Kendall Matthew S, Poti Matt, Karnauskas Kristopher B
NOAA/NCCOS/CCMA/Biogeography Branch, Silver Spring, MD, USA.
Consolidated Safety Services-Dynamac, Inc., Fairfax, VA, USA.
Glob Chang Biol. 2016 Apr;22(4):1532-47. doi: 10.1111/gcb.13159. Epub 2016 Feb 9.
Changes in larval import, export, and self-seeding will affect the resilience of coral reef ecosystems. Climate change will alter the ocean currents that transport larvae and also increase sea surface temperatures (SST), hastening development, and shortening larval durations. Here, we use transport simulations to estimate future larval connectivity due to: (1) physical transport of larvae from altered circulation alone, and (2) the combined effects of altered currents plus physiological response to warming. Virtual larvae from islands throughout Micronesia were moved according to present-day and future ocean circulation models. The Hybrid Coordinate Ocean Model (HYCOM) spanning 2004-2012 represented present-day currents. For future currents, we altered HYCOM using analysis from the National Center for Atmospheric Research Community Earth System Model, version 1-Biogeochemistry, Representative Concentration Pathway 8.5 experiment. Based on the NCAR model, regional SST is estimated to rise 2.74 °C which corresponds to a ~17% decline in larval duration for some taxa. This reduction was the basis for a separate set of simulations. Results predict an increase in self-seeding in 100 years such that 62-76% of islands experienced increased self-seeding, there was an average domainwide increase of ~1-3% points in self-seeding, and increases of up to 25% points for several individual islands. When changed currents alone were considered, approximately half (i.e., random) of all island pairs experienced decreased connectivity but when reduced PLD was added as an effect, ~65% of connections were weakened. Orientation of archipelagos relative to currents determined the directional bias in connectivity changes. There was no universal relationship between climate change and connectivity applicable to all taxa and settings. Islands that presently export large numbers of larvae but that also maintain or enhance this role into the future should be the focus of conservation measures that promote long-term resilience of larval supply.
幼体的输入、输出和自我播种的变化将影响珊瑚礁生态系统的恢复力。气候变化将改变输送幼体的洋流,还会提高海面温度(SST),加速幼体发育并缩短幼体持续时间。在此,我们使用输运模拟来估计未来的幼体连通性,这是由于:(1)仅环流改变导致的幼体物理输运,以及(2)洋流改变加上对变暖的生理反应的综合影响。来自密克罗尼西亚各地岛屿的虚拟幼体根据当前和未来的海洋环流模型进行移动。涵盖2004 - 2012年的混合坐标海洋模型(HYCOM)代表当前的洋流。对于未来的洋流,我们使用美国国家大气研究中心社区地球系统模型1 - 生物地球化学、代表性浓度路径8.5实验的分析结果对HYCOM进行了调整。基于美国国家大气研究中心的模型,预计区域海面温度将上升2.74℃,这对应于某些分类群的幼体持续时间下降约17%。这种减少是另一组模拟的基础。结果预测,100年后自我播种将增加,使得62 - 76%的岛屿自我播种增加,全区域自我播种平均增加约1 - 3个百分点,几个单个岛屿的增加幅度高达25个百分点。仅考虑洋流变化时,所有岛屿对中约一半(即随机情况)的连通性下降,但当加入幼体持续时间缩短的影响时,约65%的连接被削弱。群岛相对于洋流的方向决定了连通性变化的方向偏差。气候变化与连通性之间不存在适用于所有分类群和环境的普遍关系。目前输出大量幼体且在未来仍保持或增强这一作用的岛屿应成为促进幼体供应长期恢复力的保护措施的重点。