Skip to main content
Log in

First report of a Palaeozoic fenestrate bryozoan with an articulated growth habit

  • Research Paper
  • Published:
Journal of Iberian Geology Aims and scope Submit manuscript

    We’re sorry, something doesn't seem to be working properly.

    Please try refreshing the page. If that doesn't work, please contact support so we can address the problem.

Abstract

Purpose

The main goal of this paper is the description of the erect articulated growth habit for the first time within the Palaeozoic Order Fenestrata, and the interpretation of its occurrence within the evolutionary history of colonial morphology in fenestrates.

Methods

The present paper is based on a single specimen composed of fifteen disarticulated internodes. The specimen was extracted from the outcrop as two minute slabs, one of which was embedded in a two-component epoxy resin for preparation of acetate peels and the other one preserved without subsequent preparation for observation of exterior features.

Results

A new Devonian fenestrate bryozoan genus, Arnaopora, and its type species, A. sotoi, are described from the Emsian-Eifelian Moniello Formation (Asturias, NW Spain). Zooecial characters as well as the development of articulated colonies support the definition of this new genus, which is the first reported representative with an articulated growth habit in the Order Fenestrata, almost exclusively composed of rigidly erect unilaminar forms.

Conclusions

The occurrence of Arnaopora in the early Eifelian coincides with a peak of disparity in fenestrate bryozoan growth forms during the transition between the Early and Middle Devonian. While all previously known morphological variations of growth forms in Palaeozoic fenestrates derive from the basic reticulate habit, articulation evolved from a rigidly branching phylloporinid ancestor. Arnaopora is extremely rare within the abundant and diverse bryozoan fauna of shallow platform facies where it occurs, which is in contrast with the relatively common presence of cellariform colonies in assemblages from modern shallow environments.

Resumen

Objetivo

El propósito principal de este artículo es la descripción del hábito de crecimiento erecto articulado por primera vez en el Orden Fenestrata, y la interpretación de su presencia en el marco de la historia evolutiva de la morfología colonial en los fenestrados.

Métodos

Este trabajo está basado en un ejemplar compuesto por quince segmentos extraído en dos pequeñas lajas; una laja se embutió en resina epoxy para realizar de réplicas de acetato y la otra se conservó sin preparación adicional para observar las características externas del ejemplar.

Resultados

Se describen un nuevo género de briozoos fenestrados devónicos, Arnaopora, y su especie tipo, A. sotoi, de la Formación Moniello (Emsiense-Eifeliense, Asturias, NO de España). Los caracteres zooeciales y el desarrollo de colonias articuladas justifican la definición de este nuevo género, que es el primer representante descrito del hábito articulado en el Orden Fenestrata, casi exclusivamente compuesto por formas unilaminares erectas rígidas.

Conclusiones

La presencia del Arnaopora en el Eifeliense temprano coincide con un pico de disparidad en las formas de crecimiento de los briozoos fenestrados durante la transición entre el Devónico Temprano y Medio. Mientras que todas las variaciones morfológicas conocidas hasta el momento en los fenestrados paleozoicos derivan del hábito reticulado básico, la articulación evolucionó a partir de un phylloporínido erecto ramificado. Arnaopora es extremadamente rara entre la abundante y diversa fauna de briozoos de las facies de plataforma somera en que aparece, en contraste con la presencia relativamente común de colonias cellariformes en asociaciones de ambientes someros modernos.

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

Similar content being viewed by others

References

  • Amini, Z. Z., Adabi, M. H., Burrett, C. F., & Quilty, P. G. (2004). Bryozoan distribution and growth form associations as a tool in environmental interpretation, Tasmania, Australia. Sedimentary Geology, 167, 1–15.

    Article  Google Scholar 

  • Arbizu, M., García-Alcalde, J. L., García-López, S., Méndez-Bedia, I., Sánchez de Posada, L. C., Soto, F. M., et al. (1979). Biostratigraphical study of the Moniello Formation (Cantabrian Mountains, Asturias, NW Spain). A contribution to the Lower/Middle Devonian boundary problem. Geologica et Palaeontologica, 13, 103–124.

    Google Scholar 

  • Bassler, R. S. (1952). Taxonomic notes on genera of fossil and recent Bryozoa. Journal of the Washington Academy of Sciences, 42, 381–385.

    Google Scholar 

  • Blake, D. B. (1983a). Introduction to the Suborder Rhabdomesina. In R. A. Robison (Ed.), Treatise on invertebrate paleontology, Part G, Bryozoa, revised (pp. 530–549). Boulder: Geological Society of America and University of Kansas.

    Google Scholar 

  • Blake, D. B. (1983b). Systematic descriptions for the Suborder Rhabdomesina. In R. A. Robison (Ed.), Treatise on invertebrate paleontology, Part G, Bryozoa, revised (pp. 550–592). Boulder: Geological Society of America and University of Kansas.

    Google Scholar 

  • Borg, F. (1926). Studies on recent cyclostomatous Bryozoa. Zoologiska Bidrag från Uppsala, 10, 181–507.

    Google Scholar 

  • Cheetham, A. (1963). Late Eocene zoogeography of the Eastern Gulf Coast Region. Geological Society of America Memoir, 91, 1–879.

    Article  Google Scholar 

  • Ehrenberg, C. G. (1831). Symbolae Physicae, seu Icones et descriptiones. Pars Zoologica, IV, Animalia Evertebrata exclusis Insectis. Berlin: Berolini ex Officina Academica.

    Google Scholar 

  • Elias, M. K., & Condra, G. E. (1957). Fenestella from the Permian of West Texas. The Geological Society of America Memoir, 70, 1–158.

    Article  Google Scholar 

  • Ernst, A., & Bohatý, J. (2009). Schischcatella (Fenestrata, Bryozoa) from the Devonian of the Rhenish Massif, Germany. Palaeontology, 52, 1291–1310.

    Article  Google Scholar 

  • Ernst, A., & Königshof, P. (2010). Bryozoan fauna and microfacies from a Middle Devonian reef complex (Western Sahara, Morocco). Senckenberg Gesellschaft für Naturforschung Abhandlungen, 568, 1–91.

    Google Scholar 

  • Fernández Martínez, E. (2015). Palaeozoic from the Cantabrian Zone. Zamora, S. (coord.), Álvaro, J.J., Arbizu, M., Colmenar, J., Esteve, J., Fernández-Martínez, E., Fernández, L.P., Gutiérrez-Marco, J.C., Suárez-Andrés, J.L., Villas, E.; Waters, J. Field Trip: Palaeozoic Echinoderms from Northern Spain. In: Zamora, S.; Rábano, I. (Eds.) Progress in Echinoderm Palaeobiology. Cuadernos del Museo Geominero, 19. Instituto Geológico y Minero de España, Madrid, 247–248.

  • Fernández-Martínez, E. (1993). Tabulados y Chaetétidos de las Formaciones Moniello-Santa Lucía y Candás-Portilla (Devónico, Cordillera Cantábrica, NO de España). Unpublished PhD Memoir, Departamento de Geología, Universidad de Oviedo, 1–420

  • García-López, S., Sanz-López, J. (2002). Devonian to Lower Carboniferous conodont biostratigraphy of the Bernesga Valley section (Cantabrian Zone, NW Spain). In S. García-López, F. Bastida (Eds.), Palaeozoic conodonts from northern Spain. Eighth International Conodont Symposium held in Europe. Publicaciones del Instituto Geológico y Minero de España, Cuadernos del Museo Geominero, 1, 163–205.

  • Hageman, S. J., Bock, P. E., Bone, Y., & McGowran, B. (1998). Bryozoan growth habits: classification and analysis. Journal of Paleontology, 72(3), 418–436.

    Article  Google Scholar 

  • Hageman, S. J., Bone, Y., McGowran, B., & James, N. P. (1997). Bryozoan colonial growth-forms as paleoenvironmental indicators: Evaluation of methodology. Palaios, 12, 405–419.

    Article  Google Scholar 

  • Hall, J. (1883). Bryozoans of the Upper Heldelberg and Hamilton groups. Transactions of the Albany Institute, 10, 145–197.

    Google Scholar 

  • Hayward, P. J., & Ryland, J. S. (1995). Bryozoa from Heron Island, Great Barrier Reef. 2. Memoirs of the Queensland Museum, 38, 533–573.

    Google Scholar 

  • García-López, S. Sanz-López, J. Sarmiento, G. N. (2002). The Palaeozoic succession and conodont biostratigraphy of the section between Cape Peñas and Cape Torres (Cantabrian coast, NW Spain). In S.García-López, F. Bastida (Eds.), Palaeozoic conodonts from northern Spain. Eighth International Conodont Symposium held in Europe. Publicaciones del Instituto Geológico y Minero de España, Cuadernos del Museo Geominero, 1, 125–161.

  • Karklins, O. L. (1983). Introduction to the Suborder Ptilodictyina. In R. A. Robison (Ed.), Treatise on invertebrate paleontology, Part G, Bryozoa, revised (pp. 453–488). Boulder: Geological Society of America and University of Kansas.

    Google Scholar 

  • Kelly, S. M., & Horowitz, A. S. (1987). Growth forms and paleoecology of Mississippian bryozoans: Critical application of Stach’s 1936 model, Eastern United States. In J. R. P. Ross (Ed.), Bryozoa: present and past (pp. 137–144). Bellingham: Western Washington University.

    Google Scholar 

  • Lagaiij, R., & Gautier, Y. V. (1965). Bryozoan assemblages from marine sediments of the Rhone delta, France. Micropaleontology, 11, 39–58.

    Article  Google Scholar 

  • Lavrentjeva, V. D. (1979). Phylloporinina—a new Suborder of Paleozoic Bryozoa. Paleontological Zhurnal, 1, 59–68.

    Google Scholar 

  • Lavrentjeva, V. D. (1985). Bryozoans of the Suborder Phylloporinida. Trudy paleontologicheskogo Instituta, 214, 1–100.

    Google Scholar 

  • Ma, J. Y., Taylor, P. D., & Xia, F. S. (2014). New observations on the skeletons of the earliest bryozoans from the Fenhsiang Formation (Tremadocian, Lower Ordovician), Yichang, China. Paleoworld, 23, 25–30.

    Article  Google Scholar 

  • McKinney, F. K., & Jackson, J. B. C. (1989). Bryozoan evolution (pp. 1–238). Chicago: The University of Chicago Press.

    Google Scholar 

  • McKinney, F. K., Listokin, M. R. A., & Phifer, C. D. (1986). Flow and polypide distribution on the cheilostome bryozoans Bugula and their inference in Archimedes. Lethaia, 19, 81–93.

    Article  Google Scholar 

  • McKinney, F. K., Wyse Jackson, P. N. (2015). Part G, Revised, Volume 2, Chapter 8A: Order Fenestrata: morphology and growth. Treatise Online, 66, 1–91.

  • Méndez-Bedia, I. (1976). Biofacies y litofacies de la FormacionMoniello-Santa Lucía (Devónico de la Cordillera Cantábrica, NO de España). Trabajos de Geología, 9, 1–93, Universidad de Oviedo.

  • Méndez-Bedia, I. (1984). Primera nota sobre los estromatopóridos de la Formación Moniello (Devónico de la Cordillera Cantábrica, NW de España). Trabajos de Geología, 14, 151–159, Universidad de Oviedo.

  • Méndez-Bedia, I., & Soto, F. (1984). Paleoecological succesion in a Devonian organic buildup (Moniello Fm., Cantabrian Mountains, NW NWSpain). Geobios, 8, 151–157.

    Article  Google Scholar 

  • Méndez-Bedia, I., Soto, F., & Fernández-Martínez, E. (1994). Devonian reef types in the Cantabrian Mountains, (NW Spain) and their faunal composition. Courier Forschungs Institut Senckenberg, 172, 161–183.

    Google Scholar 

  • Milne-Edwards, H. (1838). Mémoire sur les Crisies, les Hornéres et plusieurs autres Polypes vivants ou fossiles dont l’organisation est analogue à celle des Tubulipores. Annales des Sciences naturelles, Zoologie & Biologie animale, 2(9), 193–238.

    Google Scholar 

  • Moissette, P. (2000). Changes in bryozoan assemblages and bathymetric variations. Examples from the Messinian of northwest Algeria. Palaeogeography, Palaeoclimatology, Palaeoecology, 155, 305–326.

    Article  Google Scholar 

  • Morozova, I. P. (2001). Bryozoans of the Order Fenestellida. Trudy Paleontologicheskii Instituta, 277, 1–176. (in Russian).

    Google Scholar 

  • Nelson, C. S., Hyden, F. M., Keane, S. L., Leask, W. L., & Gordon, D. P. (1988). Application of bryozoan zoarial growth-form studies in facies analysis of non-tropical carbonate deposits in New Zealand. Sedimentary Geology, 60, 301–322.

    Article  Google Scholar 

  • Nickles, J. M., & Bassler, R. S. (1900). A synopsis of American fossil Bryozoa, including bibliography and synonymy. USGS Bulletin, 173, 1–663.

    Google Scholar 

  • Okamura, B. (1985). The effects of ambient flow velocity, colony size, and upstream colonies in the feeding success of Bryozoa. II. Conopeum reticulum (Linnaeus), and encrusting species. Journal of Experimental Marine Biology and Ecology, 89, 69–80.

    Article  Google Scholar 

  • Rogers, A. F. (1900). New bryozoans from the Coal Measures of Kansas and Missouri. Kansas University Quarterly Series A, 9(1), 1–12.

    Google Scholar 

  • Sánchez de la Torre, L., Manjón, M. (1976). Facies de la Caliza de Moniello en la zona de Arnao, Asturias. Trabajos de Geología, Vol. 8, pp. 109–129, Universidad de Oviedo.

  • Schopf, T. J. M. (1969). Paleoecology of ectoprocts (bryozoans). Journal of Paleontology, 43, 234–244.

    Google Scholar 

  • Smith, A. M. (1995). Palaeoenvironmental interpretation using bryozoans: a review. In D. W. J. Bosence, P. A. Allison, (Eds.). Marine palaeoenvironmental analysis from fossils, Geological Society Special Publication, Vol. 83, pp. 231–243.

  • Soto, F., García-Alcalde, J. L. (1976). La fauna silicificada del Devónico de Piedras Blancas. Trabajos de Geología, Vol. 8, pp. 87–103, Universidad de Oviedo.

  • Soto, F., Méndez-Bedia, I. (1985). Estudio de una asociación coral rugoso-estromatopórido en el arrecife de Arnao (Fm. Moniello, Asturias, NO de España). Trabajos de Geología, Vol. 15, pp. 203–209, Universidad de Oviedo.

  • Spjeldnaes, N. (1985). Upper Ordovician bryozoans from Ojl Mir, Gotland, Sweden. Bulletin of the Geological Institutions of the University of Uppsala, N. S., 10, 1–66.

    Google Scholar 

  • Stach, L. W. (1936). Correlation of zoarial form with habitat. Journal of Geology, 44, 60–65.

    Article  Google Scholar 

  • Suárez Andrés, J. L., & Ernst, A. (2015). Lower-Middle Devonian Fenestellidae (Bryozoa) of NW Spain: implications for fenestrate palaeobiogeography. Facies, 61(415), 1–29.

    Google Scholar 

  • Suárez Andrés, J. L., & McKinney, F. K. (2010). Revision of the Devonian fenestrate bryozoan genera Cyclopelta Bornemann, 1884 and Pseudoisotrypa Prantl, 1932, with description of a rare fenestrate growth habit. Revista Española de Paleontología, 25(2), 123–138.

    Google Scholar 

  • Suárez Andrés, J. L., & Wyse Jackson, P. N. (2014). Ernstipora mackinneyi, a new unique fenestrate bryozoan genus and species with an encrusting growth habit from the Emsian (Devonian) of NW Spain. N. Jb. Geol. Paläont. (Abh.), 271, 229–242.

    Article  Google Scholar 

  • Suárez Andrés, J. L., & Wyse Jackson, P. N. (2015). Feeding currents: a limiting factor for disparity of Palaeozoic fenestrate bryozoans. Palaeogeography, Palaeoclimatology, Palaeoecology, 433, 219–232.

    Article  Google Scholar 

  • Suárez Andrés, J. L., & Wyse Jackson, P. N. (2017). Fenestrate Bryozoa of the Moniello Formation (Lower-Middle Devonian, NW Spain). Bulletin of Geosciences, 92(2), 153–183.

    Article  Google Scholar 

  • Taylor, P. D. (2005). Bryozoans and palaeoenvironmental interpretation. Journal of the Palaeontological Society of India, Golden Jubilee, 50(2), 1–11.

    Google Scholar 

  • Taylor, P. D., & Ernst, A. (2004). Bryozoans. In B. D. Webby, F. Paris, M. L. Droser, & I. G. Percival (Eds.), The Great Ordovician biodiversification event (pp. 147–156). New York: Columbia University Press.

    Google Scholar 

  • Ulrich, E. O. (1882). American Paleozoic Bryozoa. Journal of the Cincinnati Society of Natural History, 5, 121–175.

    Google Scholar 

  • Utgaard, J. (1983). Systematic descriptions for the Order Cystoporata. In R. A. Robison (Ed.), Treatise on invertebrate paleontology, Part G, Bryozoa, revised (pp. 358–439). Boulder: Geological Society of America and University of Kansas.

    Google Scholar 

  • Waschurova, L. I. (1964). Bryozoa from the Lower Devonian of Zeravshan and Turkestan Ranges. Trudy Uprav. Geol. I okhrany nedr pri Sovete Min. Tadzh. SSSR Paleontol. I Strat, 1, 75–168. (in Russian).

    Google Scholar 

  • Wyse Jackson, P. N. (1996). Bryozoa from the Lower Carboniferous (Viséan) of County Fermanagh, Ireland. Bulletin of the Natural History Museum, London (Geology), 52(2), 119–171.

  • Wyse Jackson, P. N., Ernst, A., & Suárez Andrés, J. L. (2017). Articulation in the family Rhabdomesidae (Cryptostomata: Bryozoa) from the Mississippian of Ireland. Irish Journal of Earth Sciences, 37, 35–44.

    Article  Google Scholar 

Download references

Acknowledgements

Luis Miguel Rodríguez Terente (University of Oviedo) is thanked for macro photography of the specimen. Covadonga González Álvarez helped with graphic work. The authors are grateful to the reviewers for their constructive comments. Mary Spencer Jones (NHM, London) is acknowledged for the loan of the SEM image of Crisia elongata Milne Edwards, 1838 NHMUK 1916.8.23.77 (Fig. 2h).

Author information

Authors and Affiliations

Authors

Corresponding author

Correspondence to Juan Luis Suárez Andrés.

Rights and permissions

Reprints and permissions

About this article

Check for updates. Verify currency and authenticity via CrossMark

Cite this article

Suárez Andrés, J.L., Wyse Jackson, P.N. First report of a Palaeozoic fenestrate bryozoan with an articulated growth habit. J Iber Geol 44, 273–283 (2018). https://doi.org/10.1007/s41513-018-0054-6

Download citation

  • Received:

  • Accepted:

  • Published:

  • Issue Date:

  • DOI: https://doi.org/10.1007/s41513-018-0054-6

Keywords

Palabras clave

Navigation