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Article

Reappraisal on the Phylogenetic Relationships of the Enigmatic Flightless Bird (Brontornis burmeisteri) Moreno and Mercerat, 1891

by
Federico L. Agnolin
1,2
1
Laboratorio de Anatomía Comparada y Evolución de los Vertebrados, Museo Argentino de Ciencias Naturales “Bernardino Rivadavia”-CONICET, Av. Ángel Gallardo 470, Buenos Aires C1405DJR, Argentina
2
Fundación de Historia Natural “Félix de Azara”, Departamento de Ciencias Naturales y Antropología, CEBBAD–Universidad Maimónides, Hidalgo 775 piso 7, Buenos Aires C1405BDB, Argentina
Submission received: 19 January 2021 / Revised: 8 February 2021 / Accepted: 17 February 2021 / Published: 20 February 2021
(This article belongs to the Special Issue Evolution and Palaeobiology of Flightless Birds)

Abstract

:
The fossil record of birds in South America is still very patchy. One of the most remarkable birds found in Miocene deposits from Patagonia is Brontornis burmeisteri Moreno and Mercerat, 1891. This giant flightless bird is known by multiple incomplete specimens that represent a few portions of the skeleton, mainly hindlimb bones. Since the XIX century, Brontornis was considered as belonging to or closely related to phorusrhacoid birds. In contrast to previous work, by the end of 2000 decade it was proposed that Brontornis belongs to Galloanserae. This proposal was recently contested based on a large dataset including both phorusrhacoids and galloanserine birds, that concluded Brontornis was nested among cariamiform birds, and probably belonged to phorusrhacoids. The aim of the present contribution is to re-evaluate the phylogenetic affinities of Brontornis. Based on modified previous datasets, it is concluded that Brontornis does belong to Galloanserae, and that it represents a member of a largely unknown radiation of giant graviportal birds from South America.

1. Introduction

The genus Brontornis was originally described by Moreno and Mercerat (1891) based on several specimens coming from Lower-Middle Miocene localities at Santa Cruz province, Patagonia, Argentina [1]. This genus contains a single species: B. burmeisteri Moreno and Mercerat [2,3]. Brontornis was a giant flightless bird of about 2.8 m tall that may have weighed about 350 to 400 kg [2]. Its limb proportions and shape of elements indicate that Brontornis was a graviportal bird [4,5,6,7], probably a carrion eater [7], or even herbivorous [4,6,8].
On its original description, Moreno and Mercerat [3] include Brontornis on its own family Brontornithidae in the Order Stereornithes (this later included several genera now known as phorusrhacoids). In their concept, the Stereornithes were carinate birds with a shared combination of characters between anseriformes, coconiiforms (Herodiones therein), and accipitriforms, probably “intermediate” between Anatidae and Cathartidae. Moreno and Mercerat also noted the persistence of “reptilian” (i.e., plesiomorphic) characters in phorusrhacoids. Ameghino [9] made a revision of fossil Patagonian birds and partially resolved the confusion created by Moreno and Mercerat’s [3] work. Ameghino considered the Stereornithes as belonging to Ratitae, and included Brontornis among phorusrhacids, a criterion was followed by most authors until Dolgopol de Sáez [10]. She revalidated the Brontornithidae (as Brontorniidae) and based on morphological grounds coined the Order Brontornithes to separate them from remaining phorusrhacoids (encompassed by her in the Order Stereornithes). Despite that, Dolgopol de Sáez was not able to recognize the suprageneric relationships of Brontornis and kin and considered that Gastornis may be closely related to it. Kraglievich [6,11] followed Dolgopol de Sáez and retained Brontornis on its own order Brontornithes (Brontornitiformes for Kraglievich, [6]). Subsequent authors followed Moreno and Mercerat and Ameghino views and considered Brontornis and kin as belonging to a different family or subfamily of phorusrhacoid birds [1,12,13,14], without regard of the distinctive anatomical features cited by Dolgopol de Sáez and Kraglievich.
Posteriorly, Agnolin [8,15,16] proposed that Brontornis may not be closely related to phorusrhacoids, but may be included among Galloanseres as a basal member of Anseriformes, a criterion followed by several authors [17,18,19,20,21,22]. However, Alvarenga et al. [23] returned to previous ideas and sustained that Brontornis belongs to Phorusrhacoidea. The arguments exposed by Alvarenga et al. [23] were contested by Agnolin [16], who supported the anseriform affinities for Brontornis again.
More recently, Worthy et al. [24] made a comprehensive phylogenetic analysis of Galloanseres, with special emphasis on extinct and flightless fowls. In their impressive analysis, Worthy et al. concluded that Brontornis is closely related to phorusrhacoids and considered it as part of Cariamiformes, far from Galloanseres. They argued that the strong differences observed in the postcranial anatomy of Brontornis and other cariamiforms are the result of the gigantism and graviportal locomotion of the former.
The aim of the present contribution is to describe and re-describe some materials that has referred to Brontornis, as well as to review Worthy et al.’s [24] analysis and re-consider the phylogenetic affinities of Brontornis.

2. Materials and Methods

2.1. Nomenclature

I follow the taxonomic nomenclature employed by Agnolin [16]. In that contribution I regard as valid the genus Tolmodus Ameghino, 1891 instead of Patagornis Moreno and Mercerat, 1891, following Patterson and Kraglievich ([14]; contra [2]). Following Agnolin (2006), the genus Onactornis is restricted to the species O. depressus Cabrera 1939, and probably O. pozzi Kraglievich, 1931, and the genus Devincenzia is considered as distinct from Onactornis and represented by its type species D. gallinali Kraglievich, 1932 [2,16,25].
The terms Phorusrhacoidea Ameghino, 1889, and Phorusrhacos Ameghino, 1887 are used instead of Phororhacoidea Patterson, 1941 and Phororhacos Ameghino, 1889 following Brodkorb [12] and Buffetaut [26].
I follow the anatomical nomenclature employed by Baumel and Witmer [27], with details on muscular attachments and syndesmology taken from Zinoviev [28].

2.2. Phylogenetic Analysis

With the aim to test the phylogenetic relationships of Brontornis proposed by Worthy and collaborators [24], I followed the character definition and numbers of Worthy et al. [24] (see Appendix A). The resulting data matrix was composed by 290 characters and 48 taxa.
The matrix was analyzed using TNT 1.5 [29], with all characters weighted equally. The dataset was analyzed under equally weighted parsimony. A total of 1,800,000 trees was set to be retained in memory. A first search using the algorithms Sectorial Searches, Ratchet (perturbation phase stopped after 20 substitutions), and Tree Fusing (5 rounds) was conducted, performing 1000 replications in order to find all tree islands (each replication starts from a new Wagner tree). The best tree or trees obtained at the end of the replicates were subjected to a final round of TBR (tree-branch-swapping) algorithm.
Two different phylogenetic analyses were performed (Figure 1). The first one follows strictly that of Worthy et al.’s [24] unconstrained analysis. This resulted in the recovery of 13 Most Parsimonious Trees (MPTs), of 1567 steps, with a consistency index of 0.26, and a retention index of 0.65, which were summarized using a strict consensus tree (see Discussion).
As a branch support measure, Bremer support was calculated, and as a measure of branch stability, a bootstrap resampling analysis was conducted, performing 10,000 pseudoreplicates. Bremer support was calculated after searching for suboptimal trees and not with the script that accompanies the program. Both absolute and GC bootstrap frequencies are also reported (Figure 1).
The second analysis was carried out with the modifications in the scorings of Brontornis and Gastornis remarked in the “Discussion” section. This resulted in the recovery of four most parsimonious trees (MPTs) of 1564 steps, with a consistency index of 0.26, and a retention index of 0.65, which were summarized using a strict consensus tree (see Discussion).

2.3. Institutional Abbreviations

FM-P, Field Museum of Natural History, Vertebrate Palentology Collection; MACN A, Colección Nacional Ameghino, Museo Argentino de Ciencias Naturales “Bernardino Rivadavia”, Buenos Aires, Argentina; MACN Pv, Museo Argentino de Ciencias Naturales “Bernardino Rivadavia”, Buenos Aires, Argentina; MLP, Museo de La Plata, Buenos Aires, Argentina; NHMUK, Natural History Museum of the United Kingdom, London, United Kingdom.
SYSTEMATIC PALEONTOLOGY
Neornithes Gadow, 1893
Galloanseres Sibley and Ahlquist, 1990
Brontornithes Dolgopol de Sáez, 1927
Brontornithidae Moreno and Mercerat, 1891
Brontornis burmeisteri Moreno and Mercerat, 1891
Synonymy. Rostrornis floweri Moreno and Mercerat, 1891; Brontornis platyonyx Ameghino, 1895; Liornis floweri Ameghino, 1895; Callornis giganteus Ameghino, 1895 in part; Eucallornis giganteus (Ameghino, 1895) Ameghino, 1901 in part [1,2,12,18,19].
Lectotype. MLP-88-91, left femur, tibiotarsus, fibula, and tarsometatarsus belonging to the same individual [12,30].
Diagnosis. Giant bird with graviportal proportions (tibiotarsus/tarsometatarsus ratio: 1.88) and the following unique combination of derived characters: distal end of tibiotarsus strongly anteroposteriorly compressed and with lateral margin forming an acute ridge of bone; distal end of tibiotarsus lacking supratendinal bridge [19], extensor groove shallow, poorly defined and medially tilted, retinacular tubercles feebly developed, prominent pyramidal-shaped prominence (central tubercle for attaching the lig. meniscotibiale intertarsi; [19,31]); tarsometatarsus having hypotarsus situated distal to the articular level of proximal cotylae [2], absence of posterior opening of the distal vascular foramen due to the unbifurcated condition of the canalis interosseous distalis [10], absence of fossa or scar for the first metatarsal [19], and proximodorsal margin of metatarsal trochlea III strongly projected [32].
Remarks. To date, the only certain member of Brontornithes and Brontornithidae is Brontornis burmeisteri [15]. However, recent finding of an incomplete distal tibiotarsus from the Oligocene of Bolivia [33] suggests that Brontornis-like taxa were probably more geographically and temporally widespread than thought.
Referred material. MLP 20-110, distal half of a left tibiotarsus with abraded distal condyles (Figure 2); MLP 20-581, distal end of left tibiotarsus without distal condyles (Figure 3).
Locality and horizon. The specimens come from old collections at the La Plata Museum, and thus, collecting data are scarce. MLP 20-110, originally referred by Moreno and Mercerat [3] to Rostrornis floweri (a junior synonym of B. burmeisteri; [1,9,12]), comes from the Santa Cruz Formation (Middle Miocene), at Santa Cruz province; more details on provenance are not available [3,30]. MLP 20-581 only figures in the catalogue as “?Liornis sp.” without any additional data. However, it is possible to infer that it corresponds to the distal end of tibiotarsus mentioned, and was briefly described by Dolgopol de Sáez [10]. If this is the case, MLP 20-581 was collected by Federico Berry in the Santa Cruz Formation (Middle Miocene) in Santa Cruz province.

3. Description

MLP 20-110 and MLP 20-581 represent the incomplete distal end of tibiotarsi lacking distal condyles. Because both materials are similar in all features, the description is based on the most complete individual (MLP 20-110) and is complemented in some cases by MLP 20-581.
The tibiotarsus shows a nearly straight shaft that is proximally ellipsoidal in cross-section, with convex anterior and posterior surfaces. Distally, the anterior surface of the bone becomes transversely flat. Although poorly preserved, the distal intercondylar fossa is transversely expanded and weakly undercuts the proximal margin of the distal condyles, forming a shallow transverse ridge of bone. Although distal condyles are abraded, they appear to be not strongly posteriorly extended. The posterior trochlea cartilaginis tibialis is poorly-defined, and is dorsoventrally low, with shallow delimiting crests. The extensor groove (linea extensoria in Buffetaut [33]) is aligned with the medial condyle, it is transversely wide and is poorly delimited by very shallow ridges of bone. Although there is no bony bridge on the extensor groove, there is a well-developed ridge of bone on the medial surface of the groove that indicates the insertion of a tendinal sling, which represents a low retinacular tubercle. Limiting the lateral surface of the distal end of the extensor groove there is a pyramidal bump (tubercule central of Ameghino [9]; central tubercle of Buffetaut [19,33]; attachment of the lig. meniscotibiale intertarsi; Zinoviev [28]), that is indistinguishable in size and shape from the ascending process of the astragalus [34] fused to the tibia and present in some ratite birds (e.g., Rhea, Aepyornis; see [33]) and basal ornithurines [35]. The distal crest for the attachment of the transverse ligament appears to be absent. In medial view, the shaft is smoothly convex, whereas in lateral view it shows a prominent proximodistally extended, sharp and acute bony crest.

4. Discussion

4.1. Comments on the Genus Liornis Ameghino, 1895

The genus Liornis was erected by Ameghino with the aim to include the single species L. floweri [2]. The material on which Ameghino based his species was the incomplete distal end of tibiotarsus, tarsometatarsus, and pedal phalanges of a single individual (Figure 4). Ameghino [9,36] assigned it to the Phorusrhacoidea, and distinguished Liornis from other terror birds by having the tibiotarsus with anteroposteriorly compressed and transversely expanded shaft, flat anterior surface of the distal shaft without deep muscular ridges and scars, poorly defined extensor groove, and absence of supratendinal bridge. The tarsometatarsus was characterized by its wide and anteroposteriorly compressed shaft and the absence of impression for the hallux. Due to these unique features, Dolgopol de Sáez [10], in his overview of phorusrhacoid birds, considered it as a valid genus, probably related to the genus Brontornis within the Brontornithidae (considered by that author as the Order Brontornithes). Kraglievich [6,11] retained Liornis as a valid taxon, and considered that due to its hindlimb proportions, it must be distinguished from Brontornis at the subfamily level at least, and thus, established the ad hoc subfamily Liorninae within the Brontornithidae [6]. More recently, Brodkorb, in his renowned “Catalogue of fossil birds” [12] synonymized Liornis floweri to Brontornis burmeisteri without discussing this in detail, a point of view followed by Tonni [1] among other authors. Later, Alvarenga [37] and Alvarenga and Hofling [2] considered that Liornis was a synonym of Phorusrhacos longissimus, but they did not discuss this point of view in detail; a criterion was followed by Bertelli et al. [38] and Alvarenga et al. [23]. More recently, Buffetaut [18,19,33] analyzed the materials of Liornis floweri and included it as a junior synonym of Brontornis burmeisteri. Ameghino [9] noted that the tarsometatarsus of Liornis differs from Brontornis in lacking any sign of scar for the hallux and because its tibiotarsus lacks a supratendinal bridge. However, both differences appear to be misinterpretations, probably due to the paucity of available specimens at that time. The presence of a hallux scar proposed by Ameghino (and followed by Agnolin [8]) was most probably a mistake based on artifact bone preservation. As noted by Buffetaut [19], there is no evidence of such scar in any of the available Brontornis and “Liornis” specimens. Further, the presence of a supratendinal bridge in all available specimens cannot be corroborated; instead, a pyramidal-shaped tubercle delimiting the extensor groove is present [19]. In this way, the differences reported by Ameghino between Brontornis and Liornis are not valid, and thus, Liornis should be considered its junior synonym, following previous authors.
In sum, the tibiotarsus of Brontornis (including Liornis) clearly departs from that of phorusrhacids (and most birds; Figure 5) in a unique combination of characters, including distal end strongly anteroposteriorly compressed with its lateral margin forming an acute ridge, strongly medially oriented medial condyle, small and rounded distal condyles that are joined by a transversely oriented ridge, low and poorly defined trochlea cartilaginis tibialis, absence of a supratendinal bridge, poorly excavated extensor groove that is medially tilted, feebly developed retinacular tubercles, and the presence of a prominent pyramidal-shaped prominence for attaching the lig. meniscotibiale intertarsi [3,10,19,33]. With this new evidence at hand, I re-scored the tibiotarsus of Brontornis in the Worthy et al. [24] data matrix (see below).

4.2. The Quadrate Bone Referred to Brontornis burmeisteri Moreno and Mercerat, 1891

Skull material referred to as Brontornis is very scarce and consists of isolated and incomplete jaws, as well as a single and incompletely preserved right quadrate bone [2]. The latter was ambiguously associated with Brontornis remains [3], and as such, it was not included in their data matrix by Worthy et al. [24], a criterion with which I concur.
In any way, this quadrate shows several features that are worth analyzing. This element was interpreted by Agnolin [8] as having only two condyles, constituting an important piece of evidence for galloanserine affinities of Brontornis. However, Agnolin misinterpreted the quadrate bone anatomy of Brontornis as demonstrated by Worthy et al. [24]. The later authors compared the quadrate with that of the phorusrhacid Tolmodus and found some similarities, including the presence of three quadrate condyles. In the view of these authors, the quadrate indicates that Brontornis belongs to Neoaves and not to Galloanseres.
However, the Brontornis quadrate (MLP 20-111; Figure 6) is different from the homologue of any known bird, especially with those of phorusrhacoids such as Tolmodus and Patagorhacos [39,40].
The distal end of the quadrate shows two well-defined condyles that are relatively elongate and differently oriented from that of phorusrhacids (Figure 6I,J). Worthy et al. [24] recognized the existence of a caudal condyle. However, I am not certain about the homology of this structure. At first, in contrast with phorusrhacids and other birds, this “caudal condyle” is represented by a shelf-like prominence that is dorsally positioned with respect to the distal condyles and shows a flattened to slightly concave distal “articular” surface. This condition is very different from that known in most other birds, such as in Patagorhacos, in which this condyle is at level with the medial and lateral condyles and is notably convex (Figure 6I). A bony flange somewhat similar to that present in Brontornis is exhibited by dromornithid anseriforms [41]. In Brontornis the “caudal condyle” is medially separated from the medial condyle by an oval-shaped and well-defined supracondylar depression that is unique to this taxon.
The pterygoid condyle is represented by an acute and prominent process that differs from that of most birds, including phorusrhacids, in which it is represented by a rounded articular surface. In pseudodontornithids and some anseriforms such as Anseranas and Dendrocygna, this condyle is also represented by a prominent and relatively acute process [31,42]. It is separated from the orbital process by a well-defined concave surface that is only represented by its base.
A particular trait of Brontornis is its unique and massive pyramidal-shaped quadratojugal process that is very different from the condition reported for most birds. Further, there is no evidence of a quadratojugal fossa or fovea, contrasting with the condition of most birds. Remarkably, the presence of a robust quadratojugal process and the absence of a quadratojugal fovea are features only known in conjunction in dromornithid anseriforms [41,43] and some ratites [43]. Further, Brontornis quadrate lacks any sign of pneumaticity, resembling also in this aspect dromornithids and ratite birds [43].
In sum, the quadrate of Brontornis is very apomorphic and is not matched by any known bird. The existence of a third condyle, the “caudal condyle” is somewhat dubious. The morphology of this condyle clearly departs from that of other birds, and because of its position it is possible that it does not contact the mandible; it is very similar to a bony flange present in dromornithid anseriforms. Further, as remarked by Worthy et al. [24] the association of this bone with those unambiguously belonging to Brontornis is not clear.
Characters modified from Worthy et al. (2017)
As indicated above, and based on the detailed review of new specimens, several postcranial features of Brontornis should be reinterpreted, and this has impact on the codifications carried out by Worthy et al. [24]. As follows, we discuss the changes made on Brontornis scorings.
Femur
ch#213. Brontornis burmeisteri re-scored from 1 to 0. As observed in the femur of Brontornis the patellar groove of the distal end of femur is notably transversely wide (see pl. III Figure 1 in Moreno and Mercerat [3]), being much wider than the lateral condyle. In this way, I re-score Brontornis as 0.
Tibiotarsus
ch#240. Brontornis burmeisteri re-scored from 1 to 0. As indicated in the description above, there exists a pyramidal-shaped prominence at the lateral surface of the extensor groove that represents the attachment for the lig. meniscotibiale intertarsi of Zinoviev [28]. The presence of such prominence is uncommon among birds (it is present in some flightless ratites as Emeus, among others) and may be considered an autapomorphic feature of Brontornis (see [19]; Figure 3).
ch#246. Brontornis burmeisteri re-scored from ? to 0. In the distal end of tibiotarsus MLP 20-581 the groove for the m. fibularis is anteriorly extended, as shown by the concave impression located at the lateral surface of the extensor groove (Figure 2 and Figure 3).
ch#247. Brontornis burmeisteri re-scored from ? to 0. In the distal end of tibiotarsus MLP 20-581 a ridge located adjacent to the extensor groove, represents in all probability the lateral retinacular tubercle (Figure 3).
ch#248. Brontornis burmeisteri re-scored from 1 to 0. This character is somewhat difficult to score, especially because of the absence of a supratendinal bridge in Brontornis. However, as can be extrapolated from the distal end of tibiotarsus MLP 20-581, the distal aperture of the extensor groove shows a subvertically oriented main axis, and thus, it is here scored as such (Figure 3).
Tarsometatarsus
ch#253. Brontornis burmeisteri re-scored from 1 to 0. In a completely preserved Brontornis tarsometatarsus (FM-P13259) the lateroplantar margin of the cotyle is notably dorsally projected, and consequently, it is re-scored as 0 (Figure 7). This character was previously considered by Bourdon [44] as a synapomorphy of the clade Anseriformes + Pelagornithidae.
ch#254. Gastornis parisiensis re-scored from 1 to 0. A complete tarsometatarsus of G. parisiensis described and illustrated by Martin [45], Buffetaut and Angst [46], and Mourer Chauviré and Bourdon [47] clearly showed that the intercotylar eminence of the tarsometatarsus in this taxon was prominent and proximally extended. In addition, G. geiselensis (a species closely related or even a synonym of G. parisiensis) shows prominent intercotylar eminence [48].
Gastornis giganteus was re-scored from 1 to ?. The tarsometatarsus of G. giganteus is known by fragmentary material with eroded intercotylar prominence [49,50]. Because of that, the morphology of this eminence in G. giganteus is considered as unknown.
ch#259. Brontornis burmeisteri re-scored from 4 to 2. Worthy et al. [24] consider the block-like hypotarsus as a derived trait shared between Brontornis and phorusrhacoids. In the same line of thought, Alvarenga and Hofling [2] include as diagnostic of phorusrhacoids a block-like hypotarsus that is subquadrangular in proximal view and subtriangular in posterior view, lacking crests and grooves. However, as recognized by Worthy et al. [24] the hypotarsus of Brontornis is distinctive and very different from the condition exhibited by phorusrhacids, (e.g., Phorusrhacos, Tolmodus [9,24,49]). In Brontornis the hypotarsus in proximal view is subtriangular in contour, showing a prominent and thick medial crest, and a slightly pronounced lateral edge, both separated by a longitudinal tendinal groove (Figure 7). This morphology is indistinguishable from that of Gastornis [8,45,49], and thus, is codified as such (state 2).
ch#261. Brontornis burmeisteri re-scored from 3 to 2. Brontornis was scored as having a flat or convex surface between the medial calcaneal ridge and the medial margin of the shaft. However, in Brontornis (FM-P13259) there exists a notable concave surface medial to the medial calcaneal ridge (Figure 7), and thus is scored as “2”.
ch#271. Gastornis giganteus re-scored from 0 to ?. The incomplete nature of the distal tarsometatarsus of Gastornis giganteus precludes the clear recognition of a surface for articulation with digit I. In this way, this character is coded as “?”.
ch#279. Brontornis burmeisteri re-scored from 3 to 1. The tarsometatarsus of Brontornis was scored as lacking a distal vascular foramen by Worthy et al. [24]. However, such foramen is present in available specimens [9,19] (Figure 7).
Finally, I included in the data matrix the codifications of characters from 280 to 283. These refer to the shape of pedal phalanges and were scored by Worthy et al. [24] as “?”. Probably, Worthy et al. [24] did not include these scorings because there was no direct evidence indicating the phalanges previously referred to Brontornis unambiguously belong to this taxon. However, two phalanges are preserved in the single associated specimen on which Liornis floweri (a junior synonym of Brontornis burmeisteri) is based (NHMUK PV A580) [9,19]. These phalanges are massive, transversely wide, and ventrally flat, a combination of features that are exhibited by phalanges previously referred to Brontornis [2,3,9]. In this way, the specimen NHMUK PV A580 confirms previous referral of pedal phalanges to Brontornis, and thus, are coded in the data matrix as such.

4.3. Phylogenetic Results

With the aim to test Worthy et al.’s [24] analysis, only hindlimb material was included in the data matrix. Worthy et al. [24] did not include in their work several bones that have doubtful association with material unambiguously belonging to Brontornis. These materials include vertebrae [3,9], quadrate [3], and mandible [2,3,9,18]. These elements, particularly the mandible, show several features reminiscent to giant galloanseres such as dromornithids and Gastornis [8,18], and their inclusion in the data matrix may give additional support to the galloanserine affinities of Brontornis. In any case, it is preferred to exclude the codification of these elements in the data matrix following Worthy et al. [24].
The phylogenetic analysis here performed resulted in the nesting of Brontornis among Anseriforms in a clade formed by gastornithids and dromornithids, in a position similar to that proposed by Agnolin [8] (Figure 1). It is worthy of mentioning that forcing the position of Brontornis as a cariamiform results in a tree 1569 in length, having five additional steps.
The clade grouping dromornithids and gastornithids was named by Worthy et al. [24] as Gastornithiformes, to which, based on present analysis, Brontornis may belong. In any case, this clade formed by giant graviportal fowls is sustained almost by hindlimb features (characters 202, 211, 215) and it is not improbable that this group may be the result of convergent features related to graviportality (see discussion in [24]). In their work, Worthy et al. [24] concluded that Brontornis resolved as sister to Cariamiformes, but with very low support. They recognized that Brontornis was very different from other birds, and indicated in several parts of the text that the position of Brontornis in the phylogenetic tree is unstable. Because I agree with Worthy et al. [24] in that Brontornis is still incompletely known, it is possible that its inclusion within Gastornithiformes is not strongly warranted.
Worthy et al. [24] listed some similarities shared by the hindlimb of Brontornis and phorusrhacids, including a lateral excavation at the medial surface of the lateral condyle of femur, and a block-like hypotarsus. The first condition is known to occur in Gastornis and dromornithids [50,51], suggesting that it is not only exclusive of phorusrhacids, but is also widespread among giant anseriforms. On the other side, as indicated above and as recognized by Worthy et al. [24], the morphology of the hypotarsus of Brontornis is very different from that of phorusrhacids, being very similar to the condition exhibited by Gastornis and dromornithids [19,41] (see above, analysis of character 259). Both in Gastornis and Brontornis, the hypotarsus is subtriangular-shaped in proximal view, with a prominent medial crest and a reduced lateral edge. Further, Worthy et al. [24] recognize that mandibular and hindlimb shape structure of Brontornis differ substantially from phorusrhacids. The same seems to be true for the quadrate bone, as indicated in the descriptive section of the present contribution.

5. Conclusions

A review of the character codifications for Brontornis burmeisteri carried out in the comprehensive work of Worthy et al. [24] resulted in a change in the phylogenetic position of this taxon. This change argues against the sentence of Worthy et al. [24] that declares that it was conclusively shown that Brontornis is not a galloanserine bird. After few changes in the data matrix, Brontornis results as part of a clade composed by the giant anseriforms designated by Worthy et al. [24] as Gastornithiformes. This result is in agreement with recent proposals that excluded Brontornis from phorusrhacoid cariamiforms (where it was traditionally nested) and included it among Anseriformes [8,16,18].
Graviportal anseriforms of the clade Gastornithiformes (sensu [24]) are represented by Eurasian and North American Paleogene Gastornis and kin [17] and by Paleogene and Neogene Australasian members of the Dromornithidae [41,52]. To these, it should now be added the Paleogene-Neogene brontornithes from South America [17,33]. If this phylogenetic grouping is correct, a widespread radiation of giant anseriforms occurred along several landmasses during the Paleogene. The paucity of the fossil record of these giant birds still precludes a detailed framework to understand the palaeobiogeographic history of these birds.
Finally, the nesting of Brontornis among herbivorous giant anseriforms [5,17,24,46], together with several aspects of its mandibular morphology [8,18] reinforces previous thoughts that Brontornis was herbivorous in habits (Figure 8).

Funding

This research received no external funding.

Institutional Review Board Statement

Not applicable.

Informed Consent Statement

Not applicable.

Data Availability Statement

Not applicable.

Acknowledgments

Special thanks to M.D. Ezcurra and A.G. Martinelli (MACN), and M. Reguero and M. de los Reyes (MLP) for allowing to study material under their care, and for their help during the revision of paleontological collections. E. Buffetaut shared comments regarding the status and affinities of Liornis. I thank T. Worthy for discussions about phylogeny and anatomy of basal birds. Special thanks to A. Agnolin for the life reconstruction of Brontornis in Figure 1. Special acknowledge to E. Buffetaut and D. Angst for inviting me to participate on the Special Issue “Evolution and Palaeobiology of Flightless Birds”. I thank two anonymous reviewers whose comments improved the quality of the present work. This contribution was financed by PICT 2018-01390 (ANPCyT).

Conflicts of Interest

The authors declare no conflict of interest.

Appendix A

Data matrix modified from Worthy et al. [24]. The number of characters and taxa (290 and 48, respectively) as well as character description and states follow Worthy et al. [24]. Scoring modifications are almost restricted to Brontornis and Gastornis species (see above).
Tinamus_robustus
20001000100220000000000001000012000000000-330000000?001111100001001001000000022221100211111001200311100110010010021-110212012110012121111010110101130001010002100000101001000002200212000010000000001011010001110000100022000000100101100011001100010111000110012200311021010010110101100020012000
Vegavis_iaai ??????????????????????????0?????????????1001???????????????1????0??????011???0?????????0010001001000010100?10?????0000-1000000001220-000?000???????????01102011210101?0101021?0????20?????00100000010012001100401101000112001101010020??????????00100??1???????12200???????????????????????????111
Chauna_torquata 2000111100011011021101011001101111011111100101011110100000010003000102200010100001001011000021001000000010010110111-1000000000100000-00000[30]00011000110111101200200-010000011011000000011000000100010010001010000001110000100011000011010000010121021000020011000122021100101000010010200000010?101
Anhima_cornuta 2000111000011010021101010001100101011111100101011110100010110003000102200100100001000210100001101100000000100110111-1000000000?00020-00100000011000110111101200100-0110001100011001100110000001000110010010100100101110100001010000110100110101210210000200110011200221001010000000101000000102101
Wilaru_tedfordi ???????????????????????????????????????????????????????????????????????????????????????0110001001300110110000011010010-0000000111020-000001110110003001100020101002011010002??????????????11010000110010010000101101100010001?????????000000101110210000200010010?2031200101001010010200??????2??1
Presbyornis_pervetus 00111?110112?11010110?01??0221??1000????1???1100111011011101110310011?1??????0???1000000110001001300010110000??1?10010-0000000101010-00000100011100300111002110210101001011201020??10011000001000011001001011010010110001100010000012000001110111021000020001001200011100100110020010200????3?2101
Anseranas_semipalmata 0110121100011?1010110100100221021101111110221101101010000001011310011201011111001100001000000110020000001100011100001000000000000000-00000000011000000111001010110100000000001110011011100001100000000100100001000011100000001000001101000010011102100002000000000011110000100011000020000002021-0
Dendrocygna_eytoni 211112111002021010110100100221021101111110221101111010001001011310011101001011111000011110002100110000111201011001011101010000100000-0001011001100000011000112020010000000110111101201100011100000000010010000101101100100001110000110100000001210210000200100002101311001011110100112000000302??0
Cereopsis_novaehollandiae 211112111012211110110100000220021101111110021101110110001011011311011200001010111100021000001102110011011001011011001000000000100000-0000011001110000011101102010120010100120011010201100101100000100110011010200101000001001111000111001000001210210000200000001201211011011110110111000000302100
Anser_caerulescens 011112111002101010110101100221021101111110221101111010001001111311011201001010110110101010002102110001011000011011011000010000100000-0000111001100020011001112010110110200020012000202100001100000100010011100200101100101001110000010000000101210210000000100012200311001012010210111000000302100
Malacorhynchus_membranaceus 021112111102221010111101100221021101111110221101111010001101111310011101001110121000111011002100030010111101011001011110010000111220-00011120011100210110011120210111002001210120012021100111000001000110100002011010000000011110001101000000012102100001000000120003110000111102101120000?0302100
Tadorna_tadornoides 211112111002111010111100000221021101111110221111111010001101111311011101011010121000121011002100010001011001011001011100010010110110-0001112001110020111001112010011010101020112001202100001100000100010011100200101000101000111000111100000101210210000100000002200311000011110210112000000302100
Leipoa_ocellata 210010001000111001010101000120110000?010100200001101010111010002001100000101023221102201111120200111100000100002021-010212012111001100210010010001200000012002101000101200000001211110110011001000101011010000000100000010000010100111100010111200101101000111111011000110110002000002100021022??0
Megapodius_reinwardt 2100100010001010000101010001201100000010101200001101010111010002001100000101023221102201111120200111100000110002021-010212012111001100210010010101200000012002101000101201100001201100110011001000001011010000000100000010000010100101000010111200101101100111111011000110010002000002000021022??0
Eulipoa_wallacei 010010002000101000010101000120110000001010120000110101011101000200?100000101?23221102201101120210111000000110112021-0102120121110111002100100101012000000111021020001012010000022000101100110110001000100100000101001000010010101101010000101011001011011001111010111001100100020000021000110????0
Megapodius_eremita 22001000100010100001010100012011000000101012000011010?01110100020?1100000101123221102201110120200111100000110002021-010212012111001100210010010101200000012012100000101201000001200100110011001000001011010000000100100010000010100100000010111200101101100111111011000110010002000002000021022110
Alectura_lathami 2200100010001010010101010001201100000010101200001101010111010002001100000101023211102201111120200111100000100002021-010211012111011100210010010101200000012002101000101201000001211110110011001000001011010000000100000010000010100111000010101200101101100011111011000010110002100002000021022100
Talegalla_fuscirostris 220010011000101000010100000120110000????100200001101010111010002001100000101023211102201111120210111000000100002021-020211012111021100210010010101200000012002100000101101000001211100110011000010001011010000000100100010001010100110100010111200101101100011112011000100110002000001100001022??0
Macrocephalon_maleo 120010012000101001010100100120110000001010120000110101111101000200?100000101023221102201101120210111000000110012021-0102110121110211002100100100012000000110021010001012010000012101?011?0110000000000100100000101001000100010001001000000101012001011011000111110111110000100021000021000010?2??0
Gallus_gallus 200010000101121001010101010120110000001010120000110101011111000300210000[30]10102[26]221102201110120201111101000110002021-110212112111022111210001110101200001012002101000101211000001200010100011000000100011010000101101000011000010100110[9]00010101100101101000111011011110000110101100002100000022100
Phasianus_colchicus 210010000101011001010101000120110000????101200002101000111110003000100001111020221102201110120200111100000100002031-110212112111002111210011110101200101012012112000101211000011201010100011001000100012010000111100000112000010100111100110101100101101000111011011211001110100100002000000022??0
Coturnix_pectoralis 210010000001111001010101010120110000???0101200001101010111110003002100000101?22221102200110120200311101100100002031-131212112111001111210010010101200101012002102000101210000002201010100010000000100011010000110000000011000000100110100110101200101101000111111011210000110110100002000000022??0
Acryllium_vulturinum 210010000101001010010101000120110000????101200001101010111110003000100001101123221102201110120200311101100100002021-12021211011001111121000001010120000101200210000010110000000120100010001100000010011101000000010010001000000010011010001010120010110[30]100111011011110000011001100002000000022??0
Megavitiornis_altirostris ?22010?21000?0?0000?0????0012011??00????1????0001101000100[30]1000200010?0001?1?2321?01???011012020---1---10-1-0?????--0---1----1--0--1-00100----------010---2002?-000-1---0-01000??01??0?1??1000000001101101001000010101011200000011011110000010120010110100001111101111101011000201000100100??????0
Crax_rubra 2100100000020110010101000001201100000011101200011101110111110003000100000[30]01123021102201111120200311100000110002021-1202120121110111112100010100002200000120121000101012100000012000101110100000001000100100000001010000110000001001022-0010101200101001100111112011010000110002000002100000122??0
Ortalis_vetula 2000100000020110010101000101201100000011101200111101010111110003002100000101123021102201111120200111101000110002031-12021201211102211121000001000020010001201210001010121000000120001010101100000010001101000000010110001000000000010110011010120010100110011101101101?000110002000002100000122100
Sylviornis_neocaledoniae ?22010022000001000010100100120110001????100210001101?001010100?200?100001101?2??2??????11111202-----------1-0?????1--10--2---1--0----02100----------010---200211001-10110102?0???????211??1000100011101001000000010000001100000011011010000000120020110101001111121111101000000001010220001???2??0
Dromaius_novaehollandiae
00010000110220100000001001000002000000000-331010001000010100000100100301011100222101102--1--0----------1----1-------------------0----00--------------1--------?-------------10120012020000011000101001100000104001001001101100001111101110120101-101211-21100111023032200101211011010121102000200-
Dinornis_robustus
22000000100220100000001011000011000000000-3310000010?001?10000000010030100?100222100021--1------------------1-------------------------------------------------?-------------10120012020110001001000011000010113201100111100000001000111011020000-001211021101111122031202-00001001-1-130101?0120??
Struthio_camelus
00010000010210100000000001000002000000000-331010000020010100000101100300000000221101011--1-------------1-0--1-------------------------------------------------?-------------10101002020000011000101000000000104001021001100000101021021111120001-1-021--211011010230221111012110--0-1-1210200?200-
Genyornis_newtoni ??2?1?????????????????????????10??????????????0021010?0??00100??????0?00?????02121000020-10-2----------100--1------------------------0---------------0----------------------111??0??001110001000110110001?011032011200111010111001111010100100020011210110010101021021202110001010010111112??2???-
Dromornis_stirtoni 022110?2?00?001?021?????100??010????????1102110021001000000100210?0?0??0010??02221000020-10-2----------000--1------------------------0--------------------------------------111200?20211100010000111100012011032011200011010110001111110100110020010210110010101023031200110001010110111112???1??-
Dromornis_planei 02211022?00?00110211?100100110100???????100211002101?1000??10021000?0??0???????????????--1?-2----------???--1------------------------0--------------------------------------??????????????001000011110001?01103201120001101011101?1???1010011002001021011001010102303120?110001010110111112???1??-
Dromornis_murrayi 0?2110?2?00?00110211?100000???10????????????11002001?0000??100210?0?0?20??????2121000020-10-2----------000--1------------------------0--------------------------------------??????????????00100001011000020110320112001120101?1???????10100100020010210110010101023031202?100010001101111?2???1??-
Ilbandornis_woodburnei 0?2??????00?00110211?1001001?010????????100211002101??0?1??1002?0?0?0??0??????2211000020-?0-2----------?----1------------------------0--------------------------------------011?00??021110001000010110000?011032011200111010111011111010100100020010210120010101023031203111001010010121112???0??-
Ilbandornis_lawsoni ????????????????0211??????0?????????????1002?1002101??0?1??1???????????0???????????????0-?0-2----------?----1------------------------0--------------------------------------??????????????001000010110100?011032011210111010111011112110100110020010210120010101023031202101101010[30]10011??????0??-
Barawertornis_tedfordi 0?2???????????1?0???????100??010?????????002???????????????1000100000??0????????????????-??-?----------?----?------------------------?--------------------------------------??????????????001000010?10100?011030011200111010111001112010100?100200102?01200101010230?110311?001000?10111??????0??-
Lithornis_promiscuus 000000000102200?000?0?????00001?000000000033?0100010?0010100010100100?200101100111001220110101030300100100010100021-0000000000100120-0220010102100030100112002?1100010000101000?200212011?1110000000001100000111000010002210000011010110111110111100000-00001111223011200001000010000200?????????0
Lithornis_plebius ??????????????000000?0100000001?????????00331?0000000011010???????????2?010?10?????????0110101030300110101210???0?1-1000000000100120-0211010102100030000112002?2100010100101?00??00??200??1110000000001100000111010010002210000010011110101110111100000-00011111223011200101000010000200?????????0
Paracathartes_howardae 00000?????????000000???000???????????????033?000?000?0110100??????1?????0??0?????????????10101020300100100210???0???1000000000?00120-022101000?100000000111202121010101001????????????????1110000010001100020111010010??2210000010011110001110111100000-10000111222011200101000010000200000??????0
Burhinus_grallarius
000110000112021001100110001--0120110001111000010100020101100000000000010011101221100120001000100030011110221011102001000000000001110-00200111021001300010020020200201000011100020012001100100000001110100200000001010010111000100002202-00010011101011102000100122103210010111101111021100000?2100
Porphyrio_melanotus
010110010002201001000100001--0020110001111000010110120100100000001000100111101221101121001000100000000010001000003021002020000001000-002111200000000011111201102001000000012001000001010001000000000101200000111100110001100000000021010001000120021000020011000101001100101010111-001000000002110
Antigone_rubicunda
100110000102101001000100011--002011000111100001011002010010000000000020?101000000100002001000120100000000010000-031-1000000000000000-1020002102100000011010111011011000000110010001010111010000000100010000001001001100011001100000210100000101100110010200110012211221001011110200002000000002110
Brontornis_burmeisteri ?????????????????????????????????????????????????????????????????????????????????????????????????????????????????????????????????????????????????????????????????????????????????????????????0????1001001?010?3101120010100001100?1110100001?000-11120000000000112202100010101101001-111102???????
Gastornis_parisensis ?22110????????????????????????????????????????101100?0001?01002100000??????1???????????1-10-0----------??0??1?????-------------------0---------------------------------------?????????????001000?0??0?100?011?3?011?0?101?10?000010110000001101210210?010000000?02?022100?0?00101011011??????????-
Gastornis_giganteus 022110120001?010010101001?0020100101????100211101100?10011?1002100000000110110?????????0-10-2----------100--1?????-------------------?-----------0--011-------?---1-1------21002??12101110000000011100000201103001100010120000101?011100000110121020000000010?0112202120010100?000110220102??????-
Tolmodus_inflatus 022010100102101100010100100010100111????1?1?10001110?100010000000100002?000100001100002111002010--00-00100010???????????????????????????10001?1000000?1111010200000010010101101000101011??1010000011111000011101011100111000001011111010010000110010100111001001124021102101101110010110??1???????
Cariama_cristata
000010010102121001000100101--002011000111100100011000000010000000020002000010002110012101100211[25]1300101100110000021-10-0000010001210-021110100101110001111012201001010100100001[9]001010111010000000111110000111010111001110001011001120100012001100101000200010011221212021012110100101100000002??0

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Figure 1. Phylogenetic analysis depicting the position of Brontornis burmeisteri. (A) hypothesis proposed by Worthy et al. [24]; (B) hypothesis proposed in the present study; (C) consensus tree showing branch support measures. From left to right: Bremer support, absolute bootstrap frequency, and GC bootstrap frequency. The arrow indicates the position of Brontornis. Abbreviations. Anserif., Anseriformes; Cariam., Cariamiformes; Galli., Galliformes.
Figure 1. Phylogenetic analysis depicting the position of Brontornis burmeisteri. (A) hypothesis proposed by Worthy et al. [24]; (B) hypothesis proposed in the present study; (C) consensus tree showing branch support measures. From left to right: Bremer support, absolute bootstrap frequency, and GC bootstrap frequency. The arrow indicates the position of Brontornis. Abbreviations. Anserif., Anseriformes; Cariam., Cariamiformes; Galli., Galliformes.
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Figure 2. Brontornis burmeisteri (MLP 20-110) distal half of left tibiotarsus in (A) anterior; (B) lateral; (C) posterior; (D) medial views; (E) detail of its distal end in anterior view; and (F) distal view. Abbreviations. eg, extensor groove; lc, lateral condyle; mc, medial condyle; tct, trochlea cartilaginis tibialis; tr, transverse ridge. Scale bar: 5 cm.
Figure 2. Brontornis burmeisteri (MLP 20-110) distal half of left tibiotarsus in (A) anterior; (B) lateral; (C) posterior; (D) medial views; (E) detail of its distal end in anterior view; and (F) distal view. Abbreviations. eg, extensor groove; lc, lateral condyle; mc, medial condyle; tct, trochlea cartilaginis tibialis; tr, transverse ridge. Scale bar: 5 cm.
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Figure 3. Brontornis burmeisteri (MLP 20-581) distal end of left tibiotarsus in (A) anterior; (B) posterior; (C) lateral; (D) medial; and (F) distal views; and (E) cross section of the shaft. Abbreviations. ct, central tubercle for the lig. meniscotibiale intertarsi; df, distal fossa; eg, extensor groove; fi, surface for fibula; ri, proximodistally extended lateral ridge; rt, possible lateral retinacular tubercle; ts, ridge representing medial retinacular tubercle. Scale bar: 5 cm.
Figure 3. Brontornis burmeisteri (MLP 20-581) distal end of left tibiotarsus in (A) anterior; (B) posterior; (C) lateral; (D) medial; and (F) distal views; and (E) cross section of the shaft. Abbreviations. ct, central tubercle for the lig. meniscotibiale intertarsi; df, distal fossa; eg, extensor groove; fi, surface for fibula; ri, proximodistally extended lateral ridge; rt, possible lateral retinacular tubercle; ts, ridge representing medial retinacular tubercle. Scale bar: 5 cm.
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Figure 4. Brontornis burmeisteri; specimens on which Ameghino [9] based the species Liornis floweri Ameghino, 1895 (NHMUK PV A9058 and NHMUK PV A580). (A) right distal half of tibiotarsus in anterior view; (B,C) distal end of left tarsometatarsus in (A) anterior; and (B) posterior views. (AC) modified from Ameghino (1895). Abbreviations. tr, transverse ridge. Scale bar: 5 cm.
Figure 4. Brontornis burmeisteri; specimens on which Ameghino [9] based the species Liornis floweri Ameghino, 1895 (NHMUK PV A9058 and NHMUK PV A580). (A) right distal half of tibiotarsus in anterior view; (B,C) distal end of left tarsometatarsus in (A) anterior; and (B) posterior views. (AC) modified from Ameghino (1895). Abbreviations. tr, transverse ridge. Scale bar: 5 cm.
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Figure 5. Distal end of left tibiotarsus of (A,D) Onactornis pozzii (MACN Pv-6554); (B,E) Brontornis burmeisteri (MLP 20-92/93); (C,F) Brontornis burmeisteri (MLP 20-110) in (AC) anterior; and (DF) distal views. Abbreviations. eg, extensor groove; ig, anterior intercondylar groove; sb, supratendinal bridge; tct, trochlea cartilaginis tibialis; tr, transverse ridge. Not to scale.
Figure 5. Distal end of left tibiotarsus of (A,D) Onactornis pozzii (MACN Pv-6554); (B,E) Brontornis burmeisteri (MLP 20-92/93); (C,F) Brontornis burmeisteri (MLP 20-110) in (AC) anterior; and (DF) distal views. Abbreviations. eg, extensor groove; ig, anterior intercondylar groove; sb, supratendinal bridge; tct, trochlea cartilaginis tibialis; tr, transverse ridge. Not to scale.
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Figure 6. Comparisons between the quadrate referred to Brontornis burmeisteri (B,D,F,H,J,K; plaster copy of MLP 20-111) and the phorusrhacid Patagorhacos terrificus (A,C,E,G,I) in (A,B) anterior; (C,D) lateral; (E,F) posterior; (G,H) medial; (I,J) distal; and (K) proximal views. Abbreviations. ar, extended articular surface; cc, caudal condyle; cl, lateral condyle; cm, medial condyle; co, concave surface separating the pterygoid and orbital processes; fo, quadratojugal fossa or fovea; gr, wide groove separating the quadratojugal process and the orbital process; po, orbital process; pq, quadratojugal process; pt, pterygoid process; sd, supracondylar depression or fossa. Scale bar: 2 cm for B,D,F,H,J,K; 1 cm for A,C,E,G,I.
Figure 6. Comparisons between the quadrate referred to Brontornis burmeisteri (B,D,F,H,J,K; plaster copy of MLP 20-111) and the phorusrhacid Patagorhacos terrificus (A,C,E,G,I) in (A,B) anterior; (C,D) lateral; (E,F) posterior; (G,H) medial; (I,J) distal; and (K) proximal views. Abbreviations. ar, extended articular surface; cc, caudal condyle; cl, lateral condyle; cm, medial condyle; co, concave surface separating the pterygoid and orbital processes; fo, quadratojugal fossa or fovea; gr, wide groove separating the quadratojugal process and the orbital process; po, orbital process; pq, quadratojugal process; pt, pterygoid process; sd, supracondylar depression or fossa. Scale bar: 2 cm for B,D,F,H,J,K; 1 cm for A,C,E,G,I.
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Figure 7. Left tarsometatarsus of Brontornis burmeisteri (plaster copy of FM-P13259) in (A) proximal, (B) anterior, and (C) posterior views. (D) detail of the proximal region of the tarsometatarsus in anterior view. The notation includes the characters that were modified from Worthy et al. [24]. ch#253-0, plantar-lateral side of cotyla medialis elevated proximally; ch#259-2, hypotarsus with two ridges; ch#261-2, surface from medial calcaneal ridge to anterior margin of medial shaft concave (shallow fossa parahypotarsalis medialis); and ch#279-1, foramen vasculare distale small and distinct. Scale bar for A to C: 4 cm; D, 3.5 cm.
Figure 7. Left tarsometatarsus of Brontornis burmeisteri (plaster copy of FM-P13259) in (A) proximal, (B) anterior, and (C) posterior views. (D) detail of the proximal region of the tarsometatarsus in anterior view. The notation includes the characters that were modified from Worthy et al. [24]. ch#253-0, plantar-lateral side of cotyla medialis elevated proximally; ch#259-2, hypotarsus with two ridges; ch#261-2, surface from medial calcaneal ridge to anterior margin of medial shaft concave (shallow fossa parahypotarsalis medialis); and ch#279-1, foramen vasculare distale small and distinct. Scale bar for A to C: 4 cm; D, 3.5 cm.
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Figure 8. Life reconstruction of Brontornis burmeisteri. Artwork by Agustín Agnolin.
Figure 8. Life reconstruction of Brontornis burmeisteri. Artwork by Agustín Agnolin.
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Agnolin, F.L. Reappraisal on the Phylogenetic Relationships of the Enigmatic Flightless Bird (Brontornis burmeisteri) Moreno and Mercerat, 1891. Diversity 2021, 13, 90. https://0-doi-org.brum.beds.ac.uk/10.3390/d13020090

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Agnolin FL. Reappraisal on the Phylogenetic Relationships of the Enigmatic Flightless Bird (Brontornis burmeisteri) Moreno and Mercerat, 1891. Diversity. 2021; 13(2):90. https://0-doi-org.brum.beds.ac.uk/10.3390/d13020090

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Agnolin, Federico L. 2021. "Reappraisal on the Phylogenetic Relationships of the Enigmatic Flightless Bird (Brontornis burmeisteri) Moreno and Mercerat, 1891" Diversity 13, no. 2: 90. https://0-doi-org.brum.beds.ac.uk/10.3390/d13020090

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