Dansgaard-Oeschger cycles and the California Current System: Planktonic foraminiferal response to rapid climate change in Santa Barbara Basin, Ocean Drilling Program hole 893A

Paleoceanography

Volumn 15, Issue 1, 2000, Pages 30-42

  Hendy, Ingrid L ^a   Kennett, James P ^a  

^a UNIVERSITY OF CALIFORNIA   (United States)

Author keywords

[No Author keywords available]

Indexed keywords

EID: 0002830646     PISSN: 08838305     EISSN: None     Source Type: Journal    
DOI: 10.1029/1999PA000413     Document Type: Article

References (17)

1. Andreasen, D. J., and A. C. Ravelo, Tropical Pacific Ocean thermocline depth reconstruction for the Last Glacial Maximum, Paleoceanography, 12, 395-413, 1997.
2. 14C ages obtained by mass spectiometry on corals. Radiocarbon, 35, 191-199, 1993.
3. Behl, R. J., Sedimentary facies and sedimentology of the Late Quaternary Santa Barbara Basin (Site 893), Proc. Ocean Drill. Program Sci. Results, 146 (2), 295-308, 1995.
4. Behl, R. J., and J. P. Kennett, Evidence for brief interstadial events in the Santa Barbara Basin, NE Pacific during the past 60Kyr, Nature, 379, 243-246, 1996.
5. Bender, M., T. Sowers, M. Dickson, J. Orchardo, P. Grootes, P. Mayewski, and D., Meese, Climate correlations between Greenland and Antarctica during the past 100,000 years, Nature, 372, 663-666, 1994.
6. 2 upset the current balance, Science, 278, 1582-1588, 1997.
7. Cannariato, K. G., and J. P. Kennett, Climatically related millennial-scale fluctuations in California Margin oxygen-minimum zone strength during the past 60 k.y., Geology, 27, 975-978, 1999.
8. Cannariato, K. G., J. P. Kennett, and R. J. Behl, Biotic response to late Quaternary climate flickers in the Santa Barbara Basin: Ecological and evolutionary implications. Geology, 24, 63-66, 1999.
9. Chappell, J., and N. J. Shackleton, Oxygen isotopes and sea level, Nature. 324, 137-140, 1986.
10. 4 and Greenland climate between 40 and 8 kyr BP, Nature, 366, 443-445, 1993.
11. Cooperative Holocene Mapping Project Members, Climatic changes of the last 18,000 years: Observations and model simulations. Science, 241, 1043-1052, 1988.
12. Coulbourn, W. T., F. L. Parker, and W. H. Berger, Faunal and solution patterns of planktonic foraminifera in surface sediments of the North Pacific, Mar. Micropaleontol, 5, 329-399, 1980.
13. Craig, H., Measurement of oxygen isotope paleotemperatures, in Stable Isotopes in Oceanographic Studies and Paleotemperatures, edited by E. Tongiorgi, pp. 161-182, Cons.Naz. Delle Rie., Spoleto, Italy, 1965.
14. Dansgaard, W., et al.. Evidence for general instability of the past climate from a 250-kyr ice-core record, Nature, 364, 218-220, 1993.
15. Darling, K. F., C. W. Wade, D. Kroon, A. J. Leigh Brown, and J. Bijma, The diversity and distribution of modern planktic foraminiferal small subunit ribosomal RNA genotypes and their potential as tracers of present and past ocean circulation, Paleoceanography, 14, 3-12, 1999.
16. Davis, J. C., Statistics and Data Analysis in Geology, John Wiley, New York, 1973.
17. de Vernal, A., and T. F. Pedersen, Micropaleontology and palynology of core PAR87A-10: A 23,000 year record of paleoenvironmental changes in the Gulf of Alaska, northeast North Pacific, Paleoceanography, 12, 821-830, 1997.