Book contents
- Quaternary of the Levant
- Quaternary of the Levant
- Copyright page
- Contents
- Contributors
- Acknowledgements
- 1 The Quaternary of the Levant
- Part I: The Evolution of Current Landscapes and Basins
- Part II: Palaeoclimates
- Part III: Archaeology of Human Evolution
- Part IV: Palaeoecology
- Part V: Quaternary Geomorphology
- 46 Cosmogenic-Isotope Based Erosion Rates along the Western Margin of the Dead Sea Fault
- 47 Palaeogeography and Palaeohydrology of Fluvial Systems in the Levant, Southeastern Mediterranean
- 48 Quaternary Fluvial Environments and Palaeohydrology in Syria
- 49 Stable Carbon and Oxygen Isotope Signatures of Pedogenic Carbonates in Arid and Extremely Arid Environments in the Levant
- 50 Evolution of the Southeastern Mediterranean Coastal Plain
- 51 Middle–Late Quaternary Wetlands along the Coastal Plain of Israel
- 52 The Fluvial Systems
- 53 Loess in the Negev Desert: Sources, Loessial Soils, Palaeosols, and Palaeoclimatic Implications
- 54 Isotopic Tracers of Dust and Loess in the Levant
- 55 Loess, Dunes, and Human Activities
- 56 Late Quaternary Chronologies of the Northern Sinai/Northwestern Negev Dunefield and their Palaeoclimatic and Palaeoenvironmental Implications
- 57 Aridisols in the Southern Levant Deserts and their Palaeoclimate Implications
- 58 Quaternary Sediments and Soils of Jordan
- Part VI: Humans in the Levant
- Index
- Plate section
- References
49 - Stable Carbon and Oxygen Isotope Signatures of Pedogenic Carbonates in Arid and Extremely Arid Environments in the Levant
from Part V: - Quaternary Geomorphology
Published online by Cambridge University Press: 04 May 2017
Book contents
- Quaternary of the Levant
- Quaternary of the Levant
- Copyright page
- Contents
- Contributors
- Acknowledgements
- 1 The Quaternary of the Levant
- Part I: The Evolution of Current Landscapes and Basins
- Part II: Palaeoclimates
- Part III: Archaeology of Human Evolution
- Part IV: Palaeoecology
- Part V: Quaternary Geomorphology
- 46 Cosmogenic-Isotope Based Erosion Rates along the Western Margin of the Dead Sea Fault
- 47 Palaeogeography and Palaeohydrology of Fluvial Systems in the Levant, Southeastern Mediterranean
- 48 Quaternary Fluvial Environments and Palaeohydrology in Syria
- 49 Stable Carbon and Oxygen Isotope Signatures of Pedogenic Carbonates in Arid and Extremely Arid Environments in the Levant
- 50 Evolution of the Southeastern Mediterranean Coastal Plain
- 51 Middle–Late Quaternary Wetlands along the Coastal Plain of Israel
- 52 The Fluvial Systems
- 53 Loess in the Negev Desert: Sources, Loessial Soils, Palaeosols, and Palaeoclimatic Implications
- 54 Isotopic Tracers of Dust and Loess in the Levant
- 55 Loess, Dunes, and Human Activities
- 56 Late Quaternary Chronologies of the Northern Sinai/Northwestern Negev Dunefield and their Palaeoclimatic and Palaeoenvironmental Implications
- 57 Aridisols in the Southern Levant Deserts and their Palaeoclimate Implications
- 58 Quaternary Sediments and Soils of Jordan
- Part VI: Humans in the Levant
- Index
- Plate section
- References
Summary
Pedogenic carbonate is widely used in the study of palaeoenvironments to address topics such as the evolution and spread of vegetation types, tectonic evolution of mountain ranges, Quaternary climate and the geologic carbon cycle. The most useful pedogenic carbonate palaeoenvironmental proxies developed thus far involve carbon and oxygen stable isotope geochemistry. The carbon isotopic composition of pedogenic carbonate is related to soil CO2, which is a function of atmospheric and biologically respired CO2. The latter is correlated with the proportion of C3 and C4 plant photosynthetic pathway. The oxygen isotopic composition of soil carbonates is controlled by the temperature and by the isotopic composition of soil water. In this chapter, we summarize signatures of pedogenic and pseudo-pedogenic carbonate oxygen and carbon isotopic compositions in arid and extremely arid environments in the Levant in general and in the Negev, Israel in particular. Then we demonstrate (a) how sensitive these proxies are to present-day climatic conditions, and (b) how useful these proxies are as paleoclimate indicators.
- Type
- Chapter
- Information
- Quaternary of the LevantEnvironments, Climate Change, and Humans, pp. 423 - 432Publisher: Cambridge University PressPrint publication year: 2017
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