Joe Strong on the trapeze : or, The daring feats of a young circus performer /

Mode of access: Internet.

The world's best poetry ...

Mode of access: Internet.

Lois Carrol;

Mode of access: Internet.

Church portals.

Mode of access: Internet.

School of Nursing Class of 2002

Top Row: Robyn Albrecht, Brea Anne Aldorfer, Elizabeth Andersen, Jamie Anderson, TaNea Andrews, Julie Badgero, Margarita Barrientes, Jessica Barton, Jennifer Baughman, Catherine Baxter, Jeff Bell, Jessica Bellardi, Sarah Bethel, Melissa Black, Sherese Black

Row 2: Daniela Bordei, Hannah Burgess, Tonya Melton, Patricia Kelly, Tanina Media, Lenette Whitehead, Suzanne Begeny, Jasmine Beale, Martha Richard, Stephanie A. Shafer, Sarah Wilson, Staci Byrd, Jennifer Cheng

Row 3: Rebecca Cohrs, Jeana Cox, Regina Cox, Emalee Danforth, Susan Daron, Kara Dazarow, Marites de la Fuente, Abigail Devine, Carrie Dickson, Christopher Ducher

Row 4: Jennifer Flynn, Elizabeth Foster, Nicole Gatesy, Michelle Gaudreau, Melissa Hagan, christa Hamilton, Christina Hazergian, Crystal Herwat, Rebecca Hunnicutt, Emily Johnston

Row 5: Valerie Jons, Rani Khan, Anne Konczak, Teresa Konopka, Joanne Pohl, Nola Pender, Carol Loveland-Cherry, Ada Sue Hinshaw, Margaret Calarco, Judith Lynch-Sauer, Jan L. Lee, Jill LaDronka, Shane LaGore, Melanie LaPierre, Stacy lamb

Row 6: Kathleen Laughlin, Holly Leupp, Emily Lewellen, Victoria Lilga, Bethany Lusher, Nancy Ma, Lindsay Mahlstedt, K. Luba Manko, Beverley Marchant, Anne Marlatt, Martha Mason, Deborah McConnell, Robin Meganck, Jill Messina

Row 7: Patricia Milne, Yvonne Moran, Melissa Myer, Bradley Niese, Brooke Oakley, Kristy Opasik, Amanda O'Reilly, Elisabeth Paulson, Nancy Pavelek, Johnnie Peoples, Melissa Perry, Elissa Pocze, Michelle Ponikvar, Victoria Portman, Shelley Reeves

Row 8: Michael Rempel, Jill Richert, Jennifer N. Rish, Rebekah Royce, Kristan Schoenfeld, Shawn Schofield, Holly Setterington, Heidi Sprunk, Emily Staugaard, Rachel Stevens, Linda Suh, Tiffany Sylvertooth, Kimberly Taylor-Vincent, Arik Theeke

Row 9: Kim Thomas, Stephanie Thompson, Patricia Tillman, Leigh Tooman-Letson, Ryan Upson, Nicole Vance, Jacquelynne Walsh, Jill Weirich, Monica White, Anthony Worley, Heide Wright, Kelly Yager, Marichal Young

French portraits;

Mode of access: Internet.

Systematic organic chemistry : modern methods of preparation and estimation /

Includes index.

Systematic organic chemistry, modern methods of preparation and estimation,

Mode of access: Internet.

Low-flow transport models for conservative and sorbed solutes, Uvas Creek, near Morgan Hill, California /

Bibliography: p. 73-74.

New farm homes for old; a study of rural public housing in the South,

Mode of access: Internet.

SALT II agreement, Vienna, June 18, 1979.

Includes index.

Change in abundance of dugongs in Shark Bay, Ningaloo and Exmouth Gulf, Western Australia: evidence for large-scale migration

The third in a series of five-yearly aerial surveys for dugongs in Shark Bay, Ningaloo Reef and Exmouth Gulf was conducted in July 1999. The first two surveys provided evidence of an apparently stable population of dugongs, with similar to 1000 animals in each of Exmouth Gulf and Ningaloo Reef, and 10000 in Shark Bay. We report estimates of less than 200 for each of Exmouth Gulf and Ningaloo Reef and similar to 14000 for Shark Bay. This is an apparent overall increase in the dugong population over this whole region, but with a distributional shift of animals to the south. The most plausible hypothesis to account for a large component of this apparent population shift is that animals in Exmouth Gulf and Ningaloo Reef moved to Shark Bay, most likely after Tropical Cyclone Vance impacted available dugong forage in the northern habitat. Bias associated with survey estimate methodology, and normal changes in population demographics may also have contributed to the change. The movement of large numbers of dugongs over the scale we suggest has important management implications. First, such habitat-driven shifts in regional abundance will need to be incorporated in assessing the effectiveness of marine protected areas that aim to protect dugongs and their habitat. Second, in circumstances where aerial surveys are used to estimate relative trends in abundance of dugongs, animal movements of the type we propose could lead to errors in interpretation.

Faunal evidence for a difference in clothing use between Neanderthals and early modern humans in Europe

MC is grateful to Karen Lupo and Brian Codding for the invitation to participate in the symposium honouring Jim O’Connell at the 2015 annual meeting of the Society for American Archaeology in San Francisco, and for the invitation to contribute to this special issue of the Journal of Anthropological Archaeology. We thank Conrad Brimacombe, Kate Britton, Keith Dobney, Mana Dembo, Marina Elliott, Ian Gilligan, Brian Hayden, Trenton Holliday, Vance Hutchinson, Steve Kuhn, Dana Lepofsky, Lee Lyman, Luseadra McKerracher, Kim Plomp, Bernard Wood, and an anonymous reviewer for their comments on earlier versions of this paper. Ian Gilligan’s comments in particular resulted in major changes to the interpretation of the results. MC is supported by the Social Sciences and Humanities Research Council of Canada, the Canada Research Chairs Program, the Canada Foundation for Innovation, the British Columbia Knowledge Development Fund, and Simon Fraser University. LT work on the study reported here was supported by the Social Sciences and Humanities Research Council of Canada (award no. 755-2011-0406). We are grateful to all these funding bodies. Last but not least, MC would like to express his gratitude to Jim O’Connell for his friendship and guidance over nearly 20 years. Thanks Jim. You’re the dog’s bollocks.

Nd/Ca ratios in plankton-towed and core top foraminifera

Planktic foraminifera have been used as recorders of the neodymium (Nd) isotopic composition of seawater, although there is still controversy over the precise provenance of the Nd signal. We present an extensive, multispecific plankton tow Nd/Ca data set from several geographic locations (SE Atlantic, NE Atlantic, Norwegian Sea, and western Mediterranean), together with core top samples from the Mediterranean region. The range of Nd/Ca ratios in plankton-towed foraminifera, cleaned only of organic material, from all regions (0.01-0.7 µmol/mol), is similar to previously published analyses of sedimentary foraminifera cleaned using both oxidative and reductive steps, with distribution coefficients (Kd) ranging between 4 and 302. For the Mediterranean, where core top and plankton tow data are both available, the range for plankton tows (0.05-0.7 µmol/mol) is essentially identical to that for the core tops (0.1-0.5 µmol/mol). Readsorption of Nd during cleaning is ruled out by the fact that the plankton tow samples underwent only an oxidative cleaning process. We find a relationship between manganese (Mn) and Nd in plankton tow samples that is mirrored by a similar correlation in core top samples. This relationship suggests that Fe-Mn coatings are of negligible importance to the Nd budgets of foraminifera as the Nd/Mn ratio it implies is over an order of magnitude greater than that seen in other Fe-Mn oxide phases. Rather, since both plankton tows and core tops present a similar behavior, the Nd/Mn relationship must originate in the upper water column. The data are consistent with the acquisition of Nd and Mn from the water column by binding to organic material and the fact that intratest organic material is shielded from both aggressive cleaning and diagenetic processes. Collectively, the results help to explain two abiding puzzles about Nd in sedimentary planktic foraminifera: their high REE contents and the fact that they record a surface water Nd isotopic signal, regardless of the cleaning procedure used.