Dong Xu, Chen Baohong, Wang Weili, Wang Jianjia, Zheng Xinqing
Third Institute of Oceanography, Ministry of Natural Resources, Xiamen, China; Fujian Provincial Station for Field Observation and Research of Island and Coastal Zone in Zhangzhou, Zhangzhou, China; Observation and Research Station of Island and Coastal Ecosystem in the Western Taiwan Strait, Ministry of Natural Resources, Xiamen, China.
Third Institute of Oceanography, Ministry of Natural Resources, Xiamen, China; Fujian Provincial Station for Field Observation and Research of Island and Coastal Zone in Zhangzhou, Zhangzhou, China; Observation and Research Station of Island and Coastal Ecosystem in the Western Taiwan Strait, Ministry of Natural Resources, Xiamen, China.
Mar Environ Res. 2025 Sep;210:107361. doi: 10.1016/j.marenvres.2025.107361. Epub 2025 Jul 12.
In reef-building coral habitats, the balance of community organic and inorganic carbon metabolisms can either create an oceanic sink or source of atmospheric CO. However, researchers often overlook how pre-existing seawater-oceanic water that may be out of equilibrium with atmospheric CO before entering the reef system-affects reef system carbon pattern assessments. This study shows that the Dongshan coral habitat acts as an atmospheric CO source during our observations in the summers of 2022 and 2024. Through quantitative analysis of CO source drivers, we found that this primarily results from pre-existing seawater already releasing CO, potentially amplified by external biological processes before reaching the reef system. In contrast, the balance of reef community metabolism has less impact on this dynamic and functions primarily as a carbon sink. Additionally, we found that major environmental changes-such as increased seawater turbidity or decreased chlorophyll levels-could transform this balance from a carbon sink into a source, leading to increased CO evasion. Our study highlights that pre-existing seawater plays a crucial role in shaping the CO source characteristics of Dongshan coral habitats, largely masking whether the reef system itself functions as a sink or source of CO.
在造礁珊瑚栖息地,群落有机碳和无机碳代谢的平衡既可能形成海洋对大气二氧化碳的汇,也可能形成源。然而,研究人员常常忽略了在进入珊瑚礁系统之前,可能与大气二氧化碳处于非平衡状态的原有海水(海水 - 大洋水)如何影响珊瑚礁系统碳模式评估。本研究表明,在2022年和2024年夏季的观测期间,东山珊瑚栖息地是大气二氧化碳的源。通过对二氧化碳源驱动因素的定量分析,我们发现这主要是由于原有海水已经在释放二氧化碳,在到达珊瑚礁系统之前可能被外部生物过程放大。相比之下,珊瑚礁群落代谢的平衡对这种动态的影响较小,主要起到碳汇的作用。此外,我们发现主要的环境变化,如海水浊度增加或叶绿素水平降低,可能会将这种平衡从碳汇转变为碳源,导致二氧化碳逸出增加。我们的研究强调,原有海水在塑造东山珊瑚栖息地的二氧化碳源特征方面起着至关重要的作用,在很大程度上掩盖了珊瑚礁系统本身是作为二氧化碳的汇还是源发挥作用。