Global S&T Development Trend Analysis Platform of Resources and Environment
DOI | 10.1126/science.abg1685 |
Global acceleration in rates of vegetation change over the past 18,000 years | |
Ondřej Mottl; Suzette G. A. Flantua; Kuber P. Bhatta; Vivian A. Felde; Thomas Giesecke; Simon Goring; Eric C. Grimm; Simon Haberle; Henry Hooghiemstra; Sarah Ivory; Petr Kuneš; Steffen Wolters; Alistair W. R. Seddon; John W. Williams | |
2021-05-21 | |
发表期刊 | Science |
出版年 | 2021 |
英文摘要 | Although much is known about the rapid environmental changes that have occurred since the Industrial Revolution, the patterns of change over the preceding millennia have been only patchily understood. Using a global set of >1100 fossil pollen records, Mottl et al. explored the rates of vegetation change over the past 18,000 years (see the Perspective by Overpeck and Breshears). The authors show that the rates of change accelerated markedly during the Late Holocene (∼4.6 to 2.9 thousand years ago), even more rapidly than the climate-driven vegetation changes associated with the end of the last glacial period. In addition, the Late Holocene acceleration began for terrestrial communities as a whole, suggesting that the acceleration in turnover over the past two centuries is the tip of a deeper trend. Science , abg1685, this issue p. [860][1]; see also abi9902, p. [786][2] Global vegetation over the past 18,000 years has been transformed first by the climate changes that accompanied the last deglaciation and again by increasing human pressures; however, the magnitude and patterns of rates of vegetation change are poorly understood globally. Using a compilation of 1181 fossil pollen sequences and newly developed statistical methods, we detect a worldwide acceleration in the rates of vegetation compositional change beginning between 4.6 and 2.9 thousand years ago that is globally unprecedented over the past 18,000 years in both magnitude and extent. Late Holocene rates of change equal or exceed the deglacial rates for all continents, which suggests that the scale of human effects on terrestrial ecosystems exceeds even the climate-driven transformations of the last deglaciation. The acceleration of biodiversity change demonstrated in ecological datasets from the past century began millennia ago. [1]: /lookup/doi/10.1126/science.abg1685 [2]: /lookup/doi/10.1126/science.abi9902 |
领域 | 气候变化 ; 资源环境 |
URL | 查看原文 |
引用统计 | |
文献类型 | 期刊论文 |
条目标识符 | http://119.78.100.173/C666/handle/2XK7JSWQ/328832 |
专题 | 气候变化 资源环境科学 |
推荐引用方式 GB/T 7714 | Ondřej Mottl,Suzette G. A. Flantua,Kuber P. Bhatta,et al. Global acceleration in rates of vegetation change over the past 18,000 years[J]. Science,2021. |
APA | Ondřej Mottl.,Suzette G. A. Flantua.,Kuber P. Bhatta.,Vivian A. Felde.,Thomas Giesecke.,...&John W. Williams.(2021).Global acceleration in rates of vegetation change over the past 18,000 years.Science. |
MLA | Ondřej Mottl,et al."Global acceleration in rates of vegetation change over the past 18,000 years".Science (2021). |
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