Stable carbon isotope composition of benthic foraminifera from sediments of the Skagerrak, North Sea, supplement to: Brückner, Sylvia; Mackensen, Andreas (2008): Organic matter rain rates, oxygen availability, and vital effects from benthic foraminiferal d13C in the historic Skagerrak, North Sea. Marine Micropaleontology, 66(3-4), 192-207

Sylvia Brückner & Andreas Mackensen
The sediment cores 225514 and 225510 were recovered from 420 and 285 m water depth, respectively. They were investigated for their benthic foraminiferal delta13C during the last 500 years. Both cores were recovered from the southern flank of the Skagerrak. The delta13C values of Uvigerina mediterranea and other shallow infaunal species in both cores indicate that organic matter rain rates to the seafloor varied around a mean value until approximately AD 1950 after which they...
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