scholarly journals The physical environment and major plant communities of the Tankwa- Karoo National Park

Koedoe ◽  
1998 ◽  
Vol 41 (2) ◽  
Author(s):  
Francine Rubin

Apart from Acocks (1988) there are no published descriptions of the vegetation of the greater Tanqua and Doring River drainage basin (Bayer et al. 1993). A botanical and physical description of the Tankwa- Karoo National Park (TKRNP) which occurs in Veldtype 31b (Acocks 1988) is provided. The three dominant geological formations, older glacigenic deposits of the Dwyka Group, followed by the succession of siliciclas- tic sediments of the Permian Ecca Group, with flat dolerite sills and dykes, underlie eight distinct plant communities. The plant communities can be divided into large open plains dominated by Galenia africana and Tripteris sp. in the erosion rills, Malephora luteola and Augea capensis common in the low lying areas and Zygophyllum microcarpum, Brownanthus ciliatus and Galenia crystallina common on the more shaly concave plains and low shale hills. Slightly elevated rocky areas are dominated by Ruschia cf. robusta, Ruschia spinosa communities, while crusts of stemless mesembs such as Rhinephyllum macra denium, Hereroa fimbriata and Cheiridopsis acuminata are found on the desert paved areas. Annual Asteraceae covers all the denuded and sparsely vegetated areas after good winter rains while annual mesembs colonise on the more sodic sites. A total of 259 plant species were collected sporadically over a period of eight years, this includes 65 succulents and seven species endemic to the Tanqua Karoo and immediate adjacent area of the Roggeveld Mountain Range and Sutherland. Four Tanqua Karoo endemic species were found in the park.

2014 ◽  
Vol 3 (1) ◽  
pp. 32-40
Author(s):  
Kinga Mazurek

Abstract The area of the Upper Silesian Coal Basin is the most important underground mining district in Poland. Coal mines, operating in the area since the eighteenth century, have contributed to massive transformations of the landscape structure. River valleys within range of intensive exploitation activities have been undergoing vast changes. The Slepiotka River drainage basin constitutes an interesting regional example of transformations in the river's watercourse as well as in its adjacent area. It is a left-hand tributary of the Klodnica River with a length of about 8.6 km. Changes in the landscape structure that occurred between 1824-1993 have been analyzed. The starting material consisted of topographical maps that were digitized and calibrated and served as a basis to create colorful compositions. The areas occupied by the different land cover types have been calculated, which allowed to determine their participation in the drainage basin. In about 169 years, significant changes took place in the area of research considering the share of different types of cover and land use. During this time, the river changed its course, both naturally and by human activities. Increasing urbanization and technological development contributed to the diametrical transformation of the landscape structure in the discussed area


2020 ◽  
Vol 12 (1) ◽  
pp. 50
Author(s):  
Eric Clausen

Detailed topographic maps are used to identify and briefly describe named (and a few unnamed) mountain passes crossing high elevation east-west continental divide segments encircling south- and southwest-oriented Colorado River headwaters and linking the Colorado River drainage basin (draining to the Pacific Ocean) with the North and South Platte River drainage basins (draining to the Platte, Missouri, and Mississippi Rivers and Gulf of Mexico). Previous researchers following commonly accepted geomorphology paradigm rules have not explained how most, if any of these mountain passes originated. A recently proposed geomorphology paradigm requires all Missouri River drainage basin valleys to have eroded headward across massive south- and southeast-oriented floods, which implies south- and southeast-oriented floods flowed from what are today north-oriented North Platte River headwaters across the continental divide, the present-day south- and southwest-oriented Colorado River headwaters valley, and then across what is now the continental divide a second time to reach east- and southeast-oriented South Platte River headwaters. Paradigms are rules determining how a scientific discipline governs its research and by themselves are neither correct nor incorrect and are judged on their ability to explain observed evidence. From the new paradigm perspective, a stream eroded each of the passes into a rising mountain range until the uplift rate outpaced the erosion rate and forced a flow reversal in what would have been the upstream valley. The passes and the valleys leading in both directions from the continental divide are best explained if diverging and converging south- and southeast-oriented flood flow channels crossed rising mountain ranges. While explaining observed drainage patterns and erosional landforms such an interpretation requires a fundamentally different regional middle and late Cenozoic glacial and geologic history than what previous investigators using the accepted paradigm perspective have described.


Koedoe ◽  
1996 ◽  
Vol 39 (2) ◽  
Author(s):  
Francine Rubin ◽  
A.R. Palmer

The major plant communities of the Karoo National Park are described using the methods of the Zurich-Montpellier school of phytosociology, to assist with the formulation of a management strategy for the park. The vegetation physiognomy consists of Montane Karoo grassy shrublands. Karoo grassy dwarf shrublands. Karoo succulent dwarf shrublands and riparian thicket. Steep elevation and precipitation gradients within the study area have a direct impact on gradients in the vegetation. High elevation (1 800 m), and relatively high rainfall (406 mm) montane grasslands occupy communities dominated by grasses (Merxmuellera disticha, Themeda triandra) and woody species (Diospyros austro-africana, Elytropappus rhinocerotis, Euryops annae, Passerina montana). The increasing aridity away from the escarpment edge in a northerly direction is steep, and Montane Karoo dwarf shrublands replace these mesic communities. Species such as Eriocephalus ericoides, Rosenia oppositifolia and Pteronia tricephala dominate. At lower elevation (800 m) the precipitation is very low (175 mm) and uncertain (coefficient of variation of 78 ). The substrata influence the vegetation, with the sandy substrata of the drainage lines supporting more woody taxa (Acacia karroo, Lycium cinereum) and grasses (Hyparrhenia hirta, Stipagrostis namaquensis, Cenchrus ciliaris). Moving away from the mesic environment of the riparian zone, rapid desiccation occurs and the most xeric communities are encountered, dominated by Stipagrostis obtusa, S. ciliata and Pent-da incana. This document provides descriptions of the general communities and their associated landscape, lithology and soils.


Author(s):  
Dang Hoi Nguyen ◽  
Hung Cuong Dang ◽  
S. I. Kolesnikov ◽  
Trung Dung Ngo ◽  
T. V, Minnikova

Ngoc Linh mountain range with Ngoc Linh peak of 2598m.a.s.l is an important part of forest ecosystems in Central – Highlands, Vietnam. Located on the complex terrain with stable and long-term geological components, the plant communities here contain the diversity and originality of the high mountains and contiguous areas between Central and Central Highlands Vietnam. The study area covers 65571 hectares, of which Ngoc Linh Nature Reserve covers about 40500 hectares, spread over medium and high mountain terrain. Strongly divided terrain has created the richness, diversity, and originality of ecosystems, especially the structure of natural vegetation. The article presents characteristics and differentiation of forest plantations in Ngoc Linh mountain area; study diversity, and conservation value of regional plant diversity resources; analyzing the characteristics and relationships of plants with geographical factors, especially the rules of elevation, slope, terrain direction, soil and drainage capacity of forest land. Comparison of similarities and differences with some other areas of the Central Highlands, especially the communities with the participation of coniferous plants. To implement the scientific content, various methods have been used. Among them are the main methods: Mapping method and Geographic Information Systems, Field survey methods and Phytogeography (Plant Geography) methods. The study results recorded 1128 species of vascular plants, belong to 627 genera, 175 families, 59 orders, 10 classes, 6 divisions. The flora of Ngoc Linh mountainous area fully converges the vascular plants of the plants in Vietnam, in which the species mainly focus on Magnoliophyta. This is the most diverse division with a total of 145 families, 571 genera and 1032 species, accounting for 82,39 % of families, 91,07 % of genera, and 91,48 % of species. The comparison results show that the proportion between sectors in the plants of Ngoc Linh and the plants of Vietnam has the same structure, with quite similar proportions of dominant species group. Accordingly, the absolute advantage of the Magnoliophyta is from 91.48 % and 92.62 % respectively. 80 rare and precious species have been identified in the IUCN Red List and Vietnam’s Red Data Book 2007. There are 189 endemic species of 135 genera of 66 families. In which there are 107 endemic species of Central Vietnam, the rest belong to Vietnam endemic. Some endemic species with high conservation significance is: Panax vietnamense, P. dalatensis, Quercus langbianensis. The rules of distribution according to elevation are shown in the structure of plant communities through species composition and canopy structure of the forest. Accordingly, plant communities have a high diversity with complex structures, including 3–4 layers. At 900 m.a.s.l elevation, in mixed forests, broadleaf trees form multi-dominant and diverse species. From 1000–1500 m.a.s.l, on the mountainside terrain, the dominant vegetation with P. kesiya in the emergent layer. High diversity in forest structure clearly manifests at 2000–2300 m.a.s.l. Plants are strongly differentiated; some places are multi-dominant, and some places are dominant with P. dalatensis. The most diversity of plants is concentrated at an elevation of 2000–2300 m.a.s.l and the number of the most canopy spread from 1500–2000 m.a.s.l. Gymnosperms, especially P. kesiya and P. dalatensis, participate in single dominant and codominance roles in mixed forest communities. There are differences in the distribution of major conifer species forming plant communities in Ngoc Linh mountain range compared to Chu Yang Sin National Park and Bidoup – Nui Ba National Park in Central and South – Central Highlands. Accordingly, in Ngoc Linh, P. dalatensis has a wider distribution area, higher dominance with a clear role in the formation of plant communities at elevations above 2000 m.a.s.l.


Koedoe ◽  
1993 ◽  
Vol 36 (1) ◽  
Author(s):  
C.A. Chappell ◽  
M.A. Brown

A remote sensing technique is applied in the quantification of the aereal involvement and rates of spread of sodic sites in the upper Ripape River drainage basin of the Kruger National Park. The results show changing areas of sodic site erosion over a period of 41 years. Possible cause and effect relationships are not discussed but the magnitude of soil loss suggests that the erosion has progressed at a rate which is in excess of the rate of natural denudation, under the prevailing climatic regime.


Sign in / Sign up

Export Citation Format

Share Document