Snakes are an extremely modified and long-lived clade of lizards that have either lost or highly altered many of the synapomorphies that would clearly link them to their closest sister-group among squamates. We focus here on one postcranial morphological complex, the intercentrum system which in most non-ophidian squamates is limited to the cervical and caudal regions. The Cervical Intercentrum System (CeIS) is composed of a single intercentral element that sometimes articulates with a ventral projection (hypapophyses) of the centrum; the Caudal Intercentrum System (CaIS) is formed by an intercentral element, the haemal arch/chevron bone, and paired ventral projections of the centrum, the haemapophyses. In modern snakes, the intercentrum element of the CeIS is considered lost or fused to the hypaphophysis, and the chevron bone in CaIS is considered lost. Here, we describe new specimens of the early snake Dinilysia patagonica, and reinterpret previously known specimens of Dinilysia and Najash rionegrina, that do not show the expected snake morphology. The anatomy of these fossil taxa unambiguously shows that free cervical and caudal intercentra attached to distinct downgrowths (hypapophyses and haemapophyses) of the centra, are present in basal fossil snakes, and agrees with the proposed loss of post atlas-axis intercentra in later evolving snakes.
Modern snakes are an extremely diverse clade of lizards with an improving fossil record that is revealing unexpected data on a large number of problematic snake anatomical features, i.e., the presence of small to large rear limbs1,2, the otic region and organization of the crista circumfenestralis3, or the presence of a jugal, and the identity of the circumorbital bones4. Though the skull of snakes has been implicated as the major driver of snake evolution5 (against recent claims to the contrary6), the postcranial skeleton of these animals also displays problematic anatomies by comparison to that of other lizards, limbed or limbless, short bodied, or elongate.
One of these problematic postcranial features concerns the morphology of the intercentrum system of lizards, and how that system of extra-central vertebral bodies has been modified through not just lizard evolution, but more particularly, through snake evolution (Fig. 1). The classic review of the squamate intercentrum system7, while thorough and current for the time, only reviewed the osteology of extant squamates and thus characterized the higher level groups around only the anatomy of the modern forms. With the recent discovery of new specimens of previously known fossil snakes, i.e., Dinilyisa patagonica, and new taxa of fossil snakes, i.e., Najash rionegrina, there have been a number of recent studies explicating new data and interpretations of the snake intercentrum system, and more specifically the cervical and caudal intercentrum systems8,9,10,11.
In general terms7, in all squamates with the exception of gekkotans and xantusiids, the intercentrum system is limited to the cervical and caudal regions (Fig. 1). The cervical intercentrum system (CeIS) is composed of a single intercentrum element that in most squamates articulates with a variably positioned pedicle or peduncle of bone arising from the centrum surface that is referred to as the hypapophysis; positioning of the hypapophysis is either anterior on the centrum, posterior on the centrum, or at the inter-centrum contact so that the intercentrum body, is indeed ‘intercentral’. When the intercentrum contacts both the anterior and posterior centra at their articulation, it never fuses to either centra, though it may fuse when articulating with a rostral or caudal hypapophysis.
The caudal intercentrum system (CaIS) is somewhat different by comparison to the CeIS. The intercentrum proper forms a protective arch of bone, i.e., the haemal arch, around the deep arterial system of the caudal artery and associated vasculature and nerves. The haemal arch generally forms a Y-shaped bone, or chevron, the distal extent of which serves as a muscle and ligament attachment zone for the hypaxial musculature. The right and left centrum contact points for the forks of the chevron bone/haemal arch, are a pair of pedicles or haemapophyses. The haemapophyses are generally placed posteriorly on the caudal centrum, but are, in some cases, at the inter-central articulation, and in some squamates the chevron forks fuse to the haemapophyses. In squamates with specialized adaptations such as aquatic locomotion, the haemal arch spines can be distally elongated, in many cases, longer than the neural spines, in order to increase the lateral aspect of the tail for caudal propulsion, and increase the muscle mass used to generate force.
As noted, when first7 characterized, the snake CaIS and CeIS were described based on observations of modern snakes. The ‘cervical’ region of snakes has long been considered ‘lost’ and unrecognizable anatomically, because of the absence of the pectoral girdle as a key landmark7. Still, those authors did report on the presence, often in extremely large numbers and extending some distance posteriorly, of hypapophyses on the anterior precloacals of modern snakes; these ‘hypapophyseal processes’ begin on the axis centrum (just posterior to the one certain intercentrum body present in a modern snake, the atlas intercentrum).
Recent work, looking at the anatomies of both fossil and extant snakes, has made it clear that the neck of snakes can be demarcated based on both osteological and myological anatomies, such that snakes really do possess a neck and thus, diagnosable cervical vertebrae9,11,12,13. Such a distinction is not trivial as the neck/cervical region of snakes would be predicted, based on the fact that snakes are lizards, to display features of a CeIS and thus possess hypapophyses and intercentra. A HOX-gene expression study14 examining Python, concluded that thoracic identity had been overprinted onto the ‘neck’ region in snakes based on the presence of anterior ribs. A responding study15 noted that cervical ribs had not been reacquired in snakes (the morphological feature used14 to qualify thoracic identity), but rather are a primitive feature for all vertebrates including any clade that might be considered the sister-group of snakes. The presence of hypapophyses throughout much of the column of many moderns groups of snakes was cited as indicating that cervical identity, not thoracic identity, had dominated the development and evolution of the precloacal vertebrae in snakes15.
As a result, if “cervicalization” so to speak, not “thoracalization”, has dominated snake neck and thorax evolution (the precloacal vertebral column), it should come as no surprise that the cervical region of fossil snakes is easily demarcated, and that the cervical vertebrae of fossil snakes would reveal the presence of unfused intercentra articulating with hypapophyses in the anteriormost cervicals, but still posterior to the atlas-axis intercentra9,11,12. These fossil anatomies provide important information on the presence of intercentra in the anterior part of the column, the CeIS, at an early stage in snake evolution.
With respect to the CaIS, modern snakes do not possess a Y–shaped, or chevron–shaped haemal arch, but instead generally possess paired, ventrally directed haemapophyseal processes of the centrum7,10; these paired processes in snakes have been long interpreted to represent the intercentrum in some form or another even though they are classically referred to as ‘haemapophyses’. Clarity on this problem is revealed only by reference to the anatomies preserved in fossil snakes, where new specimens have been found with well-articulated caudal elements that include distinct haemapophyses and chevrons/intercentra: Eupodophis descouensi, Haasiophis terrasanctus, and Wonambi naracoortensis11,16,17. Despite the observed anatomies, the homology of the CaIS in these fossil taxa to the CaIS of other squamates has been challenged by some authors10,18 prior to the study of Palci et al.11.
The intent of this study is to report data on the CaIS and CeIS from new specimens of the fossil snake Dinilysia patagonica Woodward, 1901. Here, we will refer to the downgrowths of the centra that act as contact points for the cervical and caudal intercentral elements as hypapophyses and haemapophyses respectively, instead of using others terms that have been used in the literature to refer to these structures (e.g., pedicles, pedicels, peduncles, hypapophyses s.s.). A secondary goal is to synthesize these new data with existing data in fossil and modern snakes. We therefore re-characterize the previously described cervical series of D. patagonica9 and compare it to known specimens of Najash rionegrina and build a set of hypothesis regarding the evolution of the CaIS and CeIS in snakes against current phylogenies. We also describe the first known caudal series of the early snake D. patagonica, based on articulated remains from the Bajo de la Carpa Formation of the Neuquén Group (Santonian, Upper Cretaceous), Río Negro Province, Argentina. The specimen described herein comprises a string of 13 vertebrae, from posterior-most precloacals to the first caudals, displaying haemapophyses and articulated chevron bones. This presents unequivocal evidence for the presence of a CaIS in Dinilysia patagonica, and additional evidence of a CaIS in snakes that is homologous to that of other squamates. Comparisons between the CaIS in Dinilysia with other fossil snakes provides important insights on the presence of a CaIS in the early evolution of snakes and it leads to an important interpretation regarding the homology of the ventral projections of the caudal vertebrae among extant snakes (see also11).
Cervical Intercentrum System (CeIS)
Re-characterization and new material of Dinilysia patagonica
Unsuspected vertebral features for the cervicals of the fossil snake Dinilysia patagonica were reported8,9 from a specimen of Dinilysia (MPCA-PV 527) collected at Paso Córdova in 2001 (i.e., a partial skull articulated to a series of five vertebrae [Fig. 2]). These authors purposefully referred to these five vertebrae as cervicals in full recognition of previous work on the subject (e.g.1,7,15,19,20,21). The reasoning used by the authors8,9 for choosing ‘cervical’ over ‘precloacal’ was straightforward: problems delimiting a ‘neck’ as a region along the body axis are distinct from the question of whether or not an anterior vertebra possesses osteological characters that identify it as a cervical vertebra. They argued that the classic criterion7 i.e., presence and position of the first dorsal vertebra with a rib articulating with the sternum, was a delimiter of ‘neck’, and we continue that logic here with the argument that ‘neck’ is not a synonym of ‘cervical’ and that there are osteologies diagnostic of cervical vertebrae in the absence of a ‘neck’. Previous authors8,9 rejected the term ‘precloacals’ in favour of the term ‘cervicals’, even though ‘cervicals’ are a subset of the ‘precloacal’ region in the absence of a defined ‘neck’.
In MPCA-PV 527, the atlas neural arches are small, though mostly still in articulation with the intercentrum; the neural spine is narrow and quite short, projecting slightly posteriorly. The atlas intercentrum is not well preserved and its articulation with the axis vertebra is difficult to clearly define. We agree9 that it is not clear if there is an articulating intercentrum and an axis hypapophysis preserved in this specimen. The third and fourth cervicals have large, posteriorly positioned hypapophyses with large, unfused intercentra (Fig. 2). The intercentrum of the fourth precloacal is not preserved, permitting observation of a deeply concave articulation surface of the hypapophysis. In MPCA-PV 527, in contrast to the more anterior precloacals, the fifth cervical bears a large hypapophysis, with a possible fused intercentrum, and may represent the fate of the intercentrum in all modern snakes, consistent with previous conclusions7 (but see below).
Another set of articulated vertebrae from Dinilysia (MACN-PV-N-116) is described here and are also referred to as cervicals and they preserve some aspects not visible in MPCA-PV 527 (Fig. 2). The intercentrum and neural arches of the atlas are not present in the five vertebrae preserved in MACN-PV-N-116. The axis bears a developed odontoid process and preserves two ventral projections; the first ventral projection, which is large and located beneath the suture of the odontoid process to the axis centrum, represents the second intercentrum. It can be seen that it is sutured to the axis and articulating directly to the centrum, but not by a distinct, raised, hypapophysis. The second ventral projection on the axis is located posteriorly, and forms the first hypapophysis, low and rounded; the corresponding free intercentrum (the third) is lost, which is inferred by the deeply concave surface on the hypapophysis. Although no intercentra are preserved in this specimen, other than the one on the axis, the concave surface of the hypapophysis suggests the articulation of a free intercentrum as seen in the known cervicals of Dinilysia. The fourth vertebra in MACN-PV-N-116 shows quite clearly the same condition that is present in MPCA-PV 527 (Fig. 2). The fifth vertebra in MACN-PV-N-116 bears a narrower and less-rounded hypapophysis that seems to have a similar concave surface to the preceding ones. There are no obvious signs of fusion of the intercentra to the hypapophyses as was proposed for MPCA-PV 5279. The sixth vertebra is broken and its condition cannot be ascertained.
Re-characterization of Najash rionegrina
The holotype of Najash rionegrina preserves parts of the cervical series (MPCA-PV 391, see22). The atlas neural arches are not preserved. As described22 the axis is elongated and bears an odontoid process and well-developed pleurapophyses. Both of the axis ventral projections are posteriorly oriented, and the second one bears on each side a characteristic hook-like lateral projection. As the condition of the axis is not well preserved in the holotype, Najash was inferred22 to show the usual condition in snakes (with the second intercentrum sutured and the third one fused to the axis) based on what is seen on another specimen from the same locality, MPCA-PV 383 (see22). Regardless of the condition of MPCA-PV 383 (which seem to show both intercentra sutured, or only partially fused), assignment to Najash rionegrina has been questioned (see23), and the holotype axis intercentra are most likely sutured to the axis. More important, subsequent description22 characterized the third and fourth vertebrae of Najash as possessing “rod-like” hypapophyses. In contrast, we interpret that the cervicals of Najash rionegrina possess free intercentra. The third vertebra is the one that shows this condition more clearly, where the intercentrum is preserved in place, articulated to the posteriorly positioned hypapophyses (Fig. 2), evidenced by the suture between the two elements. On the fourth vertebra the intercentrum is lost and the rounded hypapophysis shows a deep concave terminal surface as is seen in the cervicals of Dinilysia.
Caudal Intercentrum System (CaIS)
New material of Dinilysia patagonica
MACN-RN-1016 consists of a string of thirteen articulated vertebrae (Fig. 3). The anterior-most five vertebrae of the series show the typical morphology of posterior precloacals, i.e., a strong interzygapophyseal constriction that is more pronounced than in the middle trunk region24. They have well-developed parapophyses with a wide and low haemal keel that is anteriorly separated from the parapophyses by moderately deep depressions, and are pierced by subcentral paralymphatic foramina. None of these vertebrae show evidence of fused ribs as occurs in Najash and many non-ophidian squamates7,23. The three subsequent vertebrae (6th to 8th) are somewhat different from the posterior most precloacals in having a narrower haemal keel and lacking the smaller and more ventrally oriented parapophyses. Additionally, the 7th and 8th vertebrae preserve lymphapophyses (although only their bases are preserved) that have a ventrally directed branch and a dorsal branch, directed laterally, marking the cloacal region of the series. The 6th vertebra of the series is too badly preserved to be properly identified and it could represent either a cloacal or possibly a sacral. The configuration of the lymphapophyses resembles that of madstoiids from Patagonia25 (ROG per. obs.) and contrasts with that of scolecophidians, which have the ventral branch of the lymphapophyses more laterally oriented26. Additionally, alethinophidians typically have three to five vertebrae with lymphapophyses, whereas scolecophidians range from two to six11,26. The type specimen of Najash has been described22 as possessing three caudals bearing lymphapophyses, but that description has been contested23 with the argument that the first of these vertebrae is better interpreted as a sacral.
The succeeding vertebrae (9th to 13th) are regarded as postcloacals based on the presence of pleurapophyses along with a poorly defined haemal keel or lack of it, and, in all except the first postcloacal, haemapophyses (Fig. 3e,f). The anterior postcloacals display distinct posteroventral haemapophyses with a distally articulated chevron. The 10th vertebra preserves only one haemapophysis close to the condylar constriction and lacks an articulated chevron. The following caudals (11th and 12th) have haemapophyses articulating with chevrons preserved in place that consist of paired and elongate arches (Fig. 3e,f).
The paired haemal arches are slightly curved inward and are sutured to a blunt and rounded haemal spine. The distal porous surface of the haemal spine suggests that it was capped by cartilage as in anguimorphan lizards (e.g. Heloderma, FFG pers. obs.). The relatively short chevrons of Dinilysia do not show a long and slender haemal spine, such as the Y-shaped chevrons of aquatic Eupodophis11, which is expected in a terrestrial form27, but are longer than the remarkably short chevrons of the marine snake Haasiophis11. The pleurapophyses are badly damaged in most postcloacals of MACN-RN-1016, but in a few vertebrae they are preserved as blade-like slightly anteriorly oriented processes, partly resembling the pleurapophyses of Najash22,23. An isolated postcloacal vertebra referred to Diablophis gilmorei also shows a pleurapophysis similar in size to MACN-RN-1016, although more posteriorly oriented5. The neural spines of the caudals are higher than those of posterior precloacals as in Najash22,23. As mentioned above, the first postcloacal (9th vertebra) lacks haemapophyses and thus can be regarded as a pygal along with the cloacals (caudals lacking haemapophyses). The presence of at least one pygal is well documented in squamates7, including some fossil snakes, such as Wonambi barriei17,28. In Najash, the first caudals that bear pleurapophyses are not visible on the ventral side22,23.
Re-characterization of Najash rionegrina
The cloacal region of Najash rionegrina was recently re-described23. We agree with the new description (see23) which states that the vertebra that was originally identified2,22 as the first caudal with lymphapophyses is actually the only sacral vertebra, and that the two sacrals originally identified2,22 are better interpreted as presacral vertebrae bearing fused ribs. A more conservative approach23 recognized two or more vertebrae bearing lymphapophyses following the sacral, as the ventral side is not visible in that region. But, from the third caudal, the vertebrae show processes that are laterally and anteroventrally directed and are better interpreted as pleurapophyses22. Najash has also been described as having non-articulating blunt ‘haemapophyses’ like those of Anilius2,22. However, the short blunt ventral processes observed in the caudals of Najash, bearing semi-porous bone on the flat distal surface, are very similar to the condition reported herein for Dinilysia. Therefore, these processes in Najash rionegrina are re-interpreted as haemapophyses, and it is quite likely that the blunt flat distal ends of those processes would have articulated with chevrons in life (not preserved in the available specimens). The first two caudals, bearing lymphapophyses, lack any trace of haemapophyses. The third and fourth are not visible on the ventral side, and the fifth caudal already shows haemapophyses, so it is not possible to ascertain how many pygals were present.
In the CeIS, free cervical intercentra are not known in living snakes, apart from those present in the atlas-axis complex. The only vertebra that retains a certain free intercentrum in modern snakes is the atlas. The first vertebra, except in the Uropeltidae, is formed by the neural arches and an intercentrum, as the atlas centrum is incorporated into the axis forming the odontoid process7. The axis of modern snakes presents two ventral projections and the common condition is that the anterior of these two is sutured to the axis, although it can be fused (e.g., in most uropeltids; Xenopeltis), while the posterior ventral process is always fused19,22. According to Hoffstetter and Gasc7, these ventral projections represent the second and third intercentrum, and the remaining post-axial ‘hypapophyses’ are composed of fused intercentral elements. Other authors, based on embryological evidence29, consider the intercentra to be lost beyond the atlas-axis complex in modern snakes. The development of trunk vertebrae in macrostomatan snake embryos shows that the post-axis ventral projections are the result of a distal spreading-ossification of the pleurocentra29.
At the time of description of MPCA–PV 5279, no other fossil or extant snake was known to possess hypapophyses with unfused intercentra and a concave articulation surface on the hypapophysis (see11 for a list of new fossils snakes with hypapophyses and intercentra). It was noted9 that on the axis of Yurlungurr camfieldensis (see19) there is a large elliptical concavity on the distal tip of the hypapophysis. Also, the first axis intercentrum in Yurlunggur is likely sutured, or only partially fused to the axis centrum19. In the axis of Dinilysia, both of the intercentra are sutured, the second directly to the centrum and the third to the first hypapophysis. The posterior position of the hypapophyses in Dinilysia, Najash, potentially Yurlungurr, and other madtsoiids25, coupled with the presence of unfused intercentra are otherwise only observed in mosasaurs30, dolichosaurs31, pontosaurs32, and adriosaurs21. Varanoid lizards have often been compared to mosasaurs, but we have presented data here that indicates that the condition in Najash and Dinilysia is more similar to mosasaurs while varanids are more similar to modern snakes. In Varanus, the hypapophysis is not a rounded to ovate pedestal raised slightly above the body of the centrum and bearing an ovate depression at the tip. Rather, it is a long, thin, stalk-like structure, to which a single, or sometimes paired, “supposed”7 intercentrum element bearing extra epiphyseal chondrifications is attached at its distal tip.
The condition of the cervical vertebrae of Dinilysia and Najash indicates the presence in basal snakes of free unfused cervical intercentra articulating with a ventral posterior hypapophyses posterior to the axis. This implies, as the developmental evidence shows, that the intercentrum is lost beyond the atlas-axis complex in macrostomatans29, and that the ‘hypapophyses’ of macrostomatans snakes can be considered homologous to the proper hypapophyses present in fossil snakes and other non-ophidian squamates. However, developmental evidence of the condition in modern non-macrostomatan snakes is lacking, and the cervical series of Dinilysia shows a possible fusion of the intercentra to the posterior cervical hypapophyses9. While ‘apparent’ complete loss of the intercentra in later evolving snakes could have been accomplished by fusion of the intercentra to the hypapophyses, there is no evidence to support such a fusion, and thus simple loss (i.e., fate of the intercentra is not early stage fusion, but rather loss of the structure altogether) is supported by the evidence currently available. Moreover, because the first ventral element on the axis of Dinilysia, Najash, and possibly Yurlunggur19, is sutured to the centrum of the axis, without development of a hypapophyses, this first ventral element on the axis of modern snakes can be regarded as only the second intercentrum. This indicates that the first axis intercentrum becomes directly fused to the centrum in some extant taxa (although kept sutured in most extant taxa) (Fig. 1),while the remaining intercentra are likely lost and only the hypapophyses remain.
In the CaIS of most extant snakes, the postcloacal vertebrae present ventral projections of the caudal centra that are usually bifid distally and almost never contact each other. Some exceptions can be found, however, among males of some extant colubrine snakes (in which the distal tips of these processes may be more elongate and bent inwards contacting at the midline33) or in some sea-snakes (hydrophiines), where the haemapophyses can be very elongated and sometimes fused distally forming a complete arch34. On the other hand, there are instances in which only a single process is observed in the postcloacal vertebrae (e.g.: uropeltids7; most hydrophiines34). These structures have been generally termed ‘haemapophyses’, and they have been considered to represent the fusion of the caudal intercentra to the vertebral pleurocentra in snakes7,10. However, others consider that extant snakes have lost the intercentra throughout the vertebral column (with the exception of the atlas-axis complex) and the haemapophyses are actually downgrowths of the vertebral centrum and therefore homologous to the haemapophyses of lizards (e.g.11,29). The presence of unfused postcloacal intercentra (true chevrons) articulating with ventral projections of the centrum body (haemapophyses) in Dinilysia, suggests that the ‘haemapophyses’ of extant snakes are actually homologous to those of other squamates, with chevron elements being entirely lost. This is also supported by the typically paired nature of those processes in most extant snakes, since haemapophyses are also paired in all squamates (when present), whereas chevron bones usually form a single fused element.
Paired posteroventral processes similar to the haemapophyses of Dinilysia have been previously reported in other fossil snakes, namely Najash and madtsoiids, but these were interpreted in different ways. These were either described as typical derived ‘haemapophyses’ like those of extant snakes (considered as intercentra fused to caudal centra2,22,35,36,37,38), or as true haemapophyses, such as those of many non-ophidian squamates17,25,39,40,41. The new specimen reported here confirms the observations of the latter set of authors.
To date, indications of a full CaIS in terrestrial snakes were restricted to a single isolated vertebra bearing a chevron bone referred to Wonambi17, and in the marine simoliophiids Eupodophis and Haasiophis11,16. However, the condition in Wonambi was questioned by Rieppel et al.38, who interpreted the posteroventral elements on the cloacal vertebra of madtsoiids as ‘haemapophyses’ not-articulating with chevrons. Similarly, Najash has also been described as having non-articulating blunt ‘haemapophyses’2,22. However, as re-described here, the ventral processes observed in Najash present distal articulatory surfaces, likely for chevrons that are not preserved. This is supported by the presence of chevrons in the haemapophyses of Dinilysia that share the same morphological features with the type of haemapophyses found in Najash and madstoiids.
The CaIS of the marine simoliophiids Eupodophis and Haasiophis11,16 are very different from each other and also contrast with that of Dinilysia. The short, spatula-shaped chevrons of Haasiophis also articulated with posteroventral haemapophyses, but they are very short and posteriorly directed, whereas those of Eupodophis are seemingly attached directly to the posteroventral edge of the centrum11, and are much more elongate than the chevrons in Haasiophis and Dinilysia. It is noteworthy that the homologies of the caudal structures of these marine snakes, hindered in part by the peculiar morphology and preservation issues of the fossils, have also been hotly debated, being interpreted as true chevrons (e.g.11,16) or as neomorphic structures with no homologies to the CaIS (e.g.10,42).
In order to assess the evolution of the CeIS and the CaIS in snakes, we performed phylogenetic analyses derived from a recently published dataset5, with the addition of an extra character and a few changes regarding the scoring of Dinilysia patagonica and Najash rionegrina (only considering the holotype) based on the new information presented here (Supplementary Information). We analyzed this data set using both maximum parsimony and Bayesian inference, with the results from maximum parsimony (Fig. 4) being almost identical to those of the previous study5. Both analyses indicate agreement on placing Dinilysia and Najash outside crown-group snakes and in having simoliophiids further crownward as early diverging macrostomatans (Figs 4 and S1). This finding is consistent with most recent phylogenetic hypotheses (e.g.18,43).
The morphology of the CeIS and the CaIS in Dinilysia, Najash and madtsoiids indicates that the combination exhibited by some non-ophidian squamates of unfused cervical and caudal intercentra, articulating with distinct hypapophyses or haemapophyses respectively, defines the plesiomorphic condition for ophidians. The mapping of these structures onto our re-analyses of early snake relationships further supports the hypothesis that in the CaIS, the haemapophyses of extant snakes are homologous to those of other fossil snakes, and to those of fossil and extant lizards. However, the chevron bones appear to be lost in modern snakes, but not in the Mesozoic fossil snakes highlighted here and in Palci et al.11. In the CeIS the hypapophysis of modern snakes is the homolog of the non-ophidian squamate hypapophyses, and unless a free intercentrum is present that is then observed to fuse to the hypapophysis (by undisputed morphological or developmental data), it cannot be concluded that an intercentrum is actually present beyond the atlas and axis vertebral intercentra. These results agree with the proposed loss of post atlas-axis intercentra (cervical and caudal) in modern snakes29, but not all snakes as we made clear from an important number of fossil snakes.
All the fossil snakes that present unfused intercentra (either directly observed or inferred) in both the caudal region and post-atlas-axis anterior trunk region (Dinilysia, Najash, madtsoiid snakes, and Haasiophis8,9,11), lie outside crown-Macrostomata and so the presence of intercentra does not contradict embryological evidence29. Strict adherence to the retrieved (Figs 4, S1) and commonly held (e.g.18,43, but see11 for the alternative possibility of a more basal position for simoliophiids) phylogenetic scheme would hold that the fossil evidence indicates that post-axial intercentra were lost prior to the evolution of crown-group Serpentes, but intercentra were reacquired (a reversal) in simoliophiids (Figs S5, S6). A strict reading would again be supported by the fact that scolecophidians have anterior hypapophyses, but a complete absence of caudal intercentra can be inferred since they have significantly shortened tails (<20 vertebrae) and they lack haemapophyses altogether7,26; basal alethinophidians such as Anilius have cervical hypapophyses and caudal haemapophyses without free intercentra, and uropeltids have both cervical and caudal hypapophyses.
However, we recommend a more cautious approach to such strict readings of phylogenies, particularly when ancient fossil taxa are nesting well within the crown (e.g., simoliophiids in this case). In the case of our phylogeny (Fig. 4), uropeltids, scolecophidians and anilioids are basal to simoliophiids, which are known from ~95 million year old fossil remains, and the clade they are a part of has no modern representatives. In this and other phylogenies, uropeltids, scolecophidians and anilioids are members of clades that are basal to simoliophiids (e.g.5,18,43); but it must be remembered, these living snake species are not early evolving snake species, but rather extant (and thus recently diverging) members of their respective early evolving clades. They are 95 million years younger than simolophiids and if their phylogenetic position is accurate, then their 95 million year old clade members, currently unrepresented by fossil remains, could show one of two conditions, either the possession of intercentra in both the cervical and caudal region, as do simoliophiids, or, they might show a condition supporting the strict reading of the phylogeny as noted above.
We would thus suggest that a more relaxed reading of Fig. 4 is possible. Even if it is not for the moment, empirical, the “relaxed reading” of Fig. 4 becomes predictive and could thus be supported by either new fossil material (e.g. fossils of early anilioids or uropeltids), or a revised phylogenetic hypothesis (such as recovering simoliophiids at a more basal position). Instead of single loss of a feature, with reacquisition or re-evolution42 as the primary explanations for such phylogenetic patterns of morphological change, we consider as a valuable prediction, if not alternative, that there were multiple independent events of loss of intercentra in all these non-macrostomatan groups and in derived macrostomatans. In this model, simoliophiids are the best-known fossil group at the base of macrostomatans and demonstrate the plesiomorphic condition for that clade circa 95 million years ago. This is consistent with a similar scenario proposed for the presence of well-developed hindlimbs in these snakes.
MACN-RN-1016 (Museo Argentino de Ciencias Naturales “Bernandino Rivadavia”, Río Negro Collections, Buenos Aires, Argentina), collected in 1994–95 by a team headed by José F. Bonaparte, in the Tripailao Farm Locality, located near Paso Córdova, Río Negro province, Argentina8; MACN-PV-N 116 (Museo Argentino de Ciencias Naturales “Bernandino Rivadavia”, Paleontología de Vertebrados-Neuquén Collections, Buenos Aires, Argentina), that comes from the vicinity of the Universidad Nacional del Comahue, in Neuquén City, Neuquén Province, Argentina44; MPCA-PV 527 (Museo Provincial Carlos Ameghino, Paleontología de Vertebrados Collections, Río Negro). Najash rionegrina: MPCA-PV 391.
A maximum parsimony analysis was conducted in TNT v. 1.5-beta45 using 100 tree replicates obtained by random addition sequence (RAS), and searching for new tree topologies with tree bisection and reconnection (TBR), saving 100 trees per replication. A single most parsimonious tree (MPT) was obtained with 510 steps.
Bayesian inference analysis was conducted using Mr. Bayes v. 3.2.646,47 using the MkV model for morphological data47 and with rate variation across characters sampled from a gamma distribution. Each analysis was performed with two independent runs of 1 × 107 generations each, with eight chains per run and four swaps attempted per swapping generation. The relative burn-in fraction was set to 50% and the chains were sampled every 1000 generations. The temperature parameter for the four chains in each independent run was set to 0.04. Convergence of independent runs was assessed through the average standard deviation of split frequencies (ASDSF < 0.01) and potential scale reduction factors (PSRF ≈ 1 for all parameters) calculated at the end of the Bayesian runs. We used Tracer v. 1.648 software to determine whether the runs reached stationary phase and to ensure that the effective sample size (ESS) for each parameter was greater than 200.
Caldwell, M. W. & Lee, M. S. Y. A snake with legs from the marine Cretaceous of the Middle East. Nature 386, 705–709 (1997).
Apesteguía, S. & Zaher, H. A Cretaceous terrestrial snake with robust hindlimbs and a sacrum. Nature 440, 1037–1040 (2006).
Palci, A. & Caldwell, M. W. The Upper Cretaceous snake Dinilysia patagonica Smith-Woodward, 1901, and the Crista Circumfenestralis of snakes. J. Morphol. 00, 1–14 (2014).
Palci, A. & Caldwell, M. W. Primary homologies of the circumorbital bones of snakes. J. Morphol. 274, 973–986 (2013).
Caldwell, M. W., Nydam, R. L., Palci, A. & Apesteguía, S. The oldest known snakes from the Middle Jurassic-Lower Cretaceous provide insight on snake evolution. Nat. commun. 6(5996), 1–11 (2015).
Longrich, N. R., Bhullar, B.-A. S. & Gauthier, J. A. A transitional snake from the Late Cretaceous period of North America. Nature 488, 205–208 (2012).
Hoffstetter, R. & Gasc, J. P. Vertebrae and ribs of modern reptiles in Biology of the Reptilia, Volume 1 (eds. Gans, C., Bellairs, A. d’. A., & Parsons, T.), 201–310 (Academic Press 1969).
Caldwell, M. W. & Albino, A. M. Palaeonviroment and palaeoecology of three Cretaceous snakes: Pachyophis, Pachyrhachis, and Dinilysia. Acta Palaeontol. Pol. 46(2), 203–218 (2001).
Caldwell, M. W. & Calvo, J. Details of a new skull and articulated cervical column of Dinilysia patagonica Woodward, 1901. J. Vertebr. Paleontol. 28(2), 349–362 (2008).
Rieppel, O. & Head, J. J. New specimens of the fossil snake genus Eupodophis Rage and Escuillié, from Cenomanian (Late Cretaceous) of Lebanon. Mem. Soc. Ital. Sci. Nat. Mus. Civ, Star. Nat. Milano 32, 1–26 (2004).
Palci, A., Caldwell, M. W. & Nydam, R. L. Reevaluation of the anatomy of the Cenomanian (Upper Cretaceous) hind-limbed marine fossil snakes Pachyrhachis, Eupodophis, and Haasiophis. J.Vertebr. Paleontol. 33(6), 1328–1342 (2013).
Caldwell, M. W. & Albino, A. M. Exceptionally preserved skeletons of the Cretaceous Dinilysia patagonica Woodward, 1901. J. Vertebr. Paleontol. 22(4), 861–866 (2002).
Tsuihiji, T., Kearney, M. & Rieppel, O. Finding the neck-trunk boundary in snakes: Anteroposterior dissociation of myological characteristics in snakes and its implications for their neck and trunk body regionalization. J. Morphol. 273(9), 992–1009 (2012).
Cohn, M. & Tickle, C. Developmental basis of limblessness and axial patterning in snakes. Nature 399, 474–470 (1999).
Caldwell, M. W. “Without a leg to stand on”: on the evolution and development of axial elongation and limblessness in tetrapods. Can. J. Earth Sci. 40, 573–588 (2003).
Rage, J. C. & Escuillié, F. Un nouveau serpent bipéde du Cénomanien (Cretacé). Implications phylétiques. C. R. Acad. Sci. Paris Earth Sci. 330, 513–520 (2000).
Scanlon, J. D. & Lee, M. S. Y. The Pleistocene serpent Wonambi and the early evolution of snakes. Nature 403, 416–420 (2000).
Zaher, H. & Scanferla, C. A. The skull of the Upper Cretaceous snake Dinilysia patagonica Smith-Woodward, 1901, and its phylogenetic position revisited. Zool. J. Linn. Soc. 164, 194–238 (2012).
Scanlon, J. D. First known axis vertebra of a madtsoiid snake (Yurlunggur camfieldensis) and remarks on the neck of snakes. Beagle Rec. N. Territory Mus. Arts. Sci. 20, 207–215 (2004).
Tsuijihi, T., Kearney, M. & Rieppel, O. First Report of a Pectoral Girdle Muscle in Snakes, with Comments on the Snake Cervico-dorsal Boundary. Copeia 2, 206–215 (2006).
Palci, A. & Caldwell, M. W. Vestigial forelimbs and axial elongation in a 95 million-year-old non-snake squamate. J. Vertebr. Paleontol. 27, 1–7 (2007).
Zaher, H., Apesteguía, S. & Scanferla, C. A. The anatomy of the Upper Cretaceous snake Najash rionegrina Apesteguía and Zaher, 2006, and the evolution of limblessness in snakes. Zool. J. Linn. Soc. 156, 801–826 (2009).
Palci, A., Caldwell, M. W. & Albino, A. M. Emended diagnosis and phylogenetic relationships of the upper Cretaceous fossil snake Najash rionegrina Apesteguía and Zaher, 2006. J. Vertebr. Paleontol. 33(1), 131–140 (2013).
Rage, J. C. & Albino, A. M. Dinilysia patagonica (Reptilia, Serpentes): matériel vertébral additionnel du Crétacé supérieur d’Argentine. Etude complémentaire des vertèbres, variations intraspécifiques et intracolumnaires. Neues Jahrb. Geol. P-M. 1989, 443–447 (1989).
Gómez, R. O. & Báez, A. M. Intracolumnar variation and morphological remarks on madtsoiid snakes (Squamata, Serpentes) from the Upper Cretaceous of Patagonia. Ameghiniana 42(4), Suplemento resúmenes 30R–31R (2005).
List, J. C. Comparative osteology of the snake families Typhlopidae and Leptotyphlopidae. Illinois Biological Monographs 36, 1–112 (1966).
Romer, A. S. Osteology of the Reptiles. (University of Chicago Press 1956).
Scanlon, J. D. Cranial morphology of the Plio-Pleistocene giant madstoiid snake Wonambi naracoortensis. Acta Paleontol. Pol. 50(1), 139–180 (2005).
Gauthier, J. A., Kearney, M., Maisano, J. A., Rieppel, O. & Behlke, A. D. B. Assembling the Squamate Tree of Life: Perspectives from the Phenotype and the Fossil Record. B. Peabody Mus. Nat. Hi. 53(1), 3–308 (2012).
Russel, D. A. Systematics and morphology of American mosasaurs. B. Peabody Mus. Nat. Hi 23, 1–241 (1967).
Caldwell, M. W. On the aquatic squamate dolichosaurus Longicollis owen, 1850 (Cenomanian, Upper Cretaceous), and the evolution of elongate necks in squamates. J. Vertebr. Paleontol. 20(4), 720–735 (2000).
Caldwell, M. W. A new species of Pontosaurus (Squamata, Pythonomorpha) from the Upper Cretaceous of Lebanon and a phylogenetic analysis of Pythonomorpha. Mem. Soc. Ital. Sci. Nat. Mus. Civ, Star. Nat. Milano 34, 1–42 (2006).
Keiser, E. D. Jr. Sexual dimorphism and ontogenetic variation in the haemapophyses of ophidian postcloacal vertebrae. Herpetologica 26, 331–334 (1970).
McDowell, S. B. Notes on the Australian sea-snake Ephalophis greyi M. Smith (Serpentes: Elapidae, Hydrophiinae) and the origin and classification of sea-snakes. Zool J. Linn. Soc. 48(3), 333–349 (1969).
Scanlon, J. D. Madtsoiid snakes from the Eocene Tingamarra fauna of Eastern Queensland. Darmst. Beitr. Naturgeschichte 3, 3–8 (1993).
Albino, A. M. Una nueva serpiente (Reptilia) en el Cretácico Superior de Patagonia, Argentina. Pesquisas 21, 58–63 (1994).
Rage, J. C. Fossil snakes from the Paleocene of São José de Itaboraí, Brazil. Part I. Madtsoiidae, Aniliidae. Palaeovertebrata 27(3-4), 109–144 (1998).
Rieppel, O., Kluge, A. G. & Zaher, H. Testing the phylogenetic relationships of the Pleistocene snake Wonambi naracoortensis Smith. J. Vertebr. Paleontol. 22(4), 812–829 (2002).
Scanlon, J. D. Australia’s oldest known snakes: Patagoniophis, Alamitophis and Cf. Madstoia (Squamata: Madtsoiidae) from the Eocene of Queensland. Mem. Queensl. Mus. 51(1), 215–235 (2005).
Laduke, T. C., Krause, D. W., Scanlon, J. D. & Kley, N. J. A Late Cretaceous (Maastrichtian) snake assemblage from the Maevarano Formation, Mahajanga Basin, Madagascar. J. Vertebr. Paleontol. 30, 109–138 (2010).
Vasile, S., Csiki-Sava, Z. & Venczel, M. A new madtsoiid snake from the Upper Cretaceous of the Hateg Basin, WesternRomania. J. Vertebr. Paleontol. 33(5), 1100–1119 (2013).
Rieppel, O., Zaher, H., Tchernov, E. & Polcyn, M. J. The anatomy and relationships of Haasiophis terrasanctus, a fossil snake with well-developed hind limbs from the mid-Cretaceous of the Middle East. J. Paleont. 77(3), 536–558 (2003).
Hsiang, A. Y. et al. The origin of snakes: revealing the ecology, behavior, and evolutionary history of early snakes using genomics, phenomics, and the fossil record. BMC Evol. Biol. 15(87), 1–22 (2015).
Albino, A. M. Lepidosauromorpha in Patagonian Mesozoic Reptiles (eds. Gasparini, Z., Salgado, L. & Coria, R. A.), 87–115 (Indiana University Press 2007).
Goloboff, P., Farris, J. & Nixon, K. TNT, a free program for phylogenetic analysis. Cladistics 24, 774–786 (2008).
Ronquist, F. et al. MrBayes 3.2: Efficient Bayesian Phylogenetic Inference and Model Choice Across a Large Model Space. Syst. Biol. 61(3), 539–542 (2012).
Lewis, P. O. A Likelihood Approach to Estimating Phylogeny from Discrete Morphological Character Data. Syst. Biol. 50(1), 913–925 (2001).
Rambaut, A., Suchard, M. A., Xie, D. & Drummond, A. J. Tracer v1.6. Available from http://beast.bio.ed.ac.uk/Tracer (2014).
Conrad, J. L. Postcranial Skeleton of Shinisaurus crocodilurus (Squamata: Anguimorpha). J. Morphol. 267, 759–775 (2006).
We would like to thanks Stella Alvarez and Martín Ezcurra (MACN), as well as Carlos Muñoz and Ignacio Cerda (MPCA) for access to collections. We thank CONICET for the PhD scholarship granted to FFG, and the Willy Henning society for the free availability of the software T.N.T. Funding to MWC was provided by an NSERC Discovery Grant (#234538).
The authors declare no competing interests.
Publisher’s note: Springer Nature remains neutral with regard to jurisdictional claims in published maps and institutional affiliations.
About this article
Cite this article
Garberoglio, F.F., Gómez, R.O., Simões, T.R. et al. The evolution of the axial skeleton intercentrum system in snakes revealed by new data from the Cretaceous snakes Dinilysia and Najash. Sci Rep 9, 1276 (2019). https://doi.org/10.1038/s41598-018-36979-9
Discovery of the oldest South American fossil lizard illustrates the cosmopolitanism of early South American squamates
Communications Biology (2020)
A new Late Cretaceous snake from Patagonia: Phylogeny and trends in body size evolution of madtsoiid snakes
Comptes Rendus Palevol (2019)
New skulls and skeletons of the Cretaceous legged snake Najash, and the evolution of the modern snake body plan
Science Advances (2019)