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14C Tephrochronology With Different Fractions of Paleosol Humic Matter at Procida Island, Italy

Published online by Cambridge University Press:  18 July 2016

Marisa Alessio ,
Lucia Allegri ,
Carlo Azzi ,
Gilberto Calderoni ,
Cesarina Cortesi ,
Salvatore Improta  and
Vincenzo Petrone
Marisa Alessio
Affiliation:
Department of Physics
Lucia Allegri
Affiliation:
Department of Physics
Carlo Azzi
Affiliation:
Department of Physics
Gilberto Calderoni
Affiliation:
Department of Earth Sciences, University “La Sapienza”, Rome, Italy
Cesarina Cortesi
Affiliation:
Department of Earth Sciences, University “La Sapienza”, Rome, Italy
Salvatore Improta
Affiliation:
Department of Physics
Vincenzo Petrone
Affiliation:
Department of Physics
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Abstract

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14C apparent ages along with δ13C values for three different fractions of humic matter (HM) isolated from a suite of four paleosols (PAs) interbedded within tephra are reported. The dated HM fractions were: 1) HA, the easily released humic acids; 2) HAtot, the bulk of humic acids; 3) RES, the insoluble HM. The 14C sequence dated from 13,000–25,000 BP, in agreement with stratigraphy and previous data. Age differences up to 2540±430 were statistically significant among fractions; their order of magnitude being independent from C content and depth. All the PAs showed a common pattern of among-fraction age variation, 14C aging trending from RES to HAtot through HA. As the HM fractions exhibited quite comparable δ13C values (δ13C = −25.4±0.2), it is inferred that the primitive organic matter (OM) input to PAs was dominantly supplied by vegetation of C-3 photosynthetic pathway which underwent complete decomposition during diagenesis.

Type
II. Carbon Cycle in the Environment
Information
Radiocarbon , Volume 31 , Issue 3: June 20-25, 1988 Dubrovnik, Yugoslavia , 1989 , pp. 664 - 671
Copyright
Copyright © The American Journal of Science 

References

Alessio, M, Bella, F, Belluomini, G, Calderoni, G, Cortesi, C, Improta, S and Turi, B, 1976, University of Rome carbon-14 dates XIV: Radiocarbon, v 18, no. 3, p 321–349.Google Scholar
Alessio, M, Bella, F and Cortesi, C, 1970, Report on the equipment and activities of the Rome University's carbon-14 dating laboratory: Quaternaria, v 13, p 357–376.Google Scholar
Becker-Heidmann, PE and Scharpenseel, HW, 1986, Thin layer δ13C and D14C monitoring of “lessive” soil profiles, in Stuiver, M and Kra, RS, eds, Internatl 14C conf, 12th, Proc: Radiocarbon, v 28, no. 2A, p 383–390.Google Scholar
Calderoni, G and Miles, N (ms), 1983, Mineralogy of paleosols from Procida Island (Italy).Google Scholar
Calderoni, G and Schnitzer, M, 1984a, Effects of age on the chemical structure of paleosol humic acids and fulvic acids: Geochim et Cosmochim Acta, v 48, p 2045–2051.Google Scholar
Calderoni, G and Schnitzer, M, 1984b, Nitrogen distribution as a function of radiocarbon age in paleosol humic acids: Organic Geochem, v 5, p 203–209.Google Scholar
Campbell, CA, Paul, EA, Rennie, DA and McCallum, KJ, 1967, Factors affecting the accuracy of the carbon dating method in soil humus studies: Soil Sci, v 104, p 81–85.Google Scholar
Di Girolamo, P and Stanzione, D, 1973, Lineamenti geologici e petrologici dell'isola di Procida: Rend Soc Ital Min Petrol, v 29, p 81–125.Google Scholar
Gilet-Blein, N, Marien, G and Evin, J, 1980, Unreliability of 14C dates from organic matter of soils, in Stuiver, M and Kra, RS, eds, Internatl 14C conf, 10th, Proc: Radiocarbon, v 22, no. 3, p 919–929.Google Scholar
Nonno, U (ms), 1973, Datazioni con il metodo del radiocarbonio di alcuni livelli umificati dell'isola di Procida (Campania): Thesis, Inst Geochemi Univ Rome, Italy.Google Scholar
Polach, HA and Costin, AB, 1971, Validity of soil organic matter radiocarbon dating: buried soils in Snowy Mountains, Southeastern Australia as an example, in Yaloon, DH, ed, Paleopedology-origin, nature and dating of paleosols: Jerusalem, Internatl Soc Soil Sci, Israel Univ Press, p 89–96.Google Scholar
Rittmann, A, 1951, Cenni sulla geologia di Procida: Soc Geol Ital Bull, v 70, p 533–544.Google Scholar
Scharpenseel, HW, 1972, Natural radiocarbon measurement on soil organic matter fractions and on soil profiles of different pedogenesis, in, Rafter, TA and Grant-Taylor, T, eds, Internatl 14C conf, 8th, Proc: Wellington, New Zealand, Royal Soc New Zealand, p 382–393.Google Scholar
Schnitzer, M and Calderoni, G, 1985, Some chemical characteristics of paleosol humic acids: Chem Geol, v 53, p 175–184.Google Scholar
Senesi, N and Calderoni, G, 1988, Structural and chemical characterization of copper, iron and manganese complexes formed by paleosol humic acids, in, Mattavelli, L and Novelli, L, eds, Internatl mtg on organic geochem 13th, Proc: Org Geochem, v 13, p 1145–1152.Google Scholar
Shioya, M and Ishiwatari, R, 1983, Laboratory thermal conversion of sedimentary lipids to kerogene-like matter: Organic Geochem, v 5, p 7–12.CrossRefGoogle Scholar
Stevenson, FJ and Cheng, CN, 1970, Amino acids in sediments: recovery by acid hydrolysis and quantitative estimation by a colorimetric procedure: Geochim et Cosmochim Acta, v 34, p 77–88.Google Scholar
Stevenson, FJ, 1985, Geochemistry of soil humic substances, in Aiken, GR, McKnight, DM, Vershaw, RL and McCarthy, P, eds, Humic substances in soil, sediment and water: New York, John Wiley & Sons, p 13–52.Google Scholar
Violante, P and Wilson, MJ, 1983, Mineralogy of some Italian Andosols with special reference to the origin of the clay fraction: Geoderma, v 29, p 157–174.Google Scholar
Yamamoto, S (ms), 1983, Chemical studies on the formation process of organic geopolymers in recent sediments: PhD dissert, Tokyo Metropolitan Univ, Tokyo, Japan.Google Scholar