Saturday, January 9, 2016

[Paleontology | Ichnotaxa • 2016] Ostendichnus bilobatus • Theropod Courtship: Large Scale Physical Evidence of Display Arenas and Avian-like Scrape Ceremony Behaviour by Cretaceous Dinosaurs

Figure 6: Reconstruction of theropods engaged in scrape ceremony display activity, based on trace fossil evidence from the Dakota Sandstone, Colorado.
  Artwork and graphics coordination by Xing Lida  DOI:  10.1038/srep18952

Relationships between non-avian theropod dinosaurs and extant and fossil birds are a major focus of current paleobiological research. Despite extensive phylogenetic and morphological support, behavioural evidence is mostly ambiguous and does not usually fossilize. Thus, inferences that dinosaurs, especially theropods displayed behaviour analogous to modern birds are intriguing but speculative. Here we present extensive and geographically widespread physical evidence of substrate scraping behavior by large theropods considered as compelling evidence of “display arenas” or leks, and consistent with “nest scrape display” behaviour among many extant ground-nesting birds. Large scrapes, up to 2 m in diameter, occur abundantly at several Cretaceous sites in Colorado. They constitute a previously unknown category of large dinosaurian trace fossil, inferred to fill gaps in our understanding of early phases in the breeding cycle of theropods. The trace makers were probably lekking species that were seasonally active at large display arena sites. Such scrapes indicate stereotypical avian behaviour hitherto unknown among Cretaceous theropods, and most likely associated with terrirorial activity in the breeding season. The scrapes most probably occur near nesting colonies, as yet unknown or no longer preserved in the immediate study areas. Thus, they provide clues to paleoenvironments where such nesting sites occurred.

Ostendichnus ichnogen nov. Fig. 3
Diagnosis: large, up to 2-meter-long, bilaterally-symmetrical, bilobed to oval impressions with multiple well-defined digital scratch marks aligned parallel or sub parallel to long axis of the whole trace. Up to 10–15% as deep as long. Traces mostly with a single raised central ridge, separating left and right troughs, which may include complete or partial diagnostic tridactyl theropod tracks.

Type material: holotype Denver Museum of Nature and Science (DMNH) EPV.69705 latex mold and fiberglass replica of large digging trace, within which a diagnostic theropod track occurs. Paratypes DMNH EPV. 69703, EPV. 69704, EPV. 69706 and EPV. 69707 latex molds and fiberglass replicas of large digging traces (Fig. 3 and Supplementary Information 2).

Type horizon and locality: lower part of the Cretaceous Dakota Sandstone, Roubideau Creek, Delta County, Colorado. Information on file with DMNS, CU and BLM.

Derivation of name: from ostendo (Latin) meaning “to show”, or “to display”, and ichnos (Latin) meaning “a trace.”

Ostendichnus bilobatus ichnosp nov., Fig. 3
Type material: as for ichnogenus: holotype DMNH EPV.69705 latex mold and fiberglass replica of digging trace number 5.

Type horizon and locality: as for ichnogenus.

Derivation of ichnospecies name: bilobatus meaning two lobes.

Diagnosis: as for ichnogenus.

Description: large, bilaterally-symmetrical, bilobed to oval impressions or scrapes 0.75 to 2.00 m long and 0.50 to 1.25 m wide; depth variable, 5 to 25 cm. Multiple well-defined digital scratch marks align with the whole trace, as does a raised medial ridge defining the long axis of the trace. Some scratch marks have sharp anterior terminations, indistinguishable from typical theropod digit traces. Together with sand crescents, where sediment was pushed back by posterior motion of digits, or thrown posteriorly as a thin apron, the left and right sides of scrapes are defined. In some scrapes complete or partial theropod tracks are recognisable components of the scrapes.

Figure 1: (a). Locality map, showing outcrops of Dakota Sandstone in western USA, extensively modified in Photoshop CS5 from part of a map by Carpenter (Supplementary Information S1) (b). General view of the Roubideau Creek site (photograph by senior author, M. Lockley, with coauthors KC (foreground) and JM (background) with permission. Note conspicuous scrape marks and mid-line ridge in traces 4–6, c. general view of the Club Gulch site.

Figure 2: Map of Club Gulch site (a) prepared in Photoshop CS5 by MGL, with natural color photogrammetic image (b) at same scale by RTM and LGB. Coloured image (inset in a) shows three large scrapes, together covering 5 m. Digging traces are classified as paired (bilobed) or single, with or without scratch marks and adjacent sand aprons.

Figure 5: a1-a3: maps of Cretaceous sauropod nests from Argentina with cross, section (a4),
Note the nest rim in all cases. (b) cross section of Club Gulch dig trace with thin apron of displaced sand. Note lack of sediment rim. (a,b) drawn to approximately the same scale. c: map showing distribution of Kakapo nest scrape bowls.

Interpretation of Ostednichnus bilobatus
The sharply-terminated scratch marks found in association with diagnostic theropod tracks represent active theropod scraping or scratching. The most complete theropod tracks include a large Irenesauripus-like27,28 left theropod track on the left side of the holotype scrape (Fig. 3a) and a smaller right theropod track associated with the right side of a shallow paratype scrape (Fig. 3c). The variable size and depth of the scrapes, indicate different levels of activity and persistence by different sized theropods, which based on footprint length had hip heights between ~1.0 and ~2.0 m29 and full body lengths between ~2.5 and ~5.0 m. This implies either two or more different species, or co-occurrence of conspecific adults and sub-adults of quite different sizes. Elapsed time between scraping episodes cannot be estimated accurately, but was likely short given the similar, good preservation of all scrapes.

Interpretation of nest scrape displays
Interpretation of these scrapes as evidence of mating display arenas or courtship ritual sites requires elimination of other possible digging behaviour interpretations unrelated to mating display. We can then demonstrate whether or not the behaviour, and resultant trace fossils, are consistent with behaviours of other similar or related species, in this case extant birds.


Martin G. Lockley, Richard T. McCrea, Lisa G. Buckley, Jong Deock Lim, Neffra A. Matthews, Brent H. Breithaupt, Karen J. Houck, Gerard D. Gierliński, Dawid Surmik, Kyung Soo Kim, Lida Xing, Dal Yong Kong, Ken Cart, Jason Martin and Glade Hadden. 2016. Theropod Courtship: Large Scale Physical Evidence of Display Arenas and Avian-like Scrape Ceremony Behaviour by Cretaceous Dinosaurs. Sci. Rep. 6, 18952;  DOI:  10.1038/srep18952

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