2. 12.710 Intoduction to Marine Geology and Geophysics 11/1 Mid Term Sediments, Processes, and the Sedimentary Record 11/6 (McManus) Deep-sea sediments: composition, distribution 11/8 (McManus) Biological, chemical, and physical abyssal processes 11/13 (McManus)Dating methods and the sedimentary record 11/15 (McManus)Paleo-environmental proxies 11/20(McManus)Deep water chemistry and atmospheric p(CO 2 ) 11/22 Thanksgiving 11/27 (Hoffmann)Paleothermometry 11/29 (Thompson)Pleistocene ice-age cycles 12/4 (McManus)Sedimentary records of abrupt climate change 12/6 Final Exam

3. jökulhlaups Catastrophic flooding associated with sub-glacial volcanic eruptions

4. Past climate changes I Milankovitch and the “Astronomical” or “Orbital” theory of the ice ages. II Successes and potential failures of Milankovitch. III Abrupt climate change. IV External mechanisms of rapid climate change: Non-linear orbital forcing. Variable solar luminosity. Aliased seasonal cycle. V Internal mechanisms of rapid climate change: Binge-purge ice sheet instability. Salt oscillator ocean circulation. Tropical ocean-atmospheric dynamics.

5. Long-term decline into glaciation Oxygen isotopes in benthic foraminifera from deep-sea sediments reveal a cooling trend on Earth over tens of millions of years.

6. MARINE ISOTOPE STAGES (MIS) Warm (odd) Cold (even)  18 O forams

7. Milutin Milankovitch Serbian mathematician who painstakingly calculated the insolation effects of changes in the Earth’s orbital parameters.

8. Eccentricity Variations in the shape of the Earth’s orbit around the sun, from circular to more elliptical, occur over ~100,000 years.

9. Obliquity Variations in the tilt of the Earth’s axis of rotation, driving contrasts in seasonality, occur over ~40,000 years.

10. Precession Variations in the orientation of the Earth’s tilted axis of rotation, moving seasons along the eccentric orbit, occur over ~20,000 years.

11. Orbital variations in received insolation Each orbital influence has its own distinctive pattern of influence through time. They combine to vary sunlight on Earth.

12. Specmap Study of isotope and other paleo-climate records from deep- sea sediments around the world reveals Milankovitch signal. Period (1/frequency) in thousands of years.

13. Devil’s Hole Well dated speleothem record not consistent with Milankovitch? Should it? Remains an unsolved puzzle.

14. Abrupt climate change Evidence from ice cores and deep-sea sediments reveals climate changes that seem too abrupt to be explained orbitally.

16. Dansgaard-Oeschger Cycles discovered in Greenland ice  18 O ice warmcold

17. N. Atlantic SSTs track Greenland Air Temperatures H-events occurred during extreme cold phases of D-O cycles in Greenland ice cooler warmer

18. THE YOUNGER DRYAS IN THE SANTA BARBARA BASIN Increased bioturbation suggesting higher O 2 levels (D-O interstadials show the opposite with reduced bioturbation) Increased  18 O benthic Increased Pacific ventilation?

19. GLOBAL SIGNATURE OF D/O EVENTS: CARIACO BASIN

20. Antarctica warms during the Younger Dryas ANTI-PHASING BETWEEN HEMISPHERES

21. THE DISCOVERY OF HEINRICH EVENTS….

22. …. IN MARINE SEDIMENT ARCHIVES

23. Transport of ice-rafted debris (IRD)

24. “IRD Belt” - based on network of N. Atlantic marine sediment records Site with ice-rafted debris Site without ice-rafted debris

25. MECHANISMS BEHIND MILLENNIAL VARIABILITY EXTERNAL FORCING Suborbital (Combination tones) Solar Variability INTERNAL FORCING Ice sheets (e.g., “Binge-Purge” theory) Thermohaline circulation (e.g., Broecker’s “Salt Oscillator”) Tropical Dynamics (e.g., Eastern tropical Pacific - ENSO dynamics) ALTERNATIVE Aliasing

26. SUBORBITAL FORCING: MILANKOVITCH COMBINATION TONES Tropical Atlantic coccolith abundance records: Variations in tropical winds/upwelling cause ice rafting events? McIntyre and Molfino (1996) F. profunda (upwelling indicator) maxima coeval with Heinrich events Spectral Analysis: -spectral power at 8.4 ky (7.6 ky 14 C), a combination tone of precession and eccentricity The mechanism: Easterly winds diminish, warm water propagates northward via the Gulf Stream, delivery of heat causes ice sheet melting and subsequent iceberg discharge

27. SOLAR VARIABILITY: IRD and Cosmogenic Nuclides in the Holocene 10 Be 14 C Bond et al. (2001) Similar pacing of ice rafting events during last interglacial (MIS-5)

28. ICE SHEET STABILITY: THE BINGE-PURGE THEORY MacAyeal’s explanation for Heinrich Events ~7 ky pacing Laurentide Ice Sheet (LIS) Model: Binge (Growth) phase - basal sediment frozen, ice sheet immobile; slow growth of LIS Purge phase - geothermal flux gradually increases basal temperature, thawing basal sediments; rapid discharge of icebergs; (meltwater input reduces THC, cool North Atlantic, allowing ice growth again) BINGE PURGE BINGE

29. THERMOHALINE CIRCULATION: THE SALT OSCILLATOR Conveyor On: Northward heat transport initiates ice melting, which reduces density of upper ocean, reducing deep water formation Conveyor Off: Cooling of North Atlantic (less melt water input) and reduced salt export gradually increase density (and thus deep water formation); return to Conveyor On mode

30. Three Modes of North Atlantic Deep Ocean Circulation Oc/Atm Atm

31. TROPICAL DYNAMICS: EASTERN TROPICAL PACIFIC The Idea: El Ni ñ o/Southern Oscillation (ENSO) system in the eastern tropical Pacific affects tropical SST distribution, which controls convection/atmospheric circulation patterns - very strong teleconnections, which could explain near-global synchroneity of millennial events Experiment: Coupled ocean- atmosphere model of the tropical Pacific is run for 150,000 years, both with and without orbital (precession) forcing Result: Millennial increases or decreases in the frequency of ENSO warm or cold events and changes in their amplitudes EVENT AMPLITUDE EVENT FREQUENCY Clement et al. (1999)

32. THE PROBLEM OF ALIASING

34. D-O events show up in major ion chemistry of Greenland ice Record developed from the analysis of GISP2 major ion chemistry Proxy for relative measure of the average size and intensity of polar atmospheric circulation Generally increase (e.g., more continental dusts and marine contributions) during stadials and decrease during interstadials Polar Circulation Index (PCI)

35. SPECTRAL ANALYSIS OF THE PCI Dominant periodicity in millennial band is 1450 years

36. GLOBAL SIGNATURE OF D/O EVENTS: ARABIAN SEA Total organic carbon (TOC) records from two marine sediment cores off Pakistan showing millennial- scale variability of monsoonal surface water productivity and bottom-water oxygen laminated bioturbated Increased prod., lower O 2 Greenland  18 O ice

37. D/O temperature oscillations also occur in Antarctica (Vostok), but with generally smaller amplitudes

38. HEINRICH EVENTS Helmut Heinrich discovered a cyclic pattern of ice-rafted debris over the last 130 ky in a series of sediment records from the North Atlantic Broecker and Bond later identified six of these events between 70 and 14 ky B.P., and named them Heinrich events (H1-H6) Heinrich events occur every ~7-10 ky, and are associated with pronounced cooling in the Greenland ice core records and North Atlantic region Bond et al. (1993) noted that Heinrich events appear to occur towards the end of increasingly colder D-O cycles

39. SEDIMENTARY CHARACTERISTICS OF A HEINRICH LAYER

40. OTHER TYPES OF IRD FOUND IN THE NORTH ATLANTIC Basaltic glass, Iceland Hematite-stained grains

41. HEINRICH EVENT CHRONOLOGY IRD peaks Bond et al. (1992)

42. Bond and Lotti (1995) COLDER BOND IDENTIFIES MORE IRD PEAKS IN N. ATLANTIC SEDIMENTS In addition to Heinrich events (Huge IRD peaks, cold Greenland air temp. and cold N. Atl. SST)… Cold phases of D-O cycles - smaller amplitude IRD peaks; smaller SST signal