Figures
Abstract
Madagascar is well known for producing exceptional fossils. However, the record for selachians remains relatively poorly known. Paleontological reconnaissance on the island of Nosy Makamby, off northwest Madagascar, has produced a previously undescribed assemblage of Miocene fossils. Based on isolated teeth, ten taxonomic groups are identified: Otodus, Carcharhinus, Galeocerdo, Rhizoprionodon, Sphyrna, Hemipristis, Squatina, Rostroraja, Himantura and Myliobatidae. Six are newly described from Madagascar for the Cenozoic (Galeocerdo, Rhizoprionodon, Sphyrna, Squatina, Rostroraja and Himantura). In association with these specimens, remains of both invertebrates (e.g., corals, gastropods, bivalves) and vertebrates (e.g., bony fish, turtles, crocodylians, and sirenian mammals) were also recovered. The sedimentary facies are highly suggestive of a near-shore/coastal plain depositional environment. This faunal association shares similarities to contemporaneous sites reported from North America and Europe and gives a glimpse into the paleoenvironment of Madagascar’s Miocene, suggesting that this region was warm, tropical shallow-water marine.
Citation: Andrianavalona TH, Ramihangihajason TN, Rasoamiaramanana A, Ward DJ, Ali JR, Samonds KE (2015) Miocene Shark and Batoid Fauna from Nosy Makamby (Mahajanga Basin, Northwestern Madagascar). PLoS ONE 10(6): e0129444. https://doi.org/10.1371/journal.pone.0129444
Academic Editor: Andrew A. Farke, Raymond M. Alf Museum of Paleontology, UNITED STATES
Received: December 30, 2014; Accepted: May 7, 2015; Published: June 15, 2015
Copyright: © 2015 Andrianavalona et al. This is an open access article distributed under the terms of the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited
Data Availability: All relevant data are within the paper.
Funding: National Geographic supported fieldwork in 2010 and 2013; in 2011 it was funded by the University of Queensland, and in 2014 by Northern Illinois University.
Competing interests: The authors have declared that no competing interests exist.
Introduction
Madagascar is one of the world’s highest-priority biodiversity “hotspots” with high endemism of plants and animals [1]. These groups have been greatly shaped through isolation; originally wedged between Africa and India as part of the larger Gondwanan landmass, Indo-Madagascar separated from other landmasses ~115 Ma, with complete isolation occurring ~88 Ma [2]. The ancestors of most of the island’s living groups appear to have arrived after the island was already isolated, possibly through rare “rafting” events [3].
Subsequent diversification and multiple devastating extinction events have also played a major role, as well as substantial climatic changes that affected both the island’s marine and terrestrial fauna. These include the Paleocene/Eocene thermal maximum (~55.8 Ma), the extreme lowering of temperature during the Grande Coupure at the Eocene/Oligocene boundary, and the shift to “modern” ocean circulation patterns during the mid-Miocene [4].
Madagascar’s living sharks and rays are thought to exceed 100 modern species [5]. While Madagascar is known for producing outstanding fossils, the record of selachians is relatively poor being restricted to the Triassic [6], and Upper Cretaceous [7–9], Eocene [10,11] and Miocene [9,12].
The only other study of Madagascar’s Miocene selachians recorded “Carcharodon” megalodon, Odontaspis, “Carcharias”, Galeocerdo, “Sphyrna”, Hemipristis and Myliobatis from Nosy Makamby [12]. We report here the first comprehensive fossil selachian assemblage from the Miocene of Madagascar, likely from the same layer, consisting of isolated teeth from ten taxonomic groups representing at least 12 species, six of which are newly described from Madagascar: Galeocerdo, Rhizoprionodon, Sphyrna, Squatina, Rostroraja and Himantura. We include comparisons with other contemporaneous faunas and explore environmental indicators and other associated taxa to help shed light on this region’s paleoenvironment.
Geology and Age
Nosy Makamby (= Mahakamby) is a small (~1.6 km x 0.4 km) island SSW-NNE aligned offshore at broad of the delta of Mahavavy River, in northwest Madagascar, approximately 50 km west along the coast from the regional capital of Mahajanga (Figs 1 and 2). Very little geological information has been reported from Nosy Makamby and surrounding areas [13,14]; the only comprehensive description of the island’s fossils is the result of reconnaissance work done in the early part of the last century [12]. Recent exploration has produced a diverse assemblage of both invertebrates and vertebrates from Nosy Makamby, including foraminiferans, bivalves, gastropods, crabs, echinoids, sharks, non-diagnostic reptiles (turtles and crocodylians), and sirenians [12,14–16].
Also indicated is the port city of Mahajanga.
Within the Miocene, the oldest exposed levels occur midway down the eastern coast.
Nosy Makamby exposes one of the thickest and most complete sedimentary layers of marine Miocene in Madagascar, with lateral extensions of the succession in the regions of Cap Tanjona, Cap Sada, and Amparafaka to the west [12]. Two “formations” are exposed on the island (Fig 2)–a Miocene clastic unit, consisting mainly of medium to coarse sandstones that accumulated in a coastal plain/near-shore marine environment, and a Pliocene continental unit comprising red beds and quartz grits [12,14] (Fig 3). Geological sections on Nosy Makamby expose about 15 m of Miocene sediments. Interestingly, the thicknesses of the lithostratigraphic units mentioned in previous work are almost exactly an order of magnitude greater that the ones we observed, presumably this error occurred when Collignon and Cottereau published their manuscript [12]. A key marker bed is the informally designated “Ceremony Site Horizon” (FCSH), its “type-locality” being a 25-m-long by 10-m-wide platform on the north-eastern headland. Using this horizon together with a ~2.5 m-thick package of rocks immediately below that is rich in Kuphus tubes [17] makes the tracing of levels between exposures on the north of the island straightforward.
The view is towards the south and represents the profile of the eastern side.
The sedimentary facies associated with the Miocene rocks are highly suggestive of a near-shore/estuarine/coastal plain depositional environment (probably not unlike the mouth of the present-day Betsiboka) possessing course sands containing significant amounts of pristine and abraded biogenic material and cross-bedding indicating transport directions in opposites directions (but without herring-bone cross-bedding). While the geologic section suggests a tidal, very shallow environment, there is a decided lack of plant debris in the sediments. The only level where such material was found occurs in 0.4-cm thick bed along the eastern coast, ~8 m below the FCSH (Fig 2). Clearly not much carbonaceous material found its way into these deposits, which might provide clues as to the nature of the vegetation and/or the climate system in the Mahajanga Basin during the Miocene.
Shark teeth come from the horizon captioned as “Abundant pristine and broken invertebrates, occasional fish and shark teeth” (Fig 3). While there is no specific locality information in Collignon and Cottreau [12] we assume that our fossils come from the same layer as described in their paper.
Methods
Fossils were obtained through surface collection as well as both wet and dry screening. Residue from screening was broken down in the laboratory using acetic acid preparation techniques [18]. Residue was placed into a dilute (~5%) solution of acetic acid buffered with calcium orthophosphate. After each acid treatment, pieces were placed in water and rinsed thoroughly until completely free of acetic acid. Material disaggregated from the blocks was put through a 0.5 mm sieve and rinsed until clean. Samples were then air dried and sorted under a microscope. Photographs and standard measurements were taken, where appropriate, to aid in identification. Measurements were made with 500–172 Mitutoyo digital calipers to 0.1 mm. All specimens mentioned in this paper are deposited in the Laboratory of Paleontology and Biostratigraphy (Department of Paleontology and Biological Anthropology, UAP = Université d’Antananarivo, Antananarivo, Madagascar). All necessary permits were obtained from the Malagasy Ministry of Mines for the described study, which complied with all relevant regulations (001/2005; 002/2010;003/2011; 001/2013; 001/2014).
Systematic Paleontology
For the classification of higher taxa as well as stratigraphic and geographic distribution see Cappetta (2012) [19]. The size of the specimens can be extrapolated from the plate and are given where appropriate.
Class Chondrichthyes Huxley, 1880
Subclass Elasmobranchii Bonaparte, 1838
Superorder Galeomorphii Compagno, 1973
Family otodontidae Glickman, 1964
Genus Otodus Agassiz, 1843 sensu Cappetta, 2012
Otodus megalodon Agassiz, 1835
A, Otodus megalodon UAP-11.281; B-E, Carcharhinus priscus, B, UAP-14.239–1, lower tooth in labial view; C, UAP-14.239–1, lower tooth in lingual view; D, UAP-14.181–14, upper tooth in labial view; E, UAP-14.181–14, upper tooth in labial view; F, Carcharhinus sp. UAP-13.159; G-H, Galeocerdo mayumbensis UAP-13.167, UAP-13.172; I-J, Rhizoprionodon ficheuri UAP-14.122–9 I, labial view; J, lingual view; K, Sphyrna sp. UAP-13142; L-N Hemipristis serra UAP-10.362; O, Squatina UAP-10.505. Scale bar equals 10 mm, unless specified in the Figure.
Synonomy and selected references
See [19] for both a description and a discussion of the use of the genus Otodus for this lineage.
Material
One tooth (UAP-11.281).
One right upper anterior tooth from a juvenile individual 41.0 mm high and 34.5 mm wide at the base.
Discussion
This species of shark (often referred to as a "Megatooth shark") is one of the more common and most iconic Cenozoic fossil vertebrates. It is frequently and erroneously, referred to as "Carcharodon megalodon" implying a close relationship with the great white shark. It was also referred to the genera Procarcharodon Casier, 1960 and Carcharocles Jordan and Hannibal, 1923. Ward and Bonavia [20] briefly discussed the taxonomy, ontogeny and species concepts. In the Miocene, teeth of juvenile individuals of C. megalodon bear lateral cusps which progressively diminish in size with age, the adults having completely lost them [20]. This particular morphotype is usually referred to as O. chubutensis [21]. Collignon and Cottreau [12] list three teeth of Otodus megalodon (as Carcharodon megalodon) from Makamby. They liken one of them to an early Miocene tooth, bearing small rounded, almost vestigial lateral cusps, figured by Priem (p. 122, pl. III, Fig 4 [22]) from the south of France which Priem referred to as O. megalodon var. productus (Agassiz 1843). As our only specimen has damage to both the medial and distal cutting edge at the crown base, it is impossible to say whether it would have corresponded to this morphotype.
Order Carcharhiniformes Compagno, 1973
Family Carcharhinidae Jordan & Evermann, 1896
Genus Carcharhinus Blainville, 1816
Description
See Cappetta (p. 301, Fig 285) [19] for images of upper and lower teeth of an assortment of Recent species. Teeth of Carcharhinus generally exhibit dignathic and gradient heterodonty. Upper teeth are broadly triangular, usually slightly distally directed and serrated. The labial face is flat and does not possess a basal bulge; lingual face is slightly convex. Lower teeth are generally an inverted "T" shape with a narrower more upright crown and wide root and usually lightly serrated. Cusps are narrower and the labial face of the crown occasionally overhangs the root [19].
Carcharhinus priscus Agassiz, 1843
Material
Ninety three teeth (UAP-05.378, UAP-10.219, UAP-10.269, UAP-10.272, UAP-10.311, UAP-10.340, UAP-10.343, UAP-10.346, UAP-10.364, UAP-10.367, UAP-10.369, UAP-10.370, UAP-10.399, UAP-10.418, UAP10445, UAP-10.449, UAP10450, UAP-10.425, UAP-10.451, UAP-10.459, UAP-10.501, UAP-10.504, UAP-11.160, UAP-11.164, UAP-11.166, UAP-11.170, UAP-11.174, UAP-11.192, UAP-11.233, UAP-11.234, UAP-11.240, UAP-11.167, UAP-11.178, UAP-11.81, UAP-11.193, UAP-11.199, UAP-11.215, UAP-11.232, UAP-11.271, UAP-11.286, UAP-11.287, UAP-11.352, UAP-13.010–1, UAP-13.103, UAP-13.130, UAP-13.127, UAP-13.129, UAP-13.132, UAP-13.134, UAP-13.139, UAP-13.141, UAP-13.148, UAP-13.150, UAP-13.157, UAP-13.158, UAP-13.160, UAP-13.161, UAP-13.010–1, UAP-13.110, UAP-13.119, UAP-13.127, UAP-13.129, UAP-13.132, UAP-13.141, UAP-13.145, UAP-13.146, UAP-13.148, UAP-13.150, UAP-13.157, UAP-13.158, UAP-13.160, UAP-13.161, UAP-14.122–3, UAP-14.122-, UAP-14.122–5, UAP-14.122–8, UAP-14.128–1, UAP-14.128–2, UAP-14.129–3, UAP-14.181–3, UAP-14.181, UAP-14.181–10, UAP-14.181–11, UAP-14.181–12, UAP-14.181–14, UAP-14.181–19, UAP-14.202–2, UAP-14.215–2, UAP-14.215–4, UAP-14.215–5, UAP-14.239–1, UAP-14.239–6).
Description
See Reinecke et al. [23] and Bor et al. [24] for an extensive review of C. priscus. Upper teeth of C. priscus are characterized by having an unserrated or very lightly serrated cusps and moderately serrated crown shoulders. The crown is triangular and has uniform serrations along the entire border. Teeth are straight in labial view and the lingual surface is slightly convex. Root has a central foramen. Lower teeth have a narrower cusp well separated from the heels.
Discussion
The teeth from Nosy Makamby correspond quite closely to some of Agassiz's types from the early Miocene of Malta (Tome III, p. 235,235, pl. 26a, Figs 44, 47, 48) and also those figured by Reinecke et al. p. 64, pls 71–76 [23]. Carcharhinus priscus was recorded by Collignon and Cottreau [12] from Makamby under the name Sphyrna prisca Agassiz. It is very likely that their records of "Carcharias (Prionodon)" and "Carcharias (Aprionodon)" were also based on teeth of C. priscus, the latter being lower teeth. The genus "Carcharias" was used for teeth we now refer to Carcharhinus currently well into the 20th century and was used by Priem [22] in a paper on Neogene shark teeth from southwest France. It is likely that this publication was used by Collignon and Cottreau [12] for their identifications. C. priscus is the most common species of Carcharhinus in the European Miocene and probably gave rise to the Recent species C. brachyurus Günther, 1870, C. limbatus Valenciennes, 1839, C. perezii Poey, 1876, among others.
In contrast to the somewhat restricted NW European assemblage, Purdy et al. [25] recorded a diverse Carcharhinus assemblage from the early Miocene Pungo River Marl, of Lee Creek, Aurora, North Carolina which they referred to Recent species.
Considering the variability observed in the C. priscus dentitions from NW Europe [23] and the conservative nature of teeth in some radiating shark lineages, one must consider the likelihood that C. priscus represents a species group rather than a discrete species.
Carcharhinus sp.
(Fig 4F)
Description
The tooth described (UAP-13.159) is small; 10.5 mm wide and 9.8 mm high. It has a low, finely serrated triangular crown flanked by evenly serrated lateral shoulders. The root is deep on the lingual aspect, and the labial surface bears a slight apically directed furrow.
Discussion
The combination of fine, even serrations and a broad triangular shape with convex shoulders is not seen in any extant species of Carcharhinus. It most closely resembles upper teeth of the obscurus—leucas- amboinensis—galapagensis—longimanus group of Carcharhinus species. Broad triangular teeth appear in the late Eocene of northern and north-western Africa, relatively early in the Carcharhinus fossil record (Adnet et al., 2010, p. 864, Fig 3G [26]; Underwood et al., p. 54, Fig 4N [27]).
It is very similar in appearance to one of the syntypes of Carcharias (Prionodon) similis Probst, 1878 (Fig 12), refigured by Reinecke et al. (p. 77, text Fig 26 a-c) [23] and who regarded it as a median tooth of Galeocerdo aduncus Agassiz, 1835. The similarity is compelling. However, the Malagasy teeth differ in having a very low mesial protuberance, as opposed to the pronounced protuberance in Probst's specimen.
Genus Galeocerdo Müller & Henle, 1837
Galeocerdo mayumbensis Dartevelle & Casier, 1943
Synonomy
1943 Galeocerdo mayumbensis sp. nov. Dartevelle & Casier, p. 153, pl. 12, Figs 22–30 [24].
1999 Galeocerdo casei sp. nov. Müller, p. 50 PL 11. 1–4. [28].
2011 Galeocerdo mayumbensis (name and figures only) Rathbone & Rathbone, p. 205 [29].
2015 Galeocerdo mayumbensis Argyriou et al. [30].
Material
Twenty three teeth (UAP-05.377, UAP-10.208, UAP-10.267, UAP-10.270, UAP-10.308, UAP-10.310, UAP-10.363, UAP-10.499, UAP-11.082, UAP-11.149, UAP-13167, UAP-13172, UAP-11099, UAP-11187, UAP-11200, UAP-11279, UAP-11280, UAP-11306, UAP-13162, UAP-14128-5, UAP-14131, UAP-14143-1, UAP-14161-1).
Description
See Cappetta (p. 298) [19] for a basic description of Galeocerdo teeth. Teeth of G. mayumbensis have a tall crown with a distally directed cusp with fine serrations. The mesial cutting edge is evenly convex while the distal heel is straight or slightly concave. Both are coarsely serrated; the larger, more apical serrae are themselves serrated. The distal notch between the cusp and the distal heel is reduced when compared with all other species of Galeocerdo [31].
Discussion
The teeth of G. mayumbensis most closely resemble those of G. eaglesomei White, 1955 from the mid and late Eocene. They differ from G. eaglesomei in exhibiting less monognathic heterodonty and from G. eaglesomei and the middle Eocene species G. latidens in having compound rather than simple serrae on the mesial cutting edge and the distal heel. Teeth of the late Miocene to Recent species, G. cuvier Péron & Lesueur, 1822 differ from those of G. mayumbensis by being lower cusped but more robust with a more pronounced mesial cutting edge and curbed distal heel. In G. mayumbensis the distal heel is straight, the distal notch much less developed, and the root more arched.
The most common Miocene species of Galeocerdo, G. aduncus Agassiz, 1835, differs from G. mayumbensis by being smaller and having a less sigmoid crown and a more convex (curved) mesial cutting edge [30]. It displays strong monognathic, dignathic and possibly gynandric heterodonty, characters not present in teeth of the other species of Galeocerdo. Ward and Bonavia [20] synonymized Galeocerdo contortus Gibbes, 1849 and Galeocerdo aduncus and referred them to Physogaleus. This revision was rejected by Reinecke et al. (p. 79) [23] a view accepted here. However, as the dentition of G. aduncus lies between that of Physogaleus and Galeocerdo we feel the species G. aduncus would be better accommodated in a separate genus.
Teeth of G. mayumbensis have only been figured in scientific literature from the early Miocene of Cabinda and Bololo, Angola [32], from the eastern USA by Müller 1999 [28] and from the early Miocene of Libya by Argyriou et al. [30]. This species is well known to fossil collectors in Florida and a number are figured in a popular sharks' tooth identification guide [29]. No stratigraphic information was included, however it does occur in the phosphorite pebble beds in the mid to late Miocene Bone Valley Member of Hawthorn Group exposed off shore at Venice Beach, Florida (David J. Ward, personal observation).
Genus Rhizoprionodon Whitley, 1929
Rhizoprionodon ficheuri (Joleaud, 1912)
Material
Fifty two teeth (UAP-10.344, UAP-10.371, UAP-10.372, UAP-10.375, UAP-10.444, UAP-10.446, UAP-10.452, UAP-10.455, UAP-10.461, UAP-11.025, UAP-11.266, UAP-11.168, UAP-11.183, UAP-11.195, UAP-11.196, UAP-11.197, UAP-11.198, UAP-11.206, UAP-11.239, UAP-11.258, UAP-11.263, UAP-11.265, UAP-11.266, UAP-11.284, UAP-11.337, UAP-13.100, UAP-13.103, UAP-13.106, UAP-13.109, UAP-13.125, UAP-13.133, UAP-13.134, UAP-13.136, UAP-13.137, UAP-13.138, UAP-13.139, UAP-13.149, UAP-13.152, UAP-13.163, UAP-14.122–1, UAP-14.122–7, UAP-14.122–9, UAP-14.128–6, UAP-14.129–2, UAP-14.161–2, UAP-14.161–3, UAP-14.181–17, UAP-14.202–1, UAP-14.215–3, UAP-14.215–6, UAP-14.215–7, UAP-14.215–9).
Description
Small wide teeth comprising distally directed crown and single distal cusplet which in lower teeth may be almost separate from the crown. This is more marked in male teeth.
Discussion
Teeth of Recent species of Rhizoprionodon, Loxodon and Scoliodon, as well as those of some juvenile hammerheads (Sphyrna) exhibit a very similar morphology and are difficult to separate. The tooth figured (Fig 4I and 4J) is a wide lower lateral tooth, a shape more typical of Rhizoprionodon.
Family SPHYRNIDAE Gill, 1872
Genus Sphyrna Rafinesque, 1810
Sphyrna sp.
(Fig 4K)
Material
Sixteen teeth (UAP-10.287, UAP-10.453, UAP-10.458, UAP-11.290, UAP-11.232, UAP-11.199, UAP-13.053–2, UAP-13.120, UAP-13.140, UAP-13.142, UAP-13.144, UAP-13.156, UAP-14.181–7, UAP-14.181–13, UAP-14.181–18, UAP-14.239–2).
Description
UAP-13.142: Height = 7.3 mm, width = 8.1 mm, thickness = 2.4 mm.
Small triangular teeth with a single distally directed crown and low distal blade, both lacking serrae. Root short with central foramen. Crown with smooth edges, lacking crenellations and basal ledge on the labial aspect. The lingual root bears a well-defined notch at level of crown base.
Discussion
While the teeth figured fall within the range of variation of the fossil species Sphyrna integra Probst, 1878 (figured by Reinecke et al.) [23] the sample size is too small for a confident identification. Purdy et al. [25] referred the teeth of hammerhead sharks from the Miocene and early Pliocene of Lee Creek Mine to three extant species: S. lewini Griffith & Smith, 1834, S. cf. S. media Springer, 1940 and S. zygaena Linnaeus, 1758; the latter they regarded as a senior synonym of S. laevissima Cope, 1867.
Family Hemigaleidae Hasse, 1879
Genus Hemipristis Agassiz, 1835
Hemipristis serra Agassiz, 1835
Material
Thirteen teeth (UAP-10.263, UAP-10.265, UAP-10.266, UAP-10.309, UAP-10.497, UAP-10.454, UAP-10.362, UAP-10.398, UAP-10.414, UAP-11.180, UAP-11.212, UAP-14.196, UAP-14.239–3).
Description
A large well known species with marked gradient monognathic and dignathic heterodonty [19]. Upper teeth possess a triangular, high and thin crown that is bent at the rear [19]. Mesial cutting edge has well marked serrations that increase in size towards the apex, but do not reach the tip. The distal cutting edge has larger and less pointed serrations. Root is high and has a prominent lingual protuberance with a clear groove possessing one to several foramina. Lower teeth have a different morphology, with anterior teeth being high and sharp and lateral teeth possessing asymmetrical teeth with posteriorly bent cusps.
Discussion
Throughout the Miocene and early Pliocene H. serra is a cosmopolitan species, occurring more commonly in warmer waters. The Malagasy specimens are smaller than those from the Miocene and Pliocene of North Carolina [25] and so may be from juvenile individuals.
Order Squatiniformes De Buen, 1926
Family Squatinidae Bonaparte, 1838
Genus Squatina Duméril, 1806
Squatina sp.
(Fig 4O)
Description
UAP-10.505: height = 3.4 mm, width = 2.8 mm, thickness = 1.0 mm.
Small tooth with flattened root base. Crown upright, inclined disto-lingually with blade-like shoulders mesial and distal to the main crown. Sharp cusp in the anterior files. The basal face of the root in lateral teeth is flat.
Discussion
Teeth of different Squatina species show very little variation and are difficult, if not impossible, to separate. See Bor et al. [24] and Ward and Bonavia [20] for further discussion. Bor et al. use the name S. subserrata Münster 1846 originally described from the Vienna Basin, for teeth that they figure from the Miocene of the Netherlands. However, considering the distances involved, we feel that open nomenclature is more appropriate.
Order Rajiformes Berg, 1937
Family Rajidae Blainville, 1816
Genus Rostroraja Hulley, 1972
Rostroraja olisiponensis Jonet, 1968
(Fig 5A)
A, Rostroraja olisiponensis UAP-13.016 (12); B-G, Himantura, B-C, UAP-11.311; D-E, UAP-13050; F-G, UAP-14.181; H-I, Myliobatidae indet. UAP-13.035, UAP-14.064. Scale bar equals 1 mm, unless specified in the Figure.
Description
Height = 3.8 mm, width = 2.9 mm, thickness = 2.5 mm.
Rajid tooth with a laterally expanded ovoid crown from which protrudes a lingually inclined conical cusp. Root is raised and broadly expanded mesial-distally.
Discussion
This single tooth corresponds quite well with the type material [33] and those figured by Bor et al. [24]. This species displays a degree of ontogenetic heterodonty with relatively taller cusps present in larger teeth [33]. Bor et al. [24] suggest that this species may be ancestral to the extant white skate Rostroraja alba Lacépède, 1803, which occurs off the coast of east Africa, in the eastern Atlantic from Ireland and England southward round the Cape (South Africa) to central Mozambique [34].
Order Myliobatiformes Compagno, 1973
Family dasyatidae.Jordan, 1888
Genus Himantura Müller & Henle, 1837
Material
Six isolated teeth (UAP-13.050 [lot of 6], UAP-13.050 [lot of 10], UAP-13.050 [lot of 20], UAP-13.050, UAP-14.181–1, UAP-14.215–8).
Description
UAP-13.050 [lot of 6]: Average height = 1.9 mm, width = 1.6 mm, thickness = 0.9 mm. The labial crown is evenly pitted and slightly concave. There is a prominent, coarsely ridged transverse ridge. The lingual crown is smooth with a well-developed median lingual ridge, the base of which is developed, in presumed male specimens, into a small cusp. The root lobes are lingually placed, basally flat and separated by a broad furrow which bears a single foramina. In basal view, the labial visor is relatively broad with a narrow lingual visor.
Discussion
Cappetta [19] comments that many pre-Miocene teeth referred to Dasyatis, may well be representatives of other genera including Himantura. The Nosy Makamby teeth correspond well with those of the Recent species Himantura uarnak Forsskål 1775 figured by Cappetta (2012, Fig 411) [19], which currently inhabits the coast of Madagascar. Himantura has been recorded from the late Miocene Baripada Beds in India (as Dasyatis menoni [35]) and as Himantura sp. from the Pliocene of Italy [36].
Teeth of small-toothed rays are rarely reported unless the locality and sediment is amenable to bulk sampling techniques and thus they are usually underrepresented in faunal lists. It is very likely that many more species, as well as more specimens of groups reported here, will be discovered with further sampling.
Family Myliobatidae Bonaparte, 1838
Myliobatidae indet.
Material
Eight isolated teeth (UAP-13.013, UAP-13.035, UAP-13.060, UAP-13.071, UAP-14.133, UAP-14.166, UAP-14.215–1, UAP-14.064).
Description
Isolated chevrons, occlusal face flat, root polyaulacorhizoid with lingually displaced lobes and grooves.
Discussion
Unless the dentition is partially or wholly complete, myliobatid teeth are generally referred to "Myliobatis sp", where a more accurate determination would usually be "Myliobatidae indet." Isolated and incomplete median teeth of Myliobatis, Rhinoptera, Aetomylaeus, Aetobatus and Pteromylaeus are similar but can be separated by their general proportions, spacing and degree of lingual offset of the root lobes. In the case of Rhinoptera, there is very little lingual displacement in the root lobes, whereas in Aetobatus it is quite marked [19]. It is likely that the three figured teeth are of at least two different genera as their general proportions and lingual root offset differ significantly.
Results and Discussion
Comparisons with other contemporaneous faunas
The shark and ray teeth collected from the sections on Nosy Makamby show a degree of Recent weathering but no indication of having been reworked. Thus it is reasonable to assume that they are the same age as the surrounding sediment. Most species have ranges that span the Miocene, and therefore offer little indication as to the specific age of the deposit. However, the presence of Carcharhinus priscus and Galeocerdo mayumbensis would suggest an early to middle Miocene age. The Miocene fauna described by Priem [37] from Chandane, Mozambique, contains a number of late Eocene species (Carcharhinus frequens Dames, Galeocerdo latidens Agassiz etc.), suggesting that the assemblage is of mixed age and not useful for comparison.
The shark fauna from the Chesapeake Bay is relatively well known [38] but for taphonomic reasons the teeth of rays are particularly rare. Both sharks and rays are relatively abundant in the early Miocene of North Carolina, USA [25] but the smaller sharks and rays are poorly known.
Perhaps the best fossil elasmobranch assemblage to compare with that from Nosy Makamby is that described from the late Miocene Baripada Beds in India [35]. These were originally thought to be early Miocene [39] but are currently thought to be late Miocene based on the occurrence of a short-ranged fossil suid [35]. This fauna, which contains the ubiquitous Miocene elements like Hemipristis, Carcharhinus and Galeocerdo, also contains a number of smaller species which, with a taxonomic review, may be comparable with those from the Madagascan Miocene.
Environment
All shark genera identified occupy the neritic littoral zone, with the majority preferring tropical climates. The apparent absence of sand and mako sharks (Carcharias and Isurus) is unusual as their teeth are usually abundant in inshore Miocene deposits [23][25].
The association of sirenian fossils from the same deposits at Nosy Makamby also supports a nearshore marine, protected and calm environment that possessed sufficiently clear water and low depth. Foraminifera further support this paleoenvironmental interpretation, with groups recovered dominated by miliolids, especially Quinqueloculina [17]. This indicates an inner shelf deposit in a coastal environment, and warm temperature characteristic of a tropical area similar to that reconstructed for the selachian genera. The presence of the invertebrate species Concavus concavus Bronn 1831, also suggests that the medium was continuously subjected to the influence of the tide, which may explain the thick lumachellic deposits. This appears to be characteristic of other Miocene formations near the Mozambique Channel (e.g., Tanzania) [40].
Conclusions
Recent fieldwork on the island of Nosy Makamby, northwestern Madagascar, has produced the first comprehensive description of the island’s Miocene selachians. Of the ten taxonomic groups identified, Otodus, Carcharhinus, Galeocerdo, Rhizoprionodon, Sphyrna, Hemipristis, Squatina, Rostroraja, Himantura and Myliobatidae, six are newly described from Madagascar (Galeocerdo, Rhizoprionodon, Sphyrna, Squatina, Rostroraja and Himantura). This analysis of selachian remains combined with lithological data, and the further presence of sirenian and Concavus concavus fossils supports the age of early to mid Miocene, and suggests that this region was characterized as tropical shallow-water marine. Future work is needed to better understand the precise age, biostratigraphy and paleoenvironment of this unique island.
Acknowledgments
We thank the Ministry of Culture and Ministry of Mines (Madagascar) for permission to conduct this research, and the Department of Paleontology and Biological Anthropology, University of Antananarivo, specifically Haingoson Andriamialison. All necessary permits were obtained for the described study, which complied with all relevant regulations. Thanks to Lydia Rahantarisoa for helpful discussions, and to the field team: Lydia Raharivony, Rachel Razafimbelo, Jean-Luc Raharison, Sitraka Razafisambatra, Mitchell Irwin, Rianala, Sahondra, Sarah Roberts, Daniel Branch, Charlan Boutou, Lydia Razafiarisoa, and also villagers and fishermen of Nosy Makamby. Mr. Vinnie Valle (Florida, USA) donated comparative specimens of Galeocerdo mayumbensis for our study and Dr. Zerina Johanson and Ms. Emma Bernard (London, UK) provided access to the NHM UK, Department of Earth Sciences collections. Ngari Teakle provided important laboratory and technical support. Min Sun, head of the University of Hong Kong’s Department of Earth Sciences, is thanked for supporting JRA’s participation in the 2010 fieldtrip. We greatly appreciate comments and suggestions from Dr. Andrew Farke, Dr. Thodoris Argyriou and Dr. Thomas Reinecke.
Author Contributions
Conceived and designed the experiments: THA TNR AR KES. Analyzed the data: THA TNR DJW JRA KES. Contributed reagents/materials/analysis tools: THA TNR DJW AR KES. Wrote the paper: THA TNR DJW JRA KES.
References
- 1.
Goodman SM, Benstead JP (2003) The Natural History of Madagascar. The University of Chicago Press, Chicago, 1728 pp.
- 2. Melluso L, Sheth HC, Mahoney JJ, Morra V, Petrone CM, Storey M (2009) Correlations between silicic volcanic rocks of the St Mary's Islands (southwestern India) and eastern Madagascar: implications for Late Cretaceous India-Madagascar reconstructions. Journal of the Geological Society 166: 283–294.
- 3. Samonds KE, Godfrey LR, Ali JR, Goodman SM, Vences M, Sutherland MR, et al. (2012) Spatial and temporal arrival patterns of Madagascar's vertebrate fauna explained by distance, ocean currents, and ancestor type. Proceedings of the National Academy of Sciences, USA 109: 5352–5357. pmid:22431643
- 4. Ali JR, Huber M (2010) Mammalian biodiversity on Madagascar controlled by ocean currents. Nature 463: 653–656. pmid:20090678
- 5.
Cooke A, Lutjeharms JRE, Vasseur P (2003) Marine and Coastal Ecosystems; pp. 179–209 in Goodman S. M. and Benstead J. P. (eds.), The Natural History of Madagascar. University of Chicago Press, Chicago.
- 6. Thomson KS (1982) An early Triassic hybodont shark from northern Madagascar. Postilla 186: 1–16.
- 7.
Rabarison JA (1996) Contribution à l’étude des dents isolées des Requins du Crétacé supérieur de la région de Berivotra (Bassin de Majunga, Nord-Ouest de Madagascar). DPAB, Université d’Antananarivo, Antananarivo, 62 p, 12 pl.
- 8. Gottfried MD, Rabarison JA, Randriamiarimanana LL (2001) Late Cretaceous elasmobranchs from the Mahajanga Basin of Madagascar. Cretaceous Research 22: 491–496.
- 9. Priem F (1907a) Note sur les poissons de Madagascar. Bulletin de la Société Géologique de France 7: 462–465.
- 10. Samonds KE, Zalmout IS (2002) New selachian assemblage from the marine Paleogene of Madagascar. Journal of Vertebrate Paleontology 22: 102A.
- 11.
Samonds KE, Wallett LA, Zalmout IS, Andrianavalona TH, Rogers RR, Ward DJ (in prep.) A middle Eocene neoselachian assemblage from nearshore marine deposits, Ampazony, northwestern Madagascar.
- 12. Collignon M, Cottreau J (1927) Paleontologie de Madagascar: Fossils de Miocène marin. Annales de Paléontologie 16: 135–170.
- 13.
Besairie H (1969) Carte géologique [Majunga, No3]. 1:500,000. Service Géologique de Madagasikara.
- 14.
Besairie H (1972) Géologie de Madagascar, Volume I. Les terrains sédimentaires. Tananarive Imprimerie Nationale, Antananarivo, 463 pp., 89 plates.
- 15. Samonds KE, Zalmout IS, Irwin MT, Raharivony LL (2007) Sirenian postcrania from Nosy Mahakamby, Northwestern Madagascar. Journal of Vertebrate Paleontology 27: 139A.
- 16. Charbonnier S, Garassino A, Pasini G (2012) Review of the crabs (Crustacea, Decapoda, Brachyura) from the Miocene of the Mahakamby Island (Mahajanga, NW Madagascar) collected during the Waterlot’s Mission (1922). Geodiversitas 34: 873–881.
- 17. Ramihangihajason TN, Andrianavalona TH, Razafimbelo R, Rahantarisoa L, Ali JR, Samonds KE (2014) Miocene benthic foraminifera from Nosy Makamby and Amparafaka, Mahajanga Basin, northwestern Madagascar. Journal of African Earth Sciences 100: 409–417.
- 18. Ward DJ (1983) Collecting isolated microvertebrate fossils. Zoological Journal of the Linnean Society 82: 245–259, Figs 1–2.
- 19.
Cappetta H (2012) Handbook of Paleoichthyology Chondrichthyes 3E, Mesozoic and Cenozoic Elasmobranchii: teeth. 512 pp., 458 Figs Verlag Dr. Friedrich Pfeil, München.
- 20. Ward DJ, Bonavia CG (2001) Additions to, and a review of, the Miocene shark and ray fauna of Malta. The Central Mediterranean Naturalist 3(3): 131–146, Figs 1–3, tbls. 1–2, pls. 1–2.
- 21. Ameghino F (1901) L'âge des formations sédimentaires de Patagonie. Anales de la Sociedad Científica Argentina, 51: 20–39, 65–91.
- 22. Priem F (1914) Sur les poissons fossiles des terrains tertiaires supérieurs du Sud-Ouest de la France (note complémentaire). Bulletin de la Société Géologique de France 14 (3–4): 118–131.
- 23. Reinecke T, Louwye S, Havekost U, Moths H (2011) The elasmobranch fauna of the late Burdigalian, Miocene, at Werder-Uesen, Lower Saxony, Germany, and its relationships with Early Miocene faunas in the North Atlantic, Central Paratethys and Mediterranean. Paleontos 20: 1–170, 40 text-figures, 3 tables, 101 plates
- 24. Bor T, Reinecke T, Verschueren S (2012) Miocene Chondrichthyes from Winterswijk—Miste, the Netherlands. Palaeontos 21: 1–136, 18 text-figures, 5 tables, 58 plates. pmid:22781086
- 25.
Purdy RW, Schneider VP, Applegate SP, McLellan JH, Meyer RL, Slaughter R (2001) The Neogene sharks, rays, and bony fishes from Lee Creek Mine, Aurora, North Carolina. In: Geology and paleontology of the Lee Creek Mine, North Carolina, III, Clayton E. Ray & David J. Bohaska (eds). Smithsonian Contributions to Paleobiology 90: 71–202, 84 Figs, 1 table.
- 26. Adnet S, Cappetta H, Tabuce R (2010) A new Eocene vertebrate fauna (Selachians and mammals) from southwestern Morocco. Preliminary report, age and palaeobiogeographical implications. Geological Magazine 147(6): 860–870.
- 27. Underwood CJ, Ward DJ, King C, Antar SM, Zalmout IS, Gingerich PD (2011). Shark and ray faunas in the late Eocene of the Fayum Area, Egypt. Proceedings of the Geologists’ Association, London 103: 47–66.
- 28. Müller A (1999) Ichthyofaunen aus dem atlantischen Tertiär der USA. Leipziger geowissenschaften, 9–10: 1–360, 69 fig, 6 tabl., 17 pl.
- 29.
Rathbone J, Rathbone L (2011) Sharks Past and Present. Create Space Independent Publishers, 236 pp.26.
- 30. Argyriou T, Cook TD, Muftah AM, Pavlakis P, Boaz NT, Murray AM (2015) A fish assemblage from an early Miocene horizon from Jabal Zaltan, Libya. Journal of African Earth Sciences 102: 86–101.
- 31. Dartevelle E, Casier E (1959) Les poissons fossiles du Bas-Congo et des régions voisines. Annales du Musée du Congo Belge, Sér. A (Minéralogie Géologie, Paléontologie), 3, 2 (3): 257–568, fig 77–98, pl. 23–39.
- 32. Dartevelle E, Casier E (1943) Les poissons fossiles du Bas-Congo et des régions voisines. Annales du Musée du Congo Belge, Sér. A (Minéralogie Géologie, Paléontologie), 3, 2 (1): 1–200, fig 1–60, pl. 1–16.
- 33. Jonet S (1968) Notes d’Ichthyologie Miocène Portugaise. V–Quelques Batoïdes. Revista da Faculdade de Ciências da Universidade de Lisboa 15(2): 233–258, 3 fig, 1 pl. pmid:11770440
- 34.
Froese R, Pauly D, editors (2015) FishBase. World Wide Web electronic publication. www.fishbase.org, version (02/2015).
- 35. Sahni A, Mehrotra DK (1981) Elasmobranchs from the coastal Miocene sediments of Peninsular India. Biological Memoirs 5: 83–121.
- 36. Cappetta H, Cavallo O (2006) Les selaciens du Pliocene de la region d’Alba (Piémont, Italie Nord-Ouest). Rivista Piemontese di Storia Naturale 27: 33–76, pls 1–10.
- 37. Priem F (1907b) Poissons Tertiaires des possessions africaines du Portugal. Comunicaçóes dos Serviços Geológicos de Portugal 7: 74–79.
- 38.
Kent B (1994). Fossil Sharks of the Chesapeake Bay Region. 146pp. Egan Rees & Boyer Inc. Columbia Maryland, USA.
- 39. Sharma MK, Patnaik R (2010) Coprolites from the Lower Miocene Baripada beds of Orissa. Current Science 99: 804–808. pmid:19603504
- 40. Pickford M (2008) Middle Miocene vertebrate fauna from Pemba Island, Tanzania. South African Journal of Science 104: 231–237.