Patagonian and southern South Atlantic view of Holocene climate

QUATERNARY SCIENCE REVIEWS

卷:141

Review

Kaplan, M. R.¹  Schaefer, J. M.^1,2  Strelin, J. A.^3,4  Denton, G. H.^5,6  Anderson, R. F.^1,2  Vandergoes, M. J.⁷  Finkel, R. C.⁸  Schwartz, R.¹  Travis, S. G.⁹  Garcia, J. L.^5,6,10  Martini, M. A.⁴  Nielsen, S. H. H.¹¹ 

[1] Lamont Doherty Earth Observ, Geochem, Palisades, NY 10964 USA

[2] Columbia Univ, Dept Earth & Environm Sci, New York, NY 10027 USA

[3] IAA, Buenos Aires, DF, Argentina

[4] Ctr Invest Ciencias Tierra CONICET UNC, Cordoba, Argentina

[5] Univ Maine, Sch Earth & Climate Sci, Orono, ME 04469 USA

[6] Univ Maine, Climate Change Inst, Orono, ME 04469 USA

[7] GNS Sci, Lower Hutt 5010, New Zealand

[8] Univ Calif Berkeley, Dept Earth & Planetary Sci, Berkeley, CA 95064 USA

[9] GCI, Soldiers Grove, WI 54655 USA

[10] Pontificia Univ Catolica Chile, Fac Hist Geog & Ciencia Polit, Inst Geog, Santiago, Chile

[11] Kenex Ltd, Wellington, New Zealand

关键词: Cosmogenic dating;    Patagonia;    South Atlantic Ocean;    Paleoclimate;    Holocene;   

DOI  :  10.1016/j.quascirev.2016.03.014

来源: Elsevier

【 摘 要 】

We present a comprehensive Be-10 chronology for Holocene moraines in the Lago Argentino basin, on the east side of the South Patagonian Icefield. We focus on three different areas, where prior studies show ample glacier moraine records exist because they were formed by outlet glaciers sensitive to climate change. The Be-10 dated records are from the Lago Pearson, Herminita Peninsula-Brazo Upsala, and Lago Frias areas, which span a distance of almost 100 km adjacent to the modern Icefield. New Be-10 ages show that expanded glaciers and moraine building events occurred at least at 6120 +/- 390 (n = 13), 4450 +/- 220 (n = 7), 1450 or 1410 +/- 110 (n = 18), 360 +/- 30 (n = 5), and 240 +/- 20 (n = 8) years ago. Furthermore, other less well-dated glacier expansions of the Upsala Glacier occurred between similar to 1400 and similar to 1000 and similar to 2300 and similar to 2000 years ago. The most extensive glaciers occurred over the interval from similar to 6100 to similar to 4500 years ago, and their margins over the last similar to 600 years were well within and lower than those in the middle Holocene. The Be-10 ages agree with C-14-limiting data for the glacier histories in this area. We then link southern South American, adjacent South Atlantic, and other Southern Hemisphere records to elucidate broader regional patterns of climate and their possible causes. In the early Holocene, a far southward position of the westerly winds fostered warmth, small Patagonian glaciers, and reduced sea ice coverage over the South Atlantic. Although we infer a pronounced southward displacement of the westerlies during the early Holocene, these conditions did not occur throughout the southern mid-high latitudes, an important exception being over the southwest Pacific sector. Subsequently, a northward locus and/or expansion of the winds over the Patagonia-South Atlantic sector promoted the largest glaciers between similar to 6100 and similar to 4500 years ago and greatest sea ice coverage. Over the last few millennia, the South Patagonian Icefield has experienced successive century-scale advances superimposed on a long-term net decrease in size. Our findings indicate that glaciers and sea ice in the Patagonian-South Atlantic sector of the Southern Hemisphere did not achieve their largest Holocene extents over the last millennium. We conclude that a pattern of more extensive Holocene ice prior to the last millennium is characteristic of the Southern Hemisphere middle latitudes, which differs from the glacier history traditionally thought for the Northern Hemisphere. (C) 2016 Published by Elsevier Ltd.

【 授权许可】

Free