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东南美国沿海造礁冷水珊瑚的分布和预测气候避难所。

Distribution and predicted climatic refugia for a reef-building cold-water coral on the southeast US margin.

机构信息

Department of Biology, Temple University, Philadelphia, Pennsylvania, USA.

NOAA Office of Ocean Exploration and Research, Durham, New Hampshire, USA.

出版信息

Glob Chang Biol. 2022 Dec;28(23):7108-7125. doi: 10.1111/gcb.16415. Epub 2022 Sep 18.

Abstract

Climate change is reorganizing the planet's biodiversity, necessitating proactive management of species and habitats based on spatiotemporal predictions of distributions across climate scenarios. In marine settings, climatic changes will predominantly manifest via warming, ocean acidification, deoxygenation, and changes in hydrodynamics. Lophelia pertusa, the main reef-forming coral present throughout the deep Atlantic Ocean (>200 m), is particularly sensitive to such stressors with stark reductions in suitable habitat predicted to accrue by 2100 in a business-as-usual scenario. However, with new occurrence data for this species along with higher-resolution bathymetry and climate data, it may be possible to locate further climatic refugia. Here, we synthesize new and published biogeographic, geomorphological, and climatic data to build ensemble, multi-scale habitat suitability models for L. pertusa on the continental margin of the southeast United States (SEUS). We then project these models in two timepoints (2050, 2100) and four climate change scenarios to characterize the occurrence probability of this critical cold-water coral (CWC) habitat now and in the future. Our models reveal the extent of reef habitat in the SEUS and corroborate it as the largest currently known essentially continuous CWC reef province on earth, and also predict abundance of L. pertusa to identify key areas, including those outside areas currently protected from bottom-contact fishing. Drastic reductions in L. pertusa climatic suitability index emerged primarily after 2050 and were concentrated at the shallower end (<~550 m) of the regional distribution under the Gulf Stream main axis. Our results thus suggest a depth-driven climate refuge effect where deeper, cooler reef sites experience lesser declines. The strength of this effect increases with climate scenario severity. Taken together, our study has implications for the regional and global management of this species, portending changes in the biodiversity reliant on CWC habitats and the critical ecosystem services they provide.

摘要

气候变化正在重新组合地球的生物多样性,需要根据气候情景下分布的时空预测,对物种和栖息地进行积极的管理。在海洋环境中,气候变化主要表现为变暖、海洋酸化、脱氧和水动力变化。Lophelia pertusa 是大西洋深海 (>200m) 中主要的珊瑚礁形成珊瑚,对这些压力特别敏感,预计在“按现状发展”的情景下,到 2100 年,其适宜栖息地将大幅减少。然而,随着该物种新的出现数据以及更高分辨率的水深和气候数据,可能会找到进一步的气候避难所。在这里,我们综合了新的和已发表的生物地理、地貌和气候数据,为美国东南部大陆架上的 L. pertusa 构建了多尺度的集合栖息地适宜性模型。然后,我们将这些模型投影到两个时间点 (2050 年、2100 年) 和四个气候变化情景中,以描述现在和未来这种关键冷水珊瑚 (CWC) 栖息地的出现概率。我们的模型揭示了美国东南部珊瑚礁的范围,并证实其为地球上目前已知的最大的基本上连续的 CWC 珊瑚礁省份,还预测了 L. pertusa 的丰度,以确定关键区域,包括那些目前不受底部接触捕捞保护的区域。L. pertusa 气候适宜性指数的急剧下降主要出现在 2050 年之后,并且集中在沿湾流主轴线的区域分布的较浅端 (<~550m)。因此,我们的结果表明存在一种由深度驱动的气候避难所效应,在这种效应中,更深、更冷的珊瑚礁站点受到的影响较小。这种效应的强度随着气候情景的严重程度而增加。总的来说,我们的研究对该物种的区域和全球管理具有影响,预示着依赖 CWC 栖息地的生物多样性和它们提供的关键生态系统服务的变化。

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