The impact of recycling of organic carbon on the stable carbon isotopic composition of dissolved inorganic carbon in a stratified marine system (Kyllaren fjord, Norway)

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• 作者：van Breugel ; Y. ; Schouten ; S. ; Paetzel ; M. ; Nordeide ; R. ; Sinninghe Damst?? ; J.S.
• 刊名：Organic Geochemistry
• 出版年：2005
• 出版时间：August, 2005
• 年：2005
• 卷：36
• 期：8
• 页码：1163-1173
• 全文大小：530 K

文摘

A negative carbon isotope shift in sedimentary organic carbon deposited in stratified marine and lacustrine systems has often been inferred to be a consequence of the process of recycling of respired and, therefore, ¹³C-depleted, dissolved inorganic carbon (DIC) formed from mineralization of descending organic matter. To study this process, we measured δ¹³C_DIC and δ¹³C values of particulate organic carbon (POC) over an annual cycle in the permanently stratified Kyllaren fjord in Norway. A notable accumulation of respired DIC below the chemocline was evident from the substantially ¹³C-depleted DIC (ca. −19‰). Especially in autumn to early spring, respired DIC from the deep anoxic water is mixed into the oxygenated surface water and the calculated respired DIC contribution to the total DIC pool was up to 40 % in early spring in the upper 2 m of the water column. At 4 m depth, just below the chemocline, the respired DIC contribution reaches ca. 90 % of the total DIC pool. Assimilation of the respired DIC seems to exert only a small effect on δ¹³C_POC, which has an average δ¹³C value of −24‰. The measured photoautotrophic fractionation (ε_p) was low (<10‰) during the majority of the year. This is likely responsible for reducing the apparent impact of recycling of respired DIC on δ¹³C_POC. However, in June 2002, photoautotrophic use of the ¹³C-depleted DIC is obvious from a ¹³C-depletion of POC (−33.7‰) derived from a bloom of the protist Euglena sp.