1933 UM Football Team, full squad posed on Ferry Field

Back Row: Herman Everhardus, Sylvester Shea, ? Rygg, Willis Ward, Tom Austin, Chuck Bernard, Francis Wistert, Donald McGuire, Harvey Chapman, Willard Hildebrand, John Viergiver, Russell Fuog, Wallace Frankowski, Fred Petoskey, Roy Semeyn, Robert Swanson, Gerald Ford

Middle Row: captain Stan Fay, William Renner, Henry Raymond, Hilton Ponto, Robert Wells, James Kidston, John Kowalik, Russ Oliver, Oscar Singer, Carl Savage, Chester Beard, John Regeczi, Herbert Schmidt, William Borgmann, Steve Remias

Front Row: George Rudness, Estel Tessmer, Lee Shaw, Louis Westover, Arthur Patchin, Lawrence Ratterman, Richard James, David Hunn, Eli Soodik, George Bolas, Antone Dauksza, Winfred Nelson, Herbert Paulson, Howard Triplehorn, D. King Lewis, ? Hall

University of Michigan Football Team, 1934, full squad posed on practice field

Back Row: Cedric Sweet, Franklin Lett, Steve Remias, Carl Carr, Russ Oliver, captain Thomas Austin, Robert Johnson, Willard Hildebrandt, Edward Stone, Michael Savage, Thomas Oyler, Harry Wright, Joe Fisher, Jack Liffiton, John Viergever, Herman Everhardus, Willis Ward, Matt Patanelli, Robert Graper

Middle Row: John Mumford, James Kidston, William Borgmann, Chester Beard, Howard Triplehorn, Vincent Pope, Ernest Pederson, Joseph Ellis, Robert Amrine, Russell Fuog, Stanton Schuman, Vincent Aug, Winfred Nelson, John Regeczi

Front Row: John Connolly, Jesse Garber, David Barnett, John Rieck, Frank Bissell, Eli Soodik, William Renner, Richard James, Ferris Jennings, Harry Pillinger, Harry Lutomski, George Bolas, Charles Brandman, Gerald Ford

University of Michigan Football Team, 1934, full squad posed on practice field

Back Row: Cedric Sweet, Franklin Lett, Steve Remias, Carl Carr, Russ Oliver, captain Thomas Austin, Robert Johnson, Willard Hildebrandt, Edward Stone, Michael Savage, Thomas Oyler, Harry Wright, Joe Fisher, Jack Liffiton, John Viergever, Herman Everhardus, Willis Ward, Matt Patanelli, Robert Graper

Middle Row: John Mumford, James Kidston, William Borgmann, Chester Beard, Howard Triplehorn, Vincent Pope, Ernest Pederson, Joseph Ellis, Robert Amrine, Russell Fuog, Stanton Schuman, Vincent Aug, Winfred Nelson, John Regeczi

Front Row: John Connolly, Jesse Garber, David Barnett, John Rieck, Frank Bissell, Eli Soodik, William Renner, Richard James, Ferris Jennings, Harry Pillinger, Harry Lutomski, George Bolas, Charles Brandman, Gerald Ford

Explorations and field-work of the Smithsonian Institution ...

Mode of access: Internet.

Urinary albumin levels in the normal range determine arterial wall thickness in adults with Type 2 diabetes: a FIELD substudy

Aim Cardiovascular disease (CVD) rates are substantially higher among patients with Type 2 diabetes than in the general population. The objective of this study was to identify the determinants of carotid intima media thickness (IMT) in patients with Type 2 diabetes. Methods We measured the thickness of the intima media layer of the carotid artery, a strong predictor of the risk of future vascular events, in 397 Type 2 diabetic patients drawn from the Fenofibrate Intervention and Event Lowering in Diabetes study, prior to treatment allocation. Results The mean IMT was 0.78 mm [interquartile range (IQR) 0.23 mm], and the maximum IMT was 1.17 mm (IQR 0.36 mm). By multivariate analysis, age, sex, duration of diabetes, triglycerides, and total cholesterol were independently correlated with IMT, as was urine albumin-creatinine ratio (ACR) (P < 0.001). The effect of ACR on IMT was further examined by tertile. Clinically significant differences in IMT were associated with ACR > 0.65 mg/mmol, approximately one-fifth the standard clinical threshold for microalbuminuria (P < 0.01). Long-term diabetes, independent of other parameters, was associated with a 50% increase in age-related thickening. Conclusions IMT in people with Type 2 diabetes is independently and continuously related to urine albumin levels and to the duration of diabetes. These results support previous data linking urine albumin measurements within the normal range with increased ischaemic cardiac mortality in the setting of Type 2 diabetes, and strongly suggest that urine albumin levels within this range should trigger a formal evaluation for CVD.

Analysis of plant microfossils in archaeological deposits from two remote archipelagos: The Marshall Islands, Eastern Micronesia, and the Pitcairn Group, Southeast Polynesia

Pollen and starch residue analyses were conducted on 24 sediment samples from archaeological sites on Maloelap and Ebon Atolls in the Marshall Islands, eastern Micronesia, and Henderson and Pitcairn Islands in the Pitcairn Group, Southeast Polynesia. The sampled islands, two of which are mystery islands (Henderson and Pitcairn), previously occupied and abandoned before European contact, comprise three types of Pacific islands: low coral atolls, raised atolls, and volcanic islands. Pollen, starch grains, calcium oxylate crystals, and xylem cells of introduced non-Colocasia Araceae (aroids) were identified in the Marshalls and Henderson (ca. 1,900 yr B.P. and 1,200 yr B.P. at the earliest, respectively). The data provide direct evidence of prehistoric horticulture in those islands and initial fossil pollen sequences from Pitcairn Island. Combined with previous studies, the data also indicate a horticultural system on Henderson comprising both field and tree crops, with seven different cultigens, including at least two species of the Araceae. Starch grains and xylem cells of Ipomoea sp., possibly introduced 1. batatas, were identified in Pitcairn Island deposits dated to the last few centuries before European contact in 1790.

Data compilation of dinoflagellates growth rate, grazing rate and gross gowth efficiency from field and labratory experiments

The present data compilation includes dinoflagellates growth rate, grazing rate and gross growth efficiency determined either in the field or in laboratory experiments. From the existing literature, we synthesized all data that we could find on dinoflagellates. Some sources might be missing but none were purposefully ignored. We did not include autotrophic dinoflagellates in the database, but mixotrophic organisms may have been included. This is due to the large uncertainty about which taxa are mixotrophic, heterotrophic or symbiont bearing. Field data on microzooplankton grazing are mostly comprised of grazing rate using the dilution technique with a 24h incubation period. Laboratory grazing and growth data are focused on pelagic ciliates and heterotrophic dinoflagellates. The experiment measured grazing or growth as a function of prey concentration or at saturating prey concentration (maximal grazing rate). When considering every single data point available (each measured rate for a defined predator-prey pair and a certain prey concentration) there is a total of 801 data points for the dinoflagellates, counting experiments that measured growth and grazing simultaneously as 1 data point.