Land-use history as a guide for forest conservation and management

被引:55
|
作者
Whitlock, Cathy [1 ,2 ,3 ,4 ]
Colombaroli, Daniele [3 ,5 ,6 ]
Conedera, Marco [4 ]
Tinner, Willy [3 ,5 ]
机构
[1] Montana State Univ, Dept Earth Sci, POB 173480, Bozeman, MT 59717 USA
[2] Montana State Univ, Montana Inst Ecosyst, POB 173480, Bozeman, MT 59717 USA
[3] Univ Bern, Inst Plant Sci, Altenbergrain 21, CH-3013 Bern, Switzerland
[4] Swiss Fed Inst Forest Snow & Landscape Res WSL, Insubr Ecosyst, Ramei 18, CH-6593 Cadenazzo, Switzerland
[5] Univ Bern, Oeschger Ctr Climate Change Res, Falkenpl 16, CH-3012 Bern, Switzerland
[6] Royal Holloway Univ London, Ctr Quaternary Res, Egham TW20 0EX, Surrey, England
基金
美国国家科学基金会;
关键词
climate change; fire history; forest management; historical ecology; humanized landscapes; land-use change; paleoecology; pollen and charcoal analysis; CLIMATE-CHANGE; FIRE REGIMES; LANDSCAPE TRANSFORMATION; POSTGLACIAL VEGETATION; WHITEBARK-PINE; NEW-ZEALAND; ECOSYSTEM; FUTURE; PALEOECOLOGY; COMMUNITIES;
D O I
10.1111/cobi.12960
中图分类号
X176 [生物多样性保护];
学科分类号
090705 ;
摘要
Conservation efforts to protect forested landscapes are challenged by climate projections that suggest substantial restructuring of vegetation and disturbance regimes in the future. In this regard, paleoecological records that describe ecosystem responses to past variations in climate, fire, and human activity offer critical information for assessing present landscape conditions and future landscape vulnerability. We illustrate this point drawing on 8 sites in the northwestern United States, New Zealand, Patagonia, and central and southern Europe that have undergone different levels of climate and land-use change. These sites fall along a gradient of landscape conditions that range from nearly pristine (i.e., vegetation and disturbance shaped primarily by past climate and biophysical constraints) to highly altered (i.e., landscapes that have been intensely modified by past human activity). Position on this gradient has implications for understanding the role of natural and anthropogenic disturbance in shaping ecosystem dynamics and assessments of present biodiversity, including recognizing missing or overrepresented species. Dramatic vegetation reorganization occurred at all study sites as a result of postglacial climate variations. In nearly pristine landscapes, such as those in Yellowstone National Park, climate has remained the primary driver of ecosystem change up to the present day. In Europe, natural vegetation-climate-fire linkages were broken 6000-8000 years ago with the onset of Neolithic farming, and in New Zealand, natural linkages were first lost about 700 years ago with arrival of the Maori people. In the U.S. Northwest and Patagonia, the greatest landscape alteration occurred in the last 150 years with Euro-American settlement. Paleoecology is sometimes the best and only tool for evaluating the degree of landscape alteration and the extent to which landscapes retain natural components. Information on landscape-level history thus helps assess current ecological change, clarify management objectives, and define conservation strategies that seek to protect both natural and cultural elements.
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页码:84 / 97
页数:14
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