Science, Volume 298, Issues 5600-5602M. King, 2002 |
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Page 1979
... surface regolith would be recharged by very slow diffusion of water vapor into the subsoil ( 20 ) , where it could be released again by the next large impact . When the impacts ceased , the erosion also ceased , and today we observe a ...
... surface regolith would be recharged by very slow diffusion of water vapor into the subsoil ( 20 ) , where it could be released again by the next large impact . When the impacts ceased , the erosion also ceased , and today we observe a ...
Page 1981
... surface wa- ers and biogenic opal rain rates than previ- usly thought . During travel from the surface waters to le sediments , trophic food webs exert differ- ntial control over Si and C preservation , esulting in material that is ...
... surface wa- ers and biogenic opal rain rates than previ- usly thought . During travel from the surface waters to le sediments , trophic food webs exert differ- ntial control over Si and C preservation , esulting in material that is ...
Page 2344
... surface ocean CO2 concentrations near Bermuda . The record is derived from measurements of dissolved inorganic ... surface ocean and sea surface temperature ( 8 ) predict the in- terannual variability of oceanic CO2 up- take to be three ...
... surface ocean CO2 concentrations near Bermuda . The record is derived from measurements of dissolved inorganic ... surface ocean and sea surface temperature ( 8 ) predict the in- terannual variability of oceanic CO2 up- take to be three ...
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