Lamont-Doherty Earth Observatory of Columbia University, Palisades, NY 10964, USA.
Science. 2012 Mar 2;335(6072):1058-63. doi: 10.1126/science.1208277.
Ocean acidification may have severe consequences for marine ecosystems; however, assessing its future impact is difficult because laboratory experiments and field observations are limited by their reduced ecologic complexity and sample period, respectively. In contrast, the geological record contains long-term evidence for a variety of global environmental perturbations, including ocean acidification plus their associated biotic responses. We review events exhibiting evidence for elevated atmospheric CO(2), global warming, and ocean acidification over the past ~300 million years of Earth's history, some with contemporaneous extinction or evolutionary turnover among marine calcifiers. Although similarities exist, no past event perfectly parallels future projections in terms of disrupting the balance of ocean carbonate chemistry-a consequence of the unprecedented rapidity of CO(2) release currently taking place.
海洋酸化可能会对海洋生态系统造成严重后果;然而,评估其未来影响是困难的,因为实验室实验和野外观察分别受到生态复杂性和样本周期的限制。相比之下,地质记录中包含了大量的全球环境干扰的长期证据,包括海洋酸化以及与之相关的生物反应。我们回顾了过去 3 亿年来地球历史上大气 CO2 升高、全球变暖以及海洋酸化的证据,其中一些证据与海洋钙化生物的同时灭绝或进化更替有关。尽管存在相似之处,但没有一个过去的事件在破坏海洋碳酸盐化学平衡方面与未来的预测完全吻合,这是当前 CO2 释放速度空前的结果。