Southern California Coastal Water Research Project, Costa Mesa, CA 92626, USA.
NOAA Pacific Marine Environmental Laboratory, 7600 Sand Point Way NE, Seattle, WA 98115, USA.
Sci Total Environ. 2020 May 10;716:136610. doi: 10.1016/j.scitotenv.2020.136610. Epub 2020 Jan 22.
Ocean acidification (OA) along the US West Coast is intensifying faster than observed in the global ocean. This is particularly true in nearshore regions (<200 m) that experience a lower buffering capacity while at the same time providing important habitats for ecologically and economically significant species. While the literature on the effects of OA from laboratory experiments is voluminous, there is little understanding of present-day OA in-situ effects on marine life. Dungeness crab (Metacarcinus magister) is perennially one of the most valuable commercial and recreational fisheries. We focused on establishing OA-related vulnerability of larval crustacean based on mineralogical and elemental carapace to external and internal carapace dissolution by using a combination of different methods ranging from scanning electron microscopy, energy dispersive X-ray spectroscopy, elemental mapping and X-ray diffraction. By integrating carapace features with the chemical observations and biogeochemical model hindcast, we identify the occurrence of external carapace dissolution related to the steepest Ω calcite gradients (∆Ω) in the water column. Dissolution features are observed across the carapace, pereopods (legs), and around the calcified areas surrounding neuritic canals of mechanoreceptors. The carapace dissolution is the most extensive in the coastal habitats under prolonged (1-month) long exposure, as demonstrated by the use of the model hindcast. Such dissolution has a potential to destabilize mechanoreceptors with important sensory and behavioral functions, a pathway of sensitivity to OA. Carapace dissolution is negatively related to crab larval width, demonstrating a basis for energetic trade-offs. Using a retrospective prediction from a regression models, we estimate an 8.3% increase in external carapace dissolution over the last two decades and identified a set of affected OA-related sublethal pathways to inform future risk assessment studies of Dungeness crabs.
美国西海岸的海洋酸化(OA)正在加剧,其速度比全球海洋观测到的还要快。在近海地区(<200m)尤其如此,这些地区缓冲能力较低,同时为具有生态和经济重要性的物种提供了重要的栖息地。虽然关于实验室实验中 OA 影响的文献很多,但对当今海洋生物体内 OA 影响的了解甚少。珍宝蟹(Metacarcinus magister)常年是最有价值的商业和休闲渔业之一。我们专注于建立基于矿物学和元素甲壳的幼虫甲壳类动物与外部和内部甲壳溶解的 OA 相关易损性,使用了一系列不同的方法,包括扫描电子显微镜、能量色散 X 射线光谱、元素映射和 X 射线衍射。通过将甲壳特征与化学观察和生物地球化学模型回溯相结合,我们确定了与水柱中碳酸钙饱和度梯度(∆Ω)最陡相关的外部甲壳溶解的发生。溶解特征出现在甲壳、步足(腿)以及围绕机械感受器神经通道的钙化区域。在沿海栖息地,甲壳的溶解在长时间(1 个月)暴露下最为广泛,这可以通过使用模型回溯来证明。这种溶解有可能破坏具有重要感觉和行为功能的机械感受器,这是对 OA 敏感的途径。甲壳的溶解与蟹幼虫的宽度呈负相关,这表明存在能量权衡的基础。使用回归模型的回溯预测,我们估计在过去二十年中,外部甲壳的溶解增加了 8.3%,并确定了一组受 OA 影响的亚致死途径,为珍宝蟹的未来风险评估研究提供信息。