Botanica Marina Diatoms from the Vaal Dam Catchment Area
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I P Sonderdruck aus Botanica Marina Walter de Gruyter & Co., Berlin 30 Botanica Marina Vol. XIV, S. 17—70, 1971 Diatoms from the Vaal Dam Catchment Area Transvaal, South Africa R. B. M. ARCHIBALD (Co.ancilfor Scientific and Industrial Research; .Nktional Institute for Water Research, Grahanistows, South Africa) (Received 22. 5. 1970) The Vaal Dam is of great importance to South Africa as tributaries above the confluence of the Klip and Vaal it ensures a good supply of water to the Witwatersrand Rivers; the Waterval River System included the Water complex, South Africa’s most important industrial and val River and its tributaries together with the lower parts mining centre, and the problem of pollution and pro of the Vaal River; and finally the Wilge River System tection of the waters flowing into this dam is therefore comprising the Wilge River and all its tributaries. of very great significance. Consequently, in 1955 the The material for the investigation was collected on a “Special Sub-committee on Stream Surveys in the Wit number of different occasions by Dr. B. J. CHOLNOKY, watersrand” (organised by the National Institute for Dr. F. M. CHUTTER and the author. In July 1957 and Water Research) recommended that a survey of the Vaal July 1958 a series of samples, numbered in the range Dam Catchment Area should be undertaken (MALAN Vaal 200—299, were collected by CHOLNOKY from die 1960: 1). The objects of this survey were to gather back Wilge River System. During die entire period of the ground knowledge of die conditions in this area, and survey, i. e. from 1958 to 1960, CHUTTER made irregular to study the factors that affect the quality of the water in collections of a large number of diatom samples from the rivers and streams running into the Vaal Dam. his sampling stations (CHUI’rER 1967: 57, Table 11 and Subsequently MALAN (1960) undertook a survey of the Fig. 9); these samples were numbered in the series Vanl area with regard to the chemical quality of the surface 300—399. In August 1960 CH0LNOKY made a further waters of the catchment area. In his report on this sur collection of samples, Vaal 400—-499, from the Vaal, vey MALAN recommended that from a biological point of Klip and Waterval River Systems. Finally the author, view,,the flora and fauna of the main river systems should while on a trip round die catchment area, made a small be evaluated with a view to assessing pollution effects collection of diatom material (Vaal 500 onwards) of accurately and determining the effects of changing in which only a few were examined and analysed. dustrial and agricultural activity”. In fulfilment of this The distribution of the sampling points is shown on recommendation CHUTTER (1967) completed the studies Map 1. The numbers enclosed within a square refer to on die fauna of the catchment area, and this report is CHirrmR’s sampling stations (Cuorma 1967: Fig. 9), and presented as a contribution towards the survey of the the numbers written alongside them refer to the samples Vaal Dam Catchment Area. collected at that point. Sampling points, which did not The catchment area of the Vaal Dam covers an area of coincide with any of CHUTTER’s stations, are indicated approximately 38.000 square kilometers to the south and by a black dot next to which die sample numbers collect south-east of Johannesburg, and is a large, relatively ed at that point are noted. In the text any sampling point shallow basin. The greater part of the catchment area designated “Station” refers to CHUTTER’s sampling is flat, gently undulating grassland lying at an altitude of stations. between 1300 and 1580 meters above sea level (CHUnER In the list below, brief descriptions of the samples, 1967: 47). The highest ground lies in the south where the sampling stations and sampling points are given. Elands River rises on the northern slopes of Mont-aux Vaal 203 — A large river near the Witzieshoek Reserve Sources in the Drakensberg. The catchment area con on the road from Kestell to Witzieshoek. 24. 7. 57. sists of two main water courses (see Map 1), the Vaal Vaal 204 — A swiftly flowing river nearer to the Witzies River and its tributaries draining the more easterly re hoek Reserve. 24. 7. 57. gions of the catchment area, and the Wilge River drain Vaal 231 — The Wilge River at Frankfort. Station 13 of ing the more westerly regions. For convenience the CHUTTER. 11.7.58. catchment area was divided into four river systems, which are referred to in the text as the Vaal River System, the Vaal 233 — The Wilge River south of Frankfort, above Klip River System, the Waterval River System and die the bridge on die Frankfort—Reitz road. 11.7. 58. Wilge River System. The Vaal River System is composed Vaal 236 — A small stream near the village of Tweeling of the Vaal River and its tributaries down to the con on the Frankfort—Reitz road. 11. 7. 58. fluence of the Klip River just below Standerton; die Vaal 237 — Another small river south of Tweeling on Klip River System embraced the Klip River and its the Tweeling—Reitz road. 11.7. 58. &tanica Marina / Vol. XIV / 1971 / Suppi. I. is Archibald: Diatoms from the Vaal Dam Catchment Area, Transvaal, South Africa LLI~!!I~!? ‘P Scale 01 MileS. The Scimpting Points and Stations of the VoaL Dam Catchment Area. Botanica Msrina / Vol. XIV / 1971 / Sup Archibald: Diatoms from the Vaal Dam Catchment Area, Transvaal, South Africa 19 Vaal 238 — A large river about 5 km north of Reitz on Vaal 325 — The Waterval River where it is crossed by the Tweeing—Reitz road. 11.7. 58. the Balfour—Standerton road. Station 7 of CHUTTER. Vaal 239 — The Liebenbergsvlei River between Beth 10. 9. 59. lehem and Reitz. 11. 7. 58. Vaal 326 — The Sandspruit stream at Sandspruit on the Vaa1240— A marshy river about l6kmfromKestell on national road from Standerton to Volksrust. Station 8 of the Kestell—Bethlehern road. This is probably the CHUTTER. 16. 9. 58. Tier River. Ice was present on the water surface. Vaal 327 — The headwaters of the Wilge River, where 12. 7. 58. it is crossed by the Harrismith—Colling’s Pass road. Vaal 242 — A large tributary of the As River, about Station 9 of CrWTTER. 15. 10. 58. 24 km east of Bethlehem on the Kestell—Bethlehem Vaal 328 — The same locality as Vaal 327. Stones in road. 12. 7. 58. current. 9. 12. 58. Vaal 245 — A small tributary of the Tier River on the Vaal 330 — The Wilge River at Swinburne. Station 10 Bethlehem — Warden road, near the Sherbrooke Station. of CHUTTER. 17. 9. 58. 12. 7. 58. Vaal 331 — The Wilge River at the bridge at its entrance Vaal 249 — A small spring on the side of the road about to Harrismith. Station hA of CHUTTER. 17. 9. 58. 32 km west of Warden on the Bethlehem—Warden road. Vaal 332 — The Wilge River where it leaves Harri Probably the Russespruit stream. 12. 7. 58. smith. Station 118 of CHUTTER. 17. 9. 58. Vaal 253 — The Holspruit, swiftly flowing, where it is Vaal 333 — The Wilge River a littie below Harrismith. crossed by the Vrede—Warden road. 12. 7. 58. Station I1C of CHUTTER. 14. 10. 58. Vaal 261 — The Seekoeivlei near Memel. 13. 7. 58. Vaal 334 — The Wilge River where it is crossed by the Vaal 266 — The Cornelis River, 29 km south of Memel road from Warden to Harrismith. Station 12 of CHUTmK. on the Memel—Harrismith road. 13. 7. 58. 15. 9. 58. Vaal 301 — The headwaters of the Vaal River between Vaal 335 — The Wilge River at Frankfort. Station 13 of Breyten and Lake Chrissie. Station I of CHUTTER. CHUTTER. 18. 9. 58. 16. 9. 58. Vaal 336 — The Molen River where it is crossed by the Vaal 306 — The Vaal River where it is crossed by the Warden—Harrismith road. Station 14 of CHUTTER. Ermelo—Amsterdam road. Marginal mud. Station 2A of 17. 9. 58. CHUTTER. 22. 7. 59. Vaal 337 — The Waterval River where it is crossed by Vaal 307 — The same locality as Vaal 306. Stones in the Standerton—Leslie road at Roodebank. Stones in Current. 19. 1. 60. current. Station 17 of CHUTTER. 20. 7. 59. Vaal 309 — The Vaal River where it is crossed by the Vaal 338— The same locality as Vaal 337. 22. 9. 59. Morgenzon—Amersfoort road. Station 3 of CHUTTER. Vaal 339 — The same locality as Vaal 337. Stones in 15. 9. 58. current. 19. 1. 60. Vaal 312 — The same locality as Vaal 309. Stones in Vaal 340 — The same locality as Vaal 337. Marginal ve current 23. 9. 59. getation. 19. 1. 60. Vaal 313 — The Vaal River at Standerton. Below the Vaal 342 — The Kafflrspruit stream where it is crossed creamery effluent. Station 4 of CHUTTER. 15. 9. 58. by the Morgenzon—Ermelo road. Station 19 of CHUT Vaal 315 — The same locality as Vaal 313. Stones in TER. 15. 9. 58. current. 22. 9. 59. Vaal 343 — The same locality as Vaal 342. Stones in Vaal 316 .—. The same locality as Vaal 313. Stones in current. 22. 7. 59. current. 19. 1. 60. Vaal 344 — The same locality as Vaal 342. 20. 1. 60. Vaal 317 — The Vaal River below Station 4, below the Sewage Works at Standerton. Station 5 of CHUTTER. Vaal 345 — From a seepage on a bank of a headwaters 15. 9. 58. tributary of the Kleinvaal River.