227 resultados para Oosterbaan, Bennie Gaylord


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Front row: (l-r) George Burg, Eugene Derricotte, Clem Bauman, Bruce Hilkene, Joe Ponsetto, Bob Wiese, Bob Nussbaumer, John Lintol, Roger Choeverini, Arthur Renner, Arthur LeRoux.

Second row: Dick DeMark, Dick Rifenburg, Bill Culligan, Jim Aliber, Ralph Chubb, Edward Greer, Quentin Sickels, Charles Wahl, Jerry Brielmaier, Milan Lazetich, Tom Swift, Tom Peterson.

Third row: Joe Oeming, Dick Smith, Cecil Freihofer, John Weyers, Henry Mantho, Jack Weisenburger, John Babyak, Warren Bentz, Don Fate, Bob Mann, Don Lund, Howard Yerges, Bill Wenzlau.

Fourth, row Bob Oren, Frank Nakamura, Maurice Dunne, Bill Kerr, George Abbott, Charles Sampson, Frank Honigsbaum, Henry Milczuk, Roger Eli, George Babe, Ed Sohacki, Dave Adams, Don Drake, Don Spink.

Back row: H. 0. Crisler, head coach; Henry Hatch, equipment man; Ray Roberts, trainer; D. E. Williamson; Benny Oosterbaan, end coach; Clarence Munn, line coach; Earl T. Martineau, backfield coach.

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Top Row: Douglas Niles, Frederick Langille, Wallace Herrala, Charles Peltz, Jeff Engel.

3rd Row: asst. coach Elmer Swanson, Richard Thelwell, Carter Reese, Jerry Gerich, Stephen Overton, Charles Aquino, James Montour.

2nd Row: Rodney Denhart, William Hornbeck, Bennie McRae, John Gregg, Raymond Locke, Frank Geist, L. Bryan Gibson, Donald Chalfant.

Front now Lester Bird, Marshall Dickerson, Richard Cephas, Ergas Leps, Coach Don Canham, David Martin, James Wyman, Walter Schafer.

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Front Row, Left to Right: Thomas DeMassa, James Sytek, Jack Zachary, Robert Wojcik, Jerry Leith, Harry Newman, Jr., Dave Brown, James McPherson, Alvin Groce, Grant Walls, John Halstead, Joseph Brefeld, Richard Syring, Phil Barger, Wilfrid Grein, John Galarneault.

Second Row: Coach Don Dufek, John Batsakes, Paul Poulos, Fred Olm, Dennis Fitzgerald, Jim Byers, Doug Oppman, Robert Ptacek, John Herrnstein, Gary Prahst, Walt Johnson, Gerald Marciniak, Willie Smith, Anthony Rio, Michael Dupay, Mike Fillichio, Bob Johnson, Jim Dickey, Coach Matt Patanelli.

Third Row: Coach Jack Blott, Coach Bob Hollway, James Gray, Maynard Stetten, Gordon Morrow, Eugene Sisinyak, Guy Curtis, B. Lee Hall, Darrell Harper, Jared Bushong, Alex Callahan, Wesley Maki, Donald Kolcheff, Fred Julian, George Genyk, Gerald Smith, Robert Swanson, Willerfred Wilson, Erwin Crownley, Coach Ben Oosterbaan.

Back Row: Coach Wally Weber, Reid Bushong, Gary McNitt, Bill Stein, Tom Jobson, Donald Hannah, Gary Kane, John Walker, Willard Hildebrand, Paul Raeder, Darrell Thorpe, Daniel Snow, Thomas Kerr, Lovell Farris, David Palomaki, Bradley Myers, Donald Deskins, Arthur Lazik, John Spidel, Keith Cowan, Henry Stuart, Coach "Bump" Elliott.

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[l-r: Harry Kipke, Fritz Crisler, Bennie Oosterbaaan, Bump Elliott, Bo Schembechler]

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Without music; some tunes indicated by title.

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Mode of access: Internet.

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Thesis (doctoral)--

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This study examines cross-generational survival strategies, among Southern Rural Black women. Through their oral histories, the currents that run through the lives of five women will be examined from a Black female's perspective. While the experiences are richly different across four generations, these women have provided for their families despite the triple discrimination of being female, poor, and Black. Three important survival resources are identified: kin, education, and religion. The mothering role emerged as a master status with special emphasis on the mother-daughter relationship. ^

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Immigrants from the West Indies and other nations challenge the simple United States dichotomy of blacks versus whites. Many apparently black Caribbean immigrants proclaim that they did not know they were “black” until they arrived in the U.S. They seek to maintain their national identity and resist identity and solidarity with Black Americans. In response, many Black Americans respond that the immigrants are simply being naive, that U.S. society demands simple racial identity. Regardless of one's self-identity and personal history, in the U.S., if you look black, you are black, was their thinking. ^ This study examines the contemporary struggle of identity and solidarity among and between Black Americans and Jamaicans living in South Florida (Broward and Miami-Dade counties). Even though the primary focus of this study is to examine the relationship between Black Americans and Jamaicans, other West Indian nationals will be addressed more generally. The primary research problem of this study is to determine why the existence of common ancestry and physical traits are insufficient for an assumption of ethnic solidarity between Black Americans and Jamaicans. ^ In examining this problem, I felt that depth rather than breadth would provide insight into the current state of polarization between Black Americans and Jamaicans. To this end, a qualitative study was designed. A non-random snowball sample consisting of forty-seven informants was selected for this study. Realizing that such a technique presents problems with generalizations beyond the sample, this approach was, nonetheless, the most suitable for the current research problem. One of the initial challenges of this research was the use of the label “black” in discussing Caribbean immigrants. Unlike America, where distinctions based on skin color were at the bedrock of America's formation, this was not the case in the Caribbean. In the Caribbean skin color was an important marker as an indicator of class, rather than of race. Therefore, I refrained from using the label, “black Jamaicans,” but rather used Jamaicans throughout. ^

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Anthropogenic emissions of carbon dioxide (CO2) are causing ocean acidification, lowering seawater aragonite (CaCO3) saturation state (Omega arag), with potentially substantial impacts on marine ecosystems over the 21st Century. Calcifying organisms have exhibited reduced calcification under lower saturation state conditions in aquaria. However, the in situ sensitivity of calcifying ecosystems to future ocean acidification remains unknown. Here we assess the community level sensitivity of calcification to local CO2-induced acidification caused by natural respiration in an unperturbed, biodiverse, temperate intertidal ecosystem. We find that on hourly timescales nighttime community calcification is strongly influenced by Omega arag, with greater net calcium carbonate dissolution under more acidic conditions. Daytime calcification however, is not detectably affected by Omega arag. If the short-term sensitivity of community calcification to Omega arag is representative of the long-term sensitivity to ocean acidification, nighttime dissolution in these intertidal ecosystems could more than double by 2050, with significant ecological and economic consequences.

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The exponential growth of studies on the biological response to ocean acidification over the last few decades has generated a large amount of data. To facilitate data comparison, a data compilation hosted at the data publisher PANGAEA was initiated in 2008 and is updated on a regular basis (doi:10.1594/PANGAEA.149999). By January 2015, a total of 581 data sets (over 4 000 000 data points) from 539 papers had been archived. Here we present the developments of this data compilation five years since its first description by Nisumaa et al. (2010). Most of study sites from which data archived are still in the Northern Hemisphere and the number of archived data from studies from the Southern Hemisphere and polar oceans are still relatively low. Data from 60 studies that investigated the response of a mix of organisms or natural communities were all added after 2010, indicating a welcomed shift from the study of individual organisms to communities and ecosystems. The initial imbalance of considerably more data archived on calcification and primary production than on other processes has improved. There is also a clear tendency towards more data archived from multifactorial studies after 2010. For easier and more effective access to ocean acidification data, the ocean acidification community is strongly encouraged to contribute to the data archiving effort, and help develop standard vocabularies describing the variables and define best practices for archiving ocean acidification data.

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Funding and trial registration: Scottish Government Chief Scientist Office grant CZH/3/17. ClinicalTrials.gov registration NCT01602705.

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Earlier versions were presented at the ECPR Joint Sessions Workshop on ‘How and Why of Party Manifestos in New and Established Democracies’, University of St. Gallen, April 2011, and at PSA and EPOP Conferences in 2011. We are grateful to all participants for their feedback, and particularly Bob Harmel and Lars Svasand for their comments and leading this project. We are also grateful to Dai Moon for discussions around Welsh manifestos and highlighting some otherwise unavailable literature. The usual disclaimers naturally apply. Alistair Clark gratefully acknowledges the financial support of a British Academy Overseas Conference Grant, Award Number OC100383 for travel to the 2011 ECPR Joint Sessions. The final definitive version of this paper has been published in Party Politics by SAGE Publications Ltd and is available on the journal website at: http://ppq.sagepub.com/ All Rights Reserved © Alistair Clark and Lynn Bennie.

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Ocean acidification will likely have negative impacts on invertebrates producing skeletons composed of calcium carbonate. Skeletal solubility is partly controlled by the incorporation of "foreign" ions (e.g. magnesium) into the crystal lattice of these skeletal structures, a process that is sensitive to a variety of biological and environmental factors. Here we explore effects of life stage, oceanographic region of origin, and changes in the partial pressure of carbon dioxide in seawater (pCO2) on trace elemental composition in the purple sea urchin (Strongylocentrotus purpuratus). We show that, similar to other urchin taxa, adult purple sea urchins have the ability to precipitate skeleton composed of a range of biominerals spanning low- to high-Mg calcites. Mg / Ca and Sr / Ca ratios were substantially lower in adult spines compared to adult tests. On the other hand, trace elemental composition was invariant among adults collected from four oceanographically distinct regions spanning a range of carbonate chemistry conditions (Oregon, Northern California, Central California, and Southern California). Skeletons of newly settled juvenile urchins that originated from adults from the four regions exhibited intermediate Mg / Ca and Sr / Ca between adult spine and test endmembers, indicating that skeleton precipitated during early life stages is more soluble than adult spines and less soluble than adult tests. Mean skeletal Mg / Ca or Sr / Ca of juvenile skeleton did not vary with source region when larvae were reared under present-day, global-average seawater carbonate conditions (400 µatm; pHT = 8.02 ± 0.03 1 SD; Omega calcite = 3.3 ± 0.2 1 SD). However, when reared under elevated pCO2 (900 µatm; pHT = 7.73 ± 0.03; Omega calcite = 1.8 ± 0.1), skeletal Sr / Ca in juveniles exhibited increased variance across the four regions. Although larvae from the northern populations (Oregon, Northern California, Central California) did not exhibit differences in Mg or Sr incorporation under elevated pCO2 (Sr / Ca = 2.10 ± 0.06 mmol/mol; Mg / Ca = 67.4 ± 3.9 mmol/mol), juveniles of Southern California origin partitioned ~8% more Sr into their skeletons when exposed to higher pCO2 (Sr / Ca = 2.26 ± 0.08 vs. 2.09 ± 0.005 mmol/mol 1 SD). Together these results suggest that the diversity of carbonate minerologies present across different skeletal structures and life stages in purple sea urchins does not translate into an equivalent geochemical plasticity of response associated with geographic variation or temporal shifts in seawater properties. Rather, composition of S. purpuratus skeleton precipitated during both early and adult life history stages appears relatively robust to spatial gradients and predicted future changes in carbonate chemistry. An exception to this trend may arise during early life stages, where certain populations of purple sea urchins may alter skeletal mineral precipitation rates and composition beyond a given pCO2 threshold. This potential for geochemical plasticity during early development in contrast to adult stage geochemical resilience adds to the growing body of evidence that ocean acidification can have differing effects across organismal life stages.