Body fossils or trace fossils: a reinterpretation of mayfly larvae body impressions from the Upper Cretaceous Wapiti Formation, Alberta, Canada

Abstract In this study, we present a revised interpretation of mayfly larval body impressions previously described from the fluvial Wapiti Formation of Alberta, Canada. Unlike typical insect fossils that occur in lacustrine deposits or amber inclusions, these fossils are interpreted to have been preserved in a depositional setting characterized by currents rapid enough to erode and transport fine-grained sand. To determine how the fossils were formed, we examined the spatial relationship between the fossils and associated tool marks preserved on the same bedding surface. All 16 of the fossil specimens analyzed were in life orientation with their heads directed upstream, suggesting that the impressions were produced by live organisms. Here we propose a new ichnotaxon Kalyptichnus belli n. igen. n. isp. for shallow self-burial traces of insect larvae. UUID: https://zoobank.org/eade3ae6-2e98-4f97-ac17-2577fc562000

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Publication Details

Journal
Journal of Paleontology
Published
2026-09-09
DOI
https://doi.org/10.1017/jpa.2026.10283
Primary Topic
Fossil Insects in Amber
Type
article
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article

Body fossils or trace fossils: a reinterpretation of mayfly larvae body impressions from the Upper Cretaceous Wapiti Formation, Alberta, Canada

John‐Paul Zonneveld, Corwin Sullivan, Ryusuke Kimitsuki, Murray K. Gingras et al.
Journal of Paleontology
Fossil Insects in Amber
article

Body fossils or trace fossils: a reinterpretation of mayfly larvae body impressions from the Upper Cretaceous Wapiti Formation, Alberta, Canada

John‐Paul Zonneveld, Corwin Sullivan, Ryusuke Kimitsuki, Murray K. Gingras, KANO SASAGUCHI, Robin L. Sissons, John Acorn
article en

Abstract

Abstract In this study, we present a revised interpretation of mayfly larval body impressions previously described from the fluvial Wapiti Formation of Alberta, Canada. Unlike typical insect fossils that occur in lacustrine deposits or amber inclusions, these fossils are interpreted to have been preserved in a depositional setting characterized by currents rapid enough to erode and transport fine-grained sand. To determine how the fossils were formed, we examined the spatial relationship between the fossils and associated tool marks preserved on the same bedding surface. All 16 of the fossil specimens analyzed were in life orientation with their heads directed upstream, suggesting that the impressions were produced by live organisms. Here we propose a new ichnotaxon Kalyptichnus belli n. igen. n. isp. for shallow self-burial traces of insect larvae. UUID: https://zoobank.org/eade3ae6-2e98-4f97-ac17-2577fc562000

Journal of Paleontology
University of Alberta (CA)
Openalex Percentile: Top 7%
Fossil Insects in Amber
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