Publications

Publications

Publications

Publications

Publications

Publications

Publications

Publications

Seasonal and long-term changes in elemental concentrations and ratios of marine particulate organic matter

Agathe Talarmin, Michael W. Lomas, Yann Bozec, Nicolas Savoye, Helene Frigstad, David M. Karl, Adam C. Martiny

What is the temporal variability of the elemental stoichiometry of marine microbial communities across ocean regions? To answer this question, we present an analysis of environmental conditions, particulate organic carbon, nitrogen, and phosphorus concentrations and their ratios across 20 time series (3-25 years duration) representing estuarine, coastal, and open ocean environments. The majority of stations showed significant seasonal oscillations in particulate organic elemental concentrations and ratios. However, shorter-term changes contributed most to overall variance in particulate organic matter concentrations and ratios. We found a correlation between the seasonal oscillations of environmental conditions and elemental ratios at many coastal but not open ocean and estuarine stations. C:N peaked near the seasonal temperature minimum and nutrient maximum, but some stations showed other seasonal links. C:N ratios declined with time over the respective observation periods at all open ocean and estuarine stations as well as at five coastal station but increased at the nine other coastal stations. C:P (but not N:P) declined slightly at Bermuda Atlantic Time-series Study but showed large significant increases at Hawaii Ocean Time-series and Arendal stations. The relationships between long-term changes in environmental conditions and particulate organic matter concentrations or ratios were ambiguous, but interactions between changes in temperature and nutrient availability were important. Overall, our analysis demonstrates significant changes in elemental ratios at long-term and seasonal time scales across regions, but the underlying mechanisms are currently unclear. Thus, we need to better understand the detailed mechanisms driving the elemental composition of marine microbial ecosystems in order to predict how oceans will respond to environmental changes.

(Global Biogeochemical Cycles. vol. 30, n° 0886-6236, pp. 1699-1711, 31/08/2026)

UPMC, EPOC, EPHE, PSL, UB, INSU - CNRS, CNRS

Gene transcription profiling in wild and laboratory-exposed eels: Effect of captivity and in situ chronic exposure to pollution

L. Baillon, F. Pierron, Philippe Pannetier, E. Normandeau, P. Couture, Paul Labadie, H. Budzinski, Patrick Lambert, L. Bernatchez, M. Baudrimont

Aquatic ecosystems are subjected to a variety ofman-induced stressors but also vary spatially and temporally due to variation in natural factors. In such complex environments, it remains difficult to detect, dissociate and evaluate the effects of contaminants in wild organisms. In this context, the aim of this study was to test whether the hepatic transcriptome profile of fish may be used to detect in situ exposure to a particular contaminant. Transcriptomic profiles from laboratory-exposed and wild eels sampled along a contamination gradient were compared. During laboratory experiments, fish were exposed during 45 days to different pollutants (Hg, PCBs, OCPs or Cd) or natural factors (temperature, salinity or lowfood supply) at levels close to those found in the sampling sites. A strong differencewas observed between the transcriptomic profiles obtained fromwild and laboratory-exposed animals (whatever the sites or experimental conditions), Suggesting a general stress induced by captivity in the laboratory. Among the biological functions that were up-regulated in laboratory eels in comparison to wild eels, histonemodification was the most represented. This finding suggests that laboratory conditions could affect the epigenome of fish and thus modulate the transcriptional responses developed by fish in response to pollutant exposure. Among experimental conditions, only the transcription profiles of laboratory animals exposed to cold temperature were correlated with those obtained from wild fish, and more significantly with fish from contaminated sites. Common regulated genes were mainly involved in cell differentiation and liver.

(Science of the Total Environment. vol. 571, n° 0048-9697, pp. 92-102, 31/08/2026)

EPOC, EPHE, PSL, UB, INSU - CNRS, CNRS, IRSTEA, ULaval, UR EABX, IRSTEA

Study of benthic foraminiferal faunas along the French Mediterranean coasts: a new biotic index in the EU Water Framework Directive

Briz Parent, Christine Barras, Frans Jorissen, Erica Bicchi, L. Charrieau, Sabine Schmidt

(31/08/2026)

LPG-ANGERS, LPG, UA, UN UFR ST, UN, INSU - CNRS, CNRS, EPOC, EPHE, PSL, UB, INSU - CNRS, CNRS

Assessing recent trends in high-latitude Southern Hemisphere surface climate

Julie M. Jones, Sarah T. Gille, Hugues Goosse, Isma Abdelkader Di Carlo, Pablo Canziani, Dan Charman, Kyle Clem, Xavier Crosta, Casimir de Lavergne, Ian Eisenman, Matthew H. England, Ryan Fogt, Leela Frankcombe, Gareth Marshall, Valérie Masson-Delmotte, Adele Morrison, Anaïs Orsi, Marilyn Raphael, James Renwick, David Schneider, Graham Simpkins, Eric J. Steig, Barbara Stenni, Didier Swingedouw, Tessa Vance

Understanding the causes of recent climatic trends and variability in the high-latitude Southern Hemisphere is hampered by a short instrumental record. Here, we analyse recent atmosphere, surface ocean and sea-ice observations in this region and assess their trends in the context of palaeoclimate records and climate model simulations. Over the 36-year satellite era, significant linear trends in annual mean sea-ice extent, surface temperature and sea-level pressure are superimposed on large interannual to decadal variability. Most observed trends, however, are not unusual when compared with Antarctic palaeoclimate records of the past two centuries. With the exception of the positive trend in the Southern Annular Mode, climate model simulations that include anthropogenic forcing are not compatible with the observed trends. This suggests that natural variability overwhelms the forced response in the observations, but the models may not fully represent this natural variability or may overestimate the magnitude of the forced response.

(Nature Climate Change. vol. 6, n° 1758-678X, pp. 917-926, 31/08/2026)

SIO - UC San Diego, UC San Diego, UC, UCL-ASTR, UCLouvain, ANU, EPOC, EPHE, PSL, UB, INSU - CNRS, CNRS, NEMO R&D, LOCEAN, IPSL, ENS-PSL, UVSQ, UPMC, CEA, INSU - CNRS, X, CNES, CNRS, MNHN, IRD, UPMC, INSU - CNRS, CNRS, LSCE, UVSQ, INSU - CNRS, CNRS, DRF (CEA), CEA, GLACCIOS, LSCE, UVSQ, INSU - CNRS, CNRS, DRF (CEA), CEA, NCAR

An interlaboratory study on passive sampling of emerging water pollutants

B. Vrana, F. Smedes, R. Prokes, R. Loos, Nicolas Mazzella, Cecile Miege, H. Budzinski, E. Vermeirssen, T. Ocelka, A. Gravell, S. Kaserzon

An inter-laboratory study was organised for the monitoring of emerging aquatic pollutants (pharmaceuticals, pesticides, steroids, brominated diphenyl ethers and others) using passive samplers. Thirty laboratories participated in the sampler comparison exercise. Various samplers designs were exposed at a single sampling site to treated waste water. The organisers deployed in parallel multiple samplers of a single type, which were distributed for evaluation of the contribution of the different analytical procédures to the data variability. Between laboratory variation of results from passive samplers was about factor 5 larger than within laboratory variability. Similar results obtained for different passive samplers analysed by individual laboratories and also low within laboratory variability indicate that the passive sampling process is causing less variability than the analysis. Concentrations in composite water samples were within the range obtained by passive samplers. In future a significant improvement of analytical precision and calibration of adsorption based passive samplers is needed.

(Trends in Analytical Chemistry. vol. 76, n° 0165-9936, pp. 153-165, 31/08/2026)

MU / MUNI, IRSTEA, IRSTEA, JRC, UR EABX, IRSTEA, UR MALY, IRSTEA, EPOC, EPHE, PSL, UB, INSU - CNRS, CNRS, IRSTEA, EAWAG, IRSTEA, IRSTEA, IRSTEA, IRSTEA

Groenland. Climat, écologie, société

Valérie Masson-Delmotte, Emilie Gauthier, David Grémillet, Jean-Michel Huctin, Didier Swingedouw

(pp. 300, 31/08/2026)

LSCE, UVSQ, INSU - CNRS, CNRS, DRF (CEA), CEA, GLACCIOS, LSCE, UVSQ, INSU - CNRS, CNRS, DRF (CEA), CEA, LCE, CNRS, UMLP, UBFC, CEFE, UPVM, INRA, Montpellier SupAgro, EPHE, PSL, UM, CNRS, IRD [Occitanie], IRD, Montpellier SupAgro, CEARC, UVSQ, EPOC, EPHE, PSL, UB, INSU - CNRS, CNRS

Climatic control of sediment transport from the Himalayas to the proximal NE Bengal Fan during the last glacial-interglacial cycle

Ronan Joussain, Christophe Colin, Zhifei Liu, L. Meynadier, Léa Fournier, Kelly Fauquembergue, S. Zaragosi, Frédéric Schmidt, Virjinia Rojas, F. Bassinot

Clay mineralogy, siliciclastic grain-size, major elements, 87Sr/86Sr, and εNd analyses of deep-sea sediments cored in the north-eastern Bay of Bengal are used to reconstruct evolution of detrital sources and sediment transport to the proximal part of the Bengal deep-sea fan during the last climatic cycle. εNd values (−13.3 to −9.7) and 87Sr/86Sr ratios (0.721–0.733) indicate a mixture of sediments originating from the Ganges-Brahmaputra rivers and the Indo-Burman ranges. Interglacial Marine Isotopic Stages (MIS) 5 and 1 are associated with a higher contribution of sediments from the Ganges-Brahmaputra river system than is the case for glacial MIS 6, 4, 3, and 2. Siliciclasitic grain-size combined with Si/Al and Si/Fe ratios indicate coarser glacial sediments with numerous turbidite layers. Glacial turbidite layers display similar clay mineralogical compositions to hemipelagic sediments. Only few of turbidite layers (MIS 6, 4, and 2) are slightly unradiogenic (εNd −13.3), suggesting a higher contribution of Ganges-Brahmaputra river sediments. Independently of changes in the sedimentary sources, the smectite/(illite + chlorite) ratio of cores located on the NE Bengal Fan indicates higher inputs of primary minerals (illite and chlorite) from the highlands of the river basins (relief) during glacial MIS 6, 4, 3, and 2 and an increased contribution of pedogenic minerals (smectite and kaolinite) during interglacial MIS 5 and 1. Maximum smectite/(illite + chlorite) ratios during the warm sub-stages of MIS 5 suggest an intensification of summer monsoon rainfall associated with higher rates of physical erosion of the Indo-Gangetic flood-plain and/or dominant summer hydrological conditions transporting a higher proportion of sediments deriving from the Ganges-Brahmaputra rivers to the NE Bengal Fan. In addition, a higher production of smectite in soils of the Indo-Gangetic flood-plain during periods of intensification of monsoon rainfall cannot be excluded.

(Quaternary Science Reviews. vol. 148:, n° 0277-3791, pp. 1-16 (IF 4,521), 31/08/2026)

GEOPS, UP11, CNRS, IPGP, INSU - CNRS, UPD7, UR, IPG Paris, CNRS, EPOC, EPHE, PSL, UB, INSU - CNRS, CNRS, LSCE, UVSQ, INSU - CNRS, CNRS, DRF (CEA), CEA, PALEOCEAN, LSCE, UVSQ, INSU - CNRS, CNRS, DRF (CEA), CEA

Chronostratigraphie et paléoenvironnements du Pléistocène supérieur sur la bordure sud-Atlantique du Maroc. Les séquences de l'oued supérieur.

Luc Wengler, Abderrahman Ouammou, Jean-Philip Brugal, Pierre Carbonel, Michel Fontugne, F. Magnin, Norbert Mercier, Jean-Louis Reyss

(pp. 206-227, 31/08/2026)

UPVD, LAMPEA, AMU, CNRS, MC, EPOC, EPHE, PSL, UB, INSU - CNRS, CNRS, LSCE, UVSQ, INSU - CNRS, CNRS, DRF (CEA), CEA, GEOTRAC, LSCE, UVSQ, INSU - CNRS, CNRS, DRF (CEA), CEA, OCEANIS, LSCE, UVSQ, INSU - CNRS, CNRS, DRF (CEA), CEA

Monuments vus du ciel. Les apports de la photographie aérienne à l’urbanisme de Tritium Autrigonum (Monasterio de Rodilla, Burgos)

François Didierjean, Laurent Brassous, Benoit Guillot, Ignacio Ruiz Velez

(pp. 327-343, 31/08/2026)

LIENSs, INSU - CNRS, ULR, CNRS, EPOC, EPHE, PSL, UB, INSU - CNRS, CNRS

Groenland. Climat, Ecologie, Société

Valérie Masson-Delmotte, Emilie Gauthier, David Grémillet, Jean-Michel Huctin, Didier Swingedouw

(pp. 300, 31/08/2026)

LSCE, UVSQ, INSU - CNRS, CNRS, DRF (CEA), CEA, LCE, CNRS, UMLP, UBFC, CEFE, UPVM, INRA, Montpellier SupAgro, EPHE, PSL, UM, CNRS, IRD [Occitanie], IRD, Montpellier SupAgro, CEARC, UVSQ, EPOC, EPHE, PSL, UB, INSU - CNRS, CNRS