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Ocean acidification impacts multiple early life history processes of the Caribbean coral Porites astreoides

机译:海洋酸化影响了加勒比珊瑚多孔质Astreoides的多个早期生命历史过程

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摘要

Ocean acidification (OA) refers to the increase in acidity (decrease in pH) of the ocean's surface waters resulting from oceanic uptake of atmospheric carbon dioxide (CO2). Mounting experimental evidence suggests that OA threatens numerous marine organisms, including reef-building corals. Coral recruitment is critical to the persistence and resilience of coral reefs and is regulated by several early life processes, including: larval availability (gamete production, fertilization, etc.), larval settlement, postsettlement growth, and survival. Environmental factors that disrupt these early life processes can result in compromised or failed recruitment and profoundly affect future population dynamics. To evaluate the effects of OA on the sexual recruitment of corals, we tested larval metabolism, larval settlement, and postsettlement growth of the common Caribbean coral Porites astreoides at three pCO(2) levels: ambient seawater (380 mu atm) and two pCO(2) scenarios that are projected to occur by the middle (560 mu atm) and end (800 mu atm) of the century. Our results show that larval metabolism is depressed by 27% and 63% at 560 and 800 mu atm, respectively, compared with controls. Settlement was reduced by 42-45% at 560 mu atm and 55-60% at 800 mu atm, relative to controls. Results indicate that OA primarily affects settlement via indirect pathways, whereby acidified seawater alters the substrate community composition, limiting the availability of settlement cues. Postsettlement growth decreased by 16% and 35% at 560 and 800 mu atm, respectively, relative to controls. This study demonstrates that OA has the potential to negatively impact multiple early life history processes of P. astreoides and may contribute to substantial declines in sexual recruitment that are felt at the community and/or ecosystem scale.
机译:海洋酸化(OA)是指由于海洋吸收大气中的二氧化碳(CO2)而导致海洋地表水的酸度增加(pH降低)。越来越多的实验证据表明,OA威胁着众多海洋生物,包括造礁珊瑚。珊瑚的募集对珊瑚礁的持久性和复原力至关重要,并受到几个早期生命过程的调节,包括:幼体的可利用性(配子的生产,受精等),幼体的沉降,沉降后的生长和生存。破坏这些早期生活过程的环境因素可能导致招募工作受损或失败,并深刻影响未来的人口动态。为了评估OA对珊瑚有性募集的影响,我们测试了三种pCO(2)水平下普通加勒比珊瑚Porrites asteroides的幼体代谢,幼体沉降和沉降后生长:环境海水(380 mu atm)和两个pCO( 2)预计在本世纪中叶(560微米大气压)和末端(800微米大气压)发生的情景。我们的结果表明,与对照组相比,在560和800μatm时,幼虫的代谢分别降低了27%和63%。相对于对照,沉降在560微米大气压下减少了42-45%,在800微米大气压下减少了55-60%。结果表明,OA主要通过间接途径影响沉降,而酸化海水会改变底物群落组成,从而限制沉降线索的可用性。相对于对照组,沉降后的生长分别在560和800亩大气压下分别降低了16%和35%。这项研究表明,OA有可能对多种P. astreoides的早期生活史过程产生负面影响,并可能导致社区和/或生态系统规模的性征募集大量减少。

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