Abstract
Pollen, plant macrofossil and charcoal analyses of sediments from two Alaskan lakes provide new data for inferring Lateglacial and Holocene environmental change. The records span the past 14,700 years at Lost Lake, 240 m a.s.l., central Alaska, north of the Alaska Range and 9600 years at Grizzly Lake, 720 m a.s.l., Copper River Plateau, south of the Alaska Range. Salix shrubs expanded in the herb tundra about 14,400 cal b.p., and Betula shrub tundra became established at ca. 13,200 cal b.p. Diminished Betula shrub cover in association with the increased abundance of herbaceous taxa occurred at 12,500–11,600 cal b.p., although the timing of these changes is not well constrained. Populus expanded at 11,200 cal b.p. and formed dense stands until 9600–9400 cal b.p. when Picea glauca forests or woodlands became established at both sites. The abundance of Alnus viridis increased markedly around 8500 cal b.p. at both sites, marking the development of alder shrub thickets around the lakes and on mountain slopes in these areas. Boreal forests dominated by Picea mariana became established around 7200 cal b.p. at Grizzly Lake and 5700 cal b.p. at Lost Lake. At Grizzly Lake, marked vegetational oscillations occurred within the past 8500 years; for example, A. viridis expanded at 2750 cal b.p. and 450 cal b.p. and declined at 150 cal b.p. Some of these oscillations coincide with large-scale climatic events, such as the Little Ice Age cooling (LIA), and they probably reflect vegetational sensitivity to climatic change at this high site. Microscopic charcoal at Lost Lake suggests that fire was important in the lateglacial birch tundra, probably because of severe moisture deficits of the regional climate and/or high abundance of fine fuels. On the basis of the Grizzly Lake microscopic charcoal record, regional fires were common between 8500 and 6800 cal b.p. and between 450 and 150 cal b.p. Around Grizzly Lake, the mean return intervals of local fires estimated from macroscopic charcoal were ∼386 years between 6800 and 5500 cal b.p. when Picea glauca dominated over P. mariana, ∼254 years between 5500 and 3900 cal b.p. when P. mariana was more abundant than P. glauca, and ∼200 years after 3900 cal b.p. in both P. glauca and P. mariana dominated forests. Correlation analysis of pollen and microscopic charcoal at Grizzly Lake reveals that increased fire activity led to the reductions of P. glauca, P. mariana, and tree Betula in association with the expansions of A. viridis, Epilobium, Lycopodium clavatum, and L. annotinum.
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Acknowledgments
We thank B. Ammann, B. Curry, J. Hollis, W. Tanner, and H.E. Wright Jr. for their great help during the coring trips. R. Shaw, S. McMillan, and F. Oberli are gratefully acknowledged for laboratory work and B. Clegg, B.Y. Lee as well as J. van Leeuwen for assistance with pollen determination. We are deeply indebted to W. Oswald, T. Brown, G. Possnert, and M. Söderman for radiocarbon dating and to the Wrangell National Park (Alaska) for permission to core in the year 2000. This study was financed by the Swiss and US National Science Foundations. We thank J. Carrión, B. Vannière, and W.O. van der Knaap for useful suggestions on the manuscript.
Dedication
This study is dedicated to Brigitta Ammann. She bore this and many other projects by her steady support, encouragement, and innovative ideas. One of her most characteristic scientific attitudes is to address new questions in new landscapes with a broad set of palaeoecological tools. For instance she initiated W.T. to investigate palaeofire issues in the Alps in 1993. In 1998 she supported the idea of F.S.H. and W.T. to investigate the fire history of the Copper River Basin by offering a post-doctoral position to W.T. in Bern. Among other things this led to a Swiss NSF post-doc fellowship for W.T. to visit F.S.H. in Urbana-Champaign. This visit in 1999/2000 allowed the start of the Alaskan investigations presented in this study. During the following years Brigitta - who had joined the expedition to Alaska in 1999 - always supported our Alaskan investigations, for instance by encouraging students (R.B. and B.S.) to take over master theses on the Grizzly and Lost Lake cores or by offering laboratory assistance and financing radiocarbon dates. Thus it is difficult to express how deeply indebted we are to Brigitta for her generous, tolerant and congenial attitude during all these years!
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Tinner, W., Hu, F.S., Beer, R. et al. Postglacial vegetational and fire history: pollen, plant macrofossil and charcoal records from two Alaskan lakes. Veget Hist Archaeobot 15, 279–293 (2006). https://doi.org/10.1007/s00334-006-0052-z
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DOI: https://doi.org/10.1007/s00334-006-0052-z