Effects of climate and land management changes on conservation : of mediterranean cork oak woodlands and their bird communities

Tese de doutoramento (co-tutela), Biologia (Biologia da Conservação), Faculdade de Ciências da Universidade de Lisboa, University of East Anglia, School of Environmental Sciences, 2014

Pollen From Alder (Alnus sp.), Birch (Betula sp.) and Oak (Quercus sp.) in the UK Originate From Small Woodlands

We have analysed the pollen seasons in Worcester for the period 2005–12 for alder (Alnus), birch (Betula) and oak (Quercus) by using back trajectory calculations and produced the first detailed source maps for these three pollen types. The study shows considerable variations in the source–receptor relationship of three of the most important tree pollen types in England with respect to allergy. Long Distance Transport is observed for Quercus and Betula but not for Alnus. The new source maps show a number of high emitting areas for Betula and Quercus, mainly near London, in the Midlands and in Wales. The production of source maps is sensitive to the used type of land cover data and how well they incorporate small woodlands. Two satellite products, Corine Land Cover and Globcover, are compared with the detailed national land cover product Land Cover Map 2007. The broad scale satellite products show either up to 50% less woody coverage or a direct misplacement of woodlands. The Lagrangian back trajectory model, the pollen count observations and the source maps altogether suggest that small woodlands (below 25 ha) play a major role in the overall pollen load in urban areas in England.

[Magnificentiores selectioresque Urbis Venetiarum prospectus quos olim Michael Marieschi, Venetus pictor et architectus in plerisque tabulis depinxit, nunc vero ab ipsomet acurate delineante, incidente, tyspisque mandante, iterum in sexdecim aereis tabulis in lucem aeduntur]. [21], Templum cum Platea Sanctae Mariae Formosae, ex archetiipo Jacobi Sansovini desumptum. : [estampe] / Mich.l Marieschi del.t et inci.t

Référence bibliographique : Toledano, Marieschi, 30

Arrêt du Grand Conseil qui maintient les communautés régulières dans le droit de nommer aux bénéfices, le siège abbatial vaquant. (Maintient Ignace de Vaucanu en la possession de la cure de Notre-Dame d'Ommoy dont il a été pourvu par les religieux de Silly, contre Mich. Picot.)

[Acte. 1730-05-19. Paris]

The sedimentology of the Bloomington fan complex: an element of the Oak Ridges Moraine, Southern Ontario

The Oak Ridges Moraine is a major physiographic feature of south-central Ontario, extending from Rice Lake westward to the Niagara Escarpment. While much previous work has largely postulated a relatively simple the origin of the moraine, recent investigations have concentrated on delineating the discernible glacigenic deposits (or landform architectural elements) which comprise the complex mosaic of the Oak Ridges Moraine. This study investigates the sedimentology of the Bloomington fan complex, one of the oldest elements of the Oak Ridges Moraine. The main sediment body of the Bloomington fan complex was deposited during early stages of the formation of the Oak Ridges Moraine, when the ice subdivided, and formed a confined, interlobate lake basin between the northern and southern lobes. Deposition from several conduits produced a fan complex characterized by multiple, laterally overlapping, fan bodies. It appears that the fans were active sequentially in an eastward direction, until the formation of the Bloomington fan complex was dominated by the largest fan fed by a conduit near the northeastern margin of the deposit. Following deposition of the fan complex, the northern and southern ice margins continued to retreat, opening drainage outlets to the west and causing water levels to drop in the lake basin. Glaciofluvial sediment was deposited at this time, cutting into the underlying fan complex. Re-advancing northern ice then closed westerly outlets, and caused water levels to increase, initiating the re-advance of the southern ice. As the southern ice approached the Bloomington fan, it deposited an ice-marginal sediment complex consisting of glacigenic sediment gravity flows, and glaciolacustrine and glaciofluvial sediments exhibiting north and northwesterly paleocurrents. Continued advance of the southern ice, overriding the fan complex, ii produced large-scale glaciotectonic deformation structures, and deposited the Halton Till. The subaqueous fan depositional model that is postulated for the Bloomington fan complex differs from published models due to the complex facies associations produced by the multiple conduit sources of sediment feeding the fans. The fluctuating northern and southern ice margins, which moved across the study area in opposite directions, controlled the water level in the interlobate basin and caused major changes in depositional environments. The influence of these two lobes also caused deposition from two distinct source directions. Finally, erosion, deposition, and deformation of the deposit with the readvance of the southern ice contributed further to the complexity of the Bloomington fan complex.

Palmetto Grove, estate of Frank M. Chapman, at Cypress and Grand Avenue, Covina, California

Palmetto Grove, 80 acre estate of Frank M. Chapman, located at Cypress and Grand Avenue, Covina, California, ca. 1915.

Grant Chapman, Clarke Chapman, and Frank Chapman Jr., Palmetto Grove, Covina, California, ca. 1915

Left to right: Grant Chapman, Clarke Chapman, and Frank Chapman Jr., sons of Frank Marion and Wilhelmina Zillen Chapman, on a porch at Palmetto Grove, Covina, California, ca. 1915.

Grounds of Palmetto Grove, estate of Frank Marion Chapman, Covina, California, ca. 1915

Grounds of Palmetto Grove, estate of Frank Marion Chapman, Covina, California, ca. 1915.

Frank Chapman Jr. [?] in a touring car, beside the Palmetto Grove house, Covina, California, 1909

Frank Chapman Jr. [?] in a touring car, beside the Palmetto Grove house, Covina, California, August, 1909.

Cemetery Committee Reports, Welland County, 1946

In 1946 the cemetery committee reported at least twice to the Welland County council. The reports included the state of cemeteries within the county boundaries and recommendations for grants to be made for their maintenance. The committee consisted of George F. Broadley, Chairman, and Herbert T. Guess, Irvin Edward Michener and Ellis P. Morningstar.

Notice to Half Pay Officers and Out Pensioners of Chelsea and Kilmainham Hospitals- 1821

Discusses the half pay and pensions of Officers living within His Majesty's Dominions. At the bottom, there is also a comment made by Robert Morrogh to Daniel Shannon concerning the above notice.

Key for the Oak Chest

The key is 4 1/2 cm long and is attached to a gold cord ending in a burnt orange tassel.

Oak Chest

Oak chest measuring 36 cm in height 45 cm in width and 32 cm in depth. The cabinet contains 5 graduating drawers and it closes with 2 hinged doors, each bearing an arch. There are recessed brass handles on the 2 sides of the cabinet and one of these handles on each of the drawers. On the top of the cabinet there is an escutcheon engraved with “S.D. Woodruff Esq., St. Catharines, 157 Ontario”. The cabinet has a lock which is still functional and opens with a skeleton key which is part of this collection. The top 2 drawers have been lined with a piece of cardboard carefully cut to size and covered with brocade. There is some scratching on the top of the cabinet and one of the front doors is missing some of the wooden trim.

Notice of Location of Grave - Wailly Orchard Cemetery

Two notices from the Director of Graves Registration and Enquiries, London, England noting the location of the grave as Wailly Orchard Cemetery near Arras. One of the certificates incorrectly notes the name as S.G. Woodruff while the other correctly has S. D. Woodruff. The number listed for Lieut. S. D. Woodruff's grave site photograph is CCM/9/4433.