Natural mechanisms of erosion prevention and stabilisation in a Marakele Peatland ; implications for conservation management

The Matlabas mire, an actively peat accumulating wetland, is located in the headwaters of the Matlabas River, Marakele National Park, Limpopo Province, South Africa. Various seepage zones and artesian peat domes are contained in this peatland that consists of two tributaries of which the western one is partially channelled. The occurrence of decaying peat domes and desiccated areas with terrestrial vegetation, as well as the apparent erosion on the western tributary, have raised concerns on the health of this wetland. A network of piezometers was installed in the mire and results confirm that the system is fed primarily from seepage from the slopes of the catchment. Chemical analysis and temperature recorded indicate an isolated groundwater source of which the water does not mix with surface water. This is linked with isotope analysis of the age of peat in various sections of the mire. Erosion was attributed to anthropogenic changes in the catchment. Management recommendations include rehabilitation and reinstating the driving forces that support the mire.Environmental SciencesM. Sc. (Environmental Management

In search of spring mires in Namibia:The Waterberg area revisited

The scarcity of peatlands and mires in Namibia is well known. Peatlands have been found in the north, which is the wettest part of the country. In the 1930s, spring mires were reported by German geologists in the Waterberg area, which also has relatively high annual precipitation. This short note reports some field observations and a literature search for old documents that mention the occurrence of springs and spring mires in the Waterberg region. The search was done by IMCG members who visited the Waterberg area in August 2014. We found springs, but no real mires. However, we found remnants of what might have been a large spring mire similar to that reported by the German geologist Paul Range, who found “local spring mires (Quellmoore) with a peat thickness of several metres in northern South-West Africa”. Whether or not our peat remnants were situated at the same site as the Range discovery could not be assessed. We compared the landscape position of the peat remnants and spring in the Waterberg area of Namibia with information from an ongoing ecohydrological study in the Waterberg area of Limpopo Province, South Africa

In search of spring mires in Namibia:The Waterberg area revisited

The scarcity of peatlands and mires in Namibia is well known. Peatlands have been found in the north, which is the wettest part of the country. In the 1930s, spring mires were reported by German geologists in the Waterberg area, which also has relatively high annual precipitation. This short note reports some field observations and a literature search for old documents that mention the occurrence of springs and spring mires in the Waterberg region. The search was done by IMCG members who visited the Waterberg area in August 2014. We found springs, but no real mires. However, we found remnants of what might have been a large spring mire similar to that reported by the German geologist Paul Range, who found “local spring mires (Quellmoore) with a peat thickness of several metres in northern South-West Africa”. Whether or not our peat remnants were situated at the same site as the Range discovery could not be assessed. We compared the landscape position of the peat remnants and spring in the Waterberg area of Namibia with information from an ongoing ecohydrological study in the Waterberg area of Limpopo Province, South Africa

Anthropogenic disturbances of natural ecohydrological processes in the Matlabas mountain mire, South Africa

Matlabas is a mountain mire in Marakele National Park, located within the headwaters of the Limpopo River in South Africa. This mire consists of a complex of valley-bottom and seepage wetlands with small elevated peat domes. The occurrence of one decaying peat dome, which has burnt, and desiccated wetland areas with terrestrial vegetation has raised concerns. The aim of this study was to understand the mire features and water flows in order to identify the potential drivers causing wetland degradation. Wells and piezometers were installed to monitor the hydraulic head and collect water samples for analysis of ion composition, 18O and 2H stable isotope content, and δ13C and 14C isotope content for radiocarbon dating. Moreover, peat temperature profiles were measured and peat deposits were also dated using radiocarbon. Results indicate that the Matlabas mire developed in the lowest central-east side of the valley by paludification at the onset of the Holocene. During the Mid-Holocene, peat development was extended laterally by autogenic and allogenic processes. Three types of water flows driving peat development were identified – sheet flow, phreatic groundwater flow and deep groundwater flow – two of which are surface or near surface flows. The recent occurrence of decaying peat domes and desiccated wetland areas is possibly related to loss of exfiltrating deep groundwater flows that have resulted from drainage by the head-cut channels in the mire and interception of near surface water flow by an access road, respectively. Interventions should be undertaken to prevent further degradation of the mire. Significance: • This study is the first, as far as we are aware, on the ecohydrology of an inland mountainous mire in southern Africa. • The results highlight the importance of the current wetland management (including rehabilitation) initiatives in South Africa. • The integrative ecohydrological methods can be applied in other headwater wetlands in southern Africa