Résumé : (Exhibitions) "Patterns Past and Present: Arts of Panama" at the Samuel P. Harn Museum of Art. The creature on this mola blouse has both human and animal features. It appears to be a woman with webbed hands and feet and amphibious limbs, suggesting she is part frog or turtle. The pointed teeth suggest she may be a nia, or demon. Alternatively, she may be a beneficent being, as the xray-like view of the ribcage may be an allusion to the use of turtle bones in healing practices.
An adhesive sticker (removed) reads b15.
(Internal Comments) removed for exhibit Patterns Past & Present at Harn Museum
Recto color: olive green Verso panel missing
Panama -- Kuna Yala -- San Blas Islands

Droits : The University of Florida George A. Smathers Libraries respect the intellectual property rights of others and do not claim any copyright interest in this item. This item may be protected by copyright but is made available here under a claim of fair use (17 U.S.C. §107) for non-profit research and educational purposes. Users of this work have responsibility for determining copyright status prior to reusing, publishing or reproducing this item for purposes other than what is allowed by fair use or other copyright exemptions. Any reuse of this item in excess of fair use or other copyright exemptions requires permission of the copyright holder. The Smathers Libraries would like to learn more about this item and invite individuals or organizations to contact Digital Services (UFDC@uflib.ufl.edu) with any additional information they can provide.
2013.9.60
http://ufdc.ufl.edu/AA00018001/00001

Éditeur(s) : HAL CCSD Wiley
Résumé : International audience
The evolutionary origin of teeth from dermal denticles (odontodes) that developed in the mouth cavity, designated as outside-in hypothesis, has long been undisputed. The outside-in hypothesis is based on the conclusion that dermal denticles and teeth fulfil the criteria of homology in an exemplary manner. Over the past 15 years, this hypothesis has been challenged. Proponents of the alternative inside-out hypothesis suggest that teeth did not evolve from dermal denticles, that they are of endodermal origin (forming in conjunction with neural crest-derived mesenchyme) and that they evolved several times independently in different lineages of vertebrates. Key arguments for the inside-out hypothesis are mineralized structures of conodonts that are accepted as teeth, the exclusive acceptance of placoderm pharyngeal denticles as teeth, together with the rejection of the presence of teeth in basal placoderms. We summarize the results of recent studies that have been triggered by the fruitful discussion between the two conflicting hypotheses. New findings support the traditional outside-in hypothesis: the mineralized elements of conodonts are not teeth, and the oral cusps in basal placoderms are true teeth. Furthermore, new developmental and molecular data clarify homology between teeth and dermal denticles. Today a new synthesis is emerging about the evolutionary origin of teeth from dermal denticles and about the unity of the elements of the dermal skeleton.
ISSN: 0175-8659

hal-01545480
https://hal.archives-ouvertes.fr/hal-01545480
DOI : 10.1111/jai.12532

Résumé : Herbáceaperenne, aromática. Tallos erguidos o ascendentes de 30 a 90 cm, ramificados, glabros. Hojas lanceoladas, agudas, limbo punteadas. Flores en espigas grandes terminales, de 2.5 a 7.5 cm, la central es sobrepasada por las laterales; cáliz glabro, con dientes agudos, por lo regular ciliados; corola púrpura, raramente blanca, glabra. La existencia de variedades dentro de la especie puede variar la descripción botánica típica, aquí presentada.
Herbacéepérenne, aromatique. Tiges dressées ou ascendantes de 30 à 90 cm, ramifiées, glabres. Feuilles lancéolées, aiguës, limbe gaufré. Fleurs en longs épis terminaux, de 2,5 à 7,5 cm, celle du centre étant dépassée par les fleurs latérales; calice glabre, avec dents aiguës, en général ciliées; corolle pourpre, rarement blanche, glabre. L’existence de variétés à l’intérieur de l’espèce peut nuancer la description botanique typique indiquée ci-dessus.
Perennial aromatic herb.  Stems erect or ascending, 30-90 cm long, branched, glabrous; leaves lanceolate, acute, blade punctate; flowers in large terminal spikes, 2.5-7.5 cm long, the ones at the sides being longer than the one in the middle, calyx glabrous, with acute teeth, usually ciliate; corolla purple, rarely white, glabrous. The typical botanical description may vary due to the existence of varieties within the species.
Originaria de Europa, actualmente es cosmopolita.
Originaire d’;Europe, actuellement cultivée dans le monde entier.
Native to Europe, now cosmopolitan.

http://www.tramil.net/fototeca/plant379

Éditeur(s) : HAL CCSD Wiley-Blackwell Wiley
Résumé : The Late Early-to-Early Middle Eocene Zegdoumyidae are the oldest representatives of the order Rodentia to be known in Africa thus far. Despite the fragmentary nature of their fossil record, these early African rodents have been central in discussions surrounding the early evolutionary history of the Anomaluroidea clade (the living forms of which are the ‘scaly-tailed squirrels’, i.e. Anomaluridae). Here, we describe new dental remains attributable to Zegdoumys sbeitlai, a zegdoumyid from Tunisia (Djebel Chambi, CBI-1) dated at ca 50–45 Ma. The original material referred to this taxon was limited to four teeth documenting few dental loci. The new gathered material comprises practically all dental loci (except P4), thereby allowing a better description and characterization of this taxon. This Tunisian species is clearly distinct from its roughly coeval Algerian counterpart (Z. lavocati) or from the younger species recorded from Namibia (Z. namibiensis). We investigated the phylogenetic positions of Z. sbeitlai and the Zegdoumyidae in a high-level rodent phylogeny with a cladistic assessment of the dental evidence. Our results show that zegdoumyids represent the earliest offshoots (pectinately arranged) of a large clade that also encompasses the more advanced Eocene anomaluroids (here named Nementchamyidae), the Miocene Nonanomaluridae, and the stem and crown Anomaluridae. In this phylogenetic context, the species of Zegdoumys are the basalmost members of this large Anomaluroidea clade. Zegdoumyid taxa are therefore the oldest stem anomaluroid candidates, a statement which strengthens support for the hypothesis of the great antiquity of the Anomaluroidea clade in Africa. From a historical biogeography perspective, this assumption suggests that anomaluroids invaded Asia from Afro-Arabia sometime during the Middle Eocene, a dispersal event which was likely concomitant but opposite to the dispersals envisaged for the hystricognathous rodents and anthropoid primates from Asia to Afro-Arabia.
ISSN: 0300-3256

hal-01172007
https://hal.archives-ouvertes.fr/hal-01172007
DOI : 10.1111/zsc.12095

Éditeur(s) : HAL CCSD The Company of Biologists
Résumé : International audience
The ability to produce sound has been known for decades inBalistidae. Sounds of many species have been recorded and a varietyof sound-producing mechanisms have been proposed, includingteeth stridulation, collision of the buccal teeth and movements of thefins. The best-supported hypothesis involves movements of thepectoral fin against the lateral part of the swimbladder, called adrumming membrane. In this study, we describe for the first time thesounds made by the blackbar triggerfish Rhinecanthus aculeatus,which are like short drum rolls with an average duration of 85 ms,193 Hz dominant frequency and 136 dB SPL level at 3 cm distance.The sounds are a series of pulses that result from alternate sweepingmovements of the right and left pectoral fins, which push a system ofthree scutes that are forced against the swimbladder wall. Pulses fromeach fin occur in consecutive pairs. High-speed videos indicate thateach pulse consists of two cycles. The first part of each cyclecorresponds to the inward buckling of the scutes, whereas the secondpart of the cycle corresponds to an apparent passive recoil of thescutes and swimbladder wall. This novel sound productionmechanism is probably found in many members of Balistidaebecause these peculiar scutes occur in other species in the family.Comparison of sound characteristics from fishes of different sizesshows that dominant frequency decreases with size in juveniles butnot in adults.KEY WORDS: Acoustic, Communication, Swimbladder
ISSN: 00220949

hal-01472506
https://hal-univ-perp.archives-ouvertes.fr/hal-01472506
DOI : 10.1242/jeb.146514

Éditeur(s) : Elsevier Science Bv
Résumé : The breakup of Pangea and onset of growth of the Pacific plate led to several paleoenvironmental feedbacks, which radically affected paleoclimate and ocean chemistry during the Jurassic. Overall, this period was characterized by intense volcanic degassing from large igneous provinces and circum-Panthalassan arcs, new oceanic circulation patterns, and changes in heat and humidity transports affecting continental weathering. Few studies, however, have attempted to unravel the global interactions linking these processes over the long-term. In this paper, we address this question by documenting the global changes in continental drainage and surface oceanic circulation for the whole Jurassic period. For this purpose, we present 53 new neodymium isotope values (εNd(t)) measured on well-dated fossil fish teeth, ichthyosaur bones, phosphatized nodules, phosphatized ooids, and clastic sediments from Europe, western Russia, and North America. Combined with an extensive compilation of published εNd(t) data, our results show that the continental sources of Nd were very heterogeneous across the world. Volcanic inputs from a Jurassic equivalent of the modern Pacific Ring of Fire contributed to radiogenic εNd(t) values (− 4 ε-units) in the Panthalassa Ocean. For the Tethyan Ocean, the average surface seawater signal was less radiogenic in the equatorial region (− 6.3), and gradually lower toward the epicontinental peri-Tethyan (− 7.4), western Russian (− 7.4) and Euro-Boreal seas (− 8.6). Different Nd sources contributed to this disparity, with radiogenic Nd influxes from westward Panthalassan currents or juvenile volcanic arcs in open oceanic domains, and substantial unradiogenic inputs from old Laurasian and Gondwanan shields for the NW Tethyan platforms. Overall, the εNd(t) values of Euro-Boreal, peri-Tethyan, and western Russian waters varied quite similarly through time, in response to regional changes in oceanic circulation, paleoclimate, continental drainage, and volcanism. Three positive shifts in εNd(t) values occurred successively in these epicontinental seas during the Pliensbachian, in the Aalenian-Bathonian interval, and in the mid-Oxfordian. The first and third events are interpreted as regional incursions of warm surface radiogenic currents from low latitudes. The Aalenian-Bathonian shift seems linked to volcanic outbursts in the NW Tethys and/or circulation of deep currents resulting from extensional events in the Hispanic Corridor and reduced influences of boreal currents crossing the Viking Corridor. In contrast, the εNd(t) signals decreased and remained very low (< − 8) during the global warming events of the Toarcian and Late Oxfordian - Early Tithonian intervals. In these greenhouse contexts, a latitudinal expansion of humid belts could have extended the drainage pathways toward boreal Nd sources of Precambrian age and increased the supply of very unradiogenic crustal-derived inputs to seawater. Finally, a brief negative εNd(t) excursion recorded in parallel with regional drops in seawater temperature suggests that southward circulation of cold unradiogenic Arctic waters occurred in the NW Tethys in the Callovian - Early Oxfordian. All these results show that changes in surface oceanic circulation resulting from the Pangean breakup could have regionally impacted the evolution of seawater temperatures in the NW Tethys.
Gondwana Research (1342-937X) (Elsevier Science Bv), 2015-06 , Vol. 27 , N. 4 , P. 1599-1615

Droits : 2014 International Association for Gondwana Research. Published by Elsevier B.V. All rights reserved
http://archimer.ifremer.fr/doc/00179/29015/27443.pdf
DOI:10.1016/j.gr.2014.02.006
http://archimer.ifremer.fr/doc/00179/29015/

Éditeur(s) : HAL CCSD SAGE Publications (UK and US)
Résumé : International audience
Enamel and enameloid, the highly mineralized tooth-covering tissues in living vertebrates, are different in their matrix composition. Enamel, a unique product of ameloblasts, principally contains enamel matrix proteins (EMPs), while enameloid possesses collagen fibrils and probably receives contributions from both odontoblasts and ameloblasts. Here we focused on type I collagen (COL1A1) and amelogenin (AMEL) gene expression during enameloid and enamel formation throughout ontogeny in the caudate amphibian, Pleurodeles waltl. In this model, pre-metamorphic teeth possess enameloid and enamel, while post-metamorphic teeth possess enamel only. In first-generation teeth, qPCR and in situ hybridization (ISH) on sections revealed that ameloblasts weakly expressed AMEL during late-stage enameloid formation, while expression strongly increased during enamel deposition. Using ISH, we identified COL1A1 transcripts in ameloblasts and odontoblasts during enameloid formation. COL1A1 expression in ameloblasts gradually decreased and was no longer detected after metamorphosis. The transition from enameloid-rich to enamel-rich teeth could be related to a switch in ameloblast activity from COL1A1 to AMEL synthesis. P. waltl therefore appears to be an appropriate animal model for the study of the processes involved during enameloid-to-enamel transition, especially because similar events probably occurred in various lineages during vertebrate evolution.
ISSN: 0022-0345

hal-01545475
https://hal.archives-ouvertes.fr/hal-01545475
DOI : 10.1177/0022034514526236

Éditeur(s) : HAL CCSD American Academy of Pediatrics
Résumé : International audience
Vitamin D is an essential hormone for calcium gut absorption. It is also involved in child growth, cancer prevention, immune system responses, and tooth formation. Due to inadequate vitamin D intake and/or decreased sunlight exposure, vitamin D deficiency has resurfaced in developed countries despite known inexpensive and effective preventive methods. Vitamin D deficiency is a common cause of rickets, a condition that affects bone development in children and that can have serious dental complications. Deficiency during pregnancy can cause enamel hypoplasia of primary teeth. Enamel regeneration is currently impossible; hypoplasia is therefore irreversible, and once affected, teeth are prone to fast caries development. Deficiency during early childhood can affect permanent teeth and ensuing caries can sometimes lead to tooth loss at a young age. Oral manifestations of rickets should be diagnosed early by both physicians and dentists to prevent severe dental complications. This case study presents 2 young girls with rickets in early childhood who suffered from subsequent serious tooth decay.
ISSN: 0031-4005

hal-01545477
https://hal.archives-ouvertes.fr/hal-01545477
DOI : 10.1542/peds.2013-0733

Éditeur(s) : HAL CCSD Société des amis du Musée national de préhistoire et de la recherche archéologique — SAMRA
Résumé : International audience
Lithic technology studies have been late developed in the Antilles. The first important works about the knapping technology of the first agro-ceramist cultures (saladoid) have shown the use of the bipolar technique. A new research program based on the analysis of cedrosan and huecan saladoid lithic collections from Martinique and Guadeloupe, gave us the possibility to confirm and refine those first data. The technological analysis, associated to an experimentation program defined to help us to characterize the striking techniques used, have shown a systematic use of the bipolar technique for the débitage of good quality raw materials. The chaînes opératoires of reduction are highly efficient producing a set of small flakes. The morphology of those flakes, linked to the use of the bipolar technique, is perfectly adapted to their use as manioc grater teeth.
L'étude des restes de débitage a connu un développement tardif dans les Antilles. Les premiers travaux importants sur les débitages des premières cultures formatives (saladoïde) ont mis en évidence l'utilisation de la percussion posée sur enclume. Le développement d'un programme de recherche sur les séries lithiques saladoïdes cedrosanes et huecanes de Martinique et de Guadeloupe nous a permis de confirmer et d'affiner ces premières observations. L'analyse technologique, complétée par un programme expérimental destiné à éclaircir la question des techniques de percussion, a montré l'existence d'une utilisation systématique de la percussion posée sur enclume pour l'exploitation de matières premières de bonne qualité. Les chaînes opératoires de débitage sont d'une grande efficacité et permettent très rapidement d'obtenir des séries de petits éclats faiblement standardisés. Les caractéristiques morphologiques de ces éclats, étroitement liées à la technique de percussion employée, en font des supports parfaitement adaptés à une utilisation comme dents de râpes à manioc.
ISSN: 1145-3370

hal-00974212
https://hal.univ-antilles.fr/hal-00974212

Éditeur(s) : Springer
Résumé : Pearl oysters belonging to the genus Pinctada (Bivalvia: Pteriidae) are widely distributed between the Indo-Pacific and western Atlantic. The existence of both widely distributed and more restricted species makes this group a suitable model to study diversification patterns and prevailing modes of speciation. Phylogenies of eight out of the 11 currently recognised Pinctada species using mitochondrial (cox1) and nuclear (18S rRNA) data yielded two monophyletic groups that correspond to shell size and presence/absence of hinge teeth. Character trace of these morphological characters onto the molecular phylogeny revealed a strong correlation. Pinctada margaritifera appears polyphyletic with specimens from Mauritius grouping in a different clade from others of the French Polynesia and Japan. Hence, P. margaritifera might represent a species complex, and specimens from Mauritius could represent a different species. Regarding the putative species complex Pinctada fucata/Pinctada martensii/Pinctada radiata/Pinctada imbricata, our molecular analyses question the taxonomic validity of the morphological characters used to discriminate P. fucata and P. martensii that exhibited the lowest genetic divergence and are most likely conspecific as they clustered together. P. radiata and P. imbricata were recovered as monophyletic. The absence of overlapping distributions between sister lineages and the observed isolation by distance suggests that allopatry is the prevailing speciation mode in Pinctada. Bayesian dating analysis indicated a Miocene origin for the genus, which is consistent with the fossil record. The northward movement of the Australian plate throughout the Miocene played an important role in the diversification process within Pinctada.
Marine Biotechnology (1436-2228) (Springer), 2011-04 , Vol. 13 , N. 2 , P. 181-192

Droits : Springer Science+Business Media, LLC 2010
http://archimer.ifremer.fr/doc/00035/14635/14015.pdf
DOI:10.1007/s10126-010-9278-y
http://archimer.ifremer.fr/doc/00035/14635/

Éditeur(s) : HAL CCSD Public Library of Science
Résumé : International audience
The extinct Odontopterygiformes are the sole birds known to possess strong and sharp bony pseudoteeth, the shape and location of which are closely mimetic of real teeth. The structure of the pseudoteeth is investigated here in a late Pliocene/early Pleistocene species, Pelagornis mauretanicus, using X-ray microtomography and thin sections. The results are interpreted with regard to the pseudotooth mode of growth, and have implications concerning aspects of Pelagornis ecology. The larger pseudoteeth are hollow and approximately cone-shaped, and the smaller ones are rostro-caudally constricted. The walls of pseudoteeth are composed of bone tissue of the fibro-lamellar type, which is intensively remodeled by Haversian substitution. The jaw bones display the same structure as the pseudoteeth, but their vascular canals are oriented parallel to the long axis of the bones, whereas they are perpendicular to this direction in the pseudoteeth. There is no hiatus or evidence of a fusion between the pseudoteeth and the jaw bones. Two possible models for pseudotooth growth are derived from the histological data. The most plausible model is that pseudotooth growth began after the completion of jaw bone growth, as a simple local protraction of periosteal osteogenic activity. Pseudotooth development thus occurred relatively late during ontogeny. The highly vascularized structure and the relative abundance of parallel-fibered bone tissue in the pseudoteeth suggest poor mechanical capabilities. The pseudoteeth were most likely covered and protected by the hardened, keratinized rhamphotheca in the adult during life. The late development of the pseudoteeth would involve a similarly late and/or partial hardening of the rhamphotheca, as displayed by extant Anseriformes, Apterygiformes and some Charadriiformes. This would add support to the hypothesis of a close phylogenetic relationship between Odontopterygiformes and Anseriformes. The late maturation of the Pelagornis feeding apparatus, and hence the delayed capability for efficient prey catching, suggests that Pelagornis was altricial.
ISSN: 1932-6203

hal-01545486
https://hal.archives-ouvertes.fr/hal-01545486
DOI : 10.1371/journal.pone.0080372

Éditeur(s) : HAL CCSD Elsevier
Résumé : International audience
Based on new photographs of the wound, Tirard et al. (2015) tried to demonstrate that the shark involved in a fatal attack on a human in Lifou in 2007 had homodont teeth and that it sawed the femur instead of directly cutting it, promoting the hypothesis that it was a tiger shark instead of a white shark. They also contested the data provided by the direct witness of the attack about the behaviour of the shark, specific to this former species. The evidences they provide are not convincing and, based on the absence of tissue loss and description of a jumping behaviour, we still believe that it was a single bite-and-spit attack by a white shark.
ISSN: 1752-928X

hal-01310536
https://hal-univ-perp.archives-ouvertes.fr/hal-01310536
DOI : 10.1016/j.jflm.2016.03.004

Éditeur(s) : HAL CCSD Museum National d'Histoire Naturelle Paris
Résumé : This study focuses on new fossil faunas of bats discovered in North Africa following several field campaigns. The fossiliferous localities include those from the Early to Middle Eocene of Tunisia (Chambi) and Algeria (Glib Zegdou). Systematic and cladistic analyses carried out on the fossil material, primarily including isolated teeth, allow us to highlight the modalities of the radiation of the first modern microbats. These new faunas include eight well-identified new taxa belonging to five modern families: one Necromantidae (?Necromantis fragmentum Ravel, n. sp.), two Hipposideridae Miller, 1907 (?Palaeophyllophora tunisiensis Ravel, n. sp. and Hipposideros [Pseudorhinolophus] africanum Ravel, n. sp.), three Emballonuridae Gervais in de Castelnau, 1855 (Vespertiliavus kasserinensis Ravel, n. sp., ?Vespertiliavus aenigma Ravel, n. sp., and Pseudovespertiliavus parva Ravel n. gen., n. sp.), one Nycteridae (Khoufechia gunnelli Ravel n. gen., n. sp.) and an undetermined Vespertilionidae. Two other taxa are identified (Chambinycteris pusilli Ravel n. gen., n. sp. and Drakonycteris glibzegdouensis Ravel n. gen., n. sp.), but they show an original dental pattern which precludes a family attribution. Two cladistic analyses allow to clarify the phylogenetic position of the best documented taxa. The results highlight for Hipposideridae and Emballonuridae chiropterans a major dispersal axis from North Africa towards South Europe during the Middle Eocene.
ISSN: 1280-9659

hal-01467508
https://hal.archives-ouvertes.fr/hal-01467508
DOI : 10.5252/g2016n3a3

Éditeur(s) : HAL CCSD Elsevier
Résumé : International audience
The high proportion of crystallized apatite forming the bones and teeth should theoretically allow the use of fission track analysis to date vertebrate fossils when burying of the fossiliferous series did not subject them to temperatures exceeding 60 degrees C. However several major obstacles arise such as the complexity of fossils' internal structures, diagenetic modifications and substitutions of the hydroxyapatite by other minerals, and massive U uptake or loss during diagenesis. In this work, those various problems are addressed combining optical microscope observation of the fossils, a systematic fission track analysis of the best samples, alpha and gamma spectrometry and Secondary Ion Mass Spectrometry. Even if the problems caused by internal structures and mineral substitutions can be solved, U movements in and out of the fossils are generally too complex to allow fission track analysis dating of the fossils.
ISSN: 0009-2541

hal-00411880
https://hal.archives-ouvertes.fr/hal-00411880
DOI : 10.1016/j.chemgeo.2007.10.009

Éditeur(s) : HAL CCSD Public Library of Science
Résumé : International audience
We studied the diversity within the former genus Gymnangium in the South West IndianOcean by using an integrative approach of both traditional (morphology-based) and modernmolecular taxonomy. Nine species were recorded in the material collected. A total of 97 16Smitochondrial DNA sequences and 54 Calmodulin nuclear sequences from eight Gymnangium/Taxella species were analyzed. We found both morphological and molecular differencesin the studied Gymnangium species that make it necessary to split the genus. It isproposed to revalidate the genus Taxella which is currently regarded as a synonym ofGymnangium. Two species of the genus Taxella (T. eximia and T. gracilicaulis), until nowregarded as distinct species based on morphological characteristics, cluster together in onephylogenetic clade. Possible explanations are discussed. Two species from Madagascarnew to science are herein described and rare species from the Indian Ocean islands are redescribed.
ISSN: 1932-6203

hal-01564043
https://hal-univ-perp.archives-ouvertes.fr/hal-01564043
DOI : 10.1371/journal.pone.0174244