一种甲壳珊瑚藻对海洋酸化的环境遗留影响和适应

Maggie D. Johnson , Lucia M. Rodriguez Bravo , Noelle Lucey , Andrew H. Altieri
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引用次数: 6

摘要

预计先前暴露于可变环境条件会影响海洋生物对全球变化的适应能力。我们进行了为期4个月的补充性野外和实验室实验,以了解动态(有时是极端)环境如何影响热带造礁甲壳珊瑚藻的生长速度及其对海洋酸化(OA)的响应。采用互惠移植设计,我们量化了加勒比海珊瑚Lithophyllum sp.在极端或中等氧、温度和pH值条件下的钙化率。无论来源如何,极端位置原位珊瑚的钙化率比中等位置低90%。来自极端地点的珊瑚的负面影响即使在移植到更理想的条件20周后仍然存在。在实验室中,我们通过将来自同一地点的珊瑚暴露在环境(Amb: pH 8.04)或酸化(OA: pH 7.70)稳定条件或变量(Var: pH 7.80-8.10)或酸化变量(OA-Var: pH 7.45-7.75)条件下,测试了压力和变异性的单独和联合效应。与对照相比,所有pH值处理对石藻钙化率都有负面影响,在每个处理中,极端地点的珊瑚钙化率都低于中等地点的珊瑚钙化率,这表明地点起源对随后的实验室处理反应有遗留影响。我们的研究为理解OA对甲壳珊瑚藻类的细微影响提供了生态相关背景,并说明了当地环境制度如何影响全球变化的影响。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Environmental legacy effects and acclimatization of a crustose coralline alga to ocean acidification

Prior exposure to variable environmental conditions is predicted to influence the resilience of marine organisms to global change. We conducted complementary 4-month field and laboratory experiments to understand how a dynamic, and sometimes extreme, environment influences growth rates of a tropical reef-building crustose coralline alga and its responses to ocean acidification (OA). Using a reciprocal transplant design, we quantified calcification rates of the Caribbean coralline Lithophyllum sp. at sites with a history of either extreme or moderate oxygen, temperature, and pH regimes. Calcification rates of in situ corallines at the extreme site were 90% lower than those at the moderate site, regardless of origin. Negative effects of corallines originating from the extreme site persisted even after transplanting to more optimal conditions for 20 weeks. In the laboratory, we tested the separate and combined effects of stress and variability by exposing corallines from the same sites to either ambient (Amb: pH 8.04) or acidified (OA: pH 7.70) stable conditions or variable (Var: pH 7.80-8.10) or acidified variable (OA-Var: pH 7.45–7.75) conditions. There was a negative effect of all pH treatments on Lithophyllum sp. calcification rates relative to the control, with lower calcification rates in corallines from the extreme site than from the moderate site in each treatment, indicative of a legacy effect of site origin on subsequent response to laboratory treatment. Our study provides ecologically relevant context to understanding the nuanced effects of OA on crustose coralline algae, and illustrates how local environmental regimes may influence the effects of global change.

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