Journal
ICHNOS-AN INTERNATIONAL JOURNAL FOR PLANT AND ANIMAL TRACES
Volume 28, Issue 2, Pages 87-96Publisher
TAYLOR & FRANCIS INC
DOI: 10.1080/10420940.2021.1890590
Keywords
Bioerosion; China; Dinosauria; insects; Junggar Basin; Late Jurassic; palaeoecology; taphonomy
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Bioerosional trace fossils found on dinosaur bones in the Upper Jurassic Shishugou Formation of the northeastern Junggar Basin provide important insights into taphonomic processes and paleoecological implications. The presence of invertebrate trace fossils suggests that the dinosaur carcass was exposed for weeks under a semi-arid and seasonal climate before burial by sediment, supporting general paleoclimatological reconstructions for the region. This discovery also represents the first evidence of invertebrate-vertebrate interactions in the Late Jurassic of Asia, offering a novel glimpse into the ancient Jurassic ecosystem.
Bioerosional trace fossils can offer invaluable insights into taphonomic processes, ecosystem dynamics and environmental conditions that are not obtainable by other lines of evidence. Here, we describe the first invertebrate trace fossils on dinosaur bone from the Upper Jurassic Shishugou Formation of the northeastern Junggar Basin. The traces occur as spherical holes in the bone, closely resembling boreholes attributed to either indeterminate insects or dermestid beetles and thus they are here likewise ascribed to feeding and/or pupation by necrophagous insects. Such bioerosional trace fossils have several taphonomical and palaeoecological implications for they are only inflicted on subaerially exposed tissues and preferentially when carcasses are desiccated. We, therefore, conclude that the dinosaur carcass was exposed for at least several weeks under a semi-arid and seasonal climate before it was buried by sediment. This supports the general palaeoclimatological and paleoenvironmental reconstructions for the Shishugou Formation from sedimentological data. Moreover, this is the first evidence for invertebrate-vertebrate interactions from the Late Jurassic of Asia, offering a novel glimpse into the diverse biotic relationships of this ancient Jurassic ecosystem.
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