Seasonality of δ13C and C/N ratios in modern and mid-Holocene sediments in the Severn Estuary Levels, SW Britain

Seasonality of δ13C and C/N ratios in modern and mid-Holocene sediments in the Severn Estuary Levels, SW Britain
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英国西南部塞文河口层现代和全新世中期沉积物中 δ13C 和 C/N 比值的季节性

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发表时间:
2007
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影响因子:
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通讯作者:
Petra Dark
Petra Dark
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作者:
J. Allen;A. Lamb;Petra Dark

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具有沉积条带的中全新世盐沼沉积物的有机质δ 13 C和C/N比值揭示了粗粒和细粒沉积物之间的细微但显著的差异。这些都是一致的调查结果,从季节性采样的现代粉砂,并与解释,在物理和孢粉学的理由,细颗粒和粗颗粒的组件作为暖季和冷季存款,分别。控制被认为是有机物质供应的性质的季节性变化。
Bulk organic δ13C and C/N ratios from mid-Holocene salt-marsh deposits with sedimentary banding reveal subtle but significant differences between coarse- and fine-grained deposits. These are consistent with findings from seasonally sampled modern silts, and with the interpretation, on physical and palynological grounds, of the fine-grained and coarse-grained components as warm-season and cold-season deposits, respectively. The control is considered to be seasonal variations in the character of the organic matter supplied.