EARLY JURASSIC BENTHIC FORAMINIFERAL ECOLOGY FROM THE CENTRAL HIGH ATLAS MOUNTAINS, MOROCCO

Author:

FONVILLE TANNER12,MARTINDALE ROWAN C.1,STONE TRAVIS N.1,SEPTFONTAINE MICHEL3,BODIN STÉPHANE4,KRENCKER FRANÇOIS-NICOLAS4,KABIRI LAHCEN5

Affiliation:

1. 1 The University of Texas at Austin, Department of Earth and Planetary Sciences 2275 Speedway Stop C9000, 78712 Austin, Texas, USA

2. 2 Current Institution: Texas A&M University, Department of Geology and Geophysics 3115 TAMU, 611 Ross St, 77843 College Station, Texas, USA

3. ³1055 Froideville, Switzerland

4. 4 Aarhus University, Department of Geoscience, Høegh-Guldbergs Gade 2, 8000 Aarhus C, Denmark

5. 5 Department of Geoscience, Sciences and Techniques Faculty of Errachidia, Moulay Ismail University, BP 509, Boutalamine-Errachidia, RDT, Morocco

Abstract

Abstract The Central High Atlas Mountains of Morocco have an extensive record of Lower Jurassic deposits from the Tethyan Ocean. In the Amellago region, Ziz Valley, and Dadès Valley several fossilized reef outcrops preserve benthic foraminifera spanning the Pliensbachian and Toarcian stages. This study analyzes benthic foraminiferal assemblage changes across the bi-phased extinctions at the Pliensbachian/Toarcian boundary and the Jenkyns Event (also referred to as the Toarcian Oceanic Anoxic Event). In Pliensbachian samples, assemblages with abundant Glomospira sp., Glomospirella sp., Siphovalvulina sp., Haurania deserta, Placopsilina sp., Mesoendothyra sp., and Everticyclammina praevirguliana are observed. Following both the Pliensbachian/Toarcian boundary event and the Jenkyns Event, benthic foraminiferal density, evenness, and species richness decreased, indicating these communities underwent ecologic stress; however, loss of diversity was most substantial between samples that pre-date and post-date the Jenkyns Event. Whereas the Pliensbachian/Toarcian boundary event coincides with the demise of the large benthic foraminifera Mesoendothyra sp. and Everticyclammina praevirguliana, the Jenkyns Event was detrimental for most clades of benthic foraminifera, including many small, resilient taxa. Based on the evidence provided, we suggest that the Pliensbachian/Toarcian boundary and the Jenkyns Event were distinct events, potentially caused by distinct environmental perturbations.

Publisher

Society for Sedimentary Geology

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