Please use this identifier to cite or link to this item: http://hdl.handle.net/2445/109021
Title: Stratigraphy and biostratigraphy (charophytes) of the marine-terrestrial transition in the upper eocene of the NE Ebro foreland basin (Catalonia, Spain)
Author: Sanjuan Girbau, Josep
Martín-Closas, Carles
Serra Kiel, Jose
Gallardo, Helena
Keywords: Estratigrafia
Bioestratigrafia
Eocè
Ebre, Conca de l'
Stratigraphic geology
Stratigraphic paleontology
Eocene Epoch
Ebro River Watershead
Issue Date: Mar-2012
Publisher: (UB). (ICTJA). (IDEA). (UAB). (CSIC)
Abstract: The onset of endorheic sedimentation in the Ebro Basin is a prominent feature of the basin's evolution and has recently been characterized as a rapid event occurring in the Early Priabonian. In the north-eastern part of the basin this event coincides with the deposition of the Artés Formation (Fm.), mainly built up by red beds of alluvial origin. The marine-continental boundary has been poorly studied up to now in the so-called Lluçanès area, and what was previously thought to be the base of the Artés Fm. is actually a transitional unit, which we define as the Sant Boi Formation, which covers the underlying marine Milany Depositional Sequence and passes laterally to the Terminal Complex, extending over 15km along the eastern margin of the Ebro Basin. The Sant Boi Fm. is formed by up to 15-20m of alternating siltstones and lutite, grading upwards to brackish and lacustrine marls and lignite, and represents deposition in a brackish to freshwater floodplain. It is characterized biostratigraphically by the fossil charophyte assemblage Harrisichara lineata, Harrisichara vasiformis-tuberculata and Nodosochara jorbae, from the middle part of the Priabonian. In contrast, the overlying red beds of the Artés Fm. are characterized by assemblages containing Harrisichara tuberculata, Nodosochara jorbae and Lychnothamnus longus from the Late Priabonian. These results are largely consistent with recent magnetostratigraphic studies performed south of the studied area, and have enabled us to refine the stratigraphy of the marine-continental transition in the north-eastern Ebro Basin.
Note: Reproducció del document publicat a: https://doi.org/10.1344/105.000001708
It is part of: Geologica Acta, 2012, vol. 10, num. 1, p. 19-31
Related resource: https://doi.org/10.1344/105.000001708
URI: http://hdl.handle.net/2445/109021
ISSN: 1695-6133
Appears in Collections:Articles publicats en revistes (Dinàmica de la Terra i l'Oceà)

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