Hendy, I. L. and Pedersen, T. F. (2005): Is pore water oxygen content decoupled from productivity on the California margin? Trace element results from Ocean Drilling Program Hole 1017E, San Lucia Slope, California

Leg/Site/Hole:
ODP 167
ODP 167 1017
Identifier:
2007-021987
georefid

10.1029/2004PA001123
doi

Creator:
Hendy, I. L.
University of Michigan, Department of Geological Sciences, Ann Arbor, MI, United States
author

Pedersen, T. F.
University of Victoria, Canada
author

Identification:
Is pore water oxygen content decoupled from productivity on the California margin? Trace element results from Ocean Drilling Program Hole 1017E, San Lucia Slope, California
2005
Paleoceanography
American Geophysical Union, Washington, DC, United States
20
4
PA4026
English
Coverage:Geographic coordinates:
North:34.3205
West:-121.0625East: -121.0625
South:34.3205

Quaternary geology; Geochemistry of rocks, soils, and sediments; Cenozoic; East Pacific; Eh; geochemistry; Holocene; Leg 167; marine environment; marine sediments; North Pacific; Northeast Pacific; Ocean Drilling Program; ODP Site 1017; oxygen; Pacific Ocean; paleoecology; paleoenvironment; Pleistocene; pore water; productivity; Quaternary; San Lucia Slope; sediments; slope environment; trace elements; upper Pleistocene;

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