BACKGROUND AND OBJECTIVES: Whereas current GFR estimating equations approximate direct GFR measurement at a single time point, formulas that capitalize on changes in easily measured biologic parameters could improve the accuracy and precision of GFR estimation. DESIGN, SETTING, PARTICIPANTS, & MEASUREMENTS: In the Chronic Kidney Disease in Children Cohort (aged 1 to 16 yr), we measured GFR by plasma disappearance of iohexol (iGFR) and biomarkers in the first two annual visits. Models took the form GFR(2) = a[GFR(1)/40](b)[X(2)/X(1)](c), where GFR(2) and GFR(1) represented the current and previous years' iGFR, 40 ml/min per 1.73 m(2) was the cohort mean, and X(2)/X(1) was the change in predictors over time. Using data from 360 participants with a median age of 12.1 yr, we evaluated the predictive performance of a past GFR measurement and 20 other variables using a two-thirds random sample of the data. A one-third sample was reserved for validation. RESULTS: Previous iGFR measurements were strongly predictive of subsequent iGFR and adding change in height/serum creatinine significantly improved the explanatory power to 78%. In the validation set, the correlation between estimated and measured GFR was 0.88, and 48 and 88% of estimated GFRs were within 10 and 30% of observed iGFRs. When the past GFR measurement was not used, addition of change in markers to a cross-sectional model did not improve prediction. CONCLUSIONS: Longitudinal formulas to estimate iGFR capitalize on the high predictive power of previous iGFR measurements and in this study yielded a parsimonious prediction model with the potential for assessing progression in the clinical setting.
BACKGROUND AND OBJECTIVES: Whereas current GFR estimating equations approximate direct GFR measurement at a single time point, formulas that capitalize on changes in easily measured biologic parameters could improve the accuracy and precision of GFR estimation. DESIGN, SETTING, PARTICIPANTS, & MEASUREMENTS: In the Chronic Kidney Disease in Children Cohort (aged 1 to 16 yr), we measured GFR by plasma disappearance of iohexol (iGFR) and biomarkers in the first two annual visits. Models took the form GFR(2) = a[GFR(1)/40](b)[X(2)/X(1)](c), where GFR(2) and GFR(1) represented the current and previous years' iGFR, 40 ml/min per 1.73 m(2) was the cohort mean, and X(2)/X(1) was the change in predictors over time. Using data from 360 participants with a median age of 12.1 yr, we evaluated the predictive performance of a past GFR measurement and 20 other variables using a two-thirds random sample of the data. A one-third sample was reserved for validation. RESULTS: Previous iGFR measurements were strongly predictive of subsequent iGFR and adding change in height/serum creatinine significantly improved the explanatory power to 78%. In the validation set, the correlation between estimated and measured GFR was 0.88, and 48 and 88% of estimated GFRs were within 10 and 30% of observed iGFRs. When the past GFR measurement was not used, addition of change in markers to a cross-sectional model did not improve prediction. CONCLUSIONS: Longitudinal formulas to estimate iGFR capitalize on the high predictive power of previous iGFR measurements and in this study yielded a parsimonious prediction model with the potential for assessing progression in the clinical setting.
Authors: F Gaspari; N Perico; P Ruggenenti; L Mosconi; C S Amuchastegui; E Guerini; E Daina; G Remuzzi Journal: J Am Soc Nephrol Date: 1995-08 Impact factor: 10.121
Authors: George J Schwartz; Alvaro Muñoz; Michael F Schneider; Robert H Mak; Frederick Kaskel; Bradley A Warady; Susan L Furth Journal: J Am Soc Nephrol Date: 2009-01-21 Impact factor: 10.121
Authors: Matthias Wuttke; Craig S Wong; Elke Wühl; Daniel Epting; Li Luo; Anselm Hoppmann; Anke Doyon; Yong Li; Betül Sözeri; Daniela Thurn; Martin Helmstädter; Tobias B Huber; Tom D Blydt-Hansen; Albrecht Kramer-Zucker; Otto Mehls; Anette Melk; Uwe Querfeld; Susan L Furth; Bradley A Warady; Franz Schaefer; Anna Köttgen Journal: Nephrol Dial Transplant Date: 2015-09-28 Impact factor: 5.992