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| 1 | Corporate Social Responsibility: Strategic Implications*显示文摘 | AbagailMcWilliams Donald S.Siegel Patrick M.Wright | 2006 | Journal of Management Studies2006，，1： | 2 |
| 2 | Goodness‐of‐fit statistics for age‐specific reference intervals显示文摘 | P.Royston E. M.Wright | 2000 | Statist. Med2000，，21： | 1 |
| 3 | MEASUREMENT ERROR IN RESEARCH ON HUMAN RESOURCES and FIRM PERFORMANCE: HOW MUCH ERROR IS THERE AND HOW DOES IT INFLUENCE EFFECT SIZE ESTIMATES?显示文摘 | BARRYGERHART PATRICK M.WRIGHT GARY C.MAHAN SCOTT A.SNELL | 2006 | Personnel Psychology2006，，4： | 1 |
| 4 | Corporate Social Responsibility: Strategic Implications*显示文摘 | AbagailMcWilliams Donald S.Siegel Patrick M.Wright | 2006 | Journal of Management Studies2006，，1： | 1 |
| 5 | Stature of young people with malignant bone tumors显示文摘 | Simon J.Cotterill Charlotte M.Wright Mark S.Pearce Alan W.Craft | 2003 | Pediatr Blood Cancer2003，，1： | 1 |
| 6 | Estimating profitability of two biochar production scenarios: slow pyrolysis vs fast pyrolysis显示文摘 | Tristan R.Brown Mark M.Wright Robert C.Brown | 2011 | Biofuels, Bioprod. Bioref2011，，： | 1 |
| 7 | Corporate Social Responsibility: Strategic Implications*显示文摘 | AbagailMcWilliams Donald S.Siegel Patrick M.Wright | 2006 | Journal of Management Studies2006，，1： | 1 |
| 8 | ADAM28: A potential oncogene involved in asbestos‐related lung adenocarcinomas显示文摘 | Casey M.Wright Jill E.Larsen Nicholas K.Hayward Maria U.Martins Maxine E.Tan Morgan R.Davidson Santiyagu M.Savarimuthu Rebecca E.McLachlan Linda H.Passmore Morgan N.Windsor Belinda E.Clarke Edwina E.Duhig Ian A.Yang Rayleen V.Bowman Kwun M.Fong | 2010 | Genes Chromosom Cancer2010，，8： | 1 |
| 9 | Stature of young people with malignant bone tumors显示文摘 | Simon J.Cotterill Charlotte M.Wright Mark S.Pearce Alan W.Craft | 2003 | Pediatr. Blood Cancer2003，，1： | 1 |
| 10 | From Human Capital to Social Capital:A Longitudinal Study of Technology-based Academic Entrepreneurs显示文摘 | S.Mosey M.Wright | | 0，，06： | 1 |
| 11 | Estimating profitability of two biochar production scenarios: slow pyrolysis vs fast pyrolysis显示文摘 | Tristan R.Brown Mark M.Wright Robert C.Brown | 2011 | Biofuels Bioprod Bioref2011，，1： | 1 |
| 12 | What do teachers see?Perceptions of school-time physical activity programs on student behavior显示文摘In the United States, children are not meeting daily recommendationsfor 60 min of moderate・to・vigorous activity.1Because children spend a large portion of their days in school, ithas been further recommended that children accumulate 30 minof their physical activity (PA) during school hours.2 Our previousresearch has demonstrated with objective measures that only8%—9% of elementary school children meet this goal, with anaverage accumulation of 18 min/day.3,4 This finding is of concerngiven the numerous benefits that PA has not only on healthoutcomes,5-8 but also on academic achievement.9 For example,there is heightened awareness that children benefit from PAthroughout the school day in terms of attention to task, memory,behavior, and, ultimately, academic performance.10 Schooladministrators acknowledge this link, but still face barriers toincorporating PA for schoolchildren, including limited time andresources for physical education (PE) and recess. | Jennifer M.Sacheck Catherine M.Wright | 2020 | Journal of Sport and Health Science2020，9，1： | 0 |
| 13 | Spatial variability in carbon dioxide exchange processes within wet sedge meadows in the Canadian High Arctic显示文摘Wet sedge meadows are the most productive plant communities in the High Arctic.However,the controls on carbon dioxide(CO_(2))exchange processes within wet sedge communities-and the scale at which they operate-are poorly understood.Here,the factors controlling CO_(2)exchange of wet sedge meadows experiencing different moisture regimes are examined.Environmental data are used to create predictive models of CO_(2)exchange on multiple temporal scales.Automated chamber systems recorded CO_(2)fluxes at 30-minute intervals at wet sedge sites in the Canadian High Arctic from June to August in 2014 and 2015.Static chambers were also deployed over a larger spatial extent in 2014.Our results show that wet sedge communities were strong CO_(2)sinks during the growing season(−7.67 to−44.36 g C·m^(−2)).CO_(2)exchange rates in wetter and drier areas within wet sedge meadows differed significantly(Wilcoxon,p<0.001),suggesting that soil moisture regimes within vegetation types influence net CO_(2)balance.Random Forest models explained a significant amount of the variability in CO_(2)flux rates over time(R2=0.46 to 0.90).The models showed that the drivers of CO_(2)exchange in these communities vary temporally.Variable moisture regimes indirectly influenced CO_(2)fluxes given that they exhibit different vegetation and temperature-response characteristics.We suggest that the response of a single vegetation type to environmental changes may vary depending on microenvironment variability within that community. | Claire M.WRIGHT Amy C.BLASER Paul M.TREITZ Neal A.SCOTT | 2021 | Advances in Polar Science2021，32，1： | 0 |
| 14 | Reconstructing seafloor age distributions in lost ocean basins显示文摘Reconstructions of past seafloor age make it possible to quantify how plate tectonic forces,surface heat flow,ocean basin volume and global sea level have varied through geological time.However,past ocean basins that have now been subducted cannot be uniquely reconstructed,and a significant challenge is how to explore a wide range of possible reconstructions.Here,we investigate possible distributions of seafloor ages from the late Paleozoic to present using published full-plate reconstructions and a new,efficient seafloor age reconstruction workflow,all developed using the open-source software GPlates.We test alternative reconstruction models and examine the influence of assumed spreading rates within the Panthalassa Ocean on the reconstructed history of mean seafloor age,oceanic heat flow,and the contribution of ocean basin volume to global sea level.The reconstructions suggest variations in mean seafloor age of~15 Myr during the late Paleozoic,similar to the amplitude of variations previously proposed for the Cretaceous to present.Our reconstructed oceanic age-area distributions are broadly compatible with a scenario in which the long-period fluctuations in global sea level since the late Paleozoic are largely driven by changes in mean seafloor age.Previous suggestions of a constant rate of seafloor production through time can be modelled using our workflow,but require that oceanic plates in the Paleozoic move slower than continents based on current reconstructions of continental motion,which is difficult to reconcile with geodynamic studies. | Simon Williams Nicky M.Wright John Cannon Nicolas Flament R.Dietmar Müller | 2021 | Geoscience Frontiers2021，12，2： | 0 |
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