Department of Ecology and Conservation Biology, Texas A&M University, College Station, TX 77843-2258
Proc Natl Acad Sci U S A. 2020 Aug 4;117(31):18550-18556. doi: 10.1073/pnas.1922266117. Epub 2020 Jul 16.
Earth's ancient grasslands and savannas-hereafter old-growth grasslands-have long been viewed by scientists and environmental policymakers as early successional plant communities of low conservation value. Challenging this view, emerging research suggests that old-growth grasslands support substantial biodiversity and are slow to recover if destroyed by human land uses (e.g., tillage agriculture, plantation forestry). But despite growing interest in grassland conservation, there has been no global test of whether old-growth grasslands support greater plant species diversity than secondary grasslands (i.e., herbaceous communities that assemble after destruction of old-growth grasslands). Our synthesis of 31 studies, including 92 timepoints on six continents, found that secondary grasslands supported 37% fewer plant species than old-growth grasslands (log response ratio = -0.46) and that secondary grasslands typically require at least a century, and more often millennia (projected mean 1,400 y), to recover their former richness. Young (<29 y) secondary grasslands were composed of weedy species, and even as their richness increased over decades to centuries, secondary grasslands were still missing characteristic old-growth grassland species (e.g., long-lived perennials). In light of these results, the view that all grasslands are weedy communities, trapped by fire and large herbivores in a state of arrested succession, is untenable. Moving forward, we suggest that ecologists should explicitly consider grassland assembly time and endogenous disturbance regimes in studies of plant community structure and function. We encourage environmental policymakers to prioritize old-growth grassland conservation and work to elevate the status of old-growth grasslands, alongside old-growth forests, in the public consciousness.
地球的古老草原和稀树草原——此后称为原生草原——长期以来一直被科学家和环境政策制定者视为低保护价值的早期演替植物群落。然而,新兴研究表明,原生草原支持着大量的生物多样性,如果被人类土地利用(如耕作农业、人工林)破坏,它们的恢复速度会很慢。但是,尽管人们对草原保护越来越感兴趣,但还没有对原生草原是否比次生草原(即原生草原被破坏后形成的草本群落)支持更多植物物种多样性进行全球测试。我们综合了 31 项研究,包括六大洲的 92 个时间点,发现次生草原的植物物种比原生草原少 37%(对数响应比=-0.46),而且次生草原通常需要至少一个世纪,更常见的是几千年(预计平均 1400 年)才能恢复到以前的丰富程度。年轻的(<29 年)次生草原由杂草物种组成,即使它们的丰富度在几十年到几百年内增加,次生草原仍然缺少特征性的原生草原物种(例如,长寿的多年生植物)。鉴于这些结果,认为所有草原都是杂草群落,被火和大型食草动物困在演替的停滞状态的观点是站不住脚的。展望未来,我们建议生态学家在研究植物群落结构和功能时,应明确考虑草原组合时间和内源性干扰机制。我们鼓励环境政策制定者优先保护原生草原,并努力提高原生草原的地位,使其与原生森林一起在公众意识中得到提升。