TY - JOUR

T1 - Pedogenic carbonates

T2 - Forms and formation processes

AU - Zamanian, Kazem

AU - Pustovoytov, Konstantin

AU - Kuzyakov, Yakov

N1 - Funding information: We would like to acknowledge the German Research Foundation (DFG) for their support ( KU 1184/34-1 ). Special thanks to Dr. Otto Ehrmann ( http://www.bildarchiv-boden.de ) for providing us photos of earthworm biospherolith ( Fig. 2 , right) and calcite hypocoating ( Fig. 4 , right). Special thanks to Miss. Yue Sun for drawing graphics in Figs. 3, 4, 6 and 8 . We would like to thank the Soil Science Department, University of Tehran (Karaj, Iran), for their help in preparing soil thin sections and the University of Tarbiat Modares (Tehran, Iran) for SEM images of calcified root cells ( Fig. 3 ).

PY - 2016/6/1

Y1 - 2016/6/1

N2 - Soils comprise the largest terrestrial carbon (C) pool, containing both organic and inorganic C. Soil inorganic carbon (SIC) was frequently disregarded because (1) it is partly heritage from soil parent material, (2) it undergoes slow formation processes and (3) has very slow exchange with atmospheric CO2. The global importance of SIC, however, is reflected by the fact that SIC links the long-term geological C cycle with the fast biotic C cycle, and this linkage is ongoing in soils. Furthermore, the importance of SIC is at least as high as that of soil organic carbon (SOC) especially in semiarid and arid climates, where SIC comprises the largest C pool. Considering the origin, formation processes and morphology, carbonates in soils are categorized into three groups: geogenic carbonates (GC), biogenic carbonates (BC) and pedogenic carbonates (PC). In this review we summarize the available data and theories on forms and formation processes of PC and relate them to environmental factors. After describing the general formation principles of PC, we present the specific forms and formation processes for PC features and the possibilities to use them to reconstruct soil-forming factors and processes. The following PC are described in detail: earthworm biospheroliths, rhizoliths and calcified roots, hypocoatings, nodules, clast coatings, calcretes and laminar caps.The second part of the review focuses on the isotopic composition of PC: δ13C, δ14C and δ18O, as well as clumped 13C and 18O isotopes known as δ47. The isotopic signature of PC enables reconstructing the formation environment: the dominating vegetation (δ13C), temperature (δ18O and δ47), and the age of PC formation (δ14C). The uncertainties in reconstructional and dating studies due to PC recrystallization after formation are discussed and simple approaches to consider recrystallization are summarized.Finally, we suggest the most important future research directions on PC, including the anthropogenic effects of fertilization and soil management. In conclusion, PC are an important part of SIC that reflect the time, periods and formation processes in soils. A mechanistic understanding of PC formation is a prerequisite to predict terrestrial C stocks and changes in the global C cycle, and to link the long-term geological with short-term biological C cycles.

AB - Soils comprise the largest terrestrial carbon (C) pool, containing both organic and inorganic C. Soil inorganic carbon (SIC) was frequently disregarded because (1) it is partly heritage from soil parent material, (2) it undergoes slow formation processes and (3) has very slow exchange with atmospheric CO2. The global importance of SIC, however, is reflected by the fact that SIC links the long-term geological C cycle with the fast biotic C cycle, and this linkage is ongoing in soils. Furthermore, the importance of SIC is at least as high as that of soil organic carbon (SOC) especially in semiarid and arid climates, where SIC comprises the largest C pool. Considering the origin, formation processes and morphology, carbonates in soils are categorized into three groups: geogenic carbonates (GC), biogenic carbonates (BC) and pedogenic carbonates (PC). In this review we summarize the available data and theories on forms and formation processes of PC and relate them to environmental factors. After describing the general formation principles of PC, we present the specific forms and formation processes for PC features and the possibilities to use them to reconstruct soil-forming factors and processes. The following PC are described in detail: earthworm biospheroliths, rhizoliths and calcified roots, hypocoatings, nodules, clast coatings, calcretes and laminar caps.The second part of the review focuses on the isotopic composition of PC: δ13C, δ14C and δ18O, as well as clumped 13C and 18O isotopes known as δ47. The isotopic signature of PC enables reconstructing the formation environment: the dominating vegetation (δ13C), temperature (δ18O and δ47), and the age of PC formation (δ14C). The uncertainties in reconstructional and dating studies due to PC recrystallization after formation are discussed and simple approaches to consider recrystallization are summarized.Finally, we suggest the most important future research directions on PC, including the anthropogenic effects of fertilization and soil management. In conclusion, PC are an important part of SIC that reflect the time, periods and formation processes in soils. A mechanistic understanding of PC formation is a prerequisite to predict terrestrial C stocks and changes in the global C cycle, and to link the long-term geological with short-term biological C cycles.

KW - CaCO recrystallization

KW - Diagenesis

KW - Inorganic carbon sequestration

KW - Paleoenvironment reconstructions

KW - Pedogenic carbonate

KW - Radiocarbon dating

UR - http://www.scopus.com/inward/record.url?scp=84964822083&partnerID=8YFLogxK

U2 - 10.1016/j.earscirev.2016.03.003

DO - 10.1016/j.earscirev.2016.03.003

M3 - Review article

AN - SCOPUS:84964822083

VL - 157

SP - 1

EP - 17

JO - Earth-Science Reviews

JF - Earth-Science Reviews

SN - 0012-8252

ER -