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Silvia Ortiz

Researcher at University of the Basque Country

Publications -  39
Citations -  1077

Silvia Ortiz is an academic researcher from University of the Basque Country. The author has contributed to research in topics: Foraminifera & Stratotype. The author has an hindex of 17, co-authored 39 publications receiving 961 citations. Previous affiliations of Silvia Ortiz include University College London & University of Zaragoza.

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Extinction and recovery of benthic foraminifera across the Paleocene–Eocene Thermal Maximum at the Alamedilla section (Southern Spain)

TL;DR: A complete succession of lower bathyal-upper abyssal sediments was deposited across the Paleocene-Eocene Thermal Maximum (PETM) at Alamedilla (Betic Cordillera, Southern Spain), where the benthic foraminiferal turnover and extinction event associated with the negative carbon isotope excursion (CIE) across the PETM have been investigated as discussed by the authors.
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The Paleocene–Eocene thermal maximum: New data on microfossil turnover at the Zumaia section, Spain

TL;DR: In this paper, the benthic foraminiferal turnover and extinction event associated with the negative carbon isotope excursion (CIE) across the Paleocene-Eocene Thermal Maximum (PETM) is analyzed in the Zumaia section (Spain), one of the most complete and expanded deep-water sequences known worldwide.
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The Global Stratotype Section and Point (GSSP) for the base of the Lutetian Stage at the Gorrondatxe section, Spain

TL;DR: The GSSP for the base of the Lutetian Stage (early/middle Eocene boundary) is defined at 167.85 metres in the Gorrondatxe sea-cliff section (NW of Bilbao city, Basque Country, northern Spain; 43o22'46.47" N, 3o 00' 51.61" W). This dark marly level coincides with the lowest occurrence of the calcareous nannofossil Blackites inflatus (CP12a/b boundary), is in the middle of polarity Chron C21
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Palaeoenvironmental turnover across the Palaeocene/Eocene boundary at the Stratotype section in Dababiya (Egypt) based on benthic foraminifera

TL;DR: The first detailed analysis of Palaeocene-Eocene benthic foraminifera from Dababiya, in order to infer the palaeoenvironmental turnover across the P/E boundary was presented in this paper.