Search engine for discovering works of Art, research articles, and books related to Art and Culture
ShareThis
Javascript must be enabled to continue!

Denudation rates on cratonic landscapes: comparison between suspended and dissolved fluxes, and 10Be analysis in the Nyong and Sanaga River basins, south Cameroon

View through CrossRef
AbstractSouth Cameroon is located in a tropical and tectonically quiescent region, with landscapes characterized by thick highly weathered regolith, indicative of the long‐term predominance of chemical weathering over erosion. Currently this region undergoes huge changes due to accelerated mutations related to a growing population and economical developments with associated needs and increasing pressures on land and natural resources. We analysed two of the main south Cameroon rivers: the Nyong River and Sanaga River. The Sanaga catchment undergoes a contrasted tropical climate from sub‐humid mountainous and humid climate and is impacted by deforestation, agriculture, damming, mining and urbanization, especially in the Mbam sub‐basin, draining the highly populated volcanic highlands. By contrast, the Nyong catchment, only under humid tropical climate, is preserved from anthropogenic disturbance with low population except in the region of Yaoundé (Méfou sub‐basin). Moreover the Nyong basin is dam‐free and less impacted by agriculture and logging.We explore both denudation temporal variability and the ratio between chemical and physical denudation through two catchment‐averaged erosion and denudation datasets. The first one consists of an 11‐year long gauging dataset, while the second one comes from cosmogenic radionuclides [CRNs, here beryllium‐10 (10Be)] from sand sampled in the river mainstreams (timescale of tens to hundreds of thousands of years). Modern fluxes estimated from gauging data range from 5 to 100 m/Ma (10 to 200 t/km2/yr); our calculations indicate that the usual relative contribution of chemical versus physical denudation is 60% and 40%, respectively, of the total denudation. Beryllium‐10 denudation rates and sediment fluxes range from 4.8 to 40.3 m/Ma or 13 to 109 t/km2/yr, respectively, after correction for quartz enrichment. These fluxes are slightly less than the modern fluxes observed in Cameroon and other stable tropical areas. The highest 10Be‐derived fluxes and the highest physical versus chemical denudation ratios are attributed to anthropogenic impact. Copyright © 2016 John Wiley & Sons, Ltd.
Title: Denudation rates on cratonic landscapes: comparison between suspended and dissolved fluxes, and 10Be analysis in the Nyong and Sanaga River basins, south Cameroon
Description:
AbstractSouth Cameroon is located in a tropical and tectonically quiescent region, with landscapes characterized by thick highly weathered regolith, indicative of the long‐term predominance of chemical weathering over erosion.
Currently this region undergoes huge changes due to accelerated mutations related to a growing population and economical developments with associated needs and increasing pressures on land and natural resources.
We analysed two of the main south Cameroon rivers: the Nyong River and Sanaga River.
The Sanaga catchment undergoes a contrasted tropical climate from sub‐humid mountainous and humid climate and is impacted by deforestation, agriculture, damming, mining and urbanization, especially in the Mbam sub‐basin, draining the highly populated volcanic highlands.
By contrast, the Nyong catchment, only under humid tropical climate, is preserved from anthropogenic disturbance with low population except in the region of Yaoundé (Méfou sub‐basin).
Moreover the Nyong basin is dam‐free and less impacted by agriculture and logging.
We explore both denudation temporal variability and the ratio between chemical and physical denudation through two catchment‐averaged erosion and denudation datasets.
The first one consists of an 11‐year long gauging dataset, while the second one comes from cosmogenic radionuclides [CRNs, here beryllium‐10 (10Be)] from sand sampled in the river mainstreams (timescale of tens to hundreds of thousands of years).
Modern fluxes estimated from gauging data range from 5 to 100 m/Ma (10 to 200 t/km2/yr); our calculations indicate that the usual relative contribution of chemical versus physical denudation is 60% and 40%, respectively, of the total denudation.
Beryllium‐10 denudation rates and sediment fluxes range from 4.
8 to 40.
3 m/Ma or 13 to 109 t/km2/yr, respectively, after correction for quartz enrichment.
These fluxes are slightly less than the modern fluxes observed in Cameroon and other stable tropical areas.
The highest 10Be‐derived fluxes and the highest physical versus chemical denudation ratios are attributed to anthropogenic impact.
Copyright © 2016 John Wiley & Sons, Ltd.

Related Results

On the Rock-basins in the Granite of the Dartmoor District, Devonshire
On the Rock-basins in the Granite of the Dartmoor District, Devonshire
In this Memoir the origin of Rock-basins in the Granite of Dartmoor and its vicinity is alone considered; and it is not attempted to draw therefrom any law as to the manner of the ...
Millennial-scale denudation rates in the Himalaya of Far Western Nepal
Millennial-scale denudation rates in the Himalaya of Far Western Nepal
Abstract. The Himalayas stretch ∼3000 km along the Indo-Eurasian plate boundary. Along-strike variations in the fault geometry of the Main Himalayan Thrust (MHT) have given rise to...
Hot-spots Clusters of HIV Infection in Cameroon: Space-time Analysis from the Demographic and Health Surveys
Hot-spots Clusters of HIV Infection in Cameroon: Space-time Analysis from the Demographic and Health Surveys
Abstract Background : The Human Immunodeficiency Virus(HIV) infection prevalence in Cameroon has consecutively decreased from 5.28% in 2004 to 2.8% in 2018. However , this ...
The Multiscale TROPIcal CatchmentS critical zone observatory M‐TROPICS dataset I: The Nyong River Basin, Cameroon
The Multiscale TROPIcal CatchmentS critical zone observatory M‐TROPICS dataset I: The Nyong River Basin, Cameroon
AbstractSimultaneously acquiring time series of climate, hydrology and hydrochemical data over decades on river systems is pivotal to understand the complex interactions involving ...
Millennial-scale denudation rates in the Himalaya of Far Western Nepal
Millennial-scale denudation rates in the Himalaya of Far Western Nepal
Abstract. Over the past two decades, rates and patterns of Himalayan denudation have been documented through numerous cosmogenic nuclide measurements in central and eastern Nepal, ...
Structural Geomorphology and Tectonic Dynamism of the Lolodorf Segment, Nyong Complex, SW Cameroon
Structural Geomorphology and Tectonic Dynamism of the Lolodorf Segment, Nyong Complex, SW Cameroon
The study of the structural geomorphology and tectonic dynamism of the Lokoundjé and Nyong watersheds has made possible to discriminate the essential geological objects of the Lolo...
LANDSCAPES OF THE DZHURYN AND HNIZNA SMALL RIVER BASINS IN THE CONTEXT OF ANTHROPOGENIC TRANSFORMATIONS
LANDSCAPES OF THE DZHURYN AND HNIZNA SMALL RIVER BASINS IN THE CONTEXT OF ANTHROPOGENIC TRANSFORMATIONS
The scientific approach to the analysis of anthropogenic changes and transformations of landscape systems of small river basins of Western Podillia (on the example of the Dzhuryn a...
10Be Concentrations in Antarctic Ice
10Be Concentrations in Antarctic Ice
Measurements of the cosmogenic isotope 10Be (T½ = 1.5 Ma) on Greenland ice cores produced interesting results. Variations in the 10Be concentrations can be interpreted in terms of ...

Back to Top