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Fossil Record A palaeontological open-access journal of the Museum für Naturkunde
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Volume 12, issue 1
Foss. Rec., 12, 91–97, 2009
https://doi.org/10.1002/mmng.200800013
© Author(s) 2009. This work is distributed under
the Creative Commons Attribution 3.0 License.
Foss. Rec., 12, 91–97, 2009
https://doi.org/10.1002/mmng.200800013
© Author(s) 2009. This work is distributed under
the Creative Commons Attribution 3.0 License.

  01 Feb 2009

01 Feb 2009

A simulated bird gastric mill and its implications for fossil gastrolith authenticity

O. Wings2,1 O. Wings
  • 1Steinmann-Institut für Geologie, Mineralogie und Paläontologie, Universität Bonn, Nussallee 8, 53115 Bonn, Germany
  • 2current address: Museum für Naturkunde Berlin, Invalidenstraße 43, 10115 Berlin, Germany

Abstract. A rock tumbler, stones, water, plant material, hydrochloric acid, and pepsin were used to simulate a bird gizzard in order to study abrasion rate and influence of stomach juices and foodstuff on gastrolith surface development. The experiment lasted for six months. Each week, the "stomach" was supplied with fresh grass and stomach juices. After the end of the experiment, the set of stones had a combined weight loss of 22.4%, with softer rock types showing higher abrasion rates. The combination of stomach juices and silica phytoliths within the grass had no visible effect on stone surface development: polish or pitting did not occur. A second experiment combined only pebbles with water in the tumbler. Results indicate that rock abrasion is mainly caused by contacts between moving stones. A comparison with authentic ostrich gastroliths showed that abrasion in the artificial stomach must have been lower than in a real gizzard, but still too high to maintain or develop surface polish. If high polish occasionally seen on sauropodomorph dinosaur gastroliths was indeed caused in a stomach environment, it implies digestive processes different from those of extant birds and the "artificial gizzard". Geologic origins of polish, such as transport in hyperconcentrated flows, wind blasting, or tectonic movements must be considered for polished fossil gastroliths and isolated clasts in fine-grained sediments (exoliths).

doi:10.1002/mmng.200800013

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