Mismatch of glacier extent and summer insolation in Southern Hemisphere mid-latitudes
- Dartmouth College, Hanover, NH (United States). Dept. of Earth Sciences; Univ. of Maine, Orono, ME (United States). School of Earth and Climate Sciences and Climate Change Inst.
- Columbia Univ., Palisades, NY (United States). Lamont-Doherty Earth Observatory; Columbia Univ., New York, NY (United States). Dept. of Earth and Environmental Sciences
- Univ. of Maine, Orono, ME (United States). School of Earth and Climate Sciences and Climate Change Inst.; Columbia Univ., Palisades, NY (United States). Lamont-Doherty Earth Observatory
- Univ. of Maine, Orono, ME (United States). School of Earth and Climate Sciences and Climate Change Inst.
- Columbia Univ., Palisades, NY (United States). Lamont-Doherty Earth Observatory
- GNS Science, Dunedin (New Zealand)
- Univ. of Oslo (Norway). Dept. of Geosciences
- Dept. of Earth and Environmental Sciences, Waterloo, ON (Canada)
- Univ. of California, Berkeley, CA (United States). Dept. of Earth and Planetary Sciences; Lawrence Livermore National Lab. (LLNL), Livermore, CA (United States)
Here in this paper, we address a long-standing puzzle of ice-age climate called the “fly in the ointment of the Milankovitch theory.” Using geomorphic mapping and 10Be surface-exposure dating, we show that five moraine belts were formed during maxima of the last ice age by the Pukaki glacier in New Zealand’s Southern Alps. They afford ages of 41.76 ± 1.09 ka, 35.50 ± 1.26 ka, 27.17 ± 0.68 ka, 20.27 ± 0.60 ka, and 18.29 ± 0.49 ka. These five maxima spanned an entire precessional cycle in summer insolation intensity at the latitude of the Southern Alps. A similar mismatch between summer insolation and glacier extent also characterized the Chilean Lake District in the mid-latitudes of South America. Thus, in apparent contrast to northern ice sheets linked by Milankovitch to summer insolation at 65°N latitude, the behavior of southern mid-latitude glaciers was not tied to local summer insolation intensity. Instead, glacier extent between 41.76 ka and 18.29 ka, as well as during the last termination, was aligned with Southern Ocean surface temperature and with atmospheric carbon dioxide.
- Research Organization:
- Lawrence Livermore National Laboratory (LLNL), Livermore, CA (United States)
- Sponsoring Organization:
- National Science Foundation (NSF); USDOE
- OSTI ID:
- 1418503
- Journal Information:
- Geology, Vol. 43, Issue 5; ISSN 0091-7613
- Publisher:
- Geological Society of AmericaCopyright Statement
- Country of Publication:
- United States
- Language:
- English
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