Styles and rates of long-term denudation in carbonate terrains under a Mediterranean to hyper-arid climatic gradient
- Permanent Link:
- Styles and rates of long-term denudation in carbonate terrains under a Mediterranean to hyper-arid climatic gradient
- Series Title:
- Earth and Planetary Science Letters
- Ryb, U.
Hidy, A. J.
- Publication Date:
- Subjects / Keywords:
- Denudation ( local )
Chemical Weathering ( local )
Erosion ( local )
Carbonate Terrains ( local )
Climatic Gradient ( local )
36Cl ( local )
- serial ( sobekcm )
- Carbonate minerals, unlike silicates, have the potential to dissolve almost completely and with high efficiency. Thus, in carbonate terrains denudation rate and style (the governing process of denudation, mechanical or chemical) should be more sensitive to climatic forcing. Using 36Cl measurements in 39 carbonate bedrock and sediment samples, we calculate long-term denudation rates across a sharp climatic gradient from Mediterranean to hyper-arid conditions. Our samples were collected along the Arugot watershed, which drains the eastern flank of the Judea Range (central Israel) to the Dead Sea and is characterized by a pronounced rain shadow. Denudation rates of flat-lying bedrock outcrops sampled along interfluves differ by an order of magnitude from âˆ¼20 mmâ€‰kaâˆ’1 in the Mediterranean zone to 1â€“3 mmâ€‰kaâˆ’1 in the hyper-arid zone. These rates are strongly correlated with precipitation, and thus reflect the importance of carbonate mineral dissolution in the overall denudation process. In contrast, denudation rates of steep bedrock surfaces depend on the hillslope gradient, but in the hyper-arid climate zone, indicating that mechanical processes dominate the overall hillslope denudation within this zone. The dominance of slope-dependent mechanical erosion in the hyper-arid zone is also reflected by an increase in spatially-average denudation rates from 17â€“19 mmâ€‰kaâˆ’1 in the Mediterraneanâ€“semi-arid zones to 21â€“25 mmâ€‰kaâˆ’1 in the hyper-arid zone. These higher rates are attributed to clast contribution from steep slopes under arid climate. This suggests an increased importance of mechanical processes to the overall denudation in the hyper-arid zone.
We demonstrate that the transition between chemically-dominated denudation to mechanically-dominated denudation occurs between 100 and 200 mm of mean annual precipitation. Long-term denudation rates across the Judea Range indicate that between Mediterranean and hyper-arid climates, chemical weathering rates are limited by precipitation. Nevertheless, in more humid climates, che
- Original Version:
- Earth and Planetary Science Letters, Vol. 406 (2014-11-15).
- Source Institution:
- University of South Florida Library
- Holding Location:
- University of South Florida
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- This object is protected by copyright, and is made available here for research and educational purposes. Permission to reuse, publish, or reproduce the object beyond the bounds of Fair Use or other exemptions to copyright law must be obtained from the copyright holder.
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