--> CHRONOS Cyclostratigraphy Tools: Astronomical Calibration of Geologic Time at 0.02 to 0.40 Myr Resolution, by Linda A. Hinnov; #90052 (2006)
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CHRONOS Cyclostratigraphy Tools: Astronomical Calibration of Geologic Previous HitTimeNext Hit at 0.02 to 0.40 Myr Resolution

Linda A. Hinnov
Johns Hopkins University, Baltimore, MD

A fundamental product of the virtual CHRONOS system is access to data and techniques used to calibrate geologic Previous HittimeNext Hit. An important innovation in the Geologic Previous HitTimeNext Hit Scale 2004 was the use of astronomically forced stratigraphy, or cyclostratigraphy, to define geologic Previous HittimeNext Hit over 0-23.08 Ma at an unprecedented resolution of 0.02 myr. In addition, 'floating' astronomical Previous HittimeNext Hit scales were proposed for entire epochs and stages in the Paleogene and all three Mesozoic periods. Some of these calibrations used a new astrodynamical model with an accurate ephemeris for Earth's orbital parameters to 250 Ma. Accordingly, CHRONOS plans to host the tools and models that are used for the astronomical calibration of cyclostratigraphy. This involves the development of a Previous HittimeNext Hit series analysis toolkit customized for cyclostratigraphic applications, but appropriate for analysis of any sampled, sequenced data. Online, interactive modules will perform interpolation, tuning (correlation), multivariate spectral analysis, filtering, demodulation, and insolation modeling. The toolkit will enable CHRONOS to coordinate community projects working toward a continuous, astronomically calibrated Previous HittimeNext Hit scale for the entire Cenozoic-Mesozoic, to host a "global composite cyclostratigraphic standard," and to promote prospecting for astronomical signals in Paleozoic cyclostratigraphy. Astronomically calibrated geologic Previous HittimeTop with a 0.02 to 0.40 myr resolution represents a major breakthrough in geosciences. Estimates of rates and magnitudes for a wide range of Earth system processes that can be examined only in the context of Earth history, e.g., paleoclimatology, geodynamics, geochronology, geochemical cycles and biotic evolution, will be improved by an order of magnitude over what is possible today.