La genèse et le développement des partis politiques au Bas-Canada (1791-1840)

Ce mémoire s’intéresse à la formation des partis politiques et l’origine de la loyauté partisane à la Chambre d’assemblée du Bas-Canada entre 1791 et 1840. Pour ce faire, le présent mémoire fait une analyse systématique de tous les votes tenus en Chambre grâce à l’indice de loyauté et à la méthode de la Classification optimale (Optimal Classification) développée par Poole (2005). Il soutient la thèse selon laquelle l’ethnicité est la principale source de division entre les députés lors des votes tenus à la Chambre d’assemblée du Bas-Canada lors des premières législatures et que c’est plutôt l’opposition entre les réformistes constitutionnels et les conservateurs favorables à l’ancien régime qui explique les divisions entre les députés lors des deux dernières législatures. Il soutient également que le statut social des députés, le type de comté dans lequel ils sont élus, l’occupation civile des députés ou leur expérience parlementaire n’expliquent pas l’opposition entre les députés lors des votes au Parlement. Ce mémoire émet également l’hypothèse selon laquelle les partis politiques ont peu d’impact sur le comportement législatif de leurs membres : les députés sont libres de voter selon leurs préférences individuelles sans véritable discipline partisane.

Controls on development and diversity of Early Archean stromatolites

The ≈3,450-million-year-old Strelley Pool Formation in Western Australia contains a reef-like assembly of laminated sedimentary accretion structures (stromatolites) that have macroscale characteristics suggestive of biological influence. However, direct microscale evidence of biology—namely, organic microbial remains or biosedimentary fabrics—has to date eluded discovery in the extensively-recrystallized rocks. Recently-identified outcrops with relatively good textural preservation record microscale evidence of primary sedimentary processes, including some that indicate probable microbial mat formation. Furthermore, we find relict fabrics and organic layers that covary with stromatolite morphology, linking morphologic diversity to changes in sedimentation, seafloor mineral precipitation, and inferred microbial mat development. Thus, the most direct and compelling signatures of life in the Strelley Pool Formation are those observed at the microscopic scale. By examining spatiotemporal changes in microscale characteristics it is possible not only to recognize the presence of probable microbial mats during stromatolite development, but also to infer aspects of the biological inputs to stromatolite morphogenesis. The persistence of an inferred biological signal through changing environmental circumstances and stromatolite types indicates that benthic microbial populations adapted to shifting environmental conditions in early oceans.

Pollen-based reconstructions of biome distributions for Australia, Southeast Asia and the Pacific (SEAPAC region) at 0,6000 and 18,000 14C yr B.P.

Aim  This paper documents reconstructions of the vegetation patterns in Australia, Southeast Asia and the Pacific (SEAPAC region) in the mid-Holocene and at the last glacial maximum (LGM). Methods  Vegetation patterns were reconstructed from pollen data using an objective biomization scheme based on plant functional types. The biomization scheme was first tested using 535 modern pollen samples from 377 sites, and then applied unchanged to fossil pollen samples dating to 6000 ± 500 or 18,000 ± 1000 14C yr bp. Results  1. Tests using surface pollen sample sites showed that the biomization scheme is capable of reproducing the modern broad-scale patterns of vegetation distribution. The north–south gradient in temperature, reflected in transitions from cool evergreen needleleaf forest in the extreme south through temperate rain forest or wet sclerophyll forest (WSFW) and into tropical forests, is well reconstructed. The transitions from xerophytic through sclerophyll woodlands and open forests to closed-canopy forests, which reflect the gradient in plant available moisture from the continental interior towards the coast, are reconstructed with less geographical precision but nevertheless the broad-scale pattern emerges. 2. Differences between the modern and mid-Holocene vegetation patterns in mainland Australia are comparatively small and reflect changes in moisture availability rather than temperature. In south-eastern Australia some sites show a shift towards more moisture-stressed vegetation in the mid-Holocene with xerophytic woods/scrub and temperate sclerophyll woodland and shrubland at sites characterized today by WSFW or warm-temperate rain forest (WTRF). However, sites in the Snowy Mountains, on the Southern Tablelands and east of the Great Dividing Range have more moisture-demanding vegetation in the mid-Holocene than today. South-western Australia was slightly drier than today. The single site in north-western Australia also shows conditions drier than today in the mid-Holocene. Changes in the tropics are also comparatively small, but the presence of WTRF and tropical deciduous broadleaf forest and woodland in the mid-Holocene, in sites occupied today by cool-temperate rain forest, indicate warmer conditions. 3. Expansion of xerophytic vegetation in the south and tropical deciduous broadleaf forest and woodland in the north indicate drier conditions across mainland Australia at the LGM. None of these changes are informative about the degree of cooling. However the evidence from the tropics, showing lowering of the treeline and forest belts, indicates that conditions were between 1 and 9 °C (depending on elevation) colder. The encroachment of tropical deciduous broadleaf forest and woodland into lowland evergreen broadleaf forest implies greater aridity. Main conclusions  This study provides the first continental-scale reconstruction of mid-Holocene and LGM vegetation patterns from Australia, Southeast Asia and the Pacific (SEAPAC region) using an objective biomization scheme. These data will provide a benchmark for evaluation of palaeoclimate simulations within the framework of the Palaeoclimate Modelling Intercomparison Project.

A relação executivo-legislativo no projeto de criação da Superintendência do Planejamento Territorial Participativo (SPTP) no Estado do Pará

Este trabalho abordou a relação Executivo–Legislativo no Estado do Pará através do Projeto de Lei 01/2008 que implantaria a Superintendência do Planejamento Territorial Participativo (SPTP), durante a 16ª Legislatura da Assembleia Legislativa do Pará no período 2007-2010. Elaborado pelo Governo do Estado, o projeto previa a implantação de uma instituição que coordenaria o processo de participação popular e controle social proposto pelo governo Ana Júlia Carepa no início de seu governo. Como problemática, a pesquisa abordou a rejeição pelos parlamentares ao referido projeto, cuja questão de pesquisa foi a seguinte: que fatores contribuiram para a rejeição do Projeto de criação da SPTP pelo Poder Legislativo? Além disso, o que ela significa na relação Executivo–Legislativo segundo a literatura corrente. As hipóteses inferidas seriam as de que a rejeição foi motivada pela própria relação conflituosa entre Executivo e Legislativo na arena parlamentar ou pela percepção do conflito de interesses dos atores políticos locais quanto às fronteiras de atuação entre instituições políticas participativas e instituições políticas representativas. Os deputados contrários ao projeto não consideravam a SPTP enquanto prática efetiva de gestão democrática, mas suspeitavam que a mesma, por exemplo, pudesse estar vinculada a estratégias por parte do Executivo para fins eleitorais ou de barganha perante o Legislativo. O Desenvolvimento da pesquisa concentrou-se na busca pelas respostas a problemática apresentada bem como verificar a validade das hipótese inferidas. Quanto ao objetivo se avaliou o comportamento dos deputados na tramitação do projeto de criação da SPTP. Como ferramentas de pesquisas foram utilizadas pesquisas bibliográficas e empíricas.

Phylogenetic relationships of rock-wallabies, Petrogale (Marsupialia: Macropodidae) and their biogeographic history within Australia

The rock-wallaby genus Petrogale comprises a group of habitat-specialist macropodids endemic to Australia. Their restriction to rocky outcrops, with infrequent interpopulation dispersal, has been suggested as the cause of their recent and rapid diversification. Molecular phylogenetic relationships within and among species of Petrogale were analysed using mitochondrial (cytochrome oxidase c subunit 1, cytochrome b. NADH dehydrogenase subunit 2) and nuclear (omega-globin intron, breast and ovarian cancer susceptibility gene) sequence data with representatives that encompassed the morphological and chromosomal variation within the genus, including for the first time both Petrogale concinna and Petrogale purpureicollis. Four distinct lineages were identified, (1) the brachyotis group, (2) Petrogale persephone, (3) Petrogale xanthopus and (4) the lateralis-penicillata group. Three of these lineages include taxa with the ancestral karyotype (2n = 22). Paraphyletic relationships within the brachyotis group indicate the need for a focused phylogeographic study. There was support for P. purpureicollis being reinstated as a full species and P. concinna being placed within Petrogale rather than in the monotypic genus Peradorcas. Bayesian analyses of divergence times suggest that episodes of diversification commenced in the late Miocene-Pliocene and continued throughout the Pleistocene. Ancestral state reconstructions suggest that Petrogale originated in a mesic environment and dispersed into more arid environments, events that correlate with the timing of radiations in other arid zone vertebrate taxa across Australia. Crown Copyright (C) 2011 Published by Elsevier Inc. All rights reserved.

Southeastern Australia, 1834 (Raster Image)

This layer is a georeferenced raster image of the historic paper map entitled: Map of the discoveries in Australia : copied from the latest M.S. surveys in the Colonial Office, by permission dedicated to the Right Hon.ble Viscount Goderich, H.M. principal Secretary of State for the Colonies, and President of the Royal Geographical Society, by his Lordships obliged servant J. Arrowsmith. It was published by Pubd. by J. Arrowsmith, 35 Essex St., Strand in Feb. 15 1834. Scale [ca. 1:3,041,280]. Covers southeastern Australia with additions to the east of the Gulf of St. Vincent and Granite Island inserted in Encounter Bay.The image inside the map neatline is georeferenced to the surface of the earth and fit to the Asia South Lambert Conformal Conic coordinate system. All map collar and inset information is also available as part of the raster image, including any inset maps, profiles, statistical tables, directories, text, illustrations, index maps, legends, or other information associated with the principal map. This map shows features such as drainage, cities and other human settlements, territorial boundaries, shoreline features, and more. Relief shown by hachures and spot heights. Major explorations shown. Includes also notes and insets: The Colony of Western Australia ... -- [Map of Australia in Asia].This layer is part of a selection of digitally scanned and georeferenced historic maps from the Harvard Map Collection. These maps typically portray both natural and manmade features. The selection represents a range of originators, ground condition dates, scales, and map purposes.

Blue book for the year ... /

Chiefly tables.

Lex parliamentaria, or, A treatise of the law and custom of parliaments : shewing their antiquity, names, kinds, and qualities. With an appendix of a case in Parliament between Sir Francis Goodwyn and Sir John Fortescue, for the knights place for the county of Bucks, I. Jac. I.

Mode of access: Internet.

Report of the Bureau of Archives for the Province of Ontario.

Edited by: <1909>- , A. Fraser.

Western Australian year book.

Mode of access: Internet.

Annual report.

Report year irregular.

Report from the Committee of the Legislative Council on the Judicial Establishment of the Colony of the Cape of Good Hope : together with the minutes of evidence and appendix.

John Montagu, chairman.