- Research Article
- Open Access
A forged ‘chimera’ including the second specimen of the protostegid sea turtle Santanachelys gaffneyi and shell parts of the pleurodire Araripemys from the Lower Cretaceous Santana Group of Brazil
Swiss Journal of Palaeontology volume 142, Article number: 6 (2023)
Fossils of Cretaceous sea turtles adapted to an open marine lifestyle remain rare finds to date. Furthermore, the relationships between extant sea turtles, chelonioids, and other Mesozoic marine turtles are still contested, with one key species being Santanachelys gaffneyi Hirayama, 1998, long considered the earliest true sea turtle. The species is an Early Cretaceous member of Protostegidae, a controversial clade either placed within or closely related to Chelonioidea or, alternatively, along the stem lineage of hidden-neck turtles (Cryptodira) and representing an independent open marine radiation. Santanachelys gaffneyi is one of the most completely preserved early protostegids and is therefore critical for establishing the global phylogenetic position of the group. However, the single known specimen of this taxon is yet to be described in detail. Here we describe a second specimen of Santanachelys gaffneyi from its type horizon, the Romualdo Formation (late Aptian) of the Santana Group of the Araripe basin, NE Brazil. The skeletal elements preserved include the posterior part of the skull, neck vertebrae, shoulder girdle, anterior-most and left/central part of the carapace with few peripherals, and plastron lacking most of the hyoplastra. The remaining part of the carapace was apparently completed by fossil dealers using an anterior part of the pleurodiran Araripemydidae, tentatively identified as a shell portion of cf. Araripemys barretoi, a more common Santana fossil turtle, among other indeterminate turtle shell fragments. The purpose of this paper is to report the repatriation of the specimen to Brazil and to provide a preliminary description.
The Romualdo Formation and the underlying Ipubi and Crato formations of the Lower Cretaceous Santana Group, have so far yielded five turtle species in addition to two indeterminate pelomedusoid taxa (Oliveira et al., 2011; Romano et al., 2013). Of the five described species, all but Araripemys barretoi Price, 1973, which is known from more than 30 post-hatching specimens from the Romualdo and Crato formations (Carvalho et al., 2019; Limaverde et al., 2020; Meylan, 1996; Meylan and Gaffney, 1991; Oliveira and Kellner, 2005, 2017; Price, 1973; Romano et al., 2013), are considered to be rather rare faunal components so far only reported from the Romualdo Formation: the bothremydid pleurodiran Cearachelys placidoi is represented by seven specimens (Carvalho et al., 2019; Gaffney, 2001; Gaffney et al., 2006; Oliveira, 2007; Sena et al., 2021) and the euraxemydid pleurodiran Euraxemys essweini Gaffney, Tong and Meylan, 2006 by two specimens (Gaffney et al., 2006; Oliveira and Kellner, 2007; Romano et al., 2013), whereas the podocnemidoid pleurodiran Brasilemys josai Lapparent de Broin, 2000 and the protostegid pan-cryptodiran Santanachelys gaffneyi Hirayama, 1998 are represented so far only by their holotype specimens (Gaffney et al., 2006, 2011; Hirayama, 1998; Lapparent de Broin, 2000; Oliveira and Kellner, 2007; Oliveira and Romano, 2007).
Given its age and complete preservation, Santanachelys gaffneyi is a key taxon for understanding the evolution of adaptations to open marine lifestyle in sea turtles, but whether it is closely related to extant sea turtles (Chelonioidea) or represents a convergent marine radiation remains unclear. When first described, Santanachelys gaffneyi was found as the earliest diverging member of the extinct Protostegidae and formed a clade with leatherback sea turtles, Dermochelyidae (Hirayama, 1998). Kear and Lee (2006) reproduced these findings while sampling additional species, whereas Danilov and Parham (2006) and Joyce (2007) recovered Santanachelys gaffneyi with affinities to Mesozoic nearshore marine stem-cryptodirans such as Solnhofia parsonsi or other Thalassochelydia (see Anquetin et al., 2017 for a review of that clade), a signal that was also picked up in some subsequent large-scale analyses (e.g., Anquetin, 2012; Anquetin et al., 2015). Others placed Santanachelys in an even more stem-ward position, outside crown turtles (e.g., Sterli, 2010; Sterli and de La Fuente, 2011), but such a placement was not corroborated by more recent analyses. With the description of Desmatochelys padillai Cadena and Parham, 2015 from the Lower Cretaceous (upper Barremian–lower Aptian) of Colombia, Santanachelys gaffneyi has been no longer considered the stratigraphically oldest known marine turtle. In that study, the traditional placement of Santanachelys sensu Hirayama (1998) was recovered, but at the same time, low statistical support at the base of Pan-Chelonioidea and conflicting signals of spatiotemporal patterns and anatomy were used to question this topology (Cadena and Parham, 2015). Raselli (2018) recovered a monophyletic Protostegidae (with Santanachelys as sister to all remaining sampled protostegids) as sister group to extant Cheloniidae and Dermochelys (+ Mesodermochelys). The analysis of Evers and Benson (2019) again recovered protostegids in their traditional placement, but Santanachelys was found more deeply nested within the group. The analyses of Rabi and Kear (2016), Raselli (2018), Evers et al. (2019) and Gentry et al. (2019) corroborated the nested position within protostegids in a clade including Notochelone from Australia and Rhinochelys from Europe and, again, found Protostegidae closely related to crown-sea turtles, but representing their stem lineage. Santanachelys gaffneyi is hypothesised to be fully adapted to marine (open water) environment (Gentry et al., 2019), but its relation to crown-group sea turtles is yet to be rigorously established (Cadena and Parham, 2015).
Our understanding of the osteology of S. gaffneyi is based on the preliminary description of the holotype and single known specimen (Hirayama, 1998). Here we report a second specimen from the type horizon, a partial skeleton including an incomplete shell, posterior part of the skull, neck, and shoulder girdle elements. This fossil will contribute important data to a separate project on the detailed description of S. gaffneyi using high-resolution CT data. The goal of the present study is to provide a preliminary description, with focus on the shell elements, of the new specimen and document its repatriation to Brazil.
The Romualdo Formation, formerly known as the Romualdo Member of the Santana Formation (now considered Santana Group) is a well-known Konservat Lagerstätte in the Araripe Basin, northeastern Brazil, which is exceptionally rich in fossils (Maisey, 1991). The depositional sequence of the formation in the upper part of the Santana Group is mostly that of a fine-grained siliciclastic to carbonate-dominated series deposited during two transgressive–regressive cycles representing a marine post-rift incursion into the Araripe basin (Assine et al., 2014; Custódio et al., 2017; Fürsich et al., 2019). According to the low diversity benthic megafaunas preserved, the Romualdo Formation represents a high-stress environment (Fürsich et al., 2019). Considering only the vertebrate fossil record herein, several lineages such as crocodylomorphs, dinosaurs, and turtles are represented in the Santana Group, but it is arguably most famous for its exquisitely preserved and abundant bony fish and pterosaur faunas (Kellner et al., 2013; Martill, 2007; Sayão et al., 2020; Vila Nova et al., 2011; Wellnhofer, 1985).
Material and methods
UFRPE 5061 is a forged concretion derived from the Romualdo Formation from Chapada do Araripe basin. As is often the case with outstanding lagerstätten-type localities, a market of dealing with fossils develops, with monetary, aesthetic or academic (vs. religious/shamanistic) reasons being the main drivers behind them (Ruffell et al., 2012). Local academics, national and international lawmakers, the international scientific community, institutes, and museums, as well as private and professional fossil collectors and dealers, bring forth their arguments, often conflicting among the involved parties, concerning the legal and illegal trade of fossils (Liston, 2014), even though the social and economic impacts of such trade have become more evident (Raja et al., 2021). Without going into detail, we recognise that this phenomenon is neither new nor localised (see for example Parham, 2005 on forged marine turtle remains from Morocco), thus, given the outstanding quality of many Santana fossils (Maisey, 1991), it is not surprising that a lucrative market for dealing in either genuine or forged fossils flourishes there as well (Martill, 1994). Despite the strict protection laws that have been emplaced in Brazil since 1942, which basically render all fossils—including the Santana fossils—as state property (see discussion in Cisneros et al., 2022), an abundance of specimens has been illegally exported to other countries worldwide over the last decades, mostly bony fish, as they are among the most common finds in the strata (Martill, 1994). Faking rarer specimens such as pterosaurs or dinosaurs might drastically increase their monetary value and often an array of methods and techniques are needed to tell genuine fossils and the frauds apart (Mateus et al., 2008; Veldmeijer, 2006). In general, the forged concretions lack stratigraphic data that would allow recognising spatial and temporal fluctuations of the vertebrate faunal composition (Vila Nova et al., 2011).
Via dubious trade ways, the specimen here described found its way to Europe and finally ended up in the collections of the Palaeontological Institute in Zurich, Switzerland, more than three decades ago (previously catalogued under PIMUZ A/III 619, now a cast of the original stored at PIMUZ). The concretion containing the turtle remains was not easily identified as having been forged at first, because of its weathered appearance and damaged external bone surface and thus it remained in the PIMUZ collection simply as a ‘Testudines indet.’ specimen.
The reddish colour of the ventral side of the concretion turned out to be only a superficial layer of soft, burned-in dye covering a dense oval-shaped sedimentary matrix block. The specimen was first CT scanned in 2014 with a high-resolution peripheral quantitative CT (HR-pQCT, XtremeCT II, SCANCO Medical AG, Brüttisellen, Switzerland; see Additional video file) which yielded mixed results with low contrast and artefacts, mainly due to the dense sedimentary matrix. Especially the artefacts and low contrast prevented further segmentation of the bones. Scanning was performed at 68 kV tube voltage, 1470 μA tube current, 1.05 s integration time, and images were reconstructed using a 60.7μm isotropic voxel size. This scan, however, and initial preparation from the ventral side subsequently revealed that about the lower half of the specimen consisted of a very dense and coarse (artificial?) sediment block devoid of any bones (Fig. 1). This oval-shaped block was glued to the upper part of the specimen that contained the bones to give the impression of a concretion. Further preparation revealed that the whole concretion was thus assembled using synthetic car body filler of light grey colour and that at least two turtle specimens were included into the forgery. A similar case of forged turtle concretion was previously reported for specimen MN 6743-V of Araripemys (Oliveira, 2007) and it is, unfortunately, also a common practice among Araripe “peixeiros” (fishmongers; free translation from Portuguese).
The original sediment matrix containing most of the bones in UFRPE 5061 consists of a cream-coloured carbonate (forming the diagenetic concretion in which the fossils are preserved) that locally turns into coarser-grained carbonate matrix including scattered tiny bones and a partial articulated vertebral column of a tiny bony fish. Due to the continuity of this original matrix, the connection between the skull, neck and shell remains identified as Santanachelys could be confirmed. The remaining part of it was filled by shell bone pieces that were added haphazardly, often inside out, to give the impression of a more complete specimen. Due to the problematic nature of this Brazilian patrimonial specimen, it is now repatriated to the palaeontological collection of the Universidade Federal Rural de Pernambuco (UFRPE 5061), Brazil.
DGM-DNPM, Divisão de Geologia e Mineralogia, Departamento Nacional de Produção Mineral, Rio de Janeiro, Brazil, currently, National Mining Agency (ANM). THUg, Teikyo Heisei University, Ichihara, Chiba, Japan. PIMUZ, Department of Palaeontology (formerly Palaeontological Institute and Museum), University of Zurich, Switzerland. UFRPE, Department of Biology, Universidade Federal Rural de Pernambuco, Recife, Brazil.
Pan-Cryptodira Joyce et al., 2020 (Joyce et al., 2020a)
Protostegidae Cope, 1872 [(Joyce et al., 2021)]
Santanachelys gaffneyi Hirayama, 1998
THUg1386, a nearly complete skeleton (Hirayama, 1998) [The specimen is currently housed in Fossil and Extant Turtle Collections in Waseda University, Tokyo, Japan].
UFRPE 5061 (Fig. 2; Table 1), a forged concretion with a partial skeleton preserving the posterior part of the skull, neck, shoulder girdle, the nuchal, left and central parts of the carapace with few peripherals, and the plastron lacking most of the hyoplastra. These bones are identified as belonging to Santanachelys gaffneyi based on skull proportions, anteroposteriorly elongate oval shape of the carapace with large fontanelles between costals and peripherals, a faint radiating pattern and scute imprints on the dorsal surface of the costals, rectangular neurals, a plastron whose posterior part is identical in shape and suture pattern with the holotype specimen and framing a large central plastral fontanelle, elongate coracoids, and overall similar shell size compared to the holotype (although the latter alone is not considered a strong argument). UFRPE 5061 comes from Chapada do Araripe, Araripe basin, northeast of Brazil, but similar to the holotype specimen, no additional data about the finding situation and stratigraphic horizon are available for UFRPE 5061. Due to this lack of information, the age of the fossil is tentatively considered to be late Aptian (Arai and Assine, 2020; Fürsich et al., 2019; Melo et al., 2020).
Description of UFRPE 5061
The majority of the preserved bones in the forged concretion could be identified as a partial skeleton of Santanachelys gaffneyi, including skull remains, appendicular and axial bones and shell parts. On the dorsal surface of the concretion, the posterior part of the skull is visible in dorsal view, followed posteriorly by a few cervicals that remain largely hidden within the matrix. These are followed by the carapace in dorsal view in which the nuchal, the right peripheral 1, the left peripherals 1 and 2, the lateral parts of left costal 1 partially overlapped by the lateral part of costal 2, the posteromedial part of costal 2, left costals 3–8, neurals 2–6, and the anterior left corner of a suprapygal bone could be identified. Much of the bone surface in the anterior part of the slab containing the posterior portion of costal 2 to costal 4 is strongly damaged so that sutures between bones are difficult to trace. There are fontanelles visible between the left costal 1 and peripheral 2, and between each of the left costals 3–8. On the ventral side of the concretion a small part of the skull, some cervicals mostly embedded in matrix, the two epiplastra, the partially preserved entoplastron, the posterior sutural areas of the hyoplastra, as well as mostly complete hypo- and xiphiplastra are preserved. The hyo- and hypoplastra frame a large central fontanelle of rectangular shape. The hypo- and xiphiplastra show a slight striation on the otherwise smooth bone surface that radiates out from the growth centre of each plate. We here focus on the diagnostic shell of the new specimen; other skeletal elements will be described and discussed elsewhere.
Skull, vertebrae, and shoulder girdle bones
The posterior portion of the skull is preserved and some bones such as the supraoccipital, opisthotics, and squamosals can be identified. Three cervical vertebrae are partially exposed, as are the very prominent elongated coracoids of the shoulder region. Parts of the scapula and additional dorsal centra are partly visible as well in ventral view, but because a full description of this specimen is currently in progress elsewhere, we refrain from adding anatomical details here.
The nuchal is completely preserved and contacts peripherals 1 and 2. This is in contrast to the holotype THUg1386, in which peripheral 1 extends slightly more caudally to the level of the posterior margin of the nuchal, and therefore hindering a contact with peripheral 2 (Hirayama, 1998; pers. obs. MR, TMS, and GSF). Posteriorly the margin of the nuchal is almost straight and medially the suture zone with the first neural is visible. Scute sulci reveal a rectangular wide cervical and adjacent marginal 1 and 2, as well as the vertebral 1.
The left peripherals 1 and 2 are completely preserved and there is a small remnant of peripheral 3 still sutured to peripheral 2. Peripheral 1 seems to be reduced in size and peripheral 2 more enlarged and massive compared to THUg1386. On the right side, only peripheral 1 is preserved. All peripherals show a slightly bowed indentation where the scute sulci meet the lateral shell margin.
The preserved lateral portion of costal 1 carries a long and tapering free rib end extending slightly anterolaterally. Most of its bone surface is abraded. The posterior margin of the element is largely overlapped by the anterior margin of the lateral portion of costal 2, with its free rib part extending anterolaterally. The separated posteromedial part of costal 2 is still sutured to neural 2 medially and costal 3 posteriorly. Costal 3 is mostly complete with a rectangular medial part, just lacking the tip of the tapering free rib end facing straight laterally (the distal part of the rib is broken off but fits well, unlike other fragments that have been added as supposed distal rib ends of costals 2, and 4–6). The bone surface is undamaged in the lateral part, preserving an anteroposteriorly extending sulcus of the vertebral 2. Costal 4 is of similar rectangular shape as costal 3 but its bone surface is less damaged, preserving a triple junction of sulci of vertebrals 2 and 3 close to the anterior margin of the free rib portion of the costal. The sulcus is traceable over the bone surface as a shallow groove and the free rib part is angled slightly posterolaterally. Costal 5 is narrower than costals 3 and 4, but still rectangular in shape with straight anterior, medial and posterior margins. The free rib is largely preserved and angled posterolaterally. The bone surface is almost undamaged except a small medial portion, preserving again a triple junction of vertebrals 3 and 4 situated more of the centre of the bone. Costal 6 is even narrower anteroposteriorly with straight anterior and medial margins, but a concave posterior one. The bone surface is undamaged, revealing the slightly bent lateral sulcus of vertebral 4. Costal 7 differs from the previous costals in almost having a crescent shape formed by a convex anterior margin, a straight to slightly undulating medial margin (where it does not articulate with a neural), a short straight posteromedial margin (i.e. the suture with the suprapygal), followed laterally by a strongly concave margin (i.e. the suture with costal 8). The small free rib end is only preserved proximally, extending strongly posterolaterally. The bone surface is undamaged revealing a triple junction between vertebrals 4 and 5. Costal 8 is much shorter and of rectangular shape, thus it is excluded from reaching the midline by the costal 7, but it has an anteromedial–posterolateral extending suture with the tiny preserved portion of the suprapygal. Its smooth bone surface lacks sulci.
The neural series is continuous between neurals 2–6. Even though the lateral margins of the anterior neurals 2–4 cannot be traced completely with confidence, their outlines can at least still partially be reconstructed. Neural 1 is missing and the carapace appears to be lacking neurals posterior to number 6 in dorsal view, with costals 7 meeting in the midline in a straight to slightly undulating suture. While all neurals appear to be of elongate and narrow rectangular shape, only neurals 5 and 6 have an undamaged bone surface that allows precise shape identification. Neural 5 is hexagonal, with short sides anteriorly, whereas neural 6 is octagonal. A seventh neural is not exposed dorsally, but is rudimentarily developed beneath the costals 7 (Fig. 3).
The epiplastra are slightly crescent-shaped bones with gently curved convex anterior and concave posterior margins. The elements have a straight midline margin and the lateral margin is slightly tapering, although the bones are eroded here.
The entoplastron is T-shaped with a bowed convex anterior margin that articulates with the epiplastra, a medial posterior process of which only the proximal portion is preserved, and concave posterolateral margins. Given the separation of epiplastra and entoplastron from one another and the presence of smooth margins, the elements are interpreted as having been separate and not fused in life in UFRPE 5061.
Of the hyoplastra, only the posterior margins are preserved including the contact with the hypoplastra. Because of the missing parts of the hyoplastra, endoskeletal bones from the shoulder region (coracoids and scapulae) and at least three cervical vertebrae are exposed.
The hypoplastra have a complex shape that results from the anterior sutured margin with the hypoplastra, an anteromedial margin framing the posterior border of the central fontanelle, a strongly interdigitating medial suture, and a lateral margin which is strongly concave anterolaterally, more convex laterally (but broken in both bones) and straight to slightly concave posterolaterally. The posterior border forms a deep interdigitating socket for a xiphiplastral prong.
The xiphiplastra meet one another in a strongly interdigitating midline suture. Their anterior margin is zigzag shaped as it forms prominent tapering prongs that articulate with the posterior margin of the hypoplastra. The lateral and posterior margins are convex and smoothly curved.
Pleurodira Cope, 1865 [(Joyce et al., 2020b)]
Araripemydidae Price, 1973
cf. Araripemys barretoi Price, 1973
DGM-DNPM 756-R, a posterior portion of a shell and proximal hindlimb bones, found in the Romualdo Formation. The specimen is housed at the Agência Nacional de Mineração (National Mining Agency), previously called Departamento Nacional de Produção Mineral (DNPM), Rio de Janeiro, RJ, Brazil.
UFRPE 5061, a forged concretion with a partial shell preserving the left costals 1–3 and peripherals 3–7. As for the rest of the concretion, no additional data are available. Identification is mainly based on the suture patterning of the costals and dorsal bone surface sculpturing consisting of fine pitting (Meylan, 1996, see description below).
Description of UFRPE 5061
The left anterior part of a carapace of an araripemydid, tentatively identified as belonging to cf. Araripemys barretoi, has been used to complete the forged concretion, with the anterior tip facing now posteriorly in relation to the Santanachelys gaffneyi remains. The distal portions of the left costals 1–3 and peripherals 2–5 are still in contact. Costal 1 and 2 also show the distal margins including the free rib ends as the costals and preserved peripherals are separated by fontanelles. The tip of the rib of costal 1 meets the suture between peripheral 3 and 4 as in Araripemys barretoi (see Meylan and Gaffney, 1991) but interestingly, the rib end of costal 2 is centrally situated, giving the costal a symmetrical straight shape rib being situated in the middle. Similar costal 2 shapes are also reported for Laganemys tenerensis (Sereno and ElShafie, 2013) and Taquetochelys decorata (Pérez-García, 2019), whereas in the well preserved AMNH 22550 of Araripemys barretoi, the rib lies acentrically in the anterior portion in the costal plate creating an asymmetrical costal shape in which the rib end converges slightly towards the suture with costal 1 (see also Meylan, 1996: fig. 3). In UFRPE 5061, the rib end of costal 2 further articulates with a pit centrally situated on peripheral 4; such an articulation was also shown in Meylan’s (1996) ventral view composite interpretative sketch of the carapace of AMNH 22550 (which differs from dorsal view skeletal reconstructions of the shell of Araripemys barretoi as shown in Meylan and Gaffney, 1991 and Sereno and ElShafie, 2013). Of costal 3, only a tiny part is visible, sutured to costal 2. The sutures between peripheral 2, 3 and 4 are only partially discernible, whereas there is a clear suture between peripheral 4 and 5. All bone surfaces appear strongly weathered and abraded, but a sculpturing pattern consisting of low knobs or protrusions is still distinctly visible on all bones. The presence of scute sulci is evidenced by low ridges, visible on peripheral 4 and 5, and on costal 2 just posterior to the free rib end. Two additional bone fragments (likely being parts of costals), separate from this larger slab, also carry a distinct bone surface sculpturing and are thus likely also referable to Araripemydidae; these bones are too fragmentary to be further identified. No bones referable to Araripemydidae are visible on the ventral side of the concretion.
Indeterminate bone fragments
In addition, 18 small bone fragments on the dorsal side of the concretion appear to have been added haphazardly to fill holes between the larger shell parts mentioned above. Five of these have been identified as pertaining to costals being visible in ventral view (Fig. 2c), as they either preserve a proximal rib head or show the extent of the rib bulge within the costal. Two additional fragments likely also pertain to the plastron (one of which shows a strongly interdigitating suture between parts of a xiphiplastron and hypoplastron). Two fragments at the anterior right margin of the concretion were identified as peripherals due to their tapering cross-section, the anterolateral facing margin carrying sutural bony pegs, and the posteromedially facing margin being straight and tapering. The outer bone surface appears smooth (whether it is the dorsal or ventral bone surface remains unclear), unlike the dorsal bone surfaces of the peripherals of the Santanachelys or Araripemys peripherals. The remaining nine fragments could not be identified with confidence based on their shape or bone surface structure.
Discussion and conclusions
UFRPE 5061 preserves a genuine partial skeleton including a posterior portion of the skull of the pan-cryptodiran protostegid marine turtle Santanachelys gaffneyi and represents the second known specimen of this key taxon. The missing part of the carapace was completed by carapace fragments of pleurodiran Araripemydidae, more common turtles of the Romualdo Formation, together with other fragments of indeterminate turtles. The estimated straight carapacial length of Santanachelys gaffneyi in UFRPE 5061 (ca. 170–180 mm; see Table 1) is slightly larger than that of the holotype specimen THUg1386 (145 mm; Hirayama, 1998). UFRPE 5061 further reveals that the new specimen has only six neurals dorsally exposed as a result of costals 7 and 8 meeting one another in the midline through a slightly undulating suture above neural 7. The remnant of neural 7, as is visible in the CT scan data (see Additional video file), thus appears to have been developmentally arrested earlier due to the costal overgrowth and thus lacks dorsal exposure. Concerning neural reduction in the turtle shell, Thomson and Georges (1996, p. 82) noted that “neural bones are probably structurally important for resisting downward pressure in high-domed species, but may be a disadvantage where lateral forces in flatter forms cause torsion among carapacial elements (Pritchard, 1988). Hence, strong swimmers that move by alternating thrusts of the rear limbs, and marine turtles that alternate strokes on land, tend to have reduced neural series with areas of median contiguity between opposing pleural bones (Pritchard, 1988)”. A negative allometry in the last neural bones in side-necked turtle Bauruemys elegans has been identified by Romano and Azevedo (2007), with neurals 5 and 6 being relatively smaller in larger adult specimens, and the sacral region of the carapace was identified as a more variable region in terms of shell bone pattern formation due to potential lack of connectivity with endoskeletal elements (Zangerl, 1969). Whether the developmental arresting of neural 7 in UFRPE 5061 is due to some specific functional aspects or similar behaviour as noted for the different aquatic species above, or whether it is a pathology/aberrant developmental feature or a simple intraspecific shape variation due to size (i.e., allometry) for the species cannot be elucidated at present. Finally, it is noteworthy that the vertebral 2–3 sulcus crosses neural 4 in UFRPE 5061, instead of crossing neural 3 as in the holotype THUg1386 (Hirayama, 1998), thus adding to the growing body of scute malformation and individual shield variation in turtles (e.g., Zimm, 2019). As only the second specimen of Santanachelys gaffneyi described, UFRPE 5061 thus provides first insights into morphological variation, as well as the potential to further study the skeletal anatomy of this taxon.
Availability of data and materials
The fossil specimen described here is available for study at the UFRPE and the cast of the specimen is stored at PIMUZ. All data generated or analysed during this study are included in this published article. The CT dataset is made available at Morphosource repository project ID 000501147 (https://www.morphosource.org/projects/000501147).
Anquetin, J. (2012). Reassessment of the phylogenetic interrelationships of basal turtles (Testudinata). Journal of Systematic Palaeontology, 10, 3–45. https://doi.org/10.1080/14772019.2011.558928
Anquetin, J., Püntener, C., & Billon-Bruyat, J.-P. (2015). Portlandemys gracilis n. sp., a new coastal marine turtle from the Late Jurassic of Porrentruy (Switzerland) and a reconsideration of plesiochelyid cranial anatomy. PLoS ONE, 10, e0129193. https://doi.org/10.1371/journal.pone.0129193]
Anquetin, J., Püntener, C., & Joyce, W. G. (2017). A review of the fossil record of turtles of the clade Thalassochelydia. Bulletin of the Peabody Museum of Natural History, 58, 317–369.
Arai, M., & Assine, M. L. (2020). Chronostratigraphic constraints and paleoenvironmental interpretation of the Romualdo Formation (Santana Group, Araripe Basin, Northeastern Brazil) based on palynology. Cretaceous Research, 116, 104610. https://doi.org/10.1016/j.cretres.2020.104610
Assine, M. L., Perinotto, J. A. D. J., Custódio, M. A., Neumann, V. H., Varejão, F. G., & Mescolotti, P. C. (2014). Sequências deposicionais do Andar Alagoas da Bacia do Araripe, Nordeste do Brasil. Boletim De Geociências Da Petrobrás, 22, 3–28.
Cadena, E. A., & Parham, J. F. (2015). Oldest known marine turtle? A new protostegid from the Lower Cretaceous of Colombia. PaleoBios, 32, 1–42.
Carvalho, A. R. A., Oliveira, G. R., & Barreto, A. M. F. (2019). New occurrences of fossil Testudines of the Romualdo Formation, Aptian-Albian of the Araripe Basin, Pernambuco, Northeast Brazil. Journal of South American Earth Sciences, 94, 102211. https://doi.org/10.1016/j.jsames.2019.102211
Cisneros, J. C., Raja, N. B., Ghilardi, A. M., Dunne, E. M., Pinheiro, F. L., Regalado Fernández, O. R., Sales, M. A. F., Rodríguez-de la Rosa, R. A., Miranada-Martínez, A. Y., González-Mora, S., Bantim, R. A. M., de Lima, F. J., & Pardo, J. D. (2022). Digging deeper into colonial palaeontological practices in modern day Mexico and Brazil. Royal Society Open Science, 9, 210898. https://doi.org/10.1098/rsos.210898
Custódio, M. A., Quaglio, F., Warren, L. V., GuimarãesSimões, M., Fürsich, F. T., Perinotto, J. A. J., & Assine, M. L. (2017). The transgressive-regressive cycle of the Romualdo Formation (Araripe Basin): Sedimentary archive of the Early Cretaceous marine ingression in the interior of Northeast Brazil. Sedimentary Geology, 359, 1–15. https://doi.org/10.1016/j.sedgeo.2017.07.010
Danilov, I. G., & Parham, J. F. (2006). A redescription of ‘Plesiochelys’ tatsuensis from the Late Jurassic of China, with comments on the antiquity of the crown clade Cryptodira. Journal of Vertebrate Paleontology, 26, 573–580.
Evers, S. W., Barrett, P. M., & Benson, R. B. J. (2019). Anatomy of Rhinochelys pulchriceps (Protostegidae) and marine adaptation during the early evolution of chelonioids. PeerJ, 7, e6811. https://doi.org/10.7717/peerj.6811
Evers, S. W., & Benson, R. B. J. (2019). A new phylogenetic hypothesis of turtles with implications for the timing and number of evolutionary transitions to marine lifestyles in the group. Palaeontology, 62, 93–134. https://doi.org/10.1111/pala.12384
Fürsich, F. T., Custódio, M. A., Matos, S. A., Hethke, M., Quaglio, F., Warren, L. V., Assine, M. L., & Simões, M. G. (2019). Analysis of a Cretaceous (late Aptian) high-stress ecosystem: The Romualdo Formation of the Araripe Basin, northeastern Brazil. Cretaceous Research, 95, 268–296. https://doi.org/10.1016/j.cretres.2018.11.021
Gaffney, E. S. (2001). Cearachelys, a new side-necked turtle (Pelomedusoides: Bothremydidae) from the Early Cretaceous of Brazil. American Museum Novitates, 3319, 1–20.
Gaffney, E. S., Tong, H., & Meylan, P. A. (2006). Evolution of the side-necked turtles: The families Bothremydidae, Euraxemydidae, and Araripemydidae. Bulletin of the American Museum of Natural History, 300, 1–698.
Gaffney, E. S., Meylan, P. A., Wood, R. C., Simons, E., & Almeida Campos, D. de. ( 2011). Evolution of the side-necked turtles: the family Podocnemididae. American Museum of Natural History, Bulletin, 350, 1–237. https://doi.org/10.1206/350.1
Gentry, A. D., Ebersole, J. A., & Kiernan, C. R. (2019). Asmodochelys parhami, a new fossil marine turtle from the Campanian Demopolis Chalk and the stratigraphic congruence of competing marine turtle phylogenies. Royal Society Open Science, 6, 191950. https://doi.org/10.1098/rsos.191950
Hirayama, R. (1998). Oldest known sea turtle. Nature, 392, 705–708.
Joyce, W. G. (2007). Phylogenetic relationships of Mesozoic turtles. Bulletin of the Peabody Museum of Natural History, 48, 3–102.
Joyce, W. G., Anquetin, J., Cadena, E.-A., Claude, J., Danilov, I. G., Evers, S. W., Ferreira, G. S., Gentry, A. D., Georgalis, G. L., Lyson, T. R., Pérez-García, A., Rabi, M., Sterli, J., Vitek, N. S., & Parham, J. F. (2021). A nomenclature for fossil and living turtles using phylogenetically defined clade names. Swiss Journal of Palaeontology, 140, 5. https://doi.org/10.1186/s13358-020-00211-x
Joyce, W. G., Parham, J. F., Anquetin, J., Claude, J., Danilov, I., Iverson, J. B., Kear, B. P., Lyson, T. R., Rabi, M., & Sterli, J. (2020a). Pan-Cryptodira. In K. de Queiroz, P. D. Cantino, & J. A. Gauthier (Eds.), Phylonyms—A Companion to the PhyloCode (pp. 1059–1060). CRC Press.
Joyce, W. G., Parham, J. F., Anquetin, J., Claude, J., Danilov, I., Iverson, J. B., Kear, B. P., Lyson, T. R., Rabi, M., & Sterli, J. (2020b). Pleurodira. In K. de Queiroz, P. D. Cantino, & J. A. Gauthier (Eds.), Phylonyms—A Companion to the PhyloCode (pp. 1055–1057). CRC Press.
Kear, B. P., & Lee, M. S. Y. (2006). A primitive protostegid from Australia and early sea turtle evolution. Biology Letters, 2, 116–119.
Kellner, A. W. A., Campos, D. A., Sayão, J. M., Saraiva, A. Á. F., Rodrigues, T., Oliveira, G. R., Cruz, L. A., Costa, F. R., Silva, H. P., & Ferreira, J. S. (2013). The largest flying reptile from Gondwana: A new specimen of Tropeognathus cf. T. mesembrinus Wellnhofer, 1987 (Pterodactyloidea, Anhangueridae) and other large pterosaurs from the Romualdo Formation, Lower Cretaceous, Brazil. Anais Da Academia Brasileira De Ciências, 85, 113–135. https://doi.org/10.1590/S0001-37652013000100009
Lapparent, F., & de Broin, F. (2000). The oldest pre-podocnemidid turtle (Chelonii, Pleurodira), from the early Cretaceous, Ceará state, Brasil, and its environment. Treballs Del Museu De Geologia De Barcelona, 9, 43–95.
Limaverde, S., Vargas Pêgas, R., Damasceno, R., Villa, C., Oliveira, G. R., Bonde, N., & Leal, M. E. C. (2020). Interpreting character variation in turtles: Araripemys barretoi (Pleurodira: Pelomedusoides) from the Araripe Basin, Early Cretaceous of Northeastern Brazil. PeerJ, 8, e9840. https://doi.org/10.7717/peerj.9840
Liston, J. (2014). Fossil protection legislation: Chinese issues, global problems. Biological Journal of the Linnean Society, 113, 694–706. https://doi.org/10.1111/bij.12293
Maisey, J. G. (Ed.) (1991). Santana fossils: An Illustrated Atlas. Neptune City: T.F.H. Publications.
Martill, D. M. (1994). Fake fossils from Brazil. Geology Today, 10, 111–115. https://doi.org/10.1111/j.1365-2451.1994.tb00882.x
Martill, D. M. (2007). The age of the Cretaceous Santana Formation fossil Konservat Lagerstätte of north-east Brazil: A historical review and an appraisal of the biochronostratigraphic utility of its palaeobiota. Cretaceous Research, 28, 895–920. https://doi.org/10.1016/j.cretres.2007.01.002
Mateus, O., Overbeeke, M., & Rita, F. (2008). Dinosaur frauds, hoaxes and “Frankensteins”: How to distinguish fake and genuine vertebrate fossils. Journal of Paleontological Techniques, 2, 1–5.
Melo, R. M., Guzmán, J., Almeida-Lima, D., Piovesan, E. K., Neumann, V. H. M. L., & Sousa, A. J. (2020). New marine data and age accuracy of the Romualdo Formation, Araripe Basin, Brazil. Scientific Reports, 10, 15779. https://doi.org/10.1038/s41598-020-72789-8
Meylan, P. A. (1996). Skeletal morphology and relationships of the Early Cretaceous side-necked turtle, Araripemys barretoi (Testudines: Pelomedusoides: Araripemydidae), from the Santana Formation of Brazil. Journal of Vertebrate Paleontology, 16, 20–33.
Meylan, P., & Gaffney, E. S. (1991). Araripemys PRICE, 1973. In J. G. Maisey (Ed.), Santana fossils: An illustrated atlas (pp. 326–334). T.F.H. Publications.
Oliveira, G. R. (2007). Aspectos Tafonômicos de Testudines da Formação Santana (Cretáceo Inferior), Bacia do Araripe, Nordeste do Brasil. Anuário Do Instituto De Geociências UFRJ, Brazil, 30, 83–93.
Oliveira, G. R., & Kellner, A. W. A. (2005). Note on a plastron (Testudines, Pleurodira) from the Lower Cretaceous Crato Member, Santana Formation, Brazil. Arquivos Do Museu Nacional, Rio De Janeiro, 63, 523–528.
Oliveira, G. R., & Kellner, A. W. A. (2007). A new side-necked turtle (Pleurodira, Pelomedusoides) from the Santana Formation (Early Cretaceous), Araripe Basin, Northeastern Brazil. Zootaxa, 1425, 53–61. https://doi.org/10.11646/zootaxa.1425.1.7
Oliveira, G. R., & Kellner, A. W. A. (2017). Rare hatchling specimens of Araripemys Price, 1973 (Testudines, Pelomedusoides, Araripemydidae) from the Crato Formation, Araripe Basin. Journal of South American Earth Sciences, 79, 137–142. https://doi.org/10.1016/j.jsames.2017.07.014
Oliveira, G. R., & Romano, P. S. R. (2007). Histórico dos achados de tartarugas fósseis do Brasil. Arquivos Do Museu Nacional, Rio De Janeiro, 65, 113–133.
Oliveira, G. R., Saraiva, A. A. F., De Paula Silva, H., Gomes de Antrade, J. A. F., & Kellner, A. W. A. (2011). First turtle from the Ipubi Formation (Early Cretaceous), Santana Group, Araripe Basin, Brazil. Revista Brasileira De Paleontologia, 14, 61–66. https://doi.org/10.4072/rbp.2011.1.06
Parham, J. F. (2005). A reassessment of the referral of the sea turtle skulls to the genus Osteopygis (Late Cretaceous, New Jersey, USA). Journal of Vertebrate Paleontology, 25, 71–77.
Pérez-García, A. (2019). Identification of the Lower Cretaceous pleurodiran turtle Taquetochelys decorata as the only African araripemydid species. Comptes Rendus Palevol, 18, 24–32. https://doi.org/10.1016/j.crpv.2018.04.004
Price, L. I. (1973). Quelônio Amphichelydia no Cretáceo Inferior do Nordeste do Brasil. Revista Brasileira De Geociências, 3, 84–96.
Pritchard, P. C. H. (1988). A survey of neural bone variation among recent chelonian species, with functional interpretations. Acta Zoologica Cracoviensia, 31, 625–686.
Rabi, M., & Kear, B. P. (2016). Transitional fossils shed light on the basal divergence of advanced marine turtles. Journal of Vertebrate Paleontology, Program and Abstracts Book, 2016, 210.
Raja, N. B., Dunne, E. M., Matiwane, A., Khan, T. M., Nätscher, P. S., Ghilardi, A. M., & Chattopadhyay, D. (2021). Colonial history and global economics distort our understanding of deep-time biodiversity. Nature Ecology and Evolution, 6, 145–154. https://doi.org/10.1038/s41559-021-01608-8
Raselli, I. (2018. Comparative cranial morphology of the Late Cretaceous protostegid sea turtle Desmatochelys lowii. Peer J, 6, e5964. https://doi.org/10.7717/peerj.5964
Romano, P. S. R., Oliveira, G. R., Azevedo, S. A. K., Kellner, A. W. A., & de Almeida Campos, D. (2013). New Information about Pelomedusoides (Testudines: Pleurodira) from the Cretaceous of Brazil. In: Brinkman, D. B., Holroyd, P. A., & Gardner, J. D. (Eds.), Morphology and Evolution of Turtles. Proceedings of the Gaffney Turtle Symposium (2009) in Honor of Eugene S Gaffney. Vertebrate Paleobiology and Paleoanthropology Series (pp. 261–275). Dordrecht: Springer.
Romano, P. S., & Azevedo, S. A. K. (2007). Morphometric analysis of the Upper Cretaceous Brazilian side-necked turtle Bauruemys elegans (Suárez, 1969) (Pleurodira, Podocnemididae). Arquivos Do Museu Nacional, 65(4), 395–402.
Ruffell, A., Majury, N., & Brooks, W. E. (2012). Geological fakes and frauds. Earth-Science Reviews, 111, 224–231. https://doi.org/10.1016/j.earscirev.2011.12.001
Sayão, J. M., Feitosa Saraiva, A. Á., Brum, A. S., Bantim, R. A. M., Pedroso de Andrade, R. C. L., Xin, C., Jorge de Lima, F., De Paula Silva, H., & Kellner, A. W. A. (2020). The first theropod dinosaur (Coelurosauria, Theropoda) from the base of the Romualdo Formation (Albian), Araripe Basin, Northeast Brazil. Scientific Reports, 10, 10892. https://doi.org/10.1038/s41598-020-67822-9
Sena, M. V. A., Bantim, R. A. M., Saraiva, A. A. F., Sayão, J. M., & Oliveira, G. R. (2021). Osteohistology and microanatomy of a new specimen of Cearachelys placidoi (Testudines: Pleurodira) a side-necked turtle from the Lower Cretaceous of Brazil. The Anatomical Record, 304, 1294–1304. https://doi.org/10.1002/ar.24556
Sereno, P. C., ElShafie, S. J. (2013. A new long-necked turtle Laganemys tenerensis (Pleurodira: Araripemydidae) from the Elrhaz Formation (Aptian–Albian) of Niger. In: Brinkman, D. B., Holroyd, P. A., & Gardner, J. D. (Eds.), Morphology and Evolution of Turtles. Proceedings of the Gaffney Turtle Symposium (2009) in Honor of Eugene S Gaffney. Vertebrate Paleobiology and Paleoanthropology Series (pp. 215–250). Dordrecht: Springer.
Sterli, J. (2010). Phylogenetic relationships among extinct and extant turtles: The position of Pleurodira and the effects of the fossils on rooting crown-group turtles. Contributions to Zoology, 79, 93–106.
Sterli, J., & de La Fuente, M. (2011). A new turtle from the La Colonia Formation (Campanian-Maastrichtian), Patagonia, Argentina, with remarks on the evolution of the vertebral column in turtles. Palaeontology, 54, 63–78. https://doi.org/10.1111/j.1475-4983.2010.01002.x
Thomson, S., & Georges, A. (1996). Neural bones in Australian chelid turtles. Chelonian Conservation and Biology, 2, 82–86.
Veldmeijer, A. J. (2006). Toothed pterosaurs from the Santana Formation (Cretaceous; Aptian–Albian) of northeastern Brazil. A reappraisal on the basis of newly described material. PhD Thesis, Universiteit Utrecht, The Netherlands. pp. 269.
Vila Nova, B. C., Saraiva, A. A. F., Moreira, J. K. R., & Sayão, J. M. (2011). Controlled excavations in the Romualdo Formation Lagerstätte (Araripe Basin, Brazil) and pterosaur diversity: Remarks based on new findings. Palaios, 26, 173–179. https://doi.org/10.2110/palo.2010.p10-072r
Wellnhofer, P. (1985). Neue Pterosaurier aus der Santana-Formation (Apt) der Chapada do Araripe, Brasilien. Palaeontographica Abt. A, 187, 105–182.
Zangerl, R. (1969). The turtle shell. In C. Gans, A. D. A. Bellairs, & T. S. Parsons (Eds.), Biology of the Reptilia. Morphology A (Vol. 1, pp. 311–339). London: Academic Press.
Zimm, R. (2019). On the development of the turtle scute pattern and the origins of its variation. PhD thesis, Institute of Biotechnology, Department of Biosciences, University of Helsinki, Finland. pp. 89.
Christina Egli (Zell) is thanked for the skilful preparation and Christian Klug (PIMUZ) for granting access to the specimen while in Zurich and enabling the repatriation to Brazil. We also thank Irma Tie Yamamoto from the Agência Nacional de Mineração (National Mining Agency for protection of the national fossiliferous patrimony), Gabriel Rivas de Melo and Marcelo Brito Carneiro Leão (UFRPE) for their support during the repatriation process, and Gabriel Mestriner da Silva (USP), and Flaviana Lima and Renan Bantim (UFRPE) for their help in getting the turtle to its final destination in Recife. We further thank Serjoscha Evers (Univ. Fribourg) and one anonymous reviewer, as well as editors Walter Joyce and Daniel Marty for their helpful comments that improved the manuscript.
TMS acknowledges support by the Swiss National science Foundation (31003A‑179401). PSRR acknowledges support by the Fundação de Amparo à Pesquisa do Estado de Minas Gerais (APQ-01025-22).
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Additional file 1: Flythrough video of the CT scan data produced at SCANCO Medical AG.
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Scheyer, T.M., Oliveira, G.R., Romano, P.S.R. et al. A forged ‘chimera’ including the second specimen of the protostegid sea turtle Santanachelys gaffneyi and shell parts of the pleurodire Araripemys from the Lower Cretaceous Santana Group of Brazil. Swiss J Palaeontol 142, 6 (2023). https://doi.org/10.1186/s13358-023-00271-9
- Early Cretaceous
- Santana group
- Romualdo Formation
- Marine turtle