Pedogenic carbonates and carbon pools in gypsiferous soils of a semiarid Mediterranean environment in south Italy

被引:22
作者
Laudicina, Vito Armando [1 ]
Scalenghe, Riccardo [1 ]
Pisciotta, Antonio [3 ]
Parello, Francesco [2 ]
Dazzi, Carmelo [1 ]
机构
[1] Univ Palermo, Dipartimento Sistemi Agroambientali, I-90128 Palermo, Italy
[2] Univ Palermo, Dipartimento Sci Terra & Mare, I-90123 Palermo, Italy
[3] Ist Nazl Geofis & Vulcanol, I-90146 Palermo, Italy
关键词
Gypsiferous soils; Soil carbonates; Stable C isotopes; Soil C pools; Soil-landscape relationship; STABLE ISOTOPIC COMPOSITION; CALCIUM-CARBONATE; PRECIPITATION; DESERT; OXYGEN; RESPIRATION; VALLEY;
D O I
10.1016/j.geoderma.2012.07.015
中图分类号
S15 [土壤学];
学科分类号
0903 ; 090301 ;
摘要
Soil carbonates are key features in soils of arid and semiarid environment, playing an important role from pedogenetic, landscape history, paleoclimatic and environmental points of view. The objectives of this work were (i) to study pathways of pedogenic carbonate (PC) formation, (ii) to distinguish between lithogenic and pedogenic inorganic C by using the natural C isotope abundance, and (iii) to estimate the soil C pools in a gypsiferous semiarid Mediterranean environment (Sicily, Italy). Five soil pedons developed on calcareous and non-calcareous parent materials from Holocene (10,000 years BP) to Upper Tortonian (7.2-53 Ma BP) in age were surveyed. During field soil description, the highest stage of carbonate morphology was found in soils developed on non-calcareous Holocene colluvial deposits (youngest deposits in age) which also showed the highest amount of PC. The great amount of PC in soils developed on youngest deposits was ascribed to a soil-landscape relationships. Being located in a doline overhung by gypsum outcrops, precipitation of Ca2+ from gypsum dissolved by rainfall and biogenic CO2 is reliable. The significant positive relationship between soil organic C and pedogenic carbonates delta C-13 values confirms that PC was formed from biogenic CO2. Organic C pool in the first cubic meter of soil ranged from 17 to 42 kg, whilst pedogenic inorganic C pool from 2.8 to 30.7 kg. The estimated rate of inorganic C accumulation in soils developed on youngest deposits was 2.5 g m(-3) y(-1), whereas the rate was negligible on older parent material. The hypothesized pathways of PC formation were ex-novo precipitation of gypsum-Ca2+ and biogenic CO2 and dissolution of lithogenic CaCO3 and re-precipitation of Ca2+ with biogenic CO2. From an environmental prospective, investigated soils may act as a sink of C when Ca2+ from gypsum is available for the formation of pedogenic carbonates. (C) 2012 Elsevier B.V. All rights reserved.
引用
收藏
页码:31 / 38
页数:8
相关论文
共 64 条
[21]   Quantitative aspects of carbonate leaching of soils with differing ages and climates [J].
Egli, M ;
Fitze, P .
CATENA, 2001, 46 (01) :35-62
[22]  
Eswaran H, 2000, GLOBAL CLIMATE CHANGE AND PEDOGENIC CARBONATES, P15
[23]   Solution and recrystallisation processes and associated landforms in gypsum outcrops of Sicily [J].
Ferrarese, F ;
Macaluso, T ;
Madonia, G ;
Palmeri, A ;
Sauro, U .
GEOMORPHOLOGY, 2003, 49 (1-2) :25-43
[24]  
Fierotti G., 1988, REPORT SOIL MAP SICI
[25]  
Gardner W. H., 1986, Methods of soil analysis. Part 1. Physical and mineralogical methods, P493
[26]   Rapid uplift of the Altiplano revealed through 13C-18O bonds in paleosol carbonates [J].
Ghosh, P ;
Garzione, CN ;
Eiler, JM .
SCIENCE, 2006, 311 (5760) :511-515
[27]  
Gile L.H., 1981, NEW MEXICO BUREAU MI, V39
[28]   MORPHOLOGICAL AND GENETIC SEQUENCES OF CARBONATE ACCUMULATION IN DESERT SOILS [J].
GILE, LH ;
PETERSON, FF ;
GROSSMAN, RB .
SOIL SCIENCE, 1966, 101 (05) :347-&
[30]   The stable isotope altimeter: Do Quaternary pedogenic carbonates predict modern elevations? [J].
Hoke, Gregory D. ;
Garzione, Carmala N. ;
Araneo, Diego C. ;
Latorre, Claudio ;
Strecker, Manfred R. ;
Williams, Kendra J. .
GEOLOGY, 2009, 37 (11) :1015-1018