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[dinosaur] Eocene tracks: Svalbard coastal plain bird tracks + Washington state reptile tracks



Ben Creisler
bcreisler@gmail.com


Some non-dino papers not yet mentioned:

Ricardo N. Melchor, Alfred Uchman & Ronald J. Steel (2020)
Avian diversity and behavior in an Eocene coastal plain, Svalbard: the ichnological evidence.
Ichnos (advance online publication)
doi: https://doi.org/10.1080/10420940.2020.1744583
https://www.tandfonline.com/doi/full/10.1080/10420940.2020.1744583


This study presents an ichnotaxonomical assessment of bird footprints from a coastal plain setting in the Eocene lower to middle Aspelintoppen Formation in Brongniartfjellet and Storvola, Svalbard. These footprints are unique evidence for Paleogene birds from Svalbard and the second evidence of Paleogene avifauna of the Arctic (along with scarce fossil remains from Ellesmere Island). The analyzed footprints are assigned to six ichnotaxa belonging to three ichnofamilies: Aquatilavipes isp., avian footprint morphotype A and B (ichnofamily Avipedidae); Gruipeda cf. G. abeli, Gruipeda cf. G. dominguensis (ichnofamily Gruipedidae); and Gyeongsangornipes isp. (ichnofamily unknown). Associated invertebrate ichnofossils include Helminthoidichnites tenuis, Cochlichnus anguineus, and Helminthopsis isp. The avian footprints reflect small, medium-sized and rare large birds that can be morphologically compared to those of modern relatives including crane, heron, plover, moorhen, gallinule, oystercatcher and curlew. It is also proposed that in situ sets of shorebird footprints showing a preferred orientation, not composing trackways and showing overprinting, can be used as an indicator of the position and orientation of the shoreline.

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From 2019 but not yet mentioned:

Free pdf:

Anticusuchipes amnis ichnogen. et ichnosp. nov.

George E. Mustoe (2019)
Lower Eocene Footprints from Northwest Washington, USA. Part 1: Reptile Tracks.
Geosciences 9(7): 321
doi: https://doi.org/10.3390/geosciences9070321
https://www.mdpi.com/2076-3263/9/7/321


Lower Eocene fluvial strata in the Chuckanut Formation preserve abundant bird and mammal tracks. Reptile trace fossils include footprints from a small turtle (ichnogenus Chelonipus), and several Crocodylian trackways that consist of irregularly spaced footprints associated with linear tail drag marks. The latter trackways represent "punting" locomotion, where a submerged Crocodylian used intermittent substrate contacts to provide forward motion of their neutrally buoyant bodies. Two adjacent sandstone blocks preserve Crocodylian trace fossils that are named herein as a new ichnogenus and ichnospecies Anticusuchipes amnis. Two other Crocodylian trackways lack sufficient detail for ichnotaxonomic assignment.Â


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