Neue Laubmoosfunde aus Baltischem Bernstein

Several fossil mosses from Baltic amber are described, including a specimen of Calomnion and one of Atrichum. The genus Calomnion, presently distributed only in the southern hemisphere, is reported for the first time as a fossil. All records of fossil mosses from the Tertiary in Europe are listed and discussed.     

A comparative study of frontal bone morphology among Pleistocene hominin fossil groups

Features of the frontal bone that are conventionally used to distinguish among fossil hominin groups were quantitatively examined. Fifty-five fossil crania dating from the early to the late Pleistocene were analyzed. Using a modified pantograph, outlines of the frontal bone were collected along the midsagittal and two parasagittal planes. The profile from nasion to bregma, as well as two profiles above the medial and lateral sections of the orbit, respectively, extending from the orbital margin to the coronal suture were traced. The outlines were measured using Elliptical Fourier Function Analysis (EFFA), which enabled a quantification of aspects of the frontal bone that have historically been described primarily in nonmetric or linear terms. Four measurements were obtained: 1) overall morphology as expressed in the Fourier harmonic amplitudes; 2) maximum projection of the supraorbital torus at three points along the browridge (glabella and the medial and lateral aspects of the torus above the orbit); 3) maximum distance of the frontal squama from the frontal chord, capturing forehead curvature; and 4) nasion-bregma chord length. The results indicate that the midsagittal profile is significantly different among all Pleistocene groups in analyses that include both size and shape, as well as size-adjusted data. Homo erectus is significantly different from the late Pleistocene groups (Neandertals and early modern H. sapiens) in glabellar projection. Anatomically modern humans are significantly different from all other groups in both raw and size-standardized analyses of all three outlines that captured overall morphology, as well as forehead curvature and lateral supraorbital torus prominence, and middle Pleistocene Homo are significantly different in both medial and lateral overall parasagittal form. However, for the majority of analyses there were no significant differences among the Pleistocene archaic groups in supraorbital torus projection, frontal squama curvature, nasion-bregma chord length, or overall frontal bone morphology.     

Die Bedeutung desRamus palatinus für die Vomerspangenbildung beiSalamandra salamandra (L.)

Zusammenfassung BeiSalamandra salamandra wurde der Einfluß desRamus palatinus (VII.) und der Lage des Vomer auf die sich während der Metamorphose bildende Vomerspange untersucht. Eine Durchtrennung des Nerven stört das Wachstum der Spange nicht, da der Nerr rasch regeneriert. Nach Durchtrennung und Verlagerung desRamus palatinus bildet sich jedoch keine Vomerspange, ebenso nicht nach Exstirpation eines Teiles des Nerven. Nach Entnahme von Nervenstücken nach Beginn der Metamorphose entwikkeln sich Teilspangen. Das Vorhandensein eines intaktenRamus palatinus ist offenbar Voraussetzung für das Auswachsen der neuen knöchernen Vomerspange. Die Richtung des Spangenwachstums ist nicht von einer bestimmten Lage des Larvenvomer abhängig.

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The significance of theramus palatinus to the development of the vomerine bar inSalamandra salamandra (L.)

Summary The influence of theramus palatinus (VII.) and the postion of the vomer on the vomerine bar, which develops during metamorphosis, was studied by various amputation procedures. Cutting off the nerve cord does not prevent the development of the vomerine bar, as the nerve soon regenerates, whereas cutting off and displacement as well as the removal of portions of theramus palatinus do prevent development. Removal of portions of the nerve cord during metamorphosis produces only parts of the vomerine bar. Obviously an intact ramus palatinus is necessary for the outgrowth of the novel osseous vomerine bar. The course of this outgrowth is independent of the position of the larval vomer.

Für die Unterstützung bei der Anfertigung dieser Arbeit danke ich herzlich Herrn Professor Dr. H. Hartwig, Zoologisches Institut der Universität Köln     

福建漳浦中中新世几种藓类植物研究*

亚洲新生代藓类植物化石非常稀少,漳浦琥珀是目前已知的我国低纬度地区唯一含苔藓植物化石的新生代琥珀矿床。漳浦琥珀源自中中新世气候适宜期(~14-17 Ma)的龙脑香树脂,温暖潮湿的热带季雨林气候和广泛分布的龙脑香科植物,为藓类植物的生长、多样性演化和三维立体保存提供了条件。本研究共报道了漳浦县中中新世藓类植物化石3个属种,包括:白发藓属Leucobryum Hampe、牛舌藓属Anomodon Hook.et Taylor和扁枝藓属Homalia(Brid.)B.S.G.。首次利用三维X射线断层扫描技术(Micro-CT)研究了白发藓属化石,发现其与现生种短枝白发藓Leucobryum humillimum Cardot非常相似,因此将其命名为短枝白发藓(相似种)Leucobryum cf.humillimum。此外,当前牛舌藓属Anomodon和扁枝藓属Homalia化石是东亚地区的首例记录。漳浦琥珀中的藓类植物化石揭示了中中新世时期苔藓植物的多样性,丰富了东亚低纬度地区新生代苔藓植物的化石记录。     

First record of Cercidiphylloxylon (Cercidiphyllaceae) from the Palaeocene of Fushun,NE China

Abstract Cercidiphylloxylon spenceri (Brett) Pearson is described from the Lizigou Formation, Palaeocene in China. The growth rings are distinct; pores are diffuse, solitary, with somewhat angular outlines in cross section; vessel elements long with long scalariform perforation plates; intervessel pitting is opposite to scalariform; fiber‐tracheids are present; axial parenchyma is scarce; rays are mostly biseriate and heterogeneous. All wood characters of the fossil specimen fall into the range of those of extant Cercidiphyllum (Cercidiphyllaceae). The finding is one of the earliest fossil wood records of Cercidiphyllaceae.     

An early Cretaceous termite from southern England (Isoptera: Hodotermitidae)

Valditermes brenanae gen. et sp.n. is described from the Weald Clay (Neocomian: (?) Hauterivian; c. -120 million years) of Surrey; it is the earliest described termite and social insect. Valditemes is referred to the extinct subfamily Cretatermitinae of the family Hodotermitidae, previously known only from a single specimen (Cretatermes carpenteri Emerson, 1967) from the Ceno- manian (c. -95 m.y.) of Labrador. Valditermes represent a more generalized condition than Cretatermes and may be the ancestor of Cretatemes. The geo- logical occurrence of Valditermes, other records o f Cretaceous termites, and finds of fossil termites in Britain are summarized.     

Fossil flowers and pollen ofLauraceae from the Upper Cretaceous of New Jersey

A fossil trimerous flower from the Turonian (ca. 90 MYBP, Upper Cretaceous) of New Jersey is described as a new genus in the familyLauraceae. The fossil flower is charcoalified and preserved in exceptional detail. This fossil specimen is particularly remarkable in that several pollen grains have been preserved; pollen grains ofLauraceae generally have very thin exine and are rarely preserved in the fossil record. Although the specimen is incomplete and lacks anthers, there are sufficient structural details preserved to permit an assignment to theLauraceae, as well as comparisons with the tribePerseeae. This new genus provides an important addition to our knowledge of systematic and structural diversity in CretaceousLauraceae.     

Further fossil cephalopods from Jamaica

Fossil cephalopods are rare in the Antillean region. A deformed conch of a kossmaticeratid ammonite,Pseudokossmaticerasl sp., from the Maastrichtian of the Blue Mountain Inlier is the first ammonite from southeastern Jamaica. This tentative systematic assignment is in agreement with the age otherwise assigned to these rocks.Cimomia sp. cf.C. vaughani (Gardner) is a hercoglossid nautiloid from the Lower-Middle Eocene Chapelton Formation of western central Jamaica. This is only the fourth nautiloid from this unit; all previous records were ofHercoglossa sp. The specimen is unusual amongst Antillean fossil cephalopods in including the sponge boringEntobia isp., probably indicating a period of post-mortem residence on the sea floor.      

Impact de l’imagerie hybride TEMP/TDM dans le diagnostic et la prise en charge de l’ostéome ostéoïde

IntroductionThe osteoid osteoma is a major bone benign tumors in children. It is more common in boys. The femoral and tibial locations account for 50% of cases. Clinically, it is revealed by nocturnal pain relieved by aspirin. The pain may precede by several months the radiographic abnormality. The purpose of our work is to elucidate the contribution of SPECT/CT in addition to the planar bone scintigraphy in the diagnosis and treatment of osteoid osteoma about two cases.Case reportClinical case No. 1: a 10-year-old child who presented a limp nocturnal pain in the left hip evolving for 4 months. The radiograph of the pelvis showed bone condensation subtrochanteric left femur. SPECT/CT showed an image for an osteoid osteoma. Surgical resection of the home revealed in the histological study an osteoid osteoma of the left femoral neck. The evolution was marked by an immediate pain relief and full recovery of the left lower limb mobility. Clinical case No. 2: an 11-year-old child who had a limp nocturnal pain at the upper end of the left femur evolving for 2 months. The pain was paroxysmal, relieved by salicylates. The X-ray of the pelvis showed a metaphyseal image with peripheral condensation and thickening of the cortex. SPECT/CT showed an image for an osteoid osteoma. The intervention was a tumor excision resection. Histopathological examination revealed a small nidus consistent with an osteoid osteoma. The evolution was marked by an immediate pain relief and normalization of the mobility of the left lower limb.DiscussionThe SPECT/CT can increase the sensitivity and specificity of planar bone scintigraphy. It confirms the location of osteoid osteoma and defines its anatomical relationships in order to optimize surgical management.ConclusionThe SPECT/CT contributes significantly to the diagnosis of osteoid osteoma when radiological images are atypical or unusual clinical expression.     

The evolution,development and skeletal identity of the crocodylian pelvis: Revisiting a forgotten scientific debate

Unlike most tetrapods, in extant crocodylians the acetabulum is formed by only two of the three skeletal elements that constitute the pelvis, the ilium, and ischium. This peculiar arrangement is further confused by various observations that suggest the crocodylian pelvis initially develops from four skeletal elements: the ilium, ischium, pubis, and a novel element, the prepubis. According to one popular historical hypothesis, in crocodylians (and many extinct archosaurs), the pubis fuses with the ischium during skeletogenesis, leaving the prepubis as a distinct element, albeit one which is excluded from the acetabulum. Whereas the notion of a distinct prepubic element was once a topic of considerable interest, it has never been properly resolved. Here, we combine data gleaned from a developmental series of Alligator mississippiensis embryos, with a revised interpretation of fossil evidence from numerous outgroups to Crocodylia. We demonstrate that the modern crocodylian pelvis is composed of only three elements: the ilium, ischium, and pubis. The reported fourth pelvic element is an unossified portion of the ischium. Interpretations of pelvic skeletal homology have featured prominently in sauropsid systematics, and the unambiguous identification of the crocodylian pubis provides an important contribution to address larger scale evolutionary questions associated with locomotion and respiration. J. Morphol. , 2012. © 2012 Wiley Periodicals, Inc.     

Non‐traumatic bone infection in stegosaurs from Como Bluff,Wyoming

Palaeopathologies are relatively common in the fossil record; however, bone histological analyses of these are rare as they are more commonly discovered and described using radiological scans. Here, we describe the bone microstructure of infectious abscesses (osteomyelitis) in the long bones of two Stegosaurus individuals from the Como Bluff area of the Late Jurassic Morrison Formation. Multiple lytic, geographical lesions filled with reactive lamellar bone occur in a femur of a juvenile specimen. A single lesion was found in an adult tibia. This lesion is characterized by the presence of spiculated periosteal reactive growth perpendicular to the bone surface and the formation of new trabeculae within the lesion.     

Fossil papio cranium from !Ncumtsa (Koanaka) Hills, western Ngamiland, Botswana

Three fossils, a cranium of Papio, a cercopithecid frontal bone, and a mandible of juvenile Papio, have been recovered from cave deposits in the !Ncumtsa (Koanaka) Hills of western Ngamiland, Botswana. These specimens are significant because well‐preserved crania of Papio are extremely rare in the fossil record outside of South Africa and because this is the first report of fossil primate cranial remains from Botswana. Thermoluminescence dating of surrounding cave matrix indicates an age of ≥317 ± 114 ka, within the Middle Pleistocene, although it may be older. Based on univariate and multivariate analyses, the adult !Ncumtsa specimen falls within the range of variation seen in extant forms of Papio, yet is distinct from any living species/subspecies and represents a new taxon, named here as a new subspecies of Papio hamadryas—Papio hamadryas botswanae. Am J Phys Anthropol, 2012. © 2012 Wiley Periodicals, Inc.     

Monitor lizards: a pan-African check-list of their zoogeography (Sauria: Varanidae: Polydaedalus)

Aim This goal of this paper is to present an up‐to‐date, accurate check‐list and distribution of the monitor lizards on the African continent. No such list of their distribution has been attempted since Robert F. Mertens' (1942) treatise (Abhandlungen Senckenbergischen Naturforschenden Gesellschaft, 462 , 465 , 466 ). Location The localities included herein are all countries on the African continent, and adjacent islands, with a list of Varanus known to Yemen and Saudi Arabian Republics included for clarity. One fossil Varanus rusingensis is included, as it is the first, and only described, fossil African Varanus known. Methods Locality records were reviewed from literature sources, museum voucher specimens, personal comments, field observations and photographic records. Results A summation of 3,268 locality records are included herein from the methods listed, with maps depicting these records. Main conclusions From the locality records listed herein, it is evident that the Nile monitor (V. niloticus) has the widest distribution, and that the Yemen monitor (V. yemenensis) has the most restricted distribution; paradoxically, both features may be indicative of their relic habitation on the African continent.     

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

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

A case of mistaken identification of an amber fossil male strepsipteran (Insecta: Strepsiptera)

A well-preserved specimen of amber Strepsiptera was erroneously described as Stylops neotropicallis Kogan and Poinar, 2010. The taxonomic position of the species was based on a count of six antennomeres (typical of the Stylopidae); however, further observations showed that there are actually seven antennomeres, which places the fossil in the family Myrmecolacidae, and it is herein redescribed in the genus Palaeomyrmecolax Kulicka, 2001. Furthermore, nuclear magnetic resonance spectroscopy analysis of a sample of the amber piece containing the fossil revealed that it was Baltic rather than Dominican amber as originally thought. The fossil was compared with another specimen from Baltic amber in the Poinar collection, which shows close affinity to Palaeomyrmecolax succineus Kulicka, 2001, the type species of the genus. Palaeomyrmecolax neotropicallis (n.comb.) differs from that specimen and seems to differ also from the other four species in the genus Palaeomyrmecolax.     

New dates for the Fontéchevade (Charente, France) Homo remains

Homo I from the site of Fontéchevade, France, has long been an anomaly in the European fossil record. The specimen is a fragment of human frontal bone that lacks a supraorbital torus and appears to belong to an anatomically modern Homo sapiens. However, the level from which it was recovered in 1947 was dated on the basis of associated faunal and lithic material to the last interglacial or earlier. As a result, Homo I has been interpreted, among other things, as a representative of a pre-sapiens lineage in Europe. This paper reports on recent ESR and radiocarbon dates that indicate that the specimen almost certainly dates to oxygen isotope stage 3, which brings it in line with other evidence for the entry of modern Homo sapiens into Europe.     

TAXODIACEOUS BARK FROM THE UPPER CRETACEOUS OF ALBERTA

The structure of a piece of silicified bark of Taxodioxylon gypsaceum from near Medicine Hat in Southern Alberta is described. The fossil specimen probably came from Upper Cretaceous beds. The fossil shows affinities with the bark of modern Sequoia. Vectia luccombensis Stopes (1915) from the Lower Greensand (Aptian) of England probably constitutes an isolated piece of taxodiaceous bark, similar to the inner bark of the Alberta specimen.     

Trachypithecus auratus sangiranensis,A New Fossil Monkey from Sangiran,Central Java,Indonesia

We describe a new extinct subspecies of the Javan lutung—Trachypithecus auratus sangiranensis—based on an isolated, tooth-bearing upper jaw. The specimen was in volcanic breccia situated between the Lower Pucangan and the Upper Kalibeng Formations 500 m south of the village of Sangiran, near Surakarta, central Java, Indonesia. The new fossil monkey bears morphological similarities to the two living species of leaf monkey from Java, Presbytis comata comata and Trachypithecus auratus auratus, and to the Middle Pleistocene form, Trachypithecus cristatus [=auratus] robustus, from Tegoean, central Java. It is significantly larger than any of these forms, and differs from them in details of dental anatomy. Because the greatest number of similarities are between the new fossil and Trachypithecus auratus subspecies, we designated the specimen as T. a. sangiranensis. The geochronological age of the breccia from which the fossil came, is 1.9± 0.05 Ma (million years), making T. a. sangiranensis one of the oldest fossil monkeys from eastern Asia.     

Abnormalities in flatfishes of the south‐west Atlantic Ocean

Five adult paralichthyid specimens with various kinds of abnormalities are reported from the south‐west Atlantic Ocean. These abnormal flatfish specimens represent the first records of wholly ambicoloured Paralichthys orbignyanus specimens having a deep notch between the eye and dorsal fin and a partially albinistic specimen having skeletal deformities and only the second record of an almost totally ambicoloured specimen. We also report the first observation of reversal in Paralichthys patagonicus and an almost totally ambicoloured, reversed Xystreurys rasile.