F
Frans Jorissen
Researcher at University of Angers
Publications - 138
Citations - 13547
Frans Jorissen is an academic researcher from University of Angers. The author has contributed to research in topics: Foraminifera & Benthic zone. The author has an hindex of 58, co-authored 131 publications receiving 12421 citations. Previous affiliations of Frans Jorissen include University of Bordeaux & Centre national de la recherche scientifique.
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Reproduction and growth of the deep-sea benthic foraminifer bulimina marginata under different laboratory conditions
TL;DR: The results of this study should be useful to researchers who wish to set up experiments that require culturing deep-sea foraminifera and to obtain reproduction and growth of the open marine species B. marginata in a limited period of time.
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A 1600 year-long sedimentary record of tsunamis and hurricanes in the Lesser Antilles (Scrub Island, Anguilla)
Maude Biguenet,Maude Biguenet,Pierre Sabatier,Eric Chaumillon,Catherine Chagué,Fabien Arnaud,Frans Jorissen,Thibault Coulombier,Emeline Geba,Louise Cordrie,Pierre Vacher,Anne-Lise Develle,Emilie Chalmin,Fayçal Soufi,Nathalie Feuillet +14 more
TL;DR: In this paper, two sediment cores were taken in March 2018 in a small coastal lagoon on Scrub Island (northeastern Caribbean) to identify 25 sandy layers resulting from high-energy-marine floods.
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Production, preservation and prediction of source-rock facies in deltaic settings
TL;DR: Tyson et al. as discussed by the authors hypothesize that production and preservation of source-rock type facies in deltaic systems, both landward and seaward of a coastline, is mutually exclusive, time-successive and related to the dynamics of relative sea level.
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La distribution du phosphore inorganique dans les sédiments modernes du golfe de Gascogne
TL;DR: The phosphorus geochemistry on the Bay of Biscay margin shows that modern sediments represent a source of phosphate for overlying seawater as mentioned in this paper, however, particulate phosphorus leached with an ascorbate solution and 1 N HCl remains constant in the sedimentary column.
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Stable carbon isotope gradients in benthic foraminifera as proxy for organic carbon fluxes in the Mediterranean Sea
TL;DR: In this paper, stable carbon isotope ratios of epifaunal and shallow infaunal benthic foraminifera in the Mediterranean Sea were determined to relate the inferred gradient of pore water δ13CDIC to varying trophic conditions.