the domain, acts as a nucleation center for the polynuclear complex and that the five CXC motifs from this domain serve as the cluster-forming motifs. Oligomerization is driven by metallophilic Hg-Hg interactions. Our results provide clues as to why Hg has higher 2 affinity for the than the domain. More generally, they provide a foundation for understanding how metallothioneins mediate mercury detoxification in the cell under in vivo conditions.
(Chemistry - A European Journal. vol. 25, n° 0947-6539, pp. 997-1009, 18/01/2019)
ISTerre, IFSTTAR, INSU - CNRS, USMB [Université de Savoie] [Université de Chambéry], CNRS, UGA [2016-2019], LIENSs, INSU - CNRS, ULR, CNRS, ULR, IP, CNRS, IECB, UB, INSERM, CNRS, EPOC, EPHE, PSL, UB, INSU - CNRS, CNRS, NEEL - OPTIMA, NEEL, Grenoble INP, CNRS, UGA [2016-2019], UA, INC-CNRS, CNRS, LIONS, NIMBE UMR 3685, IRAMIS, CEA, INC-CNRS, CNRS, ESRF, NIMBE UMR 3685, IRAMIS, CEA, INC-CNRS, CNRS
Monsoon control on channel avulsions in the Late Quaternary Congo Fan
The mechanisms governing the development of deep-sea fans is a matter of debate and their understanding at Milankovitch and millenial time-scales is challenged by complex architectures and the lack of material suitable for establishing reliable chronostratigraphies. Based on a detailed investigation of the emplacement of channel-levee-lobe systems and their successive bifurcations and seaward-landward migrations (Picot et al., 2016), we present for the last 210 ka a detailed chronostratigraphic framework of the migration pattern based mainly on radiocarcarbon dating of channels and lobes abandonment or initiation.
The comparison of architectural cycles to proxies of external factors (sea-level and climate) suggest that sea-level changes have minor impacts on the architectural evolution of the Congo Fan. In contrast, comparison with climate and environmental proxies (West African monsoon, pollen grain assemblages, Kaolinite/Smectite) evidences a major impact on the timing of the development of the architectural pattern, at least for the last 38 kyr. A general scheme of the growth pattern of the Congo Fan in link with climate evolution is proposed: the stacking pattern of the Congo Fan responds to humidity/aridity cycles that generate successive progradation and retrogradation of avulsion points. These climate changes are under the control of the West African monsoon which, by controlling the rainfall and vegetation on the watershed, ultimately impacts the composition and volume of the sediment source and the transport capacity of gravity flow generated in the canyon and flowing in the turbiditic channels.(Quaternary Science Reviews. vol. 204, n° 0277-3791, pp. 149-171, 15/01/2019)
LGO, UBS, IFREMER, UBO EPE, CNRS, IFREMER, iSTeP, INSU - CNRS, SU, CNRS, EPOC, EPHE, PSL, UB, INSU - CNRS, CNRS, CSTJF, [Total Energies. Anciennement : Total, TotalFina, TotalFinaElf]
Risk perception and specific behaviors of anglers concerning mercury contamination of fish
(Human and Ecological Risk Assessment, n° 1080-7039, pp. 1-14, 15/01/2019)
IMS, UB, CNRS, ENSC, IMS, UB, CNRS, Bordeaux INP, EPOC, EPHE, PSL, UB, INSU - CNRS, CNRS
Étude des réponses adaptatives et délétères des premiers stades du développement de truite arc-en-ciel, Oncorhynchus mykiss, exposés à des produits phytosanitaires utilisés en viticulture
L’utilisation excessive de pesticides engendre des pollutions et des dégradations importantes de l’environnement y compris sur les écosystèmes aquatiques. L’activité viticole ne fait pas exception à cette règle, et c’est pour cette raison que ce travail de thèse s’est intéressé aux réponses adaptatives ou délétères aux premiers stades de vie de poissons exposés à trois produits phytosanitaires utilisés en viticulture ainsi qu’à leur mélange et à des échantillons environnementaux. La thèse s’intéresse aux stades précoces de développement de la truite arc-en-ciel, mais également à la lignée cellulaire de foie de truite RTL-W1. Les embryons de truite ont été exposés au cuivre, au glyphosate et au chlorpyrifos seuls ou en mélange. Une autre partie de ce travail a consisté à étudier les effets toxiques des échantillons environnementaux d’eau et de sédiment provenant d’un cours d’eau, La Livenne, à proximité de parcelles viticoles. Toutes les expériences ont été faites en conditions contrôlées de laboratoire. Les réponses induites par ces expositions ont été mesurées à différents niveaux d’organisation biologique : au niveau moléculaire, phénotypique et comportemental pour l’étude in vivo (larves de la truite arc-en-ciel) ; et l’analyse des effets cytotoxiques de l’induction des espèces réactives de l’oxygène (ROS) et des dommages à l’ADN pour l’étude in vitro (lignée RTL-W1). Les résultats de ce travail ont montré que l’exposition aux pesticides individuels, ou en mélange, chez les larves de truites arc-en-ciel n’a pas produit d’effets létaux aux concentrations testés. En revanche, ces substances ont provoqués différents effets sub-létaux, selon le composé et les concentrations étudiés, dont des effets tératogènes, des perturbations du comportement natatoire, des effets génotoxiques et l’expression différentielle de gènes cibles. Le cuivre s’est avéré le plus toxique provoquant un échec d’éclosion important. Des effets cytotoxiques et une production d’espèces réactives de l’oxygène (ERO) ont été observés sur cellules de truite exposées à des extraits d’eau de rivière. Par ailleurs, des effets comportementaux ont été observés sur les larves de truites exposées pendant 48 h à des sédiments et de l’eau de la Livenne. En conclusion, ces travaux de thèse ont mis en évidence des effets sub-létaux sur les cellules et les stades précoces de développement de truite arc-en-ciel exposés à des concentrations environnementales de pesticides utilisés en viticulture.
(11/01/2019)
EPOC, EPHE, PSL, UB, INSU - CNRS, CNRS