Ferretti, Annalisa

Sch\uf6nlaub, Hans Peter

Schönlaub, Hans Peter

FERRETTI, Annalisa

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42Plöcken Formationhans-Peter sChönlauB & annalisa FerrettiÖsterreichische Karte 1:50.000 Carta Topografica d’Italia 1:50.000Blatt BMN 197 Kötschach Foglio 018 Passo di Monte Croce CarnicoBlatt BMN 198 Weißbriach Foglio 032 TolmezzoBlatt BMN 199 HermagorBlatt UTM 3109 OberdrauburgBlatt UTM 3110 Kötschach-MauthenBlatt UTM 3116 Sonnenalpe NaßfeldBlatt UTM 3117 Nötsch im GailtalDefinitionCoarse-grained indistinctly bedded impure grayish to blackish limestones, which grade into calcareous pyritiferous sand-stones. DescriptionIn the lower part of the indistinctly bedded Plöcken Formation grayish shales to siltstones occur followed by impure limestones with contorted deformation structures, slumpings, channel fillings, graded beds. Loosely packed matrix-sup-ported subangular clasts of varying composition and the accumulation of fossil debris are common. This part strong-ly resembles diamictites. The upper part is composed of calcareous pyritiferous sandstones. Fossils comprise very few graptolites, brachiopods belonging to the Hirnantia Fauna and conodonts. Fossil contentAcritarchs, bivalves, brachiopods, cephalopods, chitinozoans, conodonts, echinoderms, foraminifers, gastropods, grap-tolites, ostracodes, sponge spiculae, trilobites. Areas of outcrop of the Plöcken Formation with indication of the stratotype (asterisk) and reference section (square). 43Depositional environmentMarine sediments, which are strongly marked by the Late Ordovician glacial event. The influence of the Hirnantian ice age is characterized by diamictites, channeling, erosion and local non-deposition (sChönlauB, 2000; sChönlauB et al., 2011; haMMarlund et al., 2012).StratotypeCellon Section (Beds 5-8 after Walliser, 1964), located in an avalanche gorge in the eastern slope of Mt. Cellon/Creta di Collinetta (Gaertner, 1931) at coordinates N 46°36’32”, E 13°29’03”.Reference sectionsRauchkofel South Section (sChönlauB, 1971, 1988), located on the southern slope of Mt. Rauchkofel, at coordinates N 46°36’58.5”, E 12°53’23.0”, where clear evidence of diamictite layers is present.Type areaCentral Carnic Alps.Main outcrop areasPlöckenpass, Uqua Valley, Western Karavanke Alps, Hoher Trieb-Elferspitz, Oberbuchach, Nölblinggraben, Rauchkofel South, Mt. Pizzul.ThicknessFrom 1.5 to a maximum of 9 m at the Rauchkofel South section (6.17 m at the Cellon Stratotype).The Cellon Section. a) log of the Ordovician part of the section (modified after ScHönlaub et al., 2011); b) view of the section (photo H.P. ScHönlaub).44BoundariesUnderlying units – Uqua Formation (disconformable contact).Overlying units – Kok Formation (disconformable contact).Lateral units – Bischofalm Formation (?).Derivation of nameAfter the geographic designation “Plöcken” in the central Carnic Alps.Synonymy Untere Schichten: Gaertner (1931).Bereich I [partim]: Walliser (1964).Mikrofazies-Schicht 2: “Schillsandstein” und Mikrofazies-Schicht 3 “Gradierte Sandsteine”: sChönlauB (1969).Grès Fins et Siltstones: vai (1971).Grès Moyens: vai (1971).Plöcken-Formation: sChönlauB et al. (1994), suttner et al. (2014).Chronostratigraphic ageOrdovician: Hirnantian.Views of the Plöcken Formation at Rauchkofel South Section. a) view of the section (photo H.P. ScHönlaub); b) detail of the Plöcken Formation containing ice-rafted (?) carbonate lithoclasts (photo H.P. ScHönlaub); c) micrograph of diamictite (photo H.P. ScHönlaub).45Biostratigraphy Conodonts. – Amorphognathus ordovicicus Zone (Ferretti & sChönlauB, 2001).Graptolites. – Metabolograptus persculptus Zone (ŠtorCh & sChönlauB, 2012).Chitinozoans. – Tanuchitina elongata Zone (PrieWalder, 1997).Complementary referencesGeochemistry. – sChönlauB et al. (2011). Iron, sulfur and carbon isotope geochemistry has been recently investigated. A distinctive carbonate δ13C excursion occurring at the unconformity between the underlying Uqua Formation and the Plöcken Formation in the Cellon section has been correlated with the prominent HICE carbonate δ13C peak (BerGströM et al., 2009), confirming the Hirnantian age of the Plöcken Formation (sChönlauB et al., 2011). The diagnostic brachiopod Hirnantia Fauna is reported as well at the base of the formation (sChönlauB et al., 2011 and references therein). RemarksThe conodont fauna so far recorded from the Cellon Section (Ferretti & sChönlauB, 2001) represents the only Hirnantian conodont fauna recorded and described along the Ordovician northern Gondwana margin. Several K-bentonites levels (asterisks in the log of Cellon Section) were described and discussed by histon et al. (2007).In the western Karavanke Alps the equivalents of the Uqua Formation are exposed in the Feistritzgraben section (jaeGer et al., 1975; sChönlauB, 1980).ReferencesBerGströM, s.M., Chen, x., Gutiérrez-MarCo, j.-C. & dronov, a. (2009): The new chronostratigraphic classification of the Ordovi-cian System and its relations to regional series and stages and to δ13C chemostratigraphy. – Lethaia, 42, 97–107, Oslo.Ferretti, A. & sChönlauB, H.P. (2001): New conodont faunas from the Late Ordovician of the Central Carnic Alps, Austria. – Bolletti-no della Società Paleontologica Italiana, 40/1, 3–15, Modena.Gaertner, H.R. von (1931): Geologie der Zentralkarnischen Alpen. – Denkschrift der Österreichischen Akademie der Wissen-schaften, mathematisch-naturwissenschaftliche Klasse, Abteilung 1, 102, 113–199, Wien.haMMarlund, e.u., dahl, t.W., harPer, d.a.t., Bond, d.P.G., nielsen, a.t., BjerruM, C.j., sChovsBo, n.h., sChönlauB, h.P., zalasieWiCz, j.a. & CanField, d.e. (2012): A sulfidic driver for the end-Ordovician mass extinction. – Earth and Planetary Science Letters, 331–332, 128–139, Amsterdam.histon, K., Klein, P., sChönlauB, H.P. & huFF, W.D. (2007): Lower Paleozoic K-bentonites from the Carnic Alps, Austria. – Mitteilun-gen der Österreichischen Geologischen Gesellschaft, 100, 26–42, Wien.jaeGer, h., havliCeK, v. & sChönlauB, H.P. (1975): Biostratigra-phie der Ordovizium/Silur-Grenze in den Südalpen – Ein Beitrag zur Diskussion um die Hirnantia-Fauna. – Verhandlungen der Geo-logischen Bundesanstalt, 1975, 271–289, Wien.PrieWalder, H. (1997): The distribution of the Chitinozoans in the Cellon Section (Hirnantian – Lower Lochkovian) – A preliminary report. – In: sChönlauB, H.P. (ed.): IGCP-421 North Gondwanan Mid-Palaeozoic Biodynamics, Guidebook. – Berichte der Geolo-gischen Bundsanstalt, 40, 74–85, Wien.sChönlauB, h.P. (1969): Das Paläozoikum zwischen Bischofalm und Hohem Trieb (Zentrale Karnische Alpen). – Jahrbuch der Geo-logischen Bundesanstalt, 112/2, 265–320, Wien.sChönlauB, h.P. (1971): Paleoenvironmental Studies at the Boundary Ordovician/Silurian in the Carnic Alps. – Mémories du Bureau de Recherches géologiques et Minières, 73, 367–376, Paris.sChönlauB, H.P. (1980): Carnic Alps. Field Trip A. with contribu-tions from jaeGer, h., house, M.r., PriCe, j.d., Göddertz, B., PrieWalder, h., Walliser, o.h., Kříž, j., haas, W. & vai, G.B. – In: sChönlauB, H.P. (ed.): Second European Conodont Symposium, ECOS II, Guidebook, Abstracts. – Abhandlungen der Geologi-schen Bundesanstalt, 35, 5–57, Wien.sChönlauB, H.P. (1988): The Ordovician-Silurian boundary in the Carnic Alps of Austria. – In: CoCKs, l.r.M. & riCKards, r.B. (eds.): A Global Analysis of the Ordovician - Silurian Boundary. – Bulletin of the British Museum (Natural History), Geology, 43, 107–115, London.sChönlauB, H.P. (2000): The Ordovician of the Southern Alps. – Mitteilungen der Österreichischen Geologischen Gesellschaft, 91, 39–51, Wien.sChönlauB, h.P., Kreutzer, l.h. & PrieWalder, H. (1994): Section 2 - Cellon section – In: sChönlauB, H.P. (ed.): Field Meeting East-ern + Southern Alps, Austria, Guidebook + Abstracts. – Berichte der Geologischen Bundesanstalt, 30, 83–93, WiensChönlauB, h.P., Ferretti, a., GaGGero, l., haMMarlund, e., harPer, d.a.t., histon, K., PrieWalder, h., sPötl, C., ŠtorCh, P. (2011): The Late Ordovician glacial event in the Carnic Alps (Aus-tria). – In: Gutiérrez-MarCo, j.C., ráBano, i., GarCia-Bellido, D. (eds.): Ordovician of the World. – Instituto Geológico y Minero de Espana, Cuadernos del Museo Geominero, 14, 515–526, Madrid.ŠtorCh, P. & sChönlauB, h.P. (2012): Ordovician-Silurian bound-ary graptolites of the Southern Alps, Austria. – Bulletin of Geosci-ences, 87/3, 755–766, Prague. suttner, t.j., sChönlauB, h.P. & Ferretti, a. (2014): Plöcken-Formation/Plöcken Formation. – In: Piller, W.e. (ed.): The lithostratigraphic units of the Austrian Stratigraphic Chart 2004 (sedimentary successions), Vol. I - The Paleozoic Era(them). – Abhandlungen der Geologischen Bundesanstalt, 66, 66, Wien.vai, G.B. (1971): Ordovicien des Alpes Carniques. – Mémories du Bureau de Recherches géologiques Minières, 73, 437–449, Paris.Walliser, O.H. (1964): Conodonten des Silurs. – Abhandlungen des Hessischen Landes-Amtes für Bodenforschung, 41, 1–106, Wiesbaden.

Pl\uf6cken Formation

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