Co-Chiefs: Itaru Koizumi and Mitchell Lyle | Staff Scientist: Carl Richter |
Cruise Dates: 21 April-16 June 1996 | Operations Superintendent: Scott McGrath |
Leg 167 will investigate the evolution of
oceanogaphic conditions in the northern Pacific
Ocean and will document changes in the flow of the
California Current system and associated changes in
coastal upwelling. These data will be used to
reconstruct northern Pacific climate conditions
through the Neogene, concentrating upon the time
period since the advent of Northern Hemisphere
glaciation (~2.5 Ma to the present). Approximately
one-third of the proposed drill sites will also sample
lower and middle Miocene sediments to reconstruct a
Neogene history of the California Current. The results
of Leg 167 drilling will also be used to better
understand the links between the climates of the
northern Pacific Ocean and western North America,
particularly in terms of temperature change and
changes in precipitation.
Thirteen proposed sites and five alternates are organized into three transects across the California Current (Baja Transect, ~30° N; Conception Transect, ~35° N; and Gorda Transect, ~40° N) and one coastal transect extending from northern Baja California to the California/Oregon border (30° to 42° N). Each of the three transects across the California Current will compare deep-water sites near the core of the California Current to coastal upwelling sites near shore. The coastal transect will examine variations in upwelling and productivity along the California margin as well as intermediate-water properties in many of the basins of the California Continental Borderland.
Tectonic objectives, although of secondary importance, are also necessary for paleoceanographic reconstruction because many of the sites have moved hundreds of kilometers in relation to North America during the Neogene. The continental basement underneath Site CA-2, for example, is now located just south of the Mendocino Triple Junction, but it may have been separated at one time from the rest of North America as far south as northern Baja California.
Although the highest priority on Leg 167 will be given to the sampling of upper Neogene sediments (Pliocene and younger), five of the proposed drill sites will sample middle and lower Miocene sediments. The older sedimentary sections will be instrumental to understanding the Neogene paleoceanographic evolution of the northern Pacific climate.
A decision was reached during the PPSP meeting that SEDCO/BP 471 will not drill the Santa Barbara Basin site during Leg 167 for safety reasons.
Low transit times coupled with relatively shallow-water drilling combine to ensure that this will be a record core recovery leg. An estimated 7.2 km of core will be recovered, easily surpassing the previous record of 6730.74 m on Leg 162. As a result, during Leg 167 the ship will pull into San Diego to offload cores after the third site drilled. While in San Diego, the Mexican observer will depart the ship, and Paula Weiss will board for the remainder of the leg. It is expected that the JOIDES Resolution will clear U.S. Customs and Immigrations in San Diego harbor and will not need to clear in San Francisco.
The San Francisco port call is expected to be extremely busy with public relations activities. The cryogenic magnetometer will be replaced, microscope maintenance/training will be conducted, and possible XRF maintenance will take place during this port call.