Arthropod Trace Fossils of the Upper Lower Cambrian Gog Group,Southern Rocky Mountains of Canada

The upper lower Cambrian Gog Group in the southern Rocky Mountains of Canada displays a high diversity and abundance of arthropod traces. Four ichnogenera, Cruziana, Diplichnites, Monomorphichnus, Rusophycus, and “Indeterminate Arthropod Scratches” are discussed, with a total of 17 different ichnospecies, as follows: Cruziana billingsi Fillion and Pickerill, 1990, Cruziana irregularis Fenton and Fenton, 1937, Cruziana jenningsi Fenton and Fenton, 1937, Cruziana navicella Fenton and Fenton, 1937, Cruziana omanica Seilacher, 1970, Cruziana pectinata Seilacher, 1994, Cruziana penicillata Gibb, Chatterton, and Pemberton, 2009, Cruziana plicata Crimes, Legg, Marcos, and Arboleya, 1977, Cruziana tenella Linnarsson, 1871, Diplichnites twelvetreesi (Chapman, 1928), Monomorphichnus bilinearis Crimes, 1970b, Monomorphichnus lineatus Crimes, Legg, Marcos, and Arboleya, 1977, Rusophycus eutendorfensis (Linck, 1942 Linck, O. 1942. Die spur Isopodichnus. Senckenbergiana, 25: 232–255. [Google Scholar]), and Rusophycus unilobus (Seilacher, 1970 Seilacher, A. 1970. Cruziana stratigraphy of “non-fossiliferous” Palaeozoic sandstones. In Crimes, T. P. and Harper, J. C. (eds.), Trace Fossils. Seel House Press, Liverpool, 447–476. [Google Scholar]). Three new ichnospecies, i.e., Cruziana caputinclinata isp. nov., Rusophycus subnotous isp. nov., and Diplichnites obliquus isp. nov., are proposed, described, and illustrated. The ichnofauna collected from three localities (Lake O'Hara, Mount Babel, and Redoubt Mountain) are predominantly Cruziana. Evidence of nutrient-rich substrates containing microbially induced sedimentary structures and the ichnospecies present confirm that the trace fossil bearing strata are part of the Cruziana ichnofacies and were deposited in a fully marine basin between fair weather wave base and storm wave base.     

An integrative approach underscores the taxonomic status of Lamellidens exolescens,a freshwater mussel from the Oriental tropics (Bivalvia: Unionidae)

The Oriental Region harbours the second richest fauna of freshwater bivalves in the world, including many endangered endemic taxa. However, the Oriental fauna of the Unionidae have been very poorly studied using an integrative taxonomic approach, which may provide reasonable revisions of complicated (cryptic) taxa based on morphological, molecular, biogeographic and ecological evidence. Here, we present the first example of an integrative taxonomic revision concerning the status of Unio exolescens Gould (1843 Gould, A.A. (1843). Dr. Gould had examined the shells not long since announced as having been received from the Rev. Francis Mason, missionary at Tavoy, in British Burmah. Proceedings of the Boston Society of Natural History, 1, 139–141. [Google Scholar]), a nominal mussel taxon that was accepted as a valid species within the genus Trapezoideus Simpson (1900). Currently, Trapezoideus exolescens is considered the type of the genus as far as the originally designated type species, U. foliaceus Gould (1843 Gould, A.A. (1843). Dr. Gould had examined the shells not long since announced as having been received from the Rev. Francis Mason, missionary at Tavoy, in British Burmah. Proceedings of the Boston Society of Natural History, 1, 139–141. [Google Scholar]), was considered to be a synonym of T. exolescens. Using nucleotide sequences obtained from mitochondrial (COI and 16S rRNA) and nuclear (28S rDNA) genes, we found that the topotypes of Unio exolescens Gould (1843 Gould, A.A. (1843). Dr. Gould had examined the shells not long since announced as having been received from the Rev. Francis Mason, missionary at Tavoy, in British Burmah. Proceedings of the Boston Society of Natural History, 1, 139–141. [Google Scholar]) cluster together with representatives of another mussel genus, Lamellidens Simpson (1900). Based on these results and on morphological data, we transfer Unio exolescens Gould (1843 Gould, A.A. (1843). Dr. Gould had examined the shells not long since announced as having been received from the Rev. Francis Mason, missionary at Tavoy, in British Burmah. Proceedings of the Boston Society of Natural History, 1, 139–141. [Google Scholar]) from Trapezoideus to Lamellidens and propose Lamellidens exolescens (Gould, 1843 Gould, A.A. (1843). Dr. Gould had examined the shells not long since announced as having been received from the Rev. Francis Mason, missionary at Tavoy, in British Burmah. Proceedings of the Boston Society of Natural History, 1, 139–141. [Google Scholar]) comb. nov. In addition, we revisited the status of Unio foliaceus Gould (1843 Gould, A.A. (1843). Dr. Gould had examined the shells not long since announced as having been received from the Rev. Francis Mason, missionary at Tavoy, in British Burmah. Proceedings of the Boston Society of Natural History, 1, 139–141. [Google Scholar]) as a valid species and the type of the genus Trapezoideus based on the morphological study of the type specimen, although a question concerning the true position of this taxon is still open because its molecular sequences are not available. Our findings highlight that an integrative taxonomic approach is an important tool, particularly when dealing with such species-rich Unionidae fauna as those of the Oriental Realm.     

Integrative taxonomy of the cave-dwelling mysids of the genus Hemimysis

The genus Hemimysis (Malacostraca: Mysida: Mysidae) encompasses near-bottom, demersal and cave-dwelling mysids living in the marine, brackish and freshwater habitats around the European coast, from the Caspian Sea to the Scandinavian Peninsula. We conducted cladistic analysis of 52 morphological characters of all nine species and three subspecies of the genus Hemimysis. We also completed a molecular analysis based on three molecular markers of Hemimysis lamornae (Couch, 1856) found in the English Channel, the Mediterranean Sea, and the Black Sea. Both analyses did not support monophyly of Hemimysis lamornae. We thus consider the former subspecies H. lamornae pontica (Czerniavsky, 1882 Chevaldonné, P., &; Lejeusne, C. (2003). Regional warming‐induced species shift in north‐west Mediterranean marine caves. Ecology Letters, 6, 371–379. doi:10.1046/j.1461-0248.2003.00439.x.[Crossref], [Web of Science ®] , [Google Scholar]) and H. lamornae mediterranea Bacescu, 1936 Bacescu, M. (1936). Hemimysis lamornae sbsp. reducta, nov. sbsp. et Hemimysis anomala dans les eaux roumaines de la Mer Noire (avec une etude comparative des forms de Hem. lamornae des autres mers: H. l. typica et H.l. mediterranea, nov. sbsp.). Annales Scientifiques de L’Universite de Jassy, 23, 331–338. [Google Scholar] as valid species. Analysis of mitochondrial cytochrome oxidase subunit I (COI) sequences of H. pontica shows no significant divergence between mysids living in the marine caves of Crimea and Bulgaria. Morphological trends in Hemimysis are discussed, H. pontica Czerniavsky, 1882 Chevaldonné, P., &; Lejeusne, C. (2003). Regional warming‐induced species shift in north‐west Mediterranean marine caves. Ecology Letters, 6, 371–379. doi:10.1046/j.1461-0248.2003.00439.x.[Crossref], [Web of Science ®] , [Google Scholar] is redescribed, and a new key to all 11 species of the genus is given.     

Redefinition of the hypotrichous ciliate Uncinata,with descriptions of the morphology and phylogeny of three urostylids (Protista,Ciliophora)

We investigated the morphology, morphogenesis and small subunit rRNA gene-based phylogeny of three marine urostylids, Uncinata gigantea Bullington, 1940 Bullington, W. E. (1940). Some ciliates from Tortugas. Papers from the Tortugas Laboratory, 32, 179–221. [Google Scholar], Holosticha heterofoissneri Hu & Song, 2001 Hu, X., & Song, W. (2001). Morphology and morphogenesis of Holosticha heterofoissneri n. sp. from the Yellow Sea, China (Ciliophora, Hypotrichida). Hydrobiologia, 448, 171–179. doi:10.1023/A:1017553406031.[Crossref], [Web of Science ®] , [Google Scholar], and Holosticha cf. heterofoissneri. The dorsal morphogenesis of Uncinata gigantea shows de novo formation of two groups of anlagen near the marginal rows. Holosticha cf. heterofoissneri demonstrates fragmentation of the first dorsal kinety anlage as in Holosticha heterofoissneri. Our population of H. heterofoissneri corresponds well with previously described populations in terms of its general morphology and ciliary pattern. Uncinata gigantea can be recognized by its large and highly contractile body, yellowish to brownish cell colour, two types of cortical granules, and 20–30 transversely oriented and densely arranged cirri in the left marginal row, which often overlie the buccal vertex. Based on the new data, especially infraciliature, the genus Uncinata is here redefined. Both the morphology and phylogenetic analyses suggest that the genus Uncinata should be classified within the family Urostylidae. In addition, both morphological and morphogenetic data suggest that Holosticha bradburyae Gong et al., 2001 Gong, J., Song, W., Hu, X., Ma, H., & Zhu, M. (2001). Morphology and infraciliature of Holosticha bradburyae n. sp. (Ciliophora, Hypotrichida) from the Yellow Sea, China. Hydrobiologia, 464, 63–69. doi:10.1023/A:1013901621439.[Crossref], [Web of Science ®] , [Google Scholar] should be transferred to Uncinata as U. bradburyae (Gong et al., 2001 Gong, J., Song, W., Hu, X., Ma, H., & Zhu, M. (2001). Morphology and infraciliature of Holosticha bradburyae n. sp. (Ciliophora, Hypotrichida) from the Yellow Sea, China. Hydrobiologia, 464, 63–69. doi:10.1023/A:1013901621439.[Crossref], [Web of Science ®] , [Google Scholar]) comb. nov., due to its possession of a characteristically prominent beak-like, leftwards curved projection and the developmental mode of the dorsal kineties. This assignment is supported by the phylogenetic analyses, which placed Uncinata gigantea in a clade with U. bradburyae (Gong et al., 2001 Gong, J., Song, W., Hu, X., Ma, H., & Zhu, M. (2001). Morphology and infraciliature of Holosticha bradburyae n. sp. (Ciliophora, Hypotrichida) from the Yellow Sea, China. Hydrobiologia, 464, 63–69. doi:10.1023/A:1013901621439.[Crossref], [Web of Science ®] , [Google Scholar]) comb. nov., and revealed only 1.13% (19 bp) difference in their SSU-rDNA gene sequence.     

EFFICIENT SYNTHESIS OF FUSED ISOTHIAZOLO C-NUCLEOSIDES. III. SYNTHESIS OF 7-SUBSTITUTED ISOTHIAZOLO[4,5-d]PYRIMIDINE C-NUCLEOSIDES*

The Divakar-Reese procedure has been successfully applied for transforming 7-oxo-isothiazolo[4,5-d]pyrimidine C-nucleosides (4a,b, 5a,b, 6a) via 1,2,4-triazol-1-yl intermediates (7a,b, 8a,b) into various 7-substituted C-nucle- osides 15a,b, 16a,b, 17a, 18a, 19a,b, 20a,b; their subsequent deprotection provides novel types of unusual C-glycosides 22b, 23a, 24a,b, 25b, 26b.

C-Nucleosides, possessing on its heterocyclic base other than naturally occuring oxo- or amino substituents, are important model compounds for biological or medicinal studies [2a] Hanessian, S. and Pernet, A. G. 1976. Adv. Carbohydr. Chem. Biochem., 32: 111–188. cf. [Google Scholar], [2b] Mizuno, Y. 1986. The Organic Chemistry of Nucleic Acids Amsterdam: Elsevier.  [Google Scholar], [2c] Huryn, D. M. and Okabe, M. 1992. Chem. Rev., 92: 1745–1768. [Crossref], [Web of Science ®] , [Google Scholar], [2d] Häbich, D. 1991. Chem. in uns. Zeit, 25: 295–307.  [Google Scholar], [2e] Uhlmann, E. and Peyman, A. 1990. Chem. Rev., 90: 543–584. [Crossref], [Web of Science ®] , [Google Scholar], [2f] Thuong, N. T. and Helene, C. 1993. Angew. Chem., 105: 697–723. [Crossref] , [Google Scholar], [2g] 1993. Angew. Chem. Int. Ed. Engl., 33: 666–690.  [Google Scholar], [2h] Yarchoan, R., Mitsuya, H., Zhomas, R. V., Pluda, J. M., Hartman, N. R., Perno, C. F., Marczyk, K. S., Allain, J. P., Johns, D. G. and Broder, S. 1989. Science, 245: 412–414. [Crossref], [PubMed], [Web of Science ®] , [Google Scholar], [2i] Tanaka, H., Baba, M., Hayakawa, H., Sakamaki, T., Miyasaka, T., Ubasawa, M., Takashima, H., Sekiya, E., Nitta, I., Shigeta, S., Walker, R. T., Balzarini, J. and De Clerq, E. 1991. J. Med. Chem., 34: 349–357. [Crossref], [PubMed], [Web of Science ®] , [Google Scholar] [3a] Koyama, G., Maeda, K., Umezawa, H. and Iitaka, Y. 1966. Tetrahedron Lett., : 597–602. Some C-glycosides with antibiotic, antiviral (HIV), and anticancer activities [Google Scholar], [3b] Hori, M., Wakashiro, T., Ito, E., Sawa, T., Takeuchi, T. and Umezawa, H. J. 1968. J. Antibiot., 21A: 264–270. [Chem. Abstr. 1968, 69, 11356j] [Google Scholar], [3c] Farkas, J. and ?orm. 1972. F. Collect. Czech. Chem. Commun., 37: 2798–2803.  [Google Scholar], [3d] Acton, E. M., Ryan, K. J., Henry, D. W. and Goodman, L. 1971. J. Chem. Soc., Chem. Commun., : 986–988.  [Google Scholar], [3e] Nakagawa, Y., Kano, H., Tsukuda, Y. and Koyama, H. 1967. Tetrahedron Lett., : 4105–4109.  [Google Scholar], [3f] Inoue, I. and Kuwaijama, I. 1980. J. Chem. Soc., Chem. Commun., : 251–253.  [Google Scholar], [3g] Buchanan, J. G., Stobie, A. and Wightman, R. H. 1980. ibid., : 916–917. [Crossref] , [Google Scholar], [3h] Hildebrand, S. and Leumann, C. 1996. Angew. Chem., 108: 2100–2102. Angew. Chem. Int. Ed. Engl. 1996, 35, 1968–1970 [Google Scholar]. We want to report on the synthesis of novel 7-substituted isothiazolo = [4,5-d]pyrimidine C-nucleosides. As we could show in previous papers [1] Wamhoff, H., Berressem, R. and Nieger, M. 1994. J. Org. Chem., 59: 1912–1917. Part 2 [Google Scholar], [4] Wamhoff, H., Berressem, R. and Nieger. 1993. M. J. Org. Chem., 58: 5181–5185.  [Google Scholar], there exists a simple approach to the protected C-glycosides 4–6.

     

Rediscovery of the Tagragra Tracksite (Maastrichtian,Agadir, Morocco): Agadirichnus elegans Ambroggi and Lapparent 1954 is Pterosaurian Ichnotaxon

ABSTRACT

Discovered in 1954 by Ambroggi and Lapparent, the Tagragra tracksite (Maastrichtian, Agadir, Morocco) yielded tracks of theropod dinosaurs, birds and enigmatic forms tentatively attributed to Lacertilia under the name Agadirichnus elegans. The original specimens are today considered to be lost, and the status of A. elegans has been questioned, even though these footprints can retrospectively be referred to pterodactyloid pterosaur tracks. In order to discuss the status of these foot prints, the historical site has been actively sought and recently rediscovered by one of us (MdD). New material confirms the presence of pterodactyloid footprints, with two morphotypes, in two different facies, respectively associated with bird and theropod tracks. Morphotype I is tentatively conferred to Pteraichnus Stokes 1957 Stokes, W. L. 1957. Pterodactyl tracks from the Morrison Formation. Journal of Palaeontology, 31:952–4.[Web of Science ®] , [Google Scholar], which extends the stratigraphical distribution of this ichnotaxon to the Maastrichtian. Morphotype II corresponds to the original ichnospecies A. elegans Ambroggi and Lapparent 1954 Ambroggi, R., and A. F. de Lapparent 1954. Les empreintes de pas fossiles du Maestrichtien d'Agadir. Notes du Service Géologique du Maroc, 10:43–6. [Google Scholar], which is here reassessed as a valid ichnotaxon, with the designation of a neotype. Thus, A. elegans Ambroggi and Lapparent 1954 Ambroggi, R., and A. F. de Lapparent 1954. Les empreintes de pas fossiles du Maestrichtien d'Agadir. Notes du Service Géologique du Maroc, 10:43–6. [Google Scholar] is historically the first pterosaurian ichnotaxon ever described.     

The genera Stegastopsis Kraatz, 1865 and Orostegastopsis Koch, 1962 with description of O. planioculata sp. n. from Oman (Coleoptera: Tenebrionidae: Tentyriini)

The first Asian member of Orostegastopsis Koch, 1962 Koch, C. (1962): Vierter taxonomischer Beitrag zur Kenntnis der Tenebrioniden Somalias: Über die von Prof. G. Scortecci 1953 und 1957 in der Migiurtinia-Provinz gesammelten Arten. 1. Teil. Atti della Società Italiana di Scienze Naturali, 51, 237–270. [Google Scholar] is described and figured: O. planioculata sp. n., which can be easily distinguished from the two Somalian species O. scorteccii Koch, 1962 Koch, C. (1962): Vierter taxonomischer Beitrag zur Kenntnis der Tenebrioniden Somalias: Über die von Prof. G. Scortecci 1953 und 1957 in der Migiurtinia-Provinz gesammelten Arten. 1. Teil. Atti della Società Italiana di Scienze Naturali, 51, 237–270. [Google Scholar] and O. kaszabi (Bremer, 1985 Bremer, H. J. (1985): Eine neue Stegastopsis-Art (Coleopt., Tenebrionidae, Tentyriini) aus Somalia. Entomologische Blätter, 81, 59–61. [Google Scholar]) comb. nov. by the shallow eyes. According to the shape of the clypeus, Stegastopsis kaszabi Bremer, 1985 Bremer, H. J. (1985): Eine neue Stegastopsis-Art (Coleopt., Tenebrionidae, Tentyriini) aus Somalia. Entomologische Blätter, 81, 59–61. [Google Scholar] is transferred from the genus Stegastopsis Kraatz to the genus Orostegastopsis Koch as was already indicated by Bremer (1985 Bremer, H. J. (1985): Eine neue Stegastopsis-Art (Coleopt., Tenebrionidae, Tentyriini) aus Somalia. Entomologische Blätter, 81, 59–61. [Google Scholar]) who treated Orostegastopsis as a subgenus of Stegastopsis: Orostegastopsis kaszabi (Bremer, 1985 Bremer, H. J. (1985): Eine neue Stegastopsis-Art (Coleopt., Tenebrionidae, Tentyriini) aus Somalia. Entomologische Blätter, 81, 59–61. [Google Scholar]) comb. nov. Keys to the species of Stegastopsis and Orostegastopsis are given.     

Molluskan Grazing Traces (Ichnogenus Radulichnus Voigt, 1977) on a Pleistocene Bivalve from Southern Brazil,With the Proposal of a New Ichnospecies

The ichnogenus Radulichnus Voigt, 1977 Voigt, E. 1977. On grazing traces produced by the radula of fossil and recent gastropods and chitons. In Trace fossils 2, eds. T. P. Crimes, and J. C. Harper, 335–346. Geological Journal, Special Issue 9. [Google Scholar] is recorded for the first time from a bivalve, Anomalocardia brasiliana (Gmelin, 1791 Gmelin, J. F. 1791. Caroli a Linné, Systema Naturae. Tom. I, Pars VI. Leipzig: G.E. Beer, pp. 3021–3910. [Google Scholar]), in a late Pleistocene molluskan assemblage from the southern Brazilian coastal plain. Grazing traces comprise short (<1?mm), parallel furrows, arranged in rows on the inner (concave) shell surface and mostly concentrated in its central area. Radulichnus accommodates scratches on hard substrates produced by the radula of grazing gastropod or polyplacophorans. Our literature survey on fossil and extant traces, as well as studies on the grazing mechanism in living mollusks, document at least two distinct morphotypes that are related to differences in the feeding modes of the producers. We propose to distinguish a second ichnospecies of Radulichnus, in addition to the type, R. inopinatus Voigt, 1977 Voigt, E. 1977. On grazing traces produced by the radula of fossil and recent gastropods and chitons. In Trace fossils 2, eds. T. P. Crimes, and J. C. Harper, 335–346. Geological Journal, Special Issue 9. [Google Scholar] (produced by gastropods), which is named R. transversus isp. nov., and attributed to polyplacophorans. Grazing traces on the shell of A. brasiliana match the morphotype produced by polyplacophorans mollusks, and are indicative of its complex taphonomic history in comparison with other shells in this assemblage.     

Buried Tracks: Ichnological Applications of High-Frequency Georadar

Recognition and sampling of traces in unconsolidated sands present a major challenge for ichnologists. This can be partially remedied through the application of high-resolution geophysical techniques, such as ground-penetrating radar (GPR or georadar), which uses electromagnetic impulse for continuous imaging of shallow subsurface. It addition to geological applications, GPR imaging has been used in several studies focused on animal traces as related to conservation of endangered fossorial species (Kinlaw et al., 2007 Kinlaw, A. E., Conyers, L. B. and Zajac, W. 2007. Use of ground penetrating radar to image burrows of the gopher tortoise (Gopherus polyphemus). Herpetological Review, 38: 50–56.  [Google Scholar]; Martin et al., 2011 Martin, A. J., Skaggs, S. A., Vance, R. K. and Greco, V. 2011. Ground-penetrating radar investigation of gopher-tortoise burrows: Refining the characterization of modern vertebrate burrows and associated commensal traces. Geological Society of America Abstracts with Programs, 43: 381 [Google Scholar]), slope and levee stability (Nichol et al., 2003 Nichol, D., Lenham, J. W. and Reynolds, J. M. 2003. Application of ground-penetrating radar to investigate the effects of badger setts on slope stability at St. Asaph Bypass, North Wales. Quarterly Journal of Engineering Geology and Hydrogeology, 36: 143–153.  [Google Scholar]; Di Prinzio et al., 2010 Di Prinzio, M, Bittelli, M., Castellarin, A. and Pisa, P. R. 2010. Application of GPR to the monitoring of river embankments. Journal of Applied Geophysics, 7: 53–61.  [Google Scholar]), and mapping of fossil tracks (Matthews et al., 2006 Matthews, N. A., Noble, T. A. and Breithaupt, B. H. 2006. “The application of photogrammetry, remote sensing and geographic information systems (GIS) to fossil resource management”. In Fossils from Federal Lands, Edited by: Lucas, S. G., Spielmann, J. A., Hester, P. M., Kenworthy, J. P. and Santucci, V. L. Vol. 34, 119–131. New Mexico Museum of Natural History and Science Bulletin.  [Google Scholar]; Aucoin and Hasbargen, 2010 Aucoin, C. D. and Hasbargen, L. 2010. Using GPR, GPS and close-range photography to map and characterize dinosaur tracks in the Connecticut River valley. Geological Society of America Abstracts with Programs, 42: 276 [Google Scholar]) and tracking surfaces (Webb, 2007 Webb, S. 2007. Further research of the Willandra Lakes fossil footprint site, southeastern Australia. Journal of Human Evolution, 52: 711–715. [Crossref], [PubMed], [Web of Science ®] , [Google Scholar]). Few efforts have been dedicated specifically to characterizing burrow and track characteristics (Stott, 1996 Stott, P. 1996. Ground-penetrating radar: a technique for investigating the burrow structure of fossorial vertebrates. Wildlife Research, 22: 519–530.  [Google Scholar]; Sensors & Software Inc., 2010 [compilation on geophysical projects related to animal burrows]; Buynevich and Hasiotis, 2011; Buynevich et al., 2011; Martin et al., 2011) and most of the above studies are published in journals not routinely accessed by ichnologists.     

The genus Antillophos Woodring, 1928 (Gastropoda: Buccinidae) from the China seas,with description of a new species

The species of genus Antillophos Woodring, 1928 Woodring, W.P. (1928) Miocene Mollusks from Bowden, Jamaica. 2. Gastropods and Discussion of Results. Contributions to the Geology and Paleontology of the West Indies. Carnegie Institute of Washington, Washington D.C. [Google Scholar] from the China seas are studied. Six species, Antillophos liui n. sp., Antillophos lucubratonis Fraussen & Poppe, 2005 Fraussen, K. & Poppe, G.T. (2005) Revision of Phos and Antillophos (Buccinidae) from the Central Philippines. Visaya 1, 76–115. [Google Scholar], Antillophos monsecourorum Fraussen & Poppe, 2005 Fraussen, K. & Poppe, G.T. (2005) Revision of Phos and Antillophos (Buccinidae) from the Central Philippines. Visaya 1, 76–115. [Google Scholar], Antillophos pyladeum (Kato, 1995 Kato, S. (1995) Discussion of the genus Phos. Hitaciobi 70, 15–20. [Google Scholar]), Antillophos roseatus (Hinds, 1844 Hinds, R.B. (1844) Mollusca. In: Hinds, R.B. (Ed.) The Zoology of the Voyage of H.M.S. Sulphur During the years 1836–1842. 2. Smith, Elder and Co., London, pp. 1–72. [Google Scholar]) and Antillophos sp., are described and illustrated.

http://zoobank.org/urn:lsid:zoobank.org:pub:51481997-A841-4F37-8E15-B753DC99CB4D     

Revision of the Clytra subfasciata species group (Coleoptera: Chrysomelidae: Cryptocephalinae: Clytrini)

The Clytra subfasciata species group is proposed, to comprise Clytra subfasciata Lacordaire, 1848 Lacordaire, J. T. (1848): Monographie des coléoptères subpentamères de la famille des phytophages. Tome second. Mémoires de la Société Royale des Sciences de Liége, 5, 1–890 pp. [Google Scholar], C. hajeki Medvedev &; Kantner, 2002 Medvedev, L. N., &; Kantner, F. (2002): Some new and poorly know Clytrinae (Coleoptera, Chrysomelidae) of the Old World. Entomologica Basiliensia, 24, 259–269. [Google Scholar] and C. kadleci sp. n. (Yemen). The species of the group are characterised by the peculiar shape of the aedeagus, with a dorsal plate separated from the rest of aedeagus by a deep narrow slit. Colour photographs of habitus and drawings of genitalia are provided for all three species.

http://www.zoobank.org/urn:lsid:zoobank.org:pub:F6706A76-CD49-4A5A-A109-A6E6C23514A5     

Teaching Bernoulli's Principle through Demonstrations

ABSTRACT

One proven strategy to help students make sense of abstract concepts is to sequence instruction so students have exploratory opportunities to investigate science before being introduced to new science explanations (Abraham and Renner 1986 Abraham, M. R. and Renner, J. W. 1986. The sequence of learning cycle activities in high school chemistry. Journal of Research in Science Teaching, 23: 121–143. [Crossref], [Web of Science ®] , [Google Scholar]; Renner, Abraham, and Birnie 1988 Renner, J. W., Abraham, M. R. and Birnie, H. H. 1988. The necessity of each phase of the learning cycle in teaching high school physics. Journal of Research in Science Teaching, 25: 39–58. [Crossref], [Web of Science ®] , [Google Scholar]). To help physical science teachers make sense of how to effectively sequence lessons, this article summarizes our experiences using an exploration–explanation sequence of instruction to teach Bernoulli's principle to prospective middle and secondary science teachers in a science methods course. We use demonstrations during our Bernoulli unit to help students go back and forth between their observations of phenomenon and what occurs on the microscopic level with what we have termed molecular talk. Students engage in guiding questions, consider their old and new understandings of science, and use evidence to construct new ideas during all stages of the lesson.     

Carnivore Trackways from the Miocene Site of Salinas de Añana (Alava,Spain)

A fossil tracksite of Lower Miocene age discovered near Salinas de Añana, Alava (Spain), has rendered an exceptionally well-preserved assemblage of vertebrate ichnites. The site shows a high proportion of carnivore tracks (3 out of 5 mammal ichnospecies) and a high number of individual trackways (15), some including over 50 consecutive footprints. The carnivore ichnites are classified as Felipeda lynxi Panin & Avram, 1962 Panin, M. and Avram, B. 1962. Noi urme de vertebrate in Miocenul Subcarpatilor Rominesti. Studii Cercet Geologia, 13: 521–525.  [Google Scholar], Felipeda parvula ichnosp. nov. and Canipeda longigriffa Panin & Avram, 1962 Panin, M. and Avram, B. 1962. Noi urme de vertebrate in Miocenul Subcarpatilor Rominesti. Studii Cercet Geologia, 13: 521–525.  [Google Scholar], and they are attributed to a felid, an undetermined small aeluroid, and a herpestid, respectively. The long trackways allow determination of gaits, which include lateral sequence walks and diagonal sequence trots, and of speed, which ranges from 0.4 to 1.4 m/s. Froude numbers range between 0.1 and 0.8, agreeing with gait interpretations and speed calculations. The felid trackways provide the first known evidence of group traveling in fossil cats. The herpestid footprints show modern-grade adaptations for terrestrial locomotion and digging.     

How did sea spiders recolonize the Chilean fjords after glaciation? DNA barcoding of Pycnogonida,with remarks on phylogeography of Achelia assimilis (Haswell, 1885)

The present paper reports on a first attempt at resolving the taxonomy of Chilean Pycnogonida using a combination of DNA sequence and morphological data. In a subproject of the Marine Barcode of Life (MarBoL) campaign we analysed a fragment (about 657 base pairs) of the mitochondrial protein-coding gene COI (cytochrome c oxidase subunit 1) from 76 Chilean/Subantarctic pycnogonids. Since most molecular data on pycnogonids are from the Antarctic region, the new information constitutes a significant extension. The phylogenetic consensus tree displays 10 distinct, well-supported branches corresponding to the studied species, namely Achelia assimilis (Haswell, 1885), Ammothea spinosa (Hodgson, 1907), Tanystylum cavidorsum Stock, 1957, T. neorhetum Marcus, 1940 Marcus, E. 1940. Os Pantopoda brasileiros e os demais sul-americanos. Boletin da Faculdade de Filosofia, Ciencias e Letras da Universidade de São Paulo, Ser. 4, Zoologie, 19: 1–179.  [Google Scholar], Colossendeis macerrima Wilson, 1881, C. megalonyx Hoek, 1881, C. scoresbii Gordon, 1932 Gordon, I. 1932. Pycnogonida. – Discovery Reports Vol. VI., 1–137. London: Cambridge University Press.  [Google Scholar] , Callipallene margarita (Gordon, 1932 Gordon, I. 1932. Pycnogonida. – Discovery Reports Vol. VI., 1–137. London: Cambridge University Press.  [Google Scholar]), Pallenopsis patagonica (Hoek, 1881), and Anoplodactylus californicus Hall, 1912. These represent four superfamilies, and five of the 11 existing pycnogonid families (Bamber & El Nagar, 2011 Bamber, R. N. and El Nagar, A., eds. 2011. Pycnobase: World Pycnogonida Database http://www.marinespecies.org/pycnobase, accessed June 2012 [Google Scholar]): Ammotheidae Dohrn, 1881, Colossendeidae Hoek, 1881, Callipallenidae Hilton, 1942, Pallenopsidae Fry, 1978 and Phoxichilidiidae Sars, 1891. Within Achelia assimilis, four distinct subbranches correspond to the different geographic regions represented in our samples. While these include a total of 11 distinct haplotypes, the morphological differences among the corresponding specimens lie well within the variation described in the literature for this cosmopolitan species. Therefore, the four branches of A. assimilis might represent geographically limited subspecies rather than cryptic species. Repeated drastic glaciation of the fjord region during the Cenozoic resulting in alternating extinction and recolonization phases and the holobenthic lifecycle of sea spiders are discussed as the main factors resulting in the observed phylogeographic pattern. Standard barcoding sequences are confirmed as a suitable tool in addition to morphology for taxonomic analyses in Pycnogonida. The corresponding haplotype distribution patterns allow inferences on the biogeographical history of the relatively unexplored Chilean fjord region.