Institute of Marine Science, University of Auckland, Auckland, New Zealand.
Glob Chang Biol. 2022 Sep;28(17):5269-5282. doi: 10.1111/gcb.16287. Epub 2022 Jun 20.
Increasing responsiveness to anthropogenic climate change and the loss of global shellfish ecosystems has heightened interest in the carbon storage and sequestration potential of bivalve-dominated systems. While coastal ecosystems are dynamic zones of carbon transformation and change, current uncertainties and notable heterogeneity in the benthic environment make it difficult to ascertain the climate change mitigation capacity of ongoing coastal restoration projects aimed at revitalizing benthic bivalve populations. In this study we sought to distinguish between direct and indirect effects of subtidal green-lipped mussels (Perna canaliculus) on carbon cycling, and combined published literature with in-situ experiments from restored beds to create a carbon budget for New Zealand's shellfish restoration efforts. A direct summation of biogenic calcification, community respiration, and sediment processes suggests a moderate carbon efflux (+100.1 to 179.6 g C m year ) occurs as a result of recent restoration efforts, largely reflective of the heterotrophic nature of bivalves. However, an examination of indirect effects of restoration on benthic community metabolism and sediment dynamics suggests that beds achieve greater carbon fixation rates and support enhanced carbon burial compared to nearby sediments devoid of mussels. We discuss limitations to our first-order approximation and postulate how the significance of mussel restoration to carbon-related outcomes likely increases over longer timescales. Coastal restoration is often conducted to support the provisioning of many ecosystem services, and we propose here that shellfish restoration not be used as a single measure to offset carbon dioxide emissions, but rather used in tandem with other initiatives to recover a bundle of valued ecosystem services.
人为气候变化和全球贝类生态系统丧失的响应能力不断提高,这使得人们对双壳类动物为主的系统的碳储存和固存潜力产生了浓厚的兴趣。虽然沿海生态系统是碳转化和变化的动态区域,但目前在海底环境中存在不确定性和明显的异质性,这使得难以确定旨在恢复底栖双壳类种群的正在进行的沿海恢复项目的减缓气候变化能力。在这项研究中,我们试图区分绿唇贻贝(Perna canaliculus)对碳循环的直接和间接影响,并将已发表的文献与恢复床中的现场实验相结合,为新西兰贝类恢复工作创建一个碳预算。生物成因钙化、群落呼吸和沉积物过程的直接总和表明,由于最近的恢复工作,会产生适度的碳流出(+100.1 至 179.6 g C m 年),这主要反映了双壳类动物的异养性质。然而,对恢复对底栖群落代谢和沉积物动态的间接影响的研究表明,与没有贻贝的附近沉积物相比,床实现了更高的碳固定率,并支持增强的碳埋藏。我们讨论了我们的一阶近似的局限性,并假设贻贝恢复对与碳相关的结果的意义如何随着时间的推移而增加。沿海恢复通常是为了支持许多生态系统服务的提供,我们在这里提出,贝类恢复不应作为抵消二氧化碳排放的单一措施,而是与其他恢复一系列有价值的生态系统服务的举措一起使用。