ESTONIAN ACADEMY
PUBLISHERS
eesti teaduste
akadeemia kirjastus
PUBLISHED
SINCE 1952
 
Earth Science cover
Estonian Journal of Earth Sciences
ISSN 1736-7557 (Electronic)
ISSN 1736-4728 (Print)
Impact Factor (2022): 1.1
Short communication
Ichnogenus Trypanites in the Ordovician of Estonia (Baltica); pp. 106–109
PDF | https://doi.org/10.3176/earth.2023.48

Authors
Ursula Toom, Jukka Kuva, Dirk Knaust
Abstract

Trypanites is a common boring in Ordovician hardgrounds of Estonia (Baltica). The depth of the sedimentary basin and sedimentation rates controlled the distribution of Trypanites. The trace-makers’ community was diverse and changing over time. Three ichnospecies of Trypanites can be distinguished: T. sozialisT. weisei and Trypanites isp. All three morphotypes can be recognized in the same hardground. It is impossible to distinguish between the different ichnospecies based only on the size of the boring aperture. The depth of early lithification of the seafloor determines the morphological variability seen in T. sozialis. The occurrence of elongated borings, such as T. weisei and Trypanites isp., is related to tropical environments, and their trace-makers strongly preferred substrates with a homogeneous and dense texture. The texture and available volume of hard substrate controls the ichnodiversity of Trypanites ichnospecies.

References

Christ, N., Immenhauser, A., Wood, R., Darwich, K. and Niedermayr, A. 2015. Petrography and environmental controls on the formation of Phanerozoic marine carbonate hardgrounds. Earth-Science Reviews151, 176–226.
https://doi.org/10.1016/j.earscirev.2015.10.002

Cole, A. R. and Palmer, T. J. 1999. Middle Jurassic worm borings, and a new giant ichnospecies of Trypanites from the Bajocian/ Dinantian unconformity, southern England. Proceedings of the Geologists’ Association110(3), 203–209.
https://doi.org/10.1016/S0016-7878(99)80070-4

Dronov, A. and Rozhnov, S. 2007. Climatic changes in the Baltoscandian basin during the Ordovician: Sedimentological and palaeontological aspects. Acta Geologica Sinica46, 108–113.

Eisenack, A. 1934. Über Bohrlöcher in Geröllen baltischer Obersilurgeschiebe (On borings in Baltic Upper Silurian erratic boulders). Zeitschrift für Geschiebeforschung10, 89–94.

Flügel, E. 2010. Microfacies of Carbonate Rocks. Analysis, Interpretation and Application. Springer, Berlin, Heidelberg, New York. 
https://doi.org/10.1007/978-3-642-03796-2

Hagenow, H. F. 1840. Monographie der Rügen’schen Kreide-Versteinerungen, II. Abtheilung: Radiarien und Annulaten. Nebst Nachträgen zur ersten Abtheilung (Monograph of the Cretaceous fossils of Rügen, Part II: radiaries and annulates. In addition supplements to the first part). Neues Jahrbuch für Mineralogie, Geognosie, Geologie und Petrefaktenkunde1839, 630–672.

Jaanusson, V. 1973. Aspects of carbonate sedimentation in the Ordovician of Baltoscandia. Lethaia6(1), 11–34.
https://doi.org/10.1111/j.1502-3931.1973.tb00871.x

Knaust, D., Dronov, A. V. and Toom, U. 2023. Two almost-forgotten Trypanites ichnospecies names for the most common Palaeozoic macroboring. Papers in Palaeontology9(3), e1491. 
https://doi.org/10.1002/spp2.1491

Kobluk, D. R. and Nemcsok, S. 1982. The macroboring ichnofossil Trypanites in colonies of the Middle Ordovician bryozoan Prasopora: population behaviour and reaction to environmental influences. Canadian Journal of Earth Sciences19, 679–688.
https://doi.org/10.1139/e82-057

Kočová Veselská, M., Kočí, T., Jäger, M., Mikuláš, R., Heřmanová, Z., Morel, N. et al. 2021. Sclerobionts on tubes of the serpulid Pyrgopolon (Pyrgopolondeforme (Lamarck, 1818) from the upper Cenomanian of Le Mans region, France. Cretaceous Research125, 10487. 
https://doi.org/10.1016/j.cretres.2021.104873

Mägdefrau, K. 1932. Über einige Bohrgänge aus dem Unteren Muschelkalk von Jena (On some borings from the Lower Muschelkalk of Jena). Paläontologische Zeitschrift14, 150–160. 
https://doi.org/10.1007/BF03041628

Nestor, H. and Einasto, R. 1997. Ordovician and Silurian carbonate sedimentation basin. In Geology and Mineral Resources of Estonia (Raukas, A. and Teedumäe, A., eds). Estonian Academy Publishers, Tallinn, 192–204.

Neumann, C., Wisshak, M. and Bromley, R. G. 2008. Boring a mobile domicile: an alternative to the conchiculous life habit. In Current Developments in Bioerosion (Wisshak, M. and Tapanila, L., eds). Springer, Berlin, Heidelberg, 307–327.
https://doi.org/10.1007/978-3-540-77598-0_16

Nield, E. W. 1984. The boring of Silurian stromatoporoids – towards an understanding of larval behaviour in the Trypanites organism. Palaeogeography, Palaeoclimatology, Palaeoecology48(2–4), 229–243.
https://doi.org/10.1016/0031-0182(84)90046-4

Palmer, T. J. and Wilson, M. A. 2004. Calcite precipitation and dissolution of biogenic aragonite in shallow Ordovician calcite seas. Lethaia37(4), 417–427.
https://doi.org/10.1080/00241160410002135

Põlma, L. 1982. Сравнительная литология карбонатных пород ордовика Северной и Средней Прибалтики (Comparative Lithology of the Ordovician Carbonate Rocks in the Northern and Middle East Baltic). Valgus, Tallinn.

Rozhnov, S. V. 2018. Hardgrounds of the Ordovician Baltic Paleobasin as a distinct type of sedimentation induced by cyanobacterial mats. Paleontological Journal52(10), 1098–1113.
https://doi.org/10.1134/S0031030118100118

Saadre, T. 1992. Distribution pattern of the discontinuity surfaces in the Middle Ordovician, North Estonia. In WOGOGOB: Oslo ’92: Excursions, 1920 August (Bruton, D. L., ed.). Oslo, 25–26. 

Toom, U. 2019. Ordovician and Silurian trace fossils of Estonia. PhD thesis. Tallinn University of Technology, Estonia. 

Wisshak, M., Neumann, C., Knaust, D. and Reich, M. 2017. Rediscovery of type material of the bioerosional trace fossil Talpina von Hagenow, 1840 and its ichnotaxonomic implications. Paläontologische Zeitschrift91(1), 127–135.
https://doi.org/10.1007/s12542-017-0335-y

Back to Issue