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.2022 Jan 25:10:e12782.
doi: 10.7717/peerj.12782. eCollection 2022.

A newly recognized theropod assemblage from the Lewisville Formation (Woodbine Group; Cenomanian) and its implications for understanding Late Cretaceous Appalachian terrestrial ecosystems

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A newly recognized theropod assemblage from the Lewisville Formation (Woodbine Group; Cenomanian) and its implications for understanding Late Cretaceous Appalachian terrestrial ecosystems

Christopher R Noto et al. PeerJ..

Abstract

While the terrestrial fossil record of the mid-Cretaceous interval (Aptian to Cenomanian) in North America has been poorly studied, the recent focus on fossil localities from the western United States has offered a more detailed picture of vertebrate diversity, ecosystem dynamics and faunal turnover that took place on the western landmass of Laramidia. This is in stark contrast to the terrestrial record from the eastern landmass of Appalachia, where vertebrate fossils are rare and consist mostly of isolated and fragmentary remains. However, a detailed understanding of these fossil communities during this interval is necessary for comparison of the faunal patterns that developed during the opening of the Western Interior Seaway (WIS). The Woodbine Group of Texas is a Cenomanian age (95-100 mya) deposit consisting of shallow marine, deltaic, and terrestrial communities, which were only recently separated from their western counterparts. These deposits have yielded a wealth of vertebrate remains, yet non-avian theropods are still largely unknown. Recently, multiple localities in the Lewisville Formation of the Woodbine Group have yielded new non-avian theropod material, including numerous isolated teeth and postcranial remains. While largely fragmentary, this material is sufficiently diagnostic to identify the following taxa: a large-bodied carcharodontosaur, a mid-sized tyrannosauroid, a large ornithomimosaur, a large dromaeosaurine, a small dromaeosaurid, a small troodontid, and a small coelurosaur. Some of these groups represent the first occurrence for Appalachia and provide a broader understanding of a newly expanded faunal diversity for the Eastern landmass. The Lewisville Formation theropod fauna is similar in taxonomic composition to contemporaneous deposits in Laramidia, confirming that these groups were widespread across the continent prior to extension of the WIS. The Lewisville Formation documents the transitional nature of Cenomanian coastal ecosystems in Texas while providing additional details on the evolution of Appalachian communities shortly after WIS extension.

Keywords: Appalachia; Carcharodontosauria; Cenomanian; Dromaeosauridae; Mid-Cretaceous; Ornithomimosauria; Theropoda; Transition; Troodontidae; Tyrannosauroidea.

© 2022 Noto et al.

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Conflict of interest statement

Christopher R. Noto is an Academic Editor for PeerJ.

Figures

Figure 1
Figure 1. Location and geologic position of the Woodbine Group.
(A) General stratigraphic sequence and timescale for the Cretaceous of central and north central Texas showing the position of the Woodbine Group. Terrestrial deposits represented by stippled intervals. Time scale based on Gradstein, Ogg & Smith (2004). Modified from Adams et al. (2011). B. Map of Woodbine surface exposures in the study area showing position of localities where fossils were discovered. Exposures are stippled, water bodies are solid gray. 1 = Arlington Archosaur Site, 2 = Bear Creek, 3 = Veteran’s Park, 4 = Grapevine Lake Spillway, 5 = Lewisville Lake.
Figure 2
Figure 2. Teeth assigned to Carcharodontosauria.
DMNH 2013-07-1083 showing lingual (A), labial (B), mesial (C), distal (D), basal (E) views and distal denticles (F), mesial denticles (G), distal denticles in posterior view (H), and enamel undulations (I). DMNH 2013-07-1081, showing labial (J), lingual (K), distal (L) views, and distal denticles (M), and enamel spalled surface (N). SMU 76946 showing lingual (O) view, posterior view of distal denticles (P), and enamel spalled surface (Q). (R) DMNH 2013-07-1255 showing enamel spalled surface. DMNH 2014-06-06 showing lingual (S), mesial (T), distal (U), and basal (V) views and distal denticles (W). White arrows indicate basally-oriented interdenticular sulci. Scale bars of unbordered images in A–E are 5 mm, (J)–(V) are 10 mm. Scale bars of bordered images are 1 mm.
Figure 3
Figure 3. Postcranial material assigned to Carcharodontosauria.
Chevron DMNH 2013-07-1990 in right lateral (A), left lateral (B), anterior (C), posterior (D), and proximal (E) views. FMNH PR 2716, chevron ofSiats meekerorum (Zanno & Makovicky, 2013) in proximal (F) and right lateral (G) views. Manual ungual DMNH 2013-07-0494 in distal (H), proximal (I), dorsal (J), ventral (K), and lateral (L–M) views; reconstruction of complete element in lateral view (N) with reconstruction of missing portion (dashed line filled with grey) based onSuchomimus (Sereno et al., 1998). Ap, anterior process; As, articular surface; Af, articular facet; Ed, attachment for extensor tendon; Ft, flexor tubercle; Hc, haemal canal; Pp, posterior process; R, ridge; Su, sulcus; Vc, neurovascular canal. All scale bars are 10 cm.
Figure 4
Figure 4. Teeth assigned to Tyrannosauroidea.
DMNH 2013-07-1701 shown in lingual (A), labial (B), mesial (C), distal (D), and basal (E) views, distal denticles in lateral (F) and distal (G) views, and detailed view of apical wear facet (H). SMU 77218 shown in labial (I), lingual (J), mesial (K), distal (L), and basal (M) views, distal denticles in lateral (N) and distal (O) views, mesial denticles in lateral view (P). Scale bars of unbordered images are 10 mm. Scale bars of bordered images are 1 mm, except P which is 0.5 mm.
Figure 5
Figure 5. Tibia SMU 76809 assigned to Ornithomimosauria.
Shown in proximal (A), anterior (B), lateral (C), medial (D), posterior (E), and distal (F) views. As, anterior surface; Cc, cnemial crest; Fc, fibular crest; Fs, articular surface for fibula; It, incisura tibialis; Lc, lateral condyle; Mc, medial condyle; Md, medullary cavity; Tb, exposed trabecular bone. Scale bar is 10 cm.
Figure 6
Figure 6. Teeth assigned to Dromaeosauridae.
DMNH 2013-07-1080 shown in lingual (A), labial (B), mesial (C), distal (D) and basal views (E); lateral view of distal denticles (F). DMNH 2014-06-02 shown in lingual (G), labial, (H), mesial (I), distal (J), and basal (K) views; lateral view of distal denticles (L). SMU 73779 shown in lingual (M), labial (N), mesial (O), distal (P) and basal views (Q); lateral view of distal denticles (R). SMU 77217 shown in labial (S), lingual (T), mesial (U), distal (V), and basal (W) views; lateral view of mesial denticles (X) and distal denticles (Y). SMU 76948 shown in lingual (Z), labial (AA), mesial (BB), distal (CC), and basal (DD) views. White arrow indicates basally-oriented interdenticular sulci. For (A–L), scale bars of unbordered images are 10 mm and bordered images are 1 mm. For (M–DD), scale bars of unbordered images are 1 mm and bordered images are 0.5 mm.
Figure 7
Figure 7. Other maniraptoran material.
Tooth SMU 76947 assigned to Troodontidae shown in labial (A), lingual (B), mesial (C), distal (D), and basal (E) views; distal denticles shown in lateral (F) and distal (G) views. Manual ungual DMNH 18159 shown in lateral (H–I), distal (J), proximal (K), dorsal (L), and ventral (M) views; reconstruction of complete ungual (N). Ft, flexor tubercle; Vc, neurovascular canal. Scale bar in A–G is 0.5 mm and scale bar in H–N is 5 cm.
Figure 8
Figure 8. Teeth assigned to Coelurosauria indet.
SMU 77213 shown in labial (A), lingual (B), mesial (C), distal (D), and basal (E) views; lateral view of mesial denticles (F) and distal denticles (G). SMU 73778 shown in labial (H), lingual (I), mesial (J), distal (K), and basal (L) views; lateral view of mesial denticles (M) and distal denticles (N). SMU 77214 shown in labial (O), lingual (P), mesial (Q), distal (R), and apical (S) views; lateral view of mesial denticles (T) and distal denticles (U). Black arrows indicate spalled enamel surface. Scale bars of unbordered images are 1 mm. Scale bars of bordered images are 0.5 mm.
Figure 9
Figure 9. Specimens assigned to Theropoda indet.
Tooth DMNH 2013-07-1082 shown in labial (A), lingual (B), mesial (C), distal (D), and basal (E) view. Pedal phalanx DMNH 2013-07-0492 shown in lateral (F–G), dorsal (H), ventral (I), proximal (J), and distal (K) views. Ep, extensor pit; Fl, ligament fossa; Mc, medullary cavity. Scale bars are 10 mm.
Figure 10
Figure 10. Principal components plot and loadings biplot for known and unknown teeth combined.
Graph axes represent the two principal components (PCs) with the greatest amount of variance. Known teeth from published data sets are colored and represented by the legend at the bottom, and unknown teeth reported here are in black with the legend at the top. Arrows indicate where the teeth with missing data move when fully reconstructed (Note the PC scores for most teeth were different for the observed and reconstructed analyses, but, because these changes were so small, they could not be seen between the two PC plots. We therefore combined them into one, and only show movement of reconstructed teeth).
Figure 11
Figure 11. Paleogeographic maps of the mid-Cretaceous interval.
(A) Albian, approximately 110 MY. (B) Late Albian, approximately 105 MY, formation of the Skull Creek Seaway (showing reconstruction of Slattery et al., 2015). (C) Early Cenomanian, approximately 100 MY, showing short-term regression established continental connection between Laramidia and Appalachia. (D) middle Cenomanian, approximately 95 MY, showing a continuous Western Interior Seaway. Star marks location of the Lewisville Formation. All maps are a Mollweide projection and redrawn from Scotese (2021).
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This study was supported by funding from the National Geographic Society Conservation Trust Grant (No. C325-16) and an Experiment.com crowdfunding campaign. The funders had no role in study design, data collection and analysis, decision to publish, or preparation of the manuscript.

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