The Upper Eocene South Pyrenean Coastal deposits (Liedena sandstone, navarre): Sedimentary facies, benthic formanifera and avian ichnology

Payros, Aitor; Astibia, H.; Cearreta, Alejandro; Suberbiola, Xabier Pereda; Murelaga, Xabier; Badiola, Ainara

doi:10.1007/bf02562569

Cited by 27 publications

(28 citation statements)

References 32 publications

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“…2). Lateral variations in facies and thicknesses record the synsedimentary tectonic deformation of the study area (Cendon et al, 1998;Payros et al, 2000), as it progressively became a detached piggy-back basin atop of southward displacing thrust sheets. Owing to the concomitant tectonic uplift, the Gendulain Formation records the last episode of deltaic progradation from the ESE, the closure of the South Pyrenean Sea, and its definite evolution into terrestrial conditions.…”

Section: Bay Of Biscaymentioning

confidence: 99%

“…These micropalaeontological data are added to those made in Arraitza (level ARR1.1), in Ardanatz (levels AD2.1 and AD3.1), and in the Liédena Sandstone (Liédena and other localities, facies B1, B3 and B4) (in Payros et al, 2000;Astibia et al, 2014).…”

Section: Pamplona Fmmentioning

confidence: 99%

“…The studied section culminates with the intertidal deposits of the Liédena Sandstone (Gendulain Formation) containing benthic microforaminifera of the Priabonian and abundant trace fossils of invertebrates and aquatic birds (Payros et al, 2000;Astibia et al, 2007). Identified invertebrate trace fossils in Liédena Sandstone are Cochlichnus isp., Palaeophycus tubularis and vertical tubes (Fig.…”

Section: Gendulain Formation (Liédena Sandstone Member)mentioning

confidence: 99%

“…indicates a relatively confined marginal marine environment for these deposits (Payros et al, 2000).…”

Section: Gendulain Formation (Liédena Sandstone Member) (Fig 7)mentioning

confidence: 99%

“…Macropalaeontological works on the bivalve Dimya pamplonensis (Calzada and Astibia, 1996), turtles and sirenians (Astibia et al, 1999;Buffrénil et al, 2008), and sponges and corals (Astibia et al, 2014) have been published in the latest years. Avian ichnofossils from the Gendulain Formation were cited and described in Mangin (1959Mangin ( -1960, Raaf et al (1965), Payros et al (2000), Astibia et al (2007), and Astibia et al (in press).…”

Section: Introductionmentioning

confidence: 99%

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Fossil associations from the middle and upper Eocene strata of the Pamplona Basin and surrounding areas (Navarre, western Pyrenees)

Astibia

Payros

Ortíz³

et al. 2016

Journal of Iberian Geology

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Fossil associations from the middle and upper Eocene (Bartonian and Priabonian) sedimentary succession of the Pamplona Basin are described. This succession was accumulated in the western part of the South Pyrenean peripheral foreland basin and extends from deep-marine turbiditic (Ezkaba Sandstone Formation) to deltaic (Pamplona Marl, Ardanatz Sandstone and Ilundain Marl formations) and marginal marine deposits (Gendulain Formation). The micropalaeontological content is high. It is dominated by foraminifera, and common ostracods and other microfossils are also present. The fossil ichnoasssemblages include at least 23 ichnogenera and 28 ichnospecies indicative of Nereites, Cruziana, and ?Scoyenia-Mermia ichnofacies. Body macrofossils of about 80 taxa corresponding to macroforaminifera, sponges, corals, bryozoans, brachiopods, annelids, molluscs, arthropods, echinoderms and vertebrates have been identified. Both the number of ichnotaxa and of species (e. g. bryozoans, molluscs and condrichthyans) may be considerably higher. Body fossil assemblages are comparable to those from the Eocene of the Nord Pyrenean area (Basque Coast), and also to those from the Eocene of the west-central and eastern part of South Pyrenean area (Aragon and Catalonia). At the European scale, the molluscs assemblages seem endemic from the Pyrenean area, although several Tethyan (Italy and Alps) and Northern elements (Paris Basin and Normandy) have been recorded. Palaeontological data of studied sedimentary units fit well with the shallowing process that throughout the middle and late Eocene occurs in the area, according to the sedimentological and stratigraphical data.Se describen las asociaciones fósiles del Eoceno medio y superior (Bartoniense y Priaboniense) de la sucesión sedimentaria de la Cuenca de Pamplona. Esta sucesión se acumuló en la parte oeste de la Cuenca de antepaís periférica surpirenaica y comprende desde turbiditas marinas profundas (Formación Areniscas de Ezkaba) hasta depósitos deltaicos (Formaciones Margas de Pamplona, Areniscas de Ardanatz y Margas de Ilundain) y marinos marginales (Formación Gendulain). El contenido micropaleontológico es alto y está dominado por los foraminíferos. Los fósiles de ostrácodos y otros organismos son también abundantes. Las asociaciones de icnofósiles incluyen al menos 23 icnogéneros y 28 ichnoespecies, indicativas de las icnofacies de Nereites, Cruziana, y ?Scoyenia-Mermia. Se han identificado fósiles corporales de unos 80 taxones, correspondientes a macroforaminíferos, esponjas, corales, briozoos, braquiópodos, anélidos, moluscos, artrópodos, equinodermos y vertebrados. El número de icnotaxones y de especies (p. e. briozoos, moluscos gasterópodos, bivalvos y peces condríctios) puede ser considerablemente mayor. Las asociaciones de fósiles corporales son comparables a las del Eoceno del Área norpirenaica (Costa vasca) y de las partes central y este del Área surpirenaica (Aragón y Cataluña). A escala europea, la asociación de moluscos parece endémica del Área pirenaica,...

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Section: Bay Of Biscaymentioning

confidence: 99%

Section: Pamplona Fmmentioning

confidence: 99%

Section: Gendulain Formation (Liédena Sandstone Member)mentioning

confidence: 99%

“…indicates a relatively confined marginal marine environment for these deposits (Payros et al, 2000).…”

Section: Gendulain Formation (Liédena Sandstone Member) (Fig 7)mentioning

confidence: 99%

Section: Introductionmentioning

confidence: 99%

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Fossil associations from the middle and upper Eocene strata of the Pamplona Basin and surrounding areas (Navarre, western Pyrenees)

Astibia

Payros

Ortíz³

et al. 2016

Journal of Iberian Geology

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Trace fossils from the Middle and Upper Eocene (Bartonian–Priabonian) molasse deposits of the Pamplona Basin (Navarre, western Pyrenees): palaeoenvironmental implications

et al. 2016

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An ichnological study was carried out in the Middle-Upper Eocene sedimentary succession of the Pamplona Basin. This succession represents the molasse stage of the western part of the South Pyrenean peripheral foreland basin and extends from deep-marine turbiditic (Ezkaba Sandstone Formation) to deltaic (Pamplona Marl, Ardanatz Sandstone and Ilundain Marl formations) and marginal marine deposits (Liédena Sandstone Member, Gendulain Formation). The tectonosedimentary evolution of the basin can also be recognized by means of the ichnoassemblages preserved throughout the succession and by the ichnofacies analysis. A total of 23 ichnogenera and at least 28 ichnospecies have been identified. The assemblage of the Ezkaba Sandstone is characteristic of the deep-sea Nereites ichnofacies. The Ophiomorpha rudis and the Paleodictyon ichnosubfacies can be differentiated in this unit, which are typical of channel axis and off-axis environments. Trace fossils in the Ardanatz Sandstone and Ilundain Marl formations, with dominance of Thalassinoides and especially Ophiomorpha, could be related to the Cruziana ichnofacies, developed in relatively low-energy environments, in semicohesive muddy substrates with intercalated silt and sand. The ichnofauna of the Liédena Sandstone Member is composed of bird tracks, and invertebrate horizontal and vertical structures. Microbial mat impressions also occur. The evidence suggests that microbial mats acted as a taphonomic bias favouring the preservation of vertebrate tracks and conditioning the presence of other trace fossils. Consequently, the assignation of this ichnofauna to a specific ichnofacies is tentative, most likely a combination of the Mermia and Scoyenia ichnofacies.

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Alpine Foreland Basins

Barnolas

Larrasoaña

Pujalte

et al. 2019

The Geology of Iberia: A Geodynamic Approach

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The Upper Eocene South Pyrenean Coastal deposits (Liedena sandstone, navarre): Sedimentary facies, benthic formanifera and avian ichnology

Cited by 27 publications

References 32 publications

Fossil associations from the middle and upper Eocene strata of the Pamplona Basin and surrounding areas (Navarre, western Pyrenees)

Fossil associations from the middle and upper Eocene strata of the Pamplona Basin and surrounding areas (Navarre, western Pyrenees)

Trace fossils from the Middle and Upper Eocene (Bartonian–Priabonian) molasse deposits of the Pamplona Basin (Navarre, western Pyrenees): palaeoenvironmental implications

Alpine Foreland Basins

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