Figure F4. Seismic reflection image (seismic line AGSO-169/05a) of the eastern drilling transect, showing the thick Pleistocene clinoform wedge underlying the modern outermost shelf and upper slope and the location of Sites 1127, 1129, and 1131. Bryozoan mounds are visible as individual mounds and as stacked mound complexes immediately below the seafloor seaward of the shelf edge and also buried within the sediment wedge. Dashed box shows area enlarged in Figure F7.

Figure F4. Seismic reflection image (seismic line AGSO-169/05a) of the eastern drilling transect, showing the thick Pleistocene clinoform wedge underlying the modern outermost shelf and upper slope and the location of Sites 1127, 1129, and 1131. Bryozoan mounds are visible as individual mounds and as stacked mound complexes immediately below the seafloor seaward of the shelf edge and also buried within the sediment wedge. Dashed box shows area enlarged in Figure F7.