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Grahamstown rocks!

Who would have thought that some of those awe inspiring creatures, that we usually see on television in movies like Juraissic Park, used to live on your doorstep. Their remains can actually be found right here. Yes I am talking about dinosaurs and other fossilised organisms which have held scientists and other peoples' curiosity since the first fossil was discovered. Locally the first fossil  -  a dinosaur - was found in the Bushmans River Valley near Dassieklip, Eastern Cape in the year 1845. This discovery was made by Dr. W.G Atherstone and Mr. A.G Bain while on a holiday excursion for the purpose of geological exploration with their children.

What Grahamstown is really famous for is fossil plants. In this project we will be looking at the whole process of how fossils are made and which ones are found in Grahamstown.

1. What is a Fossil?

The word fossil refers to the physical evidence of life from a period of time before human history (i.e. prehistoric). Fossilised remains of living organisms include moulds of their physical forms and trails left behind in sediment by their activities.

Our prehistoric human ancestry and the ice age age fauna like mammoths as well as other ancient groups such as the dinosaurs, ammonities and trilobites are all termed fossils.

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2. Interview with Dr De Klerk, Albany Natural History Museum.

On Tuesday the 28th of February Chantelle May and I, Vivienne Dames from Victoria Girls High had the pleasure of interview Dr De Klerk and spending the afternoon with him. Palaeontology is an area which we are both fascinated in and it was truly an amazing experience to delve into it deeper and we would like to thank Dr De Klerk for taking the time in his busy schedule to be so hospitable. 

Questions and Answers
Q1) How has the field of Palaeontology changed since you have become involved in it?
A1) Since I have been here, South Africa has always had an International edge in Palaeontology of all kinds. In 2005 especially is was identified as one of the Five Areas of Excellence along with Clear Skies, Coelacanth project and the Cape Floral Kingdom. Palaeontology gave South Africa something to be significantly proud of, it saddens me to say to you that in recent times the provincial level of funding is slowly beginning to dissipate and it is becoming increasingly difficult to sustain and maintain Palaeontology. Slowly we are heading into a national crisis because there is no succession plan, the youth need to provide us with a new generation of palaeontologist, and this is how we can save this area of excellence in our country. 
Q2) What other fields of science have you had to interact with because of palaeontology?
A2) I interact largely with the department of Geology. Not many people know this but there are several facets of this field and each is unique for example Ichnology is the study of trace fossils, Vertebrate Palaeontology (study of vertebrate fossils) which is what I am involved in, Geochronology which looks at geological time and tafonomy which is the study of the process of fossilisation. I have dealt with all these areas and more, and each one has its own fascinating methods and discoveries. In Palaeontology you will most definitely engage with more than one area and that’s what keeps it interesting.
Q3) How have paleontological discoveries changed and adapted our understanding of a life ‘before man’?
A3) In palaeontology each individual fossil gives an insight into that animal, which links into taxonomy, it’s amazing how you can tell a whole story of how this animal came to be fossilised, where it lived and how it lived. This gives us a detailed backbone for evolution; with this we can trace the origins of not only the organisms that surround us today but humans as well. 
Q4) Where is Palaeontology heading to in the near future?
A4) I hate to paint a bleak picture but in South Africa I fear it is getting weaker, I am glad to say though that on National Level things might be changing for the better. Nationally, people are noticing the crisis and organising solutions. As I said before, on a provincial level we are heading for a crisis but we hope that will change. Things at the moment are hard, but we can save it by investing not only funds but also new scientist that are currently out there amongst the youth.
Q5) Is there an order and classification in fossil records?
A5) Yes, we use the Biological Linnaean System, which is binominal meaning that is counts for both extinct and extant organisms. Taxonomy is a large part of palaeontology; it is with taxonomy that we can describe each fossil that we find.
Q6) How old is the oldest fossil found in Grahamstown?
A6) 360 Million Years old this is the age for both vertebrate and invertebrate fossils that we have found in our region. This period of time is known as the Devonian Period, these fossils have showed that all those years ago this area would of actually be an estuary which is very different to what it is today.
Q7) What is the biggest discovery of fossils found in Grahamstown?
A7) A few years ago we had the N2 Bypass Road cuttings, which was a huge discovery. When they were constructing the N2 road which we have now, they had to cut through a lot of sedimentary hills which turned out to be fossil bearing. There was a large operation to try save as much of those fossils as possible, and it was here that we discovered a mass of different types and periods of fossils which gave us extensive insight into the geological history of Grahamstown.

After all the time we spent with Dr De Klerk at the Albany Museum where he works, we were moved by his passion and excitement in the work that he does even after all these years. We would like to highlight the diversity of the field of Palaeontology and just how much we have relied on it in our lives, this is why we as the youth of today would like all those interested to follow through with Palaeontology so that we as a country can still say that this is an area of excellence.

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3. How are Fossils formed?

The word fossilisation refers to many complicated processes that preserve organic remains within the geographical record. Fossilisation only occurs under the following conditions: when the burial is fast and permanent - protecting the organism from enviromental disturbance- e.g. sinking in mud or being buried in a sand storm; the lack of oxygen limits the extent of decaying; it only occurs on sedimentary rocks and only hard parts like bones and teeth are preserved; and there must be no heating or compression otherwise the organism will be destroyed.

Fossils are often formed in sediments deposited beneath water because the conditions mentioned above occur more frequently in these environments, and of course 70% of the Earth is covered in water. After a long time as the body starts to decay, water containing mineral salts infuses  into the bones and the minerals replace the chemicals in the bones. This is called mineralisation. This whole process results in a rock-like copy of the original object.

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4. How do we know the age of Fossils?

There are many ways of dating fossils and almost all of them are pretty straight forward. The oldest existing method is called stratigraphy, basically it is studying how deeply a fossil is buried. The sedimentary rock layers are formed on top of older layers, pressurizing them into rocks. Paleontologists are able to estimate the period of time that has passed since the stratum containing the fossil was formed. The deeper the fossil is in the rock the older it is. Another common method of dating fossils and rocks is radiometric dating.

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by: Soqhama Peter
on: 2012-03-20 07:57:38