UM Women's Track Team, 1990

Outside Row, standing, bottom left to top to bottom right) Sarah Neely, Carrie Yates, Nicole Chinavare, Jennifer Reed, Stephanie Frohock, Shana Parrish, Dyan Jenkins, Karen Welke, Jennifer McPeck, Gillian Osborne, Judy Yuhn, Amy Bannister, Mindy Rowand

Front Row (kneeling): Ronda Ricketts, Andrea Baas, Alexis Collins, Amy McCormick, Kim Haluscsak, Julie Victor, Sandy Elliott, Lisa Adams

2nd Row: Kirsten McDonald, Michelle Bishop, Gina Barnett, Molly McClimon, Alana Davis, Amy Bucholz

3rd Row: Suzette Thweatt, Alison Smith, Megan Nortz

UM Women's Track Team, 1994

Front Row: Heather Grigg, Abbie Schaefer, Molly McClimon, Jennifer Barber, Christie Wilson, Amy Parker, Theresa Hall, Carrie Stewart, Mara Guillemette

Second Row: Laura Jerman, Holly Logue, Monika Black, Denise James, Katy Hollbacher, Kelly Chard, Courtney Babcock, Jackie Concaugh, Tearza Johnson, Emily Shively, Sharmila Prasad, Kim Skryd

Third Row: Kathryn Huffman, Annie Erlewine, Beth Gould, Richelle Webb, Michelle Spannagel, Kristie Wink, Chris Szabo, Karen Harvey, Jessica Kluge, Kristine Westerby, Ebony McClain, Colette Savage, Tonya Broad, Lisa Adams

Fourth Row: Ingrid Sharphorn, Elizabeth VanderVelde, Molly Lori, Jen Peterson, Ronda Meyers, Linda Stuck, Deb Mans, Jayna Greiner, Kathy Tomko, Laura Molnar

UM Women's Track Team, 1994

Front Row: Katy Hollbacher, Kristine Westerby, Chris Szabo, Courtney Babcock, Laura Jerman, Jessica Kluge, Richelle, Webb, Karen Harvey, Molly McClimon

Second Row: Ronda Meyers, Carrie Stewart, Theresa Hall, Tearza Johnson, Colette Savage, Annie Erlewine, Sharmila Prasad, Tanya Clay, Kim Skryd, Monika Black

Third Row: Emily Shively, Linda Stuck, Jen Peterson, Kathy Tomko, Tonya Broad, Julie Copley, Abbie Schaefer, Beth Gould, Mayrie Richards

Back Row: Jackie Concaugh, Mara Guillemette, Laura Molnar, Christie Wilson, Amy Parker, Jayna Greiner, Michelle Spannagel, Heather Grigg, Deb Mans

Hidrología médica española : monografía de las aguas súlfidrico-álcalino-frias del Duque ó Fuensanta [Manuscrito] /

Mode of access: Internet.

UM Women's Track Team, 1993

Front Row: Molly Lori, Katy Hollbacher, Jackie Concaugh, Jennifer Barber, Michelle Spannagel, Ebony McClain, Monika Black, Tearza Johnson, Tanya Broad, Julie Copley, Amy Parker, Christie Wilson

2nd Row: Trainer Jean Lett, Abbie Schaefer, Jen Stuht, Debbie Mans, Jessica Kluge, Chris Szabo, Jayna Greiner, Kelly Chard, Ronda Meyers, Mayrie Richards, Linda Stuck, Kathy Tomko, Theresa Hall, Christi Foster, Tanya Clay, Bryn Gerich

3rd Row: Rachel Mann, Karen Harvey, Courtney Babcock, Colette Savage, Laura Jerman, Alexis Collins, Richelle Webb

4th Row: Kristine Westerby, Kristi Wink, Amy Buchholz, Lisa Adams Top Row: Molly McClimon, Julie Victor

Paridades de poder adquisitivo para América Latina y el Caribe, 2005-2013: métodos y resultados

Este trabajo tiene como objetivo presentar algunos aspectos metodológicos y las series del producto interno bruto (pib) de América Latina y el Caribe con respecto al período 2005-2013, expresadas en paridades del poder adquisitivo (ppa), y señalar algunas limitaciones de este tipo de ejercicio. Se realizan comparaciones con las series (a precios corrientes y constantes) expresadas en dólares con tipos de cambio de mercado, y también con los resultados de la ronda del Programa de Comparación Internacional (pci) efectuada en 2005. Asimismo, se adelantan algunas hipótesis interpretativas sobre el comportamiento de las principales variables económicas calculadas en el estudio.

Intercambio entre lectores. Un proyecto con mujeres y niños en contexto de encierro

El artículo expone algunas experiencias y resultados del proyecto "Lectura y escritura en la Unidad 33. Madres, niños e instituciones educativas" que se inició como proyecto de Extensión de la Universidad Nacional de La Plata en el año 2010. El proyecto implementa con mujeres y niños que viven en situación de encierro un conjunto de acciones con diferentes grados de formalización en torno a las culturas de lo escrito y otras formas de expresión, en tanto prácticas culturales que tienen derecho de ejercer y ampliar en diversas situaciones de interacción social. Se presentan los distintos espacios de trabajo y se sintetizan algunos resultados de un un taller denominado "la ronda: historia, poesías y canciones" Del análisis de las situaciones propuestas y los datos recogidos de un corpus de entrevistas semiestructuradas a un grupo de mujeres participantes, con edades entre 19 y 33 años, se destaca el sentido y valor de las lecturas e intercambios entre lectores literarios en la vida cotidiana del encierro

Nostalgia do espaço e do tempo: uma leitura da obra memorialística de Câmara Cascudo

This dissertation addresses the work of the memoirs of the potiguar writer Luís da Câmara Cascudo (1898 - 1986) from an integrated reading of four works that comprise: O Tempo e Eu (1968), Pequeno Manual do Doente Aprendiz (1969), Na Ronda do Tempo (1971) and Ontem (1972). Produced under the contingency of the modern movement and urban reform, memories Cascudo evoke the old landscapes of old, populated by those who belonged to the old romantic and provincial Natal that no longer exists, but which still survives in the idealized memory author and that is (re)constructed by him from a written permeated with touches of imagination and a sense of nostalgia. Seeking to analyze how is the process of building memoirist of Cascudo, as well as reflect on the role that memory plays in the (re)construction of a time and a lost space, we used the studies of Maurice Halbwachs (2006) and Ecléa Bosi (1994). Within this theoretical framework, we seek, above all, to understand not only how the lived experiences of Cascudo will work in this matter of his memory, but also as this will guide a writing that touches on the history and social frameworks of the past

Petrographic and geochemical characterization of a sample taken from the beni bousera peridotite (Morocco)

Il massiccio di Beni Bousera (Marocco) è formato da diverse unità geologiche composte prevalentemente da rocce metamorfiche molto simili a quelle che si trovano nel massiccio di Ronda (Spagna). Queste due catene montuose erano connesse prima dell’estensione (iniziata nel Miocene inferiore) che le ha separate lasciando il posto al mare di Alborán. Questo studio sarà incentrato soltanto sul massiccio marocchino, in particolare sull’unità peridotitica di Beni Bousera. Questa unità è stata suddivisa in quattro domini, ognuno dei quali ha specifiche caratteristiche petrologiche e geochimiche, che sono il risultato di diverse condizioni metamorfiche e di diversi regimi tettonici. L’obiettivo di questo lavoro è di caratterizzare, dal punto di vista petrologico, un campione che è stato prelevato dal massiccio di Beni Bousera, nella zona costiera del mare di Alborán e di determinare a quale dominio esso appartiene.

Relative abundance of planktonic foraminifera in Pliocene and Pleistocene sediments of DSDP Hole 32-310 from Hess Rise, Central North Pacific (Table II)

Late Neogene planktonic foraminifera have been examined at Site 310 in the Central North Pacific and their stratigraphic ranges and frequencies are presented here. Blow's (1969) zonation developed for tropical regions has been applied where applicable. Where tropical index taxa are rare or absent in this temperate region, Globorotalia crassaformis, and the evolutionary bioseries G. conoidea - G. conomiozea and G. puncticulata - G. inflata have been found useful for zonal subdivisions. A correlation between stratigraphic ranges and frequency distributions of these species at Site 310 in the Central North Pacific, and Site 284 in the Southwest Pacific indicates that these species are relatively consistent biostratigraphic markers in temperate regions of both the North and South Pacific Oceans. An informal zonation for temperate latitudes of the Southwest Pacific has been established by Kennett (1973) and a similar zonal subdivision can be made at Site 310. Paleoclimatic/paleoceanographic interpretations based on coiling ratios, percent abundance, and phenotypic variations of Neogloboquadrina pachyderma indicate four major cold events during early, middle, and late Pliocene, and early Pleistocene. Faunal correlations of these events with similar events elsewhere in the Northeast and Southwest Pacific which have been paleomagnetically dated indicate the following approximate ages for these cold events: 4.7 Ma, 3.0 Ma, 2.6-1.8 Ma, and 1.2 Ma. Faunal assemblages have been divided into three groups representing cool, intermediate, and warmer water assemblages. Cool water assemblages are dominated by ~60% N. pachyderma; intermediate temperature faunas are dominated by species of Globigerina and Globigerinita and contain between 20% and 30% N. pachyderma. Warmer water assemblages are dominated by species of Globorotalia and contain <10% N. pachyderma. Frequency oscillations within these groups, in addition to paleotemperature parameters evident in N. pachyderma, afford refined paleoclimatic/paleoceanographic interpretations.

Distribution of planktonic foraminifera in DSDP Hole 31-296 (Table III)

Late Neogene planktonic foraminiferal biostratigraphy of DSDP Site 296, Leg 31, reveals this site as an ideal reference section for correlation of Blow's low-latitude zonation with the mid-latitude zonation for temperate faunal assemblages developed in this paper and earlier for DSDP Site 310, Leg 31 (Keller). Abundance of temperate species of Globorotalia (G. inflata, G. puncticulata, G. crassaformis, G. conomiozea) permit correlation with the zonal subdivision developed at Site 310 based on these species. Evolutionary changes within the Globorotalia inflata group also appear to be consistent biostratigraphie markers in mid latitudes; a primitive variety of this species first appears at about 3.3-3.1 Ma, G. inflata praeinflata appears at about 2.6 Ma, and the modern form appears at about 2.2-2.1 Ma. Quantitative analyses of planktonic foraminifera at DSDP Site 296 reveal an inversely reciprocal frequency oscillation between species of Globorotalia and the Globigerina-Globigerinita group. Cool climatic periods are characterized by high frequencies in the Globigerina-Globigerinita group and low frequencies in the Globorotalia group, whereas warm intervals are marked by high frequencies in the Globorotalia group and low frequencies in the Globigerina-Globigerinita group. Five cool paleoclimatic events can be recognized between early Pliocene and late Pleistocene: 4.4 Ma, 3.2-3.1 Ma, 2.4-2.2 Ma, 1.2 Ma, and 0.7 Ma. These paleoclimatic/paleoceanographic events have also been recognized in planktonic foraminifera of the Central and Northeast Pacific DSDP Sites 310 and 173 and also correlate to cold events recognized in oxygen isotope measurements of DSDP Site 310 and in equatorial Pacific cores.