Hobson, Louis A. et al. (2001): The Saanich Inlet basin; a natural collector of past biological, climatic, and land-use changes in southwestern Canada amplified by results of ODP Leg 169S

Leg/Site/Hole:
ODP 169S
Identifier:
2002-076712
georefid

Creator:
Hobson, Louis A.
Institute of Ocean Sciences, Ocean Sciences and Productivity, Sidney, BC, Canada
author

McQuoid, Melissa R.
Husky Oil Operations, Canada
author

Tunnicliffe, Verena
Goteborg University, Sweden
author

Identification:
The Saanich Inlet basin; a natural collector of past biological, climatic, and land-use changes in southwestern Canada amplified by results of ODP Leg 169S
2001
In: Srivastava, Shiri (convener), Salisbury, Matthew (convener), Enachescu, Michael (convener), Ocean drilling; successes, opportunities and challenges
Geological Association of Canada, Toronto, ON, Canada
28
4
197-202
Saanich Inlet sediments contain one of the best-preserved biological records in the world. Frozen 1-2 m cores representing the last approximately 130 years show a deforestation-related increased input of terrestrial carbon to the basin, and cyclic variations in organic carbon, diatoms, and fish remains that suggest a link to climate oscillations. Ocean Drilling Program cores from Leg 169S greatly extend the sediment record, to more than 10,000 years. Study of diatoms, carbon isotope ratios, and fish remains from these along ODP cores shows that the marine environment has been stable during the Holocene. The long ODP cores also indicate that, beginning approximately 10,000 years B.P., Saanich Inlet basin rapidly assumed the broad-scale oceano-graphic and biologic features seen today.
English
Coverage:Geographic coordinates:
North:48.3000
West:-123.1500East: -123.1500
South:48.3000

Quaternary geology; algae; biostratigraphy; British Columbia; Canada; carbon; Cenozoic; climate change; cores; diatoms; framework silicates; Holocene; human activity; land use; Leg 169S; marine sediments; microfossils; Ocean Drilling Program; opal; organic carbon; paleoclimatology; Plantae; Quaternary; Saanich Inlet; salinity; sediments; silica minerals; silicates; temperature; variations; Western Canada;

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