Summary
During the 1960's and the 1970's the Liedena Sandstone was a type deposit for “flysch-like facies” (sandstone and lutite alternations) of coastal sedimentary systems. However, the depositional system of these beds was never accurately defined. The sedimentological analysis along 100 km of outcrops in the western part of the South Pyrenean Zone (Navarre) allows these peculiar facies to be assigned to a mixed intertidal flat. Furthermore, sandy beach facies, different types of heterolithic, backbarrier deposits and conglomeratic, fluviatile facies have been recognized associated with these intriguing deposits. Generally, a northwestward-facing barrier-island system or wave-dominated delta was the likely depositional environment.
The benthic foraminiferal assemblage in the intertidal deposits exhibits the typical characteristics of a marginal marine environment: extremely high dominance of one species (Pararotalia inermis), low species diversity, and a hyaline dominance with discrete amounts of miliolids. Furthermore, the most abundant species indicates that the Liedena Sandstone was deposited during the Late Eocene.
Abundant footprints of aquatic birds are known in the tidal flat deposits. Six morphotypes have been distinguished: two (types 1 and 2) are ciconiforme-like; type 1 is here assigned to a new ichnotaxon,Leptoptilostipus pyrenaicus and is one of the oldest occurrences of Ciconiiforme-like ischmites in the fossil record. Two other morphotypes (5 and 6) are similar to those of the Charadriiformes and are refeered to asCharadriipeda. Finally, the affinities of the two remainder morphotypes (3 and 4) are unclear, they could have been made by Charadriiformes.
Synsedimentary tectonic activity controlled the evolution of the depositional system, as the area of deposition of the Liedena Sandstone was progressively incorporated into the active thrust sheets of the Pyrenean Orogen during the Late Eocene. The structural uplift and the large amount of sediments derived from the adjacent highlands induced progradation of the depositional system and the definitive retreat of the sea from the South Pyrenean Zone.
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References
Allen, J.R.L. (1984): Sedimentary structures: their character and physical basis. Developments in sedimentology,30, vol. 1 592 pp., vol. 2, 663 pp., Amsterdam (Elsevier).
Archer, A.W., Calder, J.H. &Naylor, R.D., Reid, D.R. &Wightman, W.G. (1995): Invertabrate trace fossils and agglutinated foraminifera as indicators of marine influence within the classic Carboniferous saction at Joggins, Nova Scotia, Canada.—Can. J. Earth Sci.,32, 2027–2039, Ottawa.
Aspler, L.B., Chiarenzelli, J.R. &Bursey, T.L. (1994): Ripple marks in quartz arenites of the Hurwitz Group, Northwest Territories, Canada: evidence for sedimentation in a vast, Early Proterozoic, shallow, fresh-water lake.—J. Sedim. Res.,64, 282–298, Tulsa.
Beaudoin, R. &Gigot, P. (1970): Figures de courant et traces de pattes d'oiseaux associées dans la molasse Miocène de Digne, Basses Alpes (France).—Sedimentology,17, 241–256, Oxford.
Beukes, N.J. (1996): Sole marks and combined flow storm event beds in the Brixton Formation of the siliciclastic Archean Witwatersrand Supergroup, South Africa.—J. Sedim. Res.,66, 567–576, Tulsa.
Boothroyd, J.C. (1985): Tidal inlets and tidal deltas.—In:Davis, R.A. (ed.): Coastal sedimentary environments.—2nd ed., 445–532, New York (Springer).
Buatois, L.A., Mangano, M.G., Maples, C.G. &Lanier, W.P. (1997): The paradox of nonmarine ichnofaunas in tidal rhythmites: integrating sedimentologic and ichnologic data from the Late Carboniferous of eastern Kansas, USA.—Palaios,12, 467–481, Tulsa.
Caplan, M.L. &Moslow, T.F. (1999): Depositional origin and facies variability of a Middle Triassic barrier island complex, Peejay Field, Northeastern British Columbia.—Amer. Assoc. Petrol. Geol. Bull.,83, 128–154, Tulsa.
Cearreta, A. &Murray, J.W. (2000): AMS14C dating of Holocene estuarine deposits: consequences of high-energy and reworked foraminifera.—The Holocene,10, 157–161, London.
Cendon, D.I., Ayora, C. &Pueyo, J.J. (1998): The origin of barren bodies in the Subiza potash deposit, Navarra, Spain: implications for sylvite formation.—J. Sedim. Res.,68, 43–52, Tulsa.
Clerco, S.W.G. &Holst, H.K.H. (1971): Footprints of birds and sedimentary structures from the Subalpine Molasse near Fluhli (Canton of Luzern).—Eclog. Geol. Helv.,64, 63–69, Bale.
Coleman, J.M. & Prior, D.B. (1982): Deltaics environments of deposition.—In:Scholle, P.A. & Spearing, D. (eds.): Sandstone depositional environments.—Amer. Assoc. Petrol. Geol. Mem.,31, 139–178, Tulsa.
Collinson, J.D. (1996) Alluvial sediments.—In:Reading, H.G. (ed.): Sedimentary environments: Processes, facies and stratigraphy. —3rd ed., 37–82, Oxford (Blackwell).
Ellenberger, P. (1980): Sur les empreintes de pas de gros mammiféres de l'Eocène supérieur de Garrigues-Ste-Eulalie (Gard).—Palaeovertebrata, Mém. Jubil. R. Lavocat, 37–38, Montpellier.
Fisher, R.A., Corbett, A.S. &Williams, C.B. (1943): The relationship between the number of species and the number of individuals in a random sample of an animal population.—J. Animal Ecol.,12, 42–58.
Greb, S.F. &Archer, A.W. (1995): Rhythmic sedimentation in a mixed tide and wave deposit, Hazel Patch Sandstone (Pennsylvanian), Eastern Kentucky coal field.—J. Sedim. Res.,65, 96–106, Tulsa.
Grünig, A. (1977): Paläcölologische Untersuchungen an Eozänen Benthonischen Kleinforaminiferen aus Norditalien und Nordspanien. PhD Thesis, Univ Bern, 186 pp., Bern.
Grünig, A. (1985): Systematical description of Eocene benthic foraminifera of Possagno (northern Italy), Sansoain (northern Spain) and Biarritz (Aquitaine, France).—Mem. Sci. Geol.,37, 251–301, Padova.
Guiraud, M. &Plaziat, J.C. (1993): Seismites in the fluviatile Bima sandstones: identification of paleoseisms and discussion of their magnitude in a Cretaceous synsedimentary strike-slip basin (Upper Benue, Nigeria).—Tectonophysics,225, 493–522, Amsterdam.
Haddox, C.A. &Dott, R.H. (1990): Cambrian shoreline deposits in northern Michigan.—J. Sedim. Petrol.,60, 697–716, Tulsa.
Handford, C.R. (1990): Halite depositional facies in a solar salt pond: A key to interpreting physical energy and water depth in ancient deposits?—Geology,18, 691–694, Boulder.
Haq, B.U., Hardenbol, J. & Vail, P.R. (1988): Mesozoic and Cenozoic chonostratigraphy and cycles of sea-level changes.— In:Wilgus, C.K., Hastings, B.S., Kendal, C.G.St.C., Posamentier, H.W., Ross, C.A. & Van Wagoner, J. (eds.): Sea-level changes: an integrated approach.—Soc. Econ. Paleont. Min. spec. publ.,42, 71–108, Tulsa.
Hernandez-Pacheco, F. (1929): Pistas de aves fósiles en el Oligoceno de Peralta de la Sal (Lerida).—Mem. Real Soc. Esp. Hist. Nat.,15, 379–382, Madrid.
Heward, A.P. (1981): A review of wave-dominated clastic shoreline deposits.—Earth. Sci. Rev.,17, 223–276, Amsterdam.
Hoyo, J. del, Elliot, A. &Sargatal, J. (1992): Handbook of the birds of the world.—696 pp., Barcelona (Lynx).
Hunter, R.E., Clifton, H.E. &Phillips, R.L. (1979): Depositional processes, sedimentary structures, and predicted vertical sequences in barred nearshore systems, northern Oregon coast.— J. Sedim. Petrol.,49, 711–726, Tulsa.
Jenkins, D.G. &Murray, J.W. (1981) (eds.): Stratigraphical Atlas of Fossil Foraminifera.—1–310, Chichester (Ellis Horwood Limited).
Lanier, W.P., Feldman, H.R. &Archer, A.W. (1993): Tidal sedimentation from a fluvial to estuarine transition, Douglas Group, Missourian-Virgilian, Kansas.—J. Sedim. Petrol.,63, 860–873, Tulsa.
Leon-Chirinos, T. (1985): Etude sédimentologique et reconstitution du cadre géodynamique de la sédimentation détritique fini-Eocène-Oligocène dans le bassin sud-Pyrenéen entre Sanguesa et Pamplona.—PhD Thesis, Univ. Pau, 247 pp., Pau.
Mangin, J.P. (1962): Traces de pattes d'oiseaux et flute-casts associés dans un “facès flysch” du Tertiaire Pyrenéen.—Sedimentology,1, 163–166, Oxford.
McCubbin, D.G. (1982): Barrier-island and strand-plain facies.— In:Scholle, P.A. & Spearing, D. (eds.): Sandstone depositional environments.—Amer. Assoc. Petrol. Geol. Mem.,31, 247–279, Tulsa.
Moussa, M.T. (1968): Fossil tracks from the Green River Formation (Eocene) near Soldier Summit, Utah.—J. Paleont.,42, 1433–1438.
Murray, J.W. &Wright, C.A. (1974): Palaeogene formaniferida and palaeoecology, Hampshire and Paris Basins and the English Channel.—The Palaeontol. Assoc., Special papers in Palaeoecology,14, 1–129, London.
Mutti, E., Luterbacher, L., Ferrer, J. &Rosell, J. (1972): Schema stratigrafico e lineamenti di facies del Paleogeno marino della zona centrale sudpirenaica tra Tremp (Catalogne) e Pamplona (Navarra).—Mem. Soc. Geol. Italia,11, 391–416, Roma.
Myrow, P.M. &Southard, J.B. (1996): Tempesite deposition.—J. Sedim. Res.,66, 875–887, Tulsa.
Olson, S.L. (1978): Multiple origins of the Ciconiiformes.—Proc. Conf. Colonial Waterbird Group, 165–170, Charleston.
Olson, S.L. (1985): The fossil record of birds.—Avian Biology,8, 79–238, Orlando.
Orti, F., Pueyo, J.J. &Rosell, L. (1985): La halite du bassin potassique sud-pyrenéen (Eocène superieur, Espagne).—Bull. Soc. Géol. France,6, 863–872, Paris.
Orti, F., Salvany, J.M., Rosell, L., Pueyo, J.J. & Ingles, M. (1986): Evaporitas antiguas (Navarra) y actuales (Los Monegros) de la Cuenca del Ebro.—XI Congr. Esp. Sedim., Exc., 2.1–2.36, Barcelona.
Panin, N. (1964): Coexistenta urmelor de pasi de vertebrata cu mecanoglifele in molasa miocena din Carpatii Orientali.—St. Cerc. Geol., Geof., Geogr. Serie Geol.,9, 141–163, Bucuresti.
Panin, N. &Avram, E. (1962): Noi urme devertebrate in Miocenul Subcarpatilor Rominesti.—St. Cerc. Geol., Geol., Geogr., Serie Geol.,3/4, 455–484, Bucuresti.
Payros, A., Pujalte, V. &Oruf-Etxebarria, X. (1999): The South Pyrenean Eocene carbonate megabreccias revisited: new interpretation based on evidence from the Pamplona Basin.—Sedim. Geol.,125, 165–174, Amsterdam.
Pemberton, S.G., Van Wagoner, J.C. & Wach, G.D. (1992): Ichnofacies of a wave-dominated shoreline.—In:Pemberton, S.G. (ed.): Applications of ichnology to petroleum exploration: a core workshop.—Soc. Econ. Paleont. Min. core workshop,17, 339–382, Calgary.
Plaziat, J.C. (1964): Pistes d'oiseaux et remaniements synsédimentaires dans le Luétien du détroit de Carcassone (Aude).—Bull. Soc. Géol. France,6, 289–293, Paris.
Plaziat, J.C. (1981): Late Cretaceous to Late Eocene palaeogeographic evolution of southwest Europea.—Palaeogeogr., Palaeoclim., Palacoecol.,36, 263–320, Amsterdam.
Posamentier, H.W. & Vail, P.R. (1988): Eustatic controls on clastic deposition II: sequence and systems tract models.—In:Wilgus, C.K., Hastings, B.S., Kendal, C.G.St.C., Posamentier, H.W. Ross, C.A. & Van Wagoner, J. (eds.): Sea-level changes: an integrated approach.— Soc. Econ. Palcont. Min. spec. publ.,42, 125–154, Tulsa.
Puigdefabregas, C. (1975): La sedimentación molásica en la Cuenca de Jaca.—Prineos,140, 1–188 Jaca.
Puigdefabregas, C., Munoz, J.A. &Verges, J. (1992): Thrusting and foreland basin evolution in the Southern Pyrences.—In:Clay, K.R.M. (ed.): Thrust tectonics.—247–254, London (Chapman & Hall).
Raaf, J.F.M. de (1964): The occurrence of flute casts and peudomorphs after salt crystals in the Oligocene “gress a ripplemarks” of the Southern Pyrenes.—Developments in Sedimentology,3, 192–198, Amsterdam (Elsevier)
Raaf, J.F.M. de, Beets, C., Kortenbout van der Sluijs, G. (1965): Lower Oligocene bird-tracks from northern Spain.—Nature,207, 146–148, London.
Raaf, J.F.M. de, Boersma, J.R. &Van Gelder, A. (1977): Wavegenerated structures and sequences from a shallow marine succession, Lower Carboniferous, County Cork, Ireland.—Sedimentology,24, 451–483, Oxford.
Reading, H.G. &Colinson, J.D. (1996): Clastic coats.—In:Reading, H.G. (ed.): Sedimentary environments: Processes. facies and stratigraphy.—3rd ed., 154–231, Oxford (Blackwell).
Reineck, H.E. &Wunderlich, F. (1968): Classification and origin of flaser and lenticular bedding.—Sedimentology,11, 99–104, Oxford.
Roep, T.B., Befts, D.J., Dronkert, H. &Pagnier, H. (1979): A prograding coastal sequences of wave-built structures of Messinian age. Sorbas, Almeria, Spain.—Sedim. Geol.,22, 135–163, Amsterdam.
Rossetti, D.F. (1997): Internal architecture of mixed tide- and storm-influenced deposits: an example from the Alcantara Formation, northern Brazil.—Sedim. Geol.,114, 163–188, Amsterdam.
Scrivner, P.J. &Bottjer, D.J. (1986): Neogene avian and mammalian tracks from Death Valley National Monument, California: their context, classification and preservation.—Palaeogeogr. Palacoclim., Palaeoccol.,57, 285–331, Amsterdam
Smith, A.G., Smith, D.G. &Funnell, M. (1994): Atlas of Mesozoic and Cenozoic coastlines.—99 pp., Cambridge (Cambridge University Press)
Stollihofen, H. (1998): Facies architecture variations and seismogenic structures in the Carboniferous-Permian Saar-Nahe Basin (SW Germany): evidence for extension-related transfer fault activity.—Sedim. Geol.,119, 47–83, Amsterdam.
Teixell, A. (1998): Crustal structure and orogenic material budget in the west central Pyrenees.—Tectonics,17, 395–406, Washington
Truc, G. (1978): Lacustrine sedimentation in an evaporitic environment: the Ludian (Palcogene) of the Mormoiron Basin, southeastern France.—Int. Assoc. Sedim., Spec. Publ.,2, 189–203, Oxford.
Vos, R.G. (1981): Deltaic sedimentation in the Devonian of western Libya.—Sedim. Geol.,29, 67–88, Amsterdam.
Weidmann, M. &Reichel, M. (1979): Traces de pattes d'oiseaux dans la Molasse suisse.—Eclog. Geol. Helv.,72, 953–971, Balé.
Weimer, R.J. Howard, J.D. & Lindsay, D.R. (1982): Tidal flats and associated tidal channels.—In:Scholle, P.A. & Spearing, D. (eds.): Sandstone depositional environments.-Amer. Assoc. Petrol. Geol. Mem.,31, 191–245, Tulsa.
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Payros, A., Astibia, H., Cearreta, A. et al. The Upper Eocene South Pyrenean Coastal deposits (Liedena sandstone, navarre): Sedimentary facies, benthic formanifera and avian ichnology. Facies 42, 107–131 (2000). https://doi.org/10.1007/BF02562569
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DOI: https://doi.org/10.1007/BF02562569