Skip to main content
Log in

A new lowermost middle Cambrian (Series 3, Stage 5) faunule from Saxony (Germany) and its bearing on the tectonostratigraphic history of the Saxothuringian domain

  • Research Paper
  • Published:
Paläontologische Zeitschrift Aims and scope Submit manuscript

Abstract

The core of borehole 1209/78 west of Doberlug–Kirchhain and south of Herzberg in the Torgau–Doberlug Syncline records an atypical lower part of the Tröbitz Formation with thin limestone horizons. These limestone layers include the remains of a low to moderately diverse fauna with the trilobites Protolenus (Hupeolenus) bergstroemi n. sp., Cambrunicornia saxonica n. sp., Ornamentaspis? aff. todraensis Geyer 1990a, Calodiscus? n. sp., the remains of two undetermined olenelloid? and paradoxidid? species, at least two brachiopods (Trematobolus, undetermined acrotretoid), and one hyolith. The fauna clearly suggests a position in the lower Agdzian stage of the West Gondwana chronostratigraphic scheme and correlation with the lowermost to lower Middle Cambrian strata in regions such as the Moroccan Atlas ranges and northern Spain, so the assemblages represent the oldest Middle Cambrian fauna known from the Saxothuringian domain and reconfirm the palaeogeographic position in the Perigondwanan segment. The lithological differences of the fossiliferous cores from those of the typical Tröbitz Formation and the recorded high-energy conditions indicate high-frequency sea-level changes suggesting that this part of the succession may be a late stage of the subglobally recognizable eustatic sea-level fluctuations at the traditional Lower–Middle Cambrian boundary interval.

Kurzfassung

Bohrkerne der westlich von Doberlug–Kirchhain und südlich von Herzberg in der Torgau–Doberlug–Synkline niedergebrachten Bohrung 1209/78 zeigen einen atypisch ausgebildeten unteren Teil der Tröbitz-Formation mit dünnen Kalkstein-Horizonten. Diese Kalkstein-Lagen beinhalten eine gering bis mittelstark diverse Fauna mit den Trilobiten Protolenus (Hupeolenus) bergstroemi n. sp., Cambrunicornia saxonica n. sp., Ornamentaspis? aff. todraensis Geyer 1990, Calodiscus? n. sp., Resten von zwei unbestimmbaren Arten vermutlich olenelloider und paradoxidider Trilobiten, mindestens zwei Brachiopoden (Trematobolus, ein nicht präzise bestimmbarer Acrotretide) sowie einem Hyolithen-Operculum. Die Fauna belegt eine stratigraphische Position im unteren Agdzium der für West-Gondwana gültigen chronostratigraphischen Gliederung und korreliert mit Schichten des untersten bis unteren Mittelkambrium in Regionen wie den marokkanischen Atlas-Ketten und Nord-Spanien. Damit repräsentieren die Vergesellschaftungen die ältesten mittelkambrischen Faunen, die aus dem Saxothuringikum bekannt geworden sind. Sie bestätigen ebenso die paläogeographische Position im Perigondwana-Segment. Die lithologischen Unterschiede der fossilführenden Schichten zur typischen Ausbildung der Tröbitz-Formation und die dokumentierten hochenergetischen Ablagerungsbedingungen lassen hochfrequente Meeresspiegelschwankungen in diesem Teil des Profils vermuten und scheinen eine späte Phase der subglobal nachweisbaren eustatischen Meeresspiegelschwankungen im traditionellen Übergangsbereich Unter-/Mittelkambrium abzubilden.

This is a preview of subscription content, log in via an institution to check access.

Access this article

Price excludes VAT (USA)
Tax calculation will be finalised during checkout.

Instant access to the full article PDF.

Fig. 1
Fig. 2
Fig. 3
Fig. 4
Fig. 5
Fig. 6
Fig. 7
Fig. 8
Fig. 9
Fig. 10
Fig. 11

Similar content being viewed by others

References

  • Ahlberg, P., and J. Bergström. 1978. Lower Cambrian ptychopariid trilobites from Scandinavia. Sveriges Geologiska Undersökning, Avhandlingar och Uppsatser, I 4:o, Ser. Ca, 49.

  • Ahlberg, P., and J. Bergström. 1993. The trilobite Calodiscus lobatus from the Lower Cambrian of Scania, Sweden. Geologiska Föreningens i Stockholm Förhandlingar 115: 331–334.

    Article  Google Scholar 

  • Álvaro, J.J. 2007. New ellipsocephalid trilobites from the lower Cambrian member of the Láncara Formation, Cantabrian Mountains, northern Spain. Memoirs of the Association of Australasian Palaeontologists 34: 343–355.

    Google Scholar 

  • Brause, H., 1969. Das verdeckte Altpaläozoikum der Lausitz und seine regionale Stellung. Abhandlungen der Deutschen Akademie der Wissenschaften Berlin, Klasse für Bergbau, Hüttenwesen und Montangeologie 1968 (1).

  • Brause, H. 1970. Ein neuer wichtiger Aufschluß im Kambrium von Doberlug–Kirchhain. Geologie 19: 1048–1065.

    Google Scholar 

  • Brause, H., and O. Elicki. 1997. Kambrium. In Stratigraphie von Deutschland, II. Ordovizium, Kambrium, Vendium, Riphäikum, Teil I. Courier Forschungsinstitut Senckenberg 200:308–322.

  • Buschmann, B., 1995. Tectonic facies analysis of the Rothstein Formation (Neoproterozoic, Saxothuringian Zone, E Germany). Unpublished Ph.D. Thesis, TU Bergakademie Freiberg.

  • Buschmann, B., U. Linnemann, J. Schneider, and T. Süß. 1995. Die cadomische Entwicklung im Untergrund der Torgau–Doberluger Synklinale. Zeitschrift für Geologische Wissenschaften 23: 729–749.

    Google Scholar 

  • Buschmann, B., O. Elicki, and P. Jonas. 2006. The Cadomian unconformity in the Saxo-Thuringian Zone, Germany: palaeogeographic affinities of Ediacaran (terminal Neoproterozoic) and Cambrian strata. Precambrian Research 147: 387–403.

    Article  Google Scholar 

  • Cederström, P., P. Ahlberg, and E.N.K. Clarkson. 2005. Morphology, ontogeny, and enrollment of the Lower Cambrian eodiscoid trilobite Calodiscus lobatus from Sweden. Geologiska Föreningens i Stockholm Förhandlingar 127: 46.

    Google Scholar 

  • Cederström, O., P. Ahlberg, E.N.K. Clarkson, C.H. Nilsson, and N. Axheimer. 2009. The lower Cambrian eodiscoid trilobite Calodiscus lobatus from Sweden: morphology, ontogeny and distribution. Palaeontology 52: 491–539

    Article  Google Scholar 

  • Cuvier, G., 1798. Tableau élémentaire de l’histoire naturelle des animaux. pp. i–xvi, 1–710. Paris: Baudouin.

  • Dawson, J.W., 1868. Acadian geology. The geological structure, organic remains and mineral resources of Nova Scotia, New Brunswick, and Prince Edward Island, etc. 2nd edn. i–XXVII, 1–694. London: MacMillan and Co.

  • Dies, M.E., and R. Gozalo. 2004. Agnostida (Trilobita) de la Formación Valdemiedes (Leoniense: Cámbrico Medio basal) de las Cadenas Ibéricas (NE de España). Boletín Geológico y Minero 115: 683–698.

    Google Scholar 

  • Dies, M.E., R. Gozalo, and E. Liñán. 2001. Protolenus (Hupeolenus) Geyer 1990 (Trilobita) en el Bilbiliense (Cámbrico Inferior) de Jarque (Zaragoza, Cadenas Ibéricas). In: Los Fósiles y la Paleogeografía. XVII Jornadas de la Sociedad Española de Paleontología, 1820 de octubre 2001, vol. 5.2, 301–309.

  • Dies, M.E., R. Gozalo, and E. Liñán. 2004. Zonación del límite Bilbiliense–Leoniense (Formación Valdemiedes, Cámbrico Inferior–Medio) en las Cadenas Ibéricas. Geo-Tema 6(2): 283–286.

    Google Scholar 

  • Duméril, A.M.C., 1806. Zoologie analytique, ou méthode naturelle de classification des animaux, rendue plus facile à l’aide de tableaux synoptiques. pp. i–xxxiii, 1–344. Paris: Allais.

  • Elicki, O., 1992. Faziesanalyse der unterkambrischen Karbonate Deutschlands. Unpublished Ph.D. Thesis, TU Bergakademie Freiberg.

  • Elicki, O. 1994. Lower Cambrian carbonates from eastern Germany: palaeontology, stratigraphy and palaeogeography. Neues Jahrbuch für Geologie und Paläontologie Abhandlungen 191(1): 69–93.

    Google Scholar 

  • Elicki, O. 1997. Biostratigraphic data of the German Cambrian—present state of knowledge. Paläontologie, Stratigraphie, Fazies psf 4, Freiberger Forschungshefte C 466: 155–165.

    Google Scholar 

  • Elicki, O. 1999. Beitrag zur Lithofacies und zur Lithostratigraphie im Unterkambrium von Doberlug–Torgau. Paläontologie, Stratigraphie, Fazies psf 7, Freiberger Forschungshefte C 481: 107–119.

    Google Scholar 

  • Elicki, O. 2007. Paleontological data from the Early Cambrian of Germany and paleobiogeographical implications for the configuration of central Perigondwana. Geological Society of America Special Paper 423: 143–152.

    Google Scholar 

  • Elicki, O., and F. Debrenne. 1993. The Archaeocyatha of Germany. Paläontologie, Stratigraphie, Fazies psf 1, Freiberger Forschungshefte C 450: 3–40.

    Google Scholar 

  • Elicki, O., and G. Geyer. 2010. The faunal province of the southern margin of the Rheic Ocean. Cambrian biostratigraphy. In Pre-Mesozoic Geology of Saxo-Thuringiafrom the Cadomian active margin to the Variscan Orogen, eds. Linnemann, U. and R.L. Romer, 103–114. Stuttgart: Schweizerbart.

  • Elicki, O., and G. Geyer. 2013. The Cambrian trilobites of Jordan—taxonomy, systematic and stratigraphic significance. Acta Geologica Polonica 63(1): 1–56.

    Article  Google Scholar 

  • Elicki, O., and T. Wotte. 2003. Cambroclaves from the Cambrian of Sardinia (Italy) and Germany: constraints for the architecture of western Gondwana and the palaeogeographical and paleoecological potential of cambroclaves. Palaeogeography Palaeoclimatology Palaeoecology 195(1–2): 55–71.

    Article  Google Scholar 

  • Fletcher, T.P. 2003. Ovatoryctocara granulata: the key to a global Cambrian stage boundary and the correlation of the olenellid, redlichiid and paradoxidid realms. Special Papers in Palaeontology 70: 73–102.

    Google Scholar 

  • Franke, W. 1989. Tectonostratigraphic units in the Variscan Belt of Europe. Geological Society of America, Special Papers 230: 67–90.

    Article  Google Scholar 

  • Freyer, G., and P. Suhr. 1987. Über Archaeocyathinen-Funde und den lithologischen Aufbau des Unterkambriums im Gebiet von Torgau. Zeitschrift für Geologische Wissenschaften 15: 655–680.

    Google Scholar 

  • Freyer, G., and P. Suhr, P. 1992. Über Algengemeinschaften aus der unterkambrischen Zwethauer Folge des Gebietes von Torgau. Freiberger Forschungsheft, C 445, Paläontologie:49–65.

  • Geyer, G., 1988. Agnostida aus dem höheren Unterkambrium und dem Mittelkambrium von Marokko. Teil 2: Eodiscina. Neues Jahrbuch für Geologie und Paläontologie, Abhandlungen 177(1):93–133.

  • Geyer, G. 1990a. Die marokkanischen Ellipsocephalidae (Trilobita: Redlichiida). Beringeria 3: 1–363.

    Google Scholar 

  • Geyer, G. 1990b. Revised Lower to lower Middle Cambrian biostratigraphy of Morocco. Newsletters on Stratigraphy 22(2/3): 53–70.

    Google Scholar 

  • Geyer, G., and B. Buschmann. 2006. A new earliest Middle Cambian faunule from Saxony (Germany) and its bearing on the tectonostratigraphic history of the Saxothuringian domain. In South Australia 2006. XI International Conference of the Cambrian Stage Subdivision Working Group, ed. Jago, J.B. Geological Society of Australia, Abstracts Number 84:14–15.

  • Geyer, G., and E. Landing. 2004. A unified Lower–Middle Cambrian chronostratigraphy for west Gondwana. Acta Geologica Polonica 54: 179–218.

    Google Scholar 

  • Geyer, G., and E. Landing. 2006. Ediacaran–Cambrian depositional environments and stratigraphy of the western Atlas regions. In Morocco 2006EdiacaranCambrian depositional environments and stratigraphy of the western Atlas regions, eds. Geyer, G., and E. Landing. UCL Maghreb Petroleum Research Group, Infracambrian/Early Palaeozic Field Guide Series 1 and Beringeria Special Issue 6:47–120.

  • Geyer, G., and M. Mergl. 1995. Mediterranean representatives of the obolellid Trematobolus (Brachiopoda) and a review of the genus. Paläontologische Zeitschrift 69(1/2): 179–209.

    Google Scholar 

  • Geyer, G., and J.S. Peel. 2011. The Henson Gletscher Formation, North Greenland, and its bearing on the global Cambrian Series 2–Series 3 boundary. Bulletin of the Czech Geological Survey 86(3): 465–534.

    Google Scholar 

  • Geyer, G., E. Landing, and W. Heldmaier. 1995. Faunas and depositional environments of the Cambrian of the Moroccan Atlas region. In MOROCCO ‘95—the Lower–Middle Cambrian standard of western Gondwana, eds. Geyer, G., and E. Landing. Beringeria Special Issue 2:47–119.

  • Geyer, G., A. Popp, T. Weidner, and L. Förster. 2004. New Lower Cambrian trilobites from Pleistocene erratic boulders of northern Germany and Denmark and their bearing on the intercontinental correlation. Paläontologische Zeitschrift 78(1): 127–135.

    Article  Google Scholar 

  • Geyer, G., O. Elicki, O. Fatka, and A. Żylińska. 2008. Cambrian. In The geology of central Europe, vol. 1. Precambrian and Palaeozoic, ed. T. McCann, 155–202. London: Geological Society of London.

  • Goryansky, V.Y., and L.E. Popov. 1985. Morfologiya, sistematicheskoe polozhenie i proiskhozhdenie bezzamkovykh brakhiopod c karbonatnoy rakovinoy [The morphology, systematic position and origin of the inarticulate brachiopods with calcareous shells]. Paleontologicheskiy Zhurnal’ 1985(3): 3–14.

    Google Scholar 

  • Goryansky, V.Yu., L.I. Egorova, and V.E. Savitsky. 1964. O faune nizhnego kembriya srednego sklona Anabarskogo shchita. Uchenie zapiskiy nauchno-issled. instituta geologii Arktiki (NIIGA), seriya Paleontologiya i biostratigrafiya 4:5–32.

  • Gozalo, R., E. Liñán, M.E. Dies Álvarez, J.A. Gámez Vintaned, and E. Mayoral. 2007. The Lower–Middle Cambrian boundary in the Mediterranean subprovince. In The evolution of the Rheic Ocean: from Avalonian-Cadomian active margin to AlleghenianVariscan collision, eds. Linnemann, U., R.D. Nance, P. Kraft, and G. Zulauf. Geological Society of America Special Paper 423:359–373. doi:10.1130/2007.2423(17).

  • Hall, J., 1847. Natural History of New York. Palaeontology, vol. 1. Containing descriptions of the organic remains of the lower division of the New-York System. Albany: C. van Benthuysen.

  • Holm, G., 1893. Sveriges kambrisk-siluriska Hyolithidae och Conulariidae. Sveriges geologiska Undersökning, Afhandlingar och Uppsatser C 112.

  • Howell, B.F. 1935. Cambrian and Ordovician Trilobites from Hérault, Southern France. Journal of Paleontology 9: 222–238.

    Google Scholar 

  • Kobayashi, T. 1935. 935c. The Cambro-Ordovician formations and faunas of South Chosen. Palaeontology. Part 3. Cambrian faunas of South Chosen with a special study on the Cambrian trilobite genera and families. Journal of the Faculty of Science, Imperial University of Tokyo, Section II, 4:49–344.

  • Kobayashi, T. 1943. Brief notes on the eodiscids I, their classification with a description of a new species and a new variety. Proceeding of the Imperial Academy Tokyo XIX 1: 37–42.

    Google Scholar 

  • Kuhn, O., 1949. Lehrbuch der Paläozoologie. Stuttgart: Schweizerbart.

  • Lapworth, C. 1888. On the discovery of the Olenellus fauna in the Lower Cambrian rocks of Britain. Nature 39: 212–213.

    Article  Google Scholar 

  • Latreille, P.A., 1829. Crustacés, Arachnides et partie des Insectes. In: Le Règne Animal, distribué d’après son organisation, pour servir de base a l’histoire naturelle des animaux et d’introduction à l’anatomie comparé, ed. G. Cuvier, Nouvelle édition, revue et augmentée. Tome IV: i–xxvii, 1–584. Paris.

  • Lieberman, B.S. 2001. Phylogenetic Analysis of the Olenellina Walcott, 1890 (Trilobita, Cambrian). Journal of Paleontology 75(1): 96–115.

    Article  Google Scholar 

  • Liñan, E., and R. Gozalo. 1986. Trilobites del Cámbrico inferior y medio de Murero (Cordillera Ibérica). Memorias del Museo Paleontológico, Universidad de Zaragoza 2: 1–104.

    Google Scholar 

  • Liñán, E., and M. Mergl. 2001. Lower and Middle Cambrian brachiopods from the Iberian Chains and Sierra Morena, Spain. Revista Española de Paleontología 16(2): 317–337.

    Google Scholar 

  • Liñán, E., M.E. Dies, J.A. Gámez Vintaned, R. Gozalo, and E. Mayoral. 2008. “Distinguishing eustatic and epeirogenic controls on Lower–Middle Cambrian boundary successions in West Gondwana (Morocco and Iberia)”, by Ed Landing, Gerd Geyer and Wolfram Heldmaier, published in Sedimentology (2006), 53(4), 899–918—discussion. Sedimentology 55:723–724.

  • Linnarsson, G., 1877. Om faunan i lagren med Paradoxides œlandicus. Sveriges geologiska Undersökning, Ser. C, 40, Föreningen i Stockholm Förhandlingar 1877, III (12):352–375 [1–24].

  • Linnemann, U., R. d’Lemos, K. Drost, T. Jeffries, A. Gerdes, R.L. Romer, S.D. Samson, and R.A. Strachan. 2008. Cadomian tectonics:103–154. In: The Geology of Central Europe, vol. 1. ed. T. McCann. London: The Geological Society.

  • Lochman, C. 1956. Stratigraphy and paleogeography of the Elliptocephala asaphoides strata in Cambridge and Hoosick quadrangles, New York. Bulletin of the Geological Society of America 67(10): 1331–1396.

    Article  Google Scholar 

  • Marek, L. 1963. New knowledge on the morphology of Hyolithes. Sborník geologickych věd, řada Paleontologie 1: 53–72.

    Google Scholar 

  • Matthew, G.F. 1887. Illustrations of the fauna of the St. John Group. No. 4.—on the smaller-eyed trilobites of Division I., with a few remarks on the species of the higher divisions of the group. Canadian Record of Science 2: 357–363.

    Google Scholar 

  • Matthew, G.F. 1892. Protolenus—a new genus of Cambrian trilobites. Bulletin of the Natural History Society of New Brunswick 10: 34–37.

    Google Scholar 

  • Matthew, G.F. 1893. Trematobolus. An articulate Brachiopod of the Inarticulate Order. Canadian Record of Science 5: 276–279.

    Google Scholar 

  • Matthew, G.F., 1895. The Protolenus Fauna. Transactions of the New York Academy of Science XIV (for 1894–1895):101–153.

  • Matthew, G.F. 1896. Notes on the Cambrian faunas—the genus Microdiscus. American Geologist XVIII: 28–31.

    Google Scholar 

  • Matthew, G.F., 1897. The oldest Siphonotreta. Geological Magazine, new series, Decade 4, IV:68–71.

  • Matthew, G.F., 1899. The Etcheminian Fauna of Smith Sound, Newfoundland. Transactions of the Royal Society of Canada Series 2 V:97–123.

  • Mergl, M. 1988. Inarticulate brachiopods of early Middle Cambrian age from the High Atlas, Morocco. Veštník ústřeního ústavu geologického 63(5): 291–295.

    Google Scholar 

  • Mergl, M., and O. Elicki. 2004. Cambrian lingulid and acrotretid brachiopods from the Iglesiente area (Campo Pisano Formation, southwestern Sardinia). Rivista Italiana di Paleontologia i Stratigrafia 110(3): 581–589.

    Google Scholar 

  • Nöldeke, W., 1976. Das Obervisé von Doberlug–Kirchhain. Jahrbuch für Geologie 5/6 (for 1969/70):589–706.

  • Palmer, A.R., and N.P. James. 1980. The Hawke Bay event: a circum-Iapetus regression near the Lower–Middle Cambrian boundary. In The Caledonides in the USA. ed. D.R. Wones, 15–18. Department of Geological Sciences, Virginia Polytechnic Institute State Univ., Memoir 2.

  • Popov, L.E., and L.E. Holmer. 2000. Family TREMATOBOLIDAE new family: 205–206. In Treatise on Invertebrate Paleontology. Part H. Brachiopoda, vol. 2. ed. Kaesler, R.L. Boulder, CO: Geological Society of America, and Lawrence, KS: University of Kansas Press.

  • Rasetti, F. 1952. Revision of the North American trilobites of the family Eodiscidae. Journal of Paleontology 26(3): 434–451.

    Google Scholar 

  • Raw, F. 1936. Mesonacidae of Comley in Shropshire, with a discussion of classification within the family. Quarterly Journal of the geological Society, London 92(3): 236–293.

    Article  Google Scholar 

  • Richter, R., 1932. Crustacea (Paläontologie) 840–863. In Handwörterbuch der Naturwissenschaften, 2nd edn. Jena: Fischer.

  • Richter, R., and E. Richter. 1941. Das Kambrium am Toten Meer und die älteste Tethys. Abhandlungen der senckenbergischen naturforschenden Gesellschaft 460: 1–50.

    Google Scholar 

  • Richter, R., and E. Richter. 1948. Zur Frage des Unter-Kambriums in Nordost-Spanien. Senckenbergiana 29: 23–39.

    Google Scholar 

  • Rowell, A.J., 1965. Inarticulata. In Treatise On Invertebrate Paleontology, Part H, Brachiopoda, ed. Moore, R.C.: H260–H296. Boulder, CO: Geological Society of America, and Lawrence, KS: University of Kansas Press.

  • Rowell, A.J., 1966. Revision of some Cambrian and Ordovician inarticulate brachiopods. University of Kansas Paleontological Contributions, Paper 7.

  • Schmidt, E.W., 1944. Die mittelkambrische Fauna von Doberlug. Jahrbuch der Reichsstelle für Bodenforschung 62 (for 1941):344–402.

  • Schuchert, C. 1893. A classification of the Brachiopoda. The American Geologist 11: 141–167.

    Google Scholar 

  • Sdzuy, K. 1957a. Alter und tiergeographische Stellung des Mittelkambriums von Doberlug. Geologie 6: 465–475.

    Google Scholar 

  • Sdzuy, K. 1957b. Revision der mittelkambrischen Trilobiten von Doberlug. Senckenbergiana Lethaea 38: 7–28.

    Google Scholar 

  • Sdzuy, K. 1958. Tiergeographie und Paläogeographie im europäischen Mittelkambrium. Geologische Rundschau 47: 450–461.

    Article  Google Scholar 

  • Sdzuy, K. 1962. Trilobiten aus dem Unter-Kambrium der Sierra Morena (S-Spanien). Senckenbergiana Lethaea 43(3): 181–229.

    Google Scholar 

  • Sdzuy, K. 1968. Trilobites del Cámbrico medio de Asturias. Trabajos de Geología, Facultad de Ciencias, Universidad de Oviedo 1: 77–133.

    Google Scholar 

  • Sdzuy, K. 1970. Mittelkambrische Fossilien aus neuen Bohrungen bei Doberlug und bei Delitzsch. Geologie 19: 1066–1091.

    Google Scholar 

  • Sdzuy, K., 1972. Das Kambrium der acadobaltischen Faunenprovinz—Gegenwärtiger Kenntnisstand und Probleme. Zentralblatt für Geologie und Paläontologie Teil II, Jg. 1972:1–91.

  • Sdzuy, K., E. Liñán, and R. Gozalo. 1999. The Leonian Stage (early Middle Cambrian): a unit for Cambrian correlation in the Mediterranean subprovince. Geological Magazine 136: 39–48.

    Article  Google Scholar 

  • Sjögren, A., 1872. Om några försteningar i Ölands kambriska lager. Geologiska Föreningen i Stockholm Förhandlingar 1 (5) (for 1872–1873):67–80.

  • Streng, M. 1999. Early Middle Cambrian representatives of the superfamily Acrotretoidea (Brachiopoda) from Morocco. Zeitschrift der deutschen geologischen Gesellschaft 150(1): 27–87.

    Google Scholar 

  • Vogel, K., 1962. Muscheln mit Schloßzähnen aus dem spanischen Kambrium und ihre Bedeutung für die Evolution der Lamellibranchiaten. Akademie der Wissenschaften und der Literatur, Mainz, Abhandlungen der mathematisch- naturwissenschaftlichen Klasse, Jg. 1962.

  • Walch, J.E.I., 1771. Die Naturgeschichte der Versteinerungen zur Erläuterung der Knorrischen Sammlung von Merkwürdigkeiten der Natur. Dritter Theil. [1–8], 1–235. Nürnberg: Felßecker.

  • Walcott, C.D. 1908. Cambrian Geology and Paleontology, No. 3. Cambrian Brachiopoda: description of new genera and species. Smithsonian Miscellaneous Collections LIII 3: 55–137.

    Google Scholar 

  • Walcott, C.D. 1910. Olenellus and other genera of the Mesonacidae. Smithsonian Miscellaneous Collections 53(6): 231–422.

    Google Scholar 

  • Westergård, A.H., 1936. Paradoxides oelandicus Beds of Öland with the Account of a Diamond Boring through the Cambrian at Mössberga. Sveriges geologiska undersökning, Ser. C, 394, Årsb. 30 (f. 1936), 1.

  • Westrop, S.R., and E. Landing. 2000. Lower Cambrian (Branchian) trilobites and biostratigraphy of the Hanford Brook Formation, southern New Brunswick. Journal of Paleontology 74(5): 858–878.

    Article  Google Scholar 

  • Williams, A., S. Carlson, C.H.C. Brunton, L.E. Holmer, and L.E. Popov. 1996. A supra-ordinal classification of the Brachiopoda. Philosophical Transactions of the Royal Society, London 351: 1117–1193.

    Google Scholar 

  • Wurm, A., 1925. Über ein Vorkommen von Mittelcambrium (Paradoxidesschichten) im bayrischen Frankenwald bei Wildenstein südlich Presseck. Neues Jahrbuch für Mineralogie etc., Beilagen-Band 52, Abt. B:71–93.

  • Żylińska, A., and M. Masiak. 2007. Cambrian trilobites from Brzechów, Holy Cross Mountains (Poland) and their significance in stratigraphic correlation and biogeographic reconstructions. Geological Magazine 144(4): 661–686.

    Article  Google Scholar 

  • Żylińska, A., and Z. Szczepanik. 2009. Trilobite and acritarch assemblages from the Lower–Middle Cambrian boundary interval in the Holy Cross Mountains (Poland). Acta Geologica Polonica 59(4): 413–458.

    Google Scholar 

Download references

Acknowledgments

Preparation of this article was made possible by research grant GE 549/21-1 of the Deutsche Forschungsgemeinschaft (DFG) to G.G. Most of the photography and of the preparation was performed in the research laboratory of J.S. Peel at Uppsala University, which is gratefully acknowledged. Sincere thanks are due to A. Żylińska, University of Warsaw, and R. Gozalo, Universitat de València, Burjassot, for thorough review and helpful remarks on the manuscript, to M. Streng, Uppsala University, for kind assistance and information on the acrotretoid specimens, and to E. Landing, New York State Museum, Albany, NY, for explanations of G.F. Matthew’s original stratigraphic concepts.

Author information

Authors and Affiliations

Authors

Corresponding author

Correspondence to Gerd Geyer.

Rights and permissions

Reprints and permissions

About this article

Cite this article

Geyer, G., Buschmann, B. & Elicki, O. A new lowermost middle Cambrian (Series 3, Stage 5) faunule from Saxony (Germany) and its bearing on the tectonostratigraphic history of the Saxothuringian domain. Paläontol Z 88, 239–262 (2014). https://doi.org/10.1007/s12542-013-0195-z

Download citation

  • Received:

  • Accepted:

  • Published:

  • Issue Date:

  • DOI: https://doi.org/10.1007/s12542-013-0195-z

Keywords

Schlüsselwörter

Navigation