In order to keep the contained benthos alive, multicores must be moved into a cold van as soon as possible after the corer is secured on deck. For this project, we use the FLEC method (developed by Bernhard and colleagues, see Limnology & Oceanography 2003) to determine, on the micron scale, where deep-sea benthic foraminifera are living with respect to the sediment-water interface. This provides information to better interpret the stable isotopic and trace metal signatures recorded in their shells. This work is funded by NSF Ocean Sciences Marine Geology & Geophysics, and is in collaboration with Dan McCorkle (WHOI), Tom Chandler (University of South Carolina) and Tim Shaw (University of South Carolina). (K. Hintz)