New material of Carnivora (Mammalia) from the Late Miocene of Axios Valley,Macedonia, Greece

A new collection of carnivores from the Late Miocene deposits of Axios Valley, Macedonia, Greece was collected in 2004–2009 at the localities named Xirochori 1 (XIR) and Ravin de la Pluie (RPl), dated to the Late Vallesian (MN 10), as well as at Ravin des Zouaves 5 (RZO), dated to the Early Turolian (MN 11). The studied material is described and compared morphologically and biometrically with other materials from Greece and its neighboring area. The following species are determined: XIR: Dinocrocuta sp.; RPl: Eomellivora wimani, Adcrocuta eximia leptoryncha, ?Hyaenictis sp., Metailurus parvulus; RZO: Plioviverrops orbignyi, Machairodus giganteus. This collection is interesting because it includes the upper deciduous dentition of A. eximia and Dinocrocuta, which are only known from limited material until now, especially the latter taxon. E. wimani is recognized for the first time in Greece and the Balkans, while M. parvulus is identified for the first time in the Vallesian of Greece. The possible presence of Hyaenictis in RPl is the first indication of its presence in the Vallesian. The guild structure diagrams of the carnivore fauna from the three studied localities provide some indications of their palaeoenvironment, which fits quite well with the results of previous studies on the palaeoenvironments of these localities and of the wider Eastern Mediterranean region.     

New material of Ouranopithecus macedoniensis from late Miocene of Macedonia (Greece) and study of its dental attrition

During the last five years our continued excavations in the known late Miocene mammal localities of Macedonia (Greece) provided several new specimens of the hominoid primate Ouranopithecus macedoniensis. This new material includes maxillary and mandibular remains and it is described and compared to the old material of Ouranopithecus in the present article. The material of Ouranopithecus from the three known localities “Ravin de la Pluie” (RPl), “Xirochori 1” (XIR) and “Nikiti 1” (NKT) includes a complete series of tooth rows representing all wearing stages. Thus, the study of the dental wear of Ouranopithecus upper and lower teeth is studied and compared to that of the recent hominoids Gorilla and Pan, as well as to Australopithecus afarensis. The latter species is well known by a series of tooth rows of different wearing stages. The canine’s attrition of Ouranopithecus has a more derived pattern than that of the recent hominoids (Gorilla and Pan) and less derived than A. afarensis. The p3 of Ouranopithecus has similar attrition to that of A. afarensis, the attrition of the molars in Ouranopithecus, A. afarensis and Pan follows a similar pattern, while in Gorilla it is different.     

Carnivores from the early/middle Miocene locality of Antonios (Chalkidiki, Macedonia, Greece)

The mammal locality of Antonios is one of the few known early-middle Miocene ones of Greece with large mammals. It is situated in Chalkidiki Peninsula (Macedonia, Greece) and includes both small and large mammals. The study of the carnivores found in Antonios indicates the presence of the following taxa: Proputorius cf. P. sansaniensis, Protictitherium gaillardi, Protictitherium cf. P. crassum, Percrocuta sp., Percrocutidae indet. and Pseusaelurus romieviensis. The material of each taxon is described, compared with other material from various Eurasian localities and determined. The species P. cf. sansaniensis and P. romieviensis are traced for first time in Eastern Mediterranean, while Percrocuta for first time in Greece. The presence of the other carnivoran taxa in the Antonios fauna is also interesting as they are recognized in older stratigraphic levels enriching our knowledge about their stratigraphic distribution. The carnivores of Antonios cannot offer significant data for the dating of the fauna but its age is discussed using the data coming from the carnivores as well as those from older studies of the micromammals and suoids.     

Interactions between a satellite bacteriophage and its helper

P4 is a satellite phage which relies on a helper such as P2 to supply the gene products necessary for particle construction and cell lysis (Six, 1975). P4 can activate the expression of late genes from a P2 helper phage, using a mechanism different from that employed by the helper. In the presence of P4, replication of P2 DNA is not required for late gene expression (Six & Lindqvist, 1971), and the polar effects of P2 amber mutations are suppressed.Despite its small size P4 codes for two late proteins as well as two early proteins. One of the P4 early proteins is that the product of gene α. The expression of P4 late genes is stimulated by the helper phage. Thus the P2 and P4 chromosomes exhibit reciprocal transactivation.The presence of the P4 genome causes the P2 head proteins to form a head smaller than that found after infection by P2 (Gibbs et al., 1973). P4 late proteins associate with head-like structures and may determine the small size of P4 heads.     

New material of Chalicotheriidae (Perissodactyla,Mammalia) from the Late Miocene of Axios Valley,Macedonia (Greece) with the description of a new species

Chalicotheriids are rare in the late Miocene mammal localities of Axios Valley, Macedonia (Greece). The new campaign of excavations, since 1972, has provided some specimens, which are studied in this article. They are coming from two different localities. The late early Vallesian locality of Pentalophos 1 (PNT) has provided a skull and a mandible of an Ancylotherium. The morphological characters of the PNT material as the small size, the long snout, the shallow mandibular corpus, the strong cingulum in the teeth, the short tooth rows and the short M3/m3 indicate that it differs from the known Turolian species A. pentelicum and allow the erection of a new species, named Ancylotherium hellenicum n. sp., which can be used as a biostratigraphic marker of the Vallesian. The middle Turolian locality Prochoma 1 (PXM) has provided only one M3, which is determined to the chalicotheriine Anisodon macedonicus. This species was earlier described from the middle Turolian locality Vathylakkos 3 (VAT) and the late Turolian one of Dytiko 3 (DKO) of Axios Valley. The biogeography and biostratigraphy of the late Miocene chalicotheres of the Greco-Iranian Palaeoprovince (GRIP), as well as their palaeoecology are also discussed. The common chalicothere of GRIP is A. pentelicum, expanded from the Balkans to Afganistan and ranging stratigraphically from the early to the late Turolian. Chalicotherium goldfussi is certainly present in GRIP and it also ranges from the early to the late Turolian; its possible Vallesian occurrence needs confirmation. The other two late Miocene chalicotheres of GRIP A. macedonicus and Kalimantsia bulgarica are restricted to the Turolian of the Balkan Peninsula.     

Milk molars or extra premolars in Mesotheriinae (Mesotheriidae,Notoungulata): New insights into an old controversy

A recently recovered specimen of Mesotheriinae (Mesotheriidae, Notoungulata) from the late Miocene-early Pliocene of La Rioja Province (Argentina), CRILAR Pv 433, corresponds to an individual with three upper premolars, which appears to be an “anomaly” among mesotheriines. The detailed study of this specimen, however, brings up an old controversy on the interpretation of different mesotheriine specimens with three upper or two lower premolars. After being described as different taxa, these were later considered to be juvenile representatives of other known species. The three upper or two lower teeth were interpreted as the milk molars DP2–4 and dp3–4, respectively, which would be replaced in adult life by two upper (P3–4) and one lower (p4) permanent premolars. The new material leads us to set up a different interpretation. In our opinion, all these specimens actually preserve the permanent dentition, corresponding to different ontogenetic stages of more or less young individuals. This consideration implies the necessity of a deep systematic revision of the whole subfamily, keeping in mind this new point of view and the ontogenetic variation within a species. Therefore, the presence of P2/p3 is not enough to define a different taxon at this moment. Pending this taxonomic revision, the dental morphology of CRILAR Pv 433 resembles both Typotheriopsis (e.g., upper premolars with one labial sulcus) and Pseudotypotherium (e.g., P4 with lingual groove, wide median lobe of M3) as these two late Miocene genera are currently characterized. Furthermore, P2/p3 could be expelled soon in the lifetime of individuals, and even the presence of P2/p3 could be a variable character within the same taxon; if so, this might reflect an evolutionary trend to the loss of a dental element within mesotheriines, but the revision of a large sample is necessary to support or reject these hypotheses.     

Origines du peuplement mammalien en Afrique du Nord durant le miocène terminal

The late Miocene North African mammalianassemblage is considered here from three viewpoints: survivals, extinctions, and immigrations. The Eurasiatic affinities of the large mammals slightly prevail over the Ethiopian affinities. Amongst the North African large mammals, 4 to 8 taxa are Eurasiatic immigrants, while 4 to 6 are of Subsaharian origin. Contrarily, the micromammalian fauna is highly endemic, with only one species, a murid (Paraethomys miocaenicus), considered here as being related to an Asiatic form (Karnimata darwini). Our study of Eurasian and African Miocene faunas reveals that during the late Astaracian-early Turolian interval, the Saharo-Arabic belt permitted very little latitudinal faunal exchanges. However, during the middle and late Turolian such faunal exchanges became frequent. The micromammal record unequivocally indicates that a brief period of faunal exchange occurred between Africa and western Europe at the end of the Miocene, corresponding with the Messinian Salinity Crisis. The increased intercontinental faunal exchange between Africa and Eurasia during the late Miocene coincides with, and counterbalances the extinction of more than 10 taxa at the Mio/Pliocene boundary.     

A new elasmothere (Perissodactyla, Rhinocerotidae) from the late Miocene of the Linxia Basin in Gansu, China

Ningxiatherium euryrhinus sp. nov. is a relatively large elasmothere rhino from the Linxia Basin in northwestern China found in the early Bahean, which corresponds to the early Vallesian (MN 9), ca. 11.1 Ma. It is much larger than the extant Ceratotherium simum and has a single horn. Ningxiatherium is similar to the late Miocene Parelasmotherium from Gansu and Shanxi, but differs in having partially ossified nasal septum, terminal nasal horn boss, shallower nasal notch above the P3/P4 boundary, and much shorter premolars. N. euryrhinus sp. nov. differs from N. longirhinus from the late Miocene of Zhongning, Ningxia in northwestern China by its larger size, relatively wider nasals, shallower nasal notch, and sub-quadrangular occlusal surface of M3. In the Linxia Basin, the other early late Miocene (Bahean or Vallesian) elasmotheres are known from complete skulls or isolated teeth. They include two genera and three species: Parelasmotherium linxiaense, P. simplum, and Iranotherium morgani. They lack a nasal septum, but Ningxiatherium has one. The age of N. euryrhinus is early late Miocene based on direct association with biochronologic indicator taxa, such as Dinocrocuta gigantea, Hipparion dongxiangense, and Chilotherium primigenius. N. euryrhinus is more primitive than N. longirhinus sp. nov. in having a sub-quadrangular M3, a shallower nasal notch, and the presence of DP1 in adults.     

Early Miocene Carnivora of Aktau Mountains, South Eastern Kazakhstan

New material is described ofAktaucyon brachifacialis n. gen., n. sp. (Amphicyonidae, Daphoeninae),Phoberocyon (Cinctocyon n. subgen.)akhmetievi n. sp. (Ursidae, Hemicyoninae), and Mustelidae indet. from the lower Miocene deposits of the middle Member of the Chul’adyr Formation in the Aktau Mountains, Ili Basin, SE Kazakhstan. Daphoenine remnants are reported from Asia for the first time. They are assigned to the new tribe Aktaucyonini, which are middle to large-sized amphicyonids with a shortened facial region; a reduced P/1; enlarged upper canines; an enlarged P4/ with a welldeveloped protocone, paracone and parastyle blade; enlarged M1/ and M2/, which have conical protocones, symmetrical talons, and reduced hypoconules; and an M2/ that is transversely widened with a greatly reduced metacone. The phoberocyonine described here is the first reported from Kazakhstan and for the whole western part of Central Asia. The composition of the carnivore fauna resembles that from Shanwang, eastern China (MN 4–5).     

New adapiform primate of Old World affinities from the Devil's Graveyard Formation of Texas

Most adapiform primates from North America are members of an endemic radiation of notharctines. North American notharctines flourished during the Early and early Middle Eocene, with only two genera persisting into the late Middle Eocene. Here we describe a new genus of adapiform primate from the Devil’s Graveyard Formation of Texas. Mescalerolemur horneri, gen. et sp. nov., is known only from the late Middle Eocene (Uintan) Purple Bench locality. Phylogenetic analyses reveal that Mescalerolemur is more closely related to Eurasian and African adapiforms than to North American notharctines. In this respect, M. horneri is similar to its sister taxon Mahgarita stevensi from the late Duchesnean of the Devil’s Graveyard Formation. The presence of both genera in the Big Bend region of Texas after notharctines had become locally extinct provides further evidence of faunal interchange between North America and East Asia during the middle Eocene. The fact that Mescalerolemur and Mahgarita are both unknown outside of Texas also supports prior hypotheses that low-latitude faunal assemblages in North America demonstrate increased endemism by the late middle Eocene.     

A late early to early middle Eocene mammal assemblage from Bayan Ulan (Inner Mongolia,China): Implication for the reassessment of the Arshantan Asian Land Mammal Age

Paleogene mammal localities of North China are particularly well represented in the Erlian Basin, Inner Mongolia. Among them, the locality of Bayan Ulan is most famous for its late Paleocene Gashatan fauna. However, the younger Arshantan fauna of the same site is not well known, since no extensive study has been done so far. Here, we present a small mammal assemblage based on dental and tarsal material from a new Arshantan collection retrieved from the red beds of the late early to early middle Eocene Arshanto Formation at Bayan Ulan. It consists of at least six different taxa: the basal lagomorph Dawsonolagus antiquus, the large pantodont Pantolambdodon sp., the tapiroid Schlosseria magister, and the rhinocerotoids Hyrachyus crista and Rhodopagus guoi nov. sp. The assemblage is dominated by perissodactyls, especially Lophialetidae and Hyracodontidae. For the first time, p4-m1 of Dawsonolagus antiquus, tarsal material from Pantolambdodon sp., and lower dentition and tarsals of Hyrachyus crista are described and illustrated. Unlike other described Arshantan faunas, the Bayan Ulan Arshantan mammal assemblage has been collected exclusively from a single locality, which contributes to the reassessment of the misunderstood Arshantan Asian Land Mammal Age.     

Identification of specific let-7 microRNA binding complexes in Caenorhabditis elegans

Little is known about the protein complexes required for microRNA formation and function. Here we used native gel electrophoresis to identify miRNA ribonucleoprotein complexes (miRNPs) in Caenorhabditis elegans. Our data reveal multiple distinct miRNPs that assemble on the let-7 miRNA in vitro. The formation of these complexes is affected but not abolished by alg-1 or alg-2 null mutations. The largest complex (M*) with an estimated molecular mass of >669 kDa cofractionates with the known RISC factors ALG-1, VIG-1, and TSN-1. The M* complex and two complexes, M3 and M4, with similar molecular weights of ~500 kDa, also assemble on all other miRNAs used in our experiments. Two smaller complexes, M1 (~160 kDa) and M2 (~250 kDa), assemble on the members of the let-7 miRNAs family but not lin-4 or mir-234, and their formation is highly dependent on specific sequences in the 5′ seed region of let-7. Moreover, an unidentified protein, p40, which only appears in the M1 and M2 complexes, was detected by UV triggered cross-linking to let-7 but not to lin-4. The cross-linking of p40 to let-7 is also dependent on the let-7 sequence. Another unidentified protein, p13, is detected in all let-7 binding complexes and lin-4 cross-linked products. Our data suggest that besides being present in certain large miRNPs with sizes similar to reported RISC, the let-7 miRNA also assembles with specific binding proteins and forms distinct small complexes.     

Comparison of adrenocortical responses to acute stress in lowland and highland Eurasian tree sparrows (Passer montanus): similar patterns during the breeding, but different during the prebasic molt

Previous studies indicate most free-living avian species in both extreme and temperate environments seasonally modulate the adrenocortical responses to acute stress, and those breeding in harsh environments always express reduced adrenocortical responses, which may allow them to obtain maximal reproductive success. However, recent investigations showing a human commensal species, house sparrows (Passer domesticus), expressed similar corticosterone (CORT) responses in both benign and harsh environments. In this study, focusing on another human commensal species, Eurasian tree sparrows (P. montanus), we examined the adrenocortical response to acute stress in lowland populations, among the early and late breeding, the prebasic molt, and the wintering stages, and compared them with previously published data from populations on the Tibetan Plateau. Our results show: (1) similar to highland Eurasian tree sparrows, lowland populations show no differences in baseline CORT levels among life history stages, and the stress-induced CORT (maximal CORT, total and corrected integrated CORT) levels are lower during the early breeding and the prebasic molt stages than those in the late breeding and the wintering stages; (2) highland Eurasian tree sparrows show stronger adrenocortical responses during the prebasic molt stage than lowland populations, whereas there are no differences between the early and the breeding stages (except for maximal CORT). Our results suggest that Eurasian tree sparrows from both harsh and benign environments have similar patterns of adrenocortical responses in the breeding stage, whereas they are different in the prebasic molt stage. In highland birds, the increased maximal CORT levels during the late breeding and the small increases in adrenocortical responses during the prebasic molt are interesting but remain unexplained.     

Mustelids from Sackdilling Cave (Bavaria,Germany) and their biostratigraphic significance

Sackdilling Cave is a karst fissure filled with a fossiliferous breccia including abundant fossil remains, mostly snails and small mammals. The taxonomic status of mustelid remains from this cave was previously regarded as controversial and, consequently, different authors listed different species from the locality. A detailed revision of the material shows the presence of five mustelid species: Meles sp., Martes vetus, Mustela strandi, Mustela palerminea, and Mustela praenivalis. Among them, especially noteworthy is the presence of the type specimen of Martes vetus. The Sackdilling holotype resembles Martes foina and differs from that of Martes martes in a short and broad viscerocranium; wide and less extended forward incisor row; compressed, short and wide temporal region; large, strongly inflated and convex tympanic bullae; and narrow P3 with weak lingual bulge. Some dental characters are specific for Martes vetus and show some intermediate values between Martes foina than Martes martes. Among them are the P4 protocone length and the M1 trigon length. The revised material from Sackdilling Cave of Mustela palerminea and Mustela praenivalis was compared with that from other Early and early Middle Pleistocene sites of Europe and showed the presence of intermediate characters. Subsequently, based on the entire mustelid assemblage and other faunal elements (mainly rodents), the age of this fauna was estimated as ca. 0.9–0.7 Ma.     

The Iberian record of the puma-like cat Puma pardoides (Owen, 1846) (Carnivora,Felidae)

Fossil puma-like cats (Puma pardoides) are recorded from several Late Pliocene to Early Pleistocene Eurasian localities, but the interpretation of the phylogenetic relationships between them and the extant puma (Puma concolor) remains controversial. In the past, extinct puma-like cats have been classified into several genera and species, and a close relationship with both pumas (Puma concolor) and snow leopards (Uncia uncia) has been suggested. Here, we describe the fossil remains of puma-like cats from the Iberian Peninsula. These remains (from the localities of La Puebla de Valverde, Cueva Victoria and Vallparadís) cover the whole known chronological distribution of this species in Eurasia. Although there are dentognathic similarities with U. uncia, the Iberian remains of P. pardoides most closely resemble the extant P. concolor. It is concluded that P. pardoides is closely related to living pumas, which supports a likely Eurasian origin of the puma lineage.     

The scimitar-toothed cat Machairodus aphanistus (Carnivora: Felidae) in the Vallès-Penedès Basin (NE Iberian Peninsula)

Here, we revise all the published and unpublished scimitar-toothed cat remains from the Vallès-Penedès Basin (NE Iberian Peninsula), in order to confirm their taxonomic attribution to Machairodus aphanistus as well as to provide more precise information about its chronological distribution in this basin. The studied material (including dentognathic as well as postcranial remains) comes from the following localities: Can Mata indeterminate (late MN7+8 or MN9), Creu Conill 22 (MN9), Can Poncic 1 (MN9), Can Llobateres 1 (MN9), Santiga (MN9), La Tarumba 1 (MN10), Viladecavalls (MN10), Ronda Oest Sabadell ROS-D3 (MN10), and Torrent de Febulines (MN10). Most of the studied material fits well with the morphologic and metrical features characteristic of the Vallesian species M. aphanistus, with the exception of the remains from Creu Conill 22 (an undescribed partial P4 formerly attributed to this taxon), which belongs in fact to a medium-sized hyaenid. From a biostratigraphic viewpoint, the removal of the Creu Conill material from the hypodigm of M. aphanistus has important implications, because this locality (11.1 Ma) was considered to record the first appearance datum of this taxon in the Vallès-Penedès Basin. However, the report of a previously unpublished talus from Can Mata (late MN7+8 or MN9) indicates that this taxon was present in this basin at least by the earliest Vallesian. Therefore, our results indicate that the first appearance datum of Machairodus in the Vallès-Penedès Basin might be somewhat younger than previously assumed, although dating uncertainties for the Can Mata remains preclude a more precise assessment. In contrast, the new mandibular remains from ROS-D3 (MN10) are likely coeval with those from La Tarumba 1, with the last appearance datum of M. aphanistus in the Vallès-Penedès Basin corresponding to Torrent de Febulines (ca. 9.1 Ma). The postcranial material described from various Vallès-Penedès localities further indicates that M. aphanistus displayed less cursorial adaptations than its purported descendant Homotherium.     

Identification of natural hybrids in Korean Phragmites using haplotype and genotype analyses

To elucidate natural hybridization of Korean Phragmites, we collected Phragmites plants from 29 regions in South Korea. Haplotypes of the samples, which were determined using two known chloroplast intergenic sequences in this study, were combined with previously known haplotypes. Phylogenetic analysis identified that 30 Korean Phragmites were grouped with two different haplotypes, ‘P’ or ‘W’, respectively, indicating that introduced Phragmites samples from other continents were not present in Korea. The vast majority (26) of the 27 test samples were grouped with the P haplotype, while the E4 sample and the three control Phragmites japonicus samples were grouped with haplotype W. Interestingly, parsimony network analysis revealed that Phragmites australis in Korea might have originated from various regions including Busan (S1), Icheon (M2), and Ansan (W2). Genotype analysis using the PhaHKT1 nuclear gene identified the M3 sample as Phragmites japonicus. For the first time, we found two hybrids (E4 and M3) in the wild by haplotype and genotype analyses, implying that the phenotype of Phragmites australis might be dominant in the hybrids. In summary, we suggest that hybrid speciation might be an important factor in the genetic diversity of Korean Phragmites.