Preferencje help
Widoczny [Schowaj] Abstrakt
Liczba wyników
2016 | 61 | 4 |
Tytuł artykułu

Sexual dimorphism in the Bathonian morphoceratid ammonite Polysphinctites tenuiplicatus

Treść / Zawartość
Warianty tytułu
Języki publikacji
Asphinctites tenuiplicatus [M] and Polysphinctites secundus [m] from the Asphinctites tenuiplicatus Zone (Early Bathonian), are usually considered as a sexual dimorphic pair, although authors describe them as separate species. We used statistical methods to test the sexual dimorphic correspondence between those morphospecies, based on a rather large sample of well-preserved macro- and microconchs derived from a single horizon of calcareous concretions in the Polish Jura. Our results indicate that both dimorphs or sexes have identical ontogeny up to a critical diameter, from which they diverge towards the characteristic morphology and sculpture of each dimorph. Thus, both dimorphs are described as a single species: Polysphinctites tenuiplicatus [M and m]. After review of the several nominal species usually assigned to the genera Asphinctites and Polysphinctites throughout their stratigraphic and biogeographic range in the Early Bathonian of the Tethys, it is concluded that they actually correspond to only two species of a single lineage. The corresponding name for the lineage should be Polysphinctites (= Asphinctites as a junior synonym).
Słowa kluczowe
Opis fizyczny
  • Arkell, W.J. 1951–1959. The English Bathonian ammonites. A Monograph of the Palaeontolographical Society London 1951: Part 1, Vol. 104, 1–46; Part 2, Vol. 105, 47–72; 1952: Part 3, 73–104; 1954: Part 4, Vol. 107, 103–127; 1955: Part 5, Vol. 108, 129–140; 1956: Part 6, Vol. 110, 141–162; 1958: Part 7, Vol. 111, 163–208; 1959: Part 8, Vol. 112, 209–264.
  • Brauns, D. 1865. Die Stratigraphische und Paläontologie des südöstlichen Theiles der Hilsmulde auf Grund neuer, bei den Eisenbahngauten in den Jahren 1861–1864 angestellter Beobachtungen. Palaeontographica 13: 75–146.
  • Bucher, H., Landman, N.H., Klofak, S.M., and Guex, J., 1996. Mode and rate of growth in Ammonoids. In: N.H. Landman, K.Tanabe, and R.A. Davis (eds.), Ammonoid Paleobiology. Topics in Geobiology 13: 407–461.
  • Buckman, S.S. 1909–1930. Yorkshire Type Ammonites (continued as Type Ammonites), 7 Vols. 790 plates with explanatory text. Published by the author, London.
  • Callomon, J.H. 1963. Sexual dimorphism in Jurassic ammonites. Transactions of the Leicester Literary and Philosophical Society 57: 21–56.
  • Callomon, J.H. 1969. Dimorphism in Jurassic ammonites: some reflections. In: G.E.G. Westermann (ed.), Sexual Dimorphism in Fossil Metazoa and Taxonomic Implications (IUGS, Series A1), 111–125. Schweizerbart, Stuttgart.
  • Callomon, J.H. 1981. Dimorphism in ammonoids. In: M.R. House and J.R. Senior (eds.), The Ammonoidea. Systematics Association Special Volume 18: 257–273.
  • Callomon, J.H. 1985. The evolution of the Jurassic ammonite family Cardioceratidae. Special Papers in Palaeontology 33: 49–90.
  • Currie, E.D. 1944. Growth stages in some Jurassic ammonites. Transactions of the Royal Society of Edinburgh 61: 171–198.
  • Davis, R.A, Landman, N.H., Dommergues, J.-L., Marchand, D., and Bucher, H. 1996. Mature modifications and sexual dimorphism in ammonoids. In: N.H. Landman, K.Tanabe, and R.A. Davis (eds.), Ammonoid Paleobiology. Topics in Geobiology 13: 463–539.
  • De Baets, K., Bert, D., Hoffmann, R., Monnet, C., Yacobucci, M.M., and Klug, C. 2015. Ammonoid intraspecific variability. In: C. Klug, D. Korn, K. DeBaets, I. Kruta, and R.H. Mapes (eds.), Ammonoid Paleobiology: From Anatomy to Ecology. Topics in Geobiology 43: 359–426.
  • De Grossouvre, A. 1919. Bajocien–Bathonian dans la Nièvre. Bulletin de la Societé Géologique de France 18: 337–459.
  • Dietze, V., Krieger, T., and Schweigert, G. 1997. Über Oecoptychius subrefractus (Buckman), Asphinctites tenuiplicatus (Brauns) und Polysphinctites secundus (Wetzel) (Ammonoidea) aus dem Unter-Bathonium (Mittlerer Jura) der Oberplatz (Nodost-Bayern, Süddeutchland). Stuttgarter Beiträge zur Naturkunde B 245: 1–25.
  • Fagerland, M.W. and Sandvik, L. 2009. Performance of five two-sample location tests for skewed distributions with unequal variances. Contemporary Clinical Trials 30: 490–496.
  • Fischer, P.H. 1882. Manuel de conchyliologie et de paléontologie conchyliologique. 1369 pp. Librairie F. Savy. Paris.
  • Gedl, P. and Kaim, A. 2012. An introduction to the palaeoenvironmental reconstruction of the Bathonian (Middle Jurassic) ore-bearing clays at Gnaszyn, Kraków–Silesia Homocline, Poland. Acta Geologica Polonica 62: 267–280.
  • Guex, J. 1970. Sur le sexe des ammonites. Bulletin de la Société Vaudoise des Sciences Naturelles 70: 241–246.
  • Guex, J. 1973. Dimorphisme des Dactylioceratidae du Toarcien. Eclogae geologicae Helvetiae 66: 545–583.
  • Hahn, W. 1970. Die Parkinsoniidae S. Buckman und Morphoceratidae Hyatt (Ammonoidea) des Bathoniums (Brauner Jura ε) im südwestdeutschen Jura. Jahrbuch geologische Landesamt Baden-Württemberg 12: 7–62.
  • Hammer, O. and Harper, D.A.T. 2006. Paleontological Data Analysis. 351 pp. Blackwell Publishing, Oxford.
  • Hyatt, A. 1900. Cephalopoda. In: C.R. Eastman (ed.), Text-book of Paleontology by Karl A. von Zittel, 502–604. Macmillan and Co., New York.
  • Kant, R. and Kullmann, J. 1973. “Knickpunkte” im allometrischen Wachstum von Cephalopoden-Gehäuse. Neues Jahrbuch fur Geologie und Paläontologie Abhandlungen 142: 7–114.
  • Kennedy, W.J. 2013. On variation in Schloebanchia varians (J. Sowerby, 1817) from the Lower Cenomanian of western Kazakhstan. Acta Geologica Polonica 63: 443–468.
  • Kopik, J. 1979. Stratygrafia jury środkowej regionu bełchatowskiego. Kwartalnik Geologiczny 23: 179–193.
  • Kopik, J. 1998. Lower and Middle Jurassic of the north-eastern margin of the Upper Silesian Coal Basin. Biuletyn Państwowego Instytutu Geologicznego 378: 67–120.
  • Klug, C., Zatoń, M., Parent, H., Hostettler, B., and Tajika, A. 2015. Mature modifications and sexual dimorphism. In: C. Klug, D. Korn, K. DeBaets, I. Kruta, and R.H. Mapes (eds.), Ammonoid Paleobiology: From anatomy to ecology. Topics in Geobiology 43: 253–320.
  • Landman, N.H., Kennedy, W.J., Cobban, W., and Larson, N.L. 2010. Scaphites of the “nodosus group” from the Upper Cretaceous (Campanian) of the Western Interior of North America. Bulletin of the American Museum of Natural History 342: 1–242.
  • Lehmann, U. 1981. The Ammonites: Their Life and Their World. 246 pp. Cambridge University Press, New York.
  • Maeda, H. 1993. Dimorphism of Late Cretaceous false-puzosiine ammonites, Yokoyamaoceras Wright and Matsumoto, 1954 and Neopuzosia, 1954. Transactions and Proceedings of the Palaeontological Society of Japan, New Series 169: 97–128.
  • Majewski, W. 2000. Middle Jurassic concretions from Częstochowa (Poland) as indicators of sedimentation rates. Acta Geologica Polonica 50: 431–439.
  • Makowski, H. 1962. Problem of sexual dimorphism in amonites. Palaeontologia Polonica 12: 1–92.
  • Mangold, C. and Rioult, M. 1997. Bathonien. In: E. Cariou and P. Hantzpergue (eds.), Biostratigraphie du Jurassique ouest-européen et méditerranéen: zonations paralléles et distribution des invertébres et microfossiles. Bulletin du Centre de Recherche Elf-Exploration et Production 17: 134–139.
  • Matyja, B.A. and Wierzbowski, A. 2000. Ammonites and stratigraphy of the uppermost Bajocian and Lower Bathonian between Częstochowa and Wieluń, Central Poland. Acta Geologica Polonica 50: 191–209.
  • Matyja, B.A. and Wierzbowski, A. 2001. Palaeogeographical distribution of early Bathonian ammonites of the Asphinctites–Polysphinctites group. Hantkeniana 3: 89–103.
  • Palframan, D.F.B. 1966. Variation and ontogeny of some Oxfordian am monites: Taramelliceras richei (De Loriol) and Creniceras renggeri (Oppel), from Woodham, Buckinghamshire. Palaeontology 9: 290–311.
  • Parent, H. 1997. Ontogeny and sexual dimorphism of Eurycephalites gottschei (Tornquist) (Ammonoidea) of the Andean lower Callovian (Argentine–Chile). Geobios 30: 407–419.
  • Parent, H. 1998. Upper Bathonian and lower Callovian ammonites from Chacay Melehué (Argentina). Acta Palaeontologica Polonica 43: 69–130.
  • Parent, H., Scherzinger, A., and Schweigert, G. 2008. Sexual phenomena in Late Jurassic Aspidoceratidae. Dimorphic correspondence between Physo doceras hermanni (Berckhemer) and Sutneria subeumela Schneid, and first record of possible hermaphroditism. Palaeodiversity 1: 181–187.
  • Rollier, L. 1911. Le faciès du Dogger ou oolithique dans le Jura et les régions voisines. 352 pp. Georg & Cie., Zürich. Shea, E.K. and Vecchione, M. 2002. Quantification of ontogenetic discontinuities in three species of oegopsid squids using model II piecewise linear regression. Marine Biology 140: 971–979.
  • Schairer, G. 1994. Polysphinctites polysphinctus Buckman aus dem “Parkinsonien-Oolith” von Segenthal. Mitteilungen der Bayerischen Staatssammlung für Palaontologie und Historische Geologie 34: 159–162.
  • Schloenbach, U. 1865. Beiträge zur Paläontologie der Jura- und KreideFormation im nordwestlichen Deutschland. Palaeontographica 13: 147–192, 267–332.
  • Schlögl, J., Rakus, M., Mangold, C., and Elmi, S. 2005. Bajocian–Bathonian ammonite fauna of the Czorsztyn Unit, Pieniny Klippen Belt (Western Carpathians, Slovakia); its biostratigraphical and palaeogeographical significance. Acta Geologica Polonica 55: 339–359.
  • Schweigert, G. 1997. Die Ammonitengattungen Simocosmoceras Spath und Pseudhimalayites Spath (Aspidoceratidae) im süddeutschen Oberjura. Stuttgarter Beiträge zur Naturkunde B 246: 1–29.
  • Steinmann, G. 1890. Cephalopoda. In: G. Steinmann and L. Döderlein (eds.), Elemente der Paläontologie, 344–475. Engelmann, Leipzig.
  • Sturani, C. 1971. Ammonites and stratigraphy of the “Posidonia alpina” beds of the Venetian Alps (Middle Jurassic, mainly Bajocian). Memorie Instituto Geologico e Mineralogico de la Universita Padova 28: 1–190.
  • Torrens, H.S. 1987. Ammonites and stratigraphy of the Bathonian rocks in the Digne-Barrême area (South-Eastern France, Dept. Alpes de Haute Provence). Bolletino de la Societa Paleontologica Italiana 26: 93–108.
  • Verma, H.M. and Westermann, G.E.G. 1973. The Tithonian (Jurassic) ammonite fauna and stratigraphy of Sierra Catorce, San Luis Potosi, Mexico. Bulletin of American Paleontology 63: 107–320.
  • Welch, B.L. 1937. The significance of the difference between two means when the population variances are unequal. Biometrika 29: 350–362.
  • Westermann, G.E.G. 1958. Ammoniten-Fauna und Stratigraphie des Bathonien NW-Deutschland. Beihefte zum Geologischen Jahrbuch 32: 1–103.
  • Westermann, G.E.G. 1964. Sexual-Dimorphismus bei Ammonoideen und seine Bedeutung für die Taxionomie der Otoitidae (einschliesslich Sphaero ceratinae; Ammonoidea; M-Jura). Palaeontographica A 124: 33–73.
  • Westermann, G.E.G. 1969. Proposal: classification and nomenclature of dimorphs at the genus-group level [with discussion]. In: G.E.G. Westermann (ed.), Sexual Dimorphism in Fossil Metazoa and Taxonomic Implications (IUGS, Series A1), 233–238. Schweizerbart, Stuttgart.
  • Westermann, G.E.G. and Callomon, J.H. 1988. The Macrocephalitinae and associated Bathonian and Early Callovian (Jurassic) ammonoids of the Sula Islands and New Guinea. Palaeontographica A 203: 1–90.
  • Westermann, G.E.G., Hudson, N., and Grant-Mackie, J. 2002. New Jurassic Ammonitina from New Zealand: Bathonian–Callovian Eurycephalitinae. New Zealand Journal of Geology and Geophysics 45: 499–525.
  • Wetzel, W. 1950. Fauna und Stratigraphie der Württembergica-Schichten insbesondere Nord-deutschlands. Palaeontographica A 99: 61–120.
  • Zatoń, M. 2010a. Bajocian–Bathonian (Middle Jurassic) ammonites from the Polish Jura. Part 1: Families Phylloceratidae, Nannolytoceratidae, Sonninidae, Strigoceratidae, Oppeliidae and Lissoceratidae. Palaeontographica A 292: 65–113.
  • Zatoń, M. 2010b. Bajocian–Bathonian (Middle Jurassic) ammonites from the Polish Jura. Part 2: Families Stephanoceratidae, Perisphinctidae, Parkinsonidae, Morphoceratidae and Tulitidae. Palaeontographica A 292: 115–213.
Typ dokumentu
Identyfikator YADDA
JavaScript jest wyłączony w Twojej przeglądarce internetowej. Włącz go, a następnie odśwież stronę, aby móc w pełni z niej korzystać.