The 8200-year Climate Event
PAGES IGP 3 Environmental Variability.
This figure shows snow accumulation and isotopically
inferred temperature records in the Greenland GISP2
ice core and a temperature record derived from oxygen
isotope measurements of fossil shells in the sediments
of Lake Ammersee, southern Germany. These records all
show a major climatic instability event which occurred
around 8200 years ago, during the Holocene. The
event was large both in magnitude, as reflected by
a temperature signal in Greenland of order 5 °C, and
in its geographical extent, as indicated by the close
correlation of the signal in these two locations. The
dramatic event is also seen in the methane record from
Greenland (not shown here) indicating possible major
shifts in hydrology and land cover in lower latitudes.
source: Von Grafenstein et al (1998) Climate Dynamics, 14, 73-81.
Abrupt tropical cooling ~8,000 years ago
M.K. Gagan, L.K. Ayliffe*, H. Scott-Gagan, W.S. Hantoro, B.W. Suwargadi, D. Prayudi, M.T. McCulloch
"We drilled a sequence of exceptionally large, well-preserved Porites corals within an uplifted palaeo-reef in Alor, Indonesia, with Th-230 ages spanning the period 8400 to 7600 calendar years before present (Figure 2). The corals lie within the Western Pacific Warm Pool, which at present has the highest mean annual temperature in the world's ocean. Measurements of coral Sr/Ca and oxygen 18 isotopes at 5-year sampling increments for five of the fossil corals (310 annual growth increments) have yielded a semi-continuous record spanning the 8.2 ka event. The measurements (Figure 2) show that sea-surface temperatures were essentially the same as today from 8400 to 8100 years ago, followed by an abrupt ~3°C cooling over a period of ~100 years, reaching a minimum ~8000 years ago. The cooling calculated from coral oxygen 18 isotopes is similar to that derived from Sr/Ca. The exact timing of the termination of the cooling event is not yet known, but a coral dated as 7600 years shows sea-surface temperatures similar to those of today."
Baldini, J.U.L., McDermott, F., Fairchild, I.J. 2002. Structure of the 8200-year cold event revealed by a speleothem trace element record. Science 296: 2203-2206.
"The 8200-year event is widely regarded as the strongest Holocene cooling episode,
with clear expressions in Greenland (1, 2), the North Atlantic (3), Europe (4-11),
North America (12-14), North Africa (15), and the Venezuelan Cariaco Basin (16).
Decreased snow accumulation rates, lower levels of atmospheric methane, and increased
atmospheric dust and sea-salt loadings indicate widespread dry conditions (17, 18).
Explanations usually involve a perturbation of the North Atlantic thermohaline
circulation (THC) by increased freshwater inputs asso- ciated with the decay of the
Laurentide ice sheet (6, 19). A high-resolution global circulation model (GCM)
indicates that a freshwater pulse of a magnitude similar to that associated with the
catastrophic drainage of the large proglacial lakes Agassiz and Ojibway could
have produced the 8200-year event, including a very brief warming episode within the
1. W. Dansgaard, et al., Nature 364, 218 1993.
2. P. M. Grootes, M. Stuiver, J. W. C. White, S. J. Johnsen, J. Jouzel, Nature 366, 552 1993.
3. G. Bond, et al., Science 278, 1257 1997.
4. D. Klitgaard-Kristensen, H. P. Sejrup, H. Haflidason, S. Johnsen, M. Spurk, J. Quat. Sci. 13, 165 1998.
5. D. R. Rousseau, R. Precce, N. Limondin-Lozouet, Geology 26, 651 1998.
6. U. von Grafenstein, H. Erlenkeuser, J. Muller, J. Jouzel, S. Johnsen, Clim. Dyn. 14, 73 1998.
7. U. von Grafenstein, H. Erlenkeuser, A. Brauer, J. Jouzel, S. J. Johnsen, Science 284, 1654 1999.
8. A. Korhola and J. Weckstrom, Quat. Res. 54, 284 2000.
9. A. Nesje and S. O. Dahl, J. Quat. Sci. 16, 155 2001.
10. F. McDermott, D. P. Mattey, C. Hawkesworth, Science 294, 1328 2001.
11. For U-Th data [supplement to 10], see www.sciencemag.org/cgi/content/full/294/5545/1328/DC1.
12. I. D. Campbell, C. Campbell, M. J. Apps, N. W. Rutter, A. B. G. Bush, Geology 26, 471 1998.
13. W. E. Dean, Geol. Soc. Am. Spec. Pap. 276, 135 1993.
14. F. S. Hu, H. E. Wright, E. Ito, K. Lease, Nature 400, 437 1999.
15. F. A. Street-Perrott and R. A. Perrott, Nature 358, 607 1990.
16. K. Hugen, J. T. Overpeck, L. C. Peterson, S. Trumbore, Nature 380, 51 1996.
17. R. B. Alley, et al., Geology 25, 483 1997.
18. T. Blunier, J. Chappellaz, J. Schwander, B. Stauffer, D. Raynaud, Nature 274, 46 1995.
19. D. C. Barber, et al., Nature 400, 344 1999.
20. H. Renssen, H. Goosse, T. Fichefet, J.-M. Campin, Geophys. Res. Lett. 28, 1567 2001.
BEYOND THE YOUNGER DRYAS
Collapse as Adaptation to Abrupt Climate Change in
Ancient West Asia and the Eastern Mediterranean
"The earliest Holocene abrupt climate changes occurred at 12,800, 8200, 5200,
and 4200 B.P. . . ."
In Confronting Natural Disaster: Engaging the Past to Understand the Future,
G. Bawden and R. Reycraft, editors, pp. 75-98. University of New Mexico
Press, Albuquerque, 2000.
The 8200 B.P. event,
"lasted four hundred years (6400-6000 B.C.) and, like the Younger Dryas,
generated abrupt aridification and cooling in the North Atlantic and North
America, Africa, and Asia (Alley et al. 1997; Barber et al. 1999; Hu et al.
1999; Street-Perrot and Perrot 1990). This event is well-known from the
GISP2 analyses, within which it is second only to the Younger Dryas in
magnitude of some measurable variables (Alley et al. 1997; Figure 22). The
pronounced West Asian signal for the 8200 B.P. event is present in Soreq
Cave speleothem records (Bar-Matthews et al. 1999), Negev snail isotope
variability (Goodfriend 1991, 1999), low Dead Sea levels (Frumkin et al.
1994), and the geochemistry of stage E to stage F transition at Lake Van
(Lemcke and Sturm 1997). . . ."
original bibliography compiled by
Sushma Prasad email@example.com
- Alley, R. B., P. A. Mayewski, T. Sowers, K. C. Taylor and P. U. Clark 1997. Geology 25:483-486.
- Andrews, J. T., L. Keigwin, F. Hall, and Anne E. Jennings 1999. Journal of Quaternary Science 145.:383-397.
- Baldini et al. 2002. Science 296, p: 2203.
- Barber et al., 1999. Nature, v. 400, p. 344.
- Dean, W. E., R. M. Forester, et al. 2002. Quaternary Science Reviews 2116-17.: 1763-1775.
- von Grafenstein, U., H. Erlenkeuser, J. Müller, J. Jouzel and S. Johnsen 1998. Climate Dynamics 14:73-81.
- Hu et al. 1999. Nature 400, 437-443
- Klitgaard-Kristensen et al. 1998.
A regional 8200 cal. yr B.P. cooling event in northwest Europe, induced by final stages of the
Laurentide ice-sheet deglaciation? Journal of Quaternary Science 13: 165-169.
- Noren et al. 2002. Nature 419, pp: 821.
- Renssen, Goosse and Fichefet 2002. Simulation of the 8,200 yr BP Holocene cooling event.
- Rohling, E.J. and Palike, H. 2005. Centennial-scale climate cooling with a sudden cold event around
8,200 years ago. Nature 434: 975-979. 8200VarRohlingNatr05.pdf
- Shuman et al., 2002. Quatern. Sci. Reviews, v. 21, p. 1793-1805
- Spooner et al. 2002. Journal Of Quaternary Science 2002. 177. p: 639-645.
- Teller, J. T., D. W. Levrington and J. D. Mann 2002. Quaternary Science Reviews 21:879-887.
- Tinner and Lotter 2001. Geology, 256., p: 483.
Holocene Palynology from Marion-Dufresne Cores MD99-2209 and 2207 from Chesapeake Bay: Impacts of Climate and Historic Land-Use Change
- Willard, D.A. and Korejwo, D.A. n.d.
Holocene Palynology from Marion-Dufresne Cores MD99-2209 and 2207 from Chesapeake Bay:
Impacts of Climate and Historic Land-Use Change.
U.S. Geological Survey Open-File Report 00-306: Chapter 7.
Viewed online at
- Yu Z, Eicher U. 1998. Science 282: 2235-2238.