Coral Geochemical Records Track Millennial-Scale Ecosystem Change and Resilience in the Tropical Eastern Pacific

J. Cybulski, N. Duprey, S. Connolly, A. Foreman, Erin M. Dillon, H. Vonhof, A. Martínez-García, Brigida de Gracia, A. O’Dea
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Abstract

Along the coastal Tropical Eastern Pacific (TEP), regions of strong seasonal upwelling bring cold, nutrient-rich waters, controlling ecological conditions and sustaining millions of people through large-scale fisheries. The TEP is also important for the regulation of global climate and is affected by large-scale environmental processes such as ENSO. How the nutrient dynamics of this region will respond to climate change and what the implications will be for coastal ecology remains unknown. Environmental records are needed that capture intra and inter-decadal variation and extend over millennia where these biotic and abiotic processes interact. Here, we develop a new sampling approach and construct two coral skeleton records (n = >600) from reef matrix cores that extend six millennia, from the upwelling Gulf of Panamá and the non-upwelling Gulf of Chiriquí. We ask what effects millennial-scale climate patterns have on upwelling in the region, and how the magnitude of upwelled nutrients influences ecological productivity and even human habitation. We combined multiple proxies using climatic (carbonate δ18O), nutrient (skeletal-organic matrix δ15N), diagenetic (taphonomic scoring), ecological (benthic community composition), and temporal (U-Th dates) data. Using Generalised Additive Models to assess variability, we find strong divergences in the nutrient (δ15N; range >5 ‰) records between Gulfs, while δ18O (range ~2‰) is more stable. The greatest variation in δ15N values occurs during times of high reef accretion whereas δ18O is constant, suggesting that nutrients, not temperature, are driving reef productivity. Taphonomic, taxonomic, and age data reveal periodic shifts and collapses of coral communities that differ between Gulfs. We end by drawing connections between these ecological shifts to the episodic human habitation documented during the late-Holocene and hypothesize what this may mean for ecosystem resilience and environmental management under future climate.
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热带东太平洋珊瑚地球化学记录追踪千年尺度生态系统变化和恢复力
沿着热带东太平洋沿海地区,季节性上升流强烈的地区带来了寒冷、营养丰富的水域,控制了生态条件,并通过大规模渔业维持了数百万人的生计。TEP对全球气候的调节也很重要,并受到ENSO等大规模环境过程的影响。该地区的营养动态将如何响应气候变化以及对沿海生态的影响仍然未知。需要环境记录来捕捉年代际和年代际变化,并在这些生物和非生物过程相互作用的地方延续数千年。在此,我们开发了一种新的采样方法,并从巴拿马上升流湾和Chiriquí非上升流湾的六千年珊瑚礁基质岩心中构建了两个珊瑚骨架记录(n = >600)。我们想知道千年尺度的气候模式对该地区的上升流有什么影响,以及上升流的营养物质的大小如何影响生态生产力甚至人类居住。我们结合了气候(碳酸盐δ18O)、营养(骨骼-有机基质δ15N)、成岩(地层学评分)、生态(底栖生物群落组成)和时间(U-Th日期)数据等多个指标。利用广义加性模型评估变异,我们发现养分(δ15N;δ18O值(范围>5‰)相对稳定,δ18O值(范围~2‰)相对稳定。δ15N值的最大变化发生在珊瑚礁高增生时期,而δ18O是恒定的,这表明是营养物质而不是温度驱动了珊瑚礁的生产力。地貌学、分类学和年龄数据揭示了不同海湾之间珊瑚群落的周期性变化和崩溃。最后,我们将这些生态变化与晚全新世记录的偶发性人类居住联系起来,并假设这对未来气候下的生态系统恢复力和环境管理可能意味着什么。
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