Some factors influencing the microdistribution of a population of spined loach,Cobitis taenia (L.)

Monthly observations (October 1972–October 1974) of a natural population of spined loach, Cobitis taenia (L.), in the River Great Ouse at Newport Pagnell indicated a patchy microdistribution, which varied seasonally. The distribution was clearly linked to the areas of fine substrate, which altered seasonally in position.Flow rates measured at monthly intervals in areas where Cobitis taenia (L.) were present were found to be approximately half those of areas in which Cobitis taenia L. were not found (0.148 m/sec and 0.293 m/sec). Substrate samples from areas where Cobitis taenia L. were present had a fine organic component, in contrast to the remainder of the river bed, which consisted of hard-packed gravel.In the laboratory, choice chamber experiments demonstrated a positive selection for fine organic deposits.     

Contents of Trace Elements as Indicators of Ecological Divergence between Sympatric Spined Loaches (Teleostei,Cobitidae) from the Upper Dnieper

The contents of eight trace elements (Ti, Mn, Ni, Cu, Zn, Sr, Ba, and Pb) in muscles of syntopic sexual and clonal spined loaches (the golden loach Sabanejewia baltica, diploid males and females of Cobitis taenia, and congeneric triploid clonal females) from the upper Dnieper River and in the syntopic spined loaches (males and females of C. melanoleuca and males of C. taenia) from the upper Volga River basin were determined using the X-ray fluorescence spectroscopy technique. The contents of Cu in the clonal triploid Cobitis females and diploid C. taenia females from the Dnieper are different. The intersexual differences in the contents of Pb and Zn between C. taenia males and females, as well as the interspecific differences in the content of Ti between the spined loaches from the Dnieper and Volga basins were revealed. The concentrations of Cu and Pb correlated with the individual fish size. The potential for the use of the revealed differences in the trace element contents as an indicator of the divergence of ecological niches in the syntopic spined loaches is discussed.     

Genetic diversity, origin, and geographic distribution tendencies of biotypes of polyploid spined loaches (Cypriniformes, Cobitidae, Cobitis) in Ukraine

Sixteen of 28 possible biotypes of C. elongatoides-taenia s.lato (C. taenia, C. tanaitica, C. species-1) have been found in Ukrainian waters. Presumably, the biotypes of C. aff. melanoleuca-tanaitica has also been identified. The share of polyploids among Cobitis on average was 65%, where males made up less than 1% with the same ratio among tri- and tetra-polyploids. The absence of amphydiploidy and presence of individuals with recombinant genotype and abnormal electrophoretic specters, whose frequency sometimes is considerable, are attracting increasing interest. There are two centers of polyploid biotypes creation: southern (the Lower Danube) and northern (the Upper Danube, Oder, and Rhine). The C. taenia and C. species-1 type, which is typical for the northwestern basins of Ukraine, participates in the formation of polyploids in the Rhine alongside with C. elongatoides and C. tanaitica. It is determined that biotypes (C. 2(3) elongatoidestanaitica, C. elongatoides-2(3) tanaitica) in comparison with biotypes whose genome includes the chromosome set of C. taenia are limited in distribution towards the East. This is due to the hybridization of females from these biotypes with males of C. taenia afflicted by genetic instability and reduced viability of posterity.     

Comparative histology of the testes of the spined loach Cobitis taenia L. and natural allotetraploids of Cobitis (Pisces, Cobitidae)

The spined loach Cobitis taenia L. creates exclusively diploid and mixed diploid–polyploid populations. Allotriploid females, which co-exist with C. taenia or C. elongatoides and a few tetraploid males and females dominate in most Cobitis mixed populations. They reproduce gynogenetically and produce triploid eggs that are stimulated to development by sperm from Cobitis males. Some of these eggs are fertilized, which leads to the production of bisexual tetraploids. Males of C. taenia (2n = 48) from a diploid population in Lake Klawój, Northern Poland (46 individuals) and from a mixed Cobitis population in the Bug River, Eastern Poland (7 individuals), and three tetraploid males (4n = 98) from the same mixed population were examined. All the fish were analyzed karyologically and histologically. Tubules with cysts of the testes of C. taenia from both populations were filled with germ cells at various developmental stages. Among fishes from Lake Klawój sperm maturation in batches simultaneous with the batch spawning of C. taenia females was found. The testes of the loach C. taenia, from a mixed population in the Bug River, were filled with spermatozoa over the entire reproductive season. Sperm maturation in batches was not observed. Sperm maturation in batches seems to be only connected with a few diploid males in this population. So, a continuous process of spermatogenesis in their testes is required. Only in the testes of all tetraploid Cobitis males were cells characteristic of the early stages of spermatogenesis observed, i.e. without spermatids and spermatozoa. Furthermore, the histological sections of the testis of a male captured in August, revealed fragments with connective tissue between the germ cells. However the participation of tetraploid, infertile Cobitis males in the process of reproduction in the investigated mixed population remains controversial. The results obtained so far, reveal that even the infertile sperm of tetraploid males may induce gynogenesis in Cobitis triploid females.     

Termite coprolites (Insecta: Isoptera) from the Cretaceous of western France: A palaeoecological insight

This paper presents fossil faecal pellets - also named coprolites or frass - attributed to termites, which were found in amber and lignitic clay from the Wealden (Hauterivian-Barremian?), Late Albian and Early Cenomanian of south-western France. These coprolites have a characteristic subcylindrical shape and hexagonal transverse section and are assignable to Microcarpolithes hexagonalis Vangerow. The termite families that possibly produced these coprolites are discussed. The noticeable lack of termite attacks on the fossil wood associated with amber and lignitic clay is taphonomically analyzed in relation with the palaeoflora and palaeoclimate of these amber forests. The different medium where coprolites were found (amber, wood, sediments) suggests that primitive Cretaceous termites had already developed various biologies, such as wood or cryptic foraging, but probably not yet soil-feeding.     

Late Pliocene carnivores from Včeláre 2 (Southeastern Slovakia)

Carnivores from the Late Pliocene site of V?eláre 2 are described and their taxonomy is discussed. The carnivore assemblage includes nine specimens of the families Felidae (Homotherium crenatidens), Ursidae (Ursus minimus), and Ailuridae (Parailurus sp.). The scimitar-toothed cat and ursid are common representatives of the Pliocene European fauna, whereas the lesser panda is probably a new species of Parailurus, which differs from both Pliocene species, P. anglicus and P. hungaricus. As a part of a more or less uniform Pliocene carnivore fauna of the Northern Hemisphere, the V?eláre 2 assemblage represents a forest and (or) open grassland environment.     

Pliocene Ilyocyprididae (Ostracoda) from the Ebro Basin (N. Spain)

A revision of the Pliocene representatives of the Ilyocyprididae genera Ilyocypris Brady and Norman, 1889, and Qinghaicypris Huang, 1979, obtained from lacustrine sediments of the Villarroya section (La Rioja, N. Spain) is presented in this work. Based on carapace morphology and morphometrics, the occurrence in Europe of the genus Qinghaicypris is discussed. This genus is represented in this material by a new species, Qinghaicypris riojensis nov. sp., which is described herein. The occurrence of Ilyocypris and Qinghaicypris within the lacustrine series of Villarroya is analysed in relation to the hydrological evolution of the water bodies, which were very likely climatically driven. Palaeoecological as well as palaeobiogeographical interest of those genera is pointed out in the context of the aquatorium that spread over big areas of Europe during the Pliocene.     

In situ occurrence of a gall midge (Insecta,Diptera, Cecidomyiidae) on fossilized angiosperm leaf cuticle fragments from the Pliocene sediments of eastern India

In situ preservation of fossil insect damage in plant fossils is an excellent tool to study the coevolution of flora and fauna through geological time, but finding both damage and the insect causing that damage in the same specimen is a very rare phenomenon. Galling is a common form of angiosperm leaf damage, which can be regarded as a kind of extended phenotype of the causal insects, essentially the gall midges, but galls usually lack remains of the insects themselves. Here we report the in situ occurrence of a gall midge (Insecta, Diptera, Cecidomyiidae) as well as its pupal exuviae on the abaxial cuticular surface of fossilized leaf cuticle fragments of Fabaceae leaves (cf. Albizia) that also bear galls, recovered from the latest Neogene (Rajdanda Formation, Pliocene) sediments of the Chotonagpur Plateau, Jharkhand, northeastern India. This Pliocene gall midge features well-preserved legs, segmented antenna with distinct and enlarged scape, elongate curved setae, and longer than broad terminal plate of the ovipositor lamellae. The in situ presence of a gall midge on a host fabaceous leaf cuticle indicates the existence of a host-ectoparasite relationship in the ancient warm and humid tropical monsoon-influenced forests of eastern India during the Pliocene. This is the first authentic fossil record of an in situ phytophagous insect of Cecidomyiidae from India, as well as southeast Asia. Although the identification of the recovered phytophagous insect associated with the fossil leaf cuticle is only possible to family level, this find reveals that such plant-insect relationships existed in the Pliocene of eastern India.     

Ploidy-dependent survival of progeny arising from crosses between natural allotriploid Cobitis females and diploid C. taenia males (Pisces,Cobitidae)

Crosses between 21 triploid hybrid Cobitis females and 19 C. taenia (2n = 48) males led to viable progeny; whereas no embryonic development was observed in crosses with tetraploid males (4n = 98). The ploidy status of 491 progenies randomly selected with flow cytometry (316) or chromosome analysis (175) revealed an average of 55.2 % triploids and 44.8 % tetraploids, but the ratio of 3n versus 4n fish did change during development. In the first 2 days after hatching, approximately 65.1 % of tetraploid larvae were observed. Their number decreased significantly to 30.8 and 6.2 % on average during 2–5 and 10–15 months of life, respectively. The karyotype of tetraploid progeny (4n = 98) included 3n = 74 chromosomes of the parental female and n = 24 of C. taenia male. The number of tetraploid progeny indicated indirectly that about 66 % of eggs from 3n females were fertilized with C. taenia. The rest of the eggs developed clonally via gynogenesis or hemiclonally via hybridogenesis into triploids of the same karyotype structure as parental females. We have documented for the first time that (at least under experimental conditions) tetraploids are commonly formed, but are less viable than triploids, and a ratio similar to what is found under natural conditions is finally attained. The current explanation concerning the ploidy and karyotype structure of the progeny confirms that the eggs of 3n Cobitis females are not only capable of maintaining all chromosomes but are also capable of incorporating the sperm genome, thus creating the potential to produce tetraploids.     

Cercopithecidae from the Pliocene Chiwondo beds, Malawi-rift

There are a total of 16 fossil cercopithecid specimens, representing at least 10 individuals, from the Chiwondo Beds of northern Malawi. The majority of this material is derived from the Middle Pliocene Unit 3A, but one specimen is from the Early Pliocene Unit 2. This latter specimen is from a papionin of indeterminate genus similar in size to Parapapio ado and Pliopapio alemui. Among the specimens from Unit 3A, two species can be diagnosed: an indeterminate species of Theropithecus, and a species of Parapapio similar in dental size to P. broomi. Neither of the genera from Unit 3A are exclusive to either East Africa or South Africa. Their relative abundances, however, are more similar to Middle Pliocene South African sites where Parapapio is the most common primate genus, and Theropithecus is comparatively rare. This is in contrast to similarly-aged East African sites where Theropithecus is by far the most abundant genus.     

Remains of a Pliocene Mammut borsoni (Hays, 1834) (Proboscidea,Mammalia), from Milia (Grevena,W. Macedonia,Greece)

A partial skeleton of the mastodont Mammut borsoni (Hays, 1834) (Proboscidea), was excavated from Pliocene deposits at Milia — Grevena, W. Macedonia, in 1996–1999. The skeleton includes substantial portions of the skull — maxillary area — with left and right molar series (M² + M³); with the longest upper tusks ever found in Greece (4.39 m); the most complete mandible with left and right molar series (M₂ + M₃) and two lower incisor tusks, as well as post-cranial skeleton. It represents a very large adult of about 40 years in age. The high age of the finding is partly corroborated by ESR dating studies of tooth enamel, indicating an age probably beyond the upper dating range of this technique (approx. 800 000 years). The evolutionary position of this specimen among mammutids is also discussed.     

A comparison of ventilation rates and haemoglobin concentrations between two species of loach,Noemacheilus barbatulus (L.) and Cobitis taenia (L.)

The mean haemoglobin concentration of Noemacheilus barbatulus was found to be significantly higher than that of Cobitis taenia. Under conditions of reduced oxygen saturation, both species achieved maximum rates of ventilation at 10% 0₂. An alteration in opercular beat pattern accounted for the increased ventilation rates between 20% and 30%. A slightly higher tolerance for lowered oxygen concentrations was demonstrated by Cobitis taenia with disorientation and aerial respiration occurring at lower oxygen tensions than in Noemacheilus barbatulus.     

Arvicolidae (Rodentia) from the Pliocene of Tollo de Chiclana (Granada, SE Spain)

Several new fossiliferous Pliocene localities have been identified in the continental deposits of the area of Tollo de Chiclana (Guadix Basin, SE Spain), that have yielded a rich rodent and insectivore fauna. In this paper, we study the Arvicolidae from these localities. Remains adscribed to the genera Dolomys, Mimomys and Kislangia have been found, which are very interesting from a biostratigraphical point of view.     

A new species of Castanopsis (Fagaceae) from the upper Pliocene of West Yunnan,China and its biogeographical implications

Two fossil leaves identified as Castanopsis presclerophylla n. sp. collected from a diatomite bed in the upper Pliocene (3.3–2.8 Ma) in Tengchong County, Yunnan Province, Southwest China, are characterized by elliptic laminar shapes with acuminate apex, convex base, simple trichome bases and cyclocytic stomata. The cuticles of extant leaves from six selected Castanopsis species that are similar to the Pliocene fossil leaves in laminar shape were examined in detail for the comparison. Based on the analysis of leaf architecture and cuticular characteristics, the present fossil leaves most closely resemble the extant leaves of Castanopsis sclerophylla (Lindl.) Schott., which prefers a subtropical climate. The published fossil records of Castanopsis also indicate that it was once widely distributed in North America, Europe and Asia before the Pliocene, and then rapidly retreated to the East and Southeast Asia as a result of the Pleistocene glaciation.     

New Eucyon remains from the Pliocene Aramis Member (Sagantole Formation), Middle Awash Valley (Ethiopia)

The Aramis Member (Sagantole formation) includes the Gàala Tuff Complex-Daam Aatu Basaltic Tuff interval which has produced a taxonomically diverse vertebrate assemblage including the primitive hominid Ardipithecus ramidus. New Eucyon remains recovered from this interval come from localities in the Aramis, Sagantole, and Kuseralee catchments. The chronology established for the GATC-DABT interval is 4.4 Ma. These recoveries represent the most abundant available Eucyon assemblage of the eastern African Pliocene. Here, Eucyon fossils from the Kapsomin and Lemudong’o Late Miocene Kenyan sites are compared with the Aramis representatives, showing comparable morphology although with smaller dimensions. E. intrepidus–E. wokari nov. sp., might constitute a single lineage, with increasing size and robusticity, and the derivation of some morphological traits mainly on the lower carnassial. E. wokari represents a new eastern species of the African Pliocene Eucyon lineage.     

The first representative Pliocene assemblages of passerine birds in Asia (Northern Mongolia and Russian Transbaikalia)

Passerine birds from two late Pliocene localities, Shaamar in northern Mongolia and Beregovaya in Transbaikalia (East Russia), represent the first known Neogene fossil assemblages of perching birds from Asia. A total of 11 families and 15 taxa are recognized, including a new genus and species of bunting, Pliocalcarius orkhonensis, apparently related to the Longspurs, and new species within the genera Hirundo and Rhodospiza, which are described. The avifauna is composed of open land and bush dwellers; it contains a few arid species, representing the oldest finds of the corresponding genera or lineages. This may indicate that the living Asian arid avian complex originated in Central Asia in the Neogene. Several genera (Rhodospiza, Paradoxornis) are documented in this paper for the first time in pre-Pleistocene deposits. Report of Calcarius is the first pre-Holocene evidence of the occurrence of this genus in Asia, which together with the remains of Synaptomys lemmings at Shaamar, illustrates faunal interchanges between North America and Asia in the Pliocene.     

Messinian Lago-Mare deposits near the Strait of Gibraltar (Malaga Basin,S Spain)

A new stratigraphic unit (named LM unit) located at the base of the Pliocene marine succession in the eastern sector of the Malaga Basin has been distinguished. This unit is composed of two fining-upward sequences bounded by a discontinuity related to synsedimentary tectonic activity. Both sequences are made up of basal alluvial deposits overlain by subaquatic deposits. The lower sequence contains rich mollusc faunas characterized by bivalves Lymnocardiinae and Dreissenidae of Paratethyan origin, and non-marine gastropods, typical of oligo-low mesohaline shallow waters, and low diversified ostracod faunas of Paratethyan origin (Loxocorniculina djafarovi, Tyrrhenocythere pontica, Euxinocythere (Maeotocythere) praebaquana and Amnicythere propinqua) typical of low mesohaline waters. Alternances of monospecific ostracod assemblages made of Cyprideis agrigentina or oligotypic assemblages made of C. agrigentina and Loxoconcha spp. and richer assemblages made of L. djafarovi accompanied by several Amnicythere spp. and Camptocypria sp.1 characterize the upper sequence, pointing to more unstable environment affected by salinity and depth changes. Some samples collected from this upper sequence yielded rare, planktonic and benthic foraminifera, which could suggest the sporadic establishment of quasi-normal marine conditions in the westernmost Mediterranean during the deposition of this sequence. The palaeontological data and the palaeomagnetic results obtained in both the LM unit and the overlying Pliocene marine sediments restrict the age of the former to the post-evaporitic late Messinian. The age and the environmental conditions correlate these deposits with the Lago-Mare event occurring throughout the Mediterranean before the quick and widespread marine flooding of the Mediterranean at the beginning of the Pliocene.     

A new species of Carpinus (Betulaceae) from the Pliocene of Yunnan Province, China

Macrofossils of Carpinus have been widely reported from the Cenozoic of the Northern Hemisphere. However, the leaf cuticules of the genus have rarely been described. A new species, named Carpinus tengchongensis Dai et B.N. Sun, sp. nov., is identified based on 13 leaf fossils, collected from the late Pliocene Mangbang Formation, Tengchong County of Yunnan Province, China. The important characters of the fossil are its oblong-ovate leaf shape, obliquely cordate base, doubly serrulate margin, straight and moderately thick primary vein, pinnate secondary veins, percurrent tertiary veins, orthogonally reticulate areoles, absence of veinlets, anomocytic stomata with double-layered stomatal rim, well-formed T-pieces and trichome bases, which indicates an affinity within the genus Carpinus section Carpinus subsection Monbeigianae, especially with C. tsaiana. Carpinus fossils were present from the Eocene to Pliocene with disjunctive distribution in the North Temperate Zone, which broadly reflected the present distribution pattern and probably demonstrates the tolerance of Carpinus to environmental change.     

A Remarkable Case of Micro-Endemism in Laonastes aenigmamus (Diatomyidae,Rodentia) Revealed by Nuclear and Mitochondrial DNA Sequence Data

L. aenigmamus is endemic to the limestone formations of the Khammuan Province (Lao PDR), and is strongly specialized ecologically. From the survey of 137 individuals collected from 38 localities, we studied the phylogeography of this species using one mitochondrial (Cyt b) and two nuclear genes (BFIBR and GHR). Cyt b analyses reveal a strong mtDNA phylogeographical structure: 8 major geographical clades differing by 5–14% sequence divergence were identified, most of them corresponding to distinct karst areas. Nuclear markers display congruent results but with a less genetic structuring. Together, the data strongly suggest an inland insular model for Laonastes population structure. With 8 to 16 evolutionary significant units in a small area (about 200×50 km) this represents an exceptional example of micro-endemism. Our results suggest that L. aenigmamus may represent a complex of species and/or sub-species. The common ancestor of all Laonastes may have been widely distributed within the limestone formations of the Khammuan Province at the end of Miocene/beginning of the Pliocene. Parallel events of karst fragmentation and population isolation would have occurred during the Pleistocene or/and the end of the Pliocene. The limited gene flow detected between populations from different karst blocks restrains the likelihood of survival of Laonastes. This work increases the necessity for a strict protection of this rare animal and its habitat and provides exclusive information, essential to the organization of its protection.