Recrystallization of shell carbonate in soil: 14 C labeling, modeling and relevance for dating and paleo-reconstructions

Autor: Yakov Kuzyakov, Kazem Zamanian, Konstantin Pustovoytov
Rok vydání: 2016
Předmět:
Zdroj: Geoderma. 282:87-95
ISSN: 0016-7061
DOI: 10.1016/j.geoderma.2016.07.013
Popis: Mollusk shells are commonly present in a broad array of geological and archaeological contexts. The shell carbonate can serve for numerical age determination (Δ 14 C) and as a paleoenvironmental indicator (δ 18 O, δ 13 C). Shell carbonate recrystallization in soils, however, may re-equilibrate the carbon (C) isotopic signature with soil CO 2 . The equilibration dynamics remain poorly understood because of the absence of suitable experimental approaches. Here we used the artificial 14 C-labeling technique to study the process of shell carbonate recrystallization as a function of time. Organic-free and organic-containing shell particles of Protothaca staminea were mixed with loess or a carbonate-free loamy soil. The mixtures were placed in air-tight bottles, where the bottle air containing 14 CO 2 ( p CO 2 = 2%). The 14 C activity of shells was measured over time and related to the recrystallization of shell carbonate. Recrystallization of shell carbonate already began after one day. The recrystallization rates were 10 − 3 % day − 1 in organic-containing shell embedded in soil and 1.6 · 10 − 2 % day − 1 in organic-free shells in loess. Removal of organic compounds increased shell porosity, and so, increased the contact surface for exchange with soil solution. Organic-free shells recrystallized much faster in loess (0.56% in 56 days) than in other treatments. Recrystallization was 2 to 7 times higher in loess (in the presence and absence of organic compounds, respectively) than in carbonate-free soil. Loess carbonate itself can recrystallize and accumulate on shells, leading to overestimation of shell carbonate recrystallization. A model for shell carbonate recrystallization as a function of time was developed. The model considers the presence or absence of organic compounds in shell structure and geogenic carbonates in the embedding matrix. The model enabled all results to be fitted with R 2 = 0.98. The modelled time necessary for nearly full recrystallization (95% of shell carbonate) was 88 years for organic-free shells in loess and up to 770 years for organic-containing shells in carbonate-free soil. After this period, the original isotopic signature will vanish completely and will be replaced by a new δ 13 C and Δ 14 C signature in the shell structure. Thus, shell carbonate recrystallization may proceed relatively rapidly in terms of geologic time. This is necessary to consider in the interpretation of dating results and paleoenvironmental reconstructions.
Databáze: OpenAIRE
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