Department of Animal Ecology & Systematics, Justus Liebig University Giessen, Giessen, Germany.
Red Sea Research Center (RSRC), King Abdullah University of Science and Technology (KAUST), Thuwal, Kingdom of Saudi Arabia.
Glob Chang Biol. 2021 Nov;27(21):5532-5546. doi: 10.1111/gcb.15840. Epub 2021 Sep 3.
Our understanding of the response of reef-building corals to changes in their physical environment is largely based on laboratory experiments, analysis of long-term field data, and model projections. Experimental data provide unique insights into how organisms respond to variation of environmental drivers. However, an assessment of how well experimental conditions cover the breadth of environmental conditions and variability where corals live successfully is missing. Here, we compiled and analyzed a globally distributed dataset of in-situ seasonal and diurnal variability of key environmental drivers (temperature, pCO , and O ) critical for the growth and livelihood of reef-building corals. Using a meta-analysis approach, we compared the variability of environmental conditions assayed in coral experimental studies to current and projected conditions in their natural habitats. We found that annual temperature profiles projected for the end of the 21st century were characterized by distributional shifts in temperatures with warmer winters and longer warm periods in the summer, not just peak temperatures. Furthermore, short-term hourly fluctuations of temperature and pCO may regularly expose corals to conditions beyond the projected average increases for the end of the 21st century. Coral reef sites varied in the degree of coupling between temperature, pCO , and dissolved O , which warrants site-specific, differentiated experimental approaches depending on the local hydrography and influence of biological processes on the carbonate system and O availability. Our analysis highlights that a large portion of the natural environmental variability at short and long timescales is underexplored in experimental designs, which may provide a path to extend our understanding on the response of corals to global climate change.
我们对造礁珊瑚对其物理环境变化的反应的理解主要基于实验室实验、长期现场数据分析和模型预测。实验数据为生物体如何应对环境驱动因素的变化提供了独特的见解。然而,对于实验条件在多大程度上涵盖了珊瑚成功生存的环境条件和变异性的评估还存在空白。在这里,我们编译和分析了一个全球分布的关键环境驱动因素(温度、pCO2 和溶解氧)的原位季节性和日变化的数据集,这些因素对造礁珊瑚的生长和生计至关重要。使用荟萃分析方法,我们将珊瑚实验研究中检测到的环境条件变化与它们自然栖息地中的当前和预测条件进行了比较。我们发现,到 21 世纪末预测的年温度曲线的分布变化特征是冬季变暖,夏季温暖期延长,而不仅仅是峰值温度升高。此外,温度和 pCO2 的短期小时波动可能会使珊瑚经常暴露在超出 21 世纪末预计平均增长率的条件下。珊瑚礁地点的温度、pCO2 和溶解氧之间的耦合程度不同,这需要根据当地的水文情况和生物过程对碳酸盐系统和 O 可用性的影响,采用特定地点、差异化的实验方法。我们的分析强调,在实验设计中,短时间和长时间尺度的自然环境变异性的很大一部分尚未得到充分探索,这可能为扩展我们对珊瑚对全球气候变化的反应的理解提供了一条途径。