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Stratigraphy of climate change

Stratigraphy of climate change. Lecture 19. The predominant power in this spectrum is at about 100,000, 41,000 and 19-23,000 years. from Alley, 2000. The Milankovitch hypothesis: climate change results from changes in Earth’s orbital parameters. Barbados.

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Stratigraphy of climate change

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  1. Stratigraphy of climate change Lecture 19

  2. The predominant power in this spectrum is at about 100,000, 41,000 and 19-23,000 years

  3. from Alley, 2000 The Milankovitch hypothesis: climate change results from changes in Earth’s orbital parameters

  4. Barbados

  5. Today we’ll look at examples of climate changes seen in the stratigraphic record that are NOT controlled by orbital parameters

  6. Orbital Forcing – Ice Cores • Ice core 18O records temperature • Orbital frequencies are clearly dominant, but higher frequencies are present

  7. Heinrich Events • Discovered in 1988 in marine sediment cores • Recognized as distinct layers with significant increase in lithic fragments, and large clasts in some areas

  8. Heinrich Layer Isopachs • Double maxima in isopachs • Layers thicken to NW into Labrador Sea

  9. Source of Heinrich events • Black areas are regions with large carbonate deposits • Sediment must have been ice-rafted

  10. Heinrich Layer 4 (~40,000 years BP) 18O in polar planktonic foraminifera Modeling shows about 250-year duration and 2-m rise in sea level Nature, Roche et al., 2004

  11. Modeling shows about 250-year duration and 2-m rise in sea level Nature, Roche et al., 2004

  12. Heinrich Events in context • Occur at times of coldest weather in N. Atlantic • Followed by a sharp warming • No clear periodicity Bond 1993 figure

  13. Summary of Heinrich events • Effects are global – signature of Heinrich events has been found around the world • Massive discharge of ice into N. Atlantic from the Laurentide ice sheet is well established • No clear explanation for such dynamics in the ice sheet

  14. Dansgaard-Oeschger Events • Characterized by rapid warming in the N. Atlantic, followed by slower cooling • Quasi-Periodic, with a timescale of ~1400 years • Recorded by diverse climate proxies • Evidence for global climatic effects (Data From ftp://ftp.ngdc.noaa.gov/paleo/icecore/greenland/summit/grip/isotopes/gripd18o.txt)

  15. Greenland and D-O events • Within the Greenland ice cores, several independent variables all show D-O events prominently • 18O – Temperature • Ca/Dust concentrations – varying weather in Asia? • Na/Cl concentrations – increased storminess in N. Atlantic • Etc…

  16. Other Evidence of D-O events • Sediment cores from the Santa Barbara Basin (Hendy and Kennet, 1999)

  17. Other Evidence of D-O events • Stalagmites from Eastern China (Wang et al., 2001)

  18. Global Map of D-O records http://www2.ocean.washington.edu/oc540/lec01-31/

  19. Theories for rapid climate change • Heinrich, D-O periods are too rapid for orbital frequencies • Some combination of the ocean/atmosphere/cryosphere must be responsible • Need a source with enough power to affect global climate

  20. Deep water formation Atlantic Circulation • Deep Water is formed at the Northern and Southern extents of the Atlantic Ocean • This deep circulation has an overturning timescale of ~103 years • Surface currents strongly influence climate in many areas, as in the N. Atlantic Deep water formation

  21. Stratigraphic Evidence • Recent work (April 2004) has investigated a proxy for Atlantic circulation using a marine sediment core from the Bermuda Rise • Th settles out of water faster than Pa, so the ratio between the two can provide information about the strength of flow away from source • Result – Atlantic circulation essentially shut down during Heinrich events

  22. Summary • There is still no clear trigger for Heinrich or Dansgaard-Oeschger events, nor an explanation for their periods • However, changes in Atlantic circulation seem to account for many of the side effects of both processes • More stratigraphic records = more clues

  23. End of Agriculture??? Why it all matters Beginning of Agriculture • Late Pleistocene was not simply cold – it was totally chaotic • Even modern agricultural processes probably couldn’t overcome such variability

  24. A few references… • Bradley, Raymond S. Paleoclimatology. Harcourt Press, 1999. • Siedov et al., Ed. The Oceans and rapid climate change. AGU, 2001. • Hesse, R. and Khodabakhsh, S. Depositional Facies of Late Pleistocene Heinrich Events I nthe Labrador Sea. Geology 26:2 103-106, 1998. • Dansgaard, W et al. Evidence for general instability of past climate from a 250kyr ice-core record. Nature 364, 15 July 1993. • Bond, G. et al. Evidence for massive discharges of icebergs into the North Atlantic Ocean during the last glacial period. Nature 360, 19 Nov. 1992. • Sarnthein, M. et al. Exploring Late Pleistocene Climate Variations. Eos. 81:51 2000. • Bond, G. et al. Correlations between climate records from North Atlantic sediments and Greenland ice. Nature 365, 9 Sept. 1993. • Bard, E. Climate Shock: Abrupt changes over Millennial time scales. Physics Today Dec. 2002. • Hendy and Kennett. 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, 15:1, 2000. • Phillips, FM. Climatic and hydrologic oscillations in the Owens Lake basin and adjacent Sierra Nevada, California. Science 274:5288, 1996. • Wang, YJ. A High-Resolution Absolute-Dated Late Pleistocene Monsoon Record from Hulu Cave, China. 294:5550, 2001.

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