A non‐aquatic otter (Mammalia,Carnivora, Mustelidae) from the Late Miocene (Vallesian,MN 10) of La Roma 2 (Alfambra,Teruel, Spain): systematics and functional anatomy

A new genus and species of otter‐like mustelid, Teruelictis riparius, is created on the basis of a partial skeleton from the Late Miocene (Vallesian age, MN 10) locality of La Roma 2 (Teruel, Spain), including several postcranial elements, the skull, and the mandible. The combination of a typically lutrine dentition, similar to that of other fossil otters such as Paralutra jaegeri, with a very slender postcranial skeleton, including a long back and gracile long bones and metacarpals, thus lacking any aquatic adaptations, was previously unknown in the fossil record. This mosaic of features strongly suggests the possibility that the aquatic lifestyle of otters could have appeared after the initial development of the distinctive dental morphology of this specialized group of mustelids. © 2013 The Linnean Society of London     

Astragali of Pakicetidae and other early-to-middle Eocene archaeocetes (Mammalia,Cetacea) of Pakistan: locomotion and habitat in the initial stages of whale evolution

Richard Dehm and colleagues of the Bayerische Staatssammlung für Paläontologie und Geologie in Munich made an important collection of early-to-middle Eocene mammals at Ganda Kas in Pakistan during the winter of 1955/56. The genera and species Ichthyolestes pinfoldi and Gandakasia potens were named from this collection. Both are now recognized as early and primitive archaeocete cetaceans. In addition, Dehm’s group collected 16 complete or partial astragali of archaeocetes that were misidentified as artiodactyls. These bring the total number of archaeocete astragali known from Ganda Kas to 28. They separate clearly into four species distinguished by size: from smallest to largest Ichthyolestes pinfoldi Dehm and Oettingen-Spielberg, Pakicetus attocki (West), Gandakasia potens Dehm and Oettingen-Spielberg, and Ambulocetus natans Thewissen et al. Ganda Kas artiodactyls are smaller and rare in comparison. Ichthyolestes and Pakicetus are pakicetid archaeocetes, Gandakasia is presently indeterminate to family, and Ambulocetus is an ambulocetid. Tooth size and astragalus size are highly correlated, corroborating reference of astragali to the first three archaeocete taxa based on teeth. Multivariate morphometric comparison (Auto3Dgm) shows that pakicetid astragali overlap almost completely in shape with those of early artiodactyls. Middle Eocene protocetid astragali are divergent from both. Retention of an astragalus indistinguishable from that of artiodactyls shows that pakicetids are closely related to artiodactyls phylogenetically, but does not make Ichthyolestes and Pakicetus terrestrial or cursorial. Other skeletal elements and bone microstructure indicate that pakicetids were semiaquatic like later protocetids. Tropical riverine and marginal marine facies of the Kuldana Formation are likely habitats for initial stages of the transition from terrestrial artiodactyls to semiaquatic and fully aquatic archaeocetes.     

Vb6 T-cell receptor elements in artiodactyls: conservation and germline polymorphisms

By use of primers specific for human T-cell receptor (Tcr) Vb6 gene elements, a typing system for Tcr Vb variability in several artiodactyl species has been established. The amplified polymorphic locus is homologous to the human Vb6 gene element. Like the human counterpart, the artiodactyl Vb6 element contains a polymorphic intronic simple (gt)_n repeat stretch. Extensive length polymorphism of this simple repeat sequence in some artiodactyls should allow efficient association studies in a multiplex approach, especially including MHC class II genes. On the protein level the Vb regions display little variability in the inter-species comparison among artiodactyls. The amino acid substitutions are not concentrated in the putative complementarity determining regions, suggesting evolutionary conservation. In addition, the simple repetitive element has been preserved in the same genomic location for more than 7×10⁷ years. Similar evolutionary persistence has already been demonstrated for a (gt)_n(ga)_m repeat stretch in the second intron of the MHC-DRB locus. The reasons for these parallel developments in evolution are so far not clear, but they may point to a biological meaning if not function of the intronic simple repeat element.     

Prediction of body weight of fossil Artiodactyla

Many dimensions of the postcranial skeleton of ruminant artiodactyls scale closely with body weight and are therefore potentially useful as predictors of body weight in fossil species. Using 45 dimensions of the skeleton a series of predictive equations was generated based on the scaling relationships of the family Bovidae. As a test of their usefulness these equations were used to predict body weights of a number of living ruminant artiodactyls, and six genera of fossil artiodactyls. For most species body weight estimates within 25° of actual weight were given by the mean of the predicted weights from all measurements except lengths of long bones. While femur length was a reasonable predictor of body weight, lengths of distal long bones were unreliable and should not be used as indicators of relative or absolute body weights. Some non-length measurements are biased in certain taxonomic groups; the possibility of erroneous estimates from such measurements can be reduced by using as many estimators of body weight as are available. No species of artiodactyl tested is so highly modified in all dimensions that all results were erroneous. Subsets of measurements which might be available from a typical fossil fragment also gave reliable results.     

Extinct large colobines from the Plio-Pleistocene of Africa

Three genera and six species of extinct African Plio-Pleistocene Colobinae are discussed. One new genus, Rhinocolobus and three new species, R. turkanaensis, Cercopithecoides kimeui and Paracolobus mutiwa are named. These colobines show a diversity in postcranial and dental morphology not seen among extant species. Rhinocolobus was most similar to extant Colobus in postcranial morphology and had similar high-cusped shearing teeth. Cercopithecoides shows a number of postcranial skeletal features typical of terrestrial cercopithecid species and has lower cusped teeth. Paracolobus, while generally more similar to Rhinocolobus than to Cercopithecoides, is intermediate in some features of its postcranial morphology. The distribution of the various taxa among East and South African sites with different palaeoenvironments is generally consistent with the morphological interpretation. With the exception of Cercopithecoides kimeui, which persisted a little longer, these large colobines disappear from the fossil record about 1.8 million years ago. Their disappearance coincides with an interval of increasing aridity documented at Olduvai Gorge, the Omo Valley, and East Turkana.     

Exceptionally preserved North American Paleogene metatherians: adaptations and discovery of a major gap in the opossum fossil record

A major gap in our knowledge of the evolution of marsupial mammals concerns the Paleogene of the northern continents, a critical time and place to link the early history of metatherians in Asia and North America with the more recent diversification in South America and Australia. We studied new exceptionally well-preserved partial skeletons of the Early Oligocene fossil Herpetotherium from the White River Formation in Wyoming, which allowed us to test the relationships of this taxon and examine its adaptations. Herpetotheriidae, with a fossil record extending from the Cretaceous to the Miocene, has traditionally been allied with opossums (Didelphidae) based on fragmentary material, mainly dentitions. Analysis of the new material reveals that several aspects of the cranial and postcranial anatomy, some of which suggests a terrestrial lifestyle, distinguish Herpetotherium from opossums. We found that Herpetotherium is the sister group to the crown group Marsupialia and is not a stem didelphid. Combination of the new palaeontological data with molecular divergence estimates, suggests the presence of a long undocumented gap in the fossil record of opossums extending some 45Myr from the Early Miocene to the Cretaceous.     

The petrosal and bony labyrinth of Diplobune minor,an enigmatic Artiodactyla from the Oligocene of Western Europe

Anoplotheriinae are Paleogene European artiodactyls that present a unique postcranial morphology with a tridactyl autopodium and uncommon limb orientation. This peculiar morphology led to various hypotheses regarding anoplotheriine locomotion from semiaquatic to partly arboreal or partly bipedal. The petrosal bone, housing the organs of balance, and hearing, offers complementary information to postcranial morphology on the ecology of this uncommon artiodactyl. Here, we investigate the middle ear and bony labyrinth of the small anoplotheriine Diplobune minor based on four specimens from the Early Oligocene locality of Itardies (Quercy, France). A macroscopic study coupled with a μCT scan investigation of the petrosal anatomy provides novel information on the bony labyrinth, stapes, and innervation and vasculature of the inner ear of this enigmatic taxon. The petrosal of D. minor exhibits a mosaic of plesiomorphic characters and peculiar features that shed new light into the anatomy of this poorly studied taxon of an obscure taxonomic clade. We can confidently reject that D. minor was a semiaquatic species based on the petrosal morphology: presence of a large mastoid process and nonpachyostotic tegmen tympani do not support underwater hearing. On the other hand, the average semicircular canal radius points to a slow or medium slow agility for D. minor , and fully rejects it was a fast moving animal, which is congruent with its postcranial anatomy.     

Cytochromeb gene of marine mammals: Phylogeny and evolution

The DNA sequences of the mitochondrial cytochromeb gene of marine mammals (Cetacea, Pinnipedia, Sirenia) were compared with cytochromeb genes of terrestrial mammals including the semiaquatic hippopotamus. The comparison included 28 sequences, representing 22 families and 10 orders. The dugong (order Sirenia) sequence associated with that of the elephant, supporting the Tethytheria clade. The fin whale and dolphin (order Cetacea) sequences are more closely related to those of the artiodactyls, and the comparison suggests that the hippopotamus may be the extant artiodactyl species that is most closely related to the cetaceans. The seal sequence may be more closely related to those of artiodactyls, cetaceans, and perissodactyls than to tethytheres, rodents, lagomorphs, or primates. The cytochromeb proteins of mammals do not evolve at a uniform rate. Human and elephant cytochromeb amino acid sequences were found to evolve the most rapidly, while those of myomorph rodents evolved slowest. The cytochromeb of marine mammals evolves at an intermediate rate. The pattern of amino acid substitutions in marine mammals is similar to that of terrestrial mammals.     

A hominoid distal tibia from the Miocene of Pakistan

A distal tibia, YGSP 1656, from the early Late Miocene portion of the Chinji Formation in Pakistan is described. The fossil is 11.4 million years old and is one of only six postcranial elements now assigned to Sivapithecus indicus. Aspects of the articular surface are cercopithecoid-like, suggesting some pronograde locomotor activities. However, YGSP 1656 possesses an anteroposteriorly compressed metaphysis and a mediolaterally thick medial malleolus, ape-like features functionally related to orthograde body postures and vertical climbing. YGSP 1656 lacks specializations found in the ankle of terrestrial cercopithecoids and thus Sivapithecus may have been primarily arboreal. Nevertheless, the morphology of this tibia is unique, consistent with other interpretations of Sivapithecus postcranial functional morphology that suggest the locomotion of this ape lacks a modern analog. Based on the limited postcranial remains from S. indicus, we hypothesize that this taxon exhibited substantial body size dimorphism.     

Plio-Pleistocene cercopithecids from Kanam East, western Kenya

This paper describes cercopithecid craniodental and postcranial fossils recovered by L. S. B. Leakey at Kanam East, Kenya during the early 1930s. These fossil monkeys have been generally assumed to have been derived from early Pliocene horizons, but their exact geographical and stratigraphical provenience is unknown. Although the question of the evolutionary significance of these specimens must await the recovery of more securely dated material from Kanam East, some general conclusions can be drawn concerning their taxonomic affinities and paleobiology. Based on comparative studies of the craniodental material, at least three extant genera are represented—Colobus,Lophocebus, andCercopithecus. The postcranial fossils include a number of hindlimb specimens, as well as the manubrium of a sternum and a caudal vertebra. Identification of the postcranial remains to particular genera is not possible, but they are similar in morphology to modern arboreal and semiterrestrial cercopithecid monkeys of small to medium size. It is evident that Kanam East had a diverse cercopithecid community, similar to those found today in forested and woodland habitats, and this may be of some significance in reconstructing the paleoecology of the site. Because the fossil record of most extant cercopithecid genera is rather sparse at Plio-Pleistocene sites in Africa, Kanam East represents one of only a few sites that has yielded material that can be assigned toColobus,Lophocebus, orCercopithecus. The fossil monkeys from the site, therefore, provide additional evidence to help reconstruct the paleobiology, as well as the patterns of species diversity and community structure that characterized the cercopithecid radiation during the Plio-Pleistocene.     

A new primitive alligatorine from the Eocene of Thailand: relevance of Asiatic members to the radiation of the group

Despite the report of fragmentary remains from China, the fossil record of primitive Alligatorinae is unbalanced with most of its members reported from North America and Europe. Here, we describe cranial, mandibular, and some postcranial elements of a new alligatorine taxon from the Late Eocene of Krabi Basin, southern Thailand. Krabisuchus siamogallicus gen. et sp. nov. was a small animal probably not surpassing 2 m in total length. Despite deformation, the remains show a dorsally elevated cranium similar to Arambourgia gaudryi and Osteolaemus tetraspis. The new alligatorine is characterized by a very short snout and a blunt dentition in the posterior region. Krabisuchus siamogallicus is the first fossil alligatorine from Asia to be incorporated into cladistic analysis. Results indicate a close relationship of the newtaxon to Procaimanoidea, Arambourgia gaudryi, and Allognathosuchus polyodon, all of them being sister groups to the Alligator clade. Alligatorine were widespread as early as the Late Eocene across the northern hemisphere. Scenarios of alligatorine dispersal during the Palaeogene are discussed in comparison with the European and North American alligatorine fossil record. Basal alligatorines were probably land‐dwelling animals contrary to modern‐day crocodylians. Such a mode of life may have allowed this group to colonize vast territories, especially during periods of global warm climates. © 2010 The Linnean Society of London, Zoological Journal of the Linnean Society, 2010, 158 , 608–628.     

Relationships of Cetacea (Artiodactyla) Among Mammals: Increased Taxon Sampling Alters Interpretations of Key Fossils and Character Evolution

Background

Integration of diverse data (molecules, fossils) provides the most robust test of the phylogeny of cetaceans. Positioning key fossils is critical for reconstructing the character change from life on land to life in the water.

Methodology/Principal Findings

We reexamine relationships of critical extinct taxa that impact our understanding of the origin of Cetacea. We do this in the context of the largest total evidence analysis of morphological and molecular information for Artiodactyla (661 phenotypic characters and 46,587 molecular characters, coded for 33 extant and 48 extinct taxa). We score morphological data for Carnivoramorpha, †Creodonta, Lipotyphla, and the †raoellid artiodactylan †Indohyus and concentrate on determining which fossils are positioned along stem lineages to major artiodactylan crown clades. Shortest trees place Cetacea within Artiodactyla and close to †Indohyus, with †Mesonychia outside of Artiodactyla. The relationships of †Mesonychia and †Indohyus are highly unstable, however - in trees only two steps longer than minimum length, †Mesonychia falls inside Artiodactyla and displaces †Indohyus from a position close to Cetacea. Trees based only on data that fossilize continue to show the classic arrangement of relationships within Artiodactyla with Cetacea grouping outside the clade, a signal incongruent with the molecular data that dominate the total evidence result.

Conclusions/Significance

Integration of new fossil material of †Indohyus impacts placement of another extinct clade †Mesonychia, pushing it much farther down the tree. The phylogenetic position of †Indohyus suggests that the cetacean stem lineage included herbivorous and carnivorous aquatic species. We also conclude that extinct members of Cetancodonta (whales + hippopotamids) shared a derived ability to hear underwater sounds, even though several cetancodontans lack a pachyostotic auditory bulla. We revise the taxonomy of living and extinct artiodactylans and propose explicit node and stem-based definitions for the ingroup.     

Phylogenetic Relationships Between the Orders Artiodactyla and Cetacea: A Combined Assessment of Morphological and Molecular Evidence

A character analysis of selected conservative morphological traits from extant and fossil artiodactyls and cetaceans was combined with a similar analysis of conservative nucleotide positions from the complete mitochondrial cytochrome b sequences of available extant artiodactyls, cetaceans, sirenians, perissodactyls, and other mammals. This combined analysis focuses on the evidence that supports conflicting hypotheses of artiodactyl monophyly, including the affinities of hippopotamids and the monophyly or paraphyly of odontocete cetaceans. Highly conserved morphological traits of the astragalus and deciduous dentition provide strong corroboration of artiodactyl monophyly, including extant and fossil hippopotamids. In contrast, cytochrome b gene sequences are incapable of confirming this monophyly, due to excessive homoplasy of nucleotide and amino acid traits within extant Eutheria. In like manner, highly conserved and uniquely derived morphological features of the skull and auditory regions provide robust corroboration of Odontoceti monophyly, including extant and fossil physeteroids. Several nucleotide similarities do exist between physeteroids and mysticetes; however, most are either silent third-position transversions or occur also in two or more odontocete families. We suggest that increased taxon sampling, combined with functional considerations of amino acids and their secondary structure in protein-coding genes, are essential requirements for the phylogenetic interpretations of molecules at higher taxonomic levels, especially when they conflict with well-supported hypotheses of mammalian phylogeny, corroborated by uniquely derived morphological traits from extant and fossil taxa.     

PLEISTOCENE BIRD FAUNA FROM BIR TARFAWI (EGYPTIAN WESTERN DESERT)

Bocheński, Z. 1991. Pleistocene bird fauna from Bir Tarfawi (Egyptian Western Desert). Ostrich 62: 29–34.

At Bir Tarfawi, an archaeological site in the Egyptian Sahara dated to about 135000 years (before present), 202 bone fragments were identified as belonging to 24 bird species or genera. Most of the material is apparently from owl pellets. The birds represent aquatic and terrestrial forms and include different zoogeoraphical elements; Afrotropical species such as Phalacrocorax africanus, Gyps africanus, cf. Neotis denfami, Fulica cristata, Oena capensis and Corvus albus, as well as Indo-African species such as cf. Bubulcus ibis and Turnix cf. sylvatica. The fossil bird remains as well as those of other vertebrates indicate that the Pleistocene “Grey Lake 2” was surrounded by a mosaic of different aquatic and terrestrial biotopes.     

Endocranial Volume of Mid-Late Eocene Archaeocetes (Order: Cetacea) Revealed by Computed Tomography: Implications for Cetacean Brain Evolution

The large brain of modern cetaceans has engendered much hypothesizing about both the intelligence of cetaceans (dolphins, whales, and porpoises) and the factors related to the evolution of such large brains. Despite much interest in cetacean brain evolution, until recently there have been few estimates of brain mass and/or brain–body weight ratios in fossil cetaceans. In the present study, computed tomography (CT) was used to visualize and estimate endocranial volume, as well as to calculate level of encephalization, for two fully aquatic mid-late Eocene archaeocete species, Dorudon atrox and Zygorhiza kochii. The specific objective was to address more accurately and more conclusively the question of whether relative brain size in fully aquatic archaeocetes was greater than that of their hypothesized sister taxon Mesonychia. The findings suggest that there was no increase in encephalization between Mesonychia and these archaeocete species.     

Postcranial morphology,functional adaptations and palaeobiology of Callistoe vincei,a predaceous metatherian from the Eocene of Salta,north‐western Argentina

Abstract: Callistoe vincei Babot et al., 2002 is a Paleogene borhyaenoid known from exceptionally complete postcranial elements, which provides rare information about the anatomy and evolutionary history of metatherian predators during the South American Cenozoic. The axial skeleton of Callistoe is characterized by the peculiar transverse processes of the cervical vertebrae emphasizing lateral instead of sagittal traction. There is no clavicle and eighteen thoracolumbar vertebrae, of which only five are lumbars. The shoulder and elbow joints suggest movements restricted to parasagittal flexion/extension that are consistent with primarily terrestrial locomotion, as is also emphasized in Borhyaena tuberata and Lycopsis longirostrus. On the manus, the pollex is not reduced and the ungual phalanges indicate very long claws, similar to those observed in some extant digging taxa. This feature is unique to C. vincei among borhyaenoids. The knee joint is characterized by the presence of ossified patellae but shallow femoral trochleae. This joint suggests that the leg was nearly parasagittal, a position also inferred for Borhyaena. The astragalus shape is consistent with parasagittal flexion/extension, as in all Miocene–Pliocene borhyaenoids. The hind foot is characterized by reduced claws in comparison with the manus as well as the slenderness of the first and fifth digits, another peculiarity of C. vincei. The habitat of Callistoe was a temperate humid forest and according to the known fossil record, Callistoe was the largest mammalian predator of its time, sharing the predator ecological niche with crocodiles.     

Human evolution

The common ancestor of modern humans and the great apes is estimated to have lived between 5 and 8 Myrs ago, but the earliest evidence in the human, or hominid, fossil record is Ardipithecus ramidus, from a 4.5 Myr Ethiopian site. This genus was succeeded by Australopithecus, within which four species are presently recognised. All combine a relatively primitive postcranial skeleton, a dentition with expanded chewing teeth and a small brain. The most primitive species in our own genus, Homo habilis and Homo rudolfensis, are little advanced over the australopithecines and with hindsight their inclusion in Homo may not be appropriate. The first species to share a substantial number of features with later Homo is Homo ergaster, or ‘early African Homo erectus’, which appears in the fossil record around 2.0 Myr. Outside Africa, fossil hominids appear as Homo erectus-like hominids, in mainland Asia and in Indonesia close to 2 Myr ago; the earliest good evidence of ‘archaic Homo’ in Europe is dated at between 600–700 Kyr before the present. Anatomically modern human, or Homo sapiens, fossils are seen first in the fossil record in Africa around 150 Kyr ago. Taken together with molecular evidence on the extent of DNA variation, this suggests that the transition from ‘archiac’ to ‘modern’ Homo may have taken place in Africa.     

Brief communication: New primate remains from the Miocene of Namibia,Southern Africa

Miocene primates from southern Africa are extremely rare. For this reason we wish to place on record several interesting new fossil primate specimens recently recovered from the Miocene sites of Berg Aukas and Harasib in the Otavi Mountain region of northern Namibia. The new finds consist of a virtually complete atlas vertebra from Berg Aukas attributable to the hominoid Otavipithecus namibiensis and two teeth and four postcranial fragments from Harasib referrable to Cercopithecoidea. The atlas vertebra exhibits anatomical characteristics intermediate between those of modern cercopithecoids and hominoids which may be indicative of a transition from pronograde to orthograde postures. The cercopithecoid remains show that the earliest Old World monkeys known from southern Africa were small, approximately the size of vervet monkeys. These new specimens are important because they provide the first evidence relating to possible positional behaviors of Otavipithecus and the earliest fossil record of cercopithecoids from southern Africa. © 1996 Wiley-Liss, Inc.