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What Caused the Younger Dryas Cold Event?

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What Caused the Younger Dryas Cold Event? What Caused the Younger Dryas Cold Event? Anders E. Carlson Department of Geoscience and Center for Climatic Research, University of Wisconsin, Madison, Wisconsin 53706, USA The Younger Dryas Cold Event (ca. 12.9– et al., 2007). Lake Agassiz’s eastern outlet his- high pressure, nitrogen and hydrogen can form 11.6 ka) has long been viewed as the canoni- tory also presents an issue, as the most recent ammonia. For the Tunguska increase, a poten- cal abrupt climate event (Fig. 1). The North study suggested that the outlet remained closed tial impact with permafrost could provide the Atlantic region cooled during this interval with until well after the start of the Younger Dryas, hydrogen, whereas the Laurentide Ice Sheet a weakening of Northern Hemisphere monsoon with the lake having no outlet for much of the itself might be the hydrogen source for the strength. The reduction in northward heat trans- Younger Dryas (Lowell et al., 2009). In con- Younger Dryas impact. port warmed the Southern Hemisphere due to trast, a simple consideration of Lake Agassiz’s The Melott et al. study thus lays out a test a process commonly referred to as the bipolar- water budget requires an outlet for the lake dur- for the occurrence of a Younger Dryas bolide seesaw (e.g., Clark et al., 2002). Although it is ing the Younger Dryas (Carlson et al., 2009). impact, constrained by observations of the generally accepted that the cold event resulted This ongoing debate over the ultimate cause of recent Tunguska impact. Their estimates, how- from a slowing Atlantic meridional overturning the Younger Dryas has led to a search for other ever, for the increases in nitrate and ammonium circulation (AMOC), the forcing of this AMOC potential forcing mechanisms, such as an abrupt associated with a Younger Dryas–size comet reduction remains intensely debated. discharge of meltwater to the Arctic Ocean are orders of magnitude larger than observed (Tarasov and Peltier, 2005) and a bolide impact in the Summit Greenland ice core records; the (Firestone et al., 2007). Younger Dryas nitrate and ammonium increases On page 355 of this issue of Geology, Melott are at most just half of the Tunguska increase. et al. (2010) present a quantitative assessment of Likewise, the anomalies noted at the start of the the effect a comet would have on atmospheric Younger Dryas appear to be non-unique in the nitrate, as well as estimates of its consequence highest-resolution records (Figs. 1A and 1B). for atmospheric ammonium, providing a test This may be due to the ice core sample resolu- for the occurrence of a bolide at the onset of tion. The GISP2 ~3.5 yr sample resolution could the Younger Dryas. Accordingly, comets break potentially under-sample a nitrate or ammonium down N2 in the atmosphere to nitrate (NOx), increase (Mayewski et al., 1997) because both increasing nitrate concentration. The authors compounds have atmospheric residence times use a two-dimensional atmospheric model to of a few years. As Melott et al. note, higher-res- simulate the nitrate and ozone changes associ- olution sampling from the Greenland ice cores ated with the A.D. 1908 Tunguska event where could determine if large (i.e., orders of magni- a bolide airburst occurred over Siberia, Rus- tude larger than the Tunguska event) increases sia. The model performs well for the Tunguska in nitrate and ammonium occurred at the start of event, accurately simulating the nitrate increase the Younger Dryas. of ~160 ppb observed in the Greenland Ice Several other issues still remain with the Figure 1. Nitrate (A), ammonium (B), and δ18O Sheet Project 2 (GISP2) ice core record from bolide-forcing hypothesis for the Younger (C) records from Greenland Ice Sheet Proj- Summit Greenland. Scaling the predicted nitrate Dryas. For instance, the original Firestone et al. ect 2 (GISP2) (Grootes et al., 1993; Mayewski et al., 1997). Gray bar denotes the Younger changes upward by six orders of magnitude (2007) impact-marker records have not proven Dryas Cold Event. to the suggested Younger Dryas–size bolide reproducible in a subsequent study (Surovell implies a very large increase in nitrate concen- et al., 2009). Similarly, a compilation of char- tration (i.e., 106 times larger than the Tunguska coal records do not indicate large-scale burning The most common means of slowing AMOC increase) that should be recorded in Greenland of ice-free North America at the onset of the involves the reduction of oceanic surface water ice at the start of the Younger Dryas (Fig. 1A). Younger Dryas (Marlon et al., 2009) as put for- density via an increase in freshwater discharge Greenland ice cores also show ammonium ward by Firestone et al. (2007). Another recent + to the North Atlantic. The originally hypoth- (NH4 ) increases during the Tunguska event study showed that late Pleistocene megafauna esized source of freshwater was the eastward and the Younger Dryas (Fig. 1B). While bio- extinctions, potentially attributable to a Younger routing of Glacial Lake Agassiz from the Mis- mass burning is implicated for the Younger Dryas impact (Firestone et al., 2007), signifi - sissippi River to the St. Lawrence River, as the Dryas increase (e.g., Firestone et al., 2007), the cantly preceded the Younger Dryas (Gill et al., Laurentide Ice Sheet retreated northward out of amount of burning during the Tunguska event is 2009). Furthermore, it has yet to be demon- the Great Lakes (Johnson and McClure, 1976; too small to account for the ammonium increase strated how a short-lived event, such as a bolide Rooth, 1982; Broecker, 2006). A clear Younger of >200 ppb (Melott et al., 2010). Another alter- impact (or abrupt Arctic meltwater discharge, Dryas freshwater signal in the St. Lawrence native, involving direct ammonium deposition i.e., Tarasov and Peltier, 2005), can force a Estuary (Keigwin and Jones, 1995; deVernal et from the bolide, still fails to account for the millennia-long cold event when state-of-the-art al., 1996) only becomes apparent after account- observed Tunguska increase. The authors thus climate models require a continuous freshwater ing for other competing effects on commonly suggest a third mechanism called the Haber forcing for the duration of the AMOC reduction used freshwater proxies, in agreement with process that could account for both the Younger (e.g., Liu et al., 2009). If the bolide impacted three other independent runoff proxies (Carlson Dryas and Tunguska increases, in which, under the southern Laurentide margin near the Great © 2010 Geological Society of America. For permission to copy, contact Copyright Permissions, GSA, or [email protected]. GEOLOGY,Geology, April April 2010; 2010 v. 38; no. 4; p. 383–384; doi: 10.1130/focus042010.1. 383 Downloaded from http://pubs.geoscienceworld.org/gsa/geology/article-pdf/38/4/383/3539423/383.pdf by guest on 27 September 2021 Lakes, it could have opened the eastern outlet the forcing of the Younger Dryas and our under- Keigwin, L.D., and Jones, G.A., 1995, The marine of Lake Agassiz, but Great Lake till sequences standing of abrupt climate events. record of deglaciation from the continental are not disturbed (e.g., Mickelson et al., 1983). margin off Nova Scotia: Paleoceanography, v. 10, p. 973–985, doi: 10.1029/95PA02643. REFERENCES CITED Ultimately, the bolide-forcing hypothesis pre- Liu, Z., et al., 2009, Transient simulation of last de- Berger, A., and Loutre, M.F., 1991, Insolation val- dicts that the Younger Dryas is a unique deglacial glaciation with a new mechanism for Bølling- ues for the climate of the last 10 million years: Allerød warming: Science, v. 325, p. 310–314, event, as suggested by Broecker (2006). How- Quaternary Science Reviews, v. 10, p. 297– doi: 10.1126/science.1171041. ever, high-resolution proxy records sensitive 317, doi: 10.1016/0277-3791(91)90033-Q. Lowell, T.V., Fisher, T.G., Hajdas, I., Glover, K., Loope, δ18 Broecker, W.S., 2006, Was the Younger Dryas trig- to AMOC strength (Chinese speleothem O H., and Henry, T., 2009, Radiocarbon deglacia- gered by a fl ood?: Science, v. 312, p. 1146– and atmospheric methane) document a Younger tion chronology of the Thunder Bay, Ontario area 1148, doi: 10.1126/science.1123253. and implications for ice sheet retreat patterns: Dryas–like event during termination III (the Carlson, A.E., 2008, Why there was not a Younger Quaternary Science Reviews, v. 28, p. 1597– third to the last deglaciation) (Figs. 2B and 2C; Dryas-like event during the Penultimate Deglaci- 1607, doi: 10.1016/j.quascirev.2009.02.025. Carlson, 2008; Cheng et al., 2009). The boreal ation: Quaternary Science Reviews, v. 27, p. 882– Marlon, J.R., et al., 2009, Wildfi re responses to 887, doi: 10.1016/j.quascirev.2008.02.004. summer insolation increase during termination abrupt climate change in North America: Carlson, A.E., Clark, P.U., Haley, B.A., Klinkham- III is similar to the last deglaciation, as is the Proceedings of the National Academy of Sci- mer, G.P., Simmons, K., Brook, E.J., and ences of the United States of America, v. 106, timing of the event relative to the peak in insola- Meissner, K., 2007, Geochemical proxies of p. 2519–2524, doi: 10.1073/pnas.0808212106. tion (Fig. 2D). While not as well constrained, North American freshwater routing during the Mayewski, P.A., Meeker, L.D., Twickler, M.S., Whit- Younger Dryas cold event: Proceedings of the both events occurred at approximately the same low, S., Yang, Q., Lyons, B., and Prentice, M., National Academy of Sciences of the United sea level (Fig. 2A), suggesting there may be a 1997, Major features and forcing of high-lati- States of America, v.
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