Stephan J. Jorry
IFREMER
89 Papers
500 Citations
Stephan J. Jorry is an academic researcher from IFREMER. The author has contributed to research in topics: Glacial period & Volcano. The author has an hindex of 23, co-authored 82 publications. Previous affiliations of Stephan J. Jorry include Rice University & University of Geneva.
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Papers
Rare earth elements and neodymium isotopes in world river sediments revisited
Germain Bayon,Germain Bayon,Samuel Toucanne,Charlotte Skonieczny,Luc André,Sylvain Bermell,Sandrine Cheron,Bernard Dennielou,Joel Etoubleau,Nicolas Freslon,Nicolas Freslon,T. Gauchery,Yoan Germain,Stephan J. Jorry,Guillemette Ménot,Laurence Monin,Emmanuel Ponzevera,Marie-Laure Rouget,Marie-Laure Rouget,Kazuyo Tachikawa,Jean-Alix Barrat +20 more
TL;DR: In this paper, the authors report on elemental concentrations and neodymium (Nd) isotopic compositions for a large number of sediments collected near the mouth of rivers worldwide, including some of the world's major rivers.
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Bundled turbidite deposition in the central Pandora Trough (Gulf of Papua) since Last Glacial Maximum: Linking sediment nature and accumulation to sea level fluctuations at millennial timescale
Stephan J. Jorry,André W. Droxler,Gianni Mallarino,Gerald R. Dickens,Samuel J. Bentley,Luc Beaufort,Larry C. Peterson,Bradley N. Opdyke +7 more
TL;DR: In this paper, three cores (MV-33, MV-66 and MD-40) collected in the central part of Pandora Trough (Gulf of Papua) have been analyzed, and they reveal a detailed sedimentary pattern at millennial timescale Siliciclastic turbidites disappeared during the Bolling-Allerod and Preboreal intervals to systematically reoccur during the Younger Dryas interval.
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Tracking rainfall in the northern Mediterranean borderlands during sapropel deposition
Samuel Toucanne,Charlie Morelle Angue Minto'o,Christophe Fontanier,Maria-Angela Bassetti,Stephan J. Jorry,Gwenael Jouet +5 more
TL;DR: The role of mid-latitude precipitation in the hydrological forcing leading to the deposition of sapropels in the Mediterranean Sea remains unclear as mentioned in this paper, however, it is known that during warm intervals of interglacial periods the reduced sea-surface water salinities, together with the high flux of nutrient and organic matter, produced by the monsoonal Nile (and wadi-systems) floods, were maintained throughout the winter by the Mediterranean rainfall.
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Birth of a large volcanic edifice offshore Mayotte via lithosphere-scale dyke intrusion
Nathalie Feuillet,Stephan J. Jorry,Wayne C Crawford,Christine Deplus,Isabelle Thinon,Eric Jacques,Jean Marie Saurel,Anne Lemoine,Fabien Paquet,Claudio Satriano,Chastity Aiken,Océane Foix,Philippe Kowalski,Angèle Laurent,Emmanuel Rinnert,Cecile Cathalot,Jean-Pierre Donval,Vivien Guyader,Arnaud Gaillot,Carla Scalabrin,Manuel A. Moreira,Manuel A. Moreira,Aline Peltier,François Beauducel,François Beauducel,Raphaël Grandin,Valérie Ballu,R. Daniel,Pascal Pelleau,J. Gomez,Simon Besançon,Louis Géli,Pascal Bernard,Patrick Bachèlery,Yves Fouquet,Didier Bertil,Arnaud Lemarchand,Jérôme Van der Woerd +37 more
TL;DR: In this paper, the authors present geophysical and marine data from the MAYOBS1 cruise, which reveal that by May 2019, this activity formed an 820m-tall, 5'km³ volcanic edifice on the seafloor.
Direct sediment transfer from land to deep-sea: Insights into shallow multibeam bathymetry at La Réunion Island
Nathalie Babonneau,Christophe Delacourt,Romain Cancouët,E. Sisavath,E. Sisavath,Patrick Bachèlery,Patrick Bachèlery,Aude Mazuel,Stephan J. Jorry,Anne Deschamps,Jérôme Ammann,Nicolas Villeneuve +11 more
TL;DR: In this paper, a detailed picture of canyon heads off La Reunion Island, with high-resolution multibeam bathymetry in the water depth range of 4-220m, is presented.
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