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Fossil Record A palaeontological open-access journal of the Museum für Naturkunde

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Foss. Rec., 20, 173-199, 2017
https://doi.org/10.5194/fr-20-173-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
Research article
17 Jul 2017
Classical and new bioerosion trace fossils in Cretaceous belemnite guards characterised via micro-CT
Max Wisshak1, Jürgen Titschack1,2, Wolf-Achim Kahl3, and Peter Girod4 1Senckenberg am Meer, Marine Research Department, 26382 Wilhelmshaven, Germany
2MARUM – Center for Marine Environmental Sciences, 28359 Bremen, Germany
3Bremen University, Geosciences, 28359 Bremen, Germany
4Holteistraße 2, 10245 Berlin, Germany
Abstract. The ongoing technical revolution in non-destructive 3-D visualisation via micro-computed tomography (micro-CT) finds a valuable application in the studies of bioerosion trace fossils, since their three-dimensional architecture is hidden within hard substrates. This technique, in concert with advanced segmentation algorithms, allows a detailed visualisation and targeted morphometric analyses even of those bioerosion traces that are otherwise inaccessible to the widely applied cast-embedding technique, because they either are filled with lithified sediment or cement or are preserved in inherently insoluble or silicified host substrates, or because they are established type material and should not be altered.

In the present contribution selected examples of such cases are illustrated by reference to bioerosion trace fossils preserved in Late Cretaceous belemnite guards from the European Chalk Province. These case studies comprise an analysis of a diverse ichno-assemblage found associated with the lectotype of the microboring Dendrina dendrina (Morris, 1851) in a belemnite from the upper Campanian to lower Maastrichtian chalk of Norfolk, England, and the description of two new bioerosion trace fossils with type specimens found in belemnite guards from the lower Campanian limestones of Höver, Germany. The latter are Lapispecus hastatus isp. n., a tubular and occasionally branched macroboring for which a sipunculan or a phoronid trace maker are discussed, and Entobia colaria isp. n., a camerate network formed by an excavating sponge that eroded diagnostic grated apertures at the locations of the presumed inhalant papillae or exhaling pores, adding to or replacing filtering devices that are otherwise made of tissue and spicules.

As an added value to the non-destructive visualisation procedure, the processed X-ray micro-CT scans of the studied type material provide 3-D models that may now serve as digitypes that can be studied as digital facsimile without the necessity of consulting the actual type specimens.


Citation: Wisshak, M., Titschack, J., Kahl, W.-A., and Girod, P.: Classical and new bioerosion trace fossils in Cretaceous belemnite guards characterised via micro-CT, Foss. Rec., 20, 173-199, https://doi.org/10.5194/fr-20-173-2017, 2017.
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Short summary
The ongoing technical revolution in non-destructive 3-D visualisation via micro-computed tomography (micro-CT) finds a valuable application in the studies of bioerosion trace fossils, since their three-dimensional architecture lies hidden within hard substrates. Selected examples of such cases are illustrated by reference to bioerosion trace fossils preserved in Late Cretaceous belemnite guards from the European Chalk Province, including the description of two new trace fossil ichnospecies.
The ongoing technical revolution in non-destructive 3-D visualisation via micro-computed...
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