Comment on "Determining Chondritic Impactor Size from the Marine Osmium Isotope Record"
Joanna V. Morgan
Paquay
et al. (Reports, 11 April 2008, p. 214) reported that
osmium isotope ratios in marine sediments can be used to determine
the size of a chondritic impactor. Their assumptions on the
fate of an impacting projectile may need to be reassessed, however,
because only a small, unpredictable fraction of the impactor
ends up dissolved in seawater.
Earth Science and Engineering, Imperial College London, South Kensington Campus, London SW7 2AZ, UK. E-mail: j.morgan{at}imperial.ac.uk