Department of Biosystems Science and Engineering, ETH Zurich, Basel 4056, Switzerland.
Computational Evolution Group, Swiss Institute of Bioinformatics, Lausanne 1015, Switzerland.
Philos Trans R Soc Lond B Biol Sci. 2024 May 27;379(1902):20230011. doi: 10.1098/rstb.2023.0011. Epub 2024 Apr 8.
Most emissions scenarios suggest temperature and precipitation regimes will change dramatically across the globe over the next 500 years. These changes will have large impacts on the biosphere, with species forced to migrate to follow their preferred environmental conditions, therefore moving and fragmenting ecosystems. However, most projections of the impacts of climate change only reach 2100, limiting our understanding of the temporal scope of climate impacts, and potentially impeding suitable adaptive action. To address this data gap, we model future climate change every 20 years from 2000 to 2500 CE, under different CO emissions scenarios, using a general circulation model. We then apply a biome model to these modelled climate futures, to investigate shifts in climatic forcing on vegetation worldwide, the feasibility of the migration required to enact these modelled vegetation changes, and potential overlap with human land use based on modern-day anthromes. Under a business-as-usual scenario, up to 40% of terrestrial area is expected to be suited to a different biome by 2500. Cold-adapted biomes, particularly boreal forest and dry tundra, are predicted to experience the greatest losses of suitable area. Without mitigation, these changes could have severe consequences both for global biodiversity and the provision of ecosystem services. This article is part of the theme issue 'Ecological novelty and planetary stewardship: biodiversity dynamics in a transforming biosphere'.
在未来 500 年内,大多数排放情景表明,全球的气温和降水模式将发生巨大变化。这些变化将对生物圈产生重大影响,迫使物种迁移以适应其偏好的环境条件,从而移动和分裂生态系统。然而,大多数气候变化影响的预测仅到达 2100 年,限制了我们对气候影响的时间范围的理解,并可能阻碍了适当的适应行动。为了解决这个数据缺口,我们使用一个通用循环模型,根据不同的 CO2 排放情景,每隔 20 年模拟 2000 年至 2500 年的未来气候变化。然后,我们将一个生物群落模型应用于这些模拟的气候未来,以调查全球植被气候驱动因素的变化、实施这些模拟植被变化所需的迁移的可行性,以及与基于现代人类聚居区的人类土地利用的潜在重叠。在照常营业的情景下,预计到 2500 年,高达 40%的陆地面积将适合不同的生物群落。适应寒冷的生物群落,特别是北方森林和干燥苔原,预计将经历最适宜地区的大量损失。如果不加以缓解,这些变化可能对全球生物多样性和生态系统服务的提供产生严重后果。本文是“生态新颖性和行星管理:不断变化的生物界中的生物多样性动态”主题问题的一部分。