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DOI | 10.1016/j.ecss.2024.108665 |
Saltmarsh blue carbon accumulation rates and their relationship with sea-level rise on a multi-decadal timescale in northern England | |
Gore, Catrina; Gehrels, W. Roland; Smeaton, Craig; Andrews, Luke; Mcmahon, Lucy; Hibbert, Fiona; Austin, William E. N.; Nolte, Stefanie; Garrett, Ed | |
发表日期 | 2024 |
ISSN | 0272-7714 |
EISSN | 1096-0015 |
起始页码 | 299 |
卷号 | 299 |
英文摘要 | Saltmarshes are widely thought to sequester carbon at rates significantly exceeding those found in terrestrial environments. This ability arises from the in-situ production of plant biomass and the effective trapping and storage of both autochthonous and allochthonous organic carbon. The role saltmarshes play in climate change mitigation, through accumulating 'blue' carbon, depends on both the rate at which carbon accumulates within sediments and the rapidity with which carbon is remineralised. It has been hypothesised that carbon accumulation rates, in turn, depend on the local rate of relative sea-level rise, with faster sea-level rise providing more accommodation space for carbon storage. This relationship has been investigated over long (millennial) and short (decadal) timescales but without accounting for the impact of higher quantities of labile carbon in more recently deposited sediment. This study addresses these three key aspects in a saltmarsh sediment study from Lindisfarne National Nature Reserve (NNR), northern England, where there is a comparatively pristine marsh. We quantify rates of carbon accumulation by combining a Bayesian age-depth model based on 210Pb and 137Cs activities with centimetre-resolution organic carbon density measurements. We also use thermogravimetric analyses to determine the relative proportions of labile and recalcitrant organic matter and calculate the net recalcitrant organic matter accumulation rate. Results indicate that during the 20th century more carbon accumulated at the Lindisfarne NNR saltmarsh during decades with relatively high rates of sea-level rise. The post-depositional loss of labile carbon down the core results in a weaker though still significant relationship between recalcitrant organic matter accumulation and sea-level change. Thus, that increasing saltmarsh carbon accumulation is driven by higher rates of sea-level rise is demonstrated over recent multi-decadal timescales. |
英文关键词 | Labile; Recalcitrant; Thermogravimetric analysis; Chronology; 210 Pb sediment dating; 137 Cs sediment dating |
语种 | 英语 |
WOS研究方向 | Marine & Freshwater Biology ; Oceanography |
WOS类目 | Marine & Freshwater Biology ; Oceanography |
WOS记录号 | WOS:001184295300001 |
来源期刊 | ESTUARINE COASTAL AND SHELF SCIENCE
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文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/302965 |
作者单位 | University of East Anglia; University of York - UK; University of St Andrews; Adam Mickiewicz University; Manchester Metropolitan University; UHI Millennium Institute; Centre for Environment Fisheries & Aquaculture Science |
推荐引用方式 GB/T 7714 | Gore, Catrina,Gehrels, W. Roland,Smeaton, Craig,et al. Saltmarsh blue carbon accumulation rates and their relationship with sea-level rise on a multi-decadal timescale in northern England[J],2024,299. |
APA | Gore, Catrina.,Gehrels, W. Roland.,Smeaton, Craig.,Andrews, Luke.,Mcmahon, Lucy.,...&Garrett, Ed.(2024).Saltmarsh blue carbon accumulation rates and their relationship with sea-level rise on a multi-decadal timescale in northern England.ESTUARINE COASTAL AND SHELF SCIENCE,299. |
MLA | Gore, Catrina,et al."Saltmarsh blue carbon accumulation rates and their relationship with sea-level rise on a multi-decadal timescale in northern England".ESTUARINE COASTAL AND SHELF SCIENCE 299(2024). |
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