School of Earth Sciences, The Ohio State University, Columbus, Ohio, United States of America.
CNRS-INSU, Laboratoire d'Océanographie de Villefranche, Sorbonne Université, Villefranche-sur-Mer, France.
PLoS One. 2024 Jul 30;19(7):e0306725. doi: 10.1371/journal.pone.0306725. eCollection 2024.
The global increase in anthropogenic CO2 is leading to ocean warming and acidification, which is threatening corals. In Ischia, Italy, two species of Mediterranean scleractinian corals-the symbiotic Cladocora caespitosa and the asymbiotic Astroides calycularis-were collected from ambient pH sites (average pHT = 8.05) and adjacent CO2 vent sites (average pHT = 7.8) to evaluate their response to ocean acidification. Coral colonies from both sites were reared in a laboratory setting for six months at present day pH (pHT ~ 8.08) or low pH (pHT ~7.72). Previous work showed that these corals were tolerant of low pH and maintained positive calcification rates throughout the experiment. We hypothesized that these corals cope with low pH by increasing their heterotrophic capacity (i.e., feeding and/or proportion of heterotrophically derived compounds incorporated in their tissues), irrespective of site of origin, which was quantified indirectly by measuring δ13C, δ15N, and sterols. To further characterize coral health, we quantified energy reserves by measuring biomass, total lipids, and lipid classes. Additional analysis for C. caespitosa included carbohydrates (an energy reserve) and chlorophyll a (an indicator of photosynthetic capacity). Isotopic evidence shows that ambient-sourced Mediterranean corals, of both species, decreased heterotrophy in response to six months of low pH. Despite maintaining energy reserves, lower net photosynthesis (C. caespitosa) and a trend of declining calcification (A. calycularis) suggest a long-term cost to low heterotrophy under ocean acidification conditions. Conversely, vent-sourced corals maintained moderate (C. caespitosa) or high (A. calycularis) heterotrophic capacity and increased photosynthesis rates (C. caespitosa) in response to six months at low pH, allowing them to sustain themselves physiologically. Provided there is sufficient zooplankton and/or organic matter to meet their heterotrophic needs, vent-sourced corals are more likely to persist this century and potentially be a source for new corals in the Mediterranean.
人为 CO2 的全球增加导致海洋升温酸化,这威胁到珊瑚。在意大利伊斯基亚,采集了两种地中海石珊瑚——共生的 Cladocora caespitosa 和非共生的 Astroides calycularis——来自环境 pH 点(平均 pHT = 8.05)和相邻的 CO2 喷口点(平均 pHT = 7.8),以评估它们对海洋酸化的反应。来自两个地点的珊瑚群体在实验室环境中被饲养了六个月,目前的 pH 值(pHT8.08)或低 pH 值(pHT7.72)。之前的工作表明,这些珊瑚能够耐受低 pH 值,并在整个实验过程中保持正钙化率。我们假设这些珊瑚通过增加其异养能力(即摄食和/或异养来源的化合物在组织中的比例)来应对低 pH 值,而不管其起源地如何,这通过间接测量 δ13C、δ15N 和甾醇来量化。为了进一步描述珊瑚的健康状况,我们通过测量生物量、总脂质和脂质类来衡量能量储备。对 C. caespitosa 的进一步分析包括碳水化合物(一种能量储备)和叶绿素 a(光合作用能力的指标)。同位素证据表明,两种物种的环境源地中海珊瑚都减少了异养作用,以应对六个月的低 pH 值。尽管维持了能量储备,但净光合作用降低(C. caespitosa)和钙化趋势下降(A. calycularis)表明,在海洋酸化条件下,长期的低异养作用会带来成本。相比之下,喷口源珊瑚维持适度(C. caespitosa)或高(A. calycularis)异养能力,并在低 pH 值下增加光合作用率(C. caespitosa),从而在生理上维持自身。只要有足够的浮游动物和/或有机物来满足其异养需求,喷口源珊瑚就更有可能在本世纪存活下来,并可能成为地中海新珊瑚的来源。