In situ degradation of kelp detritus: Implications for coastal carbon cycling

IF 3.5 1区 地球科学 Q1 LIMNOLOGY
Jessica R. Kennedy, Cesar T. Facimoto, Alessandro Pisaniello, Kim M. Handley, Caitlin O. Blain
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Abstract

Marine macroalgae (i.e., seaweeds) are crucial components of coastal carbon cycles and may be important contributors to marine carbon sequestration. Understanding the fate of macroalgal-derived carbon in marine systems requires an understanding of the degradation dynamics of macroalgae across environmental gradients. Therefore, we conducted an in situ kelp tissue degradation study in Tīkapa Moana/the Hauraki Gulf, Aotearoa New Zealand to assess the longevity of carbon contained within Ecklonia radiata kelp tissues. We utilized a set of six study sites which represent a natural gradient in turbidity to assess the influence of light availability on kelp decay dynamics, kelp tissue composition, and kelp surface/biofilm bacterial community. We found that half of kelp detritus disappeared within, on average, 58.37 ± 7.9 d. Light availability did not significantly influence kelp tissue longevity, although the shape of the kelp degradation curves differed across the light availability gradient. Kelp tissues maintained baseline concentrations of photosynthetic pigments throughout decomposition, while C : N (carbon : nitrogen) ratio decreased through degradation time at all sites. Degradation was associated with increased alpha diversity of kelp epiphytic bacterial communities and significant changes in kelp epiphytic bacterial community structure. This research shows that kelp tissues persist on subtidal rocky reefs in Tīkapa Moana/the Hauraki Gulf for no longer than 4 months, and that kelp degradation involves complex biogeochemical transformations that are not captured by biomass loss alone. These findings have critical implications for assessing the carbon sequestration potential of kelp forests in Aotearoa New Zealand and beyond.

海带碎屑的原位降解:对海岸碳循环的影响
海洋大型藻类(即海藻)是沿海碳循环的重要组成部分,可能是海洋碳固存的重要贡献者。了解海洋系统中巨藻衍生碳的命运需要了解巨藻在不同环境梯度下的降解动力学。因此,我们在新西兰Aotearoa的Hauraki海湾进行了一项海带组织原位降解研究,以评估辐射Ecklonia辐射海带组织中碳的寿命。我们利用代表自然浊度梯度的六个研究地点来评估光可用性对海带腐烂动力学、海带组织组成和海带表面/生物膜细菌群落的影响。研究发现,一半的海带碎屑平均在58.37±7.9 d内消失。光有效性对海带组织寿命没有显著影响,但在不同光有效性梯度下,海带降解曲线的形状有所不同。在整个分解过程中,海带组织的光合色素浓度保持在基线水平,而C: N(碳:氮)比随着降解时间的延长而降低。降解与海带附生细菌群落α多样性的增加和群落结构的显著变化有关。该研究表明,海带组织在Hauraki湾的潮下岩礁上持续不超过4个月,并且海带的降解涉及复杂的生物地球化学转化,而不仅仅是生物量损失。这些发现对评估新西兰奥特罗阿及其他地区海带森林的碳封存潜力具有重要意义。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
Limnology and Oceanography
Limnology and Oceanography 地学-海洋学
CiteScore
8.80
自引率
6.70%
发文量
254
审稿时长
3 months
期刊介绍: Limnology and Oceanography (L&O; print ISSN 0024-3590, online ISSN 1939-5590) publishes original articles, including scholarly reviews, about all aspects of limnology and oceanography. The journal''s unifying theme is the understanding of aquatic systems. Submissions are judged on the originality of their data, interpretations, and ideas, and on the degree to which they can be generalized beyond the particular aquatic system examined. Laboratory and modeling studies must demonstrate relevance to field environments; typically this means that they are bolstered by substantial "real-world" data. Few purely theoretical or purely empirical papers are accepted for review.
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