139 research outputs found

    Lawrence Head Volcanics and Dunnage MĂ©lange, Newfoundland Appalachians: Origin by Ordovician Ridge Subduction or in Back-Arc Rift?

    Get PDF
    This paper reviews the geological setting and reports new geochemical trace element data from the Ordovician Lawrence Head Volcanics (LHV) and the underlying gabbro sills in the Exploits Group. In combination with existing published analyses and ages of these rocks, the volcanic rocks and sills are indistinguishable in composition and age, and the data are consistent with the hypothesis that they represent the same (mostly E-MORB composition) magmatic event in the early–mid Darriwilian (~465 ± 2 Ma). The LHV and their enclosing strata show regional evidence for: 1) upward decline of volume and grain size of arc-derived volcaniclastic materials over the uppermost interval of turbidite sedimentary strata below the LHV; 2) change to shallow marine conditions locally by the end of the LHV event, followed immediately by significant subsidence, and 3) no evidence of coarse-grained clastic input, nor of normal faulting, during or immediately after LHV magmatism. Ridge–trench interaction (ridge subduction) at a subduction system is consistent with all of these features and spatial distribution of related elements, but a rift (back-arc) origin over a subduction zone can only accommodate the compositions, and is inconsistent with the geological evidence. The Dunnage MĂ©lange (DM) has been interpreted either as olistostromal in a developing back-arc rift basin, or as a subduction accretionary prism. Peraluminous intrusions in the mĂ©lange (Coaker Porphyry ― CP) are more readily explained by ridge subduction, and a previously reported zircon age (469 ± 4 Ma) is consistent with the age of the LHV and gabbro sills, also interpreted as products of ridge subduction. Localization of the CP in the eastern area of DM, and of most of the large LHV-derived volcanic blocks in the western DM, suggests a slightly younger age, and perhaps a different mechanism, for the origin of the western DM.SOMMAIRECet article passe en revue le contexte gĂ©ologique et prĂ©sente de nouvelles donnĂ©es gĂ©ochimiques d’élĂ©ments traces des roches volcaniques ordoviciennes de Lawrence Head (LHV) et des filons-couches de gabbro sous-jacents du Groupe Exploits.  ConsidĂ©rant la combinaison des donnĂ©es d’analyse publiĂ©es et des datations de ces roches, les roches volcaniques et les filons-couches sont indiscernables tant en composition qu’en Ăąge, et les donnĂ©es sont compatibles avec l’hypothĂšse selon laquelle ils reprĂ©sentent le mĂȘme Ă©vĂ©nement magmatique (principalement E-MORB) du Darriwilien prĂ©coce Ă  moyen (~465 ± 2 Ma).  Les LHV ainsi que les strates de l’encaissant renferment des indices rĂ©gionaux qui montrent : 1) que le volume et la granulomĂ©trie des matĂ©riaux volcanoclastiques d’arc diminuent vers le haut dans l’intervalle supĂ©rieur des strates de turbidites sĂ©dimentaires sous les LHV; 2) que le changement vers des milieux marins peu profonds localement vers la fin de l’évĂ©nement des LHV a Ă©tĂ© suivi immĂ©diatement par une subsidence importante, et 3) qu’il n’existe pas d’indices d’apports clastiques Ă  gros grains, non plus que de formation de failles normales, durant ou immĂ©diatement aprĂšs le magmatisme des LHV.  L’interaction crĂȘte-fosse (subduction de la crĂȘte) au lieu d’un systĂšme de subduction concorde avec toutes ces caractĂ©ristiques et la rĂ©partition spatiale des Ă©lĂ©ments reliĂ©s, alors qu’une origine de crĂȘte (arriĂšre-arc) au-dessus d’une zone de subduction ne peut expliquer que les compositions et qu’elle est incompatible avec l’évidence gĂ©ologique.  Le Dunnage MĂ©lange (DM) a Ă©tĂ© interprĂ©tĂ© soit comme un olistostome dans un bassin d’arriĂšre-arc en dĂ©veloppement, ou comme un prisme d’accrĂ©tion de subduction.  Les intrusions hyperalumineuses dans le mĂ©lange (Porphyre Coaker — CP), s’explique plus facilement par une subduction de crĂȘte, et un Ăąge de datation sur zircon de (469 ± 4 Ma) correspond Ă  l’ñge des LHV et des filons-couche de gabbro, aussi interprĂ©tĂ©s comme produits d’une subduction de crĂȘte.  La localisation du CP dans la portion orientale du DM, et de la majeure partie des grands blocs volcaniques dĂ©rivĂ©s des LHV de la portion ouest du DM, suggĂšre un Ăąge lĂ©gĂšrement plus jeune, et peut-ĂȘtre un mĂ©canisme diffĂ©rent, pour l’origine de la portion ouest du DM

    Bone progenitor dysfunction induces myelodysplasia and secondary leukaemia

    Get PDF
    Mesenchymal cell populations contribute to microenvironments regulating stem cells and the growth of malignant cells. Osteolineage cells participate in the hematopoietic stem cell niche. Here, we report that deletion of the miRNA processing endonuclease Dicer1 selectively in mesenchymal osteoprogenitors induces markedly disordered hematopoiesis. Hematopoietic changes affected multiple lineages recapitulating key features of human myelodysplastic syndrome (MDS) including the development of acute myelogenous leukemia. These changes were microenvironment dependent and induced by specific cells in the osteolineage. Dicer1−/− osteoprogenitors expressed reduced levels of Sbds, the gene mutated in the human bone marrow failure and leukemia predisposition Shwachman-Bodian-Diamond Syndrome. Deletion of Sbds in osteoprogenitors largely phenocopied Dicer1 deletion. These data demonstrate that differentiation stage-specific perturbations in osteolineage cells can induce complex hematological disorders and indicate the central role individual cellular elements of ‘estroma’ can play in tissue homeostasis. They reveal that primary changes in the hematopoietic microenvironment can initiate secondary neoplastic disease

    From Ideal to Practice and Back Again: Beginning Teachers Teaching for Social Justice

    Full text link
    The five authors of this article designed a multicase study to follow recent graduates of an elementary preservice teacher education program into their beginning teaching placements and explore the ways in which they enacted social justice curricula. The authors highlight the stories of three beginning teachers, honoring the plurality of their conceptions of social justice teaching and the resiliency they exhibited in translating social justice ideals into viable pedagogy. They also discuss the struggles the teachers faced when enacting social justice curricula and the tenuous connection they perceived between their conceptions and their practices. The authors emphasize that such struggles are inevitable and end the article with recommendations for ways in which teacher educators can prepare beginning teachers for the uncertain journey of teaching for social justice

    Direct application of compound-specific radiocarbon analysis of leaf waxes to establish lacustrine sediment chronology

    Get PDF
    Author Posting. © Springer, 2007. This is the author's version of the work. It is posted here by permission of Springer for personal use, not for redistribution. The definitive version was published in Journal of Paleolimnology 39 (2008): 43-60, doi:10.1007/s10933-007-9094-1.This study demonstrates use of compound-specific radiocarbon analysis (CSRA) for dating Holocene lacustrine sediments from carbonate-hosted Ordy Pond, Oahu, Hawaii. Long-chain odd-numbered normal alkanes (n-alkanes), biomarkers characteristic of terrestrial higher plants, were ubiquitous in Ordy Pond sediments. The ÎŽ13C of individual n-alkanes ranged from −29.9 to −25.5‰, within the expected range for n-alkanes synthesized by land plants using the C3 or C4 carbon fixation pathway. The 14C ages of n-alkanes determined by CSRA showed remarkably good agreement with 14C dates of rare plant macrofossils obtained from nearby sedimentary horizons. In general, CSRA of n-alkanes successfully refined the age-control of the sediments. The sum of n-alkanes in each sample produced 70–170 ÎŒg of carbon (C), however, greater age errors were confirmed for samples containing less than 80 ÎŒg of C. The 14C age of n-alkanes from one particular sedimentary horizon was 4,155 years older than the value expected from the refined age-control, resulting in an apparent and arguable age discrepancy. Several lines of evidence suggest that this particular sample was contaminated by introduction of 14C-free C during preparative capillary gas chromatography. This study simultaneously highlighted the promising potential of CSRA for paleo-applications and the risks of contamination associated with micro-scale 14C measurement of individual organic compounds.This project was funded by Petroleum Research Fund (PRF #40088-ACS) and in part by Sigma Xi, The Scientific Research Society (Grants in aid of research, 2003)

    Department of Animal Sciences research and reviews: beef and sheep

    Get PDF
    Relationship of a PCR-SSCP at the Bovine calpastatin locus with calpastatin activity and meat tenderness / H. Y. Chung, M. E. Davis, H. C. Hines, and D. M. Wulf -- Effects of calpain proteolysis and calpain genotypes on meat tenderness of angus bulls / H. Y. Chung, M. E. Davis, H. C. Hines, and D. M. Wulf -- Identification of genetic markers for growth and carcass traits in beef cattle / W. Ge, M. E. Davis, H. C. Hines, and K. M. Irvin -- Relationships of polymorphisms in the bovine leptin gene with differences in beef carcass traits / K. Tessanne, H. C. Hines, and M. E. Davis -- Effects of rate of gain during periods of restricted intake on performance and carcass characteristics in steers fed to achieve step-wise increases in rate of gain / J. E. Rossi and S. C. Loerch -- Effects of feeding regimen and days fed on performance and carcass characteristics of feedlot steers / J. E. Rossi, S. C. Loerch, S. J. Moeller, and J. P. Schoonmaker -- Effect of an accelerated finishing program on performance and carcass characteristics of early weaned bulls and steers / J. P. Schoonmaker, S. C. Loerch, F. L. Fluharty, T. B. Turner, S. J. Moeller and J. E. Rossi -- Yeast-mineral mixes and beef-cattle performance in fescue-based grazing systems: preliminary report / S. Boyles, W. Shriver, and D. Kobs -- Forage and animal evaluation of heifers at Indian Lake Hydrologic Unit CRP stocker grazing demonstration / S. L. Boyles, B. W. Stoll, and T. L. Dobbels -- Beef quality is every cattleman's business: education program / J. Yates and S. Boyles -- Effects of pelleted alfalfa and whole-shelled corn combinations on lamb growth and carcass characteristics / F. L. Fluharty -- Effects of feeding pelleted, ensiled, or a combination of pelleted and ensiled alfalfa on lamb growth and carcass characteristics / F. L. Fluharty, G. D. Lowe, and D. D. Clevenger -- Effects of corn silage vs. alfalfa haylage on lamb growth and carcass characteristics in forage-based finishing systems / F. L. Fluharty, G. D. Lowe, and D. D. Clevenger -- Effects of feed-delivery system and corn processing on lamb growth and carcass characteristics / F. L. Fluharty, G. D. Lowe, and D. D. Clevenger -- Effects of pen floor type and bedding on lamb growth and carcass characteristics / F. L. Fluharty, G. D. Lowe, and D. D. Clevenger -- A PCR-SSCP polymorphism detected in the 5' flanking region of the ovine IGF-I gene / A. Yilmaz, M. E. Davis, and H. C. Hine

    Network Economics and the Environment: Insights and Perspectives

    Get PDF
    Local interactions and network structures appear to be a prominent feature of many environmental problems. This paper discusses a wide range of issues and potential areas of application, including the role of relational networks in the pattern of adoption of green technologies, common pool resource problems characterized by a multiplicity of sources, the role of social networks in multi-level environmental governance, infrastructural networks in the access to and use of natural resources such as oil and natural gas, the use of networks to describe the internal structure of inter-country relations in international agreements, and the formation of bilateral "links" in the process of building up an environmental coalition. For each of these areas, we examine why and how network economics would be an effective conceptual and analytical tool, and discuss the main insights that we can foresee
    • 

    corecore