M
Matías Reolid
Researcher at University of Jaén
Publications - 164
Citations - 2884
Matías Reolid is an academic researcher from University of Jaén. The author has contributed to research in topics: Foraminifera & Trace fossil. The author has an hindex of 28, co-authored 147 publications receiving 2301 citations. Previous affiliations of Matías Reolid include Claude Bernard University Lyon 1 & University of Granada.
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Benthic foraminiferal morphogroups of mid to outer shelf environments of the Late Jurassic (Prebetic Zone, southern Spain): Characterization of biofacies and environmental significance
TL;DR: In this article, foraminiferal assemblages belonging to a mixed carbonate-siliciclastic shelf succession of the Upper Jurassic in the Prebetic, southern Spain, were analyzed.
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Foraminiferal Assemblages as Palaeoenvironmental Bioindicators in Late Jurassic Epicontinental Platforms: Relation with Trophic Conditions
TL;DR: Foraminiferal assemblages from the neritic environment reveal the palaeoecological impact of nutrient types in relation to shore distance and sedimentary setting as discussed by the authors, showing that benthic foraminifera increased in diversity and proportion of epifauna from eutrophic to oligotrophic conditions.
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Foraminiferal morphogroups in dysoxic shelf deposits from the Jurassic of Spitsbergen
TL;DR: In this paper, the analysis of benthic foraminiferal assemblages was performed in Bathonian to Kimmeridgian deposits through a section covering the lower half of the Agardhfjellet Formation in central Spitsbergen.
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The Early Toarcian Oceanic Anoxic Event in the External Subbetic (Southiberian Palaeomargin, Westernmost Tethys): Geochemistry, nannofossils and ichnology
TL;DR: The analysis of macroinvertebrates, trace fossils, calcareous nannofossils and geochemistry from Pliensbachian to Lower Toarcian deposits of the Subbetic (Southern Spain) allows us to interpret the incidence of the T-OAE in the boundary between the Tethys and the Hispanic Corridor as discussed by the authors.
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The Toarcian oceanic anoxic event in the Western Saharan Atlas, Algeria (North African paleomargin): Role of anoxia and productivity
TL;DR: This paper used an integrated analysis of benthic foraminiferal assemblages, geochemical proxies (paleoproductivity, redox, and detrital proxies), and C and O stable isotopes to characterize the Toarcian oceanic anoxic event along the North African paleomargin, more precisely in the Saharan Atlas.