Deep Western Boundary Current variability in the subtropical northwest Atlantic Ocean during marine isotope stages 12-10
β Scribed by Hall, Ian R.; Becker, Julia
- Book ID
- 119669054
- Publisher
- American Geophysical Union
- Year
- 2007
- Tongue
- English
- Weight
- 913 KB
- Volume
- 8
- Category
- Article
- ISSN
- 1525-2027
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ODP sites 1055^1062 recover a bathymetric transect from 1800 to 4800 water depth in the subtropical NW-Atlantic (Carolina Slope, Blake^Bahama Outer Ridge). This sediment drift region is known for high deposition rates ( s 40 cm/kyr) and offers the excellent opportunity to investigate the history of
The interval of time represented by marine isotope stages 11 and 12 (V360^470 ka) contains what may be the most extreme glacial and interglacial climate conditions of the Late Pleistocene. It has been suggested that sea level rose by V160 m at the termination of glacial stage 12. This is 30% greater