Abstract
AbstractIn this paper, seven coprolites from the Lower Cretaceous of Tsagan-Tsab formation have been described. Thus, producing a significant contribution to what we perceived as the first detailed study of coprolites from the Mesozoic deposits in Mongolia. The collected coprolites encompass a total of six spiral amphipolar and one scroll coprolites. We prominently identified four new coprolite ichnotaxa, such as: Hyronocoprus tsagantsabensis and Hyronocoprus hunti, to which both are ichnosp. nov.; followed by Megakalocoprus barremianensis and Scrollocoprus tatalensis, where both are ichnogen. et ichnosp. nov. Notably, CT scans revealed that all specimens showed various amounts of bony inclusions and scales, hence, deducing that the producers could have had a low acidic digestive track and were unable to dissolve bone matters. Moreover, SEM–EDS analysis concluded its carnivorous nature, thus, pointing towards piscivorous diet. The small sized Scrollocoprus is considered to be the second findings of Mesozoic era’s scroll coprolites, which contain possible plant pollens, a complete infraorbital bone, clusters of bone fragments and rhomboidal-shaped ganoid scales of the prey; and bioerosional scars have been observed on the surface. We suggest those amphipolar spiral ichnotaxa were produced by Asipenceriformes, with Pholidophoriformes as the prey, while Scrollocoprus represents fecal excrement of underived fish, possibly of sarcopterygian origins.
Funder
Natural Science Foundation of China
Strategic Priority Research Program of the Chinese Academy of Sciences
Publisher
Springer Science and Business Media LLC
Reference116 articles.
1. Lister, M. Letters and divers other mixt discourses in natural philosophy. New York: Printed by J. White for the author (1683).
2. Duffin, C. J. The earliest published records of coprolites. N. M. Mus. Nat. Hist. Sci. Bull. 57, 25–28 (2012).
3. Mantell, G. A. The Fossils of the South Downs Or: Illustrations of the Geology of Sussex, Lupton Relfe (1822).
4. Buckland, W. On the discovery of coprolites, or fossil faeces, in the Lias at Lyme Regis, and in other formations. Trans. Geol. Soc. Lond. Ser. 2(3), 223–236 (1829).
5. Neumayer, L. Die Koprolithen des Perms von Texas. Palaeontographica (1846–1933) 51(2–3), 121–128 (1904).