Figure F2. Seismic reflection profile through Site 1222. The sedimentary section is marked by a weakly reflective unit between the seafloor and ~62 ms two-way traveltime (TWT) below the seafloor, assumed to be clays. The next two prominent reflectors (~120 and 147 ms TWT mbsf) are interpreted to mark chert layers at the contact between middle and lower Eocene sediments and basement, respectively (see Lyle et al., this volume).

Figure F2. Seismic reflection profile through Site 1222. The sedimentary section is marked by a weakly reflective unit between the seafloor and ~62 ms two-way traveltime (TWT) below the seafloor, assumed to be clays. The next two prominent reflectors (~120 and 147 ms TWT mbsf) are interpreted to mark chert layers at the contact between middle and lower Eocene sediments and basement, respectively (see Lyle et al., this volume).