Tercera sesión del panel de expertos sobre la dinámica de la población de anchoveta peruana, julio de 1972

La tercera sesión del panel de expertos hace un reencuentro de las condiciones oceanográficas entre el año 1971 y 1972 respecto a la pesquería de la anchoveta.

Informe de la Cuarta sesión del panel de expertos de la evaluación del stock de anchoveta peruana

Se presenta una revisión de los sucesos de las pesquerías en el lapso desde la anterior reunión del Panel en Julio, 1972 y de lo que se piensa ha tenido lugar en el recurso y en su medio ambiente; se indican diversas líneas de investigación del stock. Se resume la evidencia colateral acerca de los stocks y de su medio ambiente; ésta se relaciona con el fenómeno de El Niño, con las aves guaneras, el aumento de las capturas de sardinas, el contenido graso de la anchoveta y los estadios de maduración de la misma. Cada una de estas entidades indican que recientemente han prevalecido condiciones especiales en el ambiente de la anchoveta, en la biota asociada y en ciertos aspectos de su fisiología. Se ha hecho una detallada revisión de varios tipos de investigación de las poblaciones de anchoveta y de las evidencias que, acerca del estado del recurso, pueden derivarse de tales investigaciones. Se examinó la evidencia obtenida del uso de equipo acústico en el estudio de la distribución de stocks y en la estimación de su abundancia; el trabajo se realizó mediante exploraciones de varias embarcaciones (exploraciones Eureka) y de exploraciones especiales con el barco de investigación SNP-1; también se hizo uso de equipo eco-integrador. Se discuten las fuentes de errores sistemáticos existentes en ese trabajo. Se llega a la conclusión que lo que ese trabajo indicó fue que en Febrero de 1973 existía alrededor de 4 millones de toneladas de anchoveta.

El Fenómeno El Niño 1972-1973

Las investigaciones oceanográficas del Perú, iniciadas en forma sistemática en 1961, han aportado hasta el momento un amplio conocimiento general sobre las aguas costeras del Perú y su complejo sistema de circulación. Existen muchos problemas por resolver, entre los que se encuentra la predicción del Fenómeno El Niño (FEN), fenómeno que reviste especial cuidado e importancia para el Perú, porque su aparición repercute negativamente en la economía del país al incidir principalmente en la pesquería peruana de la anchoveta que, no obstante ser singular y costera, en 1971 colocó al Perú en el primer puesto de los países pesqueros del mundo.

Faculty at 1974 Convocation

Pictured here from left to right are: Dr. Allan Booth, Classics, an unknown faculty member, and Peter Burtram, Registrar.

Women's Volleyball Team (1972-73)

Back Row: Marsia Antolak (Manager), Marcia Liddycoat, Wendy Krasovev, Violette Lavigne, Elanie Keith, Jean Nairn, Kathy Kirkpatrickm Pat Hueston (Coach) Front Row: Beth Craig, Lee Bartley, Judt Trowbridge, Jeanie Dulewicz, Miriam Ganton

Structural, stratigraphic and geochemical studies of the Horwood Peninsula - Gander Bay Area, Northeast Newfoundland /

The Horwood Peninsula - Gander Bay area is located at NE Newfoundland in the Botwood Zone (Williams et a1., 1974) or in the Dunnage Zone (Williams, 1979) of the Central Mobile Belt of the Newfoundland Appalachians. The area is underlain by Middle Ordovician to possible Lower Silurian rocks of the Davidsville and Indian Islands Groups, respectively. Three conformable formations named informally : the Mafic Volcanic Formation, the Greywacke and Siltstone Formation and the Black Slate Formation, have been recognized in the Davidsville Group. The Greywacke and the Black Slate Formations pass locally into a Melange Formation. From consideration of regional structure and abundant locally-derived mafic volcanic olisto- 1iths in the melange, it is considered to have originated by gravity sliding rather than thrusting. Four formations have been recognized in the Indian Islands Group. They mainly contain silty slate and phyllite, grey cherty siltstone, green to red micaceous siltstone and limestone horizons. Repetition of lithological units by F1 folding are well-demonstrated in one of formations in this Group. The major structure in this Group on the Horwood Peninsula is interpreted to be a synclinal complex. The lithology of this Group is different from the Botwood Group to the west and is probably Late Ordovician and/or Early Silurian in age. The effects of soft-sediment deformation can be seen from the lower part of the Davidsville Group to the middle part of the Indian Islands Group indicating continuous and/or episodic slumping and sliding activities throughout the whole area. However, no siginificant depOSitional and tectonic break that could be assigned to the Taconian Orogeny has been recognized in this study. Three periods of tectonic deformation were produced by the Acadian Orogeny. Double boudinage in thin dikes indicates a southeast-northwest sub-horizontal compression and main northeast-southwest sub-horizontal extension during the D1 deformation. A penetrative, axial planar slaty cleavage (Sl) and tight to isocJ.ina1 F1 folds are products of this deformation. The D2 and D3 deformations formed S2 and S3 fabrics associated with crenulations and kink bands which are well-shown in the slates and phyllites of the Indian Islands Group. The D2 and D3 deformations are the products of vertical and northeast-southwest horizontal shortening respectively. The inferred fault between the Ordovician slates (Davidsville Group) and the siltstones (Indian Islands Group) suggested by Williams (1963, 1964b, 1972, 1978) is absent. Formations can be followed without displacement across this inferred fault. Chemically, the pillow lavas, mafic agglomerates, tuff beds and diabase dikes are subdivided into three rock suites : (a) basaltic komatiite (Beaver Cove Assemblage), (b) tholeiitic basalt (diabase dikes), (c) alkaline basalt (Shoal Bay Assemblage). The high Ti02 , MgO, Ni contents and bimodal characteristic of the basaltic komatiite in the area are comparable to the Svartenhuk Peninsula at Baffin Bay and are interpreted to be the result of an abortive volcano-tectonic rift-zone in a rear-arc basin. Modal and chemical analyses of greywackes and siltstones show the trend of maturity of these rocks increasing from poorly sorted Ordovician greywackes to fairly well-sorted Silurian siltstones. Rock fragments in greywackes indicate source areas consisting of plagiogranite, low grade metamorphic rocks and ultramafic rocks. Rare sedimentary structures in both Groups indicate a southeasterly provenance. Trace element analyses of greywackes also reveal a possible island-arc affinity.

Decision-making theory applied to India's explosion of a nuclear device in May, 1974

This essay reviews the decision-making process that led to India exploding a nuclear device in May, 1974. An examination of the Analytic, Cybernetic and Cognitive Theories of decision, will enable a greater understanding of the events that led up to the 1974 test. While each theory is seen to be only partially useful, it is only by synthesising the three theories that a comprehensive account of the 1974 test can be given. To achieve this analysis, literature on decision-making in national security issues is reviewed, as well as the domestic and international environment in which involved decisionmakers operated. Finally, the rationale for the test in 1974 is examined. The conclusion revealed is that the explosion of a nuclear device by India in 1974 was primarily related to improving Indian international prestige among Third World countries and uniting a rapidly disintegrating Indian societal consensus. In themselves, individual decision-making theories were found to be of little use, but a combination of the various elements allowed a greater comprehension of the events leading up to the test than might otherwise have been the case.

McKinnon Columbus Chain Limited Records 1948, 1958-1960, 1963-1969, 1971, 1974-1975, 1978, n.d.

Ontario Editorial Bureau (O.E.B.)

Scott Misener Steamships Co. Ltd. Records, 1965, 1967, 1972-1977, 1987, n.d.

Ontario Editorial Bureau (O.E.B.)

A study of selected factors influencing the reproductive performance of the common tern (Sterna hirundo) at Port Colborne, Ontario in 1973 and 1974

Several study areas were investigated at two Port Colborne terneries during the summers of 1973 and 1974 in an attempt to determine the influence of clutch size, time of clutch initiation, position in the colony, proximity to Ring-billed Gulls, vegetation and nesting substrate on the reproductive performance of the Common Tern. Hatching success and reproductive success (the number of chicks fledged per egg laid) were generally higher for 3-egg than 2-egg clutches but fledging (the number of chicks fledged per egg hatched) success was usually independant of clutch size. Hatching, fledging and reproductive success declined as a function of time of clutch initiation. Mean clutch sizes also generally declined as a function of time. Nests located in the center of the colony exhibited higher fledging success than those on the periphery. Rock-based clutches had a lower hatching success than clutches initiated on sand or dried vegetation. Reproductive performance did not appear to be related to proximity to Ring-billed Gulls or vegetation within the study area.

Ontario Medical Association fonds, 1972-1973, 1977-1978, 1980-1982, 1984-1985

This archive contains materials relating to the Ontario Medical Association. The bulk of the materials are correspondence. A complete administrative history of the association is available from, The first 100 years : a history of the Ontario Medical Association / Glenn Sawyer, Toronto : The Association, 1980? (R15 O58 S39 1980).