Centre for Integrative Ecology, School of Life and Environmental Sciences, Deakin University, Burwood, Vic, Australia.
School of Biological Sciences, The University of Queensland, St. Lucia, Qld, Australia.
Glob Chang Biol. 2021 Jul;27(14):3257-3271. doi: 10.1111/gcb.15642. Epub 2021 May 4.
Australia's Great Barrier Reef (GBR) catchments include some of the world's most intact coastal wetlands comprising diverse mangrove, seagrass and tidal marsh ecosystems. Although these ecosystems are highly efficient at storing carbon in marine sediments, their soil organic carbon (SOC) stocks and the potential changes resulting from climate impacts, including sea level rise are not well understood. For the first time, we estimated SOC stocks and their drivers within the range of coastal wetlands of GBR catchments using boosted regression trees (i.e. a machine learning approach and ensemble method for modelling the relationship between response and explanatory variables) and identified the potential changes in future stocks due to sea level rise. We found levels of SOC stocks of mangrove and seagrass meadows have different drivers, with climatic variables such as temperature, rainfall and solar radiation, showing significant contributions in accounting for variation in SOC stocks in mangroves. In contrast, soil type accounted for most of the variability in seagrass meadows. Total SOC stock in the GBR catchments, including mangroves, seagrass meadows and tidal marshes, is approximately 137 Tg C, which represents 9%-13% of Australia's total SOC stock while encompassing only 4%-6% of the total extent of Australian coastal wetlands. In a global context, this could represent 0.5%-1.4% of global SOC stock. Our study suggests that landward migration due to projected sea level rise has the potential to enhance carbon accumulation with total carbon gains between 0.16 and 0.46 Tg C and provides an opportunity for future restoration to enhance blue carbon.
澳大利亚大堡礁(GBR)集水区包括世界上一些最完整的沿海湿地,拥有多样化的红树林、海草和潮汐沼泽生态系统。尽管这些生态系统在海洋沉积物中储存碳方面非常高效,但它们的土壤有机碳(SOC)储量以及气候变化(包括海平面上升)所带来的潜在变化还没有得到很好的了解。我们首次利用提升回归树(即一种用于模拟响应和解释变量之间关系的机器学习方法和集成方法)来估算 GBR 集水区沿海湿地范围内的 SOC 储量及其驱动因素,并确定了由于海平面上升导致未来储量可能发生的变化。我们发现,红树林和海草草地的 SOC 储量水平有不同的驱动因素,气候变量如温度、降雨和太阳辐射对红树林 SOC 储量的变化有显著贡献。相比之下,土壤类型占海草草地SOC 储量变化的大部分。大堡礁集水区包括红树林、海草草地和潮汐沼泽在内的总 SOC 储量约为 137 太吨碳,占澳大利亚总 SOC 储量的 9%-13%,而仅占澳大利亚沿海湿地总面积的 4%-6%。在全球范围内,这可能代表全球 SOC 储量的 0.5%-1.4%。我们的研究表明,由于预计的海平面上升导致的陆地迁移有可能增加碳的积累,总碳增益在 0.16 到 0.46 太吨碳之间,并为未来的恢复提供了一个增强蓝碳的机会。