热带-亚热带西太平洋珊瑚礁水域中的无机营养物质和有机营养物质

IF 2.7 2区 生物学 Q1 MARINE & FRESHWATER BIOLOGY
Huei-Ting Lin, Vianney Denis, Chih-Chiang Hsieh, Chieh-Jhen Chen, Wanchien Victoria Hsiao, Pei-Ling Wang, Chih-Chieh Su, Yan-Ning Kuo
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引用次数: 0

摘要

珊瑚礁生态系统承载着多样化和高生产力的群落,但全球许多地方的珊瑚正在退化。选择合适的地点,最大限度地开展珊瑚保护和恢复工作至关重要。从质量平衡的角度来看,新养分的供应对于支持富饶的珊瑚礁生态系统至关重要。对可用养分进行量化和定性,可为设定特定区域人为污染监测阈值和提出研究假设提供信息。在此,我们报告了珊瑚礁和沿岸水域 23 个采样点的无机和有机营养物水平,这些采样点覆盖了珊瑚覆盖率从高到低的区域,包括中国南海的两个偏远岛屿--东沙环礁和太平岛。所调查的一些珊瑚礁通过上升流或海底地下水排放(SGD)获得外部无机营养物供应,表明这些地点有可能产生新的营养物(即造礁)。不同地点有机碳和氮浓度的升高或降低分别证明了有机物的产生或去除。上升流和 SGD 对各种无机和有机营养物质分布的影响程度各不相同。在所有地点中,有机氮占总氮的大部分,是环境中潜在的重要氮源。总有机氮(TON)浓度与其碳氮比(C/N-TON)的高度相关性表明,C/N-TON 较低的总有机氮会产生,而在再矿化过程中,氮会被优先去除,从而留下 C/N 比值较高的 "剩余 "总有机氮。此外,我们还发现,珊瑚多样性和覆盖率高的地点有机质含量低,C/N 高,而大型藻类占主导地位的地点有机质含量高。这些新数据对未来研究提出假设很有价值,例如,与高有机质地点相比,低有机质地点是否更适合恢复造礁珊瑚。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

Inorganic and organic nutrients in tropical–subtropical Western Pacific coral reef waters

Inorganic and organic nutrients in tropical–subtropical Western Pacific coral reef waters

Coral reef ecosystems host diversified and highly productive communities, but corals are degrading in many places worldwide. Picking suitable locations to maximize coral conservation and restoration efforts is critical. From a mass balance point of view, the supply of new nutrients is crucial to support a productive and reef-building coral ecosystem. Quantifying and qualifying available nutrients provide information to set region-specific thresholds for anthropogenic pollution monitoring and to generate research hypotheses. Here, we report the inorganic and organic nutrient levels from twenty-three sampling sites in coral reefs and coastal waters covering regions from high to low coral coverage, including two remote islands, Dongsha Atoll and Taiping Island, in the South China Sea. Some of the surveyed reefs received external inorganic nutrient supply via upwelling or submarine groundwater discharge (SGD), suggesting sites potential for new production (i.e., reef-building). Production or removal of organic matter at various sites is evidenced by their elevated or depleted organic carbon and nitrogen concentrations, respectively. The degree of impact by the upwelling and SGD on various inorganic and organic nutrient distribution varies. Among all sites, organic nitrogen accounts for most of the total nitrogen and is potentially a significant nitrogen source for the environment. The highly correlated total organic nitrogen (TON) concentrations and their C-to-N ratios (C/N-TON) suggest the production of TON with low C/N-TON and preferential removal of N during remineralization processes, leaving “leftover” TON with high C/N ratios. Furthermore, we found that high coral diversity and coverage sites are featured in low organic matter with high C/N, while macroalgae-dominating sites had elevated organic matter. The new data are valuable to generate hypotheses for future research to test, for example, whether sites with low organic matter are more suitable for restoring reef-building corals than sites with high organic matter.

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来源期刊
Coral Reefs
Coral Reefs 生物-海洋与淡水生物学
CiteScore
6.80
自引率
11.40%
发文量
111
审稿时长
4-8 weeks
期刊介绍: Coral Reefs, the Journal of the International Coral Reef Society, presents multidisciplinary literature across the broad fields of reef studies, publishing analytical and theoretical papers on both modern and ancient reefs. These encourage the search for theories about reef structure and dynamics, and the use of experimentation, modeling, quantification and the applied sciences. Coverage includes such subject areas as population dynamics; community ecology of reef organisms; energy and nutrient flows; biogeochemical cycles; physiology of calcification; reef responses to natural and anthropogenic influences; stress markers in reef organisms; behavioural ecology; sedimentology; diagenesis; reef structure and morphology; evolutionary ecology of the reef biota; palaeoceanography of coral reefs and coral islands; reef management and its underlying disciplines; molecular biology and genetics of coral; aetiology of disease in reef-related organisms; reef responses to global change, and more.
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