Shimoda Marine Research Center, University of Tsukuba, Shizuoka, Japan.
Marine Biology and Ecology Research Centre, University of Plymouth, Plymouth, UK.
Glob Chang Biol. 2021 May;27(10):2174-2187. doi: 10.1111/gcb.15455. Epub 2021 Jan 10.
Long-term exposure to CO -enriched waters can considerably alter marine biological community development, often resulting in simplified systems dominated by turf algae that possess reduced biodiversity and low ecological complexity. Current understanding of the underlying processes by which ocean acidification alters biological community development and stability remains limited, making the management of such shifts problematic. Here, we deployed recruitment tiles in reference (pH 8.137 ± 0.056 SD) and CO -enriched conditions (pH 7.788 ± 0.105 SD) at a volcanic CO seep in Japan to assess the underlying processes and patterns of algal community development. We assessed (i) algal community succession in two different seasons (Cooler months: January-July, and warmer months: July-January), (ii) the effects of initial community composition on subsequent community succession (by reciprocally transplanting preestablished communities for a further 6 months), and (iii) the community production of resulting communities, to assess how their functioning was altered (following 12 months recruitment). Settlement tiles became dominated by turf algae under CO -enrichment and had lower biomass, diversity and complexity, a pattern consistent across seasons. This locked the community in a species-poor early successional stage. In terms of community functioning, the elevated pCO community had greater net community production, but this did not result in increased algal community cover, biomass, biodiversity or structural complexity. Taken together, this shows that both new and established communities become simplified by rising CO levels. Our transplant of preestablished communities from enriched CO to reference conditions demonstrated their high resilience, since they became indistinguishable from communities maintained entirely in reference conditions. This shows that meaningful reductions in pCO can enable the recovery of algal communities. By understanding the ecological processes responsible for driving shifts in community composition, we can better assess how communities are likely to be altered by ocean acidification.
长期暴露在富含 CO 的水中会极大地改变海洋生物群落的发展,通常导致系统简化,由草皮藻类主导,这些藻类的生物多样性减少,生态复杂性降低。目前对于海洋酸化改变生物群落发展和稳定性的潜在过程的理解仍然有限,这使得管理这些变化成为一个问题。在这里,我们在日本的一个火山 CO 渗漏处部署了参考(pH8.137±0.056SD)和 CO 富集条件(pH7.788±0.105SD)下的繁殖瓦片,以评估藻类群落发展的潜在过程和模式。我们评估了:(i)在两个不同季节(凉爽季节:1 月至 7 月,温暖季节:7 月至 1 月)的藻类群落演替,(ii)初始群落组成对随后群落演替的影响(通过相互移植预先建立的群落再持续 6 个月),以及(iii)由此产生的群落的群落生产力,以评估其功能如何被改变(在 12 个月的繁殖后)。在 CO 富集下,繁殖瓦片被草皮藻类所占据,其生物量、多样性和复杂性较低,这种模式在整个季节都保持一致。这使得群落锁定在物种贫乏的早期演替阶段。就群落功能而言,高 pCO 群落的净群落生产力更高,但这并没有导致藻类群落覆盖率、生物量、生物多样性或结构复杂性的增加。总的来说,这表明新的和已建立的群落都会因 CO 水平的升高而变得简化。我们从富 CO 的移植预先建立的群落到参考条件下的实验表明了它们的高弹性,因为它们与完全维持在参考条件下的群落无法区分。这表明,pCO 的显著降低可以使藻类群落得到恢复。通过了解驱动群落组成变化的生态过程,我们可以更好地评估海洋酸化如何改变群落。