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The effects of increased oceanic Carbon Dioxide on tide pool communities.

机译:海洋二氧化碳增加对潮汐池群落的影响。

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摘要

Due to anthropogenic emissions of CO2, the world's oceans are becoming more acidic. Ocean pH levels have decreased by 0.1 units since 1850 and are expected to decrease by another 0.3-0.4 units over the next 100 years. Predicting the impacts of ocean acidification on marine communities requires understanding the consequences for individual species and their interactions with other species. This change in pH is likely to have major effects on calcification, metabolic stability and larval development for a wide variety of organisms. Not all organisms are expected to be adversely affected, however, and it is predicted that some algal species may thrive in an acidified ocean environment. Due to respiration (especially at night) and photosynthesis during low tide, the pH of seawater in tide pools can vary dramatically throughout the day. This daily change is orders of magnitude more extreme than what is expected for the ocean at large over the next century. In order to examine how these communities may respond to this aspect of climate change, I exposed both natural tide pools and tide pool mesocosms to high CO2 conditions. To do this, I utilized yeast reactors to maintain low pH conditions within the range of natural pH variation seen in tide pools. Natural tide pools were used for field portions of the experiment, while split mesocosms were used in running seawater tables to examine species interactions. In response, the green alga Ulva increased in growth and cover under high CO2 conditions. High CO2 treatments also resulted in increased grazing by the herbivorous snail, Littorina littorea. Tissue analyses suggest that shifts in stoichiometry may be the reason for this behavioral shift. I also observed transient, but significant, decreases in metrics such as diversity, richness and evenness in natural tide pools following CO2 enrichment. As one of the first in natura studies of this issue, my work highlights the utility and importance of considering ocean acidification effects in a community context.
机译:由于人为排放的二氧化碳,世界海洋变得越来越酸性。自1850年以来,海洋的pH值下降了0.1个单位,并且在接下来的100年中,预计还会再下降0.3-0.4个单位。预测海洋酸化对海洋社区的影响需要了解单个物种的后果及其与其他物种的相互作用。 pH值的这种变化可能会对多种生物的钙化,代谢稳定性和幼体发育产生重大影响。但是,并非所有生物都会受到不利影响,而且据预测,某些藻类物种可能在酸性海洋环境中繁衍生息。由于呼吸(特别是在夜间)和退潮期间的光合作用,潮汐池中海水的pH值在一天中可能会发生巨大变化。每天的变化比下一个世纪对整个海洋的预期要极端得多。为了研究这些社区如何应对气候变化的这一方面,我将自然潮汐池和潮汐池中观都暴露于高CO2条件下。为此,我利用酵母反应器将低pH条件保持在潮汐池中自然pH变化范围内。天然潮汐池用于实验的田间部分,而分裂的中观空间用于运行的海水表中以检查物种之间的相互作用。作为响应,绿藻Ulva在高CO2条件下的生长和覆盖增加。高CO2处理还导致食草蜗牛Littorina littorea放牧增加。组织分析表明,化学计量的变化可能是这种行为变化的原因。我还观察到,CO2富集后,自然潮池中的指标(例如多样性,丰富度和均匀性)暂时但显着降低。作为该问题的自然研究的第一批研究,我的工作强调了在社区环境中考虑海洋酸化作用的实用性和重要性。

著录项

  • 作者

    Gillis, Brendan C.;

  • 作者单位

    Northeastern University.;

  • 授予单位 Northeastern University.;
  • 学科 Ecology.
  • 学位 M.S.
  • 年度 2014
  • 页码 50 p.
  • 总页数 50
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

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