Osmium, and stable carbon and oxygen isotope record accross the PETM, supplement to: Ravizza, Gregory E; Norris, R N; Blusztajn, Jerzy S; Aubry, Marie-Pierre (2001): An osmium isotope excursion associated with the Late Paleocene thermal maximum: Evidence of intensified chemical weathering. Paleoceanography, 16(2), 155-163

Gregory E Ravizza, R N Norris, Jerzy S Blusztajn & Marie-Pierre Aubry
In the latest Paleocene an abrupt shift to more negative d13C values has been documented at numerous marine and terrestrial sites (Bralower et al., 1997, doi:10.1130/0091-7613(1997)025<0963:HRROTL>2.3.CO;2; Cramer et al., 1999; Kaiho et al., 1996, doi:10.1029/96PA01021; Kennett and Stott, 1991, doi:10.1038/353225a0; Koch et al., 1992, doi:10.1038/358319a0; Stott et al., 1996; Thomas and Shackleton, 1996, doi:10.1144/GSL.SP.1996.101.01.20; Zachos et al., 1993). This carbon isotope event (CIE) is coincident with oxygen isotope data that indicate warming of surface waters...
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