Kennedy Jessica R, Blain Caitlin O
Leigh Marine Laboratory, Institute of Marine Science, University of Auckland, Leigh, New Zealand.
Coastal People: Southern Skies Centre of Research Excellence, University of Otago, Dunedin, New Zealand.
J Phycol. 2025 Jun;61(3):399-432. doi: 10.1111/jpy.70031. Epub 2025 May 27.
Although macroalgae are gaining recognition for their potential role in marine carbon sequestration, critical knowledge gaps related to the fate of macroalgal carbon limit our capacity to quantify rates of macroalgal carbon sequestration. Understanding the degradation dynamics of macroalgal-derived biomaterials-including tissue/wrack, particulate organic matter/carbon (POM/POC), and dissolved organic carbon (DOC)-as well as the environmental drivers of decomposition are critical for assessing the longevity of macroalgal carbon and the potential storage capacity of macroalgae. Thus, a systematic literature review of macroalgal degradation studies was conducted to compile data, estimate the relative recalcitrance (i.e., relative stability) of macroalgal biomaterials, and elucidate key drivers of macroalgal decomposition dynamics. We found that macroalgal decay trajectories are highly variable and not always best described by the often-cited exponential decay models. Our analysis demonstrated that temperature was a notable driver of decomposition, with higher temperatures eliciting faster rates of decomposition. Furthermore, we found that brown algae had significantly higher proportions of recalcitrant biomaterials when compared to red algae. The impact of other factors, including biomaterial type, degradation environment, and tissue carbon and nitrogen content on macroalgal degradation, is variable across contexts, warranting further study. These results help to provide a foundation from which to plan and assess future studies on macroalgal degradation, which will improve our understanding of how macroalgae contribute to marine carbon cycles, trophic subsidies, and, potentially, marine carbon sequestration.
尽管大型藻类在海洋碳固存中的潜在作用正逐渐得到认可,但与大型藻类碳的归宿相关的关键知识空白限制了我们量化大型藻类碳固存速率的能力。了解大型藻类衍生生物材料(包括组织/残骸、颗粒有机物质/碳(POM/POC)和溶解有机碳(DOC))的降解动态以及分解的环境驱动因素,对于评估大型藻类碳的寿命和大型藻类的潜在储存能力至关重要。因此,我们对大型藻类降解研究进行了系统的文献综述,以汇编数据、估计大型藻类生物材料的相对难降解性(即相对稳定性),并阐明大型藻类分解动态的关键驱动因素。我们发现,大型藻类的腐烂轨迹高度可变,通常引用的指数衰减模型并不总是能最好地描述这些轨迹。我们的分析表明,温度是分解的一个显著驱动因素,温度越高,分解速率越快。此外,我们发现与红藻相比,褐藻中难降解生物材料的比例显著更高。包括生物材料类型、降解环境以及组织碳和氮含量在内的其他因素对大型藻类降解的影响在不同情况下各不相同,需要进一步研究。这些结果有助于为规划和评估未来关于大型藻类降解的研究提供基础,这将增进我们对大型藻类如何促进海洋碳循环、营养补贴以及潜在的海洋碳固存的理解。