Martharaptor greenriverensis, a New Theropod Dinosaur from the Lower Cretaceous of Utah

Background

The Yellow Cat Member of the Cedar Mountain Formation (Early Cretaceous, Barremian?) of Utah has yielded a rich dinosaur fauna, including the basal therizinosauroid theropod Falcarius utahensis at its base. Recent excavation uncovered a new possible therizinosauroid taxon from a higher stratigraphic level in the Cedar Mountain Formation than F. utahensis.

Methodology/Principal Findings

Here we describe a fragmentary skeleton of the new theropod and perform a phylogenetic analysis to determine its phylogenetic position. The skeleton includes fragments of vertebrae, a scapula, forelimb and hindlimb bones, and an ischium. It also includes several well-preserved manual unguals. Manual and pedal morphology show that the specimen is distinct from other theropods from the Cedar Mountain Formation and from previously described therizinosauroids. It is here named as the holotype of a new genus and species, Martharaptor greenriverensis. Phylogenetic analysis places M. greenriverensis within Therizinosauroidea as the sister taxon to Alxasaurus + Therizinosauridae, although support for this placement is weak.

Conclusions/Significance

The new specimen adds to the known dinosaurian fauna of the Yellow Cat Member of the Cedar Mountain Formation. If the phylogenetic placement is correct, it also adds to the known diversity of Therizinosauroidea.     

A New Large-Bodied Oviraptorosaurian Theropod Dinosaur from the Latest Cretaceous of Western North America

The oviraptorosaurian theropod dinosaur clade Caenagnathidae has long been enigmatic due to the incomplete nature of nearly all described fossils. Here we describe Anzu wyliei gen. et sp. nov., a new taxon of large-bodied caenagnathid based primarily on three well-preserved partial skeletons. The specimens were recovered from the uppermost Cretaceous (upper Maastrichtian) Hell Creek Formation of North and South Dakota, and are therefore among the stratigraphically youngest known oviraptorosaurian remains. Collectively, the fossils include elements from most regions of the skeleton, providing a wealth of information on the osteology and evolutionary relationships of Caenagnathidae. Phylogenetic analysis reaffirms caenagnathid monophyly, and indicates that Anzu is most closely related to Caenagnathus collinsi, a taxon that is definitively known only from a mandible from the Campanian Dinosaur Park Formation of Alberta. The problematic oviraptorosaurs Microvenator and Gigantoraptor are recovered as basal caenagnathids, as has previously been suggested. Anzu and other caenagnathids may have favored well-watered floodplain settings over channel margins, and were probably ecological generalists that fed upon vegetation, small animals, and perhaps eggs.     

Bird-Like Anatomy,Posture, and Behavior Revealed by an Early Jurassic Theropod Dinosaur Resting Trace

Background

Fossil tracks made by non-avian theropod dinosaurs commonly reflect the habitual bipedal stance retained in living birds. Only rarely-captured behaviors, such as crouching, might create impressions made by the hands. Such tracks provide valuable information concerning the often poorly understood functional morphology of the early theropod forelimb.

Methodology/Principal Findings

Here we describe a well-preserved theropod trackway in a Lower Jurassic (∼198 million-year-old) lacustrine beach sandstone in the Whitmore Point Member of the Moenave Formation in southwestern Utah. The trackway consists of prints of typical morphology, intermittent tail drags and, unusually, traces made by the animal resting on the substrate in a posture very similar to modern birds. The resting trace includes symmetrical pes impressions and well-defined impressions made by both hands, the tail, and the ischial callosity.

Conclusions/Significance

The manus impressions corroborate that early theropods, like later birds, held their palms facing medially, in contrast to manus prints previously attributed to theropods that have forward-pointing digits. Both the symmetrical resting posture and the medially-facing palms therefore evolved by the Early Jurassic, much earlier in the theropod lineage than previously recognized, and may characterize all theropods.     

Small Theropod Teeth from the Late Cretaceous of the San Juan Basin,Northwestern New Mexico and Their Implications for Understanding Latest Cretaceous Dinosaur Evolution

Studying the evolution and biogeographic distribution of dinosaurs during the latest Cretaceous is critical for better understanding the end-Cretaceous extinction event that killed off all non-avian dinosaurs. Western North America contains among the best records of Late Cretaceous terrestrial vertebrates in the world, but is biased against small-bodied dinosaurs. Isolated teeth are the primary evidence for understanding the diversity and evolution of small-bodied theropod dinosaurs during the Late Cretaceous, but few such specimens have been well documented from outside of the northern Rockies, making it difficult to assess Late Cretaceous dinosaur diversity and biogeographic patterns. We describe small theropod teeth from the San Juan Basin of northwestern New Mexico. These specimens were collected from strata spanning Santonian – Maastrichtian. We grouped isolated theropod teeth into several morphotypes, which we assigned to higher-level theropod clades based on possession of phylogenetic synapomorphies. We then used principal components analysis and discriminant function analyses to gauge whether the San Juan Basin teeth overlap with, or are quantitatively distinct from, similar tooth morphotypes from other geographic areas. The San Juan Basin contains a diverse record of small theropods. Late Campanian assemblages differ from approximately co-eval assemblages of the northern Rockies in being less diverse with only rare representatives of troodontids and a Dromaeosaurus-like taxon. We also provide evidence that erect and recurved morphs of a Richardoestesia-like taxon represent a single heterodont species. A late Maastrichtian assemblage is dominated by a distinct troodontid. The differences between northern and southern faunas based on isolated theropod teeth provide evidence for provinciality in the late Campanian and the late Maastrichtian of North America. However, there is no indication that major components of small-bodied theropod diversity were lost during the Maastrichtian in New Mexico. The same pattern seen in northern faunas, which may provide evidence for an abrupt dinosaur extinction.     

Pollen Morphology of the Periplocaceae from Madagascar

The pollen morphology of eleven (Baroniella Constantin & Galland, Baseonema Schltr. & Rendle, Camptocarpus Decne., Cryptolepis R. Br., Cryptostegia R. Br., Gonocrypta Baill., Harpanema Decne., Ischnolepis Jum. & H. Perrier, Menabea Baill., Pentopetia Decne., and Tanulepis Balf. f.) of the 13 genera of the Periplocaceae from Madagascar have been examined using light-, scanning-, and transmission electron microscopy. All of the genera are characterized by pollen grains arranged in tetrads. The arrangement of the grains may be rhomboidal, decussate or tetragonal. The 4–6 pores present are restricted to the junction area of adjacent grains. Cryptostegia differs from the other genera in that the arrangement of pollen grains is only decussate. In Menabea the tetrads are united into a pollinium. The exine is smooth and consists of a distal stratum (tectum), subtended by a granular stratum consisting of granules of unequal size. Towards the base larger granules are present. In Camptocarpus, Harpanema and Tanulepis the exine is stratified into a distal stratum (tectum), a thin granular stratum and an almost continuous basal stratum (foot layer). The inline is well developed. The pollen grains of tetrads are connected by wall bridges (cross-wall cohesion). The internal walls in Camptocarpus, Harpanema and Tanulepis differ from the other genera in the absence of a tectum. The pollen morphology of the taxa investigated is very similar and of little value for distinguishing the species and genera investigated. The distinctive difference in exine structure between the above mentioned three genera and other genera investigated emphasizes the importance of exine ultrastructure in the Periplocaceae.     

Telling Apart Ornithopod and Theropod Trackways: A Closer Look at a Large,Late Jurassic Tridactyl Dinosaur Trackway at Serwah,Republic of Yemen

A large bipedal tridactyl dinosaur trackway from the Late Jurassic of Serwah, near Madar, Arhab district, Republic of Yemen, has been attributed to an ornithopod trackmaker. As the distinction between theropod and ornithopod dinosaurs can pose a challenge, we present additional data to support and reconfirm the previous attribution.     

Theropod dinosaur teeth from the lowermost Cretaceous Rabekke Formation on Bornholm, Denmark

The dinosaur fauna of the palynologically dated lower Berriasian Skyttegård Member of the Rabekke Formation on the Baltic island of Bornholm, Denmark, is represented by isolated tooth crowns. The assemblage is restricted to small maniraptoran theropods, assigned to the Dromaeosauridae incertae sedis and Maniraptora incertae sedis. The dromaeosaurid teeth are characterized by their labiolingually compressed and distally curved crowns that are each equipped with a lingually flexed mesial carina and a distinctly denticulated distal cutting edge. A morphologically aberrant tooth crown (referred to as Maniraptora incertae sedis) has triangular denticles of uneven width, a feature occasionally found in Upper Cretaceous hesperornithiform toothed diving birds, but also in premaxillary teeth of the velociraptorine Nuthetes from the Lower Cretaceous of England.     

Theropod fauna from southern Australia indicates high polar diversity and climate-driven dinosaur provinciality

The Early Cretaceous fauna of Victoria, Australia, provides unique data on the composition of high latitude southern hemisphere dinosaurs. We describe and review theropod dinosaur postcranial remains from the Aptian-Albian Otway and Strzelecki groups, based on at least 37 isolated bones, and more than 90 teeth from the Flat Rocks locality. Several specimens of medium- and large-bodied individuals (estimated up to ~8.5 metres long) represent allosauroids. Tyrannosauroids are represented by elements indicating medium body sizes (~3 metres long), likely including the holotype femur of Timimus hermani, and a single cervical vertebra represents a juvenile spinosaurid. Single specimens representing medium- and small-bodied theropods may be referrable to Ceratosauria, Ornithomimosauria, a basal coelurosaur, and at least three taxa within Maniraptora. Thus, nine theropod taxa may have been present. Alternatively, four distinct dorsal vertebrae indicate a minimum of four taxa. However, because most taxa are known from single bones, it is likely that small-bodied theropod diversity remains underestimated. The high abundance of allosauroids and basal coelurosaurs (including tyrannosauroids and possibly ornithomimosaurs), and the relative rarity of ceratosaurs, is strikingly dissimilar to penecontemporaneous dinosaur faunas of Africa and South America, which represent an arid, lower-latitude biome. Similarities between dinosaur faunas of Victoria and the northern continents concern the proportional representatation of higher clades, and may result from the prevailing temperate-polar climate of Australia, especially at high latitudes in Victoria, which is similar to the predominant warm-temperate climate of Laurasia, but distinct from the arid climate zone that covered extensive areas of Gondwana. Most dinosaur groups probably attained a near-cosmopolitan distribution in the Jurassic, prior to fragmentation of the Pangaean supercontinent, and some aspects of the hallmark 'Gondwanan' fauna of South America and Africa may therefore reflect climate-driven provinciality, not vicariant evolution driven by continental fragmentation. However, vicariance may still be detected at lower phylogenetic levels.     

A new polycotylid plesiosaur from the Late Cretaceous (Turonian) of Morocco

A new Polycotylidae (Plesiosauria) from the Late Cretaceous (Turonian) of southern Morocco is described. Thililua longicollis gen. et sp. nov. is based on a complete cranium and 37 associated vertebrae. It differs from other polycotylids in several cranial and especially vertebral characters, such as the occurrence of 30 cervical vertebrae, whose centra are nearly as long as high and bear laterally longitudinal ridges. Thililua is the first polycotylid hitherto found in Africa and under subtropical palaeolatitudes. To cite this article: N. Bardet et al., C. R. Palevol 2 (2003).     

A new platanaceous genus Tasymia (Angiosperms) from the Turonian of Siberia

A new extinct genus of arborescent angiosperms, Tasymia gen. nov., is described from the Turonian deposits of the upper part of the Simonovo Formation on the Kas River (left-bank tributary of the Yenisei River, Krasnoyarsk Region). The epidermal characters of leaves of the new genus testify to its platanaceous affinity. A comparison with other extinct taxa of the Platanaceae from the Chulym-Yenisei Depression and other regions of the Northern Hemisphere is accomplished.     

Phylloceras (Hypophylloceras) (Ammonoidea) from the Turonian of North Germany

PalZ - Representatives of the Phylloceratida are described from the Turonian of North Germany for the first time. The specimens are referred toPhylloceras (Hypophylloceras) sp. All phylloceratids...     

A New Sauropod Dinosaur from the Middle Jurassic of the United Kingdom

A new record of a sauropodomorph dinosaur is here described from the Middle Jurassic (Aalenian) Saltwick Formation of Whitby (Yorkshire), UK. A single caudal vertebra represents an early sauropodomorph and signifies the earliest recognised eusauropod dinosaur from the United Kingdom. The absence of pleurocoels and a narrow, dorsoventrally deep, but craniocaudally short centrum, suggests a primitive sauropodomorph. Distinct spinopostzygopophyseal laminae rise from the lateral margins of the postzygapophyses and pass caudally along what remains of the neural spine, a character unique to a subgroup of sauropods that includes Barapasaurus, Omeisaurus and other neosauropods and eusauropods. The lack of phylogenetically robust characters in sauropod caudal vertebrae usually makes it difficult to establish affinities, but the absence of mild procoely excludes this specimen from both Diplodocoidea and Lithostrotia. The vertebra cannot be further distinguished from those of a wide range of basal sauropods, cetiosaurids and basal macronarians. However, this plesiomorphic vertebra still signifies the earliest stratigraphic occurrence for a British sauropod dinosaur.     

Preliminary Report on the Courtedoux Dinosaur Tracksite from the Kimmeridgian of Switzerland

In 2002 a new dinosaur tracksite was discovered in calcareous laminites of early Late Kimmeridgian age along the future course of the “Transjurane” highway in Courtedoux, Canton Jura, Northern Switzerland. The site has an extraordinary scientific potential, as the laminites, which have been deposited in an intertidal to supratidal environment, contain at least 6 track-bearing levels in a total thickness of about 1 m. The laminites are being systematically excavated by the “Section de paleontologie” over an area of approximately 1500 m². So far the main track level has been uncovered over an area of about 650 m², which reveals 2 trackways of theropods and 17 trackways of sauropods. The sauropod tracks are the smallest known in the Kimmeridgian so far, and the trackways belong to the ichnogenus Parabrontopodus, which has been revealed for the first time in Switzerland. The tracksite belongs to the “Middle Kimmeridgian megatracksite” sensu Meyer (2000), and represents the most important dinosaur tracksite in Switzerland, perhaps with the potential for development into one of the world's largest sauropod tracksites. It will be protected in situ underneath an especially constructed highway-bridge, thus offering opportunities for future research and the development of an interpretative center for education and tourism.     

Bioactive compounds from Stuhlmannia moavi from the Madagascar dry forest

Bioassay-directed fractionation of the leaf and root extracts of the antiproliferative Madagascar plant Stuhlmannia moavi afforded 6-acetyl-5,8-dihydroxy-2-methoxy-7-methyl-1,4-naphthoquinone (stuhlmoavin, 1) as the most active compound, with an IC₅₀ value of 8.1 μM against the A2780 human ovarian cancer cell line, as well as the known homoisoflavonoid bonducellin (2) and the stilbenoids 3,4,5′-trihydroxy-3′-methoxy-trans-stilbene (3), piceatannol (4), resveratrol (5), rhapontigenin (6), and isorhapontigenin (7). The structure elucidation of all compounds was based on NMR and mass spectroscopic data, and the structure of 1 was confirmed by a single crystal X-ray analysis. Compounds 2?5 showed weak A2780 activities, with IC₅₀ values of 10.6, 54.0, 41.0, and 74.0 μM, respectively. Compounds 1?3 also showed weak antimalarial activity against Plasmodium falciparum with IC₅₀ values of 23, 26, and 27 μM, respectively.     

Euphane triterpenoids of Cassipourea lanceolata from the Madagascar rainforest

Fractionation of an ethanol extract of a Madagascar collection of the leaves and fruit of Cassipourea lanceolata Tul. led to the isolation of three euphane triterpenoids 1–3. The ¹H and ¹³C NMR spectra of all compounds were fully assigned using a combination of 2D NMR experiments, including COSY, TOCSY, HSQC (HMQC), HMBC and ROESY sequences. The three compounds showed weak antiproliferative activities against the A2780 human ovarian cancer cell line, with IC₅₀ values of 25, 25 and 32 μM, respectively.     

Cardenolides of Leptadenia madagascariensis from the Madagascar dry forest

Investigation of the endemic Madagascar plant Leptadenia madagascariensis Decne. (Apocynaceae) for antiproliferative activity against the A2780 ovarian cancer cell line led to the isolation of the four new cardenolides 1-4. The structure elucidations of these compounds were based on analyzes of their 1D and 2D NMR spectra and mass spectrometric data. The cardenolides were strongly antiproliferative to the A2780 ovarian cancer cell line, with IC₅₀ values of 0.18, 0.21, 0.17, and 0.29 ??M line, and to the H460 human lung cancer cell line, with IC₅₀ values of 0.16, 0.68, 0.37, and 0.48 ??M, respectively.     

Platidiid brachiopods from the Middle Turonian of the Bohemian Cretaceous Basin (Czech Republic)

Small-sized platidiid brachiopods as yet unknown in the Bohemian Cretaceous Basin are described from the early Middle Turonian (Marginotruncana schneegansi Zone) nearshore deposits of the Zbyslav locality northeast of Čáslav. The studied specimens probably belong to the genusAemula Steinich, 1968, but cannot be precisely determined due to the poor preservation of internal characters. Most probably, they represent the stratigraphically earliest known populations of the family Platidiidae.     

Four Miniature Species of Aloe from Madagascar

Summary.  The habitats and distribution of four Aloe species from Madagascar are described and illustrated, and their conservation status is discussed.     

Sampling a diverse flora for novel biochemicals: An analysis of NCI collections from Madagascar

An analysis of the taxonomic composition of 6,496 samples of plants collected for the National Cancer Institute is conducted and the results are presented. The results show that collecting has been highly biased towards woody plant families, as these species are often abundant, they yield samples of multiple parts, and it is often easy to collect sufficient material for isolation of chemicals present in low concentration. Conversely, herbaceous plants that are small or grow in sparse populations are underrepresented in collections. Three of the ten generically most diverse families in Madagascar have not been sampled, and of these ten families, only Rubiaceae and Euphorbiaceae have had greater numbers of samples collected than predicted if collecting was random. The causes of this bias are discussed, and solutions to ensure that bioprospecting efforts gather samples reflective of the diversity present are presented.

---

Echantillonage d’une flore diverse pour des nouveaux composes biochimiques: Une Analyze des Collections de NCI Recoltees a Madagascar

Zusammenfassung  Une analyze de la composition taxonomique de 6496 échantillons recoltés pour le National Cancer Institute est conduite et les resultants obtenus montrent que la récolte a été foretment biaisée, tendant pour une forte proportion des families des plantes ligneuses don’t les espèces sont souvent abondantes, peuvent fournir plusieurs sortes d’échantillon et souvent permettent facilement de collecter suffisament des matérielles pour l’isolation des composes chimiques presents à faible concentration. Contrairement, les plantes herbacées que sont de petites tailles our qui poussent avec des populations clairsemées sont sous representées dans les collections. Trois parmi les dix families génériquement les plus diversifies n’ont pas été recoltées, et de ces dix families, seules les Rubiaceae el les Euphorbiaceae ont eu les plus grands nombres d’échantillons que prévus si la récolte a été fait au hazard. Les cause de cette disproportion sont discutées et les solutions pour assurer que les efforts de bioprospection rassemblent des échantillons reflétant la diversité présente sont presentées.