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- W2735009747 abstract "During the Virgilian Stage of the Pennsylvanian Period, approximately 300 million years ago, the area that is now Kansas was located 5-7 degrees north of the equator. The climate was expected to be generally warm, moist, and tropical (Heckel, 1979, 1995; Joeckel, 1994). After completing a summer of measuring sections in southeastern Kansas and northeastern Oklahoma, we identified ancient soils associated with seasonal precipitation and arid conditions (Mack, 1993, 1994; Retallack, 2001). The initial field interpretations do not warrant the classification of wet equatorial soils like the Appalachian coal measures. A closer study of the soil profiles was required to find if the variation was due to local controls or if the accepted paleoreconstruction was incorrect." @default.
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- W2735009747 date "2005-04-22" @default.
- W2735009747 modified "2023-09-26" @default.
- W2735009747 title "300-million-year-old soils and their implications on predicting ancient climate conditions" @default.
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