A Late Pleistocene (MIS3) ungulate mammal assemblage (Los Rincones,Zaragoza, Spain) in the Eurosiberian–Mediterranean boundary

The Late Pleistocene archaeo-palaeontological sites in the Iberian Peninsula are located mainly on the coasts. Here, we present for the first time a palaeoenvironmental proxy for Upper Pleistocene locality (Marine Isotope Stage 3 MIS3) that is in the interior peninsular, in the Moncayo massif (Zaragoza). This is actually the boundary between Mediterranean and Eurosiberian climatic regions. This study is based in the site ungulates: Capra pyrenaica, which is larger in size than the current and fossil Capra from the Mediterranean area of the Iberian Peninsula. The horses have a small size, which is similar to that of the horses from Fontainhas and Casares. Significantly lesser in the number of specimens are the roe deer, the southern chamois and the auroch. The study and comparison of the faunal assemblage of the locality of Los Rincones with other sites of the Iberian MIS3 show a cluster of sites in the southern Peninsular, though separated, due to the abundance of Capra pyrenaica. The association of Los Rincones is similar to the southern peninsular sites such as Nerja, Gorham Cave, Cova Beneito and Zafarraya. The ungulate assemblage of Los Rincones represents a landscape with temperate climate, presence of steppe and patches of forest, similar to the current landscape surrounding the cavity today.     

Updated chronology for Middle to Late Miocene mammal sites of the Daroca area (Calatayud-Montalbán Basin,Spain)

The micromammal sequence of the Calatayud-Montalbán Basin in Northeast Central Spain is exceptional in terms of its faunal richness and dating accuracy. However, until now, several classical localities with ages close to the Middle to Late Miocene transition have never been directly tied to the Geomagnetic Polarity Time Scale. Here, we present an updated stratigraphic framework for the Daroca area, resulting in new and better-constrained ages for the micro- and macromammal-bearing sites of Toril, Carrilanga, and Pedregueras, and the macromammal site Los Andurriales. Toril is correlated to chron C5Ar.1r with an age of 12.7 Ma. Carrilanga and Los Andurriales are dated at 11.3 Ma, slightly older than the nearby sites Nombrevilla 9–10 (11.2 Ma). The fauna of these latter sites just pre-dates the entry of Hipparion, which is supposed to have its first appearance in Europe also at 11.2 Ma. The age of Pedregueras 2A is estimated at 10.6 Ma, constraining the local Zone H–I boundary and the first Iberian occurrence of Cricetulodon to 10.7 or 10.6 Ma. With an age of 10.4 Ma, the site of Pedregueras 2C is documenting the presence of very rare Murinae in Europe long (ca. half a million years) before their attainment of general dominance.     

Thick brachiopod shell concentrations from prodelta and siliciclastic ramp in a Tortonian Atlantic–Mediterranean strait (Miocene, Guadix Basin, southern Spain)

Carbonate production by brachiopods in shallow-water habitats is generally expected to be not sufficiently high and temporally persistent to allow them to form very thick and densely packed shell concentrations. The formation of thick brachiopod concentrations requires long-term persistence of populations with high density of individuals, and such circumstances are assumed to be rare especially during the Cenozoic. However, here we show that the large-sized brachiopod Terebratula terebratula, the most common species in benthic assemblages with epifaunal bivalves and irregular echinoids, formed several decameter- to meter-thick, densely packed concentrations in shallow siliciclastic, high-energy environments, in a seaway connecting the Atlantic Ocean with the Mediterranean Sea during the Latest Tortonian (Late Miocene, Guadix Basin, southern Spain). This brachiopod formed (1) meter-scale, thick, parautochthonous concentrations in a prodelta setting and (2) thin, mainly allochthonous, tide- and storm-reworked concentrations in megaripples and dunes. The abundance of brachiopods at the spatial scale of the Guadix Basin seems to be mainly related to intermediate levels of sedimentation rate and current velocity because abundance and thickness of shell concentrations decline both (1) in onshore direction towards delta foresets with high sedimentation rate generated by debris flows and (2) in offshore direction with increasing levels of tide- and storm-induced substrate instability. Although brachiopods in dune and megaripple deposits are more fragmented, disarticulated, and sorted, and have a higher pedicle/brachial valve ratio than in prodelta deposits, taphonomic damage is still relatively high in prodelta deposits. Terebratula terebratula thus formed thick concentrations in spite of that disintegration processes were relatively intense along the whole depositional gradient. Therefore, population dynamic of this species was probably characterized by production maxima that were comparable to some Cenozoic molluscs in terms of their productivity potential to form thick shell concentrations in shallow subtidal environments. We suggest that temporal changes in brachiopod carbonate production have a significant spatial and phylogenetic component because multiple large-sized species of the family Terebratulidae, which underwent radiation during the Cenozoic, attained high abundances and formed shell concentrations in temperate regions.     

Organisation of the endosperm and endosperm–placenta syncytia in bladderworts (Utricularia, Lentibulariaceae) with emphasis on the microtubule arrangement

Multinucleate cells play an important role in higher plants, especially during reproduction; however, the configurations of their cytoskeletons, which are formed as a result of mitosis without cytokinesis, have mainly been studied in coenocytes. Previous authors have proposed that in spite of their developmental origin (cell fusion or mitosis without cytokinesis), in multinucleate plant cells, radiating microtubules determine the regular spacing of individual nuclei. However, with the exception of specific syncytia induced by parasitic nematodes, there is no information about the microtubular cytoskeleton in plant heterokaryotic syncytia, i.e. when the nuclei of fused cells come from different cell pools. In this paper, we describe the arrangement of microtubules in the endosperm and special endosperm–placenta syncytia in two Utricularia species. These syncytia arise from different progenitor cells, i.e. cells of the maternal sporophytic nutritive tissue and the micropylar endosperm haustorium (both maternal and paternal genetic material). The development of the endosperm in the two species studied was very similar. We describe microtubule configurations in the three functional endosperm domains: the micropylar syncytium, the endosperm proper and the chalazal haustorium. In contrast to plant syncytia that are induced by parasitic nematodes, the syncytia of Utricularia had an extensive microtubular network. Within each syncytium, two giant nuclei, coming from endosperm cells, were surrounded by a three-dimensional cage of microtubules, which formed a huge cytoplasmic domain. At the periphery of the syncytium, where new protoplasts of the nutritive cells join the syncytium, the microtubules formed a network which surrounded small nuclei from nutritive tissue cells and were also distributed through the cytoplasm. Thus, in the Utricularia syncytium, there were different sized cytoplasmic domains, whose architecture depended on the source and size of the nuclei. The endosperm proper was isolated from maternal (ovule) tissues by a cuticle layer, so the syncytium and chalazal haustorium were the only way for nutrients to be transported from the maternal tissue towards the developing embryo.     

First porcupine fossils (Mammalia,Rodentia) from the late Miocene of NW Iran,with notes on late Miocene–Pliocene dispersal of porcupines

This paper describes the first fossil porcupine remains from Iran. Four upper cheek teeth and two fragmentary lower incisors present sufficient characters for identification as Hystrix aryanensis, a species previously known from the late Miocene locality of Molayan (Afghanistan) estimated at ca. 7–8 Ma. The dental features of porcupines are discussed to show their systematic value and highlight evolutionary trends in late Miocene and Pliocene porcupines. This study also discusses the dispersal history of fossil porcupines in relation to paleobiogeographic provinces and environmental changes during late Miocene to late Pliocene time.     

Nutrient and plant dynamics in Lake Agmon Wetlands (Hula Valley,Israel): a review with emphasis on Typha domingensis (1994–1999)

Shallow lake Agmon is a newly created subtropical wetland in north-eastern Israel. The lake is part of the Hula Project aimed at slowing down deterioration processes of the peat soils, to establish infrastructure for ecotourism as an income for the land owners, and nutrient removal from Lake Kinneret inputs. An onset of benthic filamentous macro-green algae during late winter–spring season, followed by submerged macrophytes vegetation during spring–summer was documented. The phosphorus summer loads are mostly plant–mediated internal fluxes and nitrogen intensively removed from lake waters by sedimentation and denitrification. The summer phytoplankton, mostly colonial cyanobacteria, are P limited. During 1995 and early 1996, dense Typha domingensisstands were developed in the southern half of the Lake (chalk-marl bottom sediments). The P-limited Typhavegetation collapsed within less than half a year and reappeared in the south-eastern part of the lake where sediments were exposed and oxidized. It is hypothesized that phosphorus cycle is a strong dependant of macrophyte mediation, and P deficiency in the sediments predominantly affected Typhadecline and an increase of P availability later enabled the reappearance of the Typhastands.     

New observations on the Late Miocene–Early Pliocene Lutrinae (Mustelidae: Carnivora,Mammalia) from the Middle Awash,Afar Rift,Ethiopia

New observations on the Late Miocene and Earliest Pliocene mustelids from the Middle Awash of Ethiopia are presented. The Middle Awash study area samples the last six million years of African vertebrate evolutionary history. Its Latest Miocene (Asa Koma Member of the Adu-Asa Formation, 5.54–5.77 Ma) and Earliest Pliocene (Kuseralee and Gawto Members of the Sagantole Formation, 5.2 and 4.85 Ma, respectively) deposits sample a number of large and small carnivore taxa among which mustelids are numerically abundant. Among the known Late Miocene and Early Pliocene mustelid genera, the Middle Awash Late Miocene documents the earliest Mellivora in eastern Africa and its likely first appearance in Africa, a new species of Plesiogulo, and a species of Vishnuonyx. The latter possibly represents the last appearance of this genus in Africa. Torolutra ougandensis is known from both the Late Miocene and Early Pliocene deposits of the Middle Awash. The genus Sivaonyx is represented by at least two species: S. ekecaman and S. aff. S. soriae. Most of the lutrine genera documented in the Middle Awash Late Miocene/Early Pliocene are also documented in contemporaneous sites of eastern Africa. The new observations presented here show that mustelids were more diverse in the Middle Awash Late Miocene and Early Pliocene than previously documented.     

Early effects of forest regeneration with selective and small scale clear-cutting on ground beetles (Coleoptera,Carabidae) in a Norway spruce stand in Southern Bavaria (Höglwald)

This study investigates the early effects of forest regeneration with selective, and small scale clear-cutting, on ground beetle (Coleoptera, Carabidae) community composition in a homogenous, mature spruce forest in Southern Bavaria (Höglwald), Germany. Carabid beetles were sampled with pitfall-, emergence-, and window-traps, from 1999 to 2001 during a pre-treatment year, the year of cutting, and the year after cutting. In the spruce stand we found a relatively low species richness with few dominating species. Selective cutting preserved this carabid assemblage. At the clear-cuts carabid species richness increased in the year of cutting, because of the invasion of small open field species, and the persistence of most forest species. Also, number of individuals increased due to higher numbers caught in the window-traps. The first open habitat species appeared just a few months after felling. However, in the next year the numbers of individuals, especially of forest species,were drastically reduced. Also, the number of species decreased, and was just slightly higher than on the control plot (mature stand). According to the DCA (detrended correspondence analysis) forest interior species had the same habitat preferences as net building spiders (Amaurobiidae, Linyphiidae) and other families of beetles (Staphylinidae, Curculionidae). Several groups of open habitat species responded positively on different patches found in the clear-cut: (1) diversity ofground vegetation, respectively coverage of shrubs, (2) favour for moist patterns, and water filled ruts (together with Gastropoda), or (3) low coverage of ground vegetation (together with free hunting spiders, Lycosidae). Different structures side by side (mature forest, selective cutting, open areas) may improve diversity on a forest scale. Small openings can serve as an important retreat for open habitat species. However, if clear-cuts become the dominant element, forest species maybe threatened. With selective cutting species richness of carabids is not improved; however, the remaining forest carabid species may be preserved during the early phase of the regeneration process.     

Coralline algae as depth indicators in the Sommières Basin (early Miocene,Southern France)

The aim of this work is to demonstrate the benefits of digital surface-quantification and species identification in the study of coralline algae. Within the well-constrained context of the Miocene Sommières Basin (Southern France), whose sedimentological and paleontological setting has been reconstructed by previous researches, the abundance of coralline algae is estimated through quantification of the area occupied by the different species, which are thoroughly described in order to make future taxonomic-revisions as easy as possible. Coralline distribution patterns are studied along a bathymetric gradient to assess the response of the major groups and of the different species to variations in water depth. Surface quantification highlights clear trends both at the species level and higher taxonomic ranks, showing that coralline algae can be a quite accurate instrument in paleoenvironmental reconstructions. Among the clearly identified species, Lithophyllum sp. A, Sporolithon sp. A, and Spongites fruticulosus prefer shallow-water; Mesophyllum roveretoi dominates at intermediate depth together with Lithothamnion ponzonense, while Phymatolithon sp. A occurs at the lower limit of the photic zone. The approach presented here can be applied to a variety of different contexts, providing a powerful instrument for the interpretation of coralline-algal associations.     

Effects of deforestation on structure and diversity of small mammal communities in the Moravskoslezské Beskydy Mts (Czech Republic)

During 1970s and 1980s, a large area of mountains in the Czech Republic was influenced by long-term industrial air pollution. Among the most degraded areas were the peaks of the Moravskoslezské Beskydy Mts, where vast clearings resulted from emissions and subsequent forest destruction. This study is aimed at determining the degree of deforestation that is necessary to cause changes in structure and species diversity of small mammal communities that were observed previously. Communities of rodents and insectivores were monitored for a minimum of 3 years at two mountain ranges of the Moravskoslezské Beskydy Mts (Czech Republic) by standard mouse snap-traps. The localities (Smrk and Kněhyně) differ by the degree of human disturbance. Clearings on Smrk Mt are very large (> 30 ha) with no remaining original forest growth as a result of intensive air pollution, unlike the same habitat type at Kněhyně Mt, where the clearings are minor (< 3 ha) and contain living solitary trees. Structure and diversity of small mammal communities in clearings were compared with those from original forests and other mountain habitats. Communities of small mammals at clearings in Smrk Mt (with dominatingMicrotus agrestis) are structurally very different from all other habitats, while structure of communities at Kněhyně clearings are very similar to those of original mountain forest (Complete linkage clustering based on Renkonen index). The community of the original mountain spruce forest at Kněhyně had the highest species diversity (according to Shannon-Weaver, Brillouin, and Simpson indices, Shannon evenness, and rarefaction), while species diversity at clearings of Smrk was the lowest. Shannon diversity of community at Kněhyně primeval forest is similar to that of Kněhyně clearings, while at Smrk Mt the forest diversity is higher than that of clearings. The species diversity of mountain forest and clearings at Kněhyně Mt was significantly higher than that in the same habitats at Smrk Mt. Our results obtained in disturbed habitats at Kněhyně and Smrk Mts suggest that the degree of deforestation may influence the presence and/or the degree of community changes. If the forest destruction is relatively small (clearings < 3 ha), the structure and diversity of small mammal communities do not differ from those of original forest.     

The Cenomanian Gastropoda of the Kassenberg quarry in Mülheim (Germany,Late Cretaceous)

Forty-six gastropod species are described from the Cenomanian of the Kassenberg quarry in Mülheim a. d. Ruhr, Germany, twelve of them are new. They are assigned to 33 known genera and two new genera.Deikella n. gen. is introduced for threeTurbo-like species which have strong axial ribs in contrast to the smooth RecentTurbo. Frydatinus n. gen. is introduced for a loosely coiled archaeogastropod with a round aperture and spine-like extensions on its outer side. A new species ofDelpeya is introduced, and it is suggested that this genus derived from the JurassicNummocalcar. The high number of pleurotomariids indicates that these gastropods still lived on rocky shores during the Cenomanian, in contrast to modern times, where they are restricted to hardgrounds in deep-water. The new species are:Bathrotomaria harasewychi, Deikella spinicostata, Deikella ruhrensis, Deikella? muelheimensis, Trochus rauenorum, Margarella (Promargarita) spiraloides, Margarella (Promargarita) trochoides, Semisolarium boehmi, Onkospira perrilliatae, Delpeya hilperti, Neritopsis kasei, andOtostoma kassenbergensis.     

Late Cenomanian–Early Turonian facies development and sea-level changes in the Bodenwöhrer Senke (Danubian Cretaceous Group, Bavaria, Germany)

The Upper Cenomanian–Lower Turonian litho-stratigraphic units of the Danubian Cretaceous Group of the proximal Bodenwöhrer Senke (Regensburg, Eibrunn and Winzerberg formations, the latter consisting of a lower Reinhausen Member and an upper Knollensand Member), have been investigated with a focus on facies analysis and sequence stratigraphy. Analyses of litho-, bio-, and microfacies resulted in the recognition of 12 predominantly marine facies types for the Eibrunn and Winzerberg formations. Petrographic and paleontological properties as well as gradual transitions in the sections suggest that their depositional environment was a texturally graded, predominantly siliciclastic, storm-dominated shelf. The muddy–siliceous facies types FT 1–3 have been deposited below the storm wave-base in an outer shelf setting. Mid-shelf deposits are represented by fine- to medium-grained, bioturbated, partly glauconitic sandstones (FT 4–6). Coarse-grained, gravelly and/or shell-bearing sandstones (FT 7–10) developed in the inner shelf zone. Highly immature, arkosic coarse-grained sandstones and conglomerates (FT 11 and 12) characterize an incised, high-gradient braided river system. The Winzerberg Formation with its general coarsening- and thickening-upward trend reflects a regressive cycle culminating in a subaerial unconformity associated with a coarse-grained, gravelly unit of marine to fluvial origin known as the “Hornsand” which is demonstrably diachronous. The overlying Altenkreith Member of the Roding Formation signifies the onset of a new transgressive cycle in the early Middle Turonian. The sequence stratigraphic analysis suggests that the deposition of the Upper Cenomanian and Lower Turonian strata of the Bodenwöhrer Senke took place in a single cycle of third-order eustatic sea-level change between the major sequence boundaries SB Ce 5 (mid-Late Cenomanian) and SB Tu 1 (Early–Middle Turonian boundary interval). The southeastern part of the Bodenwöhrer Senke was flooded in the mid-Late Cenomanian (Praeactinocamax plenus transgression) and a second transgressive event occurred in the earliest Turonian. In the central and northwestern parts of the Bodenwöhrer Senke, however, the initial transgression occurred during the earliest Turonian, related to pre-transgression topography. Thus, the Regensburg and Eibrunn formations are increasingly condensed here and cannot be separated anymore. Following an earliest Turonian maximum flooding, the Lower Turonian Winzerberg Formation filled the available accommodation space, explaining its constant thickness of 35–40 m across the Bodenwöhrer Senke and excluding tectonic activity during this interval. Rapid sea-level fall at SB Tu 1 terminated this depositional sequence. This study shows that Late Cenomanian–Early Turonian deposition in the Bodenwöhrer Senke was governed by eustatic sea-level changes.     

Regulation of the α-ketoglutarate dehydrogenasecomplex during hibernation in a small mammal,the Richardson's ground squirrel (Urocitellus richardsonii)

The citric acid cycle (CAC) is a central metabolic pathway that links carbohydrate, lipid, and amino acid metabolism in the mitochondria and, hence, is a crucial target for metabolic regulation. The α-ketoglutarate dehydrogenase complex (KGDC) is the rate-limiting step of the CAC, the three enzymes of the complex catalyzing the transformation of α-ketoglutarate to succinyl-CoA with the release of CO₂ and reduction of NAD to NADH. During hibernation, the metabolic rate of small mammals is suppressed, in part due to reduced body temperature but also active controls that suppress aerobic metabolism. The present study examined KGDC regulation during hibernation in skeletal muscle of the Richardson's ground squirrel (Urocitellus richardsonii). The KGDC was partially purified from skeletal muscle of euthermic and hibernating ground squirrels and kinetic properties were evaluated at 5°, 22°, and 37 °C. KGDC from hibernator muscle at all temperatures compared with euthermic controls exhibited a decreased affinity for CoA as well as reduced activation by Ca²⁺ ions at 5 °C from both euthermic and hibernating conditions. Co-immunoprecipitation was employed to isolate the E1, E2 and E3 enzymes of the complex (OGDH, DLST, DLD) to allow immunoblot analysis of post-translational modifications (PTMs) of each enzyme. The results showed elevated phospho-tyrosine content on all three enzymes during hibernation as well as increased ADP-ribosylation and succinylation of hibernator OGDH. Taken together these results show that the KGDC is regulated by posttranslational modifications and temperature effects to reorganize enzyme activity and mitochondrial function to aid suppression of mitochondrial activity during hibernation.     

Hoplitomerycidae (Ruminantia; Late Miocene,Central-Southeastern Italy): Whom and where from?

The endemic monogeneric fossil family Hoplitomerycidae currently includes six known species, the remains of which are found in Lower Tortonian coastal tidal-flat layered calcarenites at Scontrone, in Abruzzo (central Italy), as well as in karstic fissure fillings, supposedly of Messinian age, in the Gargano Promontory, Apulia (southeastern Italy). Their remains are found associated with bones of many other vertebrates which indicate the existence of a vast territory, the so-called Abruzzo-Apulia Platform, which was isolated from the nearest mainland at least from the Early Oligocene up to the latest Miocene. A recent cladistic analysis showed that the classification of the hoplitomerycids in Cervoidea, which currently enjoys vast popularity, is not justified. The family is characterized by a set of cranial and postcranial primitive traits, above all their non-parallel-sided astragalus, that suggest that the family probably stemmed from a primitive ruminant stock somewhere before the emergence of Pecora, consistent with geological evidence showing that about 29 Ma a land-bridge connected the Abruzzo-Apulia Platform with the Balkans across the Adriatic Sea, approximately where the Tremiti islands are today. The present study intended to reconnect to the results of the cladistic analysis and to extend them in the attempt to track down the possible ancestors of Hoplitomerycidae. The family expectedly radiated developing autapomorphic features that make the search quite arduous. Nonetheless, its primitive, leftover characters relate it to Oligocene basal ruminants with asymmetric astragalus. Following the distribution of the non-parallel astragalus through space and time leads to speculate a possible origin of the family from primitive Tragulina representatives that dispersed in Anatolia in the course of the Oligocene. Current reconstructions of the Early Oligocene paleogeography of the eastern Mediterranean show that the Apulian Platform was connected via a cross-Adriatic land-bridge to the Balkans, Anatolia and by that way also to middle and central Asia and central-eastern Europe.     

Mortality and morbidity in the city of Bern,Switzerland, 1805–1815 with special emphasis on infant,child and maternal deaths

This article contributes to the research on demographics and public health of urban populations of preindustrial Europe. The key source is a burial register that contains information on the deceased, such as age and sex, residence and cause of death. This register is one of the earliest compilations of data sets of individuals with this high degree of completeness and consistency. Critical assessment of the register's origin, formation and upkeep promises high validity and reliability.Between 1805 and 1815, 4,390 deceased inhabitants were registered. Information concerning these individuals provides the basis for this study. Life tables of Bern's population were created using different models. The causes of death were classified and their frequency calculated. Furthermore, the susceptibility of age groups to certain causes of death was established. Special attention was given to causes of death and mortality of newborns, infants and birth-giving women.In comparison to other cities and regions in Central Europe, Bern's mortality structure shows low rates for infants (q₀ = 0.144) and children (q_1–4 = 0.068). This could have simply indicated better living conditions. Life expectancy at birth was 43 years. Mortality was high in winter and spring, and decreased in summer to a low level with a short rise in August.The study of the causes of death was inhibited by difficulties in translating early 19th century nomenclature into the modern medical system. Nonetheless, death from metabolic disorders, illnesses of the respiratory system, and debilitation were the most prominent causes in Bern. Apparently, the worst killer of infants up to 12 months was the “gichteren”, an obsolete German term for lethal spasmodic convulsions. The exact modern identification of this disease remains unclear. Possibilities such as infant tetanus or infant epilepsy are discussed.The maternal death rate of 0.72% is comparable with values calculated from contemporaneous sources. Relevance of childbed fever in the early 1800s was low. Bern's data indicate that the extent of deaths related to childbirth in this period is overrated.This research has an explicit interdisciplinary value for various fields including both the humanities and natural sciences, since information reported here represents the complete age and sex structure of a deceased population. Physical anthropologists can use these data as a true reference group for their palaeodemographic studies of preindustrial Central Europe of the late 18th and early 19th century. It is a call to both historians and anthropologists to use our resources to a better effect through combination of methods and exchange of knowledge.     

Molecular phylogenies and mating study data in Polyporus with special emphasis on group “Melanopus” (Basidiomycota)

“Melanopus” is an unranked infrageneric group within Polyporus, a genus comprising wood-decaying homobasidiomycetes. This study compiles new information on the mating systems, phylogeny, and geographic distribution of the group. We report tetrapolar mating systems in “Melanopus,” as well as in the more distantly related Polyporus umbellatus. “Melanopus” is addressed using internal transcribed spacer (ITS) rDNA sequence data, comparing resolving power of several phylogenetic methods and depths of sequence information, including recoded secondary structure data informed by the primary sequence data. The latter, inferred structure of the ITS2 rRNA was insufficient in phylogenetic reconstruction on its own. Intercollection compatibility studies showed Polyporus varius collections from both sides of the Atlantic to be intercompatible, the same was found for Polyporus tubaeformis collections from California and Scotland. Molecular analysis supports P. tubaeformis conspecifity of Scottish and Californian collections with a Norwegian collection. Several other herbarium specimens inaccessible to successful PCR and sequencing were redetermined as P. tubaeformis by morphological characters. This improved on the current knowledge of distribution of the species, tentatively adding Idaho, North Carolina, and Germany’s Mecklenburg-Western Pomerania.Electronic supplementary material Supplementary material is available in the online version of this article at and is accessible for authorized users.     

The first record of anguine lizards (Anguimorpha,Anguidae) from the early Miocene locality Ulm – Westtangente in Germany

Abstract

The first fossil anguine material from the lower Miocene (MN 2) locality Ulm – Westtangente in Germany is described. The parietal and compound bone of the lower jaw can be attributed to Ophisaurus holeci, previously known only from younger age (MN 3–MN 7). Moreover, the parietal represents the largest parietal of this species. In other disarticulated material, such as frontal, maxilla, dentary and osteoderms, alpha taxonomy is not possible and these elements cannot be allocated at the species level. Despite a limited data source, a phylogenetic analysis was done (16 taxa, 36 characters) producing four equally parsimonious trees. The analysis shows a close relationship of O. holeci and the Eocene Ophisauriscus quadrupes. These two taxa form a monophyletic clade, a sister-clade to Ophisaurus + Anguis. However, more complete skeletal material of O. holeci is needed to support such a statement. We used our phylogenetic analysis to analyze trace character history for one frontal and three parietal characters. The palaeoenvironmental conditions of the locality Ulm – Westtangente bring further support of the previous hypothesis that O. holeci was adapted to environments with high ground water levels – environments around lakes or rivers.     

First description of milk teeth of fossil South American procyonid from the lower Chapadmalalan (Late Miocene–Early Pliocene) of “Farola Monte Hermoso,” Argentina: paleoecological considerations

The first record of milk teeth of South American fossil procyonids comes from the Late Miocene–Early Pliocene at “Farola Monte Hermoso,” Buenos Aires Province, Argentina. Five extant genera of Procyonidae inhabit South America (Bassaricyon Allen, Nasuella Hollister, Potos Geoffroy Saint-Hilaire and Cuvier, Procyon Storr, and Nasua Storr). Of these only Procyon and Nasua are present in the fossil record (Late Pleistocene–Holocene), in several localities in Brazil, Uruguay, and Bolivia. In addition, six other fossil genera were named, but only two are considered valid: Cyonasua and Chapadmalania. Thus, Cyonasua encompasses ten formally named species and Chapadmalania two. The new specimen, MLP 09-X-5-1, is assigned to cf. Cyonasua. In addition, anatomical evidence implies a much more carnivorous diet in Late Miocene–Early Pleistocene procyonids than that of extant South American taxa. Finally, I examine and discuss the “competitive displacement” hypothesis regarding the extinction of native marsupial carnivores after the arrival of immigrant placental carnivores in South America.     

Mortality patterns over 3 years in a sparse population of wild rabbits (Oryctolagus cuniculus) in New Zealand, with an emphasis on rabbit haemorrhagic disease (RHD)

A sparse rabbit population in New Zealand was monitored over 3 years to assess the temporal dynamics of rabbit mortality, in particular to understand the mortality patterns due to rabbit haemorrhagic disease (RHD). A total of 107 deaths were recorded, of which 93 could be classified by cause. The predominant cause of mortality was predation (47% of deaths), followed by RHD (20%). Deaths due to RHD were clustered in time (within 3 weeks), predation occurred most actively from late autumn to spring, while other causes of death did not show pronounced seasonal peaks. No differences in cause-specific death risk were observed between sexes. Predation was the main cause of death in younger animals, while RHD mortality occurred mainly in older rabbits. This study has shown that the impact of RHD can vary considerably between years, indicating that a variety of risk factors are required to initiate a RHD epidemic with a high mortality rate among rabbits.