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Stephan J. Jorry

Researcher at IFREMER

Publications -  87
Citations -  2196

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 receiving 1585 citations. Previous affiliations of Stephan J. Jorry include Rice University & University of Geneva.

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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

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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Hydrodynamic behaviour of Nummulites: implications for depositional models

TL;DR: In this paper, it was shown that the high primary skeletal porosity of Nummulites made them easily transportable, and the calculated threshold shear velocities confirm that large-sized Nummulate clasts can be moved by weak wave-driven currents.
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Tracking rainfall in the northern Mediterranean borderlands during sapropel deposition

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.