Geochemical consequences of increased Late Cenozoic weathering rates and the global CO₂ balance since 100 Ma

This publication has 69 references indexed in Scilit:

• Significance of weathering Himalayan metasedimentary rocks and leucogranites for the Sr isotope evolution of seawater during the early Miocene
  Geology, 1995
• Surface fluid convection during Cordilleran extension and the generation of metamorphic CO2 contributions to Cenozoic atmospheres
  Geology, 1995
• Enhanced Cenozoic chemical weathering and the subduction of pelagic carbonate
  Nature, 1992
• Variation in the strontium isotopic composition of seawater (8 Ma to present) : Implications for chemical weathering rates and dissolved fluxes to the oceans
  Chemical Geology: Isotope Geoscience section, 1990
• Phosphogenesis and weathering of shelf sediments from the southeastern United States: Implications for Miocene δ13C excursions and global cooling
  Geology, 1990
• Sensitivity of climate and atmospheric CO2 to deep-ocean and shallow-ocean carbonate burial
  Nature, 1989
• Surface area control of shallow cratonic to deep marine carbonate accumulation
  Paleoceanography and Paleoclimatology, 1988
• Tertiary paleoceanic chemical variability: Unintended consequences of simple geochemical models
  Paleoceanography and Paleoclimatology, 1988
• Pacific pelagic phosphorus accumulation during the last 10 M.Y.
  Paleoceanography and Paleoclimatology, 1988
• Tertiary oxygen isotope synthesis, sea level history, and continental margin erosion
  Paleoceanography and Paleoclimatology, 1987