Micromorphs: Response of the Ammonite Fauna during the Toarcian Oceanic Anoxic Event (T-OAE) in the Es-Saffeh Mountains (Tiaret, Western Algeria)-Reference-Cited by-同舟云学术

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Micromorphs: Response of the Ammonite Fauna during the Toarcian Oceanic Anoxic Event (T-OAE) in the Es-Saffeh Mountains (Tiaret, Western Algeria)

Published:2022-12-02 Issue: Volume: Page:
ISSN:
Container-title:IECG 2022
language:
Short-container-title:

Author:

Bengoudira Fatiha Douas¹,Touahria Abdia²,Sebane Abbes²

Affiliation:

1. Department of Biology, Faculty of Nature and life Sciences, Abdelhamid Ibn Badis University, Mostaganem 27000, Algeria

2. Department of Geology, Faculty of Geology and Universe Science, Benahmed Mohamed University, B.P 1015 El M’naouer, Oran 31000, Algeria

Publisher

MDPI

Link

https://www.mdpi.com/2504-3900/87/1/18/pdf

Reference60 articles.

1. Recovery of the marine fauna in Europe after the end-Triassic and early Toarcian mass extinctions;Hallam;Geol. Soc. Lond. Spec. Publ.,1997

2. The timing of paleoenvironmental change and cause-and-effect relationships during the Early Jurassic mass extinction in Europe;Wignall;Am. J. Sci.,2005

3. Extinction pattern of marine Ostracoda across the Pliensbachian Toarcian boundary in the Cordillera Ibérica, NE Spain: Causes and consequences;Arias;Geobios,2009

4. The Early Toarcian (Early Jurassic) ostracod extinction events in the Iberian Range: The effect of temperature changes and prolonged exposure to low dissolved oxygen concentrations;Arias;Palaeogeogr. Palaeoclimatol. Palaeoecol.,2013

5. Caracterización geoquímica de facies pobremente oxigenadas en el Toarciense inferior (Jurásico inferior) del Subbético Externo;Reolid;Rev. Soc. Geológica España,2013

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